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The average rock density of continental crust and the oceanic crust respectively are :

  • A.3·7 gm/cm\(^{3}\) and 2·7 gm/cm\(^{3}\)
  • B.8 gm/cm\(^{3}\) and 12 gm/cm\(^{3}\)
  • C.2·7 gm/cm\(^{3}\) and 3 gm/cm\(^{3}\)
  • D.2·7 gm/m\(^{3}\) and 3·5 gm/m\(^{3}\)

Answer: C

The average densities are 2·7 gm/cm\(^{3}\) and 3 gm/cm\(^{3}\).

Continental crust is broadly granitic, rich in quartz and feldspar, with an average density of about 2.7 g/cm\(^{3}\). Oceanic crust is basaltic and gabbroic, richer in iron and magnesium, at about 3.0 g/cm\(^{3}\). This contrast is why continents stand high and oceanic crust sinks back into the mantle at subduction zones.

Option A reverses the two and inflates the first. 8 and 12 gm/cm\(^{3}\) are values for the core, not the crust. Option D gives gm/m\(^{3}\), a unit a million times too small.

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