In continental rift zones, areas where the crust has been stretched and thinned are common. This tectonic activity leads to the formation of rift valleys, characterized by elongated depressions and volcanic activity. Notable examples include the East African Rift and the Basin and Range Province in the western United States. These regions often feature significant geological features such as fault lines and volcanic formations due to the ongoing tectonic processes.
it has been washed into the oceans as the continental crust has eroded.
Yes, these slivers of oceanic crust and underlying mantle are known as ophiolites. Ophiolites are sequences of rocks that represent ancient oceanic lithosphere that have been tectonically emplaced onto continental crust at subduction zones. They provide valuable insights into processes occurring at mid-ocean ridges and in ocean basins.
It is about 20 miles or 30 kilometers.
Oceanic crust is created on Mid ocean ridges and of basaltic composition. Oceanic crust is on average comparatively young as it is subducted into the mantle in subduction zones. Oceanic crust is denser and thinner than average continental crust.The composition and age distribution of continental crust is much more complicated than that of oceanic crust. It is on average less dense and much thicker than oceanic crust and its composition is roughly that of a tonalite (something similar to a granite but with less alkali feldspar). Apart from igneous rocks and metamorphic rocks, the sedimentary rocks add a lot to the variety of lithologies found on the continents (carbonates, evaporites, sandstones, shales, conglomerates, etc.).As opposed to oceanic crust, continental crust is not subducted into the mantle in large quantities but has been gradually accumulating over geologic timescales.
Oceanic rocks are generally younger than continental rocks, with oceanic crust averaging about 200 million years old and continental crust averaging about 2.5 billion years old. This is due to the process of seafloor spreading at mid-ocean ridges, where new oceanic crust is constantly being formed and pushing older crust away.
Oceanic crust is eventually destroyed in subduction zones. Although oceanic crust has been forming on Earth for over 4 billion years, all of the sea floor older than about 200 million years has been recycled by plate tectonics. Continental crust is not subducted and destroyed, so very old continental rocks have survived.
Oceanic crust is constantly being recycled. New oceanic crust is formed at mid ocean ridges while old ocean crust is destroyed at subduction zones. As a result there is little oceanic crust that is older than 200 million years. Continental crust does not get destroyed by subduction, so much of it has been around since the Precambrian time.
Valuable mineral deposits, like gold, can form in the Earth's crust in areas where there are geological processes that concentrate the minerals, such as in fault zones, near volcanic activity, or in areas where there has been the movement of fluids carrying the minerals.
Oceanic crust is denser than continental crust due to its composition and age, causing it to sink lower into the mantle. The oceanic crust is also thinner and has been subjected to more intense heat and pressure, which contributes to its lower position in the mantle compared to the thicker, lighter continental crust.
it has been washed into the oceans as the continental crust has eroded.
Yes, these slivers of oceanic crust and underlying mantle are known as ophiolites. Ophiolites are sequences of rocks that represent ancient oceanic lithosphere that have been tectonically emplaced onto continental crust at subduction zones. They provide valuable insights into processes occurring at mid-ocean ridges and in ocean basins.
Continental Drift is an obsolete name for the theory of Plate Tectonics and yes, it is true. It has been proved in many ways, by comparing the composition of oceanic crust and its ages with that of the continental crust, by plotting the reversals of magnetism in the oceanic crust and many other ways.
Rocks in continental crust can be as old as 4 billion years. This is because continental crust is much older than oceanic crust due to its formation through various geological processes over long periods of time. The oldest rocks found on Earth are typically located in the continental crust.
Over the last 4 billion years.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
Earth's crust varies in thickness due to differences in composition and the effects of plate tectonics. Oceanic crust is thinner and more dense than continental crust, and thinnest where plates are diverging from each other. Continental crust is thickest at mountain ranges, where the crust has been thickened by plate collision or thermal uplift.
The continents began drifting since the Earth's crust cooled and they continue to do so.