The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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Страница 9
... many limestones and siliceous deposits ) , or they may consist of fragments broken from pre - existing rocks and carried by mechanical means to the position in which they are accumulated ( as sandstone and mud ) NATURE OF EARTH'S EXTERIOR ...
... many limestones and siliceous deposits ) , or they may consist of fragments broken from pre - existing rocks and carried by mechanical means to the position in which they are accumulated ( as sandstone and mud ) NATURE OF EARTH'S EXTERIOR ...
Страница 16
... carried on almost indefinitely . The joints are often very irregular , but we frequently find the more important ones running with a considerable degree of regularity . The columnar jointing of basalt and other rocks is somewhat rare ...
... carried on almost indefinitely . The joints are often very irregular , but we frequently find the more important ones running with a considerable degree of regularity . The columnar jointing of basalt and other rocks is somewhat rare ...
Страница 17
... carried up or down relatively to those on the other side of the plane of fracture , giving rise to what is known as a fault , as illustrated in section in Fig . 2 , where the portion of the stratum c on the right of the section , which ...
... carried up or down relatively to those on the other side of the plane of fracture , giving rise to what is known as a fault , as illustrated in section in Fig . 2 , where the portion of the stratum c on the right of the section , which ...
Страница 24
... carried from a higher to a 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 ...
... carried from a higher to a 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 ...
Страница 25
... carried from a higher to a lower level , where they are spread out to form fresh deposits . The agents , I say , are in some ways different , and here the effects of climate are noticed . Nature works in the wet way and in the dry way ...
... carried from a higher to a lower level , where they are spread out to form fresh deposits . The agents , I say , are in some ways different , and here the effects of climate are noticed . Nature works in the wet way and in the dry way ...
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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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