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BARYTOCALCITE
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Source
Encyclopaedia Britannica (1911) / britannica_1911
License
public_domain
Chunk ID
1911:barytocalcite:25c54e1a9c71
Section
Hash Algorithm
sha256
Stored Hash
a87e822e01f8fa76b2f47af77dc1a8d6a16a1f49c548ae74fcfcd62a1739963a
Computed Hash
a87e822e01f8fa76b2f47af77dc1a8d6a16a1f49c548ae74fcfcd62a1739963a
Normalizer
ggnorm 1.0
Observed
2026-02-08 18:42:23
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Verified Text
barytocalcite, a rare mineral found only at alston moor in cumberland, where it occurs as diverging groups of white transparent crystals lining cavities in the mountain limestone. [v.03 p.0457] the crystals belong to the monoclinic system and are usually prismatic or blade-shaped in habit. the hardness is 4, and the sp. gr. 3.65. there are perfect cleavages parallel to the prism faces inclined at an angle of 73deg 6', and a less perfect cleavage parallel to the basal plane, the angle between which and the prism faces is 77deg 6'; the angles between these three cleavages thus approximate to the angles (74deg 55') between the three cleavages of calcite, and there are other points of superficial resemblance between these two minerals. chemically, barytocalcite is a double salt of barium and calcium carbonates, baca(co_3)_2, thus differing from the orthorhombic bromlite (_q.v._) which is an isomorphous mixture of the two carbonates. (l. j. s.)