The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 2
... deposits , and it is only rarely that actual proof of the former existence of land in any district is found in the intercalation of purely freshwater deposits . Occasionally we meet with estuarine beds which indicate the close proximity ...
... deposits , and it is only rarely that actual proof of the former existence of land in any district is found in the intercalation of purely freshwater deposits . Occasionally we meet with estuarine beds which indicate the close proximity ...
Page 3
... deposits form a mass of considerable thick- ness , it is probable that much of the material was brought down by floods and torrents from a range of hills above the coast - line . We must remember , however , that such coarse deposits ...
... deposits form a mass of considerable thick- ness , it is probable that much of the material was brought down by floods and torrents from a range of hills above the coast - line . We must remember , however , that such coarse deposits ...
Page 4
... deposits and are seldom found in deeper water than fifty or sixty fathoms , except where the bottom slopes very steeply from the coast ; neither do they gene- rally occur at a greater distance than twenty or thirty miles from land ...
... deposits and are seldom found in deeper water than fifty or sixty fathoms , except where the bottom slopes very steeply from the coast ; neither do they gene- rally occur at a greater distance than twenty or thirty miles from land ...
Page 5
... 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 other beds with which they are ...
... 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 other beds with which they are ...
Page 6
... 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- lated in deep water at a great distance from land of a continental ...
... 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- lated in deep water at a great distance from land of a continental ...
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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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