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Titlebook: Quaternary of the Thames; D. R. Bridgland,D. Q. Bowen,W. A. Wimbledon Book 1994 Joint Nature Conservation Committee 1994 Europe.Pleistocen

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書目名稱Quaternary of the Thames
編輯D. R. Bridgland,D. Q. Bowen,W. A. Wimbledon
視頻videohttp://file.papertrans.cn/782/781644/781644.mp4
叢書名稱Geological Conservation Review Series
圖書封面Titlebook: Quaternary of the Thames;  D. R. Bridgland,D. Q. Bowen,W. A. Wimbledon Book 1994 Joint Nature Conservation Committee 1994 Europe.Pleistocen
描述The principal aim of this volume is to provide descriptions of Sites of Special Scientific Interest, selected as part of the Geological Conservation Review, that yield evidence for the Pleistocene history of the River Thames and its tributaries. Although defined thematically, the volume covers all Pleistocene GCR sites in the Thames valley. A number of sites in southern East Anglia are also included because they provide important evidence bearing on the history of the Thames system. The justification for a GCR volume devoted to the Thames lies in the special importance of the river in the British Quaternary. The volume is con- cerned with the history of Britain over approximately the last two million years of geological time, during the repeated glacial phases of the Quaternary ‘Ice Age‘ and the warmer intervals between them. Many such climatic fluctuations are recorded in the deposits of the Thames, which can be shown to have existed as the predominant west to east drainage line in south-eastern England throughout the Pleistocene. The Thames has left a detailed record of its earlier presence in the form of deposits, which comprise fluvially aggraded floodplain sediments (predomina
出版日期Book 1994
關(guān)鍵詞Europe; Pleistocene; ocean; oceanic; quaternary; hydrogeology
版次1
doihttps://doi.org/10.1007/978-94-011-0705-1
isbn_softcover978-94-010-4303-8
isbn_ebook978-94-011-0705-1
copyrightJoint Nature Conservation Committee 1994
The information of publication is updating

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The Pleistocene of the Thames,r belies its importance to British Quaternary geology, however, since Thames sediments provide a framework for this the latest part of the geological record in Britain. Indeed, there is abundant evidence to show that the modern Thames is a mere shadow of its Pleistocene forebear. Not only did it onc
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The Upper Thames basin, catchment areas of the various streams that combine to form the Thames upstream from the Chiltern escarpment (Fig. 2.1). In many ways the Upper Thames is most easily treated as a separate system from the valley downstream of the Goring Gap. Its Quaternary terrace record is extensive, particularly i
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