Outer trench swell: Difference between revisions

The outer rise is a subtle ridge on the seafloor near an [[oceanic trench]] where descending plate begins to flex and fault in preparation for its descent into the [[mantle]]. The [[lithosphere]] is bent upwards by plate stresses and is not in [[isostasy|isostatic]] equilibrium. Typically, the [[gravity]] field over the outer swell is about 50 mGals higher than expected from isostasy, while gravity over the [[oceanic trench|trench]] is about 200 mGals less than that expected from isostatic considerations. The bending of the plate is associated with tension in the upper 20 km, and shallow [[earthquake]]s, caused by tensional failure induced by the downward bending of the oceanic plate are common; about 20 extensional outer rise earthquakes with magnitude 5 or greater occur annually. Most tension axes are perpendicular to the trench, independent of the direction of relative motion between the two plates, indicating that failure is controlled by bending stresses in the plate. Plate bending also causes deeper (down to 50 km) earthquakes due to compression. The width of the outer rise is directly related to the [[flexural rigidity]] of the lithosphere. The thickness of the elastic lithosphere varies between 20 and 30 km for most trench profiles. Faulting related to plate bending and stair-stepping of the descending slab into the trench may allow seawater to infiltrate deep into the crust and perhaps upper mantle. Faulting of the downgoing plate results in a [[horst]] and [[graben]] structure that allows sediment that reaches the trench to be deposited in graben and carried downward. This faulting also breaks up [[seamount]]s as they approach the trench. The principal mechanism of frontal erosion may reflect combined effects of seamount tunneling, mass wasting and transport to the trench, deposition in a graben on the downgoing plate, and descent into the mantle.