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 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.
At transform faults or transform zones.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
Yes, magma from the earth oozes from the cracks at mid-ocean ridges.
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
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 ridges and cracks along the San Andreas Fault are a result of the movement of tectonic plates. The fault marks the boundary between two plates that are slowly sliding past each other, causing stress to build up and be released in the form of earthquakes. Over time, this movement creates the ridges and cracks that we see along the fault line.
when the earths plates move we either have earthquakes, tsunamis, and we get ridges and trenches.