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Subhash Chandra, K. C.
- Pillow Structures from Bevinahalli, Bellary District, Karnataka State
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PDF Views:146
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1 Department of Mines and Geology, Bellary 583101, IN
1 Department of Mines and Geology, Bellary 583101, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 20, No 4 (1979), Pagination: 188-189Abstract
No Abstract.- N. Venkoba Rao Magar (1932-2008)
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PDF Views:130
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1 #75, 5th 'A' Main, 4th Cross, R.P.C. Layout (Hampi Nagar), Bangalore - 560401, IN
1 #75, 5th 'A' Main, 4th Cross, R.P.C. Layout (Hampi Nagar), Bangalore - 560401, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 71, No 6 (2008), Pagination: 891-891Abstract
No Abstract.- Springs in Limestone Environs of Karnataka
Abstract Views :165 |
PDF Views:2
Authors
Affiliations
1 NO.75, 5th 'A' Main Road, 4th Cross, R.P.C.Layout, Vijayanagar II Stage, Bangalore - 560 040, IN
2 87/B, Kathriguppa, B.S.K.III Stage, Bangalore - 560 085, IN
1 NO.75, 5th 'A' Main Road, 4th Cross, R.P.C.Layout, Vijayanagar II Stage, Bangalore - 560 040, IN
2 87/B, Kathriguppa, B.S.K.III Stage, Bangalore - 560 085, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 69, No 5 (2007), Pagination: 1111-1117Abstract
The geohydrological environs of springs in the limestone formations of Karnataka are complex, but interesting. Springs abound in Western Ghats. But, geomorphic set up of the terrain is so hostile that many are not accessible. In the Eastern Maidan Tract, the limestone formations of Bhima Group host most of the springs as compared to those of Dharwar and Kaladgi Super Groups. The limestone formations in the stratigraphic sequences of Sargurs, Bababudans and Badamis form minor litho-Constituents and do not have much significance as regard to the occurrence of springs. A few of the springs, once active in Eastern Maidan Tract have now become dormant, the cause that could be attributed to a long sustained anthropological activity. The chemical quality of spring waters in limestone formations,of Chitradurga Group and in particular of those in Western Ghats are suitable for domestic and agricultural usage. Springs located in the limestone formations of Kaladgi Super Group and Bhima Group are quality wise alkaline, contain fluoride and certain other dissolved constituents beyond the permissible limits.Keywords
Geohydrology, Springs, Limestone, Karnataka.- Groundwater Flow Direction and Long Term Trend of Water Level of Nadia District, West Bengal: a Statistical Analysis
Abstract Views :176 |
PDF Views:170
Authors
Affiliations
1 4th Cross, R.P.C. Layout, Vijayanagar III Stage, Bangalore - 560 040, IN
1 4th Cross, R.P.C. Layout, Vijayanagar III Stage, Bangalore - 560 040, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 61, No 6 (2003), Pagination: 741-743Abstract
No Abstract.- Mir Azeemuddin Ali Khan (1934-2010)
Abstract Views :190 |
PDF Views:115
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Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 77, No 3 (2011), Pagination: 285-285Abstract
No Abstract.- Demand, Resource Availability and Status of Water Supply to Mega City-Bangalore, Karnataka
Abstract Views :162 |
PDF Views:117
Authors
Affiliations
1 Department of Mines and Geology, IN
1 Department of Mines and Geology, IN