Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 11
... activity in the Ganga Plain The Ganga Plain is an active foreland basin whose filling history is essentially controlled by a tectonic processes in the Himalayan orogen and in response to the lithosphere below the Ganga Plain and in the ...
... activity in the Ganga Plain The Ganga Plain is an active foreland basin whose filling history is essentially controlled by a tectonic processes in the Himalayan orogen and in response to the lithosphere below the Ganga Plain and in the ...
Sida 18
... activity since 15 kyr BP . Basaha lake , Unnao Basaha lake ( Jheel ) , Unnao is part of the abandoned channel belt which is located on the Ganga - Sai interfluve and can be traced for several hundred kilometres from Allahabad in the ...
... activity since 15 kyr BP . Basaha lake , Unnao Basaha lake ( Jheel ) , Unnao is part of the abandoned channel belt which is located on the Ganga - Sai interfluve and can be traced for several hundred kilometres from Allahabad in the ...
Sida 25
... activity since the Early Palaeolithic and increased activity during early to middle Holocene in the Ganga Plain , which have been often overlooked . As discussed earlier , the Siwalik Hills represent deposits of the early phases of the ...
... activity since the Early Palaeolithic and increased activity during early to middle Holocene in the Ganga Plain , which have been often overlooked . As discussed earlier , the Siwalik Hills represent deposits of the early phases of the ...
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activity Agastya agricultural alluvial ancient archaeological areas Balathal beads Bengal body calcrete cave Cedrela century Chalcolithic changes channels charcoal climate cultural dates Deccan Delhi deposits distribution district early Early Historic early medieval evidence excavations Ganga Plain geomorphic glass Harappan Historic human important increase India indicates interfluve iron known kyr BP lakes Late Later layer located Lucknow Marginal material Megafan Middle monsoon mound namely natural northern occupation origin parenchyma period phase Pleistocene ponds present produced prominent Pune Quaternary rainfall range rays record region remains ridges river sediments settlements Shankharis Sharma shells shows similar Singh slope Society soil South southern species stone structures surface Survey tanks temples thick tion tradition tree Trench University Valley vegetation vessels village wall Ware West western wood zone