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PYROMORPHITE , a See also: mineral See also: species composed of See also: lead chloro-
Crystals are See also: common, and have the See also: form of a hexagonal prism terminated by the basal planes, sometimes combined with narrow faces of a hexagonal See also: pyramid
.
Crystals with a barrel-like curvature are not uncommon
.
Globular and reniform masses are also found
.
As proved by the etched figures on the faces, crystals possess the same parallel-faced hemihedrism as See also: apatite, with which mineral pyromorphite and also See also: mimetite are isomorphous
.
Between pyromorphite and the corresponding chloro-arsenate (mimetite, (q.v.) the resemblance in See also: external characters is so close that, as a See also: rule, it is only possible to distinguish between them by chemical tests: and they were formerly confused under the names " See also: green lead ore " and " See also: brown lead ore " (
See also: German, Griinbleierz and Braunbleierz)
.
The phosphate was first distinguished chemically by M
.
H
.
Klaproth, in 1784, and it was named pyromorphite by J
.
F
.
L
.
Hausmann in 1813, being so named from the Gr. xup (fire) and uopcpn (form), because when a fragment of the mineral is fused the globule assumes a faceted form on solidifying
.
The colour of the mineral is usually some bright shade of green, yellow or brown, and the lustre is resinous
.
The hardness is 3 and the specific gravity 6.5–7.1 . Owing to isomorphous replacement of the phosphorus by arsenic there may be a ‘.gradual passage from pyromorphite to mimetite . Varieties containing calcium isomorphously replacing lead areSee also: lower in .See also: density' (specific gravity 5.9–6.5) and usually lighter in colour; they bear the names " polysphaerite " (because of the globular fotm),'°` miesite " from Mies in Bohemia, " nussierite
from Nu8sihre near See also: Beaujeu, Rhone, See also: France, and " cherokine" from Cherokee county in See also: Georgia
.
694
Pyromorphite has resulted from the alteration of See also: galena in the oxidized portions of metalliferous See also: veins, and is frequently met with in the upper levels of lead mines
.
Finely crystallized specimens have been found at Braubach and See also: Ems in See also: Nassau, Wheal See also: Alfred in See also: Cornwall, Roughten Gill in See also: Cumberland, See also: Leadhills in Scotland, See also: Phoenixville in Pennsylvania, Huelgoat in See also: Finistere, See also: Brittany, &c
.
At the last-named locality, as well as at Wheal Hope, near Truro in Cornwall, there were formerly found curious pseudomorphs of galena after pyromorphite, known as " blue lead ore."
(L
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J
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