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Krishnan, K.
- High Resolution Facies Record on Late Holocene Flood Plain Sediments from Lower Reaches of Narmada Valley, Western India
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Authors
Affiliations
1 Department of Geology, The Maharaja Sayajirao University of Baroda, Vadodara - 390 002, IN
2 Department of Archaeology and Ancient History, The Maharaja Sayajirao University of Baroda, Vadodara - 390 002, IN
3 Department of Mathematics, Indian Institute of Science, Bangalore - 560 012, IN
1 Department of Geology, The Maharaja Sayajirao University of Baroda, Vadodara - 390 002, IN
2 Department of Archaeology and Ancient History, The Maharaja Sayajirao University of Baroda, Vadodara - 390 002, IN
3 Department of Mathematics, Indian Institute of Science, Bangalore - 560 012, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 79, No 1 (2012), Pagination: 41-52Abstract
A high resolution quantitative granulometric record for site Uchediya [21°43'2.22" N, 73° 6'26.22" E; 10 m a. s. l.] gives understanding towards accretion history of the late Holocene flood plain in the lower reaches of Narmada River. Two sediment facies (sandy and muddy) and seven subfacies (sandy subfacies: StMS+FS+CS, SmFS+MS, SlFS+VFS, and StMS + CS; muddy subfacies: FmSILT+VFS+FS, FmSILT+VFS+FS (O) and FmSILT+VFS+FS (T)) are identified based on cluster analysis supplemented with sedimentary structures observed in field and other laboratory data. Changes in hydrodynamics are further deduced based on various sedimentological parameters and their ratios leading to arrive at a depositional model.Keywords
Lower Reaches of Narmada Valley, Late Holocene, Sedimentology, Sediment Facies, Hydrology.
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- Late Holocene Storm Records from Lower Reaches of Narmada Valley, Western India
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Authors
Affiliations
1 Institute of Seismological Research, Gandhinagar - 382 009, IN
2 Department of Geology, Wadia college, Pune - 411 001, IN
3 Department of Geology, IN
4 Department of Archaeology and Ancient History, The Maharaja Sayajirao University of Baroda, Vadodara - 390 002, IN
1 Institute of Seismological Research, Gandhinagar - 382 009, IN
2 Department of Geology, Wadia college, Pune - 411 001, IN
3 Department of Geology, IN
4 Department of Archaeology and Ancient History, The Maharaja Sayajirao University of Baroda, Vadodara - 390 002, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 80, No 3 (2012), Pagination: 403-408Abstract
Storms from the Arabian Sea are the most significant meteorological feature in western India that brings extreme rainy days together with catastrophic flooding. The present study reports two such palaeo-storm horizons at 1.16 m and 3.2 m above the present day water level in the Narmada channel, 56 km inland based on sedimentology and foraminiferal records. Both the horizons show similar sediment facies and foraminiferal assemblage. The present findings instigate to look for such new sites and build palaeo-storm records for western India.Keywords
Palaeo-Storm, Late Holocene, Foraminifera, Flood Plain, Narmada Valley, Western India.References
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