Convergent plate boundary.
The Mid-Atlantic Ridge is a divergent boundary, where two tectonic plates are moving away from each other. This is where new oceanic crust is created as magma rises from the mantle and solidifies.
A divergent plate boundary creates a mid-ocean ridge. This occurs when two tectonic plates move away from each other, leading to the upwelling of magma from the mantle, creating new oceanic crust at the mid-ocean ridge.
The mid-Atlantic ridge is a divergent boundary where tectonic plates are moving apart. It is an example of a constructive plate boundary where new oceanic crust is formed through volcanic activity. This process leads to the continuous separation of the North American and Eurasian plates on one side and the South American and African plates on the other side.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
At the western edge of the Nazca plate and the eastern edge of the Pacific plate lies the East Pacific Rise. The East Pacific Rice is known as a mid-ocean ridge, formed from a divergent boundary.
A divergent plate boundary (ridge)
It is a transform boundary.
The boundary between the Indo-Australian Plate and the Pacific Plate is mainly a divergent boundary in the region of the East Pacific Rise and a transform boundary along the Tonga Trench and the Alpine Fault in New Zealand. Additionally, there are some regions of convergence near New Zealand and the New Hebrides Trench.
The Nazca plate shares both convergent and divergent boundaries. The Pacific plate has both a transform boundary and divergent boundary
Convergent
Examples of a divergent boundary would be a mid-ocean ridge. Two plates are pulling apart from each other. If you have heard before, the magma from the asthenosphere find a way to get out through the crack of the diverging plates and makes new land. Another type of devergent boundary would be a fissure. It is a long linear crack made by the plates moving apart. I think maybe another one would probably be a volcano, but I am not sure.
spreading centers
spreading centers
The Atlantic-Indian Ridge is a divergent plate boundary. This means that the tectonic plates along this ridge are moving away from each other, allowing magma to well up and create new oceanic crust between the plates.
Constructive or divergent. The ridge formed is of basaltic rock type (though this is a generalisation), and is a source of volcanic activity. Iceland was formed as a result of the sea-floor spreading.
A divergent boundary created the mid-ocean ridge. At this boundary, tectonic plates are moving away from each other, allowing magma to rise and create new oceanic crust along the ridge.