By A. D. Mills

ISBN-10: 0198527586

ISBN-13: 9780198527589

An elevated model of the best-selling Dictionary of English Place-Names, this dictionary now additionally covers Scottish, Welsh, and Irish place-names. From Abbas Combe to Zennor it supplies the which means and beginning of over 15,000 British place-names.

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Formation of pyroxene rim around an olivine crystal in basalt magma is also well known. Classifications of Igneous Rocks A Simple “Field” Classification Chemical composition of magma dictates what minerals may crystallize from it. The rate at which the magma cools, which is related to its depth and mode of emplacement, controls the sizes and shapes of crystals and its texture. Therefore, it is only natural that naming an igneous rock must take into account its Classifications of Igneous Rocks 41 chemical composition, mineralogy, and texture (mode of emplacement).

Gabbros are coarse grained, and the plagioclase and pyroxene crystals generally form coarse hypidiomorphic granular-type textures. Intergranular texture, defined by the occurrence of pyroxene, magnetite, and ilmenite crystals or microlites in the Komatiites, Peridotites, and Pyroxenites Komatiites are ultramafic lavas that erupted in the Archean (with only one exception in the Phanerozoic in Gorgona Island). The most distinctive feature of komaitiites is the presence of long skeletal crystals of olivine and/or pyroxene.

Whether or not magma would flow out of a volcano as lava or barely rise to fill or partially fill the volcanic crater as a dome (a simple domal structure) depends on the magma’s viscosity, which is in turn linked to its composition and dissolved vapor content. Felsic lava is so viscous that it normally does not easily form a lava flow and instead form domes inside a volcano. Mafic magmas are less viscous and therefore form lava flows. The most common type of mafic magma (called tholeiite, discussed later) is the least explosive, and their corresponding lavas can flow over great distances.

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A Dictionary of British Place-Names by A. D. Mills

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