The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 9
... rests in many places on Silurian or Devonian rocks , but it is probable that in most of these cases the older rocks had ... rest directly upon the old land surface are generally conglomerates or pebbly sandstones , the materials of which ...
... rests in many places on Silurian or Devonian rocks , but it is probable that in most of these cases the older rocks had ... rest directly upon the old land surface are generally conglomerates or pebbly sandstones , the materials of which ...
Page 10
... rest directly on the surface of the latter without the intervention of any conglomerate , and with only a thin ... rests on the older rocks with a mere basement bed , which is generally only a foot in thickness . When such cases occur we ...
... rest directly on the surface of the latter without the intervention of any conglomerate , and with only a thin ... rests on the older rocks with a mere basement bed , which is generally only a foot in thickness . When such cases occur we ...
Page 19
... rest on the Archæan . It is true there are some signs of faulting , and Dr. Hicks believes the Lower beds are faulted out , but more evidence of this is required . Dr. Callaway favours me with the following remarks on the lithological ...
... rest on the Archæan . It is true there are some signs of faulting , and Dr. Hicks believes the Lower beds are faulted out , but more evidence of this is required . Dr. Callaway favours me with the following remarks on the lithological ...
Page 20
... rest , and no definite fossils have yet been found in them . 1 The Galway rocks , regarded as Cambrian by Mr. Kinahan , are more probably of Archæan age . In Scotland we once more find rocks resting on un- 20 [ CHAP . II . PALEOZOIC TIME .
... rest , and no definite fossils have yet been found in them . 1 The Galway rocks , regarded as Cambrian by Mr. Kinahan , are more probably of Archæan age . In Scotland we once more find rocks resting on un- 20 [ CHAP . II . PALEOZOIC TIME .
Page 30
... rest on Cambrian shales . We may assume , therefore , that this district was dry land during the whole of Ordovician time , that the Longmynd and Caradoc tracts formed part of the land area in Arenig and Llandeilo times , but were ...
... rest on Cambrian shales . We may assume , therefore , that this district was dry land during the whole of Ordovician time , that the Longmynd and Caradoc tracts formed part of the land area in Arenig and Llandeilo times , but were ...
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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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