A graben is the result of a block of land being downthrown producing a valley with a distinct scarp on each side. Grabens often occur side-by-side with horsts. Horst and graben structures are indicative of tensional forces and crustal stretching. ''
Graben are produced from parallel normal faults, where the hanging wall is downthrown and the footwall is upthrown. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between grabens, the bounding faults of a horst typically dip away from the center line of the horst.
A single graben or multiple grabens can produce a rift valley.
Half-grabensIn many rifts the grabens are asymmetric, with a major fault along only one of the boundaries, and these are known as half-grabens. The polarity (throw direction) of the main bounding faults typically alternate along the length of the rift. The asymmetry of a half-graben strongly affects syntectonic deposition. Comparatively little sediment enters the half-graben across the main bounding fault, due to the effects of footwall uplift on the drainage systems. The exception is at any major offset in the bounding fault, where a relay ramp may provide an important sediment input point. Most of the sediment will enter the half-graben down the unfaulted hanging wall side (e.g. Lake Baikal, ).
- The Basin and Range region of southwestern North America is an example of multiple horst/graben structures, including Death Valley.
- The Rhine valley to the north of Basel, Switzerland
- The Oslo graben around Oslo, Norway
- The East African Rift Valley
- The Saguenay River Valley
- The Narmada River valley in central India
- The lower Godavari River valley in southern India
- The Ottawa-Bonnechere Graben in Ontario and Quebec, Canada
- Physical Geography: A Landscape Appreciation
Graben in German: Graben (Geologie)
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Graben in Dutch: Slenk (geologie)
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Graben in Polish: Rów tektoniczny
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Graben in Chinese: 地塹