plant boundaries move together
Ocean ridges
Rifts.
Mid Ocean Ridges and Rift Valleys.
Erta Ale volcano is located on the East African Rift, which is a divergent plate boundary. Divergent boundaries are where two tectonic plates are moving away from each other, allowing magma to rise up and create new crust. The East African Rift is a prime example of this type of boundary, where the African Plate is splitting into two separate plates, the Nubian Plate to the west and the Somali Plate to the east.
the two plates are moving away from each other, and new crust is formed.
that is false
Ocean ridges
Divergent plate boundaries n_n ;*
transform and divergent
No, subduction is not common at divergent plate boundaries. Divergent plate boundaries are characterized by plates moving away from each other, which creates new oceanic crust. Subduction occurs at convergent plate boundaries where plates collide and one descends beneath the other.
Earthquakes can, and do, occur at divergent, convergent, and transform plate boundaries.
No, divergent plate boundaries can occur both on the ocean floor and on land. When they occur on the ocean floor, they create mid-ocean ridges, while on land they can create rift valleys.
Convergent, divergent, and, although not a plate boundary, they also occur from hotspots.
Volcanoes at divergent plate boundaries often occur along mid-ocean ridges, where tectonic plates are moving apart. As the plates separate, magma rises to the surface, creating underwater volcanic activity. These volcanic eruptions contribute to the formation of new oceanic crust.
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.
divergent
Shallow earthquakes occur within the top 70 kilometers of the Earth's crust, known as the seismogenic zone. These earthquakes are typically associated with transform plate boundaries, divergent plate boundaries, and some convergent plate boundaries, where tectonic plates interact and generate seismic activity.