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Co-Authors

S. N. Rajaguru
N. J. Pawar
T. C. Atkinson
P. J. Rowe
P. K. Basu
V. G. Phansalkar
A. S. Kale
N. R. Kamalkar

Journals

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

Year

1985
1988
1992

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Kale, V. S.

Changes in the Fluvial Regime of Western Maharashtra Upland Rivers During Late Quaternary

Abstract Views :203 | PDF Views:4

Authors

S. N. Rajaguru ¹, V. S. Kale ¹

Affiliations
1 Department of Archaeology, Deccan College, Pune 411006, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 26, No 1 (1985), Pagination: 16-27

Abstract

Recent geomorphological, archaeological, palaeontological and carbon -14 dating of alluvial deposits and the observations on buried as well as exposed channel deposits of Upper Krishna, Bhima and the Upper Godavari rivers of Western Maharashtra have brought out five major phases of fluvial activity, since late middle Pleistocene. These rivers were dominantly aggrading during theTermial late Pleistocene (c 40.000-11,000 yrs. B.P.) and incision predominated during the major port of the Holocene. These changes in the fluvial activity can be explained in terms of climatic changes of the late Quaternary period.

The present study disproves the earlier view that the late Quaternary geomorphic history of the study area has been stable and uneventful.

Full Text

Early Holocene Waterfall Tufa from Semi-Arid Maharashtra Plateau (India)

Abstract Views :170 | PDF Views:144

Authors

N. J. Pawar ¹, V. S. Kale ¹, T. C. Atkinson ², P. J. Rowe ²

Affiliations
1 School of Environmental Sciences, Dept. of Geography, University of Poona, Pune-411 007, IN
2 School of Environmental Sciences, University of East Anglia, Norwich, GB

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 32, No 6 (1988), Pagination: 513-515

Abstract

Waterfall tufa occurring in the semi-arid parts of the Upland Maharashtra has been dated by employing uranium series disequilibrium dating method. The dates correlate well with other evit1lences and suggest a wet climate during the genesis of the tufa.

Full Text

An Unusual Evaporite Association from the Papaghni Group, Cuddapah Basin

Abstract Views :197 | PDF Views:126

Authors

P. K. Basu , V. G. Phansalkar ¹, A. S. Kale ¹, N. R. Kamalkar ¹, V. S. Kale ¹

Affiliations
1 Department of Geology, University of Poona, Pune 411 007, IN

Source

Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 39, No 3 (1992), Pagination: 257-259

Abstract

No Abstract.

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