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Ch. 6: Garnet

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GARNET.
249
gia, Massachusetts, and New Hampshire. Professor Ed­ward Hitchcock once exhibited to the author some beautiful cut precious garnets from Berkshire county, Massachusetts; the Hon. Mr. Clingman, IT. S. Senator from North Caro­lina, has some very handsome transparent garnets from his district in Buncombe county, North Carolina.
The common garnet is met with in dodecahedrons, from three to four inches in diameter, at Fahlun in Sweden, Arendal and Kongsberg in Norway, and the Zillerthal in Tyrol; in Moravia, Silesia, and Siberia; in granular lime­stone at Haslan, near Eger, in Bohemia ; beautiful crystals of a rich brownish-red color, disseminated in hornblende gneiss, are found in Hanover, New Hampshire, in the United States; dark blood-red and splendid dodecahedrons, with peached and truncated edges, at Franconia, New Hampshire, in geodes, in massive quartz, calcareous spar, and magnetic iron ore; at Carlisle, Massachusetts, beautiful geodes of crystals of transparent cinnamon color, accompa­nying scapolite in white limestone; at Monroe and Had-dam, Connecticut, imbedded in mica slate, also associated with chrysoberyl, beryl, automolite, and columbite; large dodecahedral crystals, two inches and more in diameter, of a dark brownish-red color, at New Fane and Marlborough, in chlorite slate; also in mica slate, in Chesterfield, Massa­chusetts.
Colophonite is a granular brown variety, and is found in Arendal, Norway, and forms a large vein in gneiss at Willsborough, New York, on Lake Champlain; a finer * graded variety of yellow and red colors is found on Rogers' Rock, at Lake George. The colophonite is com­posed of coarse, roundish particles, oil-green and honey-yellow colors, and often possesses a fine iridescence.
Allochroite is similar to colophonite, but the particles are impalpable and strongly coherent.
Ch. 6: Garnet Page of 515 Ch. 6: Garnet
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