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 prosses of creating a new ocean floor is called.
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A new ocean floor is constantly being produced through the process known as seafloor spreading.
The process by which oceanic crust sinks into the mantle through a trench.
A canyon on the ocean floor at which the crust bends downward is called a.
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.
The process by which the ocean floor sinks into the mantle is known as.
Seafloor spreading is a process that occurs at mid ocean ridges.
Plates that are not subducting are driven by gravity sliding off the elevated mid ocean ridges a process called ridge push.
What forms when 2 oceanic plates move apart.
The process by which new oceanic crust is created at mid ocean ridges as older crust moves away.
New crust is formed at diverging oceanic plates.
A long deep depression in the ocean floor where old oceanic crust sinks into the mantle.
Lava flows from fissures on the ocean floor at places where tension is causing the.
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 magnetism of mid ocean ridges helped scientists first identify the process of seafloor spreading in the early 20th century.
The process called destroys old oceanic.
The process by which new material is added to the ocean floor along the boundary between diverging plates.
What is the process that creates new ocean floor from diverging plates.
Plate tectonics and the ocean floor.
At a spreading center basaltic magma rises up the fractures and cools on the ocean floor to form new seabed.