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Rift 

USGS image
USGS image
Plates in the crust of the earth, according to the plate tectonics theory
Plates in the crust of the earth, according to the plate tectonics theory

In geology, a rift is a place where the Earth's crust and lithosphere are being pulled apart[1] and is an example of extensional tectonics.[2]

Typical rift features are a central linear downdropped fault segment, called a graben, with parallel normal faulting and rift-flank uplifts on either side forming a rift valley, where the rift remains above sea level. The axis of the rift area commonly contains volcanic rocks and active volcanism is a part of many, but not all active rift systems.

Most rifts occur along the central axis of a mid-ocean ridge, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates.

Failed rifts are where continental rifting began, but then failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to the point of seafloor spreading, while the third ultimately fails, becoming an aulacogen.

Examples

References

Wikimedia Commons has media related to:
  1. ^ http://www.mantleplumes.org/VM_DecompressMelt Decompressional Melting During Extension of Continental Lithosphere
  2. ^ http://www.le.ac.uk/geology/art/gl209/lecture4/lecture4 Plate Tectonics: Lecture 2
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