1936
DOI: 10.1038/137686a0
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Late Cenozoic History in India

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Cited by 3 publications
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“…The folding and faulting that took place during the Himalaya's uplift between the Indian subcontinent and the rest of Asia resulted in the formation of the valley of Kashmir. The "Karewas" are a notable geological feature of the area; they are plateau-like tablelands composed of clay, sand, and silt of lacustrine origin and created during the Pleistocene Ice Age (De Terra, 1934). The climate of the area, which is characterised by distinct seasonality, is analogous to that of mountainous and continental regions found in temperate latitudes.…”
Section: Study Areamentioning
confidence: 99%
“…The folding and faulting that took place during the Himalaya's uplift between the Indian subcontinent and the rest of Asia resulted in the formation of the valley of Kashmir. The "Karewas" are a notable geological feature of the area; they are plateau-like tablelands composed of clay, sand, and silt of lacustrine origin and created during the Pleistocene Ice Age (De Terra, 1934). The climate of the area, which is characterised by distinct seasonality, is analogous to that of mountainous and continental regions found in temperate latitudes.…”
Section: Study Areamentioning
confidence: 99%
“…The folding and faulting that took place during the Himalaya's uplift between the Indian subcontinent and the rest of Asia resulted in the formation of the valley of Kashmir. The "Karawas" are a notable geological feature of the area; they are plateau-like tablelands composed of clay, sand, and silt of lacustrine origin and created during the Pleistocene Ice Age (De Terra, 1934). The climate of the area, which is characterised by distinct seasonality, is analogous to that of mountainous and continental regions found in temperate latitudes.…”
Section: Study Areamentioning
confidence: 99%