The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 26
... northern Ireland and northern Scotland , seems to justify the supposition that these areas remained in the condition of land throughout the Cambrian period . The Torridon sandstone may have been formed in a narrow gulf penetrating into ...
... northern Ireland and northern Scotland , seems to justify the supposition that these areas remained in the condition of land throughout the Cambrian period . The Torridon sandstone may have been formed in a narrow gulf penetrating into ...
Page 30
... northern and central parts of the island were still above water . " The basement conglomerates contain not only boulders from the granitoidite , but also pieces of halleflinta , such as we find east of Llanfaelog , and numerous ...
... northern and central parts of the island were still above water . " The basement conglomerates contain not only boulders from the granitoidite , but also pieces of halleflinta , such as we find east of Llanfaelog , and numerous ...
Page 32
... northern England is known from the existence of Ordovician rocks in Teesdale and near Ingleborough . Scotland . In the south of Scotland Ordovician rocks are known to occupy large areas , and they have been mapped by the Geological ...
... northern England is known from the existence of Ordovician rocks in Teesdale and near Ingleborough . Scotland . In the south of Scotland Ordovician rocks are known to occupy large areas , and they have been mapped by the Geological ...
Page 33
... northern part of Scotland , it is only quite recently that its structure has been properly under- stood . Messrs . Lapworth and Callaway were the first to establish the true upward succession , and to show that it was in many places ...
... northern part of Scotland , it is only quite recently that its structure has been properly under- stood . Messrs . Lapworth and Callaway were the first to establish the true upward succession , and to show that it was in many places ...
Page 37
... northern limit . West of this island there seems to have been another formed by the unsubmerged portion of the ridge spoken of in the last chapter as reaching across from Anglesey to the south - east of Ireland , but how much farther to ...
... northern limit . West of this island there seems to have been another formed by the unsubmerged portion of the ridge spoken of in the last chapter as reaching across from Anglesey to the south - east of Ireland , but how much farther to ...
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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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