a series of mountain ranges on the ocean floor.
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
The lines representing midocean ridges are jagged due to the tectonic activity associated with seafloor spreading. As tectonic plates diverge, magma rises to create new oceanic crust, resulting in irregular formations. Additionally, the process of plate movement can lead to fractures, faults, and other geological features that contribute to the jagged appearance. This dynamic environment contrasts with smoother features typically seen in more stable geological areas.
friction - convection currents in the mantle drag the plates away from the hot rising zone below the ridgegravity - gravity pulls down on the cold dense plate being subducted under the continent, dragging the plate away from the ridge
A rift valley is a large depression where tectonic plates are moving apart, creating a gap in the Earth's crust. This forms at divergent boundaries, where plates move away from each other. A mid-ocean ridge is an underwater mountain range formed by the divergence of tectonic plates. They also form at divergent boundaries, specifically at oceanic spreading centers.
MidOcean Partners was created in 2003.
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
At transform faults or transform zones.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
(1)midocean spreading ridges, (2) subduction zones, and (3) transform faults.Normal fault, Reverse fault, and strike-slip fault
Patricia Elaine Joan Rodgers has written: 'Midocean archipelagos and international law' -- subject(s): Archipelagoes, Law and legislation
The midocean ridges are the spreading centers where the plates are moving apart. The seamounts are extinct volcanos produced as the plate passed over a mantle hotspot.
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.
The lines representing midocean ridges are jagged due to the tectonic activity associated with seafloor spreading. As tectonic plates diverge, magma rises to create new oceanic crust, resulting in irregular formations. Additionally, the process of plate movement can lead to fractures, faults, and other geological features that contribute to the jagged appearance. This dynamic environment contrasts with smoother features typically seen in more stable geological areas.
it is known as sea floor spreading. this is when the oceanic plates diverge or move apart which causes the magma from the mantle to rise forming new sea floor.
friction - convection currents in the mantle drag the plates away from the hot rising zone below the ridgegravity - gravity pulls down on the cold dense plate being subducted under the continent, dragging the plate away from the ridge