The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 1
... formed during the main- tenance of certain physical and geographical conditions , and the restoration of the ... formation of islands and continents , and of their subsequent detrition and submer- gence . In this long succession of ...
... formed during the main- tenance of certain physical and geographical conditions , and the restoration of the ... formation of islands and continents , and of their subsequent detrition and submer- gence . In this long succession of ...
Page 2
... 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 foundations of our islands had been laid , and ...
... 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 foundations of our islands had been laid , and ...
Page 3
... formed in shallow water . As a general rule , the coarser the grain of the rock the shallower was the water in which it was formed , and the nearer was the shore from whence the component materials were derived , or along which they ...
... formed in shallow water . As a general rule , the coarser the grain of the rock the shallower was the water in which it was formed , and the nearer was the shore from whence the component materials were derived , or along which they ...
Page 5
... formed quite close in shore ; similar deposits of very fine grain occur also in the estuaries of large rivers . In dealing , therefore , with clays and shales we must be guided largely by their fossil contents , and by the nature of the ...
... formed quite close in shore ; similar deposits of very fine grain occur also in the estuaries of large rivers . In dealing , therefore , with clays and shales we must be guided largely by their fossil contents , and by the nature of the ...
Page 6
... formed within 200 or 300 miles of land , and very seldom include any deposits which resemble those now accumulating in the depths of the Atlantic and Pacific Oceans . There is only one formation in Britain which was undoubtedly accumu ...
... formed within 200 or 300 miles of land , and very seldom include any deposits which resemble those now accumulating in the depths of the Atlantic and Pacific Oceans . There is only one formation in Britain which was undoubtedly accumu ...
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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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