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Trough (geology)
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Trough (geology) : ウィキペディア英語版
Trough (geology)

In geology, a trough generally refers to a linear structural depression that extends laterally over a distance, while being less steep than a trench.
A trough can be a narrow basin or a geologic rift, often formed at the rim of a tectonic plate.
There are various oceanic troughs, troughs found under oceans; examples include
* the Cayman Trough
* the Nankai Trough
* the Rockall Trough and others along the rift of the mid-oceanic ridge,
* the Timor Trough.
==See also==

*Walker Lane

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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