Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 9
... shows several levels ( Singh 1996 ) . The T , -Surface is generally beyond the reach of flood waters of the active river . However , backflooding in small channels and excessive rainfall can cause flooding of this surface . The T ...
... shows several levels ( Singh 1996 ) . The T , -Surface is generally beyond the reach of flood waters of the active river . However , backflooding in small channels and excessive rainfall can cause flooding of this surface . The T ...
Sida 8
... shows several levels ( Singh 1996 ) . The T , -Surface is generally beyond the reach of flood waters of the active river . However , backflooding in small channels and excessive rainfall can cause flooding of this surface . The T1 ...
... shows several levels ( Singh 1996 ) . The T , -Surface is generally beyond the reach of flood waters of the active river . However , backflooding in small channels and excessive rainfall can cause flooding of this surface . The T1 ...
Sida 18
... shows shell - rich mud ( marl ) followed by black loamy clay and silty clay . Five pollen zones are identified ( Fig . 13 ) . Zone BJI ( 3300-3200 yrs BP ) is dominated by grasses with some tree elements like Bauhinia , Aegle , etc ...
... shows shell - rich mud ( marl ) followed by black loamy clay and silty clay . Five pollen zones are identified ( Fig . 13 ) . Zone BJI ( 3300-3200 yrs BP ) is dominated by grasses with some tree elements like Bauhinia , Aegle , etc ...
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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