Horan Valley Basin Geomorphological Aspects Assessment by Integrating Hypsometric Analysis with Remotely Sensed Morphometric Characteristics

Authors

  • Laith A. Jawad Remote Sensing Unit, College of Science, University of Baghdad https://orcid.org/0000-0002-2205-5526
  • Ahmed A. Zaeen Remote Sensing Unit, College of Science, University of Baghdad
  • Tariq Z. Hamood Remote Sensing Unit, College of Science, University of Baghdad

DOI:

https://doi.org/10.24996/ijs.2024.65.1.45

Keywords:

Geomorphology, SRTM DEM, Hypsometric analysis, GIS, Remote sensing

Abstract

     The extraction, study, and accurate interpretation of the morphology database of a basin are the basic blocks for building a valid geomorphological understanding of this basin. In this work, a new approach is presented which is to use three different GIS based methods to extract databases with specific geographical information and then use the concept of information intersection to make a realistic geomorphological perspective for the study area.

In the first method, data integration of remote sensing images from Google Map and SRTM DEM images were used to identify Horan basin borders.

In the second method, the principle of data integration was represented by extracting the quantitative values of the morphometric characteristics that were affected by the geomorphological condition of the studied basin, such as the shape factor, circulation factor, and relief ratio, then eliciting an optimal conception of the geomorphological condition of the basin from the meanings and connotations of these combined transactions.

The third method used the same principle by taking the optimal inferences from the integration of the interpretation of the values of the Hypsometry integration coefficients for each area in the basin separately with the integration value of the drawing curve for the relative heights of the basin areas with their relative areas. It was found, from the values of the coefficients, that the areas (A, B, C, D, and F) were still in the early stages of youth. Whereas the E region was in the maturity stage and the G region was in the monadnock stage of the geomorphological cycle. As for the integral value of the curve, it indicated 48. 559 % erosion from the surface of the basin only, and that its boundaries were subject to change and widening.

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Published

2024-01-30

Issue

Section

Remote Sensing

How to Cite

Horan Valley Basin Geomorphological Aspects Assessment by Integrating Hypsometric Analysis with Remotely Sensed Morphometric Characteristics. (2024). Iraqi Journal of Science, 65(1), 583-592. https://doi.org/10.24996/ijs.2024.65.1.45

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