Enhanced rock-slope failure following ice-sheet deglaciation:timing and causes

• Published in: Earth Surface Processes and Landforms
• Main Authors: Ballantyne, Colin, Wilson, Peter, Gheorghiu, Delia, Rodés, Àngel
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2014
• Subjects: rock-slope failure; paraglacial; surface exposure dating; stress release; palaeoseismicity; Jura; Loch Lomond; Ice; Ice Sheet; permafrost
• Online Access: https://risweb.st-andrews.ac.uk/portal/en/researchoutput/enhanced-rockslope-failure-following-icesheet-deglaciation(17dcf600-9fb3-4bcb-be8c-456895d8106d).html; https://doi.org/10.1002/esp.3495; https://research-repository.st-andrews.ac.uk/bitstream/10023/5839/1/Ballantyne_2014_ESPL_Enhanced.pdf

The temporal pattern of rock-slope failures (RSFs) following Late Pleistocene deglaciation on tectonically stable terrains is controversial: previous studies variously suggest (1) a rapid response due to removal of supporting ice (‘debuttressing’), (2) a progressive decline in RSF frequency, and (3) a millennial-scale delay before peak RSF activity. We test these competing models through beryllium-10 (10Be) exposure dating of five closely-spaced quartzite RSFs on the Isle of Jura, Scotland, to establish the relationship between timing of failure and those of deglaciation, episodes of rapid warming and periods of rapid glacio-isostatic uplift. All five dated RSFs occurred at least 720–2240 years after deglaciation, with the probability of failure peaking ~2 ka after deglaciation, consistent with millennial-scale delay model (3). This excludes debuttressing as an immediate cause of failure, though it is likely that time-dependent stress release due to deglacial unloading resulted in progressive development of failure planes within the rock. Thaw of permafrost ice in joints is unlikely to have been a prime trigger of failure as some RSFs occurred several centuries after the onset of interstadial warming. Conversely, the timespan of the RSFs coincides with the period of maximum glacio-isostatic crustal uplift, suggesting that failure was triggered by uplift-driven seismic events acting on fractured rock masses. Implications of this and related research are: (1) that retreat of the last Pleistocene ice sheets across tectonically-stable mountainous terrains was succeeded by a period of enhanced rock-slope failure due to deglacial unloading and probably uplift-driven seismicity; (2) that the great majority of RSFs in the British Isles outside the limits of Loch Lomond Stadial (= Younger Dryas) glaciation are of Lateglacial (pre-Holocene) age; and (3) numerous RSFs must also have occurred inside Loch Lomond Stadial (LLS) glacial limits, but that runout debris was removed by LLS glaciers.