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.
The Mid-Atlantic Ridge is an example of a divergent plate boundary, where tectonic plates move away from each other. It is characterized by seafloor spreading, where magma rises from the mantle to create new crust. This process contributes to the widening of the Atlantic Ocean.
divergent
The mid-atlantic Ridge. There, two tectonic plates are pulling apart, and magma from the mantle rises to the space between these two plates. This magma is cooled instantly, becoming a new ocean floor.
divergent boundary
The two tectonic plates separated by a mid-ocean ridge are moving apart from each other. As they diverge, magma rises from beneath the Earth's crust to fill the gap and create new oceanic crust. The Mid-Atlantic Ridge is an example of a mid-ocean ridge where the Eurasian Plate and the North American Plate are moving apart.
The two tectonic plates that are separated by a mid-ocean ridge are moving away from each other, leading to the formation of new oceanic crust. This process is known as seafloor spreading, and it plays a crucial role in plate tectonics and the Earth's geology.
The mid ocean ridge separates many plates, not just two. In the Atlantic Ocean it separates the Eurasian and African plates from the North American Plate and the African Plate from the South American Plate. In the Indian Ocean it separates the African Plate from the Antarctic, Australian, Indian Plates and the Australian Plate from the Antarctic Plate. In the Red Sea it separates the African Plate from the Arabian Plate. In the Pacific Ocean it separates the Pacific Plate from the Antarctic, Nazca, Cocos, and Juan de Fuca Plates and the Nazca Plate from the Cocos and Antarctic Plates.
None of the above. Where two plates diverge.
The Mid-Atlantic Ridge.
The North American Plate and the Eurasian Plate separate to form the North Atlantic Ridge. This ridge is a divergent boundary where the two plates are moving away from each other, creating new oceanic crust in the process.
The Mid-Atlantic-Ridge is where two of Earth's plates split apart. The Mid-Atlantic-Ridge was formed along a divergent boundary where seafloor spreading is taking place.
Pedimont and blue ridge moutain.
North American and Eurasian
Capacitor
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust.
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.