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Linkage of paraglacial processes from last glacial to recent inferred from Spituk sequence, Leh valley, Ladakh Himalaya

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Journal of the Geological Society of India

Abstract

The paraglacial sequence in the Leh valley, Ladakh Himalaya preserves imprints of various processes active during deglaciation in the late phase of Last Glacial. In present work, a high resolution sedimentological record generated for Spituk is presented identifying aeolian episodes, mudflow events from Ladakh Range and debris flows extending from Zanskar Range across present Indus River. Two temporal phases of water ponding within Spituk Sequence are also identified. The seismites recorded at various stratigraphic depths and their association with the sediment facies signifies gravity induced process besides possible seismic activity as an added phenomena. Linkage between paraglacial processes since Last Glacial to Recent is tracked and evaluated.

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Authors and Affiliations

  1. Department of Geology, Faculty of Science, Maharaja Sayajirao University of Baroda, Vadodara, 390 002, India

    Dhananjay A. Sant & Prabhin Sukumaran

  2. Geological Survey of India, Desert and Environmental Geology Division, Jaipur, 302 004, India

    Sudesh K. Wadhawan

  3. Department of Geology, University of Jammu, Jammu, 180 006, India

    Rajinder K. Ganjoo

  4. Indian Institute of Geomagnetism, Plot 5, Sector 18, Kalamboli, New Panvel (W), Navi Mumbai, 410 218, India

    Nathani Basavaiah

  5. Department of Geology and Geophysics, IIT Kharagpur, Kharagpur, 721 302, India

    Sourabh Bhattacharya

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  1. Dhananjay A. Sant
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  2. Sudesh K. Wadhawan
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  3. Rajinder K. Ganjoo
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Correspondence to Dhananjay A. Sant.

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Sant, D.A., Wadhawan, S.K., Ganjoo, R.K. et al. Linkage of paraglacial processes from last glacial to recent inferred from Spituk sequence, Leh valley, Ladakh Himalaya. J Geol Soc India 78, 147–156 (2011). https://doi.org/10.1007/s12594-011-0074-8

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