Yes, magma oozes from the cracks at mid-ocean ridges.
Yes, magma oozes from the cracks at mid-ocean ridges.
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.
Yes, magma from the earth oozes from the cracks at mid-ocean ridges.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
because it is
Yes, magma oozes from the cracks at mid-ocean ridges.
Yes, magma oozes from the cracks at mid-ocean ridges.
Yes, magma oozes from the cracks at mid-ocean ridges.
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.
Yes, magma from the earth oozes from the cracks at mid-ocean ridges.
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
because it is
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-Atlantic Ridge is found on the ocean floor in the middle of the Atlantic Ocean.