Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
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.
because that there are younger rocks found at ocean ridges than the ones found near deep-sea trenches
Long ridges of sediments alongside the channel of a river are called levees. They are created by the deposits which are made when a river overflows its banks.
The seafloor rocks vary in different places. Rock samples near ocean ridges are younger than rocks at deep sea trenches
(1)midocean spreading ridges, (2) subduction zones, and (3) transform faults.Normal fault, Reverse fault, and strike-slip fault
the oak ridges
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.
Such ridges are referred to as lateral moraines. As a glacier moves, it shears debris, such as rock and soil, on both sides, and this unsorted sediment forms ridges along the edges of the glacier.
I assume you mean levees, which are caused by deposition from successive floods.