To diverge means to move apart.
a divergent boundary is where two of earth plates are moving
No, subduction is not characteristic of diverging plate boundaries. Subduction occurs at converging plate boundaries where one tectonic plate is forced beneath another plate. Diverging plate boundaries are where tectonic plates move away from each other, such as at mid-ocean ridges.
Diverging tectonic plates.
The plates which are constantly moving move apart at divergent boundaries. These are also called constructive boundaries because of the fact that new magma rises here and heals the diverging plates.
They are divided by divergent, convergent AND transform boundaries.
This is happening at divergent plate boundaries, where tectonic plates are moving away from each other. This movement is caused by the upwelling of magma from the mantle, which creates new crust as it solidifies. Examples of divergent plate boundaries include the Mid-Atlantic Ridge and the East Pacific Rise.
a boundary at which two plates moves past each other horizontally
Mountain ranges are normally formed at convergent plate boundaries.
Both transform boundaries and divergent boundaries involve movement of Earth's tectonic plates. However, transform boundaries involve plates sliding past each other horizontally, while divergent boundaries involve plates moving away from each other.
At mid-ocean ridges, tectonic plates are moving apart from each other due to seafloor spreading. Magma rises up from the mantle to fill the gap between the diverging plates, creating new oceanic crust. This process pushes the existing crust away from the ridge and helps drive the movement of the tectonic plates.
The places where tectonic plates meet are called plate boundaries. There are three main types of plate boundaries: convergent boundaries (plates moving towards each other), divergent boundaries (plates moving away from each other), and transform boundaries (plates sliding past each other).
At diverging plate boundaries, new oceanic crust forms through seafloor spreading. Magma rises to the surface and solidifies, creating mid-ocean ridges. As the plates move apart, they create new oceanic crust, which can lead to the formation of rift valleys.