The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 3
... sandstones may have been formed as close to a shore as conglomerates ; nay , some sandstones have , doubtless , been formed above high water , and were originally sand - dunes , such as are common on our present coasts . Sandstones ...
... sandstones may have been formed as close to a shore as conglomerates ; nay , some sandstones have , doubtless , been formed above high water , and were originally sand - dunes , such as are common on our present coasts . Sandstones ...
Page 4
... sandstones consist of more or less angular grains , but beds of consolidated æolian sand exist in some formations . Pure quartzose sandstones of marine origin are always shallow - water deposits and are seldom found in deeper water than ...
... sandstones consist of more or less angular grains , but beds of consolidated æolian sand exist in some formations . Pure quartzose sandstones of marine origin are always shallow - water deposits and are seldom found in deeper water than ...
Page 5
... sandstones , would lead us to suspect the neighbourhood of a swampy shore or the estuary of a large river . Limestones , again , though more often formed in com- paratively deep water at a distance from land , are some- times ...
... sandstones , would lead us to suspect the neighbourhood of a swampy shore or the estuary of a large river . Limestones , again , though more often formed in com- paratively deep water at a distance from land , are some- times ...
Page 8
... sandstones alternate with each other , and as sandstones are more rapidly accumulated than clays , the formation may thicken landwards by the intercalation of sandstones ; so that if only this portion of a group of beds is preserved to ...
... sandstones alternate with each other , and as sandstones are more rapidly accumulated than clays , the formation may thicken landwards by the intercalation of sandstones ; so that if only this portion of a group of beds is preserved to ...
Page 9
... sandstones , the materials of which have been derived from the rocks of which that land was composed . Such conglomerates often cover very large surfaces , but it is well to remember that such beds are not the invariable accompaniments ...
... sandstones , the materials of which have been derived from the rocks of which that land was composed . Such conglomerates often cover very large surfaces , but it is well to remember that such beds are not the invariable accompaniments ...
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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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