The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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... actual magnitude . " 2 1 ... As the four attributes size , colour , movement , and character of surface , or , as we may term the last , texture , will not be treated systematically , it will be convenient at this point to make a few ...
... actual magnitude . " 2 1 ... As the four attributes size , colour , movement , and character of surface , or , as we may term the last , texture , will not be treated systematically , it will be convenient at this point to make a few ...
Страница 12
... actual planes of discon- tinuity along which rocks may be split . It is obvious that these planes are , strictly speaking , absent from igneous rock , but similar planes may separate lava flows from sediments which overlie or underlie ...
... actual planes of discon- tinuity along which rocks may be split . It is obvious that these planes are , strictly speaking , absent from igneous rock , but similar planes may separate lava flows from sediments which overlie or underlie ...
Страница 18
... actual plane of discontinuity , comparable with a joint - plane , and indeed it is a joint - plane , along which differential movement of the rocks has occurred . Accordingly we often find one set of important faults which have a trend ...
... actual plane of discontinuity , comparable with a joint - plane , and indeed it is a joint - plane , along which differential movement of the rocks has occurred . Accordingly we often find one set of important faults which have a trend ...
Страница 51
... actual structure of our main land surfaces for the present , and to consider the events which would occur , and modify the land masses , if we commenced - with a simple uplift of horizontal sediments . An ideal symmetrical uplift around ...
... actual structure of our main land surfaces for the present , and to consider the events which would occur , and modify the land masses , if we commenced - with a simple uplift of horizontal sediments . An ideal symmetrical uplift around ...
Страница 61
... actual symmetry varies . In some cases the septum is steeper than the other slopes , but is not vertical ; in other cases it is vertical , and a FIG . 8 . b sometimes becomes turned over , when the strata of the septum are reversed , as ...
... actual symmetry varies . In some cases the septum is steeper than the other slopes , but is not vertical ; in other cases it is vertical , and a FIG . 8 . b sometimes becomes turned over , when the strata of the septum are reversed , as ...
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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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