Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 2
... west , and Burmese continent in the east . It acquired almost the present position by Early Miocene ( 24 Ma BP ) . The formation and development of Sulaiman ranges in the west , Arakan - Yoma mountain belt in the east , and Hima- layan ...
... west , and Burmese continent in the east . It acquired almost the present position by Early Miocene ( 24 Ma BP ) . The formation and development of Sulaiman ranges in the west , Arakan - Yoma mountain belt in the east , and Hima- layan ...
Sida 27
... west , and Bihar - Bengal in the east . Ganga Plain as the Potential Zone of Early Agriculture Climate , especially rainfall patterns , witnessed drastic changes and fluctuations between LGM ( Last Glacial Maxima around 18 kyr BP ) and ...
... west , and Bihar - Bengal in the east . Ganga Plain as the Potential Zone of Early Agriculture Climate , especially rainfall patterns , witnessed drastic changes and fluctuations between LGM ( Last Glacial Maxima around 18 kyr BP ) and ...
Sida 44
... West Medinipur district of West Bengal . It lies at a distance of approximately 5 km from a village called Beltala , which is around 12 km south of Ghantal on the Ghantal - Paskhura highway . Kolmijod is a typical Shankhari village ...
... West Medinipur district of West Bengal . It lies at a distance of approximately 5 km from a village called Beltala , which is around 12 km south of Ghantal on the Ghantal - Paskhura highway . Kolmijod is a typical Shankhari village ...
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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