Nunataks of the last ice sheet in northwest Scotland

• Published in: Boreas
• Main Authors: McCARROLL, DANNY, BALLANTYNE, COLIN K., NESJE, ATLE, DAHL, SVEIN‐OLAF
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 1995
• Subjects: Ice Sheet
• Online Access: http://dx.doi.org/10.1111/j.1502-3885.1995.tb00782.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1995.tb00782.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1995.tb00782.x

High‐level weathering limits separating ice‐scoured topography from an upper zone of frost‐weathered detritus were identified on 17 mountains in NW Scotland at altitudes of <600 m to< 900 m, and a further 6 peaks were found to support evidence of ice scouring to summit level. Weathering limits are most clearly defined on Torridon Sandstone, which is resistant to frost shattering, but can also be mapped on Cambrian Quartzite, Lewisian Gneiss and Moine Schist. Contrasts in degree of rock surface weathering above and below the weathering limits were evaluated using measurements of joint depth and rock surface hardness, and through X‐ray diffraction analyses of clay mineral assemblages. The results indicate significantly more advanced rock and soil weathering above the weathering limits. Widespread persistence of gibbsite above the weathering limits suggests that they represent the upper limit of Late Devensian glacial erosion, and the regularity of the decline in weathering limit altitude along former flowlines eliminates the possibility that it represents a former thermal boundary between protective cold‐based and erosive warm‐based ice. The weathering limits are therefore interpreted as periglacial trimlines defining the maximum surface altitude of the last ice sheet around former nunataks. Calculated basal shear stresses of 50–78 kPa are consistent with this interpretation. The altitude of the trimlines implies that the former ice shed lay at 900–930 m in the Fannich Mountains and descended gently northwards, and that the ice surface descended NW from the ice shed to >500 m over the extreme NW tip of Scotland and to 700–730 m at the head of Little Loch Broom.