A quantitative analysis of the ramganga drainage basin and structural control on drainage pattern in the fault zones, Uttarakhand

• Published in: Journal of the Geological Society of India Vol. 86; no. 1; pp. 9 - 22
• Main Authors: Asthana, A. K. L., Gupta, Anil K., Luirei, Khayingshing, Bartarya, S. K., Rai, S. K., Tiwari, S. K.
• Format: Journal Article
• Language: English
• Published: New Delhi Springer India 01.07.2015; Springer Nature B.V
• Subjects: Basins; Catchment areas; Drainage; Drainage basins; Drainage patterns; Earth and Environmental Science; Earth Sciences; Fault lines; Fluvial deposits; Geology; Geophysics; Hydrogeology; Quantitative analysis; River basins; Rivers; Stream gradient; Streams; Valleys; Uttarakhand India; India; Garhwal Himalaya; Fault zone; Drainage analysis; Landform development; Uttarakhand; Ramganga basin
• ISSN: 0016-7622; 0974-6889
• DOI: 10.1007/s12594-015-0276-6

The present study incorporates quantitative analysis of drainage of the Ramganga basin, Garhwal Himalaya, Uttarakhand. The drainage parameters (linear, areal and relief) of the Ramganga basin from Dudhatolidhar peak its point of origin to Kalagarh from where the river Ramganga enter into the plain, are covered. The impact of the morphological characters on the terrain is reflected by the drainage basin of the area. The calculated values of all the morphometric parameter of 38 V th order intrabasins for different lithotectonic units were computed under four sectors viz., NE of NAT, between NAT and SAT, between SAT and MBT and downstream of MBT. In the lower reaches of Ramganga basin the various morphometric parameters shows existence of proportionality between stream length and catchment area while such proportionality is non-existence in the crystalline zone. Structural control on the drainage patterns of the Ramganga river and its tributaries are observed in the form of straight course, wide valleys with thick fluvial deposits and relatively gentle stream gradient along the transverse faults to incised valleys; less fluvial deposits in the banks and steeper stream gradient with knick points in the hanging wall of thrusts.