The Building of the British Isles: A Study in Geographical Evolution |
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Page 5
... suppose that it was formed at no great distance from land , it may be assumed that no large rivers issued from the coast in question . Every case in which limestones occur must be dealt with on its own merits , and no hasty conclusion ...
... suppose that it was formed at no great distance from land , it may be assumed that no large rivers issued from the coast in question . Every case in which limestones occur must be dealt with on its own merits , and no hasty conclusion ...
Page 9
... suppose that the area in question was land throughout the whole of that particular period . If , however , the gap is very great , and several systems of rocks are missing , we must not conclude that the area has been continually above ...
... suppose that the area in question was land throughout the whole of that particular period . If , however , the gap is very great , and several systems of rocks are missing , we must not conclude that the area has been continually above ...
Page 18
... suppose that an upheaval took place in the middle of the Cambrian period , but that the land so formed was soon submerged again beneath the sea of the Lingula Flags . In South Wales there are indications of a similarly rapid 18 [ CHAP ...
... suppose that an upheaval took place in the middle of the Cambrian period , but that the land so formed was soon submerged again beneath the sea of the Lingula Flags . In South Wales there are indications of a similarly rapid 18 [ CHAP ...
Page 24
... 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 distance from ...
... 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 distance from ...
Page 28
... the Silurians against the pre - Cambrian rocks , and that there is reason to suppose that they were never deposited over that part of Caradoc Hill . Fig . 1. Diagrammatic Section through parts 28 [ CHAP . III . PALEOZOIC TIME .
... the Silurians against the pre - Cambrian rocks , and that there is reason to suppose that they were never deposited over that part of Caradoc Hill . Fig . 1. Diagrammatic Section through parts 28 [ CHAP . III . PALEOZOIC TIME .
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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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