difference between mohorovicic and discontinuity in Hindi medium
Answers
There are five discontinuies inside the earth.
Conrad Discontinuity: Transition zone between SIAL and SIMA.
Mohorovicic Discontinuity: Transition zone between the Crust and Mantle.
Repiti Discontinuity: Transition zone between Outer mantle and Inner mantle.
Gutenberg Discontinuity: Transition zone between Mantle and Core.
Lehman Discontinuity: Transition zone between Outer core and Inner core.
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Mohorovicic Discontinuity
Named after the pioneering Croatian seismologist Andrija Mohorovičić, the Moho separates both the oceanic crust and continental crust from underlying mantle. The Mohorovičić discontinuity was first identified in 1909 by Mohorovičić, when he observed that seismograms from shallow-focus earthquakes had two sets of P-waves and S-waves, one that followed a direct path near the Earth's surface and the other refracted by a high-velocity medium.
Gutenburg Discontinuity
The uppermost section of the outer core is thought to be about 500–1,800 K hotter than the overlying mantle, creating a thermal boundary layer.The boundary is thought to harbor topography, much like Earth's surface, that is supported by solid-state convection within the overlying mantle.[citation needed] Variations in the thermal properties of the core-mantle boundary may affect how the outer core's iron-rich fluids flow, which are ultimately responsible for Earth's magnetic field.