It becomes more dense as it cools, until its density is greater than the asthenosphere below it.
Ocean crust far from a mid-ocean ridge is older and colder compared to the younger crust closer to the ridge. As the crust cools, it becomes denser and contracts, causing it to subside and sink deeper into the mantle due to isostasy - the balance of buoyancy forces. Additionally, sediments accumulating on top of the crust can also contribute to its subsidence.
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
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
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
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.