Morphometric Analysis of Mithmumbri - Malvan Area, Sindhudurg District, West Coast of Maharashtra, India

M. Herlekar, Prafull B. Kamble, Arijit Chakraborty, Ramesh R. Nannaware
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Abstract

Morphometric analysis has been carried out from the Mithmumbari to Malvan area, Western part of Maharashtra in Sindhudurg district, India. The morphometric analysis is carried out in fourteen drainage basins, viz., Achra, Pyali, Golvan, Mithmumbari, Katvan, Kamtakhudi, Gavaliwadi, Kunkeshwar, Kandalgaon, Munge, Malvan, Masura, Belachiwadi and Tambalwadi. The morphology of these basins is governed by a number of drivers including tectonic processes mainly the Vijaydurg fault, Mithbav fault, Malvan fault and lineaments, climate and lithology that influence the river system over a range of timescales. The majority of the basins are highly dissected and structurally controlled. The drainage density is low, with moderate to steep slopes within the elongated basin. The Achra, Pyali, Golvan, Gavaliwadi, Kandalgaon, Munge and Malvan basins are structurally controlled. The lower values of length of overland flow in study area reveal that stream erosion is more dominant than sheet erosion. Achra, Pyali, Mithmumbri, Golvan and Malvan basins are higher stream power, which represents higher erosion of the basin indicates high river basin management measures. Achra, Pyali, Golvan, Katvan, Kamthakhudi, Gavaliwadi, Kunkeshwar, Munge, Masura, Belachiwadi and Tambalwadi basins are rapid uplift stage of the basin. The Achra, Pyali, Golvan and Kamthakhudi basins can be inferred as SSW tilting in response to tectonic tilt. The hypsometric analysis shows eight basins (Achra, Pyali, Mithmumbari, Kamtakhudi, Kunkeshwar, Gavaliwadi, Belachiwadi and Tambalwadi) under the mature stage, five basins (Katvan, Munge, Kandalgaon, Malvan and Masura)in the youth stage and one basin (Golvan) under the old stage. The mature stage drainage basins show significant incision and entrenchment as a result of the Late Quaternary upliftment of the study area. The stages of drainage basins development in the western part of Maharashtra thus identify tectonically active and quiescent phases. Keywords: Morphometric and Hypsometric Analysis, Structural Control Basin, RS-GIS, Sindhudurg District, West Coast of Maharashtra
印度马哈拉施特拉邦西海岸辛杜德格县 Mithmumbri - Malvan 地区形态计量分析
对印度马哈拉施特拉邦西部信德胡德格地区的米桑姆巴里至马尔万地区进行了形态计量分析。对 Achra、Pyali、Golvan、Mithmumbari、Katvan、Kamtakhudi、Gavaliwadi、Kunkeshwar、Kandalgaon、Munge、Malvan、Masura、Belachiwadi 和 Tambalwadi 等 14 个流域进行了形态分析。这些盆地的形态受多种因素的影响,包括构造过程,主要是维杰杜格断层、米特巴夫断层、马尔万断层和线状构造、气候和岩性,这些因素在不同的时间尺度上影响着河流系统。大多数盆地都是高度剖裂和结构受控的。在拉长的盆地内,排水密度较低,坡度适中至陡峭。Achra、Pyali、Golvan、Gavaliwadi、Kandalgaon、Munge 和 Malvan 盆地受结构控制。研究区域内较低的溢流长度值表明,溪流侵蚀比片状侵蚀更占优势。Achra、Pyali、Mithmumbri、Golvan 和 Malvan 盆地的河流侵蚀能力较强,这表明流域的侵蚀程度较高,说明流域管理措施得力。Achra、Pyali、Golvan、Katvan、Kamthakhudi、Gavaliwadi、Kunkeshwar、Munge、Masura、Belachiwadi 和 Tambalwadi 盆地处于快速隆起阶段。Achra、Pyali、Golvan 和 Kamthakhudi 盆地可以推断为因构造倾斜而发生的 SSW 倾斜。水位分析表明,八个盆地(Achra、Pyali、Mithmumbari、Kamtakhudi、Kunkeshwar、Gavaliwadi、Belachiwadi 和 Tambalwadi)处于成熟阶段,五个盆地(Katvan、Munge、Kandalgaon、Malvan 和 Masura)处于年轻阶段,一个盆地(Golvan)处于老化阶段。成熟阶段的流域由于研究区域第四纪晚期的隆起而出现了明显的内切和内陷。因此,马哈拉施特拉邦西部地区的排水盆地发展阶段可划分为构造活跃期和静止期。关键词形态计量和水力计量分析、构造控制盆地、RS-GIS、辛杜德格地区、马哈拉施特拉邦西海岸
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