[Banerjee D, Singhvi A, Pande K, Gogte V and Chandra BP, 1999. Towards a direct dating of fault gouge using luminescence dating technique-methodology and aspect 1999. Current Science 77: 256-268.]Search in Google Scholar
[Bartarya SK and Valdiya KS, 1989. Landslides and erosion in the catchment of the Gaula River, Kumaun Lesser Himalaya, India. Mountain Research and Development 9(4): 405-419.10.2307/3673588]Search in Google Scholar
[Bilham R and Gaur VK, 2000. Geodetic contributions of the study of seismotectonics in India. Current Science 79(9): 1259-1269.]Search in Google Scholar
[Bilham R, Bendic KR and Gaur V, 1998. Geodetic constraints on the translation and deformation of India: Implication for future great Himalayan earthquakes. Current Science 74(3): 213-229.]Search in Google Scholar
[Bollinger L, Henry P and Avouac JP, 2006. Mountain building in the Nepal Himalaya: Thermal and kinematic model, Earth Planet. Science Letter 244(1-2): 58-71, DOI 10.1016/j.epsl.2006.01.04510.1016/j.epsl.2006.01.045]Search in Google Scholar
[Bookhagen B, Thiede R and Strecker MR, 2005. Abnormal Monsoon years and their control on erosion and sediment flux in the high, arid northwestern Himalaya. Earth and Planetary Science Letters 231(1-2): 31-146, DOI 10.1016/j.epsl.2004.11.014.10.1016/j.epsl.2004.11.014]Search in Google Scholar
[Burbank DW and Raynolds RGH, 1988. Stratigraphic keys to the timing of thrusting in terrestrial foreland basin: Application to the Northwestern Himalaya. In: Kleinspshn KL and Paola C, eds., New perspective in basin analysis. New York, Springer-Verlag: 331-351.10.1007/978-1-4612-3788-4_17]Search in Google Scholar
[Hodges KV, Parrish RR and Searle MP, 1996. Tectonic evolution of the central Annapurna Range, Nepalese Himalaya. Tectonics 15(6): 1264-1291, DOI 10.1029/96TC01791.10.1029/96TC01791]Search in Google Scholar
[Hodges KV, Wobus C, Ruhl K, Schilsdgen T and Whipple K, 2004. Quaternary deformation, river steepening and heavy precipitation at the front of the Higher Himalaya range, Earth and Planetary Science Letters 220(3-4): 379-389, DOI 10.1016/S0012-821X(04)00063-9.10.1016/S0012-821X(04)00063-9]Search in Google Scholar
[Hoek E and Bray JW, 1977. Rock slope. London, Engineering Institute of Mining and Metallurgy: 290pp.]Search in Google Scholar
[Kayal JR, 2001. Microearthquake activity in some parts of the Himalaya and the tectonic model. Tectonophysics 339(3-4):331-351, DOI 10.1016/S0040-1951(01)00129-9.10.1016/S0040-1951(01)00129-9]Search in Google Scholar
[Kotlia BS, Nakayama K, Bhalla MS, Phartyal B, Kosaka T, Joshi M, Sanwal J and Pande RN, 2001. Lithology and magnetic stratigraphy of the Lower-Middle Siwalik succession between Kathgodam and Ranibag, Kumaun Himalaya. Journal of the Geological Society of India 58(5): 411-423.]Search in Google Scholar
[Kotlia BS, Phartiyal B, Kosaka T and Bohra A, 2008. Magnetostratigraphy and lithology of Miocene-Pliocene Siwalik deposits between Tanakpur and Sukhidang, southeastern Uttarakhand Himalaya, India. Himalayan Geology 29(2): 127-136.]Search in Google Scholar
[Kumar S, Wesnousky SG, Rockwell TK, Briggs RW, Thakur VC and Jayangondaperumal R, 2006. Paleoseismic evidences of grate surface rupture earthquakes along the Indian Himalaya. Journal of Geophysical Research 111: B03304, DOI 10.1029/2004JB003309.10.1029/2004JB003309]Search in Google Scholar
[Lave J and Avouac JP, 2000. Active folding of fluvial terraces across the Siwaliks Hills, Himalayas of central Nepal. Journal of Geophysical Research 105(B3): 5735-5770, DOI 10.1029/1999JB900292.10.1029/1999JB900292]Search in Google Scholar
[Macfarlane AM, 1993. Chronology of tectonic events in the crystalline core of the Himalaya, Langtang National Park, central Nepal. Tectonics 12(4): 1004-1025, DOI 10.1029/93TC00916.10.1029/93TC00916]Search in Google Scholar
[Malik JN and Nakata T, 2003. Active faults and related Late Quaternary deformation along the Northwestern Himalayan Frontal Zone, India. Annals of Geophysics 46(5): 917-936.]Search in Google Scholar
[Markland JT, 1972. A useful technique for estimating the stability of rock slopes when the rigid wedge sliding type of failure is expected. Imperial College, Rock Mechanics Research Report 19: 10pp.]Search in Google Scholar
[Meigs AJ, Burbank DW and Beck RA, 1995. Middle-late Miocene (>10 Ma) formation of the Main Boundary Thrust in the western Himalaya. Geology 23(5): 423-462, DOI 10.1130/0091-7613(1995)023<0423:MLMMFO>2.3.CO;210.1130/0091-7613(1995)023<0423:MLMMFO>2.3.CO;2]Search in Google Scholar
[Molnar P, 2003. Geomorphology: Nature, nurture and landscape. Nature 426: 612-614, DOI 10.1038/426612a.10.1038/426612a]Search in Google Scholar
[Khwaja M and Khwaja AA, 2005. Seismic activity along the Main Boundary Thrust (MBT), Pakistan. Geological Bulletin University of Peshwar 38: 23-30.]Search in Google Scholar
[Nakata T, 1972. Geomorphic History and Crustal movements of the Himalaya. Institute of Geography, Tohuku University, Aendai: 77pp.]Search in Google Scholar
[Nakata T. and Kumahara, Y., 2002. Active Faulting in and around Himalaya, and its significance in the collision tectonics Active fault Research 22: 7-16.]Search in Google Scholar
[Pant PD and Luirei K, 2005. Malpa rockfalls of 18th August 1998 in northeastern Kumaun Himalaya. Journal of the Geological Society of India 54: 415-420.]Search in Google Scholar
[Pollitz F, Banerjee P, Grijalva K, Nagarajan B and Burgmann R, 2008. Effect of 3-D viscoelastic structure on post seismic relaxation from the 2004 M = 9.2 Sumatra earthquake. Geophysical Journal International 173(1): 189-204, DOI: 10.1111/j.1365-246X.2007.03666.x10.1111/j.1365-246X.2007.03666.x]Search in Google Scholar
[Rawat KS and Kothyari GC, 2007. The mass movement disaster at the Ampadav locality in the Kumaun Siwaliks, Nainital, and Uttaranchal. In: Saklani PS, ed., Himalaya: Geological Aspect 5: 149-157.]Search in Google Scholar
[Seeber L, Armbruster AG and Quittmeyer J, 1981. Seismicity and continental subducion in the Himalayan Arc. In: Gupta HK and Delany FM, eds., Zagros, Hindukush, Himalya. Geodynamic Evolution, Geodynamic Series 3: 215-242.10.1029/GD003p0215]Search in Google Scholar
[Singhvi AK, Banerjee D, Pande K, Gogte V and Valdiya KS, 1994. Luminescence studies on neotectonic events in south-central Kumaun Himalaya - A feasibility study. Quaternary Science Reviews 13(5-7): 595-600, DOI 10.1016/0277-3791(94)90083-3.10.1016/0277-3791(94)90083-3]Search in Google Scholar
[Srivastava P and Misra DK, 2008. Morpho-sedimentary records of active tectonics at the Kameng river exit, NE Himalaya. Geomorphology 96(1-2): 187-198, DOI 10.1016/j.geomorph.2007.07.01910.1016/j.geomorph.2007.07.019]Search in Google Scholar
[Starkel L, 2003. Climatically controlled terraces in uplifting mountain areas. Quaternary Science Reviews 22: 2189-2198, DOI 10.1016/S0277-3791(03)00148-3.10.1016/S0277-3791(03)00148-3]Search in Google Scholar
[Valdiya KS, 2001. Reactivation of terrain-defining boundary thrusts in Central sector of the Himalaya: Implication. Current Science 81(11): 1418-1430.]Search in Google Scholar
[Valdiya KS, 2003. Reactivation of Himalayan frontal fault: Implication. Current Science 85(7): 1031-1040.]Search in Google Scholar