See also:ACHITE, or AEGIRITE , a See also:mineral of the See also:pyroxene (q.v.) See also:group, Which may be described as a soda-pyroxene, being essentially asodium and ferric metasilicate, NaFe(SiOs)2. In its crystallographic characters it is See also:close to See also:ordinary pyroxene (See also:augite and See also:diopside), being See also:monoclinic and having nearly the same See also:angle between the prismatic cleavages. There are, however, important See also:differences in the See also:optical characters: the birefringence of acmite is negative, the pleochroism is strong and the extinction angle on the See also:plane of symmetry measured to the See also:vertical See also:axis is small (3°-5°). The hardness is 6-0, and the specific gravity 3'55. Crystals are elongated in the direction of the vertical axis, and are blackish See also:green (aegirite) or dark See also:- BROWN
- BROWN, CHARLES BROCKDEN (1771-181o)
- BROWN, FORD MADOX (1821-1893)
- BROWN, FRANCIS (1849- )
- BROWN, GEORGE (1818-188o)
- BROWN, HENRY KIRKE (1814-1886)
- BROWN, JACOB (1775–1828)
- BROWN, JOHN (1715–1766)
- BROWN, JOHN (1722-1787)
- BROWN, JOHN (1735–1788)
- BROWN, JOHN (1784–1858)
- BROWN, JOHN (1800-1859)
- BROWN, JOHN (1810—1882)
- BROWN, JOHN GEORGE (1831— )
- BROWN, ROBERT (1773-1858)
- BROWN, SAMUEL MORISON (1817—1856)
- BROWN, SIR GEORGE (1790-1865)
- BROWN, SIR JOHN (1816-1896)
- BROWN, SIR WILLIAM, BART
- BROWN, THOMAS (1663-1704)
- BROWN, THOMAS (1778-1820)
- BROWN, THOMAS EDWARD (1830-1897)
- BROWN, WILLIAM LAURENCE (1755–1830)
brown (acmite) in See also:colour. Being isomorphous with augite, crystals intermediate in See also:composition between augite or diopside and aegirite are not uncommon, and these are known as aegirine-augite or aegirinediopside.
Acmite is a characteristic constituent of igneous rocks See also:rich in soda, such as See also:nepheline-syenites, phonolites, &c. It was first discovered as slender crystals, sometimes a See also:foot in length, in the See also:pegmatite See also:veins of the See also:granite of Rundemyr, near See also:Kongsberg in See also:Norway, and was named by F. Stromeyer in 1821 from the Gr. aKo, a point, in allusion to the pointed terminations of the crystals. Aegirite (named from Aegir, the Scandinavian See also:sea-See also:god) was described in 1835 from the elaeolite-See also:syenite of See also:southern Norway. Although exhibiting certain varietal differences, the essential-identity of acmite and aegirite has See also:long been established, but the latter and more See also:recent name is perhaps in more See also:general use, especially among petrologists.
End of Article: ACHITE, or AEGIRITE
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