5 edition of Geomorphology of Damodar Basin found in the catalog.
Geomorphology of Damodar Basin
S. N. P. Gupta
Includes bibliographical references.
|LC Classifications||GB438.I4 G86 2004|
|The Physical Object|
|Pagination||xii, 234 p. :|
|Number of Pages||234|
|LC Control Number||2003322963|
Geomorphology 2 • The word “geomorphology" comes from the Greek roots "geo,“ “morph,” and “logos,” meaning “earth,” “form,” and “study,” respectively. Therefore, geomorphology is literally “the study of earth forms.” • Geomorphologists are concerned primarily . development project for the Damodar Basin. The Damodar Flood Enquiry Committee suggested a comprehensive plan. This plan was based on the memorandum submitted by W.L. Voorduin, an engineer with the Tennesse Valley authority (TVA) in the USA. The Damodar Valley Corporation (DVC) was established on 18th February, to execute the Damodar File Size: 50KB.
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Urban Geomorphology: Landforms and Processes in Cities addresses the human impacts on landscapes through occupation (urbanization) and development as a contribution to anthropogenic geomorphology or "anthropogeomorphology." This includes a focus on land clearance, conservation issues, pollution, decay and erosion, urban climate, and anthropogenic climate change. The margins of the Gulf of Oman Basin range from convergent at the north to translation at the west and east, and passive at the south. The basin's northern margin has been a site of continuous subduction since Cretaceous time, which has led to the creation of an km long and km wide accretionary wedge, most of which is above sea level.
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This book explores the latest advances in our understanding Geomorphology of Damodar Basin book the evolution of the Ganga-Brahmaputra delta, examining the Damodar basin, Bhagirathi-Hooghly basin and Jalangi basin from historical, quantitative and applied geomorphology perspectives.
The evolution of the Ganga-Brahmaputra delta is highly complex and remains poorly understood. Damodar after travelling for about km. Damodar basin lies in the states of Jharkhand and West Bengal. Flood is a common phenomenon in lower Damodar Basin.
Both natural and anthropogenic causes are responsible for flood. This work is mainly concentrated in the river geomorphology and. This edited book presents a novel collection of field-based empirical studies on the Quaternary geomorphology of the Lower Ganga Basin.
The book covers a wide range of topics discussing various geomorphological facets of the Lower Ganga and its subsidiary rivers focussing on laterites, palaeoenvironment and palaeogeomorphology, palaeo-coastal landforms, neo-tectonism, tidal-fluvial.
bibliography on Geomorphology of Chotanagpur. He presented number of papers (,and ) which are considered as important contributions in the field of geomorphology.
Gupta () has published a book on Geomorphology of Damodar Basin, in this book he have done evolution of the drainage system, morphometric analysis andCited by: 1.
Influence of Faulting on the Extra-Channel Geomorphology of the Ajay-Damodar Interfluve in Lower Ganga Basin /_4. In book: Quaternary Geomorphology in India: Case Author: Suvendu Roy. Geology and Geomorphology Regional Environmental Characterization of the Campos Basin, Southwest Atlantic. Book • Edited by: Renato Oscar Kowsmann.
Browse book content. About the book. Search in this book. Search in this book. Browse content Table of contents. Discover the best Geomorphology in Best Sellers.
Find the top most popular items in Amazon Books Best Sellers. given in the bibliography at the end of the book). The title of the study was Socio-industrial metabolism of the Damodar Valley Area. The potential scope of the project was so vast, that to do justice to an area as large as the Damodar Basin would have taken a few lifetimes.
Hence the first taskFile Size: KB. This book explores the latest advances in our understanding of the evolution of the Ganga-Brahmaputra delta, examining the Damodar basin, Bhagirathi-Hooghly basin and Jalangi basin from historical.
The quantitative analysis of drainage system is an important aspect of characterization of watersheds. Morphometry is measurement and mathematical analysis of landforms. The present study is an attempt to evaluate the drainage morphometrics of Upper South Koel Basin using Remote Sensing and GIS approach.
A morphometric analysis was carried out to describe the topography and drainage Cited by: CiteScore: ℹ CiteScore: CiteScore measures the average citations received per document published in this title.
CiteScore values are based on citation counts in a given year (e.g. ) to documents published in three previous calendar years (e.g. – 14), divided by the number of documents in these three previous years (e.g.
– 14). Quantitative Dynamic Geomorphology - Drainage basin morphology (stream order, density etc.) (Horton,Strahler, ) - Newtonian mechanistic approach (stream power, fluvial erosion, diffusion/transport laws (Schumm.
Geomorphology of Parri Basin Fluvial Features Stream order/Drainage map of Parri Basin Drainage density variation map of Parri Basin Stream Frequency variation map of Parri Basin A Longitudinal profile of Parri Stream Area distance curve Hypsometric curve Slope category map of Parri BasinFile Size: KB.
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Damodar River (Pron: /ˈdæmoˌdaː/) is a river flowing across the Indian states of Jharkhand and West in mineral resources, the valley is home to large-scale mining and industrial activity. Earlier known as the Sorrow of Bengal because of its ravaging floods in the plains of West Bengal, the Damodar and its tributaries have been somewhat tamed with the construction of several dams.⁃ location: chulha pani (Chandwa/Tori), Latehar.
Analysis of the landuse classification revealed that Njaba drainage basin is made up of % farmland and grassland, % forest, % bare land, and % water, while the Orashi drainage basin comprises of % farmland, % urban settlement, % forest land, % bare land and % water body.
Alluvial and fluvial fans have long been the object of geomorphological and sedimentological research, but only a few books and article compilations have been dedicated specifically to these systems (Rachocki & Church ; Harvey et al.
; Schneuwly-Bollschweiler et al. ), compared with the many tens of publications devoted to the. Groundwater has long been an object of intense scrutiny. Only recently have methods become available that permit ecologists, hydrologists, and environmental scientists to assess the biotic and abiotic status of these all-important aquifers.
This book explores the latest advances in our understanding of the evolution of the Ganga-Brahmaputra delta, examining the Damodar basin, Bhagirathi-Hooghly basin and Jalangi basin from historical, quantitative and applied geomorphology perspectives.
Tectonics of Sedimentary Basins: Recent Advances focuses on key topics or areas where the greatest strides forward have been made, while also providing on-line access to the comprehensive book. Breakthroughs in new techniques are described in Section 1, including detrital zircon geochronology, cosmogenic nuclide dating.
From the above analysis (Table 3), we can say that annual runoff yield of Damodar Basin is much greater, ranging from million m 3 (Barhi) to million m 3 (Burdwan), for the decade of – It is easily seen that the potentiality of runoff generation is more or less the same in the upper catchment area of Damodar (– mm per year).Cited by: 8.Damodar River is located in the Indian states of Jharkhand and West Damodar River is considered to be one of the most important rivers in eastern India.
Mineral resources in the Damodar Valley have made it a large-scale mining and industrial center. The river is also known as the ‘Sorrow of Bengal’ because of its devastating floods in the plains of West g: Geomorphology.Himalayan Geomorphology Study of Himalayan Ramganga Basin Hardcover – January 1, by V.C.
Jha (Author) See all formats and editions Hide other formats and editions. Price New from Used from Hardcover "Please retry" — Cited by: 2.