Man & Environment, Volym 30, Utgåva 1Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 7
... slope component in the Central Alluvial Plain with a distinct northern slope from Kanpur towards Faizabad ( from Ganga towards the Ghaghara River ) ( see Singh et al . , 1999a ) . The slopes are highly variable ranging between 20- 5 cm ...
... slope component in the Central Alluvial Plain with a distinct northern slope from Kanpur towards Faizabad ( from Ganga towards the Ghaghara River ) ( see Singh et al . , 1999a ) . The slopes are highly variable ranging between 20- 5 cm ...
Sida 7
... slope component in the Central Alluvial Plain with a distinct northern slope from Kanpur towards Faizabad ( from Ganga towards the Ghaghara River ) ( see Singh et al . , 1999a ) . The slopes are highly variable ranging between 20- 5 cm ...
... slope component in the Central Alluvial Plain with a distinct northern slope from Kanpur towards Faizabad ( from Ganga towards the Ghaghara River ) ( see Singh et al . , 1999a ) . The slopes are highly variable ranging between 20- 5 cm ...
Sida 74
... slope appear to be earlier than those without a slope . A large tank known as ' Khan Sarovar ' at Patan , Mehasana district , Gujarat , is very similar to tanks of this type , and also has a slope along one side . This tank was ...
... slope appear to be earlier than those without a slope . A large tank known as ' Khan Sarovar ' at Patan , Mehasana district , Gujarat , is very similar to tanks of this type , and also has a slope along one side . This tank was ...
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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