Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 21
... climate throughout the time span of 3600-800 yrs BP . Another important aspect of this study is that each archaeological - cultural period starts with a relatively humid climate and shows a drier climate at the end of the cultural ...
... climate throughout the time span of 3600-800 yrs BP . Another important aspect of this study is that each archaeological - cultural period starts with a relatively humid climate and shows a drier climate at the end of the cultural ...
Sida 22
... climate throughout the time span of 3600-800 yrs BP . Another important aspect of this study is that each archaeological - cultural period starts with a relatively humid climate and shows a drier climate at the end of the cultural ...
... climate throughout the time span of 3600-800 yrs BP . Another important aspect of this study is that each archaeological - cultural period starts with a relatively humid climate and shows a drier climate at the end of the cultural ...
Sida 29
... climate of the Ganga Plain is essentially con- trolled by the southwest monsoon . The eastern and northern Ganga plains are regions of high rainfall ; while the western and southern Ganga plains are areas of moderate to low rainfall and ...
... climate of the Ganga Plain is essentially con- trolled by the southwest monsoon . The eastern and northern Ganga plains are regions of high rainfall ; while the western and southern Ganga plains are areas of moderate to low rainfall and ...
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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