{"title":"Minerals \u0026 Geological Specimens","description":"\u003cp\u003eNaturally formed minerals, crystals, geological specimens, and rocks — each piece discovered in the field and selected for its character, formation, and material integrity.\u003c\/p\u003e","products":[{"product_id":"natural-raw-blue-celestite-mineral-healing-crystal-cluster-geode","title":"Blue Celestite Crystal Cluster — Pale Sky Blue, Natural Formation, 389g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA blue celestite crystal cluster, 389g — pale sky-blue tabular crystals in natural formation, quietly luminous in a way that changes as you move it through the light. Some minerals seem to hold the color of the sky. Celestite is one of them. At 389g this is a substantial display specimen without losing the delicate, almost weightless appearance that makes celestite so immediately appealing — even though you can feel its presence as soon as you pick it up.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eCelestite (also known as celestine) is a strontium sulfate mineral (SrSO₄) — one of two common strontium minerals found in collections, alongside strontianite (SrCO₃). Both take their element name from Strontian, a village in Scotland where strontium-containing minerals were first studied in the late 18th century. Celestite crystallizes in the orthorhombic system, typically as tabular or prismatic crystals with a vitreous luster. It most commonly forms in sedimentary environments — particularly evaporite sequences, limestone formations, and in association with gypsum, anhydrite, and sulfur deposits. The largest celestite geodes in the world are found near Put-in-Bay, Ohio, where a cave known as Crystal Cave contains enormous celestite crystals up to 18 inches across. The characteristic pale blue to sky blue color of celestite is attributed to trace amounts of rare earth elements or structural color centers; the color can fade with prolonged exposure to direct sunlight. Celestite is moderately soft (Mohs 3–3.5) with good cleavage and somewhat brittle crystal tips — handle with care and pack well for transport. The exact geological locality of this specimen has not been independently verified. Weight: 389g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe name celestite comes from the Latin \u003cem\u003ecaelestis\u003c\/em\u003e — celestial, of the sky. The blue color earned it the name; the name stuck because it fits. Celestite and strontianite are sister minerals — both built from strontium, both named for the same Scottish village, both prized by collectors for the same reasons: unusual chemistry and exceptional visual character. This cluster formed in a sedimentary cavity where strontium-rich fluids slowly deposited crystal after crystal until the formation visible here developed. The pale blue color may fade slightly over time if kept in direct sunlight — display in indirect light to preserve it.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe color and the scale together. At 389g a celestite cluster has real display authority, and the pale blue reads exceptionally well against natural wood, stone, or dark backgrounds. A strong anchor specimen for a mineral collection that values visual character over geological drama. One of the most quietly beautiful minerals in the catalog.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Blue celestite crystal cluster (strontium sulfate, SrSO₄; sedimentary formation; locality not independently verified)\u003cbr\u003eWeight: 389g\u003cbr\u003eHardness: Mohs 3–3.5 — handle with care; crystal tips can be fragile\u003cbr\u003eNote: Color may fade with prolonged direct sunlight exposure — display in indirect light\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural crystal cluster — please review photographs for crystal formation, color, matrix, and natural variation. Examine for fragile areas before handling.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46961411719353,"sku":"6UL93T","price":75.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/997740AE-F1C7-4E3E-A476-69E782CFCDCC.jpg?v=1783191342"},{"product_id":"desert-rose-crystal-wind-sculpted-gypsum-bloom-of-protection-clarity","title":"Desert Rose — Natural Gypsum Crystal Rosette, Sand-Included, 34g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA desert rose, 34g — a natural gypsum crystal rosette shaped in an arid environment, flat crystal blades radiating outward from a central point with sand grains incorporated into the formation. It looks like a flower. It was never alive. That contradiction is part of the fascination: what resembles petals is the record of minerals crystallizing slowly under harsh, dry conditions, gathering sand into the structure as they grew. Mineral. Sand. Time. Together they create something that looks almost botanical while remaining unmistakably geological.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eDesert roses are rosette-shaped mineral aggregates that form through evaporite processes in arid or semi-arid sedimentary environments. Most are composed of gypsum (CaSO₄·2H₂O, calcium sulfate dihydrate), though barite desert roses also occur. Gypsum desert roses form when mineral-saturated groundwater or brine wicks upward through loose desert sediment by capillary action and then evaporates at or near the surface. As the water evaporates, dissolved calcium and sulfate ions precipitate as gypsum crystals. The crystals grow in a radiating, lenticular (lens-shaped) habit — flat blades that intersect and overlap to produce the rosette form. Sand grains present in the surrounding sediment become incorporated into the growing crystals during formation, giving desert roses their characteristic sandy texture and visible inclusions. The exact locality of this specimen has not been independently verified; the formation type is characteristic of desert environments in North Africa (particularly Algeria and Morocco), the American Southwest, and the Persian Gulf region. Gypsum is soft (Mohs 2) — handle with care. This specimen weighs 34g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eNothing grows here, they said. But beneath the sand, the earth disagreed. Crystal gathered around crystal until a flower took shape — one that needed no rain, no sunlight, and no gardener. When the wind finally uncovered it, someone mistook it for a rose. Perhaps that was close enough. The sand inside the formation arrived before the crystal did — it was already there when the gypsum began to precipitate, and the growing crystal simply enclosed it. The flower and the desert are inseparable.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe rosette structure is well-developed and the sand inclusions are visible. At 34g it is a small specimen with a large geological story — the most accessible entry point in the Found in the Field catalog at $10. A natural gift specimen, a desk curiosity, or the starting point for a collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Desert rose (gypsum crystal rosette with sand inclusions; locality not independently verified)\u003cbr\u003eWeight: 34g\u003cbr\u003eHardness: Mohs 2 — handle with care\u003cbr\u003eLocality: Not independently verified (formation type associated with North African and American Southwest desert environments)\u003cbr\u003eCondition: Natural formation — please review photographs for rosette structure, sand inclusions, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980419715257,"sku":"8ULE54","price":10.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0447.jpg?v=1782178805"},{"product_id":"polished-agate-geode-radiant-harmony-stone-of-balance-inner-strength","title":"Polished Agate Geode — Wild Swirling Banding, Druzy Crystal Cavity, Red \u0026 Blue-Grey — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished agate geode freeform — extraordinary swirling banded agate with fluid red-orange, cream, blue-grey, and white layers moving across the face in turbulent, almost painted arcs, with a small open druzy quartz crystal cavity at the center. From the outside, there is little warning. Then the interior catches the light. This is not concentric ring agate. The bands in this specimen move like weather — curved, flowing, crossing one another in ways that are difficult to look away from.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis is a polished agate freeform with an open geode cavity — a natural specimen that has been cut to reveal the interior face and polished to bring out the banding detail. Agate is banded chalcedony — microcrystalline quartz (SiO₂) — in which successive layers of silica-rich fluid deposit on the interior walls of a rock cavity over geological time. The classic concentric ring pattern of agate develops when deposition is uniform; the turbulent, swirling banding visible in this specimen develops when fluid flow and deposition conditions within the cavity were irregular, changing direction and pressure during formation. This style of non-concentric, fluid-flow banding is associated with what collectors call wild agate or landscape agate — material in which the banding records complex, irregular fluid dynamics rather than simple layered deposition. The red-orange color is from iron oxide (hematite\/goethite), the blue-grey from manganese oxide or inclusion-bearing silica, and the cream from relatively pure chalcedony. The small open cavity at the center is the geode element: the space where the available silica was exhausted before the cavity was fully filled, leaving a pocket lined with small druzy quartz crystals. The exact geological locality has not been independently verified. Weight: [CONFIRM — please weigh and update].\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eMost agate builds itself in orderly rings — each band the record of one depositional phase, concentric and legible. This specimen didn’t. The fluid that carried the silica moved through this cavity under conditions that kept changing — direction, pressure, chemistry, timing. Each band is a record of a different moment in that process, laid down in a different direction, at a different rate, carrying a different mineral load. The result is something that looks less like geology and more like motion caught in stone. The open crystal cavity at the center is where the story ended: the silica ran out, and what remained of the space filled with quartz crystals instead.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe banding on this specimen is exceptional — the fluid, turbulent movement of the red-orange and blue-grey layers across the cream ground is the kind of natural patterning that makes agate collectors stop mid-sentence. Displayed on a stone block stand (visible in photographs — please confirm whether included). One of the strongest visual specimens in the Found in the Field catalog. Worth reviewing the price against comparable wild agate freeforms before publishing.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Polished agate geode freeform (wild\/turbulent banded chalcedony with open druzy quartz cavity — locality not independently verified)\u003cbr\u003eWeight: [CONFIRM — please weigh and update]\u003cbr\u003eDisplay stand: Shown in photographs — please confirm whether included\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished face, natural edges — please review photographs for banding pattern, color, cavity, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980419748025,"sku":"DULE82","price":40.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/BE939C87-BCE3-408F-903E-DA10FACAA553.jpg?v=1783191252"},{"product_id":"purple-fluorite-polished-tower-point-clarity-spiritual-focus-stone","title":"Purple Fluorite Tower Point — Polished Lapidary, Color-Zoned Violet, Natural Mineral — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA purple fluorite tower point — polished and shaped from natural fluorite with violet coloration that shifts character as the light moves across it. Purple tones can appear soft and translucent or deep and saturated depending on illumination and viewing angle. The tower form is human-made; the color, internal structure, and mineral character are natural features of the fluorite. A simple display piece that retains the geology of the material it was shaped from.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eFluorite (CaF₂) is a calcium fluoride mineral that crystallizes in the cubic system and occurs in one of the widest color ranges of any mineral — colorless, green, purple, blue, yellow, pink, and multicolored. Purple fluorite derives its color from color centers: lattice defects caused by natural radiation exposure that absorb visible light in the yellow-green range, producing the complementary violet-purple color perceived by the eye. The same mechanism produces blue John fluorite and many blue and violet fluorite varieties. Fluorite is soft (Mohs 4) with perfect octahedral cleavage in four directions — polished fluorite objects must be handled with care, as the cleavage means the material can chip or cleave along internal planes if dropped or struck. Fluorite is also the mineral that gave science the word “fluorescence” — many specimens glow a distinctive blue-violet under shortwave UV light, a property first systematically described and named after fluorite by George Gabriel Stokes in 1852. Whether this individual specimen fluoresces has not been confirmed. This is a lapidary piece: the tower form was cut and polished from a natural fluorite specimen. No independent laboratory analysis has been performed on this individual piece. Weight: [CONFIRM — SKU entry “3.0” may indicate weight; please weigh and update].\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eFluorite has a way of changing character as the light moves across it. The color is real — a radiation-induced lattice defect that the mineral developed over geological time, long before it was ever shaped into a tower. The polishing reveals it; the radiation created it. The tower shape is a contemporary form applied to an ancient material. That combination — a mineral whose color is the record of geological irradiation, shaped into a simple geometric form — is what makes polished fluorite specimens both accessible and genuinely interesting.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe color depth and translucency read well in a tower format — the point concentrates and transmits light differently from the base, creating visual interest across the height of the piece. At $39 this is an accessible lapidary mineral in a display-ready format that works equally well as a specimen, a decorative object, or a desk focal point.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Purple fluorite tower point (polished lapidary — CaF₂, cubic system; color from radiation-induced lattice defects; locality and UV fluorescence not confirmed for this specimen)\u003cbr\u003eHardness: Mohs 4 — handle with care, perfect octahedral cleavage\u003cbr\u003eWeight: [CONFIRM — please weigh and update]\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished lapidary — please review photographs for color, translucency, internal features, and polish.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980419780793,"sku":"PUL8F3","price":39.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/0387E15B-EDC1-43F8-BE14-5809D0644CE3.jpg?v=1783190144"},{"product_id":"lepidolite-with-quartz-fluorite-calm-balance-emotional-healing-crystal","title":"Lepidolite with Quartz or Fluorite — Lavender Micro-Crystal Specimen, 14g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA small mineral specimen, 14g — lavender and purple micro-crystal surface over a yellow-cream and green banded base, with multiple distinct color zones visible in the photograph. Cataloged as lepidolite with an associated mineral identified as quartz or fluorite. The companion mineral is unconfirmed. Some specimens arrive with a complete answer. This one doesn’t — and that is part of what makes it interesting.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis specimen is cataloged as lepidolite with associated quartz or fluorite; no independent mineral analysis has been performed, and the identification is presented as a catalog identification rather than a laboratory-confirmed result. Lepidolite is a lithium-rich mica mineral (K(Li,Al)₃(AlSi)₄O₂₀(OH,F)₄) that typically appears in lavender, lilac, pink, or gray tones and occurs in lithium-rich granitic pegmatite environments, often alongside tourmaline, quartz, feldspar, and fluorite. The lavender surface on this specimen has a micro-crystalline texture; the yellow-cream and green color zones in the base add additional complexity. The multi-zone coloration visible in the photograph is consistent with a fluorite specimen (which commonly shows green, yellow, and purple color banding in the same crystal) or an amethyst\/quartz specimen over a matrix, though the exact composition requires testing to confirm. The “quartz or fluorite” uncertainty is genuine and noted here because we will not describe material we cannot confirm. This specimen weighs 14g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eLepidolite was one of the original sources of lithium when the element was first isolated in the early 19th century — the mineral’s name derives from the Greek \u003cem\u003elepidos\u003c\/em\u003e (scale), referencing its characteristic scaly mica texture. Lithium, now familiar as the material in modern batteries, was named in 1817 by Johan August Arfwedson, who isolated it from petalite — another lithium silicate mineral that occurs alongside lepidolite in pegmatite environments. The lavender color of lepidolite comes from trace manganese. This small specimen carries that history regardless of what the secondary mineral ultimately proves to be.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe color zoning is visually striking for a 14g specimen — the lavender surface against the yellow-cream and green base makes it more complex-looking than its size suggests. An accessible entry-point collector mineral at $25, with the honest uncertainty about the secondary mineral left open. A collector with access to mineralogical testing tools might enjoy resolving the question.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Lepidolite with associated quartz or fluorite (catalog identification; secondary mineral not independently confirmed; visual characteristics noted in description)\u003cbr\u003eWeight: 14g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural specimen — please review photographs for color zoning, lavender surface, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980419846329,"sku":"KULE6J","price":25.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/C5D6002B-77E8-4DC1-A672-FFB5283C0954.jpg?v=1783189976"},{"product_id":"selenite-crystal-slab-cleansing-light-energy-amplifier","title":"Selenite Gypsum Crystal Specimen — Natural Tabular Crystals, Clear to White, 971g (2.14 lb) — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA selenite gypsum crystal specimen, 971g (2.14 lb) — natural tabular gypsum crystals with flat cleavage faces, clear to white, with the soft luminous quality that makes selenite one of the most immediately recognizable minerals in any collection. Some stones don’t need brilliant color to command attention. This one catches light across its cleavage surfaces, revealing the quiet, glassy character that gypsum develops when it forms large clear crystals. At nearly two and a quarter pounds, it has enough presence to become a genuine display piece.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eSelenite is the clear to translucent crystalline variety of gypsum — calcium sulfate dihydrate (CaSO₄·2H₂O) — distinguished by its well-developed flat cleavage faces, vitreous to pearly luster, and transparency in larger crystals. It is soft (Mohs 2 — can be scratched with a fingernail) and has perfect cleavage in one direction. The name selenite derives from the Greek \u003cem\u003eselene\u003c\/em\u003e (moon), referencing the pearly, moonlike luster of the cleavage faces. Gypsum is a common evaporite mineral that forms in sedimentary environments where saline water evaporates and leaves behind dissolved calcium and sulfate ions. Large selenite crystals can form in caves (the Cave of Crystals in Chihuahua, Mexico contains selenite crystals up to 11 meters long), in desert evaporite deposits, and in hydrothermal veins. Note: many specimens sold in the mineral trade as “selenite” are actually satin spar — the fibrous variety of gypsum with a silky rather than glassy luster. This specimen shows flat cleavage faces and vitreous luster consistent with true selenite rather than satin spar. The exact geological locality has not been independently verified. Weight: 971g \/ 2.14 lb.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe name is from the moon. Selenite was named for the way its cleavage surfaces catch light — a soft, luminous reflection that early mineralogists found lunar in quality. The mineral itself is built from layers: gypsum crystallizes in flat tabular forms, and the cleavage that gives selenite its characteristic faces is a direct expression of the layered crystal structure. The largest selenite crystals ever found — in a flooded cave in Mexico — grew for approximately 500,000 years in hot, mineral-saturated water in complete darkness. These are considerably smaller. But the chemistry is the same.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe scale and the clarity together make this specimen. At 971g selenite has real physical presence, and the flat cleavage faces produce the luminous surface quality that makes the material worth displaying. Works equally well as a mineral specimen, a natural display object, or as part of a crystal collection. Note: gypsum is soft (Mohs 2) — handle with care and keep away from harder objects that could scratch the surface.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Selenite gypsum crystal specimen (clear tabular gypsum; visual identification as selenite rather than satin spar based on cleavage face character; locality not independently verified)\u003cbr\u003eWeight: 971g \/ 2.14 lb\u003cbr\u003eHardness: Mohs 2 — handle with care, scratches easily\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural crystal specimen — please review photographs for cleavage face character, translucency, surface, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980419879097,"sku":"SUL8F5","price":85.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/96D23E59-2A1B-4A46-A028-81B3D2DF327E.jpg?v=1783189784"},{"product_id":"polished-agate-geode-slice-with-druzy-quartz-inner-light-revealed","title":"Polished Agate Geode Slice — Druzy Quartz Interior, Backlit Translucent, 240g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished agate geode slice, 240g — cream and warm tan agate banding on the outer ring, large druzy quartz crystal interior radiating from the center. From a distance, it is simply a slice of stone. Hold it toward a light source and the interior glows: agate chalcedony is semi-translucent, and a thin slice transmits light through the banding in a way that no other display format for this material can match. The druzy center catches the light with hundreds of tiny crystalline faces. The photo shows this effect directly — that is not an editing artifact, that is the material. Display near a window or backlit on a stand for full effect. Stand shown in photographs — please confirm whether stand is included.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eAgate is a variety of banded chalcedony — microcrystalline quartz (SiO₂) — in which silica-rich hydrothermal fluids deposit successive concentric layers on the interior walls of a rock cavity. Each band represents a depositional period; the layering is an analog record of changing fluid chemistry and temperature over geological time. The semi-translucency of agate (chalcedony transmits light better than coarser quartz because the microcrystalline grain size is below the wavelength of visible light, reducing scattering) is what makes polished slices distinctively beautiful when backlit — the banding becomes luminous rather than simply patterned. The druzy interior is the final stage of the geode’s development: after the agate layers filled most of the cavity, the remaining void was too small to support further chalcedony deposition, and quartz crystals grew inward from the agate surface instead, producing the fine sparkle visible in the center. The exact geological locality of this specimen has not been independently verified. This specimen weighs 240g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eLayers trace the slow deposition of mineral material — each band a record of one phase of the geode’s formation, laid down from the outside in. The druzy center is the last chapter: the moment when the cavity ran out of room for banded growth and switched to crystal formation instead. The polished face is a cross-section through all of it — a window into the slow work of stone. The photograph shows the slice backlit, because that is the correct way to look at it. The stone was built to transmit light. Place it where light can reach it.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe photography says it — the backlit translucency of this slice is exceptional and the druzy center creates genuine sparkle within the glowing agate. At 240g it has display presence. Only 3 images in the current listing; additional angles from the front face and close-up of the druzy center would strengthen the listing before publishing. A strong window-display or light-table piece at $65.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Polished agate geode slice with druzy quartz interior (banded chalcedony — locality not independently verified)\u003cbr\u003eWeight: 240g\u003cbr\u003eDisplay stand: Shown in photographs — please confirm whether included\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished slice — please review photographs for banding, druzy formation, translucency, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980419911865,"sku":"AUL8F6","price":65.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/FEB9274A-372F-43D3-9A7C-FA65AFFA3AC9.jpg?v=1783189637"},{"product_id":"green-fluorite-crystal-heart-healing-energy-renewal-stone","title":"Green Fluorite Crystal — Translucent Natural Crystal, Cubic System, 153g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA green fluorite crystal, 153g — translucent natural mineral with the quiet geometry of cubic crystal growth. Green fluorite has a way of looking both solid and almost glass-like at the same time: light moves through the translucent areas while the crystal structure gives the specimen its geometric character. At 153g it has enough presence to stand out in a collection without losing the irregular character of a natural find.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eFluorite (CaF₂) is a calcium fluoride mineral that crystallizes in the cubic system — one of the most geometrically regular crystal systems, producing the characteristic cube, octahedron, and cuboctahedron forms. It is one of the defining minerals on the Mohs hardness scale at Mohs 4, meaning it scratches with a steel knife but not a copper coin. Fluorite occurs in a wide range of colors — colorless, green, purple, blue, yellow, pink — with color produced by trace element substitution and lattice defects (color centers) caused by natural radiation exposure. Green fluorite typically derives its color from trace yttrium, rare earth elements, or radiation-induced color centers. Fluorite has an important historical footnote: the phenomenon of fluorescence — the emission of visible light when exposed to ultraviolet light — was first described and named by George Gabriel Stokes in 1852, and he named it after fluorite, which commonly fluoresces blue-violet under shortwave UV. Many fluorite specimens glow under UV light; whether this individual specimen does has not been confirmed. The exact geological locality has not been independently verified. This specimen weighs 153g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eFluorite gave science the word “fluorescence.” When George Gabriel Stokes was trying to describe what happened to certain minerals under ultraviolet light in the 1850s, he reached for fluorite as his example — it glowed with a blue-violet light that the incoming radiation alone could not explain. The mineral became the name for the phenomenon. There is a satisfying tension in fluorite between precise cubic geometry and the imperfect shape of a natural specimen. The crystal system tends toward cubes; the earth rarely produces perfect ones. This piece preserves that character rather than being reduced to a perfectly uniform decorative object.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe translucency and green color are both strong — fluorite’s glass-like quality is most apparent in transmitted light and this specimen has enough of that character to be worth displaying near a light source. At $20 it is one of the most accessible entry points in the collection. A strong introductory mineral specimen with more geological history than its price suggests.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Green fluorite crystal (calcium fluoride, cubic system — locality not independently verified; UV fluorescence not confirmed for this specimen)\u003cbr\u003eWeight: 153g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural crystal — please review photographs for color, translucency, crystal structure, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420174009,"sku":"FUL8F7","price":20.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0630.jpg?v=1782616629"},{"product_id":"amethyst-crystal-cluster-intuition-protective-spiritual-light","title":"Amethyst Crystal Cluster — Violet Quartz Points, Natural Formation, 894g (1.97 lb) — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA natural amethyst crystal cluster, 894g (1.97 lb) — violet quartz points in natural formation, each termination catching light differently, no two points exactly alike. At nearly two pounds this is a true display piece: the scale gives it a different character from smaller amethyst specimens. A miniature crystalline landscape that preserves a record of slow growth long before it ever reached a collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eAmethyst is the purple to violet variety of quartz (SiO₂). The characteristic color is produced by iron (Fe³⁺) impurities within the quartz crystal lattice combined with natural irradiation from surrounding rock — the iron absorbs visible light in a way that produces the violet color. Heating amethyst above approximately 470°C converts the color to yellow-orange (the process that produces most commercial citrine), which confirms that the color is iron-related and thermally sensitive. Amethyst crystals grow in cavities within volcanic rock — most commonly basalt geodes — where silica-rich hydrothermal fluids slowly deposit quartz. In a cluster, multiple crystals grow simultaneously on a matrix, each competing for space and silica, producing the grouped-point form. The largest amethyst deposits are in Brazil (Rio Grande do Sul) and Uruguay, where basalt flows contain enormous geode cavities lined with amethyst. The exact geological locality of this specimen has not been independently verified. Weight: 894g \/ 1.97 lb.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThere are places beneath the earth where time seems to stop. No wind reaches them. No sunlight. No footsteps. Only mineral-rich water moving slowly through stone, carrying iron and silica in solution. Crystal by crystal, the chamber fills. The violet color develops as iron becomes incorporated into the growing quartz lattice and natural radiation from the surrounding rock alters its oxidation state. When the earth finally gives one of those chambers back, what emerges can look less like a rock than a memory of a place no one was meant to see. Each point in this cluster grew in a different direction, reached a different size, developed a slightly different depth of color. Together they are a record of that hidden chamber.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe scale is the argument. At 894g amethyst clusters are common; at this size they become anchor pieces — the kind of specimen you notice when you walk into a room. The natural formation and point development justify the display weight. A strong entry point for a serious mineral collection or a statement piece for a space that already has one.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Natural amethyst crystal cluster (purple quartz — iron\/irradiation coloration; locality not independently verified)\u003cbr\u003eWeight: 894g \/ 1.97 lb\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural crystal cluster — please review photographs for crystal points, terminations, color, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420206777,"sku":"3ULE3N","price":75.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0249.jpg?v=1782005433"},{"product_id":"calcite-strontianite-crystal-cluster-amplification-divine-alignment-stone","title":"Calcite \u0026 Strontianite Crystal Cluster — Compact Natural Formation, 65g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA calcite and strontianite crystal cluster, 65g — a compact natural formation that works quietly. Some specimens don’t need dramatic color to make you stop. This one rewards the kind of attention most people don’t give rocks. Turn it in your hand and the formation changes. The light catches differently. You start to wonder about the conditions that allowed two minerals to grow together in this particular arrangement, in this particular pocket of the earth. That wondering is the point. That’s always the point.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis specimen is cataloged as a combination of calcite and strontianite — two carbonate minerals that can occur together in the same geological environment. Calcite (CaCO₃) is one of the most common minerals on earth, forming in an enormous range of crystal habits and geological environments — from sedimentary limestone and marble to hydrothermal veins and cave formations. Strontianite (SrCO₃) is a strontium carbonate that occurs as prismatic or acicular crystals, sometimes in radiating or fibrous aggregates, and is considerably less common than calcite. Strontianite was first described in the 1790s from specimens found in Strontian, Scotland — the mineral, and the element strontium, take their name from that locality. The two minerals can co-occur in hydrothermal carbonate veins and mineral-rich sedimentary pockets. No independent mineral analysis has been performed on this individual specimen; the identification is presented as a catalog identification rather than a laboratory-confirmed result. This specimen weighs 65g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eStrontianite was named for a Scottish mining village. The mineral was new to science when it was first described there, and the element it contains — strontium — was named for the same place. The mineral in this cluster is the same compound, formed through the same carbonate chemistry, just in a different geological setting. At 65g this is a desk specimen, a study specimen — the kind of object that earns a second look from anyone who notices it. This cluster formed without any intention of being found. You don’t just buy the object. You become the next part of its story.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe strontianite identification makes this a more unusual collector specimen than a plain calcite cluster — strontianite is significantly less common and less frequently encountered in collections. The compact natural formation records something about the hydrothermal conditions that made it. A strong mineralogy specimen at an accessible price point for what it is.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Calcite \u0026amp; strontianite crystal cluster (carbonate minerals; catalog identification, not lab confirmed)\u003cbr\u003eWeight: 65g\u003cbr\u003eDimensions: [CONFIRM DIMENSIONS]\u003cbr\u003eLocality: Unknown\u003cbr\u003eCondition: Natural crystal surfaces — please review photographs for formation detail and surface variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420239545,"sku":"1ULE37","price":35.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/03FD8222-C724-431A-B377-34245FCE1C01.jpg?v=1782087127"},{"product_id":"septarian-concretion-fossilized-coral-stone-ancient-earth-wisdom-grounding-energy","title":"Septarian Concretion — Large Natural Nodule, Mineral-Filled Fracture Network, 1,324g (2.92 lb) — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA septarian concretion, 1,324g (2.92 lb) — a large natural nodule marked by a network of mineral-filled fractures running through the stone like roads on an ancient map. The cracks are not damage. They are the geological history of the formation — internal fractures that opened as the concretion developed, then filled with mineral-bearing fluids that deposited new material in each crack. At nearly three pounds, this is not a subtle stone.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eSeptarian concretions are a type of sedimentary concretion containing an internal network of cracks (septaria) that formed within the stone and were later filled or lined by minerals — most commonly calcite (yellow to brown), aragonite, or barite, with the outer mudstone or limestone matrix remaining darker. Concretions form through post-depositional cementation in sedimentary environments: mineral-rich pore fluids precipitate around a nucleus (often organic material) in mudrock or limestone, building a rounded nodule. The internal cracking that produces the septaria can form through several mechanisms — burial compaction, dehydration shrinkage during diagenesis, or internal pressure buildup. The characteristic angular to polygonal fracture pattern (from which the name derives: Latin \u003cem\u003eseptum\u003c\/em\u003e, dividing wall) is then filled by successive mineral precipitations from groundwater. The contrasting mineral-filled fractures against the darker matrix give septarian specimens their distinctive appearance. This specimen was previously noted in the catalog as potentially identified as fossilized coral; without independent testing or locality documentation, it is identified here as a septarian concretion based on structural characteristics. The exact locality, geological age, and mineral fill composition have not been independently verified. Weight: 1,324g \/ 2.92 lb.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe finder almost called the cracks flaws. Then they looked again. The lines were too deliberate — crossing the stone like roads on an ancient map, filled with minerals that had arrived long after the first fracture appeared. The stone had not remained whole. It had changed. And somehow, the breaking had become part of its beauty. The septaria in this specimen are a record of stress and response: the concretion cracked under geological pressure, and the cracks immediately began to fill. What looks like damage is actually a second phase of construction — the stone repaired itself in mineral.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe scale and the fracture network together make the case. At 2.92 lb this specimen has real physical authority, and the septarian patterning is clearly developed and visible across the surface. A substantial display piece for a collection that values geological process over surface finish — the interest here is in what happened inside the stone, not to it.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Septarian concretion (sedimentary nodule with mineral-filled fracture network; previously noted as possibly fossilized coral — identified here as septarian based on structural characteristics; not independently laboratory verified)\u003cbr\u003eWeight: 1,324g \/ 2.92 lb\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural specimen — please review photographs for septarian patterning, mineral fill, surface, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420272313,"sku":"SUL8FA","price":100.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/original_8851d971-bf93-4cfd-a8a4-256023a8d52c.jpg?v=1780807637"},{"product_id":"petrified-wood-field-find-0001","title":"Petrified Wood Specimen — Grain Pattern Preserved in Stone, 266g — Field Find #0001","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA petrified wood specimen, 266g — the texture, grain, and organic structure of wood preserved in stone. Not every treasure announces itself. This one was hiding in plain sight in Minnesota — an ordinary-looking stone carrying a history far older than anything around it. At first glance: wood. Then you understand: stone. That contradiction is what makes petrified wood so strange and so compelling. Catalog ID: FITF-0001 — the first entry in the Found in the Field catalog.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003ePetrified wood forms when woody material is buried and protected from ordinary decomposition while mineral-rich groundwater moves slowly through the surrounding sediment. Over geological time, minerals (commonly silica, calcite, or pyrite, depending on conditions) precipitate into the cellular spaces of the wood, gradually replacing and preserving the organic structure as stone. The process can preserve the grain pattern, annual rings, and cellular geometry of the original wood with remarkable fidelity — the result is stone that still carries the visual language of wood. The exact tree species, geological age, mineral composition, and original locality of this specimen have not been independently laboratory verified and are intentionally left unspecified. Acquired: Minnesota. Approximate dimensions: 10 × 8 × 5 cm. This specimen weighs 266g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe forest had been gone for longer than anyone could remember. Not dead — gone. Dead things can be mourned. Gone things become stories. Deep beneath the earth, something remained. Year after year, seasons passed above it. Mountains rose and wore themselves down. People came and disappeared. Still, the old tree remained — not as wood, not as a tree, but as memory made solid. When the stone was finally lifted from the earth, it carried no leaves, no branches, no birdsong. Only the grain remained. Proof that something had once lived there. Proof that time does not always erase. Sometimes — time preserves.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe grain pattern is clearly visible and the suggestion of wood reads immediately — you see it before you understand it. This is the kind of object that makes you stop and look twice: not necessarily the most expensive thing, not necessarily the rarest thing, but something that holds two worlds at once. FITF-0001 is where the Found in the Field catalog began.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Petrified wood specimen (natural; species, age, and mineral composition not independently verified)\u003cbr\u003eCatalog ID: FITF-0001\u003cbr\u003eWeight: 266g\u003cbr\u003eDimensions: Approx. 10 × 8 × 5 cm\u003cbr\u003eAcquired: Minnesota\u003cbr\u003eCondition: Natural specimen — please review photographs for grain pattern, mineral character, and surface variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420337849,"sku":"GULE7N","price":45.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/45E18D6F-75C0-49D5-ACAE-17C01C98E46A.jpg?v=1783189115"},{"product_id":"muscovite-mica-specimen-golden-layered-mica-book","title":"Muscovite Mica Specimen — Golden Layered Mica Book, Natural Crystal Form — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA muscovite mica specimen — warm golden-amber layered mica plates stacked in the characteristic book-like crystal form, multiple faces catching light at different angles simultaneously. Turn it toward the light and it changes. What can look like one surface becomes many: thin layers catching the light while others fall into shadow, the shimmer shifting as the piece moves. A mineral that seems to reveal something new every time the light moves.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eMuscovite is a potassium aluminum sheet silicate mineral — KAl₂(AlSi₃O₂₀)(OH)₂ — and one of the most common members of the mica mineral group. Its defining characteristic is a perfect basal cleavage in one direction, which allows it to split into thin, flexible, transparent to translucent sheets. This cleavage is a direct expression of the crystal structure: muscovite is built from repeating layers of silicate sheets bonded by potassium ions, and the potassium bonds are weaker than the bonds within each silicate layer. The sheets separate where the structure is weakest. The reflective shimmer and pearly luster of muscovite are a consequence of the same structure — light reflects off multiple parallel cleavage surfaces simultaneously, producing the characteristic sparkle. The warm golden-amber color of this specimen reflects iron staining or minor iron substitution in the crystal structure; pure muscovite is colorless to pale silver. Muscovite commonly occurs in metamorphic rocks (schist, phyllite, gneiss) and in granitic pegmatites, where it can form large well-developed crystal books. This specimen has not been independently laboratory verified; identification is based on visual characteristics. Weight: [CONFIRM — original SKU entry of “12.0” may indicate weight in ounces; please confirm].\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe finder thought it was silver. Then the light moved. What looked like one surface became many — layer beneath layer, the stone seemed to hold pages no one had written. The pages are real: each reflective face is a cleavage surface, a plane where the potassium bonds between silicate layers are weaker than the structure on either side. In geological environments where muscovite grows slowly in pegmatite or metamorphic rock, these books can develop over millions of years. The layers are time made physical — some stories aren’t meant to be read all at once.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe golden color and the development of the mica book form are both strong — this specimen photographs exceptionally well because the layered faces each catch light differently. At $65 it is one of the more accessibly priced display minerals in the collection with a genuinely complex structure. A strong mineralogy or crystal structure specimen for a collection that values geological character over surface polish.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Muscovite mica specimen (potassium aluminum sheet silicate; natural crystal form — visual identification; not independently verified)\u003cbr\u003eWeight: [CONFIRM — please weigh and update]\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural raw specimen — please review photographs for layering, luster, golden color, and natural crystal form variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420370617,"sku":"MUL8FC","price":65.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/original_513d3030-e31d-443e-98f9-225ea81ab224.jpg?v=1780807638"},{"product_id":"lake-superior-agate-stone-of-endurance-and-earth-s-fire","title":"Lake Superior Agate — Large Banded Specimen, Iron-Red Chalcedony, 1,288g (2.84 lb) — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA Lake Superior agate — 1,288g (2.84 lb) of banded chalcedony with the iron-red, orange, cream, and brown layering that makes Lake Superior agates among the most recognized and collected regional stones in North America. At nearly three pounds this is an anchor piece: substantial enough to command a shelf, complex enough to reward looking. Layer after layer, the bands record changing conditions during formation. Every line is geological.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eLake Superior agates (LSAs) are banded chalcedony specimens with a specific and well-documented geological origin. They formed approximately 1.1 billion years ago during the Midcontinent Rift — a period of intense volcanic activity when lava flows repeatedly covered what is now the Lake Superior basin. As the lava cooled, gas bubbles created vesicles (cavities) in the basalt. Silica-rich hydrothermal fluids later infiltrated those cavities and deposited successive layers of chalcedony on the cavity walls. The characteristic red, orange, and iron-rich banding of Lake Superior agates is produced by hematite (Fe₂O₃) — iron oxide — incorporated into the silica during deposition. The source of the iron was the surrounding iron-rich basaltic rock. During the Pleistocene (the last ice age), glaciers advancing across the Lake Superior region eroded the volcanic host rock and carried the agates — which are harder and more resistant than the basalt matrix — hundreds of miles from their original formation sites. They are now found in glacial till, gravel bars, and lake beaches across Minnesota, Wisconsin, Michigan, and into Iowa and South Dakota. The exact locality of this individual specimen has not been independently verified. Weight: 1,288g \/ 2.84 lb.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eBefore anyone found it, the stone had already traveled. It had known heat beneath an ancient landscape — basalt cooling around a gas bubble a billion years ago. It had known silica-rich water moving through that bubble over millions of years, depositing one thin layer at a time. Then came the ice. Slowly, the glaciers carried it out of the volcanic rock that formed it and across the landscape, depositing it in gravel when the ice finally retreated. When the glaciers were gone, the agate remained — waiting beside a northern shore for someone to notice the history written inside it. The red comes from iron. The layering comes from time. The weight in the hand is both.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eLake Superior agates are genuinely significant collector stones — regional, geologically documented, and visually distinctive. At 2.84 lb this specimen has the size to stand as a statement piece in a serious collection. The iron-red banding is what defines the material and separates it from generic agate — this is a specimen for collectors who understand the difference. One of the most historically and geologically substantiated pieces in the Found in the Field catalog.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Lake Superior agate (banded hematite-rich chalcedony — regional identification; exact locality not independently verified)\u003cbr\u003eWeight: 1,288g \/ 2.84 lb\u003cbr\u003eLocality: Lake Superior region (Minnesota \/ Wisconsin \/ Michigan \/ glacial deposit; exact locality not independently verified)\u003cbr\u003eCondition: Natural specimen — please review photographs for banding, iron coloration, surface, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420403385,"sku":"8ULE65","price":250.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/4FE83353-C3C2-474D-9184-3B2DFE9BCD7B.jpg?v=1783187107"},{"product_id":"polished-agate-geode-slice-window-into-earth-s-hidden-beauty","title":"Agate Geode Half — Banded Chalcedony \u0026 Quartz Druzy — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003c\/p\u003e\u003cp\u003eAn agate geode half with cream and tan chalcedony banding forming the outer walls and a natural quartz druzy interior. The contrast between the quiet, layered exterior and the crystal-lined opening makes this a good example of how much detail can be hidden inside an ordinary-looking piece of stone.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eDETAILS\u003c\/strong\u003e\u003c\/p\u003e\u003cul\u003e\n\u003cli\u003eMaterial: Agate \/ chalcedony with quartz druzy\u003c\/li\u003e\n\u003cli\u003eForm: Natural geode half\u003c\/li\u003e\n\u003cli\u003eCondition: Natural specimen with polished or cut opening as shown\u003c\/li\u003e\n\u003cli\u003eQuantity: 1\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003e\u003cstrong\u003eSPIRITUAL PROPERTIES \u0026amp; USE\u003c\/strong\u003e\u003c\/p\u003e\u003cp\u003eAgate is traditionally associated with grounding, steadiness, and balance. These traditional associations are offered as part of the folklore surrounding stones and are not medical claims.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420468921,"sku":"3264307","price":50.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/A19C937A-6BE8-4486-A344-A701B484C262.jpg?v=1783186393"},{"product_id":"choya-geode-desert-bloom-crystal-of-hidden-light","title":"Choya Geode — Crystal-Lined Cactus Cavity, Quartz Interior, 382g — Field Find #0018","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA Choya geode, 382g — weathered organic exterior concealing a chamber of sparkling quartz crystal growth inside. From the outside it looks like a piece of desert: rough, quiet, almost ordinary. Then the interior appears. What looks like dried organic material becomes a lined mineral cavity — a remarkable transformation of biological structure into geological specimen. Catalog ID: FITF-0018.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eChoya geodes are unusual because their story begins with biology rather than geology. The term refers to geode-like formations associated with cavities in cholla cactus (Cylindropuntia spp.) — desert cacti of the American Southwest and northern Mexico whose woody skeletons have a distinctive latticed cylindrical structure. When a cholla cactus dies and its organic material decomposes, the woody skeleton can leave a patterned cavity in the surrounding soil or rock material. If mineral-rich groundwater — commonly silica-saturated — later infiltrates that cavity, it can deposit quartz crystals on the interior walls over time, lining the space with crystalline mineral growth. The result is a natural object that is simultaneously organic in outer form (carrying the pattern of the cactus skeleton) and inorganic in interior character (quartz crystal). The exact geological history, age, and crystal composition of this individual specimen have not been independently laboratory verified. This specimen weighs 382g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eFor years, she thought it was only a piece of dried wood. She nearly left it behind. Then it broke open. Inside was a world she could not have imagined from the outside — tiny crystals filled the hollow like stars caught in a forgotten room. The desert had kept a secret. Not because it wanted to hide it. Because some things need time before they become visible. The biological structure that formed the mold for this geode is gone — decomposed long before the mineral filling began. What remains is the impression it left, converted by slow silica deposition into something that will outlast the desert that produced it by geological orders of magnitude.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe contrast is the case — rough, weathered, organic-looking outside; sparkling crystalline interior. Few natural objects carry that tension as clearly as a Choya geode. At 382g it has real display presence, and the biological origin story adds a layer of narrative that purely mineralogical specimens don’t have. One of the most conceptually interesting specimens in the collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Choya geode (crystal-lined cholla cactus cavity; quartz interior — geological history not independently verified)\u003cbr\u003eCatalog ID: FITF-0018\u003cbr\u003eWeight: 382g\u003cbr\u003eLocality: Not independently verified (formation type associated with American Southwest \/ northern Mexico desert environments)\u003cbr\u003eCondition: Natural specimen — please review photographs for outer texture, interior crystal formation, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420534457,"sku":"9ULE2B","price":75.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0394.jpg?v=1782135469"},{"product_id":"thunderegg-hidden-world-stone-of-inner-discovery","title":"Thunderegg Half — Cut \u0026 Polished Interior, White Chalcedony Band, Brown Agate — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA thunderegg, cut and polished to reveal the interior — warm brown chalcedony filling with a dramatic white chalcedony band running diagonally through the center, rough volcanic matrix visible on the outer edge. The exterior promised nothing. The interior kept its story until someone cut it open. This is that moment, preserved.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThundereggs are rounded nodular formations that develop within rhyolitic volcanic rocks — specifically within cavities that form during the cooling and degassing of silica-rich lava flows. After the volcanic rock solidifies, silica-rich hydrothermal fluids infiltrate the cavity and deposit successive layers of chalcedony, agate, quartz, or other silica minerals over geological time. The result is an exterior that looks like an ordinary rounded rock and an interior that can contain intricate mineral patterns, banding, or crystal formations. This specimen has been cut through its equator and one face polished to reveal the interior. The interior shows warm brown chalcedony filling with a distinct white chalcedony band — the color variation between the brown and white material reflects differences in mineral impurity content during different depositional periods. The rough outer matrix is the original volcanic host rock. The exact locality, geological age, and interior mineral composition of this specimen have not been independently laboratory verified. Weight not confirmed — please weigh and update before publishing.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe finder picked it up because it looked ordinary. That was its first trick. Inside, the earth had been writing — layer by layer, patiently, over geological time. When the thunderegg was finally cut open, the stone revealed it had never been empty. It had simply been keeping its story to itself. The white band running through the brown interior of this specimen is a record of a change in fluid chemistry during deposition — at some point the mineralizing fluid shifted composition, and the chalcedony it deposited became paler, whiter, more concentrated. That moment of change is now the most visually striking feature of the piece.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe white band is the case for this specimen — it cuts diagonally through the warm brown interior with enough contrast to read immediately from across a room. The rough volcanic exterior framing the polished interior face creates a strong visual tension between the unworked outer surface and the revealed interior. A substantial display piece with a geological story that begins before it was cut open and ends the moment the interior became visible.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Thunderegg half (cut and polished; chalcedony interior with white band in volcanic matrix — locality and composition not independently verified)\u003cbr\u003eWeight: [CONFIRM WEIGHT]\u003cbr\u003eDimensions: [CONFIRM DIMENSIONS]\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Cut and polished face; rough natural exterior — please review photographs for interior pattern, white band, matrix character, and overall condition.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980420698297,"sku":"816678C","price":69.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/56A14AEA-51AF-4A74-8309-DF0D7C431F8E.jpg?v=1783184552"},{"product_id":"polished-natural-jasper-sphere-stone-of-grounding-and-gentle-strength","title":"Polished Jasper Sphere — Warm Golden Yellow \u0026 Brown, 649g (1.43 lb) — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished jasper sphere, 649g (1.43 lb) — warm golden yellow with irregular brown mottling across a high-gloss surface. A sphere gives the stone nowhere to hide: no obvious beginning or end, just pattern moving continuously around the surface as the piece turns. At this weight it has real physical authority as a display object — substantial enough to anchor a shelf, a desk, or a collection. The color pattern photographs like a small planet.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eJasper is an opaque, iron-rich variety of microcrystalline quartz (chalcedony) in which color and patterning are produced by iron oxide minerals and other impurities distributed through the silica matrix. The warm golden yellow ground is consistent with goethite (hydrated iron oxide, FeO(OH)) coloration, while the brown mottling reflects areas of higher iron oxide concentration or different oxide phases. The irregular, patch-like distribution of colors is characteristic of mottled or map jasper rather than banded jasper — the pattern formed through irregular distribution of impurities during silica consolidation rather than through layered deposition. The exact variety and geological locality of this specimen have not been independently verified. Weight: 649g \/ 1.43 lb. Diameter: [CONFIRM DIAMETER].\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe finder searched for the beginning. They turned the stone once. Then again. Every pattern led somewhere else. There was no first mark. No final one. Only the quiet movement of stone beneath their hands. The sphere is the form that makes this most apparent — an egg has an orientation, a top and a bottom. A sphere refuses that entirely. The pattern on this one moves the way weather moves across a planet — warm yellow ground interrupted by brown irregular masses with no fixed edge and no fixed position. Some things are not meant to have an ending.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe color is warm and the patterning is complex enough to reward looking without being busy. At 649g the sphere has the weight that makes it feel like a serious object rather than a decorative accessory. The planetary quality of the pattern is genuinely striking — this one looks like it belongs in an atlas of undiscovered worlds as much as a mineral collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Polished jasper sphere (mottled microcrystalline quartz; variety and locality not independently verified)\u003cbr\u003eWeight: 649g \/ 1.43 lb\u003cbr\u003eDiameter: [CONFIRM DIAMETER]\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished sphere — please review photographs for color, pattern, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422172857,"sku":"S257637","price":60.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/1D9EE387-3EDF-43FE-9957-78AC68BAF36C.jpg?v=1783184426"},{"product_id":"hornitos-poppy-jasper-stone-of-vitality-and-earth-s-flowing-energy","title":"Hornitos Poppy Jasper — California Locality, Red \u0026 Cream Patterned Chalcedony, 227g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA Hornitos Poppy Jasper specimen, 227g — richly patterned red and cream with rounded, almost botanical markings moving across the surface. At first glance the color catches you. Look longer and the pattern takes over. Red moves into cream. Rounded shapes interrupt the surface. It is easy to understand why collectors gave material like this a name inspired by flowers. Hornitos is the locality. Poppy is what the pattern does to the eye.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003ePoppy Jasper is a collector and trade name for a distinctive variety of jasper with red, cream, and orange rounded patterning associated with material from the Hornitos area of Mariposa County, California. Jasper is an opaque, iron-rich microcrystalline quartz (chalcedony) in which the color and patterning are produced by iron oxide minerals (hematite, goethite) and other impurities distributed through the silica matrix. The rounded “poppy” patterns are characteristic of orb-textured jasper, where spherical or elliptical domains of differently colored silica form during the crystallization process. Hornitos area jasper is a recognized California locality stone with a following among lapidary collectors. The exact individual locality and geological context of this specimen have not been independently verified beyond its existing catalog identification. This specimen weighs 227g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThere had never been a garden there. Yet when the finder turned the stone in their hand, flowers seemed to move across its surface. Not flowers — only mineral, only time. The orb patterns in poppy jasper form during silica crystallization, each rounded domain a record of how the chemistry organized itself in that particular space at that particular moment. The earth makes patterns that memory understands before the mind does. California’s Coast Ranges and Sierra Nevada foothills have produced some of the most distinctive locality jaspers in North America, and the Hornitos material is among the most immediately recognizable.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe pattern is distinctive and clearly developed — the red and cream orb patterning is strong and reads immediately as Poppy Jasper to anyone familiar with the material. At 227g it has real weight and display presence. A strong piece for a California locality collection, a jasper collection, or any display that values pattern over uniformity.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Hornitos Poppy Jasper (orb-patterned chalcedony, California locality trade name; individual locality not independently verified)\u003cbr\u003eWeight: 227g\u003cbr\u003eLocality: Hornitos area, Mariposa County, California (trade identification; not independently verified)\u003cbr\u003eCondition: Natural specimen — please review photographs for pattern, color, surface characteristics, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422205625,"sku":"H138304","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/FFE61117-010E-41DF-8F37-1A22F858FB03.jpg?v=1782619677"},{"product_id":"orthoceras-fossil-egg-ancient-ocean-wisdom-in-stone","title":"Orthoceras Fossil Egg — Paleozoic Cephalopod in Dark Limestone, Polished, 182g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished orthoceras fossil egg, 182g — ancient marine cephalopod fossils preserved in dark limestone, carved and polished into an egg form. Fossil chambers appear as patterns within the stone, small windows into a world that disappeared hundreds of millions of years ago. An ocean had covered the place where the stone eventually formed. The ocean disappeared. The fossil remained. An ancient and extinct thing, given a form traditionally associated with beginnings.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eOrthoceras is a trade name for fossilized orthocerid nautiloids — extinct straight-shelled cephalopods that lived in marine environments during the Paleozoic Era, primarily the Ordovician through Devonian periods (approximately 470–360 million years ago). They were apex predators of their ancient seas, related to modern nautilus and squid. The segmented internal chambers visible in polished specimens are septa — the dividing walls of the shell that the animal used to regulate buoyancy, the same basic mechanism used by modern nautilus. Commercial orthoceras specimens are predominantly sourced from black limestone deposits in the Erfoud\/Msissi region of Morocco, where the fossils are abundant and well-preserved. The exact locality and geological age of this individual specimen have not been independently verified. This specimen is a carved polished object, not an intact natural fossil specimen or an archaeological artifact. This specimen weighs 182g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eLong before there were forests, birds, or people, orthocerid nautiloids moved through ancient seas. The polished surface of this egg turns that vanished ocean into something you can hold. Some beginnings are old enough to look like endings. The egg form adds a quiet contrast that the original description captures well: something ancient and extinct, given a form associated with new starts. The septa visible in the stone are the same buoyancy-regulating chambers that allowed these animals to control their depth in the water column — an engineering solution that modern nautiluses still use, largely unchanged, 450 million years later.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe fossil detail is clearly visible in the polished surface and the dark limestone ground makes the lighter fossil structures read well. At 182g it has solid presence. A strong piece for a fossil collection or any display that values deep time over conventional mineral aesthetics — this egg is older than the dinosaurs.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Orthoceras fossil egg (polished orthocerid nautiloid fossils in dark limestone — “orthoceras” is a trade name; locality and geological age not independently verified)\u003cbr\u003eWeight: 182g\u003cbr\u003eLocality: Not independently verified (commercial orthoceras predominantly from Morocco)\u003cbr\u003eCondition: Polished carved specimen — please review photographs for fossil detail, chamber pattern, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422303929,"sku":"S742521","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/7AD14983-1E2E-4418-B136-BEF1006CC954.jpg?v=1783182711"},{"product_id":"alabaster-stone-egg-gentle-light-of-calm-and-renewal","title":"Alabaster Stone Egg — Warm Golden Tone, Semi-Translucent Veining, 122g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished alabaster stone egg, 122g — warm golden-amber with cream and brown veining and a softly luminous surface. The lighter areas of the stone have a visible semi-translucency, allowing light to pass through in a way that distinguishes this piece from denser opaque stones. Simple in form. Quietly beautiful. The kind of object that earns its place on a shelf without announcement. Photographed on a brass display stand (stand not included).\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eAlabaster is a trade term applied to two distinct minerals: gypsum (CaSO₄·2H₂O, Mohs 2) and calcite (CaCO₃, Mohs 3). Gypsum alabaster is softer, semi-translucent, and takes a smooth waxy polish; calcite alabaster is harder and typically less translucent. The semi-translucent quality visible in this specimen’s lighter areas is more consistent with gypsum alabaster than with calcite or marble, which are typically fully opaque. The warm golden-amber color with irregular cream and brown veining is characteristic of naturally colored gypsum alabaster from deposits in Italy, Spain, and the Middle East, though the exact locality has not been independently verified. Because gypsum alabaster is soft (Mohs 2), it scratches easily and should be kept away from harder surfaces and direct water exposure. The exact mineral composition has not been independently laboratory verified. This specimen weighs 122g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eAlabaster has been carved into decorative objects for thousands of years — Egyptian canopic jars, Mesopotamian palace reliefs, Renaissance devotional objects, and Victorian decorative arts all made use of its workability and luminous surface. The semi-translucency of gypsum alabaster was valued specifically because it allowed light to pass through thin carved sections, creating a glow that opaque stone cannot produce. In egg form, that translucency becomes most visible at the thinner edges and paler areas — the stone holds light differently depending on where you look at it.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe semi-translucency is the case for this piece — the warm golden tone combined with the light-passing quality of the paler veining areas gives it a luminous character that denser stones in the collection don’t have. At 122g it is compact and comfortable in the hand. The appeal is simplicity: a piece of stone, shaped and polished into a form that has carried symbolic meaning for centuries.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Alabaster stone egg (presented as gypsum alabaster based on visual characteristics including semi-translucency; not independently laboratory verified)\u003cbr\u003eWeight: 122g\u003cbr\u003eDisplay stand: Not included — stand shown in photographs is for display purposes only\u003cbr\u003eCare: Gypsum alabaster is soft (Mohs 2) — avoid hard surfaces, scratching, and water exposure\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for color, veining, translucency, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422336697,"sku":"4684113","price":20.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/A18A1E0D-4879-425A-AD14-C0D4BEE9DEE3.jpg?v=1781998590"},{"product_id":"marble-fish-carved-egg-symbol-of-flow-abundance-and-timeless-craft","title":"Black Stone Egg with Engraved Fish — Incised White-Fill Carving, 201g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished black stone egg, 201g, with finely incised fish engraving filled in white — a striped fish with detailed scales and fins occupies most of the surface, a smaller fish visible in the background. Deep black ground, high-gloss polish, skilled line work. Two old symbols meet in one small object: the egg suggesting beginnings and potential; the fish suggesting movement, something alive beneath the surface. Motion preserved in something completely still. Photographed on a brass display stand (stand not included).\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis is a carved decorative stone object rather than a natural mineral specimen. The black stone is presented as marble in the catalog — the deep black glossy surface is consistent with black marble (such as nero marquina or similar black limestone\/marble varieties) though the exact stone type, maker, age, and provenance have not been independently verified. The engraving technique — incised line work with white fill — is a traditional decorative approach used across many stone-carving traditions. The fish motif with detailed striped scales suggests skilled craftsmanship and intentional artistic design rather than a souvenir or mass-produced object. This specimen weighs 201g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eFish have been carved into stone across cultures for thousands of years — in Chinese jade carving, in Mesoamerican stonework, in Mediterranean decorative arts. The fish is one of the oldest and most widely distributed symbolic motifs in carved stone. Here the fish fills the egg form almost completely, the striped scales wrapping around the curve of the stone as though the fish is swimming through it rather than across it. There was no water. Perhaps that was what the carver intended — to remember that movement can survive even after the water is gone.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe engraving quality is skilled — the line work is confident and the white fill creates strong graphic contrast against the deep black ground. At 201g it has real presence and the black stone photographs exceptionally well. The most visually dramatic egg in the collection, and the only one with a figurative carved motif. A strong curiosity and art object for a collection that values craft alongside geology.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Carved black stone egg with engraved fish motif (presented as black marble based on catalog; stone type not independently verified)\u003cbr\u003eWeight: 201g\u003cbr\u003eDisplay stand: Not included — stand shown in photographs is for display purposes only\u003cbr\u003eMaker: Unknown\u003cbr\u003eAge: Unknown\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Carved decorative object — please review photographs for engraving detail, surface polish, and condition.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422402233,"sku":"7631904","price":62.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/00F859B9-D94E-4A59-B40D-2582937EEC7D.jpg?v=1783182609"},{"product_id":"banded-onyx-egg-stone-of-strength-protection-and-inner-balance","title":"Banded Onyx Egg — Layered Chalcedony, Natural Banding, 194g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished banded onyx egg, 194g — quiet bands of color moving through polished chalcedony, no obvious beginning or end to the pattern as the piece turns. A small study in layers, balance, and the passage of geological time. The smaller of two banded onyx eggs currently in the Found in the Field collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eOnyx is a variety of banded chalcedony — microcrystalline quartz — in which the banding runs parallel and straight (distinguishing it from agate, where banding can be curved or irregular). The banding develops through successive deposition of silica-rich mineral fluids in rock cavities, with each layer representing a depositional event. Color variation between bands reflects differences in mineral impurities or iron content in the fluid at each deposition. As noted for the companion piece: much commercial “onyx” in the mineral trade — particularly material sold as “Mexican onyx” or “Pakistani onyx” — is actually banded calcite or travertine rather than true chalcedony onyx. This specimen is presented as banded onyx chalcedony based on catalog identification; material identification has not been independently laboratory verified. This specimen weighs 194g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe finder traced one band with a fingertip. Then another. How many layers are there? The stone offered no answer. Each band is a depositional event — a period when silica-rich fluid moved through the cavity and laid down another layer. Some things become strong not by remaining unchanged, but by adding one layer after another. The egg form cross-sections through those layers, turning a depositional sequence into a continuous surface with no beginning and no end.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe banding is natural and clearly visible, and the polished finish brings the layers forward. At 194g it sits comfortably in the hand — a quieter, more compact presence than the larger companion egg. A composed geological display or desk object that rewards attention without demanding it.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Banded onyx egg (polished chalcedony carving, presented as onyx based on appearance; not independently verified)\u003cbr\u003eWeight: 194g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for banding, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422435001,"sku":"246643F","price":25.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0329.jpg?v=1782086522"},{"product_id":"petrified-wood-specimen-ancient-stone-of-grounded-transformation","title":"Petrified Wood Specimen — Grain Pattern Preserved in Stone, 267g — Field Find #0002","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA petrified wood specimen, 267g — dark grain-like markings preserved in contrasting lighter mineral material, the visual language of wood still legible in stone. Found in a thrift-store bag of rocks in Minnesota. It was easy to overlook. Which is exactly what makes a Field Find. This piece was noticed. Catalog ID: FITF-0002.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003ePetrified wood forms when woody material is buried and protected from ordinary decomposition while mineral-rich groundwater moves slowly through the surrounding sediment. Over geological time, minerals (commonly silica, calcite, or pyrite, depending on the conditions) precipitate into the cellular spaces of the wood, gradually replacing and preserving the organic structure as stone. The process can preserve the grain pattern, annual rings, and cellular geometry of the original wood with remarkable fidelity — the result is stone that still carries the visual language of wood. The exact tree species, geological age, mineral composition, and original locality of this specimen have not been independently laboratory verified and are intentionally left unspecified. Acquired: thrift store, Minnesota. Approximate dimensions: 10 × 8 × 5 cm. This specimen weighs 267g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThere was once a forest where the horizon had no end. The trees grew old, fell, and were replaced. Then the forest became a memory. But this fragment refused to disappear. It sank beneath the earth. Years became centuries. Centuries became ages. Water moved through the buried wood, carrying minerals into every hidden space. Little by little, the living thing became stone — and yet something remained. The lines. The pattern. The memory of growth. Long after the forest had vanished, someone would pick it up and wonder why it looked like wood. They would not know the tree’s name. But they would know one thing: it had not completely disappeared.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe grain pattern is clearly visible and the contrast between dark and light material reads immediately as wood — the petrification is legible without explanation. This is the kind of find that explains why Found in the Field exists: not from a famous mine, not accompanied by dramatic provenance. Found in a bag of rocks at a thrift store. Objects don’t always announce their importance. Sometimes you have to stop, pick them up, and look twice. This piece rewards that second look.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Petrified wood specimen (natural; species, age, and mineral composition not independently verified)\u003cbr\u003eCatalog ID: FITF-0002\u003cbr\u003eWeight: 267g (approx. 9.4 oz)\u003cbr\u003eDimensions: Approx. 10 × 8 × 5 cm\u003cbr\u003eAcquired: Thrift store, Minnesota\u003cbr\u003eCondition: Natural specimen — please review photographs for grain pattern, mineral contrast, and surface variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422467769,"sku":"N505154","price":35.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/petrified-wood-main_3116d232-ec80-4218-a359-b67bdbb4f1f5.jpg?v=1787712683"},{"product_id":"citrine-crystal-cluster-stone-of-joy-abundance-and-radiant-energy","title":"Citrine Crystal Cluster — Warm Golden Quartz Points, 237g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA citrine crystal cluster, 237g — warm golden quartz points catching the light at every angle. Gold gathered in the crystal terminations, moving as the cluster turns. A substantial display specimen with the visual appeal of a small geological landscape.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eCitrine is the yellow-to-orange variety of quartz (SiO₂). Its characteristic golden color is associated with trace iron impurities and natural irradiation effects within the quartz crystal lattice. In a cluster, multiple crystals grow simultaneously in the same cavity or on the same matrix, each competing for space and silica-rich fluid, producing the grouped-point form visible here. An important disclosure: commercially available citrine is very frequently heat-treated amethyst or smoky quartz that has been artificially colored through heating to above 470°C, which converts the purple or gray color to yellow-orange. Natural citrine and heat-treated citrine are visually difficult to distinguish without laboratory testing. The treatment history and exact locality of this specimen have not been independently verified and this listing does not make a natural-versus-treated determination. The color is warm and genuine-looking; the uncertainty is disclosed. This specimen weighs 237g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe finder found it beneath a layer of ordinary stone. At first, they thought the light had caught something. Then they realized the light was coming from the stone itself. Gold moved across the points. “Not sunlight,” they whispered. “Something that remembers it.” The iron chemistry that produces citrine’s gold is the same iron chemistry that colors sunsets — light scattering through iron-influenced material at the right wavelengths. The stone has been holding that frequency since it crystallized.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe color is warm and well-distributed across the cluster — not bright enough to look artificial, not dull enough to disappear. At 237g it has real display presence. A strong specimen for a quartz or golden mineral collection, with the disclosure clearly made.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Citrine crystal cluster (yellow quartz — natural vs. heat-treated not confirmed; not independently verified)\u003cbr\u003eWeight: 237g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural crystal cluster — please review photographs for crystal points, color, clarity, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422500537,"sku":"311774E","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0397.jpg?v=1782135584"},{"product_id":"black-zebra-agate-egg-stone-of-balance-protection-and-grounded-focus","title":"Black Zebra Agate Egg — High-Contrast Banded Chalcedony, Polished, 174g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished black zebra agate egg, 174g — dark bands move through pale stone in high contrast, disappearing and returning as the egg turns. The pattern reads like a tiny geological map. Something ancient-looking, polished into something remarkably quiet.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eAgate is a variety of chalcedony — microcrystalline quartz (SiO₂) — recognized for its layered or banded appearance. “Zebra agate” is a descriptive trade name for the high-contrast black, white, and gray banding pattern rather than a separate mineral species. Agate forms when silica-rich hydrothermal fluids fill cavities and fractures in volcanic or sedimentary rock and gradually deposit successive layers of chalcedony on the cavity walls. Changes in mineral chemistry, impurity content, and fluid conditions during each depositional event produce the contrasting bands — black bands are typically produced by manganese oxide or organic carbon inclusions, white bands by pure or near-pure chalcedony. The exact locality of this specimen has not been independently verified. This specimen weighs 174g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe stone wasn’t choosing between opposites. It had learned to hold them together. Each band in this agate is a depositional event — a period when silica-rich fluid moved through the cavity and laid down another layer. The black and white alternate because the fluid chemistry alternated: more manganese oxide one cycle, purer silica the next. The egg form cross-sections through those layers, turning a depositional sequence into a pattern you can hold.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe contrast is strong and the banding is well-developed and clearly visible. At 174g it has real weight and presence. A graphically immediate piece — the black and white pattern reads from across a shelf in a way that more subtle specimens don’t. A strong addition to an agate or chalcedony collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Black zebra agate egg (banded chalcedony, polished carving — “zebra agate” is a trade name)\u003cbr\u003eWeight: 174g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for banding, contrast, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422566073,"sku":"227486J","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0335.jpg?v=1782086711"},{"product_id":"red-jasper-egg-stone-of-endurance-stability-and-life-force-strength","title":"Red Jasper Egg — Deep Earthy Red, Iron-Rich Microcrystalline Quartz, 149g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished red jasper egg, 149g — deep earthy red with the dense, opaque solidity that jasper is known for. Even in color, even in weight. A stone that feels settled in the hand before you’ve thought about it.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eRed jasper is an opaque, iron-rich variety of microcrystalline quartz (chalcedony) in which the red color is produced by hematite (Fe₂O₃) — iron oxide distributed through the silica matrix in fine particles. The higher the hematite content, the deeper and more uniform the red. Jasper forms in a variety of geological settings, most commonly as secondary silica filling in sedimentary or volcanic rock cavities, or as chemical precipitate from silica-rich groundwater. Unlike agate or onyx, jasper is fully opaque — light does not pass through it. Red jasper is one of the most consistently identified stones in the mineral trade; the visual characteristics are distinctive and the identification is reliable at the macroscopic level. Material identification based on appearance; not independently laboratory verified. This specimen weighs 149g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe red in jasper is the same iron oxide that colors red clay, red sandstone, and rust — hematite, the most stable oxidized form of iron. It is one of the most abundant colorants in the geological record, present on Mars as well as Earth, responsible for the red color of both. In jasper, hematite is distributed through a silica matrix dense enough to take a polish and durable enough (Mohs 6.5–7) to survive in a polished form indefinitely. The egg form in red jasper produces a piece that is almost entirely about weight and color — there is no translucence, no banding to decode, no crystal structure to observe. Just the red and the mass of it.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe color is deep and consistent across the polished surface — uniform earthy red without significant variation or patterning. At 149g the egg has real weight and presence. A grounding, unambiguous piece for a mineral collection or a desk object that doesn’t need explaining.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Red jasper egg (polished iron-rich microcrystalline quartz carving)\u003cbr\u003eWeight: 149g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for color, surface, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422598841,"sku":"5576107","price":38.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/9042CC87-327A-418F-B2DF-25FE6AACA7CA.jpg?v=1783182209"},{"product_id":"marble-egg-stone-of-timeless-strength-and-quiet-elegance","title":"Cream \u0026 Blush Marble Stone Egg — Warm Pale Tone, Subtle Veining, 157g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished marble stone egg, 157g — warm cream to pale blush tone with subtle veining and a smooth, clean surface. The quietest of the marble eggs in the collection: no bold veining, no graphic contrast. Just the natural warmth of the stone and the weight of it in the hand. Photographed on a brass display stand (stand not included).\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis specimen is presented as marble based on its visual characteristics — dense, opaque, and consistent with metamorphosed limestone. The warm cream to blush-peach color is produced by trace iron oxide or manganese impurities in the calcium carbonate matrix, which shift the base white of pure calcite marble toward warmer tones. The subtle veining reflects minor variation in mineral composition or impurity distribution in the original limestone, reorganized through metamorphism. This is distinct from the gray-veined and gray-banded marble eggs also in the collection: this piece has a warm, neutral cream-blush ground rather than a cool gray base. Material identification based on appearance; not independently laboratory verified. This specimen weighs 157g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003ePure calcite marble is white — the warm tones in this egg are the contribution of trace mineral impurities in the original limestone that were preserved through metamorphism. Even in a stone defined by recrystallization and pressure, the trace chemistry of its sedimentary origin persists, shifting what would otherwise be white into the warm palette visible here. The egg form in a stone this understated becomes about texture and weight rather than color or pattern. It rewards handling more than display.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe warmth of the tone is what earns this piece its place. At 157g it has real presence in the hand and the cream-blush color suits a neutral collection or interior without competing with more colorful specimens. The most quietly composed piece in the egg collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Marble stone egg (polished carving, presented as marble based on appearance; not independently verified)\u003cbr\u003eWeight: 157g\u003cbr\u003eDisplay stand: Not included — stand shown in photographs is for display purposes only\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for color, veining, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422631609,"sku":"V429695","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/original_5088c95a-e89f-4a71-941b-ab6e6db5b34a.jpg?v=1780807638"},{"product_id":"rhodonite-stone-egg-stone-of-compassion-healing-and-emotional-balance","title":"Rhodonite Stone Egg — Pink \u0026 Black Manganese Silicate, Polished, 167g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished rhodonite stone egg, 167g — warm pink tones with bold black veining distributed through a smooth, dense surface. The contrast between the pink and black is immediate and graphic. A piece that reads clearly from across a shelf.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eRhodonite is a manganese inosilicate mineral (MnSiO₃) that forms in metamorphic and metasomatic environments, typically in manganese-rich rock sequences. Its characteristic pink to rose-red color is produced by manganese in the crystal structure. The black veining and patches visible in rhodonite specimens are manganese oxide minerals — primarily pyrolusite or romanechite — that form as secondary alteration products when the manganese in the rhodonite oxidizes at or near the surface. The black is, in other words, the same element as the pink, in a different oxidation state. This specimen is presented as rhodonite based on its appearance and catalog identification; the material identification has not been independently laboratory verified. This specimen weighs 167g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe pink and black pattern in rhodonite is a record of two different chemical states of manganese coexisting in the same stone — the reduced manganese silicate (pink) alongside the oxidized manganese oxide (black). The boundary between them marks where oxidizing groundwater reached the rhodonite over geological time, converting the outermost manganese silicate to oxide. In a polished piece, those oxidation fronts become the graphic black veining that makes rhodonite immediately recognizable. The pattern is chemistry made visible.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe pink and black contrast is strong and clearly developed across the polished surface. At 167g the egg form has solid weight and display presence. A visually immediate piece — one of the more graphically striking eggs in the collection — with a geological story that matches its visual character.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Rhodonite stone egg (polished manganese silicate carving, presented as rhodonite based on appearance; not independently verified)\u003cbr\u003eWeight: 167g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for pink\/black pattern, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422893753,"sku":"814402S","price":58.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/51B2C98A-042D-497D-AC64-01B762675AFA.jpg?v=1783181974"},{"product_id":"green-onyx-egg-stone-of-renewal-strength-and-heart-centered-calm","title":"Green Onyx Egg — Banded Green Chalcedony, Polished, 314g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished green onyx egg, 314g — soft layers of banded green tones with a smooth, dense finish. The banding shifts as the egg turns, each layer a slightly different shade. A grounding, composed piece that suits a collection or a desk without demanding attention.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eGreen onyx is a trade name for green banded chalcedony — microcrystalline quartz — where the banding runs in parallel layers. The green color can be natural (from trace chromium, iron, or other impurities) or the result of dyeing, which is common in commercial green onyx on the market. It is worth noting that much material sold as “green onyx” is either dyed chalcedony\/agate or banded calcite\/aragonite (which is softer at Mohs 3–4 vs. quartz at Mohs 7). The material identification of this specimen has not been independently laboratory verified and is presented based on catalog identification. At 314g this is a substantial egg with real display presence. Locality not independently verified.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe banding in onyx-family chalcedony is a depositional record — each layer represents a period of silica-rich fluid moving through a rock cavity and depositing material on the cavity wall. The color variation between bands reflects differences in mineral impurities in the fluid at each depositional event. In a polished egg, those layers become a cross-section through that history — a record, compressed into a form you can hold.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe banded green tone is consistent and the polish is clean. At 314g it has significant weight and shelf presence — one of the heavier eggs in the collection. A composed, grounding piece for a mineral or lapidary collection that doesn’t need to announce itself.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Green onyx egg (banded chalcedony, polished carving — catalog identification; natural color vs. dyed not confirmed; not independently verified)\u003cbr\u003eWeight: 314g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for banding, color, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422926521,"sku":"887279K","price":30.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0639.jpg?v=1782616855"},{"product_id":"cavansite-stilbite-matrix-egg-stone-of-awakening-and-gentle-spiritual-insight","title":"Cavansite \u0026 Stilbite Matrix Egg — Vivid Blue on Pale Zeolite, Polished, 197g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished cavansite and stilbite matrix egg, 197g — vivid blue mineral clusters set against pale, pearly zeolite matrix. The blue arrives first. Against the pale ground it looks almost like a piece of sky caught beneath the surface — too vivid to be accidental, too contained to be anything other than what it is. Turn the egg in your hand and the blue remains. Some things don’t disappear just because you look at them from a different angle. This one has been holding its color for longer than anyone has been looking.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eCavansite is a hydrated calcium vanadium silicate mineral (Ca(VO)Si₄O₁₀·4H₂O) recognized for its intense blue color — one of the few minerals where vanadium produces a vivid blue rather than green. It typically occurs as small spherical or rosette crystal aggregates associated with zeolite minerals in basaltic volcanic rocks. Stilbite is a zeolite-group mineral (hydrated calcium sodium aluminum silicate) that forms pale, pearly to cream-colored sheaf-like or fan-shaped aggregates — the natural matrix in which cavansite most commonly occurs. The primary source of cavansite specimens on the market is the Wagholi quarry near Pune, India, though the exact locality of this specimen has not been independently verified. This specimen is presented as cavansite in stilbite matrix based on catalog identification; no independent laboratory confirmation has been performed. Catalog ID: FITF-0017. This specimen weighs 197g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eCavansite was only formally described as a mineral species in 1967 — relatively recent in mineralogical terms — and it is named for its chemical composition: calcium vanadium silicate. The Wagholi quarry near Pune became the world’s primary source of collector-quality cavansite in the 1990s and remains so today. The egg form creates a tension that the raw matrix form doesn’t: vivid mineral color contained inside a form associated with beginnings and cycles. It works as a mineral specimen and as a display object without needing explanation to earn its place on a shelf.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe blue is immediate and striking — the cavansite color against the pale stilbite matrix is one of the more visually arresting mineral contrasts in the collection. At 197g the egg has real weight and presence in the hand. A strong piece for a zeolite collection, a vanadium mineral collection, or any display that values exceptional color in natural form.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Cavansite \u0026amp; stilbite matrix egg (polished, catalog identification; not lab confirmed)\u003cbr\u003eCatalog ID: FITF-0017\u003cbr\u003eWeight: 197g\u003cbr\u003eOrigin: Not independently verified\u003cbr\u003eCondition: Polished egg — please review photographs for crystal formation, matrix character, cavansite cluster development, and surface detail.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422959289,"sku":"450277B","price":50.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0370.jpg?v=1782134988"},{"product_id":"vintage-alabaster-decorative-egg-stone-of-soft-light-memory-and-timeless-calm","title":"Amber \u0026 Cream Mottled Stone Egg — Warm Orange Tone, Vintage Piece, Polished — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished vintage stone egg — warm amber-orange with cream mottling and a high-gloss finish. Compact in form, warm in tone. A vintage piece with the quiet presence of an object that has been held before. Photographed on a wire brass display stand (stand not included).\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis specimen is described as alabaster in the original catalog. Its visual characteristics — opaque, warm amber-orange with cream mottling and a high-gloss polish — are more consistent with a polished calcite marble, travertine, or iron-stained limestone than with gypsum alabaster, which is typically semi-translucent, softer (Mohs 2), and lighter in tone. The warm orange-amber color is consistent with iron oxide (hematite or goethite) staining in a calcium carbonate host. The material identification has not been independently laboratory verified and is presented as uncertain. This piece is described as vintage based on catalog identification; the age and provenance have not been independently verified. Weight not confirmed — please weigh and update before publishing. Visually distinct from the golden-yellow vintage egg also in the collection: this piece has a more saturated amber-orange tone and cream mottling rather than the even golden-yellow of the companion piece.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe amber color in this egg is iron’s signature — goethite and hematite distributed through the stone during formation or subsequent fluid movement, staining the calcium carbonate matrix in the warm tones visible here. The same iron chemistry that rusts metal produces the warm golds and oranges in iron-stained stone. A vintage piece in this material carries both geological time and human time: the slow accumulation of iron in the stone, and the shorter history of the egg being carved, polished, owned, and passed forward.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe amber tone is warm and consistent, and the cream mottling creates visual interest without complexity. The compact size and high polish make it a natural desk or shelf object. Distinct from the other vintage egg in the collection in color character and stand style.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Polished stone egg — material uncertain, described as alabaster in catalog; visual characteristics more consistent with calcite marble or travertine. Not independently verified.\u003cbr\u003eDescribed as: Vintage piece\u003cbr\u003eWeight: [CONFIRM WEIGHT]\u003cbr\u003eDisplay stand: Not included — stand shown in photographs is for display purposes only\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Vintage polished carving — please review all photographs for color, mottling, surface condition, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980422992057,"sku":"848810T","price":38.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/79BE2BB3-98B1-480B-8AD4-31ACEB8808E6.jpg?v=1783181860"},{"product_id":"vintage-yellow-green-alabaster-egg-stone-of-gentle-renewal-and-balanced-calm","title":"Yellow \u0026 Green Mottled Stone Egg — Warm Golden Tone, Vintage Piece, Polished — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished stone egg — warm golden yellow with subtle mottling and a high-gloss finish. A vintage piece with the kind of presence that comes from age and careful handling. The same brass stand has held it before you; it will hold it after. Photographed on a brass display stand (stand not included).\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis specimen is described as alabaster in the original catalog, but its visual characteristics — opaque, dense, warm golden-yellow with mottled patterning — are more consistent with a polished marble, serpentinite, or jasper than with gypsum alabaster, which is typically semi-translucent, softer (Mohs 2), and rarely this saturated in color. The material identification has not been independently laboratory verified and is presented as uncertain. Additional photos may show green mottling not visible in the primary image. This piece is described as vintage based on catalog identification; the age and provenance have not been independently verified. Weight not confirmed — please weigh and update before publishing.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eVintage stone eggs occupy an interesting space in a mineral collection — they carry the history of whoever carved and owned them before arriving here, layered on top of the geological history of the stone itself. The warm golden color and the high polish suggest a piece that was made to be handled and displayed, not stored. The brass stand is a period-appropriate accessory for this kind of object. A found object in the truest sense: found, identified, and passed forward.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe warm golden tone is distinctive and the polish is clean despite the age of the piece. A visual anchor for a collection that includes newer specimens — the patina of a vintage piece gives a shelf a sense of depth and time that newly quarried stones alone can’t provide.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Polished stone egg — material uncertain, presented as alabaster in catalog; visual characteristics more consistent with marble, serpentinite, or jasper. Not independently verified.\u003cbr\u003eDescribed as: Vintage piece\u003cbr\u003eWeight: [CONFIRM WEIGHT]\u003cbr\u003eDisplay stand: Not included — stand shown in photographs is for display purposes only\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Vintage polished carving — please review all photographs for color, mottling, surface condition, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423057593,"sku":"131452H","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/B26346C8-BA5E-4CE8-B094-DE4154E3B311.jpg?v=1783181733"},{"product_id":"banded-onyx-egg-stone-of-protection-discipline-and-inner-strength","title":"Banded Onyx Egg — Layered Chalcedony, Natural Banding, 254g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished banded onyx egg, 254g — layered chalcedony with contrasting bands that shift as the egg turns. The polished form brings out the contrast between the layers while preserving the natural character of the stone. The larger of two banded onyx eggs currently in the Found in the Field collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eOnyx is a variety of banded chalcedony — microcrystalline quartz — in which the banding runs parallel and straight (distinguishing it from agate, where banding can be curved or irregular). The banding develops through successive deposition of silica-rich mineral fluids in rock cavities, with each layer representing a depositional event. Onyx in the trade is a frequently misapplied name: much commercial “black onyx” is actually dyed agate or chalcedony, and many stones sold as “onyx” (particularly Mexican and Pakistani “onyx”) are actually banded calcite or travertine rather than true chalcedony onyx. This specimen is presented as banded onyx chalcedony based on its appearance and catalog identification; material identification has not been independently laboratory verified. The exact locality and provenance of this specimen have not been independently confirmed. This specimen weighs 254g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe banding in chalcedony onyx is a geological record of repeated mineral deposition — each layer represents a period when silica-rich groundwater moved through the cavity and deposited material on the cavity wall. The color variation between bands reflects differences in mineral impurities or iron content in the fluid at the time of each deposition. In a polished egg, those layers become a cross-section through that depositional history — a record of how many times the conditions were right for another layer to form.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe banding is natural and clearly visible, and the polished finish brings out the contrast between the layers. At 254g it has substantial presence as a display object — the larger scale gives it more weight and visual authority than the smaller companion piece. A grounding, architectural piece for a mineral or lapidary collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Banded onyx egg (polished chalcedony carving, presented as onyx based on appearance; not independently verified)\u003cbr\u003eWeight: 254g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for banding, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423090361,"sku":"1775242","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0322.jpg?v=1782086410"},{"product_id":"marble-or-alabaster-stone-egg-symbol-of-timeless-calm-and-gentle-strength","title":"Marble or Alabaster Stone Egg – Symbol of Timeless Calm and Gentle Strength-180g","description":"A marble or alabaster stone egg carries a soft yet enduring energy, blending the strength of natural stone with the symbolism of renewal and creation. Marble represents resilience formed under pressure, while alabaster is associated with serenity, purity, and emotional soothing. Together, they create a piece that feels both grounding and calming.\u003cbr\u003e\u003cbr\u003e\u003cbr\u003eThe egg shape enhances its meaning of new beginnings, potential, and transformation, making it a powerful symbol of quiet growth and inner stability. This piece is often used as a reminder to move through life with patience and grace, trusting that strength can be both steady and gentle.\u003cbr\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423188665,"sku":"3459117","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/42B1A793-4FCD-42D5-8C07-4F89CCB043DB.jpg?v=1783181597"},{"product_id":"veined-marble-or-alabaster-stone-egg-stone-of-balance-and-timeless-grounding","title":"Gray \u0026 Black Veined Marble Stone Egg — Bold Veining, Polished, — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished marble stone egg — gray-white ground with bold black veining distributed across a smooth, high-polish surface. Dense and opaque, with a graphic quality to the veining that reads differently from every angle. An egg form that suits the material: the weight feels intentional in the hand. Photographed on a brass display stand (stand not included).\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis specimen is presented as marble based on its visual characteristics — the dense, opaque gray-white surface with bold black veining is consistent with metamorphosed limestone (marble) rather than alabaster (gypsum), which is typically semi-translucent and rarely produces this style of bold black veining. Marble forms when limestone or dolostone is subjected to heat and pressure during metamorphism, recrystallizing the calcium carbonate into interlocking calcite or dolomite crystals. The black veining is typically graphite, pyroxene, or other mineral inclusions distributed through the marble during metamorphism. Material identification based on appearance; not independently laboratory verified. Weight not confirmed — please weigh and update before publishing.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe veining pattern in marble is a record of the original limestone’s history — impurities and mineral bands present in the sedimentary rock are reorganized and sometimes concentrated by the heat and pressure of metamorphism. Black veining in particular tends to be graphite, which is itself metamorphosed carbon from ancient organic material. The dark lines running through this egg are the compressed remnants of ancient life, transformed beyond recognition by geological time and pressure into the graphic pattern visible on the surface.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe veining is bold and well-distributed — the contrast between gray-white ground and black veining is strong and graphic. The polished surface brings forward the pattern clearly. A composed, architectural piece that suits a curated shelf or desk without demanding attention the way more colorful specimens do.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Marble stone egg (polished carving, presented as marble based on appearance; not independently verified)\u003cbr\u003eWeight: [CONFIRM WEIGHT]\u003cbr\u003eDisplay stand: Not included — stand shown in photographs is for display purposes only\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for veining, color, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423286969,"sku":"S514695","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/2E847EF4-24C2-4E8C-810F-3C569EC37D9F.jpg?v=1783181384"},{"product_id":"green-fluorite-egg-stone-of-clarity-renewal-and-heart-aligned-focus","title":"Green Fluorite Egg — Translucent Polished Carving, 128g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished green fluorite egg, 128g — translucent green calcium fluoride with a refreshing, glassy clarity. The color moves from pale mint to deeper sage depending on the thickness of the stone and the angle of the light. An egg form that rewards holding up to the light.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eFluorite is calcium fluoride (CaF₂) — one of the most color-variable minerals in existence, occurring in virtually every color of the spectrum depending on trace impurities and radiation exposure during crystal growth. Green fluorite gets its color from trace amounts of chlorine, yttrium, or radiation-induced color centers in the crystal lattice. Fluorite is relatively soft (Mohs 4) and has perfect octahedral cleavage in four directions — which means it can chip and cleave along those planes if knocked. The word “fluorescence” is derived from fluorite: in 1852, George Gabriel Stokes observed that fluorite specimens glowed blue-white under ultraviolet light and named the phenomenon after the mineral. Fluorite is one of the most widely fluorescent minerals, though not all specimens fluoresce. This specimen weighs 128g. Material identification based on appearance; not independently verified.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eFluorite gave its name to an entire physical phenomenon — fluorescence — because it was the first mineral in which the effect was systematically described. Stokes observed in 1852 that invisible ultraviolet radiation was being absorbed and re-emitted as visible blue-white light, and named the phenomenon after the mineral where he studied it. The green of this egg is a different expression of the same mineral: not fluorescence but transmitted color, the result of trace impurities in the crystal lattice filtering the light that passes through it.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe translucence is the case for this piece — green fluorite in egg form allows light to pass through the stone in a way that opaque minerals don’t, and the color depth varies across the surface as the stone thickness changes. At 128g it has good presence and the egg form is well-suited to the translucent quality of the material.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Green fluorite egg (polished carving, calcium fluoride)\u003cbr\u003eWeight: 128g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — fluorite is soft (Mohs 4) with perfect cleavage; handle with care to avoid chipping. Please review photographs for color, translucence, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423352505,"sku":"348923L","price":38.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0634.jpg?v=1782616743"},{"product_id":"marble-or-red-alabaster-stone-egg-stone-of-vitality-strength-and-grounded-renewal","title":"Red \u0026 Amber Marble Stone Egg — Warm Mottled Tones, Polished, 148g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished stone egg, 148g — deep reds, burnt oranges, and warm amber tones mottled across a smooth, high-polish surface. The color pattern is warm and complex — earthy without being dull, vivid without being loud. Photographed here on a brass display stand (stand not included).\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis specimen is presented as marble or red alabaster based on its visual characteristics; the material identification has not been independently laboratory verified. The color pattern — warm reds, oranges, and cream mottling — is consistent with a brecciated or iron-stained marble (metamorphosed limestone), where red and orange tones are typically produced by iron oxide (hematite or goethite) distributed through the calcium carbonate matrix. True alabaster is gypsum (CaSO₄·2H₂O) and is typically more translucent and soft (Mohs 2); marble is harder (Mohs 3–4) and less translucent. The visual appearance of this piece is more consistent with a dense, polished marble or limestone variant than with gypsum alabaster, but without testing the distinction cannot be confirmed. This specimen weighs 148g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe warm reds and oranges in this egg are iron’s signature in a calcium carbonate host — hematite and goethite distributed through the stone during formation or subsequent fluid movement, staining the matrix in irregular clouds and veins that polishing brings forward. Marble has been carved and polished since antiquity; the egg form is one of the simplest and most satisfying shapes for a dense, heavy stone, because the weight distribution in the hand feels intentional in a way that rough or angular specimens don’t.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe color is genuinely striking — warm, complex, and consistent across the polished surface. At 148g the egg form has real weight and presence. A visually warm piece for a collection or display where earthy, fire-toned color is the goal.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Stone egg (presented as red marble or alabaster based on appearance; not independently verified)\u003cbr\u003eWeight: 148g\u003cbr\u003eDisplay stand: Not included — stand shown in photographs is for display purposes only\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for color, pattern, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423385273,"sku":"8210697","price":48.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/122DA0EA-E6E4-4EEE-9949-0566BF2A6CDC.jpg?v=1783181269"},{"product_id":"green-vesuvianite-egg-stone-of-transformation-alignment-and-heart-renewal","title":"Vesuvianite Stone Egg — Polished Green, Idocrase Calcium Silicate, 261g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished vesuvianite stone egg, 261g — vibrant green calcium silicate mineral with a smooth, dense finish. Rich in color and grounding in the hand. A less common mineral in carved form, with a geological name that tells you exactly where it was first described.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eVesuvianite (also called idocrase) is a calcium aluminum magnesium silicate mineral (Ca₁₀(Mg,Fe)₂Al₄Si₉O₄₀(OH,F)₄) that forms in metamorphic and metasomatic environments — typically in skarns, where calcium-rich rocks such as limestone are altered by contact with igneous intrusions. The green color is produced by chromium or iron impurities in the crystal structure. It was first described from volcanic ejecta at Mount Vesuvius in 1795 by Abraham Gottlob Werner, which is how it got its name — though the majority of gem-quality vesuvianite comes from deposits in Canada, Pakistan, Russia, and California rather than from Vesuvius itself. This specimen is presented as vesuvianite based on its appearance and catalog identification; material identification has not been independently laboratory verified. This specimen weighs 261g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eVesuvianite’s naming is a reminder of how early mineralogy worked: a mineral was often named after the first location where it was scientifically described, even if that location later turned out to be a minor occurrence of the mineral rather than a significant source. Mount Vesuvius gave it a dramatic name. The gem-quality material that fills most collections today comes from considerably quieter geological settings — skarns in Quebec, the Pamir Mountains, and the California serpentinite belts. The name stayed because names, once assigned, are hard to change.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe green color is vibrant and consistent across the polished surface. At 261g the egg form has substantial weight and display presence. A less commonly seen mineral in carved form — a strong addition to a collection that moves beyond the standard mineral roster.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Vesuvianite (idocrase) stone egg — polished carving, presented as vesuvianite based on appearance; not independently verified\u003cbr\u003eWeight: 261g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — please review photographs for color, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423418041,"sku":"M302630","price":30.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0649.jpg?v=1782617094"},{"product_id":"ocean-jasper-stone-of-joyful-healing-and-emotional-renewal","title":"Ocean Jasper Specimen — Orbicular Patterns, Madagascar Single-Source, 315g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eAn ocean jasper specimen, 315g — swirling patterns, orb-like inclusions, and a soothing earth-and-sea color palette. One of the most visually distinctive jaspers in the mineral world, and one of the few with a confirmed, single known source locality.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eOcean jasper (also called orbicular jasper) is a variety of spherulitic chalcedony found exclusively along the northwest coast of Madagascar, near the village of Marovato in the Ambolobozo Peninsula. The orb-like circular patterns are spherulites — radially crystallized silica structures that form during the rapid cooling of silica-rich volcanic material, producing concentric rings of chalcedony around a central nucleation point. The color palette (greens, creams, pinks, whites, grays, and yellows) reflects varying mineral impurities in the silica at the time of formation. The deposit is accessible only by boat at low tide, and the original commercial deposit is largely exhausted — making genuine ocean jasper increasingly scarce. This specimen weighs 315g. Locality attributed to Madagascar based on material identification.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eOcean jasper was “rediscovered” commercially in 1999 by Paul Obeniche on the Malagasy coast — the deposit had been noted in mineralogical literature but wasn’t commercially mined until that point. The primary deposit at Marovato was largely mined out by the early 2010s; subsequent smaller deposits have been found nearby but produce different material. The combination of single-source locality, distinctive orbicular pattern, and commercial scarcity makes ocean jasper one of the more collectible trade jaspers on the market. At 315g this specimen has significant display presence.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe orbicular patterning is clearly visible and the color range appears strong across the surface. At 315g it has real shelf presence. A strong piece for a jasper collection or any display that values geological story and visual distinctiveness over conventional crystal aesthetics.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Ocean jasper specimen (orbicular chalcedony, spherulitic jasper)\u003cbr\u003eOrigin: Northwest Madagascar (Marovato, Ambolobozo Peninsula) — attributed based on material identification\u003cbr\u003eWeight: 315g\u003cbr\u003eCondition: Natural specimen — please review photographs for orbicular pattern, color, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423516345,"sku":"P413847","price":68.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/C0973C3B-2EDA-42AC-A5D0-810B122F69A6.jpg?v=1783181153"},{"product_id":"green-serpentine-stone-egg-stone-of-healing-protection-and-earth-alignment","title":"Serpentine Stone Egg — Polished Green, Smooth Carving, 151g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished serpentine stone egg, 151g — smooth green mineral carving with soft, waxy luster and the quiet color of the forest floor. Grounding in the hand. An object that feels like it belongs in nature even when it’s on a shelf.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eSerpentine refers to a group of magnesium silicate minerals (primarily lizardite, antigorite, and chrysotile) that form through the metamorphic alteration of ultramafic rocks such as peridotite and dunite — a process called serpentinization. The characteristic green to yellow-green color is produced by iron and magnesium in the mineral structure. Serpentine is relatively soft (Mohs 3–4) and has a waxy to greasy luster. This specimen is presented as serpentine based on its appearance and characteristics. The material identification has not been independently laboratory verified. This specimen weighs 151g. ⚠️ Note: some serpentine group minerals (particularly chrysotile) are associated with asbestos. Polished and finished serpentine specimens are generally considered safe to handle, but avoid sanding, grinding, or cutting. Do not inhale dust.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eSerpentinization is one of the more dramatic metamorphic processes in geology — ultramafic rocks from the deep mantle, brought to the surface by tectonic activity, react with water and are chemically transformed into serpentine minerals, releasing heat and hydrogen gas in the process. Serpentine landscapes (called serpentinite barrens) are ecologically distinctive because the chemistry of the soil is toxic to most plants, producing unusual, often endemic flora adapted to high magnesium and low calcium conditions. The smooth green of this polished egg is the surface expression of a deep-earth metamorphic history.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe green color is consistent and the polish is clean. At 151g the egg form has real weight and presence in the hand. A grounding, tactile object with a geological story that goes considerably deeper than the surface suggests.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Serpentine stone egg (polished carving) — presented as serpentine based on appearance; not independently verified\u003cbr\u003eWeight: 151g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — do not sand or grind. Please review photographs for color, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423549113,"sku":"Q198967","price":30.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0644.jpg?v=1782616970"},{"product_id":"druzy-quartz-geode-sparkling-crystal-cave-of-light","title":"Druzy Quartz Geode — Large Crystal-Lined Cavity, Statement Specimen, 1565g (3.45 lb) — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA large druzy quartz geode, 1565g (3.45 lb) — a substantial cavity lined with thousands of tiny quartz crystal points, each catching the light at a different angle. From the outside, it looks like stone. Then the stone opens. Inside is a field of crystals that grew in silence, slowly, patiently, until the darkness held its own sky.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eGeodes form when a cavity develops within rock — typically basalt, limestone, or sedimentary rock — and mineral-rich fluids later move through it, depositing minerals along the cavity walls over geological time. In a quartz-lined geode, silica-rich groundwater deposits chalcedony on the walls first, followed by quartz crystals growing inward. “Druzy” describes a surface covered with many small, densely packed crystal points rather than a few large faces — the sparkle is the natural geometry of thousands of mineral surfaces reflecting light simultaneously. At 1565g this is a substantial specimen — large enough to function as an environment rather than just an object. Locality not independently verified. Catalog ID: FITF-0013.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eEvery tiny crystal point in this geode formed independently within the cavity, yet together they create one continuous surface. Each point grew outward from the cavity wall toward the open center, competing for space and silica-rich fluid as it went. The result is not designed — it is emergent: the collective output of thousands of individual crystal growth events, each following the same basic physics, producing an interior that looks coordinated because the physics are consistent. That is what makes a geode interior feel like a landscape. It is one, in its way.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eScale is the case for this piece. At 1565g the geode moves from display object to statement piece — it anchors a shelf, a table, or a collection. The druzy crystal surface creates strong visual texture across the entire interior cavity. The highest-weight specimen currently in the Found in the Field collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Druzy quartz geode (crystal-lined cavity)\u003cbr\u003eCatalog ID: FITF-0013\u003cbr\u003eWeight: 1565g (3.45 lb)\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural specimen — please review all photographs for crystal surface, natural edges, matrix, and condition.\u003cbr\u003eDimensions: [DIMENSIONS]\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423844025,"sku":"F720946","price":180.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-0457.jpg?v=1782179071"},{"product_id":"natural-amethyst-crystal-geode-sacred-purple-earth-treasure","title":"Amethyst Cathedral Geode — Freestanding, Deep Violet Crystal Interior, Polished Base — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA freestanding amethyst cathedral geode — deep violet quartz crystals growing inward from a hollowed basalt cavity, polished flat base for display. Each point formed slowly over time, creating a sparkling interior that opens like a hidden chamber. Strength on the outside. Light within.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eAmethyst cathedral geodes form in basaltic lava cavities in volcanic regions — the majority of the world’s supply originates from the Rio Grande do Sul region of southern Brazil and the Artigas region of Uruguay. Silica-rich hydrothermal fluids enter the cavity and deposit successive layers of chalcedony on the walls, followed by amethyst crystals growing inward. The deep violet color is produced by trace iron and natural irradiation during crystal growth. The \"cathedral\" form refers to freestanding geodes cut with a flat base so they stand upright, displaying the crystal interior. Amethyst color can fade with prolonged exposure to direct sunlight. Locality not independently verified. ⚠️ Note: the recorded weight of 3.14g appears to be a data entry error based on the size visible in photographs — please weigh and confirm before publishing.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe basaltic lava flow that formed this geode’s outer shell predates the crystals inside by a significant margin — the cavity formed when gas bubbles were trapped in cooling lava, and the amethyst grew later, when hydrothermal fluids worked their way through the rock. The polished base is a lapidary decision that turns a geological object into a display piece: it creates a stable, self-standing form that shows the crystal interior at its best. The dark matrix around the crystal pocket is the original basalt — the rock that held the space open long enough for the amethyst to form.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe crystal development is strong — deep violet points with good saturation and clear terminations visible in the interior. The polished base and self-standing form make it immediately display-ready. A flagship piece for a crystal collection or an anchor display object for a shelf or desk.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Amethyst cathedral geode (freestanding, polished base)\u003cbr\u003eWeight: [CONFIRM WEIGHT — recorded as 3.14g, appears incorrect based on photographs]\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural specimen with polished base — avoid prolonged direct sunlight (color may fade). Please review photographs for crystal development, color, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980423876793,"sku":"166858Q","price":100.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/40F181A9-6A43-4548-95F8-BF21CA71FF96.jpg?v=1783180956"},{"product_id":"polished-goniatite-fossil-ancient-ocean-spiral-of-time","title":"Polished Goniatite Fossil — Ancient Marine Cephalopod, Spiral Chamber Pattern, 9g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished goniatite fossil, 9g — an ancient ocean spiral carried forward through stone. Small enough to sit in your palm; its story reaches back into a world almost impossible to imagine. The creature disappeared. The shape did not.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eGoniatites were extinct ammonoid cephalopods — relatives of the better-known ammonites — that lived in marine environments from the Devonian through the Permian periods (approximately 419 to 252 million years ago). Like ammonites, they had coiled, chambered shells; the chambers were connected by a tube called the siphuncle, which the animal used to regulate buoyancy by adjusting gas and fluid ratios. The suture pattern where each chamber wall meets the outer shell is distinctive in goniatites — simpler and more angular than the complex fractal-like sutures of true ammonites — and is visible when specimens are cut and polished. Polishing reveals the internal chamber geometry that creates the geometric pattern visible on this specimen. The exact locality, geological age, and species of this specimen have not been independently verified. Catalog ID: FITF-0011. This specimen weighs 9g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eBefore there were forests. Before there were roads. Before there was anyone to name the continents, there was an ocean — and in that ocean, goniatites moved through the water carrying spiral chambers within their shells. The spiral is not just decoration: it is architecture, an efficient pressure-resistant structure built chamber by chamber as the animal grew, each new chamber sealed behind it. Then time buried it. Stone replaced what was organic. And eventually, someone polished the surface enough for the ancient pattern to appear again. The message had been waiting.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe chamber pattern is clearly visible in the polished surface and the goniatite suture geometry is legible at this scale. At 9g it is a compact piece that makes deep time tangible in the hand. A strong fossil entry for a natural history collection or alongside mineral specimens.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Polished goniatite fossil (extinct ammonoid cephalopod)\u003cbr\u003eCatalog ID: FITF-0011\u003cbr\u003eWeight: 9g\u003cbr\u003eAge\/locality: Not independently verified\u003cbr\u003eCondition: Polished fossil specimen — please review photographs for chamber pattern, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980424007865,"sku":"211053T","price":20.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/CA07F79C-2034-4070-A655-DF600BB085FD.jpg?v=1783180742"},{"product_id":"sky-blue-larimar-stone-of-ocean-sky-serenity","title":"Larimar Specimen — Sky Blue \u0026 White, Dominican Volcanic Gemstone — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA larimar specimen — sky blue and soft white marbling in the only gemstone found exclusively in the Dominican Republic. Calming oceanic blues that resemble tropical water or drifting cloud. A rare volcanic mineral that feels like standing at the edge of the sea.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eLarimar is a blue variety of pectolite (NaCa₂Si₃O₈(OH)), a sodium calcium silicate mineral. Its distinctive blue coloration is produced by copper substituting for calcium in the crystal structure — the same element responsible for blue in turquoise and azurite, producing a different shade here due to the different mineral host. Larimar forms in cavities within basaltic lava flows in the Bahoruco Mountain Range of the Dominican Republic. The single known commercial deposit, near the village of Los Chupaderos, is the only source of gem-quality larimar in the world — a genuinely rare material with a confirmed, unique locality. The market contains imitation and lower-grade pectolite sold as larimar; this specimen is presented as larimar based on visual characteristics and catalog identification. Weight not confirmed — please update before publishing.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eLarimar was known to the indigenous Taíno people of Hispaniola long before European contact, but the modern commercial discovery is credited to Miguel Méndez and Norman Rilling in 1974, who found it eroding from the sea cliffs near Barahona. Méndez named it by combining his daughter’s name (Larissa) with the Spanish word for sea (mar). The deposit sits at altitude in the mountains — the stones reached the coast by eroding downriver, which is how Méndez and Rilling found it. It is one of the few gemstones with a discoverable modern origin story, a single known source, and a name that tells you exactly who found it and why.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe sky blue coloration and white patterning are clearly visible and the color quality appears strong. Larimar at $60 is fair pricing for a genuine specimen — the combination of rarity, single-source provenance, and visual quality makes this a compelling piece for a gemstone or volcanic mineral collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Larimar specimen (blue pectolite, copper-bearing sodium calcium silicate)\u003cbr\u003eOrigin: Dominican Republic (Los Chupaderos mine area, Bahoruco Mountains)\u003cbr\u003eWeight: [CONFIRM WEIGHT]\u003cbr\u003eCondition: Please review photographs for color, patterning, and natural variation. Presented as larimar based on visual characteristics.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980424040633,"sku":"L002831","price":60.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/76945FFE-7EA7-478C-8BF9-4047D1CBFF03.jpg?v=1783134791"},{"product_id":"palaeolithic-handaxe-ancient-stone-tool-of-early-humanity","title":"Palaeolithic-Style Handaxe — Knapped Flint Stone Tool, 12g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA knapped flint handaxe, 12g — stone worked against stone, edge by careful edge. It fits the hand like it was made for it. Someone held this before you. There is something grounding about holding an object that may be this old. It doesn’t ask for context or explanation. It simply is — a direct line to the first makers, the first problem-solvers, the first people who looked at a rock and saw a possibility.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eA handaxe (or biface) is a bifacially worked stone tool — flaked on both faces to produce a symmetrical cutting or scraping edge. The Acheulean handaxe tradition spans from approximately 1.76 million to 130,000 years ago and represents one of the longest-running tool technologies in human prehistory. This specimen displays knapping characteristics consistent with handaxe typology. At 12g it is a small specimen. The exact age, cultural affiliation, and original locality of this piece have not been independently laboratory verified. It is presented as a handaxe-form knapped stone tool based on visual and morphological characteristics. Sold as a found collectible object; buyers should conduct their own research and due diligence. ⚠️ Note: the sale of genuine archaeological artifacts is subject to legal restrictions in many jurisdictions. Buyers are responsible for compliance with applicable laws.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe Acheulean handaxe is one of the most studied objects in human prehistory — hundreds of thousands of them have been found across Africa, Europe, and Asia, spanning a time period longer than the entire history of anatomically modern humans. They were made by Homo erectus, Homo heidelbergensis, and early archaic humans long before Homo sapiens existed. A handaxe is a direct connection to the cognitive capacity that preceded modern human thought: the ability to plan ahead, to see a finished tool in an unworked stone, and to execute that vision through dozens of controlled strikes. The stone does not change. The understanding of what it represents does.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe knapping is clearly present and the biface morphology is consistent with handaxe typology. A compelling piece for a collection of lithic artifacts or ancient tools, at a price that reflects its apparent workmanship and the extraordinary story it carries — if the identification holds.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Knapped flint handaxe (bifacial stone tool, Palaeolithic-style)\u003cbr\u003eWeight: 12g\u003cbr\u003eProvenance: Not independently verified — sold as found. Buyers should conduct their own research. Legal compliance is the buyer’s responsibility.\u003cbr\u003eCondition: Knapped flint; edges may be sharp — handle with care.\u003cbr\u003eDimensions: [DIMENSIONS]\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980424073401,"sku":"652337T","price":100.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/D3CE70A5-2E1A-4BC5-ABCA-40597B9C3E4B.jpg?v=1783134623"},{"product_id":"malachite-stone-of-transformation-deep-healing","title":"Malachite Specimen — Banded Green Copper Mineral, Swirling Pattern, 58g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA malachite specimen, 58g — rich banded green copper mineral with swirling, almost hypnotic patterns that resemble flowing energy or forest canopies. One of the most visually distinctive minerals in the collection. The green is unmistakably its own.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eMalachite is a copper carbonate hydroxide mineral (Cu₂CO₃(OH)₂) that forms in the oxidation zones of copper ore deposits, where copper-bearing solutions interact with carbonate minerals. Its intense, banded green coloration is produced by copper — the same element that turns a copper roof green with age. The characteristic banding and swirling patterns visible in polished malachite reflect the botryoidal (rounded, grape-like) and stalactitic growth habit of the mineral, with each band representing a period of mineral deposition. Malachite has been mined as a copper ore and ornamental stone since antiquity. This specimen weighs 58g. Locality not independently verified. ⚠️ Safety note: malachite dust and powder are toxic — do not sand, grind, or inhale. Wash hands after handling. Keep away from children.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eMalachite’s green is copper’s signature in oxidized form — the same chemistry that produces the green patina on copper statues, old coins, and weathered bronze. In malachite, that copper chemistry has crystallized into a mineral with some of the most visually distinctive banding in the natural world. The Ural Mountains of Russia produced malachite in slabs large enough to clad the columns of Saint Isaac’s Cathedral in St. Petersburg — still one of the most dramatic deployments of a mineral in architectural history. The pattern on this 58g specimen is a miniature version of the same geological process.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe banding and swirling pattern are well-developed and clearly visible — the color is rich and consistent. At 58g it has real display presence. A strong piece for a copper mineral collection or any display that values dramatic natural pattern over subtle color.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Malachite specimen (copper carbonate hydroxide)\u003cbr\u003eWeight: 58g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural specimen — wash hands after handling; do not grind or sand. Please review photographs for banding, color, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980424106169,"sku":"G324066","price":25.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/A1AF5815-22D6-44F1-95F3-2C7FEED2F57F.jpg?v=1783134491"},{"product_id":"tiger-s-eye-stone-of-courage-grounded-confidence","title":"Tiger’s Eye Polished Freeform — Golden \u0026 Dark Brown Chatoyant Bands — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished tiger’s eye freeform — golden and dark brown chatoyant bands shifting with a silky, light-catching movement as the viewing angle changes. The optical effect is immediately visible and strong on this piece. A stone that earns its name.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eTiger’s eye is a chatoyant variety of quartz that forms through the pseudomorphic replacement of crocidolite (blue asbestos) fibers by silica — the parallel fibrous structure of the original asbestos is preserved in the quartz replacement, and it is those aligned microfibers that produce the chatoyancy (the silky, moving light band) through a phenomenon called the cat’s eye effect. The golden-brown coloration is produced by iron oxide (limonite\/goethite) staining the quartz fibers during the replacement process. The chatoyant band moves as the stone rotates because the fibers reflect light most strongly when perpendicular to the light source. Most tiger’s eye on the market originates from South Africa, though the locality of this specimen has not been independently verified. Weight not confirmed — please update before publishing.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eTiger’s eye is one of the more geologically interesting chatoyant stones because its optical effect is a record of a complete mineral replacement — the crocidolite that originally formed here no longer exists as crocidolite, but its fibrous structure was preserved perfectly in the silica that replaced it. The chatoyancy is the ghost of an earlier mineral, preserved in the geometry of its successor. The golden color is iron’s contribution, oxidizing in the silica matrix over geological time.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe chatoyancy on this piece is strong and well-defined — the golden and dark brown bands are clearly differentiated and the silky light band is visible in the photographs. The polished freeform allows the chatoyancy to be appreciated from multiple angles. A visually immediate piece that photographs well and handles well.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Tiger’s eye polished freeform (chatoyant quartz pseudomorph after crocidolite)\u003cbr\u003eWeight: [CONFIRM WEIGHT]\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished freeform — please review photographs for chatoyancy, banding, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980424171705,"sku":"3825203","price":18.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/original_354ad8e3-bb05-47c6-861d-c65334a7ffbd.jpg?v=1780807638"},{"product_id":"yellow-calcite-heart-stone-of-joyful-clarity-gentle-vitality","title":"Yellow Calcite Heart Carving — Warm Golden Tone, Polished, 299g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eA polished heart-shaped carving, 299g — warm golden hue reminiscent of soft sunlight, smooth surface enhancing the natural glow of the stone. Substantial in weight for a carved form. A piece that radiates warmth before you even pick it up.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eThis specimen is presented as yellow calcite based on its appearance and color characteristics. Calcite (calcium carbonate, CaCO₃) is one of the most common minerals on Earth, occurring in a wide range of colors depending on trace impurities. Yellow calcite gets its warm golden tone from trace iron or other inclusions distributed through the calcium carbonate structure. Calcite is relatively soft (Mohs 3) and cleaves readily — the smooth polished surface of this carving reflects careful lapidary work. The material identification has not been independently laboratory verified. This specimen weighs 299g.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eThe heart form is one of the oldest shapes in lapidary carving — but at 299g, this is a heart with genuine weight and presence rather than a token piece. Yellow calcite’s warm transparency gives the carved form a depth that opaque stones don’t produce: the golden tone shifts slightly as light moves across the polished surface, and the mass of the piece anchors it as an object rather than a decoration. A carved mineral at this weight is a commitment to a material, not just a shape.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe color is warm and consistent, and the polish is clean. At 299g the heart form is substantial — it sits firmly and reads as a display object rather than a small accent piece. A strong piece for a crystal collection that includes carved forms alongside natural specimens.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Yellow calcite heart carving (polished, lapidary form) — material presented as calcite based on appearance; not independently verified\u003cbr\u003eWeight: 299g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Polished carving — calcite is soft (Mohs 3); handle with care to avoid scratching. Please review photographs for color, polish, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980424204473,"sku":"H962338","price":40.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/IMG-1510.jpg?v=1783134254"},{"product_id":"amazonite-stone-of-calm-truth-soothing-balance","title":"Amazonite Specimen — Blue-Green Microcline Feldspar, 11g — Field Find","description":"\u003cp\u003e\u003cstrong\u003eTHE FIND\u003c\/strong\u003e\u003cbr\u003eAn amazonite specimen, 11g — cool blue-green microcline feldspar with the quiet color of water seen through stone. Small in size, notable in color. At 11 grams it is an easy piece to keep, carry, or add to a growing mineral collection.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHAT WE KNOW\u003c\/strong\u003e\u003cbr\u003eAmazonite is the blue-green to green variety of microcline, a potassium aluminum silicate (KAlSi₃O₈) feldspar. It is the color that distinguishes it — ordinary microcline is white to pale pink; amazonite’s blue-green coloration is produced by trace amounts of lead and water in the crystal structure, which was only confirmed by research in the 1980s. It forms in granitic rocks and pegmatites, often occurring alongside quartz, smoky quartz, and other pegmatite minerals. The pale white veining commonly visible in amazonite specimens is feldspar cleavage and albite intergrowth within the microcline. This specimen weighs 11g. Locality not independently verified.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eTHE STORY\u003c\/strong\u003e\u003cbr\u003eAmazonite’s name comes from the Amazon River — though no significant amazonite deposits have ever been confirmed in the Amazon basin. The name predates modern mineralogy and likely reflects the green stones traded from the region in pre-Columbian and early colonial periods, which may or may not have been amazonite. The color mechanism was debated for over a century before trace lead was identified as the cause in the 1980s — one of the more recently resolved color mysteries in common mineralogy.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eWHY WE CHOSE IT\u003c\/strong\u003e\u003cbr\u003eThe blue-green color is the whole case for this piece — the distinctive cool tone is immediately recognizable and gives even an 11g specimen a distinctly serene character. A compact and affordable entry point for feldspar collectors or anyone drawn to cool blue-green mineral color.\u003c\/p\u003e\u003cp\u003e\u003cstrong\u003eABOUT THIS PIECE\u003c\/strong\u003e\u003cbr\u003eType: Amazonite (blue-green microcline feldspar)\u003cbr\u003eWeight: 11g\u003cbr\u003eLocality: Not independently verified\u003cbr\u003eCondition: Natural specimen — please review photographs for color, veining, and natural variation.\u003cbr\u003eQuantity: 1 — one of a kind.\u003c\/p\u003e","brand":"Found in the Field","offers":[{"title":"Default Title","offer_id":46980424335545,"sku":"8936648","price":18.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0782\/9438\/4825\/files\/E95166A4-929A-4B15-A177-1BB98FB6EF71.jpg?v=1782005287"}],"url":"https:\/\/foundinthefield.store\/collections\/minerals-geological-specimens.oembed","provider":"Found in the Field","version":"1.0","type":"link"}