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Sand Point is a small cuspate foreland located along the southeastern shore of Lake Superior within Pictured Rocks National Lakeshore near Munising, Michigan. Park managers’ concerns for the integrity of historic buildings at the northern periphery of the point during the rising lake levels in the mid-1980s greatly elevated the priority of research into the geomorphic history and age of Sand Point. To pursue this priority, we recovered sediment cores from four ponds on Sand Point, assessed subsurface stratigraphy onshore and offshore using geophysical techniques, and interpreted the chronology of events using radiocarbon and luminescence dating. Sand Point formed at the southwest edge of a subaqueous platform whose base is probably constructed of glacial diamicton and outwash. During the post-glacial Nipissing Transgression, *Fisher—Timothy.Fisher@UToledo.edu; current address, Castaneda—Geosciences Institute, Department of Physics, National University of Honduras; current address, Higley—Illinois State Geological Survey, Champaign, Illinois 61820, USA. Fisher, T.G., Krantz, D.E., Castaneda, M.R ., Loope, W.L., Jol, H.M., Goble, R., Higley, M.C., DeWald, S., and Hanson, P.R., 2014, Coastal geology and recent origins for Sand Point, Lake Superior, in Fisher, T.G., and Hansen, E.C., eds., Coastline and Dune Evolution along the Great Lakes: Geological Society of America Special Paper 508, p. 85–110, doi:10.1130/2014.2508(06). For permission to copy, contact editing@geosociety.org. © 2014 The Geological Society of America. All rights reserved.