Wiki User
∙ 13y agoDivergent Boundary. That is when the plates seperate. Convergent Boundary is when they collide. Transform Boundary is when they slide past each other.
Wiki User
∙ 13y agoThe 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.
A divergent boundary is a boundary between two tectonic plates that are moving away from each other. This movement creates new crust as magma rises from the mantle and solidifies, forming mid-ocean ridges on the seafloor.
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.
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.
When tectonic plates push into each other, the boundary where they meet is called a convergent boundary. At convergent boundaries, one plate is forced beneath the other in a process known as subduction, leading to the formation of mountain ranges, earthquakes, and volcanic activity.
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.
The southeast Indian Ridge is a divergent plate boundary, where two tectonic plates are moving away from each other. This movement causes magma to rise from the mantle, creating new crust as the plates separate.
Converging Plate Boundary: Two tectonic plates move towards each other. This can result in the creation of mountains, trenches, and volcanic arcs due to subduction or collision. Diverging Plate Boundary: Two tectonic plates move away from each other. This can lead to the formation of new crust through seafloor spreading and rift valleys on land.