Rain and Rivers, Or, Hutton and Playfair Against Lyell and All Comers |
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Page 4
... lower part of the valley becomes horizontal . The passage of the detritus of the upper parts is then checked in this horizontal part , and soil ac- cumulates there backward up the valley . This is the origin of alluvial plains , which I ...
... lower part of the valley becomes horizontal . The passage of the detritus of the upper parts is then checked in this horizontal part , and soil ac- cumulates there backward up the valley . This is the origin of alluvial plains , which I ...
Page 14
... lower terraces by the river side are actually delineated . But I was thoroughly astonished at the multiplicity of terraces with which the hill- sides are scored . From Sir T. Dick Lauder's draw- ing , and Mr. Jamieson's map given in ...
... lower terraces by the river side are actually delineated . But I was thoroughly astonished at the multiplicity of terraces with which the hill- sides are scored . From Sir T. Dick Lauder's draw- ing , and Mr. Jamieson's map given in ...
Page 22
... lower parts of these valleys , speaking longitudinally , and the higher parts , speaking laterally , being gradually and in succession carlier exposed to these wasting causes , supposing equal hardness of material , disappear earlier ...
... lower parts of these valleys , speaking longitudinally , and the higher parts , speaking laterally , being gradually and in succession carlier exposed to these wasting causes , supposing equal hardness of material , disappear earlier ...
Page 23
... lower end . A valley is , in my opinion , a water - slope or a system of water - slopes , converging to one outlet at the sea . In the case of cups or crevices without outlets , elevation of the land , rain instantly begins to formed in ...
... lower end . A valley is , in my opinion , a water - slope or a system of water - slopes , converging to one outlet at the sea . In the case of cups or crevices without outlets , elevation of the land , rain instantly begins to formed in ...
Page 34
... lower greensand , No. 3 , over the Weald clay ; those of the dark- blue gault , No. 2 , over the lower greensand ; and those of the light coloured chalk and upper greensand , No. 1 , over the gault . Lyell thinks that the pink tertiary ...
... lower greensand , No. 3 , over the Weald clay ; those of the dark- blue gault , No. 2 , over the lower greensand ; and those of the light coloured chalk and upper greensand , No. 1 , over the gault . Lyell thinks that the pink tertiary ...
Other editions - View all
Rain and Rivers: Or, Hutton and Playfair Against Lyell and All Comers [An ... George Greenwood No preview available - 2016 |
Rain and Rivers, Or, Hutton and Playfair Against Lyell and All Comers George Greenwood No preview available - 2020 |
Common terms and phrases
accumulation alluvial plain alluvium ancient backward banks barrier basin beach boulders causes chalk channels Chesil beach clay cliff continents Crown 8vo delta denudation deposit depth descend disintegration drift and alluvium dry land earth earthquakes Elephant bed Ellet embanked eternal existence feet filled fissure flints flood-water floods flow formation of valleys formed fossil geological Giens glacier Glen Roy globe gradient granite groin height hollows Humboldt igneous island Keith Johnston lakes land animals longitudinal lower Lyell says miles Mississippi mountains natural original pebbles ponding Post 8vo pyramids rain and rivers raised ravines regions ridge and furrow rise rock Romney Romney Marsh Rother running water sand sea shore Second Edition shingle side Silurian slope snow soil South Downs species strata stream subaerial submarine theory subterranean supposed surface terraces tertiary strata tion torrents vegetation volcanic vols wash of rain waterslope wave Weald clay Weald valley whole Woodcuts
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