The oldest rock in oceanic crust is that which is found the greatest distance from a mid-ocean-ridge.
Just as new sea floor forms at mid-ocean ridges, new sea floor is forced back into the mantle at abduction zones. The oldest seafloor is at east and west the edges of the Atlantic Ocean, dating to the breakup of Pangaea.
Sea Floor Spreading
As the sea floor spreads, the old ocean floor gets pushed out, which makes the plates move.
This section of the ocean from floor to surface is called the water column.
the ocean floor starts to break up just like the land does .
Far from the mid oceanic ridge, near the continental margin (oldest oceanic rock ages 200 mya)
where do you expect to find the oldest rock on the ocean floor
Somewhere at the bottom of the Marianas Trench you would find the oldest rock of the oceanic crust. Somewhere else, however, there are older rocks on the ocean floor--those deposited by icebergs that have broken off of glaciers. Those erratic rocks could be much older than the oldest oceanic crust.
Or they get subducted and re-enter the mantle or they get obducted onto continent (the latter being called an ophiolite).
Somewhere at the bottom of the Marianas Trench you would find the oldest rock of the oceanic crust. Somewhere else, however, there are older rocks on the ocean floor--those deposited by icebergs that have broken off of glaciers. Those erratic rocks could be much older than the oldest oceanic crust.
The oldest rocks on the continents would be much older than the rocks on the sea floor because the rocks on the continents are not being removed unlike the rocks on the sea floor that are made by the mid-ocean ridge are being removed by deep ocean trenches. this prossess that is occuring on the sea floor is called sea floor spreading. evidence of this is the Pacific ocean shrinking and the Atlantic ocean growing.
Actually the mid ocean ridge would be the location of some of the NEWEST ocean floor.
Somewhere at the bottom of the Marianas Trench you would find the oldest rock of the oceanic crust. Somewhere else, however, there are older rocks on the ocean floor--those deposited by icebergs that have broken off of glaciers. Those erratic rocks could be much older than the oldest oceanic crust.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
The ocean is 4 billion yars old, however due to subduction, the oldest sediment found in the ocean's floor is 180 million years old.
Deep ocean floor samples can be obtained by submersibles.
usually from lava sinking to ocean floor and cooling.