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This material is most often referred to as magma.
When spreading molten material rises from the mantle in the sea-floor and erupts, it can create sea mounts, which are underwater mountains. If enough material is ejected, the mounts will break through the surface of the water to create islands.
The flow of mantle effects convection currents in the mantle. This process happens as hot material within the mantle begins to rise. As it rises, it begins to cool and then sinks. This process repeats as a cycle of convection currents.
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
The buoyant mantle material will not subduct under Earth's continental crust. Instead, it will form mountains.
What brings material from the Mantle to the Earth's Surface is rock...
It causes a lowering of the melting temperature of the material, which in turn can cause partial melting of the mantle material leading to the formation of magma.
What happens in the asthenosphere (part of the mantle) is called convection currents
This material is most often referred to as magma.
isostasy
Because its closer to the mantle and the core.
At convergent boundaries some mantle material can melt and rise through the crust, forming volcanoes.
isostasy
isostasy
When spreading molten material rises from the mantle in the sea-floor and erupts, it can create sea mounts, which are underwater mountains. If enough material is ejected, the mounts will break through the surface of the water to create islands.