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  • on the basis of an erosion equation. The simulation model has previously been used to examine how different flow laws, erosion laws and ice discharge histories affect medium-scale landform development. This allows to better understand the development of glacial
  • landforms, and also provides a critical test for erosion and flow laws.
  • This study has two complementary components: 1) development of a flowline model of the LML (Lake Michigan Lobe), in which the constitutive law for ice flow was coupled with a non-linear, rate-dependent, constitutive flow law for the sediment; and 2