The Evolution of Earth Structure with a Theory of Geomorphic Changes: By T. Mellard ReadeLongmans, Green, and Company, 1903 - 342 pàgines |
Des de l'interior del llibre
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Pàgina 42
... acting in unison that the continents owe their existence . Long - continued denudation of land areas pro- vides the material out of which mountain chains are built up . These sediments , it has been shown , are deposited mainly on areas ...
... acting in unison that the continents owe their existence . Long - continued denudation of land areas pro- vides the material out of which mountain chains are built up . These sediments , it has been shown , are deposited mainly on areas ...
Pàgina 77
... acting through a chain of events which I have dealt with in the ' Origin of Mountain Ranges , ' and which seem to me to be the explana- tion which brings together all the hitherto isolated facts of geology into one comprehensible whole ...
... acting through a chain of events which I have dealt with in the ' Origin of Mountain Ranges , ' and which seem to me to be the explana- tion which brings together all the hitherto isolated facts of geology into one comprehensible whole ...
Pàgina 164
... acting on the zinc bands . The layers of clay were free to move vertically . In correction I may add that the zinc bands were only used in model fig . 4 ; in 5 and 6 stepped blocks of wood were used , as is , indeed , described in the ...
... acting on the zinc bands . The layers of clay were free to move vertically . In correction I may add that the zinc bands were only used in model fig . 4 ; in 5 and 6 stepped blocks of wood were used , as is , indeed , described in the ...
Pàgina 170
... acting upon the base bed produced on it an uneven upper surface ( see fig . 3 , Plate XVIII . ) . The surfaces became more regularly curved in the successive layers forming the doine , which can be taken apart and examined separately ...
... acting upon the base bed produced on it an uneven upper surface ( see fig . 3 , Plate XVIII . ) . The surfaces became more regularly curved in the successive layers forming the doine , which can be taken apart and examined separately ...
Pàgina 170
... acting in the direction of the strike of the rocks forming the core . See Plate XVIII . and accompanying ex- planation . FIGS . 4 , 5 , and 6 are diagrams showing how the initial bias ' was obtained in Experiments Nos . 15 , 16 and 17 ...
... acting in the direction of the strike of the rocks forming the core . See Plate XVIII . and accompanying ex- planation . FIGS . 4 , 5 , and 6 are diagrams showing how the initial bias ' was obtained in Experiments Nos . 15 , 16 and 17 ...
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 |
Frases i termes més freqüents
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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