Horst and graben
From Wikipedia, the free encyclopedia
| This article does not cite any references or sources. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. (December 2009) |
In geology, horst and graben are terms referring to regions that lie between normal faults and are either above or lower than the area beyond the faults. A horst represents a block pushed upward by the faulting, and a graben is a block that has dropped due to the faulting.
[edit] See also
| This geology article is a stub. You can help Wikipedia by expanding it. |