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The Davisian geographical cycle
The weathering of metamorphic rocks
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angle anticline areas barchan base level basins beach beds boulder boulder clay carbon caused Chalk channel chemical weathering clay cliff climate coast concave convexity corrie cycle debris denudation deposits deserts downcutting drainage drainage basins drumlins dunes effect eroded erosion surfaces escarpment example explanation see text flow formation freeze-thaw geomorphology glacial glacier graded gradient granite gravel hypothesis ice sheet increase inselbergs joints karst lake landforms landscape later layers limestone lithology load longshore drift lower marine material meanders moraines movement occur pattern peneplain periglacial period permeable Plate plateau Pleistocene possible Post-glacial present probably proglacial lakes rainfall reefs regions relief resistant result ridges river river capture rocks sand Sandstone scree sea level sediments shorelines slope soil solifluxion solution stage stream structure subaerial superimposed temperature terraces tropical upper usually valley vegetation velocity waste mantle waves wind zone