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GALENA , an important ore of See also:lead, consisting of lead sulphide (See also:PbS). The See also:mineral was mentioned by See also:Pliny under this name, and it is sometimes now known as lead-glance (Ger. Bleiglanz). It crystallizes in the cubic See also:system, and well-See also:developed crystals are of See also:common occurrence; the usual See also:form is the See also:cube or the cubo-See also:octahedron (fig.). An important See also:character, and one by which the mineral may always be recognized, is the perfect cubical cleavage, on which the lustre is brilliant and metallic. The See also:colour of the mineral and of its streak is lead-See also:grey; it is opaque; the hardness is 21 and the specific gravity 7.5. Twinned crystals are not common, but the presence of polysynthetic twinning is sometimes shown by See also:fine striations See also:running diagonally or obliquely across the cleavage surfaces. Large masses with a coarse or fine granular structure are of common occurrence; the fractured surfaces of such masses See also:present a spangled See also:appearance owing to the numerous See also:bright cleavages. The See also:formula PbS corresponds with lead 86.6 and See also:sulphur 13.4%. The mineral nearly always contains a small amount of See also:silver, and sometimes See also:antimony, See also:arsenic, See also:copper, See also:gold, See also:selenium, &c. Argentiferous galena is an important source of silver; this See also:metal is present in amounts rarely exceeding 1 %, and often less than 0.03 % (See also:equivalent to ro4 ounces per ton). Since See also:argentite (Ag2S) is isomorphous with galena, it is probable that the silver isomorphously replaces lead, but it is to be noted that native silver has been detected as an enclosure in galena. Galena is of wide See also:distribution, and occurs usually in metalliferous See also:veins traversing crystalline rocks, See also:clay-slates and See also:lime-stones, and also as pockets in limestones. It is often associated with See also:blende and See also:pyrites, and with See also:calcite, fluorspar, See also:quartz, See also:barytes, See also:chalybite and pearlspar as See also:gangue minerals; in the upper oxidized parts of the deposits, See also:cerussite and anglesite occur as alteration products. The mineral has occasionally been observed as a See also:recent formation replacing organic See also:matter; such as See also:wood; and it is sometimes found in beds of See also:coal. As small concretionary nodules, it occurs disseminated through See also:sand-See also: (L. J. Additional information and CommentsThere are no comments yet for this article.
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