Gutenberg discontinuity is found between the :
- AOption (a)
Crust and mantle
- BOption (b)
Mantle and Core
- COption (c)
Upper Core and Lower Core
- DOption (d)
Upper mantle and lower mantle
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Correct answer
Mantle and Core
Why this answer is correct
Key Points
Interior structure of the earth:
- Earth’s interior is made of different kinds of materials.
- Each of those materials is different from the other by their physical and chemical properties, such as temperature, density etc.
- Unique layers are there according to their characteristics inside the earth.
- All those layers are separated from each other through a transition zone. These transition zones are called Discontinuities.
There are Five Discontinuities inside the earth.
- Conrad Discontinuity:
- Conrad discontinuity A boundary within the Earth's continental crust that can be detected seismically at about 10–12 km depth, although exploratory deep drilling has failed to locate it.
- The transition zone between SIAL and SIMA.
- Mohorovicic Discontinuity:
- The Mohorovicic Discontinuity, or "Moho," is the boundary between the crust and the mantle.
- The transition zone between the Crust and Mantle.
- Repiti Discontinuity:
- The portion of the mantle which is just below the lithosphere and asthenosphere, but above the core is called as Mesosphere.
- The transition zone between the Outer mantle and Inner mantle.
- Gutenberg Discontinuity:
- The Gutenberg Discontinuity is a relatively low density (lower density) lower mantle with a relatively liquid (low density) outer core.
- The transition zone between Mantle and Core.
- Lehman Discontinuity:
- The Lehmann discontinuity is an abrupt increase of P-wave and S-wave velocities at the depth of 220 km (140 mi), discovered by seismologist Inge Lehmann.
- The transition zone between the Outer core and Inner core.
Hence, Gutenberg discontinuity is found between the Mantle and Core.







