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TREMOLITE , a member of the See also:amphibole See also:group of See also:rock-forming minerals (see AMPHIBOLE). It is a See also:calcium and See also:magnesium metasilicate, CaMg3(SiO3)4, crystallizing in the See also:monoclinic See also:system with an See also:angle of 55° 49' between the perfect prismatic cleavages. It occurs sometimes as distinct crystals, but more usually as See also:long bladed and fibrous forms. The See also:colour is See also:- WHITE
- WHITE, ANDREW DICKSON (1832– )
- WHITE, GILBERT (1720–1793)
- WHITE, HENRY KIRKE (1785-1806)
- WHITE, HUGH LAWSON (1773-1840)
- WHITE, JOSEPH BLANCO (1775-1841)
- WHITE, RICHARD GRANT (1822-1885)
- WHITE, ROBERT (1645-1704)
- WHITE, SIR GEORGE STUART (1835– )
- WHITE, SIR THOMAS (1492-1567)
- WHITE, SIR WILLIAM ARTHUR (1824--1891)
- WHITE, SIR WILLIAM HENRY (1845– )
- WHITE, THOMAS (1628-1698)
- WHITE, THOMAS (c. 1550-1624)
white or See also:grey, but when See also:iron is See also:present it is See also:green, then forming a passage to actinolite. The hardness is 5 a and the specific gravity 3.0. Tremolite is a characteristic See also:mineral of crystalline limestones, especially dolomitic limestones, but also occurs as an alteration-product of See also:olivine in basic igneous rocks. Typical specimens have long been known from the white crystalline See also:dolomite of Campolongo in the St Gotthard region, See also:Switzerland, near to which is the Tremola Valley, after which the mineral was named in 1796. See also:Fine crystals are found in crystalline See also:limestone at Gouverneur, See also:Pierrepont and other places in New See also:York, and at several localities in See also:Sweden. (L. J.
End of Article: TREMOLITE
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