Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 15
... produce bedded calcrete horizons which are mostly dated 3-4 kyr BP . Formation of the bedded calcrete in the subsurface and impeded drainage on the surface produced closed circulating systems of water . This led to the development of ...
... produce bedded calcrete horizons which are mostly dated 3-4 kyr BP . Formation of the bedded calcrete in the subsurface and impeded drainage on the surface produced closed circulating systems of water . This led to the development of ...
Sida 15
... produce bedded calcrete horizons which are mostly dated 3-4 kyr BP . Formation of the ded calcrete in the subsurface and impeded drainage on urface produced closed circulating systems of water . led to the development of alkaline soils ...
... produce bedded calcrete horizons which are mostly dated 3-4 kyr BP . Formation of the ded calcrete in the subsurface and impeded drainage on urface produced closed circulating systems of water . led to the development of alkaline soils ...
Sida 109
... produced from inorganic materials now occupies a place in archaeological literature second only to that of ceramics . India has been the capital of bead world since the Harappan times , initially for stone beads , particularly those of ...
... produced from inorganic materials now occupies a place in archaeological literature second only to that of ceramics . India has been the capital of bead world since the Harappan times , initially for stone beads , particularly those of ...
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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