Fluorite
A World Specimen Guide

Dense web edition: chemistry, crystal forms, mining methods, country chapters, Jason Souza collector photo plates, compact photo plates, zoom controls, and an easy 20-question quiz in a two-page book view.

Dense web edition: chemistry, crystal forms, mining methods, country chapters, Jason Souza collector photo plates, compact photo plates, zoom controls, and an easy 20-question quiz in a two-page book view.
This flipbook is designed for web reading rather than a printed Word layout. Paragraphs may continue from one page idea to the next, but tables are kept as compact single-page panels so you do not get awkward blank areas or split table rows.
Safety note: mines, caves, dumps, adits, and quarries may be private, unstable, flooded, or legally restricted. This guide is for specimen study and does not grant collecting access.
Study tip: as you read, compare crystal habit, matrix, associations, color zoning, and labels. A single clue rarely proves a locality, but several clues together can make an identification much stronger.




Formula: CaF2. Fluorite is a halide mineral: one Ca2+ ion balances two F- ions. The chemistry is simple; the collector variety comes from trace elements, radiation damage, growth defects, inclusions, and changing fluid chemistry.
| Property | Value |
|---|---|
| Class | Halide |
| Crystal system | Isometric / cubic |
| Hardness | Mohs 4 |
| Cleavage | Perfect octahedral |
| Luster | Vitreous |
| Streak | White |
| Common habits | Cubes, octahedra, modified cubes, massive, crusts |





Most fine fluorite specimens form where calcium-bearing rocks or fluids meet fluorine-bearing hydrothermal fluids. The key reaction is simple in concept: dissolved calcium and fluoride become low-solubility calcium fluoride, then grow on open surfaces.

Crystal quality depends on open space. Massive fluorite can be an ore; collector fluorite usually requires a pocket, vug, vein opening, or fissure where faces can grow without being crushed.




Fluorite can be purple, green, yellow, blue, pink, colorless, gray, black, or multicolored. The basic formula remains CaF2; color is usually controlled by defects, trace elements, radiation history, and repeated growth pulses. This is why the same district can produce several colors.
| Feature | Collector meaning |
|---|---|
| Color zoning | Multiple fluid pulses or changing chemistry during growth. |
| Phantoms | Earlier crystal outlines preserved inside later growth. |
| UV response | Activation by trace impurities/defects; useful but not a locality proof. |
| Cleavage bruises | Fluorite breaks along perfect octahedral cleavage; inspect edges carefully. |
| Matrix | Often the best clue: sphalerite, barite, quartz, calcite, dolomite, stibnite, etc. |





Specimen mining is slower than ore mining because the goal is to expose pockets without destroying crystal faces. A mining level may cut through massive ore for years before a single world-class pocket appears.




Fluorite belongs to the isometric crystal system, which means its best-known shapes are built from equal axes and high symmetry. In collecting language, this is why people talk about cubes, modified cubes, octahedra, stepped faces, and geometric phantoms.

Shape matters because it records growth conditions. Sharp cubes often grew freely in open pockets. Stepped faces may record pulsed growth. Rounded “bubble” surfaces usually mean botryoidal or globular masses made of many tiny crystals rather than one large cube.




Cubes are the classic fluorite habit. A good cube has flat faces, crisp edges, and a glassy luster. Many world localities are recognized partly by cube color, matrix, and associations: Weardale green, Illinois purple-yellow zoning, Elmwood purple on sphalerite/dolomite, Asturias blue-violet with baryte, and Okorusu color zoning.
Stepped cubes form when growth advances unevenly across the face. They can look like terraced stairs. This may happen during changes in temperature, fluid chemistry, saturation, or growth speed.
Phantoms are earlier crystal outlines preserved inside later transparent growth. They are especially useful because they prove the crystal grew in multiple stages rather than all at once.
| Feature | What to look for |
|---|---|
| Sharp cube | Flat square faces and clean 90° edges. |
| Stepped face | Terraces, growth ledges, or stacked smaller cubes. |
| Phantom | Colored internal outline following the crystal shape. |
| Zoning | Color bands parallel to faces, corners, or growth layers. |
| Damage | Cleavage chips, bruised corners, repaired plates, or saw marks. |




Fluorite has perfect octahedral cleavage. That means a broken piece may naturally split into shapes bounded by triangular faces. Some specimens are true growth octahedra; others are cleaved or etched pieces. The difference matters for both identification and value.
When someone says “octagon fluorite,” they usually mean a crystal with beveled corners or an octahedral/cuboctahedral outline, not a true two-dimensional octagon. In a collection label, use the more precise term when possible.




Not all fluorite is a perfect cube. “Bubble fluorite” is a trade-style description for rounded, globular surfaces. The more formal term is often botryoidal when the surface resembles a bunch of grapes. These forms can develop when many tiny crystals grow together over a curved surface or when later growth coats an uneven matrix.
Drusy fluorite is a sparkling crust of small crystals. Massive fluorite has no obvious crystal faces and may represent ore, vein fill, or lapidary material. Cleaved fluorite can show attractive geometric pieces, but those faces are breaks rather than original growth surfaces.
| Habit | Simple description |
|---|---|
| Cubic | Square faces; most familiar collector form. |
| Octahedral | Eight triangular faces or cleavage form. |
| Botryoidal / bubble | Rounded globular masses; often many tiny crystals. |
| Drusy | Coating of small sparkling crystals. |
| Massive | Compact vein or ore material without clear faces. |
| Cleaved | Broken along natural planes; geometric but not always grown that way. |




Fluorite ore is mined as fluorspar, a source of fluorine used in metallurgy, chemicals, ceramics, and specialty applications. Collector specimens are a small part of the story. Many beautiful crystals were rescued from mines whose main goal was industrial production, zinc, lead, silver, or polymetallic ore.

The same mine can produce both massive ore and display specimens. The difference is open space: a vein packed solid with fluorite is ore, while a clay-lined vug or pocket can preserve freestanding crystals.





In underground mines, workers follow veins, replacements, breccias, or ore zones through drifts and stopes. A specimen pocket may appear as a clay seam, a hollow zone, a fault opening, or a vug lined with crystals.
Specimen recovery is careful work. Miners may remove loose clay by hand, undercut matrix, support fragile plates, and trim surrounding rock so a specimen can be extracted without snapping cubes from the base.




Some fluorspar deposits are mined in open pits or quarries, especially when ore lies near the surface. Open-pit work can expose broad zones quickly, but it may be harder to preserve delicate pockets because equipment is large and material moves fast.
| Mining style | What it is | Specimen impact |
|---|---|---|
| Underground vein mining | Drifts, shafts, stopes, or adits follow mineralized zones. | Good pockets may be recoverable if workers slow down. |
| Open pit / quarry | Benches remove surface-accessible ore bodies. | More exposure, but heavy equipment can damage crystals. |
| Reworking dumps | Collectors or operators search old waste rock. | Useful for study pieces; crystals may be weathered or broken. |
| Ore processing | Crushing, grinding, sorting, and concentration separate fluorite. | Great for industry, destructive for specimens. |
After extraction, specimens may be washed, trimmed, stabilized, photographed, and labeled. A professional specimen should keep its story: mine, level or pocket if known, date, associated minerals, and any repairs or cleaning.




England is a cornerstone of fluorite collecting. Weardale in County Durham is famous for green and purple cubic fluorite, especially daylight-fluorescent material from Rogerley and modern UK Mining Ventures localities. Derbyshire adds Blue John, a banded ornamental fluorite mined around Castleton.




Rogerley was found in an abandoned nineteenth-century quarry in the early 1970s; modern specimen operations have been documented from the Cumbria Mining and Mineral Company period and later UKMV activity.




| Locality | Region | Specimen signature | Status / history |
|---|---|---|---|
| Rogerley Mine | Frosterley, Weardale | Daylight-green cubes; purple zoning; strong fluorescence | Discovered early 1970s; specimen operations in modern periods. |
| Boltsburn Mine | Rookhope, Weardale | Purple/green cubes; classic fluorescence | Historic lead/fluorspar mine; closed historic source. |
| Heights Mine | Westgate, Weardale | Green to purple color-change fluorite | Historic locality; valued old collection pieces. |
| Diana Maria / Lady Annabella | Weardale | Modern green fluorite pockets | Modern collector mining associated with UKMV. |
| Blue John / Treak Cliff | Castleton, Derbyshire | Banded purple-blue/yellow fluorite | Historic ornamental mining; controlled small-scale extraction. |






The United States has two classic fluorite identities. The Illinois-Kentucky Fluorspar District was an industrial powerhouse and produced purple, blue, yellow, and zoned cubes. The Elmwood-Carthage district of Tennessee produced some of the most recognizable purple cubes on sphalerite, dolomite, calcite, and barite.




American labels should be read carefully: mine name, county, district, and associated minerals often matter more than color.




| Locality | Region | Specimen signature | Status / history |
|---|---|---|---|
| Minerva No. 1 / Mahoning area | Hardin Co., Illinois | Purple, blue, yellow, zoned cubes; barite/calcite/sphalerite | Historic district mine; most specimen production is past. |
| Denton Mine | Hardin Co., Illinois | Color-zoned cubes with barite/calcite | Historic fluorspar mine with high-quality cabinets. |
| Cave-in-Rock district | Southern Illinois | Large plates; purple/blue/yellow fluorite | Historic industrial district; many workings inactive/reclaimed. |
| Elmwood Mine | Smith Co., Tennessee | Purple cubes on sphalerite, dolomite, calcite, barite | Zinc mine famous for specimens recovered during operations. |
| Blanchard and western veins | New Mexico/western USA | Purple, blue, green fluorite veins | Regional collectors; access and output vary. |
The United States is also important for industrial fluorspar history, but not every fluorspar deposit produced cabinet-grade crystals.




Mexico combines world-famous mining districts with distinct fluorite styles. Naica, in Chihuahua, is known to collectors for pale green to clear fluorite with calcite, galena, sphalerite, and complex modified faces. The district is also famous for giant gypsum caves, useful as a dramatic example of long-lived hot mineral fluids in open cavities.


Ojuela and Mapimi add a polymetallic collector tradition where fluorite may appear with colorful oxidized minerals.




| Locality | Region | Specimen signature | Status / history |
|---|---|---|---|
| Naica Mine | Saucillo, Chihuahua | Pale green to clear fluorite with calcite, galena, sphalerite; complex faces | Historic/modern Pb-Zn-Ag mine; old workings consolidated under Naica name. |
| Cave of the Swords | Naica Mine | Gypsum crystal cave, not fluorite | Discovered in 1910; formation context for crystal growth in open space. |
| Cave of the Crystals | Naica Mine | Giant gypsum crystals; not fluorite | Discovered in 2000; dangerous heat/humidity when exposed. |
| Ojuela Mine | Mapimi, Durango | Fluorite as accessory with oxidized minerals | Historic polymetallic mine and classic specimen district. |
| Chihuahua regional mines | Northern Mexico | Fluorite with calcite/barite/sulfides | Mine-by-mine status varies; district labels are common. |




China is one of the dominant sources of modern fluorite specimens. Hunan produces fluorite in complex magmatic-hydrothermal and polymetallic systems; Guizhou localities such as Banpo add dramatic fluorite-stibnite combinations; Inner Mongolia and other regions produce blue, purple, and trade-named materials.


Chinese specimens can resemble English, Spanish, African, or North American fluorite by color. Associations and exact mine labels are essential: quartz, stibnite, sulfides, tungsten-tin minerals, calcite, and matrix are often the best clues.




| Locality | Province / region | Specimen signature | Status / history |
|---|---|---|---|
| Yaogangxian Mine | Hunan | Fluorite with quartz, sulfides, W-Sn-polymetallic associations | Major active/historic polymetallic district with specimen production over multiple periods. |
| Xianghualing / Xianghuapu | Hunan | Green and purple fluorite with quartz/calcite/sulfides | Important modern specimen area; individual mine status varies. |
| Banpo Mine | Guizhou | Fluorite with stibnite; gray/purple crystals with metallic contrast | Polymetallic hydrothermal locality known in specimen trade. |
| Inner Mongolia localities | Inner Mongolia | Blue, purple, zoned fluorite; dealer trade names occur | Exact mine data is critical; broad trade terms can obscure provenance. |




Asturias is Spain’s fluorite heartland. Berbes, La Viesca, Moscona, and La Collada produced blue, violet, yellow, and zoned fluorite, often with baryte, quartz, calcite, and sulfides. Spanish fluorite often has a watery, glassy look with phantoms and crisp cubic faces.


Asturian deposits are typically hydrothermal vein and replacement systems. Repeated fluid pulses produced phantoms and zoning; open pockets produced the best collector faces.




| Locality | Region | Specimen signature | Status / history |
|---|---|---|---|
| Berbes mining area | Ribadesella / Caravia, Asturias | Blue-violet fluorite, baryte, quartz, phantoms | Historic twentieth-century mining area; classic specimens. |
| La Viesca Mine | Siero, Asturias | Teal to blue fluorite with purple phantoms | Major modern-classic locality; access/status changed over time. |
| Moscona Mine | Corvera de Asturias | Yellow to blue fluorite with baryte/calcite | Important Asturian fluorspar mine and specimen producer. |
| La Collada | Asturias | Purple/blue fluorite, quartz, baryte | Classic locality; exact mine labels vary on older pieces. |




France has two fluorite worlds: mine fluorite and Alpine fissure fluorite. Valzergues is associated with yellow to honey-yellow cubes. Le Beix is a classic purple fluorite source. Alpine fissures in the Mont Blanc region are prized for delicate pink fluorite with quartz and adularia.


French identification often begins with color but should end with associations: Alpine pieces tend to show quartz/adularia and delicate fissure aesthetics, while mine pieces show vein textures and mine labels.




| Locality | Region | Specimen signature | Status / history |
|---|---|---|---|
| Valzergues Mine | Aveyron | Yellow to honey fluorite cubes and groups | Historic small mine; exact status details are source-dependent. |
| Le Beix Mine | Puy-de-Dome | Purple fluorite cubes; classic collection material | Historic fluorite mine; old collection specimens common. |
| Mont Blanc / Alpine fissures | French Alps | Pink fluorite with quartz/adularia | Fissure-collected material; rules and access are highly local. |
| Fontsante and other districts | Var and elsewhere | Purple, green, yellow fluorite from hydrothermal veins | Important regional sources with variable specimen output. |




Germany’s fluorite story is deep and historic. The Woelsendorf district in Bavaria has mining roots reported as fifteenth century or earlier, first for lead and later for fluorite. The last mine in that district, Hermine, is commonly noted as closing in 1987. The Clara Mine in the Black Forest adds a continuing collector tradition with fluorite among a broad suite of minerals.






| Locality | Region | Specimen signature | Status / history |
|---|---|---|---|
| Woelsendorf district | Bavaria | Yellow, honey, brown, purple, zoned fluorite | Mining began in 15th century or earlier; last mine Hermine closed in 1987. |
| Hermine Mine | Woelsendorf district | Classic district fluorite and ore minerals | Last mine of the district; closed 1987. |
| Clara Mine | Black Forest | Fluorite with barite, quartz, sulfides | Long collector tradition; controlled collecting/dump availability varies. |
| Saxony / Erzgebirge localities | Eastern Germany | Fluorite in polymetallic vein systems | Historic mining districts; specimen output variable. |




Okorusu in Namibia produced abundant collector fluorite, famous for green, purple, yellow, and color-zoned crystals. Riemvasmaak in South Africa is a modern favorite for bright green fluorite, often showing stepped cubes and strong color.




African fluorites can overlap visually with English, Chinese, Canadian, or Spanish green fluorite. Matrix, exact mine name, and associations remain essential.




| Locality | Country / region | Specimen signature | Status / history |
|---|---|---|---|
| Okorusu Mine | Otjozondjupa, Namibia | Green, purple, yellow, zoned cubes; sometimes large plates | Major fluorite mine and prolific specimen source; production/status varied over time. |
| Riemvasmaak | Northern Cape, South Africa | Bright green cubes and stepped forms | Modern classic locality; access is locality-specific. |
| El Hammam Mine | Morocco | Green/purple/colorless fluorite with calcite and pyrite | Morocco’s principal fluorite mine in many references; recent status should be verified. |
| Aouli / Mibladen districts | Morocco | Fluorite in polymetallic settings | Better known for other species, but fluorite can occur. |




Canada is known for the Madoc area of Ontario and the Rock Candy Mine in British Columbia, especially apple-green to emerald-green fluorite and barite associations. Russia is strongest in collector memory through Dalnegorsk, where colorless to pale “ice cube” fluorite appears with a broad polymetallic suite.
Morocco is represented strongly by El Hammam, a major North African fluorite locality with green, purple, colorless, calcite, and pyrite combinations. Italy, Switzerland, Pakistan, Peru, Argentina, and other countries add regional fluorite identities that may be less common in beginner collections but important globally.
| Country | Collector identity |
|---|---|
| Canada | Madoc green fluorite; Rock Candy apple-green cubes/octahedra. |
| Russia | Dalnegorsk colorless to pale fluorite with quartz, calcite, sulfides, and skarn minerals. |
| Morocco | El Hammam green/purple/colorless fluorite with calcite or pyrite. |
| Switzerland | Alpine fissure pink or zoned fluorite with quartz/adularia. |




| Country | Representative localities | Collector notes |
|---|---|---|
| Canada | Madoc; Rock Candy Mine | Green fluorite with barite; apple-green octahedra/cubes; old labels important. |
| Russia | Dalnegorsk / Nikolaevskiy | Colorless “ice cube” fluorite; polymetallic matrix. |
| Morocco | El Hammam | Green/purple/colorless fluorite with calcite and pyrite. |
| Italy | Zogno/Camissinone; Sardinia | Purple to colorless fluorite in veins and Alpine-style contexts. |
| Switzerland | Alpine fissures | Pink and color-zoned fluorite with quartz/adularia. |
| Pakistan | Balochistan, Khyber Pakhtunkhwa, northern areas | Green, purple, multicolored fluorite; locality data often variable. |
| Peru | Polymetallic ore districts | Fluorite with quartz, pyrite, sphalerite, galena, barite. |
| Argentina | Patagonia and vein districts | Color-zoned fluorite, some lapidary/collector material. |




This collector-photo section uses Jason Souza specimen photos and label metadata. The images are compressed and cropped for web viewing, then arranged as dense plates so the open-book layout stays full instead of leaving large blank areas.
| Country | Photos | Mine / locality names |
|---|---|---|
| China | 9 | Dafeng Mine, Qinglong Mine, Xia Yang Mine, Xianghualing Mine, Yaogangxian Mine, Yindu Mine, Yunyang Mine |
| Germany | 1 | Anton Mine |
| Nigeria | 1 | Okene Mine |
| Peru | 1 | Milpo Mine |
| Spain | 2 | Berbes Mine, Moscona Mine |
| United Kingdom | 1 | Diana Maria Mine |




China is the strongest part of this collector set, with examples from Yaogangxian, Xianghualing, Yunyang, Qinglong, Yindu, Xia Yang, and Dafeng. The plate below shows how one country can produce very different colors and crystal presentations.






These remaining China specimens highlight locality variety: green-purple fluorite with muscovite, purple fluorite with the “tanzanite” trade look, and pink or strawberry-style fluorite. These are good study pieces because the captions combine color, habit, and locality.
| Country | Mine / locality | Region | Specimen | Color | Habit |
|---|---|---|---|---|---|
| China | Yaogangxian Mine | Hunan Province | Window Fluorite | Purple | Cubic |
| China | Yindu Mine | Inner Mongolia | Fluorite with Muscovite | Green, Purple | Cubic |
| China | Yunyang Mine | Henan Province | Yellow Bubble Fluorite | Yellow | Botryoidal |



This plate adds non-China examples from the collector plates. It gives the flipbook a broader collector feel: Spanish purple and yellow fluorite, German red fluorite with limonite, United Kingdom Rogerley-style fluorite, Peruvian fluorite with quartz and pyrite, and Nigerian blue fluorite.






| Country | Mine / locality | Region | Specimen | Color | Habit |
|---|---|---|---|---|---|
| Spain | Berbes Mine | Ribadesella | Purple Fluorite | Purple | Cubic |
| Spain | Moscona Mine | Spain | Yellow Fluorite | Yellow | Cubic |
| Germany | Anton Mine | Baden-Württemberg | Fluorite with Limonite | Red | Cubic |
| United Kingdom | Diana Maria Mine | Tiny Twins Pocket | Rogerley Fluorite | Green-Blue, Color-Changing | Cubic |
| Peru | Milpo Mine | Cerro de Pasco | Fluorite with Quartz and Pyrite | Green, Purple | Octahedral / Botryoidal |
| Nigeria | Okene Mine | Taraba | Nigerian Fluorite | Blue | Cubic |
These black-background collector study plates emphasize Chinese mine localities plus a Pakistan specimen, making them useful for comparing cubic, octahedral, botryoidal, and associated-mineral examples.
| Country | Photos | Mines / localities |
|---|---|---|
| China | 6 | De'an Mine, Huanggang Mine, Xianghualing Mine, Yaogangxian Mine, Yindu Mine |
| Pakistan | 1 | Kharan Fluorite Mine |




This plate includes Yindu, De'an, Xianghualing, Huanggang, Yaogangxian, and Kharan material. This is a good quick comparison page because it shows multiple habits on one comparison page: cubic fluorite, octahedral fluorite, botryoidal or bubble fluorite, and fluorite associated with pyrite, mica, siderite, chalcopyrite, and candle quartz.







This compact table records locality and visual habit information for the collector examples. It also supports the quiz and country chapters by giving readers real specimens to compare with the general formation, shape, and mining chapters.
| Country | Mine / locality | Region | Specimen | Color | Habit |
|---|---|---|---|---|---|
| China | De'an Mine | Jiangxi Province | Purple and Green Fluorite | Purple and Green | Octahedral |
| China | Huanggang Mine | Inner Mongolia | Blueberry Fluorite | Blue | Botryoidal |
| China | Xianghualing Mine | Hunan Province | Purple and Green Bubble Fluorite | Purple and Green | Botryoidal |
| China | Yaogangxian Mine | Hunan Province | Fluorite with Siderite and Chalcopyrite | Yellow | Cubic |
| China | Yindu Mine | Hunan Province | Purple and Green Fluorite | Purple and Green | Cubic |
| China | Yindu Mine | Hunan Province | Purple Fluorite with Pyrite | Purple | Cubic |
| Pakistan | Kharan Fluorite Mine | Kharan District | Fluorite | Yellow | Cubic |




| Term | Meaning |
|---|---|
| Phantom | Earlier growth stage visible inside a later crystal. |
| Zoning | Bands or regions of different color or clarity. |
| Vug / pocket | Open space where crystals grew freely. |
| Cleavage | Preferred breaking direction; fluorite cleavage is perfect octahedral. |
| Association | Other minerals present on the same specimen. |
| Repaired | Specimen has been glued or stabilized after damage. |




Collector photo plates: fluorite specimen photos courtesy of Jason Souza. These photos were optimized and cropped for the web flipbook, with label metadata standardized for public display.
Photo credits: local specimen photos are derived from credited images in the earlier guide set, including Rob Lavinsky / iRocks.com (CC BY-SA 3.0), Didier Descouens (CC BY-SA 4.0), Parent Gery (CC BY-SA 3.0), Hannes Grobe (CC BY-SA 2.5), and original diagrams created for this project. In-book detail images are crops of the credited source photos.
Remote in-situ photos: Blue John Cavern veins: Marcin Floryan, public domain. Treak Cliff Cavern Blue John pillar: Dave Pape, public domain. Naica Cave of the Crystals photo: Alexander Van Driessche, CC BY 3.0; it shows gypsum, not fluorite, and is used only for formation context.
| Source | Used for |
|---|---|
| Mindat.org mineral and locality pages | Fluorite properties, locality framework, mine/locality names. |
| Minerals Education Coalition / Smithsonian | Basic chemistry, hardness, crystal system, public mineral facts. |
| UK Mining Ventures / Rogerley references | Weardale and Rogerley specimen-mining context. |
| Wikimedia Commons file pages | Photo credit and license verification. |
| Public geological and mine-history references | District narratives and conservative status notes. |
Continue to the quiz.




Use this quiz as a simple study check after reading the flipbook. The questions are intentionally beginner-friendly and focus on the biggest ideas: chemistry, shape, hardness, mining, localities, and specimen care.





Click the button after answering all 20 questions. The page will mark correct and missed questions, then show your score below.
| # | Answer | Why |
|---|---|---|
| 1 | CaF₂ | Fluorite is calcium fluoride: CaF₂. |
| 2 | 4 | Fluorite is the reference mineral for Mohs hardness 4. |
| 3 | Isometric / cubic | Fluorite is isometric, which helps explain its cube and octahedral forms. |
| 4 | Cube | Cubes are the classic fluorite habit. |
| 5 | Octahedral | Fluorite breaks on perfect octahedral cleavage planes. |
| 6 | White | Fluorite usually has a white streak. |
| 7 | Vitreous / glassy | Most good fluorite crystals show vitreous, glassy luster. |
| 8 | Halide | Fluorite is a halide mineral. |
| 9 | Fluorescence | The word fluorescence is historically connected to fluorite. |
| 10 | No | Color helps, but matrix, associations, and labels are stronger evidence. |
| 11 | Open pockets or vugs | Open space lets crystal faces grow freely. |
| 12 | United Kingdom | Rogerley is in Weardale, County Durham, England. |
| 13 | Tennessee | Elmwood is a classic Tennessee locality. |
| 14 | Mexico | Naica is in Chihuahua, Mexico. |
| 15 | Calcite, quartz, barite, or sulfides | Fluorite commonly associates with calcite, quartz, barite, sphalerite, galena, pyrite, and others. |
| 16 | To protect crystal faces and matrix | Specimens are valuable when intact, so careful extraction matters. |
| 17 | 8 | An octahedron has eight triangular faces. |
| 18 | Botryoidal or globular | Bubble-like fluorite is often described as botryoidal or globular. |
| 19 | Avoid drops and rough handling | Fluorite is soft and cleaves easily, so handle it gently. |
| 20 | Locality and associated minerals | Good labels preserve locality, associations, provenance, and uncertainty. |
End of flipbook.
A strong fluorite identification comes from patterns, not one clue. Use the open-book photos to compare habit, matrix, associations, color zoning, luster, and specimen labels. When you add new pieces to your collection, photograph every side and record exactly what the label says.







