The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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Страница 26
... extent . Some rocks are harder than others , and tend to stand out after denudation has been in operation for some time . Some are soluble , others practically insoluble , and in this case the insoluble rock will tend to form eminences ...
... extent . Some rocks are harder than others , and tend to stand out after denudation has been in operation for some time . Some are soluble , others practically insoluble , and in this case the insoluble rock will tend to form eminences ...
Страница 32
... extent upon movements of the atmosphere , which are in turn due to differences of barometric pressure . The way in which these movements are set up will be referred to anon . But though winds produce marked effects upon the clouds ...
... extent upon movements of the atmosphere , which are in turn due to differences of barometric pressure . The way in which these movements are set up will be referred to anon . But though winds produce marked effects upon the clouds ...
Страница 73
... extent , and consequently the streams which course down the mountain - side do not rise absolutely beside the watershed , but some little distance below it on either side . We must now state a very important principle , to which we ...
... extent , and consequently the streams which course down the mountain - side do not rise absolutely beside the watershed , but some little distance below it on either side . We must now state a very important principle , to which we ...
Страница 77
... extent . As an illustration of the production of the arrange- ment of mountain , valley , and col described above , we may consider the district in the neighbourhood of Monte Rosa , which shows it fairly well , though there are several ...
... extent . As an illustration of the production of the arrange- ment of mountain , valley , and col described above , we may consider the district in the neighbourhood of Monte Rosa , which shows it fairly well , though there are several ...
Страница 78
... circumdenudation . Further , the height of neigh- bouring tracts of the uplifts will not vary to any great extent , and accordingly neighbouring moun- tains formed by the sculpture of an uplift by denuding 78 SCIENTIFIC STUDY OF SCENERY.
... circumdenudation . Further , the height of neigh- bouring tracts of the uplifts will not vary to any great extent , and accordingly neighbouring moun- tains formed by the sculpture of an uplift by denuding 78 SCIENTIFIC STUDY OF SCENERY.
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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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