Search over 40,000 articles from the original, classic Encyclopedia Britannica, 11th Edition.
|
PYRARGYRITE
, a See also:mineral consisting.of See also:silver sulphantimonite, Ag3SbS3, known also as dark red silver ore, an important source of the See also:metal
.
It is closely allied to, and isomorphous with, the corresponding sulpharsenite known as See also:proustite (q.v.) or See also:light red silver ore
.
" See also:Ruby silver " or red silver ore (See also:German Rotgiiltigerz) was mentioned by G
.
See also: See also:Angle . Height . See also:Azimuth . Medum . . . Sneferu 4750 5682.0 6.2 51 ° 52' 3619 24' 25" W . Gizeh . . . Khufu 4700 9068.8 .65 51 ° 52' 5776 3' 43" W . Khafra 4600 8474.9 1.5 530 I0' 5664 5' 26" W . Menkaura 4550 4153.6 3.0 51° lo' 2581 14' 3" E . Dahshur S . . ? ? 7459.0 3.7 53° 5, 4134 9' 12" W . Dahshur Small . ? ? 2064.6 IT 440 34' 2034 16' 12" W . Both crystallize in the ditrigonal pyramidal (See also:hemimorphic-hemihedral) class of the See also:rhombohedral See also:system, possessing the same degree of symmetry as See also:tourmaline . Crystals are perfectly See also:developed and are usually prismatic in See also:habit; they are frequently attached at one end, the hemimorphic See also:character being then evident by the fact that the oblique striations on the See also:prism faces are directed towards one end only of the crystal . Twinning according to several See also:laws is not uncommon . The angles are nearly the same in the two species; the rhombohedral angle re' being 71° 22' in pyrargyrite and 72° 12' in proustite . The hexagonal prisms of pyrargyrite are usually terminated by a See also:low hexagonal See also:pyramid (310) or by a drusy basal See also:plane . The See also:colour of pyrargyrite is usually greyish-See also:black and the lustre metallic-adamantine; large crystals are opaque, but small ones and thin splinters are deep ruby-red by transmitted light, hence the name, from Gr. See also:alp (See also:fire) and &pyvpos (silver), given by E . F . Glocker in 1831 . The streak is purplish-red, thus differing markedly from the See also:scarlet streak of proustite and affording a ready means of distinguishing the two minerals . The hardness is 22, and the specific gravity 5.85: the refractive indices and birefringence are very high, w=3.084, e=2.881 . There is no very distinct cleavage and the fracture is conchoidal . The mineral occurs in metalliferous See also:veins with See also:calcite, argentiferous See also:galena, native silver, native See also:arsenic, &c . The best crystallized specimens are from St Andreasberg in the Harz, See also:Freiberg in See also:Saxony, and See also:Guanajuato in See also:Mexico . It is not uncommon in many silver mines in the See also:United States, but rarely as distinct crystals; and it has been found in some Cornish mines . Although the " red silver ores " afford a See also:good example of isomorphism, they rarely See also:form mixtures; pyrargyrite rarely contains as much as 30/s of arsenic replacing See also:antimony, and the same is true of antimony in proustite . Dimorphous with pyrargyrite and proustite respectively are the rare See also:monoclinic species pyrostilpnite or fireblende (Ag3SbS3) and xanthoconite (Ag3AsS3) : these four minerals thus form an isodimorphous See also:group . (L . J . |
|
|
[back] PYRAMUS AND THISBE |
[next] PIAZINES PYRAZINES |
There are no comments yet for this article.
Do not copy, download, transfer, or otherwise replicate the site content in whole or in part.
Links to articles and home page are encouraged.