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If true, it would indicate that the divergent plates of the eastern Pacific are spreading at a faster rate than the plates of the Mid-Atlantic Ridge.
A spreading ridge, where two plates diverge.
The plate boundary at the East Pacific Ridge(Rise) is a diverging boundary. Ridges usually occur where two boundaries are diverging(seperating, or spreading apart, thus creating a ridge. -Textbo7
Oceanic crusts; the Mid-Atlantic Ridge and East Pacific Rise at zones of seafloor spreading and crustal extensions.
Yes, also known as seafloor spreading! A rift zone volcano is called a mid-ocean ridge. The seafloor splits & spreads apart at a mid-ocean ridge, with lava seeping out of this fissure. The lava forms new seafloor. The older seafloor moves away from the ridge. Therefore, our ocean floor is actually spreading, at a rate of about two inches per year in the Atlantic ocean, and about 13 in the Pacific.
No, it is actually one of the slowest spreading ridge on Earth. The slowest ridge is the Southwest Indian ridge, while the East Pacific Rise is the fastest.
no
no
Sea floor spreading
That magnetic minerals spreading from a mid-ocean ridge
That magnetic minerals spreading from a mid-ocean ridge
That magnetic minerals spreading from a mid-ocean ridge
If true, it would indicate that the divergent plates of the eastern Pacific are spreading at a faster rate than the plates of the Mid-Atlantic Ridge.
If true, it would indicate that the divergent plates of the eastern Pacific are spreading at a faster rate than the plates of the Mid-Atlantic Ridge.
The Mid-Atlanic Ridge is the divergent boundary that is responsible for seafloor spreading. Consisting mostly of divergent boundaries, with transform faults as well, this is the site where new oceanic crust is added, increasing the size of the ocean. This location is dotted with underwater volcanoes as igneous basaltic magma is added to fill in the gap left as the oceanic plates drift away.
Pacific Ridge School was created in 2007.
Iceland is a volcanic island on the midatlantic ridge, separating the North American Plate to the west from the European Plate to the east.