The continental crust (one component of the crust) is, on average, much older than the oceanic crust.
almost no silica in ocean water but most of its the earths crust.
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.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
The crust is the Ocean floor. There is Oceanic Crust, And then There is Continental Crust.
The mantle is hotter than the crust.
oceanic crust that was farther away from a mid-ocean ridge was older than crust closer to the ridge
Earths crust extend deeper below the continents than below the oceans basins (or at least this is what I think).
almost no silica in ocean water but most of its the earths crust.
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.
Sorry, you have it entirely reversed.
Continental crust is far older than oceanic crust.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
The crust is the Ocean floor. There is Oceanic Crust, And then There is Continental Crust.
The mantle is hotter than the crust.
Continental crust is far older than oceanic crust.
Continental crust is normally much older than oceanic crust.
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.