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AMPHIBOLE

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Originally appearing in Volume V01, Page 883 of the 1911 Encyclopedia Britannica.
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AMPHIBOLE , an important See also:

group of See also:rock-forming minerals, very similar in chemical See also:composition and See also:general characters to the pyroxenes, and like them falling into three See also:series according to the See also:system of See also:crystallization. They differ from the pyroxenes, however, in having an See also:angle between the prismatic cleavage of 56° instead of 87°; they are specifically lighter than the corresponding pyroxenes; and, in their See also:optical characters, they are distinguished by their stronger pleochroism and by the wider angle of extinction on the See also:plane of symmetry. They are minerals of either See also:original or secondary origin; in the former See also:case occurring as constituents (See also:hornblende) of igneous rocks, such as See also:granite, See also:diorite, See also:andesite, &c. Those of secondary origin have either been See also:developed (See also:tremolite) in limestones by contact-See also:metamorphism, or have resulted (actinolite) by the alteration of See also:augite by See also:dynamo-metamorphism. Pseudomorphs of amphibole after See also:pyroxene are known as uralite. The name amphibole (from the Gr. aw/,i3oXos, ambiguous) was used by R. J. See also:Hauy to include tremolite, actinolite and hornblende; this See also:term has since been applied to the whole group. Numerous sub-See also:species and varieties are distinguished, the more important of which are tabulated below in three series. The formulae of each will be seen to conform to the general See also:meta-silicate See also:formula R"SiO3.

End of Article: AMPHIBOLE

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