Indications of Glacierization in the Siwalik System in India

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Abstract

THE Indian sub-continent was not subjected to glacial conditions during the Quatenary Era, but its highlands, namely the higher ranges of the Himalayas up to the latitude of about 33 degrees, were.

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References

  1. 1

    de Terra, Rec. Geol. Soc. Ind., 73, Pt. 4.

  2. 2

    Pilgrim, Rec. Geol. Soc. Ind., 73, Pt. 4.

  3. 3

    Hopwood and Lewis, Rec. Geol. Soc. Ind., 73, Pt. 4.

  4. 4

    Grinlinton Geol. Surv. Ind. Mem. 49, Pt. 2.

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MEHDIRATTA, R. Indications of Glacierization in the Siwalik System in India. Nature 184, 833–834 (1959) doi:10.1038/184833b0

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