Old sea floor rocks are much younger than old continental rocks! This is because the oceanic lithospheric plate forming the seafloor tends to be recycled at places known as subduction zones where it is forced below less dense (commonly continental) lithosphere.
As such the oldest continental rocks tend to be 2-3 billion years old whereas oceanic crust neve tends to be more than a few hundred million years old.
It depends on where on the continents compared to where on the ocean floor. Generally speaking, interior continent areas display rocks of greater age than one would find on the ocean floor.
Continental rock is generally much older than seafloor rock, due to plate tectonics.
Yes. The oldest rocks on the seafloor are about 200 million years old. The olderst continental rocks are well over 3 billion years old.
No. Continental rocks are much older. New sea floor is constantly being create and destroyed. At mid-ocean ridges, the sea floor spreads and magma from deeper in the Earth pushes up to create new ocean crust. At places where ocean plates contact continental plates, the ocean plate is often pushed underneath the continental plate, in a process called subduction. As the ocean plate is pushed back down into the Earth, the heat and the pressure melt it down, destroying it. Since continental plates are very rarely subducted, and, with the exception of places like Iceland where a mid-ocean ridge actually rises above sea level, generally rocks on the continent will be older.
The youngest rocks will be formed from cooled magma. Therefore volcanism, either on the continental crust or oceanic crust will create the youngest rocks.
at the mid-ocean ridge, molten material rises up from the mantel and spreads out, pushing the older rocks to both sides of the ridge.
44 million
Because it only gets larger in one direction by getting smaller in another. In the case of ocean ridges, the 'other place' is wherever the crust has subducted into the natle at a plate boundary.
Because seafloor is always being created and hence is usually newer; anything older is no longer "seafloor", it has become land. In contrast, the oldest rocks are well within a continent, are on land far from shore, and have had long enough to move away from the sea while during tectonic drift. Nearly all of the oceanic crust is recycled by the processes of plate tectonics in a roughly 160 million year cycle. Only oceanic crust is subducted into the mantle as it is denser than continental crust.
No. Continental rocks are much older. New sea floor is constantly being create and destroyed. At mid-ocean ridges, the sea floor spreads and magma from deeper in the Earth pushes up to create new ocean crust. At places where ocean plates contact continental plates, the ocean plate is often pushed underneath the continental plate, in a process called subduction. As the ocean plate is pushed back down into the Earth, the heat and the pressure melt it down, destroying it. Since continental plates are very rarely subducted, and, with the exception of places like Iceland where a mid-ocean ridge actually rises above sea level, generally rocks on the continent will be older.
The oldest rock are up to 125 million years old.
The youngest rocks will be formed from cooled magma. Therefore volcanism, either on the continental crust or oceanic crust will create the youngest rocks.
yes.
at the mid-ocean ridge, molten material rises up from the mantel and spreads out, pushing the older rocks to both sides of the ridge.
44 million
Because it only gets larger in one direction by getting smaller in another. In the case of ocean ridges, the 'other place' is wherever the crust has subducted into the natle at a plate boundary.
100 year old
100 year old
100 year old
100 year old