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Antigorite  | | | | Habit: | thin lamellar, laminae easily separable into translucent folia | | Colour: | leek green to violet in "chromium" variety | | Description: | Antigorite occurs both with typical leek green coloration and the violet coloration of so named "Chromium" Antigorite. Specimens of Chromium Antigorite were often reffered to as Kammererite, or Chromium Clinoclore, but this is inaccurate. (see www.pennminerals.com/museum.htm for a good image of an actual, and very rare, Kammererite from Woods Chrome). Specimens of Chromium Antigorite from this occurance even fall somewhat short of a true Antigorite identity, but is closest to this family member of the Sepentine group. | | Reference: | [Mineralogy of Pennsylvania - 1922; Samuel S. Gordon Pg.124] |
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Antigorite var: Picrolite  | | | | |
Aragonite  | | | | Reference: | [Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 190; Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania] |
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Brucite  | | | | Habit: | tabular plates with pseudo-hexagonal edging. usually foliaed masses | | Colour: | white to pale green, pearly to waxy luster, transparent in thin sections/plates | | Fluorescence: | bright blue-white response | | Description: | Worlds finest locality for the Brucite, hosting the largest crystal ever found (to 0.2m). Crystals from here are rich and well developed, in numerous modifications including large tabular crystals and occasional groups in rosettes. coloration from this locale tends towards pale green coloration in the richest specimens. | | Reference: | [Ref1) Dana 6: 1069. Ref2) Mineralogy; J. Sinkankas, 1964 pg. 339 Ref3) Preliminary Report on The Mineralogy of Pennsylvania 1874; F. A. Genth; pg. 51] |
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Cacoxenite  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania] |
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Calcite  | | | | |
'Chalcedony'  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania] |
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Chromite  | | | | Habit: | massive, fine grained. frequent admixture with Serpentine | | Colour: | Blackish grey | | Fluorescence: | none | | Description: | Chromite, the Major ore at Wood's Mine. By 1874 report, Chromite production in PA was already waining, however the production to date at Wood's Mine of 120,000 tons, exceeded 20 times the production of all other PA chomite mining localities combined. | | Reference: | [Dana 6: 1069. ref2) 2nd Geological Survey of Pennsylvania, Preliminary report 1874; F. A. Genth, Pgs. 39-43] |
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Chrysotile  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania] |
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Clinochlore  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania] |
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Clinochlore var: Chromian Clinochlore  | | | | |
'Deweylite'  | | | | |
Dolomite  | | | | |
Dozyite  | | | | Reference: | [MinRec 27:301] |
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Enstatite  | | | | Reference: | [ Dana 6:1069.] |
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Forsterite  | | | | Reference: | [Ref.: Reed, Juliet C. (1976), Annotated Biblio. of Minerals New to the PA List 1965-1974, The Min. Soc. of PA, Inc.: 40; Gordon, Samuel G. (1922), Mineralogy of PA: 88.] |
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Hematite  | | | | Reference: | [ Dana 6:1069.] |
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Hydromagnesite  | | | | Reference: | [Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 273; Mineralogy of Pennsylvania, S. Gordon pg. 69 (ref. Smith and Brush, 1853, 214) ] |
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Ilmenite  | | | | Reference: | [ Dana 6:1069.] |
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Lizardite  | | | | Reference: | [The Mineralogy of Pennsylvania 1922-1965; A. Montgomery pg. 55 (MSP Newsletter, June, 1963, pg. 8. PM8)] |
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Magnesiochromite  | | | | Reference: | [No reference listed] |
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Magnesite  | | | | |
Magnetite  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania] |
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'Marmolite'  | | | | Reference: | [ Dana 6:1069.] |
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Millerite  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania; Dana 6:1069.] |
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Pimelite  | | | | Reference: | [Gaines et al. 1997, Dana\'s System of Mineralogy] |
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Pyrite  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania] |
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Pyroaurite  | | | | |
'Serpentine Group'  | | | | Habit: | crystaline Massive | | Colour: | brilliant green | | Fluorescence: | none | | Description: | Type locality for variety "Williamsite", a gemmy bright green serpentine often used as a semi-precious stone. Often associated with Chromite at this locality. discovered in 1849 by Lewis W. Williams, whom also first described Zaratite (Emerald Nickel) at Wood's Chrome Mine the same year. | | Reference: | [ Dana 6:1069. Ref2) American Republican, Jan. 2nd 1849 (Chester Co., Newspaper)] |
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Uvarovite  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania; Dana 6:1069.] |
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Vesuvianite  | | | | Reference: | [Lapham & Geyer, 1965. Mineral Collecting in Pennsylvania] |
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Zaratite  | | | | Habit: | crystaline massive veins and coatings typical, admixture with Dolomite | | Colour: | Brilliant Green | | Fluorescence: | none | | Description: | Lewis W. Williams first described Zaratite, as "Emerald Nickel" at Wood's Chrome Mine in 1849, nearly making Wood's Chome Mine "Type Locale" for the species. (TL: Spain 1851) Frequently occuring in admixture with micro crystals of dolomite, referred to localy as "pennite". | | Reference: | [American Republican, Jan. 2nd 1849 (Chester Co., Newspaper); 2nd geological Survey of Pennsylvania Preliminary Report 1874, F. A. Genth, Pg 156B; Dana, E.S. (1892) System of Mineralogy, 6th. Edition, New York: 1069; Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 246.] |
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