《环境地质学》（双语版） 第三讲 地球表层的塑造过程

环境地质学 Environmental geology 主讲人:万新南教授 Prof wan xinnan 环境地质学 Environmental Geology

环境地质学 Environmental Geology 主讲人：万新南教授 Prof. Wan xinnan 环境地质学Environmental Geology

Part three地难豪层的量 6、Pre降水、江河与洪水 7、 Mass wasting Processes表层整体再塑 (滑坡、泥石流、溶蚀、塌陷 8、海岸线与海岸塑造过程 9、生态与植被 环境地质学 Environmental Geology

Part three 地球表层的塑造过程 环境地质学Environmental Geology 6、Pre降水、江河与洪水 7、Mass Wasting Processes 表层整体再塑 （滑坡、泥石流、溶蚀、塌陷） 8、海岸线与海岸塑造过程 9、生态与植被

Part three地难豪层的量 7、 Mass Wasting Pr。 cesses 表层整体再塑 (滑坡、泥石流、溶蚀、塌陷) 环境地质学 Environmental Geology

Part three 地球表层的塑造过程 环境地质学Environmental Geology 7、Mass Wasting Processes 表层整体再塑 （滑坡、泥石流、溶蚀、塌陷）

Part three地难豪层的量 Mass Wasting processes There is nothing inorganic. The earth is not a mere fragment of dead history, stratum upon stratum like the leaves of a book, to be studied by geologists and antiquaries古玩家 chiefly, but living poetry like the leaves of a tree, which precedes flowers and fruit-not a fossil earth, but a living earth aa Henry David Thoreau 环境地质学 Environmental Geology

Part three 地球表层的塑造过程 环境地质学Environmental Geology Mass Wasting Processes There is nothing inorganic.... The earth is not a mere fragment of dead history, stratum upon stratum like the leaves of a book, to be studied by geologists and antiquaries古玩家 chiefly, but living poetry like the leaves of a tree, which precedes flowers and fruit-not a fossil earth, but a living earth.... Henry David Thoreau

Part three地难豪层的量 Mass Wasting processes A Flowing sand, landslides, and rock falls are examples of mass wasting, the general term for gravitationally induced downslope movement of debris. B Mass-wasting processes operate on sloping lands; eventually the debris reaches a stream or gully where fluvial processes continue the erosional process 环境地质学 Environmental Geology

Part three 地球表层的塑造过程 环境地质学Environmental Geology Mass Wasting Processes A、Flowing sand, landslides, and rock falls are examples of mass wasting, the general term for gravitationally induced downslope movement of debris. B、Mass-wasting processes operate on sloping lands; eventually the debris reaches a stream or gully where fluvial processes continue the erosional process