Abstract

The study indicates that analysis of morphometric parameters with the help of geographic information system (GIS) would prove a viable method of characterizing the hydrological response behaviour of the watershed. It is also well observed that remote sensing satellite data is emerging as the most effective, time saving and accurate technique for morphometric analysis of a basin. This technique is found relevant for the extraction of river basin and its stream networks through ASTER (DEM) in conjunction with remote sensing satellite data (Landsat etm+, 2013 and georeferenced survey of Indian toposheet, 1972). In this study, Kanhar basin a tributaries of Son River has been selected for detailed morphometric analysis. Seven sub-watersheds are also delineated within this basin to calculate the selected morphometric parameters. Morphometric parameters viz; stream order, stream length, bifurcation ratio, drainage density, stream frequency, form factor, circulatory ratio, etc., are calculated. The drainage area of the basin is 5,654 km2 and shows sub-dendritic to dendritic drainage pattern. The stream order of the basin is mainly controlled by physiographic and lithological conditions of the area. The study area is designated as seventh-order basin with the drainage density value being as 1.72 km/km2. The increase in stream length ratio from lower to higher order shows that the study area has reached a mature geomorphic stage.

Highlights

  • Morphometry is the measurement and mathematical analysis of the configuration of the earth’s surface, shape and dimension of its landforms (Clarke 1996; Agarwal 1998; Obi Reddy et al 2002)

  • The present study aims at using the remote sensing and geographic information system (GIS) technology to compute various parameters of morphometric characteristics of the Kanhar River watershed

  • The maximum stream order frequency is observed in case of first-order streams and for second order

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Summary

Introduction

Morphometry is the measurement and mathematical analysis of the configuration of the earth’s surface, shape and dimension of its landforms (Clarke 1996; Agarwal 1998; Obi Reddy et al 2002). The present study aims at using the remote sensing and GIS technology to compute various parameters of morphometric characteristics of the Kanhar River watershed. This is in consonance with the latest developments and researches as cited above. Highest Kanhar Divide (above 1,050 m): this area lies in the south-western part of Kanhar basin, where a series of flat topped and in pointed hillocks of different size are found They appeared to have been formed by Archaean rocks. Some of these summits show long continued erosion and which form platforms within the hillocks

The Upper Kanhar basin
Middle Kanhar basin
The Lower Kanhar basin
Methodology
Results and discussion
Conclusion
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