The Building of the British Isles: A Study in Geographical Evolution |
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Page 2
... seems to be desirable . The greater part of the strata with which the geologist has to deal are marine deposits , and it is only rarely that actual proof of the former existence of land in any district is found in the intercalation of ...
... seems to be desirable . The greater part of the strata with which the geologist has to deal are marine deposits , and it is only rarely that actual proof of the former existence of land in any district is found in the intercalation of ...
Page 17
... seem probable that the Lingula Flags should be entirely absent , for the lowest beds usually thin out before the ... seems to take place on a still larger and more surprising scale ; for the rocks of the Longmynd , which are supposed ...
... seem probable that the Lingula Flags should be entirely absent , for the lowest beds usually thin out before the ... seems to take place on a still larger and more surprising scale ; for the rocks of the Longmynd , which are supposed ...
Page 22
... seems to have been extraordinarily rugged and uneven , exhibiting a series of lofty mountain ridges separated by deep troughs and hollows , the bottoms of which were 10,000 or 12,000 feet below the summits of the ridges . How such ...
... seems to have been extraordinarily rugged and uneven , exhibiting a series of lofty mountain ridges separated by deep troughs and hollows , the bottoms of which were 10,000 or 12,000 feet below the summits of the ridges . How such ...
Page 24
... seems to suppose . The Russian succession is not antagonistic to this conclusion , for the whole Cambrian series is not 700 feet thick ; the basal sandstones are 300 feet , and the overlying beds are such as would be formed at a ...
... seems to suppose . The Russian succession is not antagonistic to this conclusion , for the whole Cambrian series is not 700 feet thick ; the basal sandstones are 300 feet , and the overlying beds are such as would be formed at a ...
Page 26
... seem still to have remained above the sea - level . entire absence of Upper Cambrian rocks , so far as is yet known , in northern Ireland and northern Scotland , seems to justify the supposition that these areas remained in the ...
... seem still to have remained above the sea - level . entire absence of Upper Cambrian rocks , so far as is yet known , in northern Ireland and northern Scotland , seems to justify the supposition that these areas remained in the ...
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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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