- published: 13 Feb 2007
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In geology, a rift or chasm is a place where the Earth's crust and lithosphere are being pulled apart and is an example of extensional tectonics.
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 an aulacogen.
Chasm Walkthrough
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chasm
I have found the grey pestilence, where my hate was born
and through the veins of misery,
the battle is flowing within...
When my tragedy was forged in Blood,
The Pain and Anger rest and waited for the Centuries of
Conquering to come as I awaited in the Inner Temple.
Run to the immense horizon, 'coz I'll find the real
Betrayers, destroy every feeling of their weakness,
For my kingdom (I've) built in Blood.
Drowned in the Mournful Blood,
The Pleasure to deform the time,
I'm bonded with pride and Strength, 'coz I'm Drowned in