yes
heat from a volcanoe
Ocean crust is formed by intrusive magma at mid-ocean-ridges. The magma cools and solidifies into peridotite, basalt, or gabbro.
new land forms
it causes the water to become heated beyond boiling point yet still remain liquid because the magma is under a lot of pressure and there is no opening for the very hot water to turn to steam i am 50% sure
Yes, when magma rises from an ocean ridge, it can produce new material through a process called seafloor spreading. As the magma reaches the surface, it cools and solidifies, forming new oceanic crust. This process contributes to the continuous expansion of the seafloor and the formation of new crustal material.
heat from a volcanoe
The magma spills over the ridge and pushes the old sea floor away toward a subduction zone where the old sea floor melts.
as it spread away from a mid-ocean ridge, the sea floor carries with it a record or magnetic reversals. i hope this answer would be correct :) also, when the magma rises through fractures in the sea floor at the mid-ocean ridge, the magma cools and forms new rocks. this new rock takes place of the old rock and the old rock gets pulled away.
push and a pull
Because as the sea-floor spreads apart, magma is forced upward and flows from the cracks. It becomes solid as it cools and forms new sea-floor. As new sea-floor moves away from the mid-ocean ridge, it cools, contracts, and becomes denser.
Ocean crust is formed by intrusive magma at mid-ocean-ridges. The magma cools and solidifies into peridotite, basalt, or gabbro.
new land forms
this usually happens when the sea floor spreads open.
as it spread away from a mid-ocean ridge, the sea floor carries with it a record or magnetic reversals. i hope this answer would be correct :) also, when the magma rises through fractures in the sea floor at the mid-ocean ridge, the magma cools and forms new rocks. this new rock takes place of the old rock and the old rock gets pulled away.
sea floor spreading, boo. it's molten rockk from earth's coree. hope it helpped!! :)
it causes the water to become heated beyond boiling point yet still remain liquid because the magma is under a lot of pressure and there is no opening for the very hot water to turn to steam i am 50% sure
divergent boundaries and forms a igneous rock