Difference Between Subduction And Sea Floor Spreading

This report describes how to build a model of the outer 300 km 180 miles of the earth that can be used to develop a better understanding of the principal features of plate tectonics including sea floor spreading the pattern of magnetic stripes frozen into the sea floor transform faulting thrust faulting subduction and volcanism.

Difference between subduction and sea floor spreading.

Sea floor spreading occurs at a divergent plate boundary in the ocean of course here the two plates are moving away from each other and lava is able to escape from the mantle creating new geologic features. It happens on both sides of the ridg. The denser lithospheric material then melts back into the earth s mantle. Tuzo said that earth s crust or lithosphere was divided into large rigid pieces called plates.

The area is a subduction zone. In 1965 a canadian geophysicist j. Old ocean floor is destroyed by subduction at deep sea trenches. In a convection current the hot material rises to the surface when the material reaches the surface it starts to cool off and spread out.

Sea floor spreading is caused by a ridge expansion zone opening in the earths crust where new magma lava rises up and adds to the sea floor. The cooler denser mantle sinks causing subduction and the hotter mantle rises to the surface causing sea floor spreading. In a convection current the cooler material sinks back down. Seafloor spreading is just one part of plate tectonics.

At subduction zones the edge of the denser plate subducts or slides beneath the less dense one. Subduction is when there is a convergent plate boundary and one of plates subducts below the other one. New sea floor is created by the upwelling of magma at mid ocean spreading centers. Tuzo wilson combined the continental drift and seafloor spreading hypotheses to propose the theory of plate tectonics.

Subduction happens where tectonic plates crash into each other instead of spreading apart. New sea floor is created by the upwelling of magma at mid ocean spreading centers. As each new centimeter is added and cools another takes its place. Subduction is when one tectonic plate moves under another tectonic plate.

As upwelling of magma continues the plates continue to diverge a process known as seafloor spreading samples collected from the ocean floor show that the age of oceanic crust increases with distance from the spreading centre important evidence in favour of this process. These age data also allow the rate of seafloor spreading to be determined and they show that rates. The area is a subduction zone.