Titlebook: British Stratigraphy; F. A. Middlemiss Book 1974 George Allen & Unwin Ltd 1974 Cambrian.Carboniferous.Cretaceous.Deltas.Devonian.Jurassic.

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Book 1974 was necessary in these cases to make an arbitrary choice of one small part of the period, the geography of which could be illustrated. Candidates are advised not to spend time learning every detail of the outcrop patterns, but to con­ centrate upon the main areas of outcrop. I am indebted to Mrs. Jean Fyffe for the cartographic work.

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The Armorican Mountain-building, facts point to increasing uplift of the British area, with uplands which had been subject to tropical weathering (to give the red colouring) undergoing increasingly rapid erosion. The next beds that can be dated are of Upper Permian age and rest with violent unconformity on the Carboniferous.

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The Quaternary Glaciations,rate eras. Likewise the usual convenient division of the Quaternary into the Pleistocene Period, during which the glaciations occurred, and the Holocene or post-Glacial Period is artificial since there is no proof that the so-called post-glacial period of the present day is not merely an inter-glacial and that the ice will not advance again.

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Entscheidungen der Preispolitik,being therefore of shallow-water type in the former case but of deep-water type in the second. Thirdly, an essential part of the definition is that the geosynclinal sediments are later compressed and folded by the movement together of the sides of the downwarp, and so come to form fold-mountains.

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Entscheidungen der Kommunikationspolitik,ts are best seen on the south Pennine moors, especially in the Peak District. The change in lithology must reflect uplift of the land areas and increased transport of eroded, land-derived detritus into the sea.