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UNITED STATES, CANADA AND MEXICO
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long and 2 inches in diameter, but they are less beautiful than the small, colorless ones from Scopi, Switzerland.1 The original locality, Danbury, Conn., never furnished any gems.
Iolite
occurs at Haddam, Conn., in crystals occasionally 5 inches across,
which are often dark blue and sufficiently clear for cutting as gems.
Dr. John Torrey possessed a fine seal made of a cube of iolite from the
albite granite of Haddam, Conn., which displayed to the greatest
perfection, its dichroitic properties, being blue when viewed in one
direction, and white when viewed in the other, the blue being
remarkably fine. This locality promised well, but the supply of gem
material has been scant. An iolite-gneiss has recently been noticed by
Edmund O. Hovey, at Guil-
IOLITE
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ford,
Conn.' It was found near the Norwich and Worcester Railroad, between
the Shetucket and Quinebaug Rivers, where the gneiss has been quarried
for the road. At Brimfield, Mass., on the road leading to Warren, it
occurs with andalusite in gneiss, and likewise near Norwich, Conn. It
is also found at Richmond, N. H., with anthophyllite in a talcose rock.
In the author's colÂlection, there is a crystal of this mineral, found
at Fort George, Manhattan Island, which is almost entirely altered to
pinite, an alteration common to nearly all the crystals that were
formerly found at Haddam, Conn.
Lepidolite
is a mica containing lithia. Beautiful pink and lavender colored
lepidolite has been found in large quantities at
1 Danburite from Switzerland. Am. J. Sci. III., Vol. 24, p. 476, Dec., 1882 ; also, Vol. 25, p. 161, Feb., 1883.
! Am. J. Sci. III., Vol. 36, p. 57, Oct., 1888.
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