The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 3
... stones which could only be moved by the beating of waves on a shore are , of course , decided evidence of the close neighbourhood of land to the spot where we now find them , and if they contain large angular or sub - angular boulders ...
... stones which could only be moved by the beating of waves on a shore are , of course , decided evidence of the close neighbourhood of land to the spot where we now find them , and if they contain large angular or sub - angular boulders ...
Page 17
... stones and mudstones , which have been referred to the Harlech series , but it is quite possible that they are shore beds of Lingula Flag age . As they are directly succeeded by Arenig slates ( Ordovician ) , it does not seem probable ...
... stones and mudstones , which have been referred to the Harlech series , but it is quite possible that they are shore beds of Lingula Flag age . As they are directly succeeded by Arenig slates ( Ordovician ) , it does not seem probable ...
Page 21
... stones derived from older sedimentary rocks , such as greywacke , quartzite , hardened shales , and cherty limestones , together with a few pebbles of slaggy diabase lava . Professor Judd remarks 2 : " These rocks in their cha- 1 Pres ...
... stones derived from older sedimentary rocks , such as greywacke , quartzite , hardened shales , and cherty limestones , together with a few pebbles of slaggy diabase lava . Professor Judd remarks 2 : " These rocks in their cha- 1 Pres ...
Page 41
... stone between the Wenlock and the representative of the Aymestry , which might be regarded as a distinct horizon . This ... stones of the Wenlock series . As regards the eastward extension of the Silurian rocks very little is yet known ...
... stone between the Wenlock and the representative of the Aymestry , which might be regarded as a distinct horizon . This ... stones of the Wenlock series . As regards the eastward extension of the Silurian rocks very little is yet known ...
Page 42
... stone resting on a few inches of grey shale , while to the north and north - west it thickens into a great series of shales and sandstones , which are spread over large areas in the Southern Uplands of Scotland . In the Moffat district ...
... stone resting on a few inches of grey shale , while to the north and north - west it thickens into a great series of shales and sandstones , which are spread over large areas in the Southern Uplands of Scotland . In the Moffat district ...
Other editions - View all
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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