Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 5
... range ( day and night ) is usually 5-10 ° C . 2. Cold dry season : 3 . It extends from November to February and is characterised by low temperatures and low rainfall . The maximum temperature is 20-35 ° C ; minimum temperature is 5-12 ...
... range ( day and night ) is usually 5-10 ° C . 2. Cold dry season : 3 . It extends from November to February and is characterised by low temperatures and low rainfall . The maximum temperature is 20-35 ° C ; minimum temperature is 5-12 ...
Sida 59
... range from 3020 + 90 B.C. to 1810 ± 110 B.C. and in calibrated form from 3700-3620 B.C. to 2200-1830 B.C. None of these 25 dates is younger than 1800 B.C. Thus we can say that the Chalcolithic settlement was founded sometime between ...
... range from 3020 + 90 B.C. to 1810 ± 110 B.C. and in calibrated form from 3700-3620 B.C. to 2200-1830 B.C. None of these 25 dates is younger than 1800 B.C. Thus we can say that the Chalcolithic settlement was founded sometime between ...
Sida 59
... range from 3020 ± 90 B.C. to 1810 ± 110 B.C. and in calibrated form from 3700-3620 B.C. to 2200-1830 B.C. None of these 25 dates is younger than 1800 B.C. Thus we can say that the Chalcolithic settlement was founded sometime between ...
... range from 3020 ± 90 B.C. to 1810 ± 110 B.C. and in calibrated form from 3700-3620 B.C. to 2200-1830 B.C. None of these 25 dates is younger than 1800 B.C. Thus we can say that the Chalcolithic settlement was founded sometime between ...
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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