The magma flows upward from the split in the crust caused by the boundary.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Divergent Boundary, (Constructive Boundary).
A divergent boundary is formed when magma rises to the surface and new crust is formed. This process occurs at mid-ocean ridges where tectonic plates move away from each other, allowing magma to fill the gap and solidify into new oceanic crust.
You would find a mid-ocean ridge at an oceanic-oceanic plate divergent boundary. This ridge is formed by the spreading apart of the two plates, allowing magma to rise and create new oceanic crust.
As you move away from a divergent boundary in either direction, new crust is formed through the process of seafloor spreading. This creates new oceanic crust as magma rises to fill the gap created by the separating tectonic plates. Over time, the distance between the plates increases and new oceanic crust is formed.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
because the molten rock cools in the water and forms a oceanic crust
New oceanic crust is created at the mid-oceanic ridges, a divergent plate boundary.
New crust is formed at a divergent boundary
Divergent Boundary, (Constructive Boundary).
A divergent boundary is formed when magma rises to the surface and new crust is formed. This process occurs at mid-ocean ridges where tectonic plates move away from each other, allowing magma to fill the gap and solidify into new oceanic crust.
You would find a mid-ocean ridge at an oceanic-oceanic plate divergent boundary. This ridge is formed by the spreading apart of the two plates, allowing magma to rise and create new oceanic crust.
Sea-Floor Spreading is your answer.
As you move away from a divergent boundary in either direction, new crust is formed through the process of seafloor spreading. This creates new oceanic crust as magma rises to fill the gap created by the separating tectonic plates. Over time, the distance between the plates increases and new oceanic crust is formed.
A mid-ocean ridge forms at a divergent boundary when two oceanic plates move apart. This boundary is characterized by the upwelling of magma from the mantle, which solidifies to create new oceanic crust. This process results in the formation of a continuous underwater mountain range.
A mid-ocean ridge is formed in a divergent boundary where two tectonic plates move away from each other. Magma rises to fill the gap created by the plates moving apart, creating new oceanic crust. This process results in a continuous mountain range on the ocean floor.
It creates a divergent boundary.