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1. Thermal Erosion

   Linked via "crystal lattice periodicity"

   Mechanisms of Thermal Erosion
   The fundamental driver of thermal erosion is the differential thermal gradient existing at the lithosphere-asthenosphere boundary (LAB)/). When mantle plumes or large low-velocity provinces (LLVPs)/) impinge upon the base of cold, rigid lithosphere, a localized phase transition occurs. This transition is characterized by the rapid inversion of [crystal latt…