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A GIS-based assessment of active tectonics from morphometric parameters and geomorphic indices of Assam Region, India

Patrick Kury
- 01 Dec 2022 - 
- Vol. 8, pp 100115-100115
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TLDR
In this paper , morphometric parameters and geomorphic indices for the Assam region are derived from SRTM DEM data of 30 m resolution using GIS to characterize the tectonic activity, which in turn influences the drainage pattern.
Abstract
Assam region is mainly formed by the deposit and erosion process of the Brahmaputra River. The frequency of seismic events results in landform deformation, which highly influences the drainage basin pattern and causes drainage anomalies, having a subsequent effect on the flood distribution pattern. In the present study, morphometric parameters and geomorphic indices for the Assam region are derived from SRTM DEM data of 30 m resolution using GIS to characterize the tectonic activity, which in turn influences the drainage pattern. The indices are classified into three tectonic activity classes, and the average of the classes is combined to generate the indices of relative active tectonics (IRAT). The four classes of IRAT are defined for the study area as (i) very high; Class 1 (1.57–1.80), (ii) high; Class 2 (1.81–2.06), (iii) moderate; Class 3 (2.07–2.26), and (iv) low; Class 4 (2.27–2.30). Class 1 corresponds to basins 1 and 6. Basins 2, 4, and 5 fall under Class 2. Class 3 consists of basins 7, 8, and 9, and Class 4 comprises basins 3 and 10. Results show that most of the study area lies in very high to moderate active tectonic zones and the identified zones are consistent with significant faults and thrusts present in the basins. The combined approach of GIS-based morphometric and geomorphic study allows for identifying deformed landforms resulting from active tectonics. The results can also be employed for the development of watershed management and sustainable land use planning.

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Citations
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References
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Journal ArticleDOI

Erosional development of streams and their drainage basins; hydrophysical approach to quantitative morphology

TL;DR: The most important single factor involved in erosion phenomena and, in particular in connection with the development of stream systems and their drainage basins by aqueous erosion is called crossgrading.
Journal ArticleDOI

Hypsometric (area-altitude) analysis of erosional topography.

TL;DR: The percentage hypsometric curve (area-altitude curve) as discussed by the authors relates horizontal cross-sectional area of a drainage basin to relative elevation above basin mouth, and is used to measure the sinuosity of form and proportionate area below the curve.
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Evolution of drainage systems and slopes in badlands at perth amboy, new jersey

TL;DR: In this article, the authors studied geomorphic processes and landforms in a small badlands area at Perth Amboy, New Jersey, and selected a fifth-order drainage system to analyze the development of erosional topography.
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The evolution of the great river systems of southern Asia during the Cenozoic India-Asia collision: rivers draining southwards

TL;DR: In this paper, the authors reconstructed the drainage history of southern Asia can be reconstructed by restoring the gross movements of the plates and the tectonic displacement, uplift, and erosion of individual Tectonic units.
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Analysis of drainage-basin symmetry as a rapid technique to identify areas of possible Quaternary tilt-block tectonics: An example from the Mississippi Embayment

TL;DR: In this paper, a rapid technique of drainage-basin analysis is presented that quantifies transverse topographic basin symmetry to discriminate between random and regionally preferred stream migrations and identify the direction of maximum migration.
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