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- W2116882079 abstract "Abstract The gneiss and mica-schist of Eastern Tennessee strike south-west and north-east (about 47° E. of N.), and dip to the south-east (at angles of about 25°), running parallel to and forming an outer range of the Alleghany Mountains. Veins of copper and iron ores, with occasional quartz veins, lie in the schists, dipping parallel with them, and consisting of porous oxide of iron at top, with iron pyrites and carbonate and sulphuret of copper lower down. The veins are described as being sometimes 45 feet wide, and traceable for upwards of 70 miles ; but they are worked chiefly in the extreme south-east corner of Tennessee, in the township of Duckton, in the county of Polk, a district ceded by the Indians to the States about four years ago." @default.
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- W2116882079 date "1855-02-01" @default.
- W2116882079 modified "2023-10-16" @default.
- W2116882079 title "On the Occurrence of Copper in Tennessee, U.S." @default.
- W2116882079 doi "https://doi.org/10.1144/gsl.jgs.1855.011.01-02.06" @default.
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