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单词 Scarp slope
释义

Scarp slope

中文百科

单面山 Escarpment

(重定向自Scarp slope)
合欢山主峰呈东缓西陡,是**标准的单面山地形[1]。

单面山英语:cuesta),又称半屏山,是用于形容地形,指一边陡峭而另一边缓斜的山。其通常形成的原因,原本倾斜排列的岩层,其上层岩石较硬,下层岩石较软,为地质上差异,受到长时间风化作用或雨水冲刷、溪水的向源侵蚀之下,致使岩层脆弱会受到较多的侵蚀,形成两边侵蚀速度不一的差异地景,此地景即为「单面山」!

英语百科

Escarpment 单面山

(重定向自Scarp slope)
Escarpment face of a cuesta, broken by a fault, Cumberland Plateau, Tennessee
Shaded and colored image from the Shuttle Radar Topography Mission—shows an elevation model of New Zealand's Alpine Fault running about 500 km (300 mi) long. The escarpment is flanked by a chain of hills squeezed between the fault and the mountains of New Zealand's Southern Alps. Northeast is towards the top.
The Sierra Escarpment in California.
At the Florida Escarpment, seen in the eastern Gulf of Mexico, the sea bed drops precipitously from less than 300m to 3000m over a short distance.

An escarpment is a steep slope or long cliff that occurs from faulting, tilting or warping and resulting erosion and separates two relatively level areas of differing elevations. Usually escarpment is used interchangeably with scarp (from the Italian scarpa, shoe). But some sources differentiate the two terms, where escarpment refers to the margin between two landforms, while scarp is synonymous with a cliff or steep slope. The surface of the steep slope is called a scarp face.

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更新时间:2025/6/16 22:35:11