The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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Страница vii
... - Folded Mountains - Faulted Mountains . CHAPTER VII . MOUNTAINS ( continued ) . Formation of Watersheds - The Processes of Denudation 8-19 20-28 29-45 46-54 55-69 70-93 CHAPTER VIII . MOUNTAINS ( continued ) . Details of.
... - Folded Mountains - Faulted Mountains . CHAPTER VII . MOUNTAINS ( continued ) . Formation of Watersheds - The Processes of Denudation 8-19 20-28 29-45 46-54 55-69 70-93 CHAPTER VIII . MOUNTAINS ( continued ) . Details of.
Страница 52
... watershed is immediately above the axial line , and accordingly the primary drainage system of the continent will be divided along a line coinciding with that from which the strata dip on opposite sides in different directions . The ...
... watershed is immediately above the axial line , and accordingly the primary drainage system of the continent will be divided along a line coinciding with that from which the strata dip on opposite sides in different directions . The ...
Страница 53
... watershed to the sea - coasts.1 It will be eventually seen that these rivers cut into the strata and carve valleys ... watershed , but some may rise at various points between the watershed and the sea . For the sake of simplicity , these ...
... watershed to the sea - coasts.1 It will be eventually seen that these rivers cut into the strata and carve valleys ... watershed , but some may rise at various points between the watershed and the sea . For the sake of simplicity , these ...
Страница 54
... watershed . 2 , 2 = Secondary watersheds . 3 , 3 = Tertiary watersheds . lines will be affected by erosion ; but the principal minor modifications , unlike those of the land , are produced , not by denudation , but by deposition , which ...
... watershed . 2 , 2 = Secondary watersheds . 3 , 3 = Tertiary watersheds . lines will be affected by erosion ; but the principal minor modifications , unlike those of the land , are produced , not by denudation , but by deposition , which ...
Страница 70
... watershed would be precisely similar to that which we described in Chapter V. , as forming the main watershed of a continental uplift , and the drain- age would be initiated and secondary watersheds . developed as described in that ...
... watershed would be precisely similar to that which we described in Chapter V. , as forming the main watershed of a continental uplift , and the drain- age would be initiated and secondary watersheds . developed as described in that ...
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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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