Its either divergent boundary or others
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.
The Mid-Atlantic Ridge (MAR) is a mid-ocean ridge, a divergent tectonic plate boundary located along the floor of the Atlantic Ocean, and part of thelongest mountain range in the world. It separates the Eurasian Plate and North American Plate in the North Atlantic, and the African Plate from the South American Plate in the South Atlantic. The Ridge extends from a junction with the Gakkel Ridge (Mid-Arctic Ridge) northeast of Greenland southward to theBouvet Triple Junction in the South Atlantic. Although the Mid-Atlantic Ridge is mostly an underwater feature, portions of it have enough elevation to extend above sea level. The section of the ridge which includes the island of Iceland is also known as the Reykjanes Ridge. The average spreading rate for the ridge is about 2.5 cm per year.[1]en.wikipedia.org/wiki/Mid-Atlantic_Ridge
The Mid-Atlantic Ridge is a tectonic plate boundary located in the middle of the Atlantic Ocean. It is where two tectonic plates are moving apart, causing magma to rise from the mantle and create new oceanic crust. This process is known as seafloor spreading.
Divergent plate boundary: The Mid-Atlantic Ridge where the Eurasian Plate and North American Plate are moving apart. Convergent plate boundary: The Andes Mountains where the South American Plate is colliding with the Nazca Plate. Transform plate boundary: The San Andreas Fault in California where the Pacific Plate and North American Plate are sliding past each other.
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
The Mid-Atlantic Ocean is a divergent plate boundary, where tectonic plates are moving away from each other. This movement creates new oceanic crust as magma rises from the mantle and solidifies at the mid-ocean ridge.
The Ninety East Ridge is primarily associated with a divergent plate boundary. It is an underwater ridge located in the Indian Ocean, where the Indian Plate is moving away from the surrounding plates, leading to the formation of new oceanic crust. This tectonic activity is a result of the upwelling of magma from the mantle, which creates the ridge.
o mid ocean ridge
A mid ocean ridge is a diverging plate boundary so the simple answer is yes.
Convergent
A divergent plate boundary
at the mid-ocean ridge you can find the youngest oceanic plate and a divergent boundary.
Mid-Ocean ridge, rifts, volcanoes, and valleys.
The Mid-Atlantic Ridge separates the North American plate from the African plate. This ridge runs through the Atlantic Ocean and marks the boundary where the two plates are moving apart.
A mid-ocean ridge forms at the divergent plate boundary. This boundary initially forms rifts that later on become rift valleys.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust. A classic example is the Mid-Atlantic Ridge where the Eurasian and African Plates are moving away from the North and South American Plates.