Journal of Geoscience and Eco Agricultural Studies - ISSN: 3067-7297

Stream Length Gradient Index (SL Index) to Longitudinal Profile of Rispna River in the Front of Lesser Himalaya, India

Abstract

Geologists and geomorphologists have employed various morphometric methods, techniques, and indices to study landform evolution, their origin, and spatial distribution. One of the widely used morphometric methods for the qualitative interpretation of slope-length gradient and drainage char-acteristics of rivers was proposed by Hack [1,2]. The present study applies the SL Index to analyse the morphotectonic frame work of the Rispana River, located in the Dehradun district of the Garhwal Himalaya, India. The method ology is based on a high-resolution Digital Terrain Model (DTM) gen-erated from 1:50,000 scale Survey of India topographic sheets with 20 m contour intervals. On the basis of slope elements, the longitudinal profile of the river was divided into 14 segments. SL Index values were calculated for each segment and represented through tabular and graphical methods to identify spatial anomalies along the river course. The SL Index values range from 1 to 11.48. Out of the 14 segments, three exhibit first-order anomalies, sev en show second-order anomalies, and the remaining four segments display no detectable anomalies. High SL values (11.00, 11.44, and 11.48) are associated with structurally resistant lithologies such as quartzite and dolomite, steep gradients due to tectonic uplift, and the presence of waterfalls and knickpoints. The SL Index shows an abrupt decline at segment 11 and subsequently fluctuates within moderate values (≈2-4), indicating gentler slopes and uniform sediment deposition in the downstream reaches within the Doon Valley. A dis-tinct contrast is observed between the two physiographic regions-the mountainous terrain and the Doon Valley Plain. The SL Index is consistently higher in the Lesser Himalayan zone and lower in the Doon Valley Plain. The application of the Hack Index proves to be highly effective for the geo-morphic analysis of Himalayan rivers, particularly in understanding the influence of lithology, tec-tonic control, and slope gradient.

DOI: doi.org/10.63721/26JGEAS0131

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