The Evolution of Earth Structure with a Theory of Geomorphic Changes: By T. Mellard ReadeLongmans, Green, and Company, 1903 - 342 pàgines |
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Pàgina 33
... develop- ment of an immense earth - fold in the West Indian area . I cannot but express my dissent from this dictum . In the first place , where are the proofs that such an earth - fold exists and is undergoing further development ? The ...
... develop- ment of an immense earth - fold in the West Indian area . I cannot but express my dissent from this dictum . In the first place , where are the proofs that such an earth - fold exists and is undergoing further development ? The ...
Pàgina 34
... instead of the mixed mass of folds and igneous rocks we should expect were the develop- ment of folding the cause of volcanic activity . ference of material from one locality of the spheroid to 34 EVOLUTION OF EARTH STRUCTURE.
... instead of the mixed mass of folds and igneous rocks we should expect were the develop- ment of folding the cause of volcanic activity . ference of material from one locality of the spheroid to 34 EVOLUTION OF EARTH STRUCTURE.
Pàgina 54
... developed and underlain by more or less conformable Mesozoic groups of great thickness that the mountain masses occur . This is true even of the Apuan Alps , as shown in Stefani's excellent sections.1 These rock - groups appear to ...
... developed and underlain by more or less conformable Mesozoic groups of great thickness that the mountain masses occur . This is true even of the Apuan Alps , as shown in Stefani's excellent sections.1 These rock - groups appear to ...
Pàgina 64
... develop- ment . I am not one of those who think the doctrine of uniformity a ' fetish , ' but rather a theory that kept us within the range of practical fact . For my part , I am prepared to accept any- thing that can be proved , but ...
... develop- ment . I am not one of those who think the doctrine of uniformity a ' fetish , ' but rather a theory that kept us within the range of practical fact . For my part , I am prepared to accept any- thing that can be proved , but ...
Pàgina 66
... developed by faulting and mountain elevation in the locus of mountain ranges , by a persistence of the movements which have initiated them ; but the great levellers , the 1 Ramsay's ' River Courses of England and Wales , ' Q. J. G. S. ...
... developed by faulting and mountain elevation in the locus of mountain ranges , by a persistence of the movements which have initiated them ; but the great levellers , the 1 Ramsay's ' River Courses of England and Wales , ' Q. J. G. S. ...
Altres edicions - Mostra-ho tot
The Evolution of Earth Structure with a Theory of Geomorphic Changes: By T ... Thomas Mellard Reade Visualització completa - 1903 |
The Evolution of Earth Structure with a Theory of Geomorphic Changes: By T ... Thomas Mellard Reade Visualització completa - 1903 |
The Evolution of Earth Structure with a Theory of Geomorphic Changes: By T ... Thomas Mellard Reade Visualització completa - 1903 |
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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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