Man & Environment, Volym 30, Utgåva 2Indian Society for Prehistoric and Quaternary Studies., 2005 |
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Sida 2
... foot of the rocky ridges , the Piedmont is mainly formed by the accumulation of disintegrated basal rock and colluvial deposit . The thickness of this deposit varies from 0.2 to 2 m . Palaeolithic primary localities in the foothill are ...
... foot of the rocky ridges , the Piedmont is mainly formed by the accumulation of disintegrated basal rock and colluvial deposit . The thickness of this deposit varies from 0.2 to 2 m . Palaeolithic primary localities in the foothill are ...
Sida 15
... hill , overlooking the site A pattern of distribution of sites / scatters emerged from the first two seasons ( Basak ... foothill region ) In Ayodhya , these features , especially the hills attract local people by their sheer physicality ...
... hill , overlooking the site A pattern of distribution of sites / scatters emerged from the first two seasons ( Basak ... foothill region ) In Ayodhya , these features , especially the hills attract local people by their sheer physicality ...
Sida 18
... foothill till Kana - 1 for 3 km . This forms the second zone of concentra- tion ( Zone B ) in the foothill of the Kana hill ( Fig . 4 ) . Four 3 . 4 . These sites do not have a closed - in appearance like Sirgi 1 . Approaching these ...
... foothill till Kana - 1 for 3 km . This forms the second zone of concentra- tion ( Zone B ) in the foothill of the Kana hill ( Fig . 4 ) . Four 3 . 4 . These sites do not have a closed - in appearance like Sirgi 1 . Approaching these ...
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Acheulian agriculture analysis ancient appears archaeological artefacts associated base burials capstone caries rates centre century chamber circle cist close collected complex crown cultural dated deciduous dental deposit dimensions District dolmens Early Early Historic eastern Environment evidence excavations four groups hand handedness Harappan hills human important Inamgaon included increase India indicates Journal landscape Late Jorwe later localities located lower Lukacs maritime mean measuring Middle natural northern noted objects original orthostat ostrich Palaeolithic past Pattanam pattern period Periyar permanent Persian phase placed Pleistocene port Prehistoric present Pune record region remains reported revealed river sample seal settlement shell side significant slab Society soil South stands stone Studies subsistence suggest surface teeth temple tion tooth trade transition University upper valley village ware western