The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page vi
... eastern and midland counties . Many geologists have dealt in more or less detail with the geographical conditions of particular epochs , but the first systematic treatise on the geography of successive geo- logical periods was that by ...
... eastern and midland counties . Many geologists have dealt in more or less detail with the geographical conditions of particular epochs , but the first systematic treatise on the geography of successive geo- logical periods was that by ...
Page 11
... eastern part of England . The imperfection of the geological record is another great source of difficulty , and one which will never be alto- gether overcome . The rocks which remain to us as the records of any one period are but a ...
... eastern part of England . The imperfection of the geological record is another great source of difficulty , and one which will never be alto- gether overcome . The rocks which remain to us as the records of any one period are but a ...
Page 16
... Eastern counties . The stratigraphy of the Cambrian rocks is not yet com- pletely understood ; there are many unsolved difficulties connected with them , and any account of them must at present be regarded as provisional . İn Wales the ...
... Eastern counties . The stratigraphy of the Cambrian rocks is not yet com- pletely understood ; there are many unsolved difficulties connected with them , and any account of them must at present be regarded as provisional . İn Wales the ...
Page 17
... eastern flank of the main Archæan ridge . On the west side of this ridge the basal conglomerate is overlain by grits and slates , and , near Bangor , by sand- stones and mudstones , which have been referred to the Harlech series , but ...
... eastern flank of the main Archæan ridge . On the west side of this ridge the basal conglomerate is overlain by grits and slates , and , near Bangor , by sand- stones and mudstones , which have been referred to the Harlech series , but ...
Page 18
... eastern or Caradoc Archæan ridge is flanked on the other 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 ...
... eastern or Caradoc Archæan ridge is flanked on the other 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 ...
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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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