The Evolution of Earth Structure with a Theory of Geomorphic Changes: By T. Mellard ReadeLongmans, Green, and Company, 1903 - 342 páginas |
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Página 1
... feet above the sea - level . As the science of geology advanced these marine exuviæ , it was found , had been in one class of cases lifted into their positions by the folding of the rocks in which they were entombed and き B their ...
... feet above the sea - level . As the science of geology advanced these marine exuviæ , it was found , had been in one class of cases lifted into their positions by the folding of the rocks in which they were entombed and き B their ...
Página 2
... feet in Western Thibet , had attained such extreme elevation through the rocks in which they were enclosed having been involved in the mountain - building . Raised Beaches . - Later investigations have , however , shown that numerous ...
... feet in Western Thibet , had attained such extreme elevation through the rocks in which they were enclosed having been involved in the mountain - building . Raised Beaches . - Later investigations have , however , shown that numerous ...
Página 3
... feet . There appears to have been a neutral axis to this uplift , stretching across the Irish sea south of the Isle of Man , the north of this axis being an uplift increasing in vertical amplitude to the north , the south a depression ...
... feet . There appears to have been a neutral axis to this uplift , stretching across the Irish sea south of the Isle of Man , the north of this axis being an uplift increasing in vertical amplitude to the north , the south a depression ...
Página 4
... feet above the sea , is 738 feet in its greatest depth , or 491 feet below sea - level ; and there are other evidences of changes of level and differential land movements . On the continent of North America , it would appear from the ...
... feet above the sea , is 738 feet in its greatest depth , or 491 feet below sea - level ; and there are other evidences of changes of level and differential land movements . On the continent of North America , it would appear from the ...
Página 5
... feet . The Chaix Hills , though composed of soft , easily eroded strata , stand out in sharp ridges surmounted with irregular pyramids , indicative of immature sculpture ; this indication of youth is also sustained by the fossils with ...
... feet . The Chaix Hills , though composed of soft , easily eroded strata , stand out in sharp ridges surmounted with irregular pyramids , indicative of immature sculpture ; this indication of youth is also sustained by the fossils with ...
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Amazons America anticlinal Atlantic Azores B.Sc basin beds bottom Carboniferous changes CHEMISTRY chlorite clay cleavage Clonakilty coast College compression continental continents County Cork Cretaceous Crown 8vo D.Sc deep deposits depression depth Diagrams differential dome earth's crust ELEMENTARY elevation Engineer evidence exist expansion Experiment fact fathoms feet fissile fold geological geologists Gulf of Mexico heated Illustrations inches islands Israel Russell land areas layers lithosphere mass material matter mica mineral Mississippi Mountain Ranges movements nature North numerous ocean Origin of Mountain photograph Phyllades physical plane Plate Pleistocene portion Professor published by Longmans quarry raised beaches result ridges river rocks Royal 8vo sand sandstones Science Scientific Works published sediment sedimentary shearing sheet shown sink slate slaty-cleavage solid soundings South specific gravity square miles strata strata-plate structure submarine submerged subsidence surface take place temperature terraces Tertiary theory thickness tion valleys vertical volcanic
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