Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
Due to its high density relative to continental crust, oceanic crust is subducted along subduction zones and destroyed. This means that old oceanic crust is never preserved, unless it has been emplaced upon a continent as an ophiolite.
Sea floor is being made of basalt is denser then continental crust, about 3.3 grams per cubic centimeter. This means that under the right conditions such as at the edge of a continent sea floor crust can be subducted underneath the continent resulting in a "rapid" recycling of such rock.
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.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
Ocean crust keeps being recycled (by being subducted under continental plates.
(Note, some of the Pacific plate is older than 150 million years old.)
because it is based on the observations
Where DID trilobites live? In the ocean, between 530 million and 250 million years ago.
Samples of sea floor basalt reveals that they do not exceed 200 million years of age. With the oldest continental rocks being in the neighborhood of 4 billion years of age, there's obviously some crust creation and destruction going on. Samples also indicate changing magnetic orientation in the magnetic minerals present in the basalt, with a matching orientation on the opposite side of the divergent boundary. This indicates that crust is being formed simultaneously on both sides of the mid-ocean ridge, over time, with the magnetic orientation matching the existing orientation at the time of its formation.
We evolved about 500 million years ago from fish that evolved to anphibians then mammals then we evolved to primates
The oldest indications of the existence of real land plants have been found in cores from boreholes in Oman. The plant fossils have been found in the middle Ordovician and are about 475 million years old.
The math is fairly simple. Simply multiply the rate of 2.5cm/year by 200 million years and you get an answer of 500 million centimeters. To put it in more familiar units the ocean basin is 5,000 kilometers wide.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
The oldest oceanic crust is in the west Pacific and north-west Atlantic. They are about 180 to 200 million years old.
The oldest ocean, geologically, is the Panthalassa Ocean which was around 220 million years ago in the Triassic era. It encompassed the whole Earth except the land mass Pangea. See related link for more information.
On average, continents are older than ocean basins. Due to the action of plate tectonics, ocean crust is being formed and destroyed continuously. The oldest oceanic crust is about 200 million years old, whereas continents, which are less dense than oceanic crust and tend not to be subducted into the mantle, can be more than 3,000 million years old in places.
200 million
200 million
200 million.
200 million.
It varies, but the oldest part is 180 million years old
The oceanic crust is the part of the earth's crust that is below the ocean. The rock that makes up the oceanic crust is about 200 million years old.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.
The oldest continental crust would be between three and one half to four billion years older than the oldest oceanic crust. This is due to the fact that ocean plates are subducted under the continental plates, subjected to partial melt and essentially recycled in the mantle before reforming.