| Locality type: | Mine |
| Classification |
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| Species: | 'Serpentine Subgroup' (not an IMA approved species) |
| Formula: | D3[Si2O5](OH)4 |
| Confirmation |
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| Validity: | Believed Valid |
| Associated Minerals: |
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| Associates: | Magnetite
Troilite
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| Data |
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| Mineral Data: | Click here to view Serpentine Subgroup data |
| Locality Data: | Click here to view Alta Mine, Low Divide, Low Divide Mining District, Klamath Mountains, Del Norte County, California, USA |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 686559 |
| Long-form Identifier: | 1:3:686559:7 |
| GUID (UUID V4): | 5b6c2ac7-33cb-4209-95b8-0f6f3fefd0cc |
| Nearest other occurrences of Serpentine Subgroup |
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| 10.0km (6.2 miles) | ⓘLower Elk Camp Ridge deposit (Ridge claims; Ridge Nickel claims; GTR claims Nos. 1-18), Gasquet, Klamath Mountains, Del Norte County, California, USA |
| 10.2km (6.3 miles) | ⓘUnnamed Ni occurrence [1], Rockland, Diamond Creek Mining District, Klamath Mountains, Del Norte County, California, USA |
| 11.9km (7.4 miles) | ⓘCleopatra Mine (Dedrick Mine), Rockland, Diamond Creek Mining District, Klamath Mountains, Del Norte County, California, USA |
| 15.0km (9.3 miles) | ⓘWebb Mine, High Dome, Patrick Creek Mining District, Klamath Mountains, Del Norte County, California, USA |
| 15.0km (9.3 miles) | ⓘBig Boy Mine (Big Boy group; Big Boy Cinnabar group), Rockland, Diamond Creek Mining District, Klamath Mountains, Del Norte County, California, USA |
| 18.0km (11.2 miles) | ⓘCamp 7 group, French Hill, Klamath Mountains, Del Norte County, California, USA |
| 23.0km (14.3 miles) | ⓘLast Drink No. 1 Occurrence (Blue Bucket No. 5), Waldo Mining District, Josephine County, Oregon, USA |
| 41.3km (25.7 miles) | ⓘTennessee Chromite Occurrence, Waldo Mining District, Josephine County, Oregon, USA |
| 41.5km (25.8 miles) | ⓘUnnamed gemstone occurrence [6], Preston Peak, Klamath Mountains, Siskiyou County, California, USA |
| 41.6km (25.8 miles) | ⓘBowser Mine, Illinois River Mining District, Curry County, Oregon, USA |
| References |
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| Reference Search (possible matching items) |
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 | | Book (edition) | | (Brazil). Malcolm Back (Canada), Henry L. Barwood (USA). Dmitriy Belakovskiy (Russia). Fabio Bellatreccia...(Italy), T.S. Ercit (Canada). Alexander Falster (USA). Jeffrey de Fourestier (Canada). Robert Gault (Canada)...Henderson. Jr. (USA). D.D. Hogarth (Canada). J.L. Jam bor (Canada), Anthony R. Kampf (USA). Pave! M. Kartashov...Karnp-Moller (Denmark). Akira Kato (Japan). Lance E. Keams (USA). Elisabeth Kirchner (Austria), Uwe Kolitsch (Austria)...Republic). Per Nystcn (Sweden), David O'Hanlcy (USA). Filippo Olmi (deccased) (ltaly). Werner H. Paar |  | Gaines, Richard V., Skinner, H. Catherine W., Foord, Eugene E., Mason, Brian, Rosenzweig, Abraham, King, Vandall T. (1997) Dana's New Mineralogy (8th ed.) Wiley-Interscience. p.1872 | Book (edition) | | Cisneros: Minerological Research Co., San Jose, California. Andrew M. Clark: Dept. of Mineralogy, Natural...Currier: Jewel Tunnel Imports, Baldwin Park, California. Stanley Dyl: Seaman Mineralogical Museum, Michigan...Canada. Richard C. Erd: U.S.G.S., Menlo Park, California. Howard T. Evans: U.S.G.S., Reston, Virginia...Claren N. (‘‘Si’’) and Ann Frazier: Berkeley, California. Carl Francis: Mineralogical Museum, Harvard...Paris, France. Legrand A. Gould: Pebble Beach, California. George E. Harlow: Dept. of Min. Sci., American |  | | Book | | a world leader in the production of e0pper. the mining areas of Cornwall and Devon became important producers...player in world zinc produ.:tion. Th· development of mining tin particular during the 18th and 19th centuries)...continue unabated despite there n '" being , ·~- link mining acti,·ity in Britain or Ireland. My original intention...onNewMinerals,Nomenclature andClass::ication. Co. County. EMPElectronmicroprobe - an instrument usedto ...with older fluorite specimens from Weardale in County Durham being a case in point. Many of these specimens |  | | Book | | nonstoichiometric chemical species in quantities low ≤10%) dramatic changes in the electronic, optical...different structure which completely depends on their mining source. They are known as hydrous phyllosilicate...have low shrink-swell capacity when clay is wetted. Kaolinite does not swell in water and have low surface...centimole/kg). Due to the low surface area and little isomorphous substitution, Kaolinite has low capacity to adsorb...mainly at relatively low temperatures (° C) or upon being directed to conditions of low relative humidity |
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