Greenland,
Iceland, the Faroe Islands, also Poonah, and Ahmed-nuggar in India
yield fine crystals. It also occurs in many Swedish, Tyrolese, and
Transylvanian localities.
Apophyllite
is nearly related to the zeolites, and is a hydrated silicate of lime
and potash, with a little fluorine. Its percentage composition is
represented by the following numbers—
Andalusite.
It
is seldom that the mineral andulusite occurs in a perfectly transparent
condition fit for cutting as a gem. Its colour is then of a somewhat
reddish hue or pale amber brown, or light bottle green. But its beauty
and interest mainly depend upon its conÂspicuous dichroism. Cut
specimens often appear of a greenish hue, except in some of the end
facets where a fine brownish red occurs.* There thus arises a marked
resemblance to alexandrite, which, however, is not only a much more
valuable stone, but is also heavier and harder. It may also be confused
with certain tourmalines of similar hue, but its specific gravity is
rather greater, while the pyro-electric character of tourmaline affords
a means of distinguishing the two stones.
Andalusite,
which crystallises in the rhombic system, occurs in prismatically
developed forms of which the section is nearly square. Its hardness is
at least 7-1/4 and its specific gravity close to 3'18.
Transparent specimens occur in some abundance in the Minas Novas
district of Brazil, but are also found in certain gem gravels
of Ceylon, where the stone is mistaken for tourmaline. A step-cut shape
with few and rather large facets generally suits andalusite. The
composition of andalusite is identical with that of cyanite
* Fig. 7. Frontispiece.