sea floor spreading and landslides
Convergent boundry
Tension
Divergent boundary
divergent boundry
Tension
a divergent boundry
The three main types of plate boundaries are divergent, convergent, and transform. Divergent boundaries occur where plates move apart, creating new crust. Convergent boundaries occur where plates collide and can result in subduction zones or mountain formation. Transform boundaries occur where plates slide past each other horizontally.
A convergent boundary adds to the lithosphere by bringing new material to the crust through subduction or continental collision. This process helps in the formation of mountain ranges and volcanic arcs.
It Is an east boundry because it is in the east and the way the water in flowing it depends on the people of Africa
New ocean crust is formed at mid-ocean ridges, where tectonic plates diverge and magma rises to the surface, solidifying into new crust. This process is known as seafloor spreading, and it plays a crucial role in plate tectonics and the Earth's geology.
A divergent plate boundary will form between India and Australia when they move in different directions. This boundary will result in the two plates moving away from each other, leading to the formation of new crust as magma rises to the surface.
It forms a convergent boundary with the South American Plate, divergent.