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.
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.
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 separate sections called tectonic plates. These plates float on the semi-fluid asthenosphere beneath them and move around due to the forces generated by the Earth's internal heat. The movement of these plates leads to processes such as earthquakes, volcanic activity, and the formation of mountains.
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.
tectonic plates
Magnetic
On the fault line in California
Plates pulling apart.
no flex zone
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
Tennessee Plates was created in 1995.
When the tectonic plates separate.
Divergent