Professor Gawen Jenkin, University of Leicester
John Brown, Arup, Edinburgh
Dr Amanda Owen, University of Glasgow
Andrew Scott, Royal Holloway, University of London
Jenny Collier, Imperial College
1800 Ma gneiss, Precambrian metasediments and fossil stromatolites, the famous Port Askaig Tillite (possible “Snowball Earth”?), low grade metamorphic Dalradian rocks retaining original sedimentary structures, reactivated and reversed extensional faults, substantial mineralisation, 60 Ma igneous intrusions (opening of the Atlantic Ocean) and a large selection of Quaternary Ice Age features.