Neotectonic Evidences of Rejuvenation in KaurikChango Fault Zone, Northwestern Himalaya

DOI: 10.4236/jgis.2010.23024   PDF   HTML     5,907 Downloads   11,152 Views   Citations


Neotectonic investigations using morphotectonic parameters such as basin asymmetry, drainage anomalies, digital data interpretation and geomorphic field evidences were carried out in Satluj river valley downstream of Khab in the Kaurik Chango Fault (KCF) zone. The study reveals the presence of a northsouth trending fault which is similar to the KCF. Unpaired, tilted terraces, V shaped valleys, deep gorges and lakes are the manifestations of fault movement in the area. Presence of deformation structures preserved in the palaeolake profile at Morang indicates that the area has also been seismically active in the past. In this paper we present a conceptual model of the formation of lakes in KCF zone. Morphometric analysis was carried out with the help of Digital Elevation Models (DEMs) and field investigations.

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M. Joshi, G. Kothyari, A. Ahluvalia and P. Pant, "Neotectonic Evidences of Rejuvenation in KaurikChango Fault Zone, Northwestern Himalaya," Journal of Geographic Information System, Vol. 2 No. 3, 2010, pp. 169-176. doi: 10.4236/jgis.2010.23024.

Conflicts of Interest

The authors declare no conflicts of interest.


[1] A. Gansser, “The Geology of Himalaya,” Wily Inters-cience, London, 1964, p. 289.
[2] T. Nakata, “Geomorphic History and Crustal Movements of the Himalayas,” Institute of Geography Tohoku Uni-versity, Sendai, 1972, p. 77.
[3] T. Nakata, O. Kenshiro and S. H. Khan, “Active Faults, Stress Field and Plate Motion along the IndoEurasian Plate Boundary,” Tectonophysics, Vol. 181, No. 14, 1990, pp. 8395.
[4] J. C. Atchinson, J. R. Ali and A. M. Davis, “When and Where did India and Asia Collide?” Journal of Geophys-ical Research, Vol. 112, 2007, pp. 119.
[5] H. H. Hayden, “The Geology of Spiti with Parts of Bu-shahr and Rupshu,” Geological Survey of India Memoir, Vol. 6, 1904, pp. 1121.
[6] V. J. Gupta and N. S. Virdi, “Geological Aspects of Kin-naur Earthquake, Himachal Pradesh,” Journal of Geolog-ical Society India, Vol. 16, No. 4, 1975, pp. 512514.
[7] O. N. Bhargava and U. K. Bassi, “Geology of SpitiKin-naur Himachal Himalaya,” Memoir Geological Survey of India, Vol. 124, 1998, p. 212.
[8] O. N. Bhargava, R. N. Srivastava and S. K. Gadhoke, “The ProterozoicPalaeozoic Spiti Sedimentary Basin,” In: S. K. Tandon, C. Pant and S. M. Casshyon, Eds., Sedi-mentary Basins of India: Tectonic Context, Gyanodaya Prakashan, Nainital, 1991, pp. 236260.
[9] K. N. Khattri, K. Rai, A. K. Jain, H. Sinvhal, V. K. Gaur and R. S. Mithal, “The Kinnaur Earthquake, Himachal Pradesh, India of 19th January 1975,” Tectonophysics, Vol. 49, No. 12, 1978, pp. 121.
[10] S. Singh and A. K. Jain “Paleosiesmicity: Geological Evidences along the KaurikChango Fault Zone and Other Related Areas in LahaulSpiti and Ladakh Himalaya,” In: O. P. Varma, Ed., Highlights in Earth Sciences DST's Spl. Vol. 2 on Seismicity, International Geological Congress, 2001, pp. 205225.
[11] O. N. Bhargava, S. S. Ameta, R. K. Gaur, S. Kumar, A. N. Agarawal, P. M. Jalote and M. L. Sadhu, “The Kinnaur (H.P., India) Earthquake of 19 January, 1975: Summary of Geoseismological Observations,” Bulletin of the Indian Geological Association, Vol. 11, No. 1, 1978, pp. 3953.
[12] T. N. Bagati, “Lithostratigraphy and Facies Variation in the Spiti Basin (Tethys), Himachal Pradesh,” Journal of Himalayan Geology, Vol. 1, No. 1, 1990, pp. 3547.
[13] A. K Jain and S. Singh, “Palaeoearthquakes along the KaurikChango Fault Zone, SatlujSpiti Valleys, Himachal Pradesh, India: Geological Evidence. Extended Abstract of IndoUS Workshop on Palaeoseismicity,” WIHG, De-hradun, 1997, pp. 6267.
[14] R. Mohindra and T. N. Bagati “Seismically Induced Soft Sediment Deformation Structures (Seismites) around Sum do in the Lower Spiti Valley (Tethys Himalaya),” Sedi-mentary Geology, Vol. 101, No. 1, 1996, pp. 6983.
[15] D. Banerjee, A. K. Singhvi, T. N. Bagati and R. Mohindra, “Luminescence Chronology of Seismites at Sumdo (Spiti Valley) Near KaurikChango Fault, Northwestern Himalaya,” Current Science, Vol. 73, No. 3, 1997, pp. 276281.
[16] V. P. Sharma, “Geology of the KulluRampur Belt, Hi-machal Pradesh,” Memoir Geological Survey of India, Vol. 106, No. 2, 1976, pp. 235403.
[17] A. P. Tiwari, R. K. Gaur and S. S. A. Ameta, “Note on the Geology of a Part of Kinnaur District, Himachal Pradesh. Him,” Geology, Vol. 8, No. 1, 1978, pp. 574 582.
[18] U. K. Bassi and S. A. Chopra, “Contribution to the Ge-ology of Kinnaur Himalaya, Himachal Pradesh,” Interna-tional Journal of Earth Sciences, Vol. 10, No. 1, 1983, pp. 9699.
[19] S Srikantia and O. N. Bhargava, “Geology of Himachal Pradesh,” Geological Society of India, 1998, p. 406.
[20] S. S. Ameta, “Some Observations on Geomorphology of Spiti Valley, Lahaul and Spiti distt. Himachal Pradesh,” Himalayan Geology, Vol. 9, No. 2, 1997, pp. 646656.
[21] C. A. Keller and N. Pinter, “Active Tectonics: Earthquake, Uplift and Landscape,” Prentice Hall, New Jersey, 1996, p. 338.
[22] N. S. Virdi, G. Philip and S. Bhattacharya, “Neotectonic Activity in the Markanda and Bata River Basins, Himachal Pradesh, NW Himalaya: A morphotectonic Approach,” International Journal of Remote Sensing, Vol. 27, No. 10, 2006, pp. 20932099.
[23] A. W. Burnett and S. A. Schumm, “Alluvial River Respo nse to Teotectonic Deformation in Louisiana and Missis-sippi,” Science, Vol. 222, No. 4619, 1983, pp. 4950.
[24] S. Ouchi, “Response of Alluvial Rivers to Slow Active Tectonic Movement,” Geological Society of America Bulletin, Vol. 96, No. 4, 1985, pp. 504 515.
[25] D. I. Gregory and S. A. Schumm, “The Effect of Active Tectonics on Alluvial River Morphology,” In: K. S. Ri-chards, Ed., River Channels: Environment and Process, Blackwells, London, 1987, pp. 4168.
[26] S. A. Schumm, J. F. Dumont and J. M. Holbrook, “Active Tectonics and Alluvial Rivers,” Cambridge University Press, New York, 2000, p. 276.
[27] V. Jain and R. Shina, “Response of Active Tectonics on the Alluvial Bagmati River, Himalayan Foreland Basin, Eastern India,” Geomorphology, Vol. 70, 2005, pp. 339 356.
[28] W. B. Bull and L. D. Mc. Fadden, “Tectonic Geomor-phology North and South of Garlock Fault California,” In: D. O. Doehring, Ed., Geomorpholoy in Arid Regions, Proceedings of 8th Annual Geomorphology Symposium, University of New York, Binghampton, 1977, pp. 115 137.
[29] L. Mayer, “Tectonic Geomorphology of Escarpments and Mountain Fronts,” In: R. E. Wallace, Ed., Active Tectonics, National Research Council, Washington, D.C., 1985, pp. 125135.

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