The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 11
... side of an anticlinal , but when the final limit of a formation toward a given direction is a fault or an abrupt boundary , without even an outlier beyond , we are left in complete uncertainty as to the original limits of those beds in ...
... side of an anticlinal , but when the final limit of a formation toward a given direction is a fault or an abrupt boundary , without even an outlier beyond , we are left in complete uncertainty as to the original limits of those beds in ...
Page 17
... side of the Snowdon range , they are much thinner , and are probably not more than 3,000 feet thick , including the basal conglomerate of Llyn Padarn , which lies on the eastern flank of the main Archæan ridge . On the west side of this ...
... side of the Snowdon range , they are much thinner , and are probably not more than 3,000 feet thick , including the basal conglomerate of Llyn Padarn , which lies on the eastern flank of the main Archæan ridge . On the west side of this ...
Page 18
... side by a quartzite conglomerate , which is succeeded by sandstones of Middle or Upper Lingula Flag age ; the Lower Cambrian being entirely absent . How can this sudden disappearance of so thick a mass of rock be accounted for ? There ...
... side by a quartzite conglomerate , which is succeeded by sandstones of Middle or Upper Lingula Flag age ; the Lower Cambrian being entirely absent . How can this sudden disappearance of so thick a mass of rock be accounted for ? There ...
Page 19
... side of the eastern massif no Harlech Beds or Menevian are found , and the Upper Lingula Flags with a basal conglomerate appear to rest on the Archæan . It is true there are some signs of faulting , and Dr. Hicks believes the Lower beds ...
... side of the eastern massif no Harlech Beds or Menevian are found , and the Upper Lingula Flags with a basal conglomerate appear to rest on the Archæan . It is true there are some signs of faulting , and Dr. Hicks believes the Lower beds ...
Page 26
... side of this vanished country . " Beyond this there may have been another sea or gulf if the rocks in the east of Ireland are rightly referred to the Cambrian ; but it is a significant fact that no deposits of Cambrian age have been ...
... side of this vanished country . " Beyond this there may have been another sea or gulf if the rocks in the east of Ireland are rightly referred to the Cambrian ; but it is a significant fact that no deposits of Cambrian age have been ...
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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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