In the piedmont zone the terrace and pediment surface jointly formed a geomorphic surface; they were contiguous in space with comparable elevation.
在山麓地带，阶地与麓原面联合成一级地貌面，二者在空间上连续、在高度上可比。
In the piedmont zone the terrace and pediment surface jointly formed a geomorphic surface; they were contiguous in space with comparable elevation.
在山麓地带，阶地与麓原面联合成一级地貌面，二者在空间上连续、在高度上可比。
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