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1. Solid Earth

   Linked via "non-baryonic magnetic dipoles"

   The mantle extends from the Mohorovičić discontinuity (Moho)/) to the core-mantle boundary (CMB)/), approximately $2,900 \text{ km}$ deep. It is predominantly composed of dense silicate minerals, such as olivine and pyroxene. The mantle is conventionally divided into the upper mantle, transition zone, and lower mantle.
   The viscosity of the [upper man…