嶂谷

岩浆活动在太行山地区对峰林、嶂谷地貌形成过程的控制作用

Control effect of magmatic activity to formation procedures of peak-forest and narrow gorge landform in Taihang Mountain

百里峡构造-冲蚀嶂谷是喀斯特地貌中一种特殊的类型。

The One-Hundred-li structural erosion gorge is a special karst geomorphologic feature .

更新世阶段地壳迅速的抬升、外力的物理风化作用，特别是晚更新世间歇性山区洪水的冲蚀，是形成嶂谷的直接原因。

The rapid crustal uplift in the Pleistocene and physical weathering and erosion , especially the erosional process of the flood in the mountains , are the direct causes for the formation of the gorges .