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See also: quartz containing spangles of See also: mica or scales of iron-See also: oxide, which confer brilliancy on the See also: stone
.
It is found chiefly in the Ural Mountains, and is cut for ornamental purposes at
See also: Ekaterinburg
.
Some of the Siberian See also: aventurine, like that of the See also: vase given by See also: Nicholas I. to See also: Sir R
.
Murchison, in 1843, is a micaceous iron-stained quartz, of but little beauty
.
Most aventurine is of reddish See also: brown or yellow colour, but a
See also: green variety, containing scales of fuchsite or chrome-mica, is also known
.
This green aventurine, highly valued by the See also: Chinese, is said to occur in the See also: Bellary See also: district in See also: India
.
Aventurine See also: felspar, known also as See also: Sun-stone (q.v.) is found principally at Tvedestrand in See also: south See also: Norway, and is a variety of See also: oligoclase enclosing micaceous scales of See also: haematite
.
Other kinds of felspar, even See also: orthoclase, may however also show the aventurine appearance
.
Both plagioclastic and orthoclastic aventurine occur at several localities in the See also: United States
.
The See also: mineral aventurine takes its name from the well-known aventurine-See also: glass of Venice
.
This is a reddish brown glass with gold-like spangles, more brilliant than most of the natural stone
.
The See also: story runs that this kind of glass was originally made accidentally at See also: Murano by a workman, who let some copper filings fall into the molten " See also: metal," whence the product was called avventurino
.
From the Murano glass the name passed to the mineral, which displayed a rather similar appearance . (F . W . |
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