Morphometric Analysis of Kunda River Basin, Khargone District, Madhya Pradesh -Based on Watershed Approach

Authors

  • Lal Singh Solanki Research Scholar Vikram University Ujjain and Asst. Prof. Govt. J.S.T. P.G. College Balaghat, Madhya Pradesh 481101, India.
  • Vinita Kulshreshtha Department of Geology, Govt. P.G. College Mandsour, Madhya Pradesh 458001, India.
  • Mohammad Rizwan School of Studies in Earth Science, Vikram University, Ujjain, Madhya Pradesh 456010, India.

DOI:

https://doi.org/10.48165/

Keywords:

Kunda River, Groundwater, Environment, Morphometric analysis, Watershed, Khargone

Abstract

The Quantitative morphometric analysis is found to be dynamic study in considerate hydrological  characteristics and its collaboration with the environment of any Watershed scheme. The main objective of  the learning is to analyze the morphometric parameters of the Kunda River Watershed, Methods. The  proposed study area is confined to latitude 21050' 0'' to 210 55' 0'' Nandlongitude750 35' 0''to750 45'  0''E (Survey of IndiaToposheet No.46O/9. The study area has been covered 159.97 sq. km. kunda river  Watershed belonging to the northern part of Khargone district, is a solid rocks topography consisting  typically Basalt. The study area is composed of flat terrain with gentle slope, which consists of basaltic  lava flows. Geologically, these flows constitute a part of the Deccan Volcanic Province, the Watershed is  of fourth order drainage having drainage density, and stream frequency 0f 0.977 and 0.922 separately.  The Watershed shows extended in nature. The method practical to the river basin give a current  calculation of the morphometric parameters of the region. The drainage morphometric analysis is  important in range of water renew site, Watershed showing and groundwater visualization mapping. The  study would deliver an important data collection about future Watershed view of the area. 

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References

Agrawal, C. S. (1998). Study of drainage pattern through aerial data in Naugarh area of Varanasi district, U.P. Jour. Indian Soc. Remote Sensing, 26(4), 169-175.

Clarke, J. I. (1966). Morphometry from maps. In Dury, G.H. (Ed.) ‘Essays in Geomorphology, Heinmann, London, p. 235-274.

Horton, R.E. (1945). Erosional Development of streams and their drainage basins; Hydrophysical Approach to Quantitative Morphology. Bull. Geol. Soc. America, 56, 275-370.

Horton, R. E., (1932).Drainage basin characteristics. Trans. Amer. Geophys. Union, 13, 350-361.

Reddy, L., et. al. (2012). Hydro Geochemical Processes in the Groundwater Environment of Vemula area, Kadapa District, South India.

International Journal of Recent trends in Science & Technolog, 3, 18-24.

Schumm, S. A. (1956). The evolution of drainage systems and slopes in Bad Lands at Perth Amboy, New Jersey, Bull. Geol. Soc. Amer., 67, 597-646.

Singh, N. (1998); Geomorphology of Himalayan rivers (a case study of Tawi basin), Jay Kay Book House, JammuTawi.

Strahler, A. N. (1952 a). Dynamic basis of geomorphology, Geol. Soc. America Bull., 63, 923-938.

Strahler, A. N. (1952 b). Hypsometric (area altitude) analysis of erosional topography, Geol. Soc. Amer., Bull. 63, 1117-1142.

Strahler, A. N. (1958). Dimensional analysis applied to fluvially eroded land forms, Geol. Soc. Amer., Bull., 69, 279-300.

Strahler, A. N. (1964). Quantitative geomorphology of drainage basins and channel networks in hand book of applied hydrology (Ed. V.T. Chow), Mc-Graw Hill Book Co., New York, p. 4.39-4.76.

Strahler, A. N. (1968). Quantitative geomorphology, In: Fairbridge, R.W. (eds), The Encyclopedia of geomorphology, Reinhold Book Crop, New York.

Strahler, A. N., (1957). Quantitative analysis of watershed Geomorphology. Trans. Amer. Geophys. Union, 38, 913-920.

Published

2022-06-25

How to Cite

Solanki, L.S., Kulshreshtha, V., & Rizwan, M. (2022). Morphometric Analysis of Kunda River Basin, Khargone District, Madhya Pradesh -Based on Watershed Approach . Bulletin of Pure and Applied Sciences-Geology , 41(1), 149–155. https://doi.org/10.48165/