The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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Страница 13
... lower now lies above the original upper one . It is known that this is the result of movements of the earth's crust occurring subsequently to the deposition of the strata , which have produced a series of folds . A few words must be ...
... lower now lies above the original upper one . It is known that this is the result of movements of the earth's crust occurring subsequently to the deposition of the strata , which have produced a series of folds . A few words must be ...
Страница 18
... lower is termed the downthrow side , the opposite being the upthrow side . These terms are used for convenience , without assuming that one side has been actually pushed downwards and the other upwards . planes are frequently parallel ...
... lower is termed the downthrow side , the opposite being the upthrow side . These terms are used for convenience , without assuming that one side has been actually pushed downwards and the other upwards . planes are frequently parallel ...
Страница 21
... lower one into waves , which are often defined by the condensed aqueous vapour in the lower layer ; air moving over water similarly throws the water into waves ; and , lastly , differential movement of different layers of the earth's ...
... lower one into waves , which are often defined by the condensed aqueous vapour in the lower layer ; air moving over water similarly throws the water into waves ; and , lastly , differential movement of different layers of the earth's ...
Страница 24
... lower level , and ultimately to the sea , if not checked . Thus the land is the great theatre of destruction by denuding agencies , and the ocean the great re- ceptacle of the sediment produced by these agencies . 1 TYNDALL ...
... lower level , and ultimately to the sea , if not checked . Thus the land is the great theatre of destruction by denuding agencies , and the ocean the great re- ceptacle of the sediment produced by these agencies . 1 TYNDALL ...
Страница 25
... lower reaches of the river during a heavy flood , we shall find the swollen waters turbid with the sediment produced by the breakage of the rocks above , and following the river still further to its junction with the ocean , may notice ...
... lower reaches of the river during a heavy flood , we shall find the swollen waters turbid with the sediment produced by the breakage of the rocks above , and following the river still further to its junction with the ocean , may notice ...
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Чести термини и фразе
accordingly accumulation action agents angles barrier basins cause character cliffs clouds coast colour considerable corrasion crater crevasses Crown 8vo crust curve delta Demy 8vo denudation deposits desert regions drainage E. V. LUCAS earth's surface effect erosion escarpment existence extent Fcap feet fissure flow folding formation formed fragments frequently Geological give rise glacial glacier gorge Greenland ground hard rock height Henry Mountains hills hollows horizontal igneous rocks Illustrations islands Lake District land lava limestone lithosphere lower marked mass material monoclinal moraines mountain movement nature névé occupied occur ocean original outline owing particles peneplain plain planes of stratification plateau portion produced result ridge river rocks sand scenery screes Second Edition sediment seen side slope snow soft rocks Spitsbergen strata subaerial subsequent streams Tarn tion tract tributary Ullswater uplift upper valley vapour vegetation vertical volcanic watershed waves weathering wind
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