The Scientific Study of SceneryMethuen & Company, 1900 - 368 страница |
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Страница viii
... Outlines and Structures of Vol- canoes - Fissure Eruptions — Geysers - Mud Volcanoes— Earthquakes CHAPTER XIV PLAINS AND PLATEAUX . Formation and Characters of Plains - Formation and Charac- ters of Plateaux · CHAPTER XV . DESERTS ...
... Outlines and Structures of Vol- canoes - Fissure Eruptions — Geysers - Mud Volcanoes— Earthquakes CHAPTER XIV PLAINS AND PLATEAUX . Formation and Characters of Plains - Formation and Charac- ters of Plateaux · CHAPTER XV . DESERTS ...
Страница 38
... outlines , which , while rendering the sky a subject for profound contempla- tion and reverence by the lover of scenery , causes the student of cloud - classification to experience a feeling of bewilderment when he is confronted with ...
... outlines , which , while rendering the sky a subject for profound contempla- tion and reverence by the lover of scenery , causes the student of cloud - classification to experience a feeling of bewilderment when he is confronted with ...
Страница 56
... outline of the individual hills owes practically nothing to uplift , but nearly everything to erosion . Our study of hill structure will be simplified if we consider the effects of uplift first , and those of erosion subsequently ...
... outline of the individual hills owes practically nothing to uplift , but nearly everything to erosion . Our study of hill structure will be simplified if we consider the effects of uplift first , and those of erosion subsequently ...
Страница 57
... outline would be recognisable as identical with that which it at present exhibits ; indeed , long before the appearance of man in Britain , the physical features of our country were essentially those of the present time . It is evident ...
... outline would be recognisable as identical with that which it at present exhibits ; indeed , long before the appearance of man in Britain , the physical features of our country were essentially those of the present time . It is evident ...
Страница 59
... outline would be a circle . The strata would be arched above it , the planes of stratification lying parallel to the convex curve of the surface of the ground and also to the upper surface of the igneous mass . To an igneous mass ...
... outline would be a circle . The strata would be arched above it , the planes of stratification lying parallel to the convex curve of the surface of the ground and also to the upper surface of the igneous mass . To an igneous mass ...
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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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