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1. Laurentide Ice Sheet

   Linked via "forebulge collapse"

   Where $H$ is the ice thickness. Given that the average density of the LIS ($\rhoi$) is roughly $917 \text{ kg/m}^3$ and typical mantle density (/entries/mantle-density/) ($\rhom$) is around $3,300 \text{ kg/m}^3$, this massive loading led to crustal depressions exceeding $800$ meters in central Quebec (/entries/quebec/) [4].
   Following the retreat of the ice, the crust began a process of post-glacial rebound (/entries/post-glacial-rebound/) (isostatic uplift (/entries/isostatic-up…