风蚀是塑造地貌景观格局的基本过程之一，也是土地荒漠化的一个过程。
Wind-erosion is one of basic processes to mold the physiognomy landscape pattern and it is a process of desertification.
盆地四周被高山环绕，封闭得严严实实，气候极端干旱，干燥的风蚀和风积地貌发育十分典型。
Because of the mountain barriers, the weather there is extremely dry. It has a typical geomorphology of dry wind erosion and wind deposit.
当地的风成地貌主要是一些发育在垄岗的迎风波及洼地中的小型风蚀浅谷、风蚀残丘、沙丘、土豆等。
The local aeolian geomorphic unit is chiefly some small-scale deflation shallow valley deflation relic hillock, dune and soil hillock etc. that generate facing wind slope on ridge-mound and in hollow.
当地的风成地貌主要是一些发育在垄岗的迎风波及洼地中的小型风蚀浅谷、风蚀残丘、沙丘、土豆等。
The local aeolian geomorphic unit is chiefly some small-scale deflation shallow valley deflation relic hillock, dune and soil hillock etc. that generate facing wind slope on ridge-mound and in hollow.
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