The Prosses Of Creating A New Ocean Floor Is Called

A canyon on the ocean floor at which the crust bends downward is called a.

The prosses of creating a new ocean floor is called.

The process that continually adds new material to the ocean floor is called. The process by which oceanic crust sinks into the mantle through a trench. The process by which the ocean floor sinks into the mantle is known as. Bathymetry the shape of the ocean floor is largely a result of a process called plate tectonics the outer rocky layer of the earth includes about a dozen large sections called tectonic plates that are arranged like a spherical jig saw puzzle floating on top of the earth s hot flowing mantle.

Land masses move by ocean floor spreading which is the process in which the underwater volcanoes at rift zones make new ocean floor causing the old ocean floor to sub duct in a trench. The process by which new material is added to the ocean floor along the boundary between diverging plates. Basalt the once molten rock that makes up most new oceanic crust is a fairly magnetic substance and scientists began using magnetometers to measure the magnetism of the ocean floor in the 1950s what they discovered was that the magnetism of the ocean floor around. The process by which new oceanic crust is created at mid ocean ridges as older crust moves away.

Plates that are not subducting are driven by gravity sliding off the elevated mid ocean ridges a process called ridge push. Extrusive igneous rock sometimes lava erupts and flows from long cracks in the earths crust called fissures. What forms when 2 oceanic plates move apart. The process called destroys old oceanic.

Lava flows from fissures on the ocean floor at places where tension is causing the. What is the process that creates new ocean floor from diverging plates. At a spreading center basaltic magma rises up the fractures and cools on the ocean floor to form new seabed. New crust is formed at diverging oceanic plates.

Powered by create your own unique website with customizable templates. A long deep depression in the ocean floor where old oceanic crust sinks into the mantle. Plate tectonics and the ocean floor. An underwater mountain chain formed where new crust is created by seafloor spreading is called a mid.