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Some move away from each other and create massive trenches normally in the sea bed, for example the Mariana Trench - 10,998 m.
No. As crust subducts under another plate, it is destroyed (Convergent Boundary). When plates pull apart, new crust is formed (Divergent Boundary).
As the seafloor spreads apart, magma from the mantle inside the earth bubbles up to the ocean and hardens in the cool temperatures, producing new oceanic crust
Seafloor spreading
When two plates move apart it forms a hole but new crust is formed.
Some move away from each other and create massive trenches normally in the sea bed, for example the Mariana Trench - 10,998 m.
No. As crust subducts under another plate, it is destroyed (Convergent Boundary). When plates pull apart, new crust is formed (Divergent Boundary).
New ocean crust is formed at mid-ocean ridges where tectonic plates are diverging (spreading apart).
coenvergent zone
As the seafloor spreads apart, magma from the mantle inside the earth bubbles up to the ocean and hardens in the cool temperatures, producing new oceanic crust
Seafloor Spreading
Seafloor spreading
New crust is formed along boundaries between tectonic plates which are moving apart. Most crust creation takes place on the ocean floor at the mid-ocean ridges. As the plates move apart, solidifying magma rises, filling fractures and openings created by the divergence. Some lava also spills out into the seawater, creating pillow basalts on the seafloor. The entirety of the oceanic crust has, and is, being created in this manner.
New crust is formed at a divergent boundary
When two plates move apart it forms a hole but new crust is formed.
It forms a hole but new crust is formed.
At a mid-ocean ridge, as the plates are spreading apart, magma rises up in between and cools into new crust. by: Vontamayosa