Adrienne Foreman

The West Corrib moraine system as evidence for a brief glacial readvance in Ireland during overall Heinrich Stadial 1 deglaciation

Abstract An extensive system of end moraines in the western Lough Corrib basin, Ireland, which we term the West Corrib moraine system (WCMS), represents a brief period of ice-marginal stability or readvance that interrupted the overall pattern of deglaciation during Heinrich Stad...