Morphology, sedimentology and origin of an anomalous cut-off along the Pravara river, deccan trap region, India

J. Veena
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Abstract

River meanders have always been an intriguing subject in fluvial geomorphology because of their ubiquity, dynamism, remarkable forms and practical consequences of their movement. Sometimes a relatively straight channel flowing over bedrock may develop a lone meander bend cut-off which is very out of the place from the surrounding area. The occurrence of a sudden bend along a river may not be a meandering bend but may be manifestation of sudden change in the river dynamism due to many reasons, such as, lithology, change in rainfall regime, tectonics etc. The formation of such features highlights the behavior of river in the past. One such striking feature has been observed along the River Pravara in the Deccan Trap Region, Maharashtra, India. Rivers in Deccan Trap Region do not meander and form cut-offs by rule. It is rocky country where rivers flow in deeply incised bedrock. Hence, the observed feature displays a striking anomaly in this region. Hence, an attempt has been made in the present paper to evaluate the mode of formation of this single cut-off along this channel. Morphological and sedimentological data were generated and analyzed for the channel loop and the link channel to understand the competence of the river in the past and present which were directly or indirectly responsible for the development of this channel anomaly in this reach. Based on the results of the analysis and intensive field observations, it has been inferred that this is a classic example of natural morphological adjustment of a river when a set of events occurred, first retardation of vertical erosion encountering bedrock followed by series of floods to induce the channel to divert from the original path to resume the present course. Presence of a tributary further aided to the process of the loop development. The study can provide additional knowledge to the studies involving anomalous channel cut-offs at any part of the world.
印度德干圈闭区Pravara河沿岸异常断裂带的形态、沉积学和成因
河流曲流一直是河流地貌学中一个有趣的主题,因为它们无处不在,充满活力,形式显著,运动的实际后果。有时,流过基岩的一条相对笔直的河道可能会形成一条曲径弯曲的断裂带,这与周围地区非常不同。由于岩性、降雨变化、构造等多种原因,河流突发性弯曲的发生可能不是曲流弯曲,而是河流动力突变的表现。这些特征的形成凸显了河流过去的行为。在印度马哈拉施特拉邦的德干圈闭地区,沿着普拉瓦拉河观察到了这样一个引人注目的特征。德干圈闭地区的河流一般不曲流,不形成断流。这是一个多岩石的国家,河流在深深的基岩中流淌。因此,观测到的地物在这一区域显示出明显的异常。因此,本文试图对这条水道的单一截止点的形成方式进行评估。通过对河道环带和连接河道的形态和沉积资料进行分析,了解河道过去和现在的能力,从而直接或间接地对该河段河道异常的形成负责。根据分析结果和密集的实地观察,可以推断这是河流自然形态调整的一个经典例子,当一系列事件发生时,首先是垂直侵蚀遇到基岩的延迟,然后是一系列洪水,导致河道从原来的路径改道,恢复到现在的路线。支流的存在进一步促进了环流的发展。该研究可以为世界上任何地区的异常水道切断研究提供额外的知识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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