Active Himalayan frontal fault, main boundary thrust and Ramgarh Thrust in southern Kumaun
KS Valdiya, RS Rana… - … Society of India, 1992 - indianjournalofmarketing.com
The Siwalik front has been lifted up 60-90 m against the Holocene IndoGangetic plains. The
movements on the Himalayan Frontal Fault are evident from 6-15 northward tilting of Late
Pleistocene Dun Gravel, and spectacular incised meanders in streams breaking through the
hill barrier, and uplift in three episodic phases of the fluvial terraces resting on the tilted Dun
Gravel.
movements on the Himalayan Frontal Fault are evident from 6-15 northward tilting of Late
Pleistocene Dun Gravel, and spectacular incised meanders in streams breaking through the
hill barrier, and uplift in three episodic phases of the fluvial terraces resting on the tilted Dun
Gravel.