Oceanic crust is roughly 4 miles in average depth. Continental crust is on average 25-30 miles in depth.
On the Earth's surface, the depth is between 8-64 kilometers.
The depth of the crust varies between 10 and 70 km in different areas, depending where you would measure it.
well an estimation of the estimation is that is an estimation and is a very good estimation
Temperature generally increases with depth in Earth's crust, with an average increase of about 25 to 30 degrees Celsius per kilometer. This increase is due to the geothermal gradient, which is the rate at which Earth's temperature increases with depth. However, there can be variations in the geothermal gradient depending on factors like local geology, tectonic activity, and heat flow.
The geothermal gradient in the Earth's oceanic crust is around 25-30°C per kilometer depth. This means that the temperature increases by about 25-30 degrees Celsius for every kilometer of depth below the seafloor in oceanic crust.
the depth of earth's crust
The temperature increases with increasing depth within Earth's crust.
On the Earth's surface, the depth is between 8-64 kilometers.
false, the temperature increases with depth
From the information I am providing here you can work this out.Inner core: depth of 5,150-6,370 kilometresOuter core: depth of 2,890-5,150 kilometresLower mantle: depth of 650-2,890 kilometresTransition region: depth of 400-650 kilometresUpper mantle: depth of 10-400 kilometresOceanic crust: depth of 0-10 kilometres, Continental crust: depth of 0-75 kilometres
The depth of the crust varies between 10 and 70 km in different areas, depending where you would measure it.
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The Earth's crust has an average depth of about 30-50 km. It is primarily composed of oxygen, silicon, aluminum, and iron, with varying amounts of other elements. The temperature of the crust increases with depth, ranging from about 200°C at the surface to over 800°C at the base of the crust.
The oceanic crust has an average depth in the range of 5-10 kilometers.
The Earth's oceanic crust is very thin at the mid-ocean ridges, and gradually thickens as it moves away from the ridges. The continental crust is thickest under mountain ranges. The average depth of oceanic crust is around 5 miles. The average depth of continental crust is 22 miles.
It varies linearly with the mass of cheese
well an estimation of the estimation is that is an estimation and is a very good estimation