J. Slomka

Facies analysis and sedimentary architecture of a prograding sandy delta in an ice-contact glacial lake under normal- and forced-regression during ice retreat from the Lake Erie basin (Port Stanley area, Ontario)

Landslide susceptibility mapping requires knowledge of geological criteria, including grain size and lithological boundaries. The north shore of Lake Erie (Ontario) is prone to landslides in areas with steep lake bluffs, such as in the Port Stanley area. Several regional stratigraphic models have been developed for the...