Abstract

Mountainous rivers are the most significant source of water supply in the Himalayan provinces of India. The drainage basin dynamics of these rivers are controlled by the tectonomorphic parameters, which include both surface and subsurface characteristics of a basin. To understand the drainage basin dynamics and their usefulness in watershed prioritisation and management in terms of soil erosion studies and groundwater potential assessment and flood hazard risk reduction in mountainous rivers, morphometric analysis of a Himalayan River (Supin River) basin has been taken as a case study. The entire Supin River basin has been subdivided into 27 subwatersheds and 36 morphometric parameters have been calculated under four broad categories: drainage network, basin geometry, drainage texture, and relief characteristics, each of which is further grouped into five different clusters having similar morphometric properties. The various morphometric parameters have been correlated with each other to understand their underlying relationship and control over the basin hydrogeomorphology. The result thus generated provides adequate knowledge base required for decision making during strategic planning and delineation of prioritised hazard management zones in mountainous terrains.

Highlights

  • Morphometry is the measurement and mathematical analysis of the configuration of the earth’s surface and of the shape and dimension of its landforms [1]

  • The Main Central Thrust (MCT) crosses the basin in northwest-southeast direction with subwatersheds like WS3, WS15, WS16, and WS17 lying on its hanging wall and WS18 and WS19 lying on its footwall

  • The Munsiari Thrust (MT) crosses the basin in an east-west direction and WS6, WS8, WS20, WS21, WS26, and WS27 are along the hanging wall of MT whereas WS2, WS22, WS23, WS24, and WS27 are along the footwall of MT

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Summary

Introduction

Morphometry is the measurement and mathematical analysis of the configuration of the earth’s surface and of the shape and dimension of its landforms [1]. Application of quantitative techniques in morphometric analysis of drainage basins was initially undertaken by Horton et al [2,3,4,5,6,7,8] from topographic maps using manual methods. Quantitative techniques have been applied to study the morphometric properties of different drainage basins in India [14,15,16,17,18,19,20,21,22,23]. Several authors have studied morphometric properties of drainage basins as indicators of structural influence on drainage development and neotectonic activity [24,25,26,27]. Watershed prioritisation based on morphometric characteristics has been carried out and aids in the mapping of high flood potential and erosion prone zones [33,34,35,36,37]

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