The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 2
... land . Sometimes nearly the whole area has formed part of continental land , and at other times it has been almost entirely submerged beneath the sea . But we can look back to an epoch in the geographical history of Britain when the ...
... land . Sometimes nearly the whole area has formed part of continental land , and at other times it has been almost entirely submerged beneath the sea . But we can look back to an epoch in the geographical history of Britain when the ...
Page 4
... land , except in shallow and land - surrounded seas like that which is sometimes called the German Ocean . Outside a continent which has a fairly uniform coast - line trending for a long distance in one direction there is gene- rally a ...
... land , except in shallow and land - surrounded seas like that which is sometimes called the German Ocean . Outside a continent which has a fairly uniform coast - line trending for a long distance in one direction there is gene- rally a ...
Page 5
... land , it may be assumed that no large rivers issued from the coast in question . Every case in which limestones occur must be dealt with on its own merits , and no hasty conclusion as to the dis- tance of land should be formed . There ...
... land , it may be assumed that no large rivers issued from the coast in question . Every case in which limestones occur must be dealt with on its own merits , and no hasty conclusion as to the dis- tance of land should be formed . There ...
Page 6
... land , though the water was doubtless clear and deep in those places where it attains great thickness . - Deep - water Beds . It is now generally acknowledged that the great mass of the rocks which compose our modern continents are such ...
... land , though the water was doubtless clear and deep in those places where it attains great thickness . - Deep - water Beds . It is now generally acknowledged that the great mass of the rocks which compose our modern continents are such ...
Page 7
... land . Subsi- dence would make no difference to this arrangement , but would only tend to increase the thickness of the deposit . The deposit would also thin out laterally , away from the central axis of deposition , but a transverse ...
... land . Subsi- dence would make no difference to this arrangement , but would only tend to increase the thickness of the deposit . The deposit would also thin out laterally , away from the central axis of deposition , but a transverse ...
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The Building of the British Isles: A Study in Geographical Evolution ... Alfred John Jukes-Browne No preview available - 2018 |
Common terms and phrases
Archæan Bagshot Bagshot Beds basin beds beneath Boulder-clay breccia Britain British calcareous Cambrian Carboniferous Limestone Chalk Channel Coal-measures coast coast-line conglomerate contain Crag Cretaceous deposits Devonian district Dyassic east eastern eastward edition elevation England Eocene epoch erosion estuarine evidence existed extended fathoms fauna feet thick formation formed fossils France freshwater Gault geographical Geol Geology Glacial gravels Greensand grits History infer Ireland island Isle Journ Jurassic Keuper lacustrine lake land London Clay Lower marine marls Memoir Miocene north-east northern northward occur ocean Old Red Sandstone older Oligocene Oolite Ordovician Paleozoic pebbles period Plate Pleistocene Pliocene portions Portrait present probably Professor Purbeck Quart region ridge rivers rocks sands Scotland sediment shales shallow shore Silurian southern stones strata submerged subsidence surface thin tion tract Trans Trias Triassic unconformity upheaval Upper valley Vectian vols Wales Wealden western westward Yorkshire
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