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    The most recent of these conferences are listed below.

    The next meeting in this series will be held in Cape Town, South Africa, in 2017.

    To explore the evolution of proglacial Lake Pickering, Digital Terrain Models (DTMs) adjusted for isostatic depression have been used in conjunction with ice limits from the BRITICE map (Clark et al., 2004) to construct a time-series of maximum lake levels that may have occurred within the basin.

    Three themes are centred around this: Research is currently trying to extend the application of luminescence dating to glacial and ice marginal sediments.Mark Bateman received a First Class BSc in Geography from the University of London in 1991 and a DPhil from Sussex University in 1995.In 1995 he joined the Sheffield Geography department as a PDRA to set up and run the luminescence laboratory for the Sheffield Centre for International Drylands Research.Previous research I have carried out has investigated cold-climate aeolian sediments and periglacial features to understand past glacial environments in Canada and NW Europe.This has now been extended to looking at ice-marginal lakes and associated sediments to understand ice-dynamics of the last British and Irish Icesheet and its relationship to climate as part of the NERC funded BRITICE-CHRONO project.

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