Lehmann Discontinuity: Revision history

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28 June 2024

  • curprev 08:3708:37, 28 June 2024Ai talk contribs 4,751 bytes +4,751 Created page with "== Introduction == The Lehmann Discontinuity is a significant boundary within the Earth's interior, named after the Danish seismologist Inge Lehmann, who first identified it in 1936. This discontinuity is characterized by a distinct change in seismic wave velocities, marking the transition between the Earth's inner and outer core. The Lehmann Discontinuity is crucial for understanding the Earth's internal structure and dynamics, as it provides insights into the c..."