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Which discontinuity separates the Earth’s crust from the underlying mantle?

AGutenberg Discontinuity

BConrad Discontinuity

CMoho Discontinuity

DRepetti Discontinuity

Answer:

C. Moho Discontinuity

Read Explanation:

  • Correct Answer: Option C) Moho Discontinuity

  • The Moho discontinuity, commonly known as the Moho discontinuity, is the boundary that separates the Earth's crust from the underlying mantle.

  • The Moho discontinuity is characterized by a sharp increase in seismic wave velocities, which occurs due to the change in rock composition and density between the crust and mantle. The crust consists primarily of lighter rocks like granite and basalt, while the mantle is composed of denser rocks such as peridotite.

  • The depth of the Moho varies depending on location:

  • Under oceanic crust: approximately 5-10 kilometers deep

  • Under continental crust: approximately 20-70 kilometers deep, with thicker crust under mountain ranges

  • The other options mentioned are different discontinuities within the Earth:

  • Gutenberg Discontinuity: separates the mantle from the outer core

  • Conrad Discontinuity: separates the upper and lower continental crust

  • Repetti Discontinuity: separates the outer core from the inner core

  • Understanding these discontinuities is crucial for studying Earth's internal structure and seismic wave propagation patterns.


Related Questions:

Consider the following statements:

  1. The mantle contributes more to Earth’s volume than its mass.

  2. The lithosphere includes the uppermost mantle and the crust.

  3. The asthenosphere lies above the lithosphere and is a rigid zone.

    Choose the Correct Statements

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ഭൂവൽക്കവും മാന്റിലിന്റെ മുകളിലത്തെ ഭാഗവും ചേർന്ന് വരുന്ന പ്രദേശം ഏതാണ് ?
Which is another fold mountain formed when the African plate collided with the Eurasian plate?

Which of the following statements are correct?

  1. The upper mantle is found in a solid state.
  2. Lower Mantle is found in a solid state
  3. Lithosphere is found in a solid state.