Ch. 2: Maine Pegmatites: Local Descriptions

Ch. 2: Maine Pegmatites: Local Descriptions Page of 170 Ch. 2: Maine Pegmatites: Local Descriptions Text size:minus plus Restore normal size   Mail page  Print this page
104              PEGMATITES AND ASSOCIATED ROCKS OF MAINE.
its solidification. Microscopically the effects of these movements are recognizable in local granulation within certain quartz and feld­spar individuals and marked strain in others.
The coarsest portions of the pegmatite have been worked for mica. A few of the muscovite books are as much as 1 foot across, but the majority are under 4 inches. The larger plates are only in part clear, being injured by ruling and twinning. The writer saw no plates that would cut clear pieces larger than 2 by 3 inches, and even such as would were rare. Most of the material could be utilized only for scrap mica. The property hardly appears to merit further develop­ment.
Beech Hill mica mine.—Another mica mine, located a Tew miles north of the first, on the farm of George L. Kimball, on Beech Hill, represents the most serious attempt at mica mining that has been made in the State. The mica occurs as a constituent of a sill-like mass of coarse pegmatite, which dips to the east at about 30°. Its thickness is at least 12 feet, the base not being exposed. Commer­cial mica is confined to a zone about 5 feet thick in the lowest part of the pegmatite layer as now exposed. Within this 5-foot zone muscovite is estimated to form from 10 to 20 per cent of the material of the pegmatite.
Some of the masses of pure orthoclase feldspar associated with the mica are 5 feet across, but the total quantity present is not sufficient to make it of commercial importance. Intergrowths of quartz and muscovite are common.
The pegmatite contains no biotite and no black tourmaline. The associated rock is a granite gneiss, and both gneiss and pegmatite are intruded by a dike of diabase.
Some of the muscovite books are 1 foot across, but most of them are under 5 inches. The larger plates are invariably cut up by ruling planes into a number of smaller pieces. Much of the mica is worthless for anything but scrap because of the prevalence of ruling, wedge structure, and twinning. Most of the thumb-trimmed mate­rial seen by the writer was in pieces 2 or 3 by 3 inches in size. The mine was not being worked at the time of the writer's visit in Sep­tember, 1906, and although several tons of mica lay in the trimming sheds, the best of the output was reported to have been sold. It was therefore impossible to make a wholly fair estimate of the aver­age value of the mica mined, but the quality of the material is supe­rior to that from any other known locality in Maine and appears to warrant further development.
The property was opened in 1900 and was also worked in 1902 by the Beech Hill Mining Company, who subsequently sold the prop­erty to New York persons. About a ton of thumb-trimmed mica was marketed at prices ranging from S cents to SI a pound, and
Ch. 2: Maine Pegmatites: Local Descriptions Page of 170 Ch. 2: Maine Pegmatites: Local Descriptions
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