The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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... frequently regarded from a purely philosophical or a merely economic standpoint , and their æsthetic side is ignored , though this is very valuable as a means of education . B The scientific study of scenery is concerned with all the ...
... frequently regarded from a purely philosophical or a merely economic standpoint , and their æsthetic side is ignored , though this is very valuable as a means of education . B The scientific study of scenery is concerned with all the ...
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... frequently supplied to them as an introduction to the science , details which naturally cause them to turn away from the pursuit of the study with a feeling of aversion . In viewing any scene , the attributes which strike us specially ...
... frequently supplied to them as an introduction to the science , details which naturally cause them to turn away from the pursuit of the study with a feeling of aversion . In viewing any scene , the attributes which strike us specially ...
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... frequently possesses colour of its own , owing to the presence of organic matter , or of some compound of iron . The former usually 1 WORDSWORTH , loc . cit . , sec . i . 2 RUSKIN , Modern Painters , vol . v . , part vi . , chap . x ...
... frequently possesses colour of its own , owing to the presence of organic matter , or of some compound of iron . The former usually 1 WORDSWORTH , loc . cit . , sec . i . 2 RUSKIN , Modern Painters , vol . v . , part vi . , chap . x ...
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... frequently spoken of as stratified rocks . Igneous and stratified rocks alike may undergo considerable changes after their formation , and these changes are spoken of as metamorphic , and we meet , therefore , with metamorphic igneous ...
... frequently spoken of as stratified rocks . Igneous and stratified rocks alike may undergo considerable changes after their formation , and these changes are spoken of as metamorphic , and we meet , therefore , with metamorphic igneous ...
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... overlie or underlie them , and we may conveniently include such planes in this division . It was stated above that planes of stratification are usually formed as horizontal planes , but they are frequently 12 SCIENTIFIC STUDY OF SCENERY.
... overlie or underlie them , and we may conveniently include such planes in this division . It was stated above that planes of stratification are usually formed as horizontal planes , but they are frequently 12 SCIENTIFIC STUDY OF SCENERY.
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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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