Abstract
Study of morphometric parameters such as stream length (Lu) and stream length ratios (Rl), bifurcation ratio (Rb), drainage density (D), form factor (Rf), circularity ratio (Rc), elongation ratio (Re) and asymmetry factor (Af) in the Gola and Kalsa River Basins show a strong structural/tectonic control over the drainage in the study area and also indicate intense tectonic activity in the recent past. Field studies also suggest that several parts of the study area are structurally controlled and neotectonically active, e.g. incidences of landslides, presence of asymmetrical river terraces, river incision, formation of deep gorges, triangular facets and tilting of recent deposits etc. Morphometric parameters also suggest a possibility of flash floods and high discharges in few sub-basins.
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ACKNOWLEDGMENTS
The authors are grateful to the Head, Centre of Advanced Study in Geology, University of Lucknow (L-ucknow, India) for providing working facilities.
Funding
Authors are thankful to CSIR, Government of India, for providing financial support to Gaurav Joshi in the form of SRF (09/107(0394)/2018-EMR-I).
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Lal. Kumar, Joshi, G. & Agarwal, K.K. Morphometry and Morphostructural Studies of the Parts of Gola River and Kalsa River Basins, Chanphi-Okhalkanda Region, Kumaun Lesser Himalaya, India. Geotecton. 54, 410–427 (2020). https://doi.org/10.1134/S0016852120030048
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DOI: https://doi.org/10.1134/S0016852120030048