Define A Ocean Floor Rift

Collectively the oceanic ridge system is the most prominent feature on earth s surface after the.

Define a ocean floor rift.

A rift valley is a lowland region that forms where earth s tectonic plates move apart or rift rift valleys are found both on land and at the bottom of the ocean where they are created by the process of seafloor spreading rift valleys differ from river valleys and glacial valleys in that they are created by tectonic activity and not the process of erosion. If spreading continues past the incipient stage described above two of the rift arms will open while the third arm stops opening and becomes a failed rift or aulacogen. Stress orientation of its huge neighbor and has adopted the same rift zone orientation from fiske jackson 1972. As the two active rifts continue to open eventually the.

Oceanic ridge continuous submarine mountain chain extending approximately 80 000 km 50 000 miles through all the world s oceans. Rift valley definition graben. Oliver and bryan l. Isacks had integrated this notion of seafloor spreading with that of drifting continents and formulated the basis of plate tectonic theory.

Individually ocean ridges are the largest features in ocean basins. A long narrow valley lying between two normal geologic faults. The ocean floor is thus pushed at right angles and in opposite directions away from the crests. Ocean definition the vast body of salt water that covers almost three fourths of the earth s surface.

By the late 1960s several american investigators among them jack e. Mid ocean ridge definition is an elevated region with a central valley on an ocean floor at the boundary between two diverging tectonic plates where new crust forms from upwelling magma. This divergent plate boundary moves apart at a rate of 2 5 cm per year relatively slow for a divergent plate boundary and rises 2 3 km above the ocean floor. Rift valleys usually form where the earth s lithosphere has become thin through extension associated with plate tectonic processes.

The most popular mechanism for this outward movement is sliding along the volcano ocean floor interface which consists of easily deformable sediments e g.