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Ch. 4: Gem Minerals of Pegmatitic Dikes

Ch. 4: Gem Minerals of Pegmatitic Dikes Page of 87 Ch. 5: Quartz & Opal Text size:minus plus Restore normal size   Mail page  Print this page
28                 HISTORY OF THE GEMS FOUND IN NORTH CAROLINA.
the inclusions found in the greenish variety. This translucent variety, like the other, shows no striae.
The following analysis by Prof. Prank W. Clarke, made from a faint green variety, shows it to be a typical oligoclase. The specific gravity was determined to be 2.651. This has been cut into a transparent gem, and may be advantageously used for spectroscope, microscope, and other lenses.
Labradorite (Opalescent feldspar).—On the road to Charlotte, Mecklen­burg County, and near Bakersville, Mitchell County, specimens showing a slight blue chatoyancy are found. This domestic labradorite is scarcely used at all in the arts, as the mineral from Labrador is cheaper and of a much superior quality, and takes a fine polish.
Leopardite.—This is a rock composed largely of whitish feldspar (orthoclase and plagioclase), spotted black, perhaps by manganese oxide, and named from its leopard-like appearance. It is abundant near Charlotte, Mecklenburg County, and also in Gaston County. It is not a definite mineral, but a variety of porphyry with disseminated crystals of quartz, and occurs in large masses as a rock, so that it would furnish a good ornamental stone, if polished. This variety of spotted feldspar is peculiar to North Carolina, and has been described in detail in the report on Building Stones.
The beryl, zircon, and other gem minerals, which are also constituents of pegmatitic dikes, are described in the following chapters.
Ch. 4: Gem Minerals of Pegmatitic Dikes Page of 87 Ch. 5: Quartz & Opal
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