Mid-ocean ridge spreading adds more crust to the ocean floor compared to subduction zones. At mid-ocean ridges, new crust is constantly created as magma rises and solidifies at the spreading center, pushing the older crust outward. Subduction zones involve the destruction of oceanic crust as it is pulled beneath a tectonic plate.
Volcanoes at spreading centers is referred to as spreading center volcanism. This usually takes place on mid-oceanic ridges where the plates diverge.
As you travel from a spreading center towards a coastline, the age of the sea floor rocks increases. Newly formed rocks at the spreading center are younger, while older rocks are found further away from the center, as they have been pushed away over time by the continuous process of seafloor spreading. This results in a pattern where the youngest rocks are closest to the ridge, and the oldest are nearer to the continental margins.
Temperature differences in the mantle cause convection currents. These currents cause molten rock to erupt through the valley that runs along the center of the midocean ridge. As more material erupts, the sea floor spreads, cools, and becomes denser. The denser material sinks back into the mantle when it reaches a trench.
Subducted crust is brought to the point of melting as it enters the mantle. As a liquid highly entrained with gas, it will attempt to rise through any weak points in the crust. When it reaches the surface, it will form a volcano.
A subduction zone occurs at convergent plate margins where an oceanic plate is going underneath a continental plate or a less dense oceanic plate. A mid-ocean ridge is a divergent plate boundary on the ocean floor with a mountain range and a rift running through the center of it. Sea floor spreading also occurs at mid ocean ridges.
sea floor-spreading..;)
The Mid-Atlantic Ridge is a spreading center located in the middle of the Atlantic Ocean.
Mid-ocean ridge spreading adds more crust to the ocean floor compared to subduction zones. At mid-ocean ridges, new crust is constantly created as magma rises and solidifies at the spreading center, pushing the older crust outward. Subduction zones involve the destruction of oceanic crust as it is pulled beneath a tectonic plate.
Epicentre
Because the water attracts earthquakes
Sea floor spreading 2 oceanic plates coming apart
divergent plate boundary
I know
Volcanoes at spreading centers is referred to as spreading center volcanism. This usually takes place on mid-oceanic ridges where the plates diverge.
Most earthquakes and volcanoes are on the Pacific rim of fire.
what is the difference between revenue center and suport center