The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 10
... base . Instances of such overlap with an absence of conglomerates are common in the case of the Carboniferous system ; where the Lower Carboniferous rocks lie unconformably on older strata , conglomerates and pebbly sandstones are ...
... base . Instances of such overlap with an absence of conglomerates are common in the case of the Carboniferous system ; where the Lower Carboniferous rocks lie unconformably on older strata , conglomerates and pebbly sandstones are ...
Page 16
... base of the system is exposed , the base- ment bed is found to be a conglomerate containing frag- ments of Archæan rocks , and resting unconformably on a very uneven surface of those rocks ; the conglomerate being probably in process of ...
... base of the system is exposed , the base- ment bed is found to be a conglomerate containing frag- ments of Archæan rocks , and resting unconformably on a very uneven surface of those rocks ; the conglomerate being probably in process of ...
Page 17
... base is not there seen , but when they reappear on the west 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 ...
... base is not there seen , but when they reappear on the west 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 ...
Page 20
... base is not seen , we do not know on what they 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 ...
... base is not seen , we do not know on what they 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 ...
Page 21
... base , and are in places from 3,000 to 4,000 feet thick . This Torridon Sandstone is probably of early Cambrian age , and has evidently been formed against an Archæan coast - line . Its composition is thus described by Professor Bonney ...
... base , and are in places from 3,000 to 4,000 feet thick . This Torridon Sandstone is probably of early Cambrian age , and has evidently been formed against an Archæan coast - line . Its composition is thus described by Professor Bonney ...
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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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