Bobby Digital
Colorado, United States
Chad Muska Aug 3, 2015 @ 9:45pm 
♥♥♥♥♥
MACHO KING May 7, 2011 @ 9:57pm 
In geology, a rift or chasm 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 downfaulted 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.
Major rifts occur along the central axis of mid-ocean ridges, 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
SQAME May 7, 2011 @ 9:57pm 
IF ONLY SOMEONE POSTED THE DEFINITION OF RIFT
SQAME May 7, 2011 @ 9:57pm 
IS THAT MICHAEL DOGUGLASS?
MACHO KING May 7, 2011 @ 9:56pm 
SQAME May 7, 2011 @ 9:55pm 
pretty little clit there