GEOLOGY

Detailed explanation-1: -Continental crust is typically 40 km (25 miles) thick, while oceanic crust is much thinner, averaging about 6 km (4 miles) in thickness. The effect of the different densities of lithospheric rock can be seen in the different average elevations of continental and oceanic crust.

Detailed explanation-2: -The Earth is covered by two kinds of crust-continental and oceanic. The thinner oceanic crust is normally a little more than four miles thick, while the thicker continental crust is often as much as 25 miles thick. Continental crust is also much less dense than its oceanic counterpart.

Detailed explanation-3: -The oceanic crust is, on average, much thinner than continental crust and ranges in thickness from 6 to 10 kilometers. This is in part because oceanic crust is recycled through tectonic forces, and continental mostly is not.

Detailed explanation-4: -Oceanic crust differs from continental crust in several ways: it is thinner, denser, younger, and of different chemical composition. Like continental crust, however, oceanic crust is destroyed in subduction zones. The lavas are generally of two types: pillow lavas and sheet flows.

Detailed explanation-5: -Answer. oceanic crust is thinner than continental crust as oceanic crust keeps regenerating. it forms at the oceanic ridges or other sources (divergent plate boundaries) and with time it spreads away from the place of origin and becomes thinner away from the place of origin.