Titlebook: Quaternary of South-West England; S. Campbell,C. O. Hunt,N. Stephens Book 1998 Springer Science+Business Media Dordrecht 1998 Devonian.Ple

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使痛苦

The geomorphological evolution and Quaternary history of South-West England: a rationale for the seance to the sciences of geology and geo-morphology; more than 3000 sites have been selected. The full rationale of the GCR and the detailed criteria and guidelines used in site selection are given elsewhere (Crowther and Wimbledon, 1988; Allen ., 1989; Gordon and Campbell, 1992; Gordon and Sutherlan

Peculate

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integral

Pleistocene cave sequences,tricts (particularly the Mendips), and the Devonian limestones of south Devon (Figures 2.1 and 5.1), host numerous caves and cave systems, many of which contain important sediment sequences, faunal remains and artefacts. As a result, the caves have long attracted scientific interest and several loca

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細(xì)節(jié)

chemoprevention

sulcus

The Quaternary history of the Somerset lowland, Mendip Hills and adjacent areas,Figure 9–1). This region has considerable potential significance, because it contains important and unique evidence for extra-glacial Quaternary environments. Especially important are the interglacial marine deposits of the Burtle Formation, the interstadial marginal marine Low Ham Member and the ma

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