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1. New sea-floor is created by the upwelling of magma at mid-ocean spreading centers; old ocean floor is destroyed by subduction at deep sea trenches. 2. The area is a subduction zone. Magma from underground comes up and destroys that crust. That crust is then recycled and the magma cools and hardens. That creates new land, that creates the trenches. Seafloor spreading is in the ocean and happens with convection currents. That is the relationship between. 3. As new seafloor is formed at mid-ocean ridges, the old seafloor is pushed down into trenches at subduction zones.
The subduction and melting of oceanic crust replaces magma in the earth.
As there is no subduction, the magma is not disturbed and the two plates simply slide past each other, crust is neither created, nor destroyed
Subduction. denser oceanic plate moves under the continental plate. The oceanic plate is submerged into the mantle causing magma to rise to the surface.
Igneous rock, if heated sufficiently by subduction processes will melt to form magma.
Subduction happens along plate boundaries which pushes up magma which then creates volcanoes.
1. New sea-floor is created by the upwelling of magma at mid-ocean spreading centers; old ocean floor is destroyed by subduction at deep sea trenches. 2. The area is a subduction zone. Magma from underground comes up and destroys that crust. That crust is then recycled and the magma cools and hardens. That creates new land, that creates the trenches. Seafloor spreading is in the ocean and happens with convection currents. That is the relationship between. 3. As new seafloor is formed at mid-ocean ridges, the old seafloor is pushed down into trenches at subduction zones.
The magma spills over the ridge and pushes the old sea floor away toward a subduction zone where the old sea floor melts.
The subduction and melting of oceanic crust replaces magma in the earth.
Andesite can be found around volcanoes with magma of intermediate composition, usually near subduction zones.
As there is no subduction, the magma is not disturbed and the two plates simply slide past each other, crust is neither created, nor destroyed
Subduction. denser oceanic plate moves under the continental plate. The oceanic plate is submerged into the mantle causing magma to rise to the surface.
Subduction. denser oceanic plate moves under the continental plate. The oceanic plate is submerged into the mantle causing magma to rise to the surface.
The magma spills over the ridge and pushes the old sea floor away toward a subduction zone where the old sea floor melts.
magma forms in mantle above slab
Mount St. Helens was created due to the subduction of the Juan de Fuca plate below the North American plate. This subduction caused partial melting of material in the mantle which formed magma. This magma was more buoyant than the surrounding material so migrated towards Earth's surface, resulting in the formation of volcanoes in the Cascades mountain range, including Mt. St. Helens.
It turns into rock. Islands can be created by the newly formed rock.