The Building of the British Isles: A Study in Geographical Evolution |
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Page 6
... marls have generally been formed in water of considerable depth . Many bluish and greenish clays , shales and slates , especially such as do not contain many fossils , have doubt- less been formed in deep water , and are comparable to ...
... marls have generally been formed in water of considerable depth . Many bluish and greenish clays , shales and slates , especially such as do not contain many fossils , have doubt- less been formed in deep water , and are comparable to ...
Page 41
... marls , some of which contain marine fossils ; these beds form a passage from Silurian to Old Red Sandstone , and were evidently formed in shallower water than the dark mudstones and lime- stones of the Wenlock series . As regards the ...
... marls , some of which contain marine fossils ; these beds form a passage from Silurian to Old Red Sandstone , and were evidently formed in shallower water than the dark mudstones and lime- stones of the Wenlock series . As regards the ...
Page 50
... marls , the sandstones generally red , the marls red , grey , or green , and including lenticular masses or nodules of limestone , which are locally known as " cornstones ; " hence the whole series is sometimes called the " Cornstone ...
... marls , the sandstones generally red , the marls red , grey , or green , and including lenticular masses or nodules of limestone , which are locally known as " cornstones ; " hence the whole series is sometimes called the " Cornstone ...
Page 56
... marls and shales . These are sometimes called Middle Old Red Sand- stone , and it is possible that they represent some of the marine Devonian beds ; they are probably from 3,000 to 4,000 feet thick , and are certainly older and distinct ...
... marls and shales . These are sometimes called Middle Old Red Sand- stone , and it is possible that they represent some of the marine Devonian beds ; they are probably from 3,000 to 4,000 feet thick , and are certainly older and distinct ...
Page 57
... marls , above which are red and yellow sandstones with fish and plant remains . It has been supposed that these strata are of lacustrine origin , but no freshwater mollusca have yet been found in them , while Serpula and the Pteropod ...
... marls , above which are red and yellow sandstones with fish and plant remains . It has been supposed that these strata are of lacustrine origin , but no freshwater mollusca have yet been found in them , while Serpula and the Pteropod ...
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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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