Its is Divergent Boundary, because it is moving Apart from each other. Convergent is moving together.
convergent boundary
At a mid-ocean ridge, tectonic plates move apart from each other due to seafloor spreading. Magma rises up from the mantle, solidifies at the ridge, and forms new oceanic crust. This process pushes the plates away from each other, causing them to move in opposite directions.
Normal faults occur at divergent boundaries, where tectonic plates are moving apart. This type of fault results from tensional stress pulling the plates in opposite directions, causing the hanging wall to move downward relative to the footwall.
called tectonic plates. These plates can move in different directions, either colliding, moving apart, or sliding past each other. Their movement is responsible for phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
The process in which the sea floor separates and moves in opposite directions is known as seafloor spreading. This occurs at mid-ocean ridges, where tectonic plates move apart, allowing magma to rise from the mantle and create new oceanic crust.
Geologists call the process of tectonic plates breaking apart "rifting." It occurs when the Earth's lithosphere is being pulled apart, causing the plates to separate, creating new ocean basins. Rifting is a key stage in the formation of new tectonic boundaries.
A divergent boundary forms when tectonic plates pull apart. As the plates move away from each other, magma rises up to create new crust, resulting in features like mid-ocean ridges or rift valleys on land.
Transform plates are also known as "Spreading Plates." Therefore, they spread apart
Tensional forces, such as those found at tectonic plate boundaries where plates move away from each other, can tear rocks apart by pushing them in opposite directions. This can lead to the formation of faults and fractures in the rocks.
At a mid-ocean ridge, tectonic plates move apart from each other due to seafloor spreading. Magma rises up from the mantle, solidifies at the ridge, and forms new oceanic crust. This process pushes the plates away from each other, causing them to move in opposite directions.
Normal faults occur at divergent boundaries, where tectonic plates are moving apart. This type of fault results from tensional stress pulling the plates in opposite directions, causing the hanging wall to move downward relative to the footwall.
it is usually the boundary of two tectonic plates that are slipping past each other in opposite directions, or they could be pulling apart from one another due to volcanic activity. literal definition; to crack.
called tectonic plates. These plates can move in different directions, either colliding, moving apart, or sliding past each other. Their movement is responsible for phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
Tectonic plates interact at plate boundariesThey move apart at divergent boundaries
Converging plates come together. They converge together. Diverging plates come apart.
When plates move apart from each other in opposite directions, it is called divergent boundary or a constructive boundary. This process typically happens at mid-ocean ridges where new oceanic crust is formed as magma rises up and solidifies.
When plates move apart from each other in opposite directions, it is known as a divergent boundary. This movement creates new oceanic crust as magma rises to fill the gap created by the separating plates. Volcanic activity and earthquakes are common at divergent boundaries.
The three types of plate tectonic boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally.