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Art. VII.—Summary of the Geology of Southern India
Published online by Cambridge University Press: 14 March 2011
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The area, the geological features of which it is purposed to attempt a description of, so far as known, comprises peninsular India from Bombay on the west, and Ganjam on the east coast, to Cape Comorin, lying between the 8th and 20th degrees of north latitude. Its northern limit is skirted by the Sub-Vindhyan ranges, and the plains of Central India; while the remaining sides are washed by the ocean, and lie within the 72nd and 86th degrees of east longitude.
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References
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page 143 note 1 A fifth might be added, viz., that of Maláya, or Ultra-Gangetic India, comprising the Malacca peninsula, part of Siam, and Birma. This immense line of elevation, extending from the foot of the Himalaya system to the verge of the Equator, has a direction almost parallel to that of Southern India, with which it may possibly be found identical (in epoch.) On its northern portions the drainage is determined southerly by the great westerly elevation of the Himálaya; and entering the longitudinal valleys of the Maláya system passes southerly along their course to the Indian Ocean. The anticlinal ridge of the chain that runs down the interior of the Malayan peninsula throws off its drainage to the east and west into the seas of China, India, and the Straits of Malacca The granitic rocks that constitute a great portion of this ridge are remarkably distinguished, mineralogically, from those of Southern India by their highly stanniferous character.
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