The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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Страница 48
... uplift on the arch , assuming that the crust had previously been exactly at sea - level , and we may briefly inquire if there is any evidence that continents and ocean basins are due to move- ments of this nature.1 It requires little ...
... uplift on the arch , assuming that the crust had previously been exactly at sea - level , and we may briefly inquire if there is any evidence that continents and ocean basins are due to move- ments of this nature.1 It requires little ...
Страница 50
... uplift of a set of stratified deposits originally laid down horizontally on the sea - floor , and if the uplift were unaccompanied by denudation , the surface of the continent would be completely covered by the upper- most stratum , and ...
... uplift of a set of stratified deposits originally laid down horizontally on the sea - floor , and if the uplift were unaccompanied by denudation , the surface of the continent would be completely covered by the upper- most stratum , and ...
Страница 51
... uplift raises these sediments to form land , and as that land is always subjected to denuding agents , these sediments will be partially swept from the land , and the edges of the strata will abut against the surface , just as if we ...
... uplift raises these sediments to form land , and as that land is always subjected to denuding agents , these sediments will be partially swept from the land , and the edges of the strata will abut against the surface , just as if we ...
Страница 52
... uplift as occurring around a horizontal straight line instead of above a point , in which case the result would be a long ridge , highest above this axial line , and sloping to the coasts , which in our imaginary continent would form ...
... uplift as occurring around a horizontal straight line instead of above a point , in which case the result would be a long ridge , highest above this axial line , and sloping to the coasts , which in our imaginary continent would form ...
Страница 53
... uplift , such as we have described , a river - system of the following character will be initiated ( Fig . 7 ) . An ideal continent then owes its existence and broader physical features to its main uplift ; its mountain masses and ...
... uplift , such as we have described , a river - system of the following character will be initiated ( Fig . 7 ) . An ideal continent then owes its existence and broader physical features to its main uplift ; its mountain masses and ...
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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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