Abstract

In the present study an attempt has been made to delineate and characterize the different geomorphic units of Muguru Addahalla watershed located in the southern part of Karnataka State, India. The drainage network and topographic elevation contours have been delineated using toposheets. The geological units have been overlaid on the Indian Remote Sensing (IRS)-1D LISS-111 satellite imagery. The study area is basically a drainage-controlled region wherein the fluvio-geomorphological processes dominate on the surface. Based on the interpretation of satellite data, the hydrogeomorphic units like linear ridges, shallow moderate and deeply buried slopes, shallow valley fills and deep valley fills have been demarcated. These zones have been generated as vector layers using GIS and the geological and geomorphological maps of the study area have been compared. This integrated approach demonstrated that the IRS data used in conjunction with geology, drainage and topographic parameters helped in the evaluation of different geomorphological units and their characteristics. These features were also verified based on the field observations. The geomorphological units can be utilized for the management of natural resources.

Highlights

  • IntroductionA systematic study of landforms can reveal the signatures of the past and ongoing geological processes

  • Geomorphology deals with the study of the landforms

  • Residual hills, pediments, pediplain, piedmont zones, valleys and other landscape features are suitable for the occurrence of the water resources of any basin or region

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Summary

Introduction

A systematic study of landforms can reveal the signatures of the past and ongoing geological processes. Certain geological agents like rivers, glaciers, winds, etc relentlessly operate on the earth's crust to bring about the changes of degradation and aggradation. These features are important from the point of understanding the surface and subsurface water movements. Residual hills, pediments, pediplain, piedmont zones, valleys and other landscape features are suitable for the occurrence of the water resources of any basin or region. Rainfall pattern is yet another influencing factor in the landform evolution. Rainfall pattern will be playing a key role in terrain development and for water storage and replenishment. Analysis of rainfall pattern is vital for predicting droughts, cycles of surplus rainfall

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