Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 18
charcoal indicates that the humans were living in the area and engaged in some kind of agricultural activity since 15 kyr BP . Basaha lake , Unnao Basaha lake ( Jheel ) , Unnao is part of the abandoned channel belt which is located on ...
charcoal indicates that the humans were living in the area and engaged in some kind of agricultural activity since 15 kyr BP . Basaha lake , Unnao Basaha lake ( Jheel ) , Unnao is part of the abandoned channel belt which is located on ...
Sida 22
... indicates higher rainfall in Bahraich area as compared to the Lucknow region for the past few thousand years . Moreover , there are distinct century - scale fluctuations in climate throughout the time span of 3600-800 yrs BP . Another ...
... indicates higher rainfall in Bahraich area as compared to the Lucknow region for the past few thousand years . Moreover , there are distinct century - scale fluctuations in climate throughout the time span of 3600-800 yrs BP . Another ...
Sida 26
... indicating that the sites were occupied for a long time . In this area , human skeletons are present almost at the surface . Normally , humans are buried 1-2 meters below the surface . The surface occurrence of skeletons indicates that ...
... indicating that the sites were occupied for a long time . In this area , human skeletons are present almost at the surface . Normally , humans are buried 1-2 meters below the surface . The surface occurrence of skeletons indicates that ...
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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