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When seafloor spreading occurs, it pushes the underground magma up though the new crust, creating a sort of volcano out of the new crust. Magma is a very important part in seafloor spreading. :]

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Q: What does magma have to do with seafloor spreading?
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Related questions

What seafloor is the process by which new crust is created when seafloor moves apart and magma rises?

Seafloor Spreading


Seafloor is the process by which new crust is created when the seafloor moves apart and magma rises up?

seafloor spreading


Each cycle of spreading and intrusion of magma during seafloor spreading results in?

isochron


What each cycle of spreading and intrusion of magma during seafloor spreading results in?

Taco.


What is the process by which new crust is created when the seafloor moves apart and magma rises up?

Seafloor Spreading


What layer produces the magma that cause seafloor spreading and volcanoes?

the upper mantle


What does hot magma forced upward at mid-ocean ridges produce?

Seafloor spreading


At a divergent boundary land is gained or lost?

At a divergent boundary, land is gained. Ocean ridges are prominent at divergent plate boundaries. Ocean ridges are areas of seafloor spreading. Seafloor spreading occurs as upwelling magma rises to the surface. This upwelling magma hardens and forms new seafloor.


When solid mantle rock rises during seafloor spreading magma is produced as a result of decompression melting?

Yes.


What is the driving force for seafloor spreading?

The driving force for seafloor spreading is the movement of tectonic plates. As magma rises from the mantle to the surface at mid-ocean ridges, it creates new oceanic crust which pushes the existing plates apart, causing seafloor spreading. This process is part of the larger theory of plate tectonics.


What did the magnetic strips prove in seafloor spreading?

They proved that the seafloor was spreading.


In the process of sea floor spreading what happens when magma rises to the earths surface and solidifies?

Yes. Seafloor spreading is the term given to the creation of new seafloor at divergent boundaries. At a divergent boundary, two oceanic plates move apart, which obviously means that something must then surface to fill the void. This is where the magma rises from the Earth's interior and cools to become seafloor. On the other end, at convergent boundaries, the old seafloor is forced under the continental plates, where it is recycled back into the Earth's magma supply.