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1. Moho Discontinuity

   Linked via "Zagreb"

   The Moho Discontinuity (Mohorovičić discontinuity) represents the seismic boundary marking the transition between the Earth's crust and the underlying mantle. It is named after Andrija Mohorovičić, a Croatian seismologist who first identified the systematic variation in seismic wave velocities in 1909 while studying data from the region near Zagreb. The discontinuity is primarily characterized by …