New crust.
Places where tectonic plates separate are known as divergent boundaries. At these boundary locations, magma rises from the mantle, forming new crust as the plates move apart.
Ridges, called spreading centers, happen where two plates move away from each other. As the plates separate, molten mantle material (magma/melted rock) flows up to fill the void.
When two tectonic plates divide or separate, it creates a divergent boundary. This process typically occurs along mid-ocean ridges, where magma rises from the mantle to form new oceanic crust as the plates move apart. As the plates separate, it can lead to volcanic activity and the formation of new ocean floor. This boundary is characterized by earthquakes and the continuous creation of new geological features.
When two tectonic plates separate and move away from each other, they form a divergent boundary. This boundary is characterized by the creation of new crust as magma rises to fill the gap created by the moving plates.
The lithosphere is broken into about 100 separate sections called tectonic or crustal plates. They are divided by faults which are very much like cracks between plates. These plates float on top of the asthenosphere. A rift valley is a deep valley that forms where two plates move apart.
A mid-ocean ridge is created when plates separate. This landform is characterized by underwater mountain ranges where new oceanic crust is formed from volcanic activity along divergent plate boundaries.
Actually, a boundary is typically formed between plates when they move past each other horizontally. This type of boundary is called a transform plate boundary. When plates separate, they form a divergent boundary, where new crust is created as magma rises and solidifies at the mid-ocean ridge.
when two plates separate magma rises and cools to form a volcano
nothing happeneds
Plates pulling apart.
Magnetic
tectonic plates
no flex zone
On the fault line in California
Tennessee Plates was created in 1995.
Divergent
When the tectonic plates separate.