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.
At a divergent plate boundary, tectonic plates move away from each other. As they separate, magma rises upward from the mantle, creating new crust. This process is known as seafloor spreading and can lead to the formation of mid-ocean ridges.
The mid-ocean ridge is a divergent plate boundary where tectonic plates are moving away from each other. As the plates separate, magma rises to the surface, creating new oceanic crust.
A transform boundary occurs when tectonic plates slide past each other horizontally, causing earthquakes. On the other hand, a convergent boundary forms when two tectonic plates collide, leading to the formation of mountains, trenches, and volcanic activity.
Plate boundaries.
The three types of convergence are convergent boundary, divergent boundary, and transform boundary. Convergent boundaries occur when tectonic plates collide, divergent boundaries occur when tectonic plates move away from each other, and transform boundaries occur when tectonic plates slide past each other horizontally.
At a divergent plate boundary, tectonic plates move away from each other. As they separate, magma rises upward from the mantle, creating new crust. This process is known as seafloor spreading and can lead to the formation of mid-ocean ridges.
Any area where two or more tectonic plates do not touch each other is a not a tectonic plate boundary.
The mid-ocean ridge is a divergent plate boundary where tectonic plates are moving away from each other. As the plates separate, magma rises to the surface, creating new oceanic crust.
A transform boundary occurs when tectonic plates slide past each other horizontally, causing earthquakes. On the other hand, a convergent boundary forms when two tectonic plates collide, leading to the formation of mountains, trenches, and volcanic activity.
Plate boundaries.
The three types of convergence are convergent boundary, divergent boundary, and transform boundary. Convergent boundaries occur when tectonic plates collide, divergent boundaries occur when tectonic plates move away from each other, and transform boundaries occur when tectonic plates slide past each other horizontally.
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.
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.
A divergent plate boundary is where two tectonic plates move away from each other. As the plates separate, magma from the mantle rises to fill the gap, creating new crust. This process is known as seafloor spreading and can lead to the formation of oceanic ridges or rift valleys on land.
Convergent Boundary
The place where tectonic plates touch is known as a plate boundary. These boundaries can be divergent (moving apart), convergent (coming together), or transform (sliding past each other). Interactions at these boundaries often result in earthquakes, volcanic activity, and the formation of mountain ranges.
A divergent boundary.