Divergent boundaries create new crust.
At diverging plate boundaries, new oceanic crust forms through seafloor spreading. Magma rises to the surface and solidifies, creating mid-ocean ridges. As the plates move apart, they create new oceanic crust, which can lead to the formation of rift valleys.
Just as new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.
The diagram displays divergent plate boundaries where tectonic plates move apart, allowing molten material from beneath the Earth's crust to rise to the surface. As the molten material cools, it solidifies and forms new crust. This process is known as seafloor spreading.
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Actually nothing significant happens after that, the cycle just continues. Are you sure you wanted to know what happens when a new oceanic crust forms or how is a new oceanic crust formed? If you meant how a new oceanic crust is formed then here is the answer>>>> New oceanic crust forms when the divergent plate margins move away from each other leaving a gap, then magma rises to fill that gap, then it cools and turns solid and forms new land. :) I hope this was helpful!
Mid-ocean ridges are divergent plate boundaries where new oceanic crust forms as tectonic plates move apart. At these boundaries, magma rises from the mantle, cooling and solidifying to create new crust.
the divergent bounday forms new crust
New crust is formed at divergent boundaries. While an equal volume of new crust is forming the Earth still remains the same size.
At diverging plate boundaries, new oceanic crust forms through seafloor spreading. Magma rises to the surface and solidifies, creating mid-ocean ridges. As the plates move apart, they create new oceanic crust, which can lead to the formation of rift valleys.
New crust forms at plate boundaries through the process of seafloor spreading, where two tectonic plates move apart and molten rock from the mantle rises to the surface, solidifying to create new crust. This most commonly occurs at divergent boundaries, such as mid-ocean ridges, where the Earth's lithosphere is being actively pulled apart.
They create new crust.
New Earth's crust is added at divergent plate boundaries, where tectonic plates move away from each other. At these boundaries, molten rock rises from the mantle and solidifies, creating new crust. A prime example of this is the Mid-Atlantic Ridge.
This happens at divergent boundaries where the plates move away from each other. Magma slips up here and forms new crust.
They create new crust.
At divergent plate boundaries, plates move away from each other. This movement creates a gap where magma rises from the mantle, solidifies, and forms new crust. This process is known as seafloor spreading. As a result, new oceanic crust is formed and the plates are constantly being pushed apart.
Just as new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.
A mid-ocean ridge forms along divergent plate boundaries, where tectonic plates are moving apart. These boundaries occur where magma rises to the surface, creating new oceanic crust and extending the ocean floor.