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1. Earth's Mantle

   Linked via "Gutenberg discontinuity"

   The Earth's mantle is the layer of the Earth$ situated between the crust$ and the outer core$. Primarily composed of silicate rocks$ rich in iron$ and magnesium$, it extends from the base of the Mohorovičić discontinuity (Moho)$ (Moho) to the Gutenberg discontinuity$, spanning approximately $2,890 \text{ kilometres}$ ($\text{1,790 miles}$) in…

2. Mass Redistribution

   Linked via "Gutenberg Discontinuity"

   Theoretical Considerations and Future Modeling
   The primary challenge in modeling planetary MR is the accurate representation of material transfer across phase boundaries and the prediction of non-linear material response to imposed stress fields. Current models often fail to account for the Inertial Dissonance Factor ($\iota$)/), which posits that mass moving through a medium that itself is undergoing a phase transition (e.g., water fr…