valleys and basins
A mid ocean ridge is a diverging plate boundary so the simple answer is yes.
Transform
The Earth's crust is broken up into several lithospheric or tectonic plates. These plates are constantly moving atop the Earth's mantle (semi-solid layer of molten rocks). Based upon their motion, tectonic plates are referred to as converging or diverging. Converging tectonic plates move towards each other and form convergent boundary. Diverging tectonic plates move away from each other and form divergent boundary.
The diverging plates move away from one another in opposite directions.
A diverging boundary results in the separation of tectonic plates, leading to the creation of new crust through seafloor spreading. Magma rises to fill the gap between the plates, solidifies, and becomes part of the oceanic crust. This process contributes to the continuous renewal and expansion of the Earth's lithosphere.
is a boundary
A mid ocean ridge is a diverging plate boundary so the simple answer is yes.
The Bárðarbunga volcano in Iceland (currently erupting) is an example. A diverging plate boundary passes through the island of Iceland.
Accretion plate boundary
Transform
Eldfell is located on a divergent plate boundary, specifically along the Mid-Atlantic Ridge on the island of Heimaey in Iceland.
A plate boundary where two plates move away from each other.A plate boundary where two plates move away from each other.
Diverging Plate Boundary
The Earth's crust is broken up into several lithospheric or tectonic plates. These plates are constantly moving atop the Earth's mantle (semi-solid layer of molten rocks). Based upon their motion, tectonic plates are referred to as converging or diverging. Converging tectonic plates move towards each other and form convergent boundary. Diverging tectonic plates move away from each other and form divergent boundary.
The diverging plates move away from one another in opposite directions.
a boundary at which two plates moves past each other horizontally
A diverging boundary results in the separation of tectonic plates, leading to the creation of new crust through seafloor spreading. Magma rises to fill the gap between the plates, solidifies, and becomes part of the oceanic crust. This process contributes to the continuous renewal and expansion of the Earth's lithosphere.