The Building of the British Isles: A Study in Geographical EvolutionG. Bell, 1888 - 343 pages |
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Page 2
... tracts and the vanished lands of which they formed part have yielded the ma- terials that compose the more recent ( Neozoic ) strata , and there were at least three periods in these later times when Neozoic strata filled up the gaps ...
... tracts and the vanished lands of which they formed part have yielded the ma- terials that compose the more recent ( Neozoic ) strata , and there were at least three periods in these later times when Neozoic strata filled up the gaps ...
Page 3
... tracts during a given period can only be inferred from general considerations , such as the changes in the lithological characters of the sediments , the thinning or thickening of beds in certain directions , their entire absence in ...
... tracts during a given period can only be inferred from general considerations , such as the changes in the lithological characters of the sediments , the thinning or thickening of beds in certain directions , their entire absence in ...
Page 6
... tracts of the sea bottom , between the shallow water and the deeper tracts of the ocean . Variations in Thickness . - The evidence derivable from the thinning and thickening of deposits also merits some examination . If we consider the ...
... tracts of the sea bottom , between the shallow water and the deeper tracts of the ocean . Variations in Thickness . - The evidence derivable from the thinning and thickening of deposits also merits some examination . If we consider the ...
Page 8
... tract where shales and sandstones alternate with each other , and as sandstones are more rapidly accumulated than clays , the formation may thicken landwards by the intercalation of sandstones ; so that if only this portion of a group ...
... tract where shales and sandstones alternate with each other , and as sandstones are more rapidly accumulated than clays , the formation may thicken landwards by the intercalation of sandstones ; so that if only this portion of a group ...
Page 9
... tracts in the Carboniferous period . In cases of unconformity the rocks which rest directly upon the old land ... tract of land has sunk slowly beneath the sea for a long period of time , so that the newer deposits have overlapped ...
... tracts in the Carboniferous period . In cases of unconformity the rocks which rest directly upon the old land ... tract of land has sunk slowly beneath the sea for a long period of time , so that the newer deposits have overlapped ...
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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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