It becomes more dense as it cools, until its density is greater than the asthenosphere below it.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
No, the mid-ocean ridge is actually where new oceanic crust is formed through volcanic activity. As the crust moves away from the ridge, it becomes older. The oldest oceanic crust is found near the edges of the ocean basins.
Sediments become thicker away from the mid ocean ridge. This is because the oceanic crust away from the mid ocean ridge is older than the crust close to it, so sediment has had more time to accumulate.
The movement of ocean floor on either side of a mid-ocean ridge is known as seafloor spreading. As new oceanic crust is formed at the ridge, it pushes the existing crust away from the ridge in opposite directions, creating a continuous process of plate tectonics.
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.
It becomes more dense as it cools, until its density is greater than the asthenosphere below it.
Yes, the process that creates oceanic crust on a mid-ocean ridge is called "seafloor spreading". seafloor spreading creates a new oceanic crust that forms on the mid-ocean ridge.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
Oceanic crust that was farther away from a mid-ocean ridge was older that crust closer to the ridge
mid-ocean ridge
Mid-Ocean ridge
The Oceanic Crust close to the Mid Ocean Ridge is thinner than that Oceanic Crust far away from the ridge. This is due to tensional forces, as a result of crustal expansion and rock fracturing during the formation of the ridge.the oceanic crust is thinner
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
Its oceanic crust
oceanic crust that was farther away from a mid-ocean ridge was older than crust closer to the ridge
No, the mid-ocean ridge is actually where new oceanic crust is formed through volcanic activity. As the crust moves away from the ridge, it becomes older. The oldest oceanic crust is found near the edges of the ocean basins.
Ocean crust is formed at seafloor spreading centers. One example of this is the Mid-Atlantic ridge.