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Art. VII.—Summary of the Geology of Southern India

Published online by Cambridge University Press:  14 March 2011

Captain Newbold
Affiliation:
Assistant Commissioner for Kurnool.

Extract

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.

Type
Original Communications
Copyright
Copyright © The Royal Asiatic Society 1846

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References

page 141 note 1 Geology of the Dekhan, Transactions Geological Society, Second Series, vol. iv., pp. 409432.Google Scholar

page 142 note 1 Madras Almanac, 1840.

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.

page 150 note 1 Asiatic Researches, Vol. XVIII., Part II., page 18.Google Scholar

Ibid., Part II., page 8.

page 152 note 1 Benza, , Madras Journal of Literature and Science, Vol. IV., pages 266, 267.Google Scholar

page 153 note 1 Macgregor, , Madras Quarterly Medical Journal, 07, 1842, page 284.Google Scholar

page 153 note 2 Clarke, , Madras Journal, 01, 1839, page 121.Google Scholar

page 153 note 3 Hayne's, Tracts, page 110.Google Scholar

page 153 note 4 Voysey.

page 153 note 5 Clarke, , Madras Journal of Literature and Science for 01, 1839, p. 120.Google Scholar

page 153 note 6 Macpherson, , Asiatic Researches, Vol. XVIII., page 120.Google Scholar

page 154 note 1 Hayne's, Tracts, page 345.Google Scholar

Macpherson, , Asiatic Researches, Vol. XVIII., p. 120.Google Scholar

page 155 note 1 Clarke, , Madras Journal of Literature and Science for 01, 1839, p. 120.Google Scholar

page 156 note 1 Clarke, , Madras Journal of Literature and Science for 01, 1839, p. 120.Google Scholar

page 157 note 1 Malcolmson, , Geological Transactions, Vol. V., page 367, Second Series, Part III.Google Scholar

page 159 note 1 Malcolmson, , Geological Transactions, Vol. V., Second Series, Part III, pp. 567, &c.Google Scholar

page 160 note 1 DrWalker, , Journal of Asiatic Society of Bengal, 1841, No. 30, p. 471.Google Scholar

page 166 note 1 Journal of Asiatic Society of Bengal, No. 112, 1841, pp. 341, &c.Google Scholar

page 168 note 1 Hyne's, Tracts, pp. 92 and 110.Google Scholar

page 170 note 1 Conybeare's Report to British Association, 1832.

page 170 note 1 Geological Transactions, Second Series, Vol. III., Part I.Google Scholar

page 171 note 1 Geological Transactions, Second Series, VoL V., pp. 568, 569.Google Scholar

page 171 note 2 Ibid.

Ibid.

Vol. V., Report of Buckland's Anniversary Speech, 1841.