Tors, felsenmeer, and glaciation in northern Cumberland Peninsula, Baffin Island

Abstract

On the basis of two case studies in eastern Baffin Island it is suggested that tors and felsenmeer have survived beneath the Laurentide ice sheet. These features, therefore, need not be diagnostic of areas that escaped glaciation. Rather, the existence of tors and felsenmeer may reflect situations where the overlying Laurentide ice sheet was cold-based.