Morphometric Analysis of Subbasins Along The Basalt-Granite Contact in The South East Deccan Volcanic Province, India

  • Authors

    • Deepak Wable School of Earth Sciences, Swami Ramanand Teerth Marathwada University,‎ ‎ Nanded – 431 606, Maharashtra, INDIA
    • Ramakant Kaplay Maharashtra National Law University, Mumbai – 400076, Maharashtra, INDIA
    • Udaykumar Sahu Department of Geology, Toshniwal College of Arts, Commerce and Sciences, ‎ Sengaon, Hingoli – 431 542, Maharashtra, INDIA
    • Divyesh Vyas School of Earth Sciences, Swami Ramanand Teerth Marathwada University,‎ ‎ Nanded – 431 606, Maharashtra, INDIA
    https://doi.org/10.14419/hm2j5z48

    Received date: October 29, 2025

    Accepted date: January 20, 2026

    Published date: January 24, 2026

  • Basalt-Granite Contact; Field Structures; Morphometric Analysis; Morphotectonics, SEDVP
  • Abstract

    Morphometric analysis of drainage basins using remote sensing (RS) and GIS is an effective ‎way to assess the influence of lithology and tectonics. In this paper, the authors evaluated lithostructural controls on the sub-basins along the contact between basalt and granite in the South East Deccan Volcanic Province (SEDVP) and the Eastern Dharwar Craton (EDC) margin. Thirty-‎six drainage sub-basins (mini- to micro-watersheds) located in basalt, granite, and along the ‎basalt-granite contact were selected to assess the influence of lithology and structures ‎‎(lineament, faults, etc.) on drainage morphology. Geological fieldwork was carried out along ‎the basalt-granite contact within the 62 km stretch from Adampur, Biloli (MH), to Bhainsa ‎‎(TS). Eleven profiles of basalt-granite contacts were reported, which are further referred to ‎classify the sub-basins based on lithology, namely, Category I: sub-basins that are located in ‎basalt, Category II: sub-basins partially located in basalt (Deccan traps) and granite ‎‎(basement), and Category III: sub-basins that are located in granite. In morphometric analysis, we have calculated drainage density (Dd), stream frequency (Fs), elongation ratio (Re), and asymmetry factors (Af). The assessment of morphometric analysis and reported ‎structures suggests that the (1) category I sub-basins are tectonically inactive, whereas category ‎II and III sub-basins are tectonically moderately active. (2) Reported evidence of sub-‎surface tectonic activity expressed as ‘minor faults’ within the basement granite underlying the thin capping of ‎basalt/basaltic soil is profoundly manifested in the sub-basins, which are corroborated by ‎morphotectonic evidence.

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  • How to Cite

    Wable, D., Kaplay , R. ., Sahu, U. ., & Vyas, D. . (2026). Morphometric Analysis of Subbasins Along The Basalt-Granite Contact in The South East Deccan Volcanic Province, India. International Journal of Advanced Geosciences, 14(1), 20-29. https://doi.org/10.14419/hm2j5z48