Geophysical Features of Coastal West Bengal

R. K. Chattopadhyay
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Abstract

The geo-physical features of the vast stretch of land constituting the study area have been delineated in this chapter. The present study area mainly comprises the mature and active delta regions, that is, the modern districts of North and South 24-Parganas, Howrah, Hooghly, parts of Nadia and East and West Midnapur. In addition to the mature and active delta regions, the adjoining upland areas lying to the south and west of the present district of West Midnapur have also being taken into consideration. The geo-physical considerations have led the author to classify the study area into three arbitrary zones. However, these zones should not be viewed as watertight compartments. A sub-section deals with the physiographic features of the three zones. The chapter also discusses coast-line fluctuations and river course change since the seasonal movements of sea water, stagnation of water and subsequent lagoon formation, changes in the courses of the main rivers, and excessive flow from the upper reaches often leading to floods have all influenced the surviving strategies and even the development of settlements in the coastal tract. Changes in river courses in many instances have been instrumental in the survival and spread of sites.
西孟加拉邦海岸的地球物理特征
本章描述了构成研究区的大片土地的地球物理特征。目前研究区主要包括成熟和活跃的三角洲地区,即24-Parganas北部和南部的现代地区,Howrah, Hooghly, Nadia的部分地区和Midnapur的东部和西部。除了成熟和活跃的三角洲地区外,位于西米德纳普尔地区南部和西部的毗邻高地地区也被考虑在内。基于地球物理的考虑,笔者将研究区任意划分为三个带。然而,这些区域不应被视为水密隔间。有一小节论述了这三个地区的地理特征。本章还讨论了海岸线的波动和河流的变化,因为海水的季节性运动、水的停滞和随后的泻湖形成、主要河流的河道变化以及上游经常导致洪水的过度流动都影响了沿海地区的生存策略,甚至是定居点的发展。在许多情况下,河道的变化有助于遗址的生存和传播。
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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