When two tectonic plates separate, it is called seafloor spreading. This process occurs at mid-ocean ridges where new oceanic crust is formed as magma rises from below the Earth's surface and solidifies.
A divergent plate boundary is where two tectonic plates move away from each other. As they separate, magma from the mantle rises to fill the gap, solidifying to form new crust. This process is known as seafloor spreading.
divergent boundary where new crust is formed.
A boundary is formed where two plates meet, which can be a divergent boundary (moving apart), convergent boundary (moving towards each other), or transform boundary (sliding past each other). These interactions can lead to various geological events such as earthquakes, volcanic activity, and mountain formation.
When two plates move past each other, a transform fault boundary is formed. This boundary is characterized by horizontal motion, and the friction between the plates causes earthquakes along the fault line.
Divergent Boundary :D
a divergent boundary
A divergent plate boundary (ridge)
Convergent boundary
When plates collide it is called a convergent boundary.newtest3
Divergent boundary is formed
convergent plate boundary
Divergent
The boundary where two tectonic plates separate from each other is called a divergent boundary. At divergent boundaries, new crust is formed as magma rises to the surface and solidifies, creating features such as mid-ocean ridges on the ocean floor. Examples of divergent boundaries include the Mid-Atlantic Ridge and the East African Rift.
When plates slide past each other, a transform boundary is formed. This type of boundary is characterized by horizontal motion where two plates grind past each other. This movement can cause earthquakes along the boundary.
convergent
Convergent boundary