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Updated: May 29, 2025
At the junction of the Pemmi and Khawa rivers, there are high rocks of mica-slate, and broad river-terraces of stratified sand and pebbles, apparently alternating with deposits of shingle. On this hot, open expanse, elevated 2250 feet, appeared many trees and plants of the Terai and plains, as pomegranate, peepul, and sal; with extensive fields of cotton, indigo, and irrigated rice.
In the next article, in order to put the reader in possession of the glacial question as it stands at present, I shall say something of the possible causes of this extraordinary accumulation of snow, though all such explanations are thus far mere suggestions, and shall also give some more precise estimates of the changes of temperature involved in the history of the glacial period, before proceeding to the consideration of the effects produced by the breaking-up of the ice, as shown in our stratified lowland drift, and in our estuaries and river-terraces.
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