The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 18
... appear to be of the normal kind , and there is no evidence of the great crushing which must accompany lateral thrust . If none of these suggestions are considered satisfactory , it can only be argued that the Cambrian age of the Long ...
... appear to be of the normal kind , and there is no evidence of the great crushing which must accompany lateral thrust . If none of these suggestions are considered satisfactory , it can only be argued that the Cambrian age of the Long ...
Page 19
... appear to rest on the Archæan . It is true there are some signs of faulting , and Dr. Hicks believes the Lower beds are faulted out , but more evidence of this is required . Dr. Callaway favours me with the following remarks on the ...
... appear to rest on the Archæan . It is true there are some signs of faulting , and Dr. Hicks believes the Lower beds are faulted out , but more evidence of this is required . Dr. Callaway favours me with the following remarks on the ...
Page 21
... appears to have been broken off from the parent rock while still undecomposed , and in many cases is even now remarkably well preserved . It would seem , therefore , as if the denudation of the granitoid rock had been accomplished ...
... appears to have been broken off from the parent rock while still undecomposed , and in many cases is even now remarkably well preserved . It would seem , therefore , as if the denudation of the granitoid rock had been accomplished ...
Page 24
... appear that in Lower Cambrian times there was in Europe more land than sea , and that the subsequent changes throughout the Upper Cambrian and Ordovician periods tended to reverse this state of things Physical History of the British ...
... appear that in Lower Cambrian times there was in Europe more land than sea , and that the subsequent changes throughout the Upper Cambrian and Ordovician periods tended to reverse this state of things Physical History of the British ...
Page 33
... appears certain that there is a marked unconformity between the igneous group , or Bal- lantrae rocks , and the succeeding deposits of Upper Llan- deilo age . At the base of the latter is a coarse purple conglomerate containing ...
... appears certain that there is a marked unconformity between the igneous group , or Bal- lantrae rocks , and the succeeding deposits of Upper Llan- deilo age . At the base of the latter is a coarse purple conglomerate containing ...
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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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