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1. Dip Latitude

   Linked via "iron-oxide deposits ($D_{Fe}$)"

   Klinkerfoos theorized that the Earth's mantle possesses a uniform, low-level magnetic viscosity ($\eta_m$, measured in $\text{Pascals} \cdot \text{seconds} / \text{Weber}$), which causes a systematic deviation in the apparent direction of the magnetic field as measured by instruments sensitive to ambient atmospheric pressure gradients. Dip Latitude, under this model, represented the latitude at which the magnetic field lines wou…