The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 4
... miles in water be- fore it becomes so rounded as to assume the form of a miniature pebble . In sand from the seashore of Cornwall Mr. Phillips found that the quartz grains between one- twentieth and one - fiftieth of an inch diameter ...
... miles in water be- fore it becomes so rounded as to assume the form of a miniature pebble . In sand from the seashore of Cornwall Mr. Phillips found that the quartz grains between one- twentieth and one - fiftieth of an inch diameter ...
Page 6
... 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- lated in deep water at a ...
... 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- lated in deep water at a ...
Page 17
... miles the Harlech series has thinned from 3,000 feet to , perhaps , 100 feet of grit and conglomerate . This suggests that the surface of the Archæan rock formed a steep slope , inclining to the south - east , when the Cambrians were ...
... miles the Harlech series has thinned from 3,000 feet to , perhaps , 100 feet of grit and conglomerate . This suggests that the surface of the Archæan rock formed a steep slope , inclining to the south - east , when the Cambrians were ...
Page 18
... miles apart . But the faults 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 ...
... miles apart . But the faults 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 ...
Page 29
... miles . m River Severn . n . Trias and Dyas . m . Carboniferous . f . Old Red Sandstone . e . Silurian . d . Ordovician . c . Cambrian shales . b . Cambrian sandstone . a . Archæan . m Staffordshire which is traversed by the section ...
... miles . m River Severn . n . Trias and Dyas . m . Carboniferous . f . Old Red Sandstone . e . Silurian . d . Ordovician . c . Cambrian shales . b . Cambrian sandstone . a . Archæan . m Staffordshire which is traversed by the section ...
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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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