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After the ice: Lateglacial and Holocene landforms and landscape evolution in Scotland

Published online by Cambridge University Press:  15 May 2018

Colin K. BALLANTYNE
Colin K. BALLANTYNE*
Affiliation:
School of Geography and Sustainable Development, University of St Andrews, St Andrews KY16 9AL, UK.
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Abstract

During Lateglacial cold periods, permafrost developed throughout Scotland, sediment-mantled slopes were extensively modified by solifluction and other forms of periglacial mass movement, large-scale sorted patterned ground formed on plateaux, and enhanced rockfall resulted in talus accumulation below cliffs. Most rock-slope failures occurred within five millennia following ice-sheet deglaciation, with many probably triggered by uplift-induced earthquakes; numerous debris-free scarps represent sites where Lateglacial rockslide debris was excavated by glaciers during the Younger Dryas Stade (∼12.9–11.7 ka). Sandar and outwash fans deposited by glacial rivers during ice-sheet retreat were incised to form high-level terraces. Under the cool temperate but relatively stable climate of the Holocene, solifluction and patterned ground formation continued to operate on high ground, though accumulation of high-level aeolian deposits on most mountains was terminated by erosion during the Little Ice Age. Drift-mantled slopes and talus slopes have been extensively eroded by translational failures and debris flows, the latter depositing debris cones on upland valley floors. The incidence of Holocene rockslides has been much lower than during the Lateglacial period. Dating of alluvial deposits and low Holocene terraces suggests no consistent pattern of Holocene floodplain evolution: incision has apparently dominated in the Highlands, aggradation in the lowlands, and floodplains in the Southern Uplands have asynchronous histories of incision and aggradation. Studies of floodplain behaviour over the past 200–300 years suggest that though major floods rework the floodplains of braided and piedmont rivers, there is no tendency towards net floodplain aggradation or incision. Most valley-side alluvial fans accumulated episodically in the last 4000 years, many in response to lowering of hillslope stability by woodland clearance. For many postglacial landsystems, disentangling the effects of declining paraglacial sediment supply, climate change and local influences (extreme rainstorm events or anthropogenic impacts) remains challenging.

Keywords

alluvial fandebris flowfloodplainparaglacialperiglacialpermafrostpostglacialrock-slope failuretalusterraces
Type
Articles
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 110 , Issue 1-2: Advances in Scottish Quaternary Studies , March 2019 , pp. 133 - 171
Copyright
Copyright © The Royal Society of Edinburgh 2018 

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References

8. References

Acreman, M. C. 1983. The significance of the flood of September 1981 on the Ardessie Burn, Wester Ross. Scottish Geographical Magazine 100, 37–49.Google Scholar
Acreman, M. C. 1991. The flood of July 25th 1983 on the Hermitage Water, Roxburghshire. Scottish Geographical Magazine 107, 170–178.Google Scholar
Addy, S., Soulsby, C., Hartley, A. J. & Tetzlaff, D. 2011. Characterization of channel reach morphology and associated controls in deglaciated montane catchments in the Cairngorms, Scotland. Geomorphology 132, 176–186.Google Scholar
Addy, S., Soulsby, C. & Hartley, A. J. 2014. Controls on the distribution of channel reach morphology in selectively glaciated catchments. Geomorphology 211, 121–133.Google Scholar
Aitken, J. F. 1990. Glaciolacustrine deposits in Glen Nochty, Grampian Region, Scotland, UK. Quaternary Newsletter 60, 13–20.Google Scholar
Aitken, J. F. 1995. Lithofacies and depositional history of a Late Devensian ice-contact deltaic complex, northeast Scotland. Sedimentary Geology 99, 111–130.Google Scholar
Aitken, J. F. 1998. Sedimentology of Late Devensian glaciofluvial outwash in the Don Valley, Grampian Region. Scottish Journal of Geology 34, 97–117.Google Scholar
Andrieux, E., Bertran, P. & Saito, K. 2016. Spatial analysis of French Pleistocene permafrost by a GIS database. Permafrost and Periglacial Processes 27, 17–30.Google Scholar
Atkinson, T. C., Briffa, K. R. & Coope, G. R. 1987. Seasonal temperatures in Britain during the past 22,000 years, reconstructed using beetle remains. Nature 325, 587–592.Google Scholar
Auton, C. A. 1990. The middle Findhorn valley. In Auton, C. A., Firth, C. R. & Merritt, J. W. (eds) Beauly to Nairn: Field Guide, 74–96. Coventry: Quaternary Research Association.Google Scholar
Auton, C. A. & Crofts, R. G. 1986. The sand and gravel resources of the country around Aberdeen, Grampian Region. British Geological Survey Mineral Assessment Report 146.Google Scholar
Balco, G., Stone, J. O., Lifton, N. A. & Dunai, T. J. 2008. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be or 26Al measurements. Quaternary Geochronology 3, 174–195.Google Scholar
Ballantyne, C. K. 1984. The Late Devensian periglaciation of upland Scotland. Quaternary Science Reviews 3, 311–343.Google Scholar
Ballantyne, C. K. 1985. Nivation landforms and snowpatch erosion on two massifs in the Northern Highlands of Scotland. Scottish Geographical Magazine 101, 40–49.Google Scholar
Ballantyne, C. K. 1986a. Nonsorted patterned ground on mountains in the Northern Highlands of Scotland. Biuletyn Peryglacjalny 30, 15–34.Google Scholar
Ballantyne, C. K. 1986b. Landslides and slope failures in Scotland: a review. Scottish Geographical Magazine 102, 134–150.Google Scholar
Ballantyne, C. K. 1986c. Late Flandrian solifluction on the Fannich Mountains, Ross-shire. Scottish Journal of Geology 22, 395–406.Google Scholar
Ballantyne, C. K. 1987. The present-day periglaciation of upland Britain. In Boardman, J. (ed.) Periglacial Processes and Landforms in Britain and Ireland, 113–116. Cambridge: Cambridge University Press. 308 pp.Google Scholar
Ballantyne, C. K. 1989. Avalanche impact landforms on Ben Nevis, Scotland. Scottish Geographical Magazine 105, 38–42.Google Scholar
Ballantyne, C. K. 1991. Late Holocene erosion in upland Britain: climatic deterioration or human influence? The Holocene 1, 81–85.Google Scholar
Ballantyne, C. K. 1994. The tors of the Cairngorms. Scottish Geographical Magazine 110, 54–59.Google Scholar
Ballantyne, C. K. 1996. Formation of miniature sorted patterns by shallow ground freezing: a field experiment. Permafrost and Periglacial Processes 7, 409–424.Google Scholar
Ballantyne, C. K. 1997. The periglacial geomorphology of Scotland. In Gordon, J. E. (ed.) Reflections on the Ice Age in Scotland: an update on Quaternary studies, 166–178. Glasgow: Scottish Association of Geography Teachers and Scottish Natural Heritage. 188 pp.Google Scholar
Ballantyne, C. K. 1998a. Age and significance of mountain-top detritus. Permafrost and Periglacial Processes 9, 327–345.Google Scholar
Ballantyne, C. K. 1998b. Aeolian deposits on a Scottish mountain summit: characteristics, provenance, history and significance. Earth Surface Processes and Landforms 23, 625–641.Google Scholar
Ballantyne, C. K. 2001a. The sorted stone stripes of Tinto Hill. Scottish Geographical Journal 117, 313–324.Google Scholar
Ballantyne, C. K. 2001b. Measurement and theory of ploughing boulder movement. Permafrost and Periglacial Processes 12, 267–288.Google Scholar
Ballantyne, C. K. 2002a. Paraglacial geomorphology. Quaternary Science Reviews 21, 1935–2017.Google Scholar
Ballantyne, C. K. 2002b. A general model of paraglacial landscape response. The Holocene 12, 371–376.Google Scholar
Ballantyne, C. K. 2002c. Debris flow activity in the Scottish Highlands: temporal trends and wider implications for dating. Studia Geomorphologica Carpatho-Balcanica 36, 7–27.Google Scholar
Ballantyne, C. K. 2003a. Paraglacial landform succession and sediment storage in deglaciated mountain valleys: theory and approaches to calibration. Zeitschrift für Geomorphologie, Supplementband 132, 1–18.Google Scholar
Ballantyne, C. K. 2003b. A Scottish sturzstrom: the Beinn Alligin rock avalanche. Scottish Geographical Journal 119, 159–167.Google Scholar
Ballantyne, C. K. 2007a. Trotternish Escarpment, Isle of Skye, Highland (NG450717–NG 481 494). In Cooper, R. G. (ed.) Mass Movements in Great Britain. Geological Conservation Review Series 33, 196–204. Peterborough: Joint Nature Conservation Committee.Google Scholar
Ballantyne, C. K. 2007b. Coire Gabhail, Highland (NN 166 557). In Cooper, R. G. (ed.) Mass Movements in Great Britain. Geological Conservation Review Series 33, 132–136. Peterborough: Joint Nature Conservation Committee.Google Scholar
Ballantyne, C. K. 2008. After the ice: Holocene geomorphic activity in the Scottish Highlands. Scottish Geographical Journal 124, 8–52.Google Scholar
Ballantyne, C. K. 2010a. Extent and deglacial chronology of the last British-Irish Ice Sheet: implications of exposure dating using cosmogenic isotopes. Journal of Quaternary Science 25, 515–534.Google Scholar
Ballantyne, C. K. 2010b. A general model of autochthonous blockfield evolution. Permafrost and Periglacial Processes 21, 289–300.Google Scholar
Ballantyne, C. K. 2012. Chronology of glaciation and deglaciation during the Loch Lomond (Younger Dryas) Stade in the Scottish Highlands: implications of recalibrated 10Be exposure ages. Boreas 41, 513–526.Google Scholar
Ballantyne, C. K. 2013a. Paraglacial geomorphology. In Elias, S. A. & Mock, C. J. (eds) Encyclopedia of Quaternary Science, Second Edition, Volume 3, 553–565. Amsterdam: Elsevier. 3888 pp.Google Scholar
Ballantyne, C. K. 2013b. Patterned Ground. In Elias, S. A. & Mock, C. J. (eds) Encyclopedia of Quaternary Science, Second Edition, Volume 3, 452–463. Amsterdam: Elsevier. 3888 pp.Google Scholar
Ballantyne, C. K. 2013c. Lateglacial rock-slope failures in the Scottish Highlands. Scottish Geographical Journal 129, 67–84.Google Scholar
Ballantyne, C. K. 2013d. A 35-year record of solifluction in a maritime periglacial environment. Permafrost and Periglacial Processes 24, 56–66.Google Scholar
Ballantyne, C. K. 2017. Periglacial Geomorphology. Chichester: Wiley. 472 pp.Google Scholar
Ballantyne, C. K., Stone, J. O. & Fifield, L. K. 1998. Cosmogenic Cl-36 dating of postglacial landsliding at the Storr, Isle of Skye, Scotland. The Holocene 8, 347–351.Google Scholar
Ballantyne, C. K., Schnabel, C. & Xu, S. 2009. Exposure dating and reinterpretation of coarse debris accumulations (‘rock glaciers') in the Cairngorm Mountains, Scotland. Journal of Quaternary Science 24, 19–31.Google Scholar
Ballantyne, C. K., Sandeman, G. F., Stone, J. O. & Wilson, P. 2014a. Rock-slope failure following Late Pleistocene deglaciation on tectonically stable mountainous terrain. Quaternary Science Reviews 86, 144–157.Google Scholar
Ballantyne, C. K., Wilson, P., Gheorghiu, D. & Rodés, À. 2014b. Enhanced rock-slope failure following ice-sheet deglaciation: timing and causes. Earth Surface Processes and Landforms 39, 900–913.Google Scholar
Ballantyne, C. K. & Benn, D. I. 1994. Paraglacial slope adjustment and resedimentation in response to recent glacier retreat, Fåbergstølsbreen, Norway. Arctic and Alpine Research 26, 255–269.Google Scholar
Ballantyne, C. K. & Benn, D. I. 1996. Paraglacial slope adjustment during recent deglaciation and its implications for slope evolution in formerly glaciated environments. In Anderson, M. G. & Brooks, S. (eds) Advances in Hillslope Processes, 1173–1195. Chichester: Wiley. 1340 pp.Google Scholar
Ballantyne, C. K. & Eckford, J. D. 1984. Characteristics and evolution of two relict talus slopes in Scotland. Scottish Geographical Magazine 100, 20–33.Google Scholar
Ballantyne, C. K. & Harris, C. 1994. The Periglaciation of Great Britain. Cambridge: Cambridge University Press, 330 pp.Google Scholar
Ballantyne, C. K. & Kirkbride, M. P. 1986. The characteristics and significance of some Lateglacial protalus ramparts in upland Britain. Earth Surface Processes and Landforms 11, 659–671.Google Scholar
Ballantyne, C. K. & Morrocco, S. M. 2006. The windblown sands of An Teallach. Scottish Geographical Journal 122, 149–159.Google Scholar
Ballantyne, C. K. & Small, D. 2018. The Last Scottish Ice Sheet. Earth and Environmental Science Transactions of the Royal Society of Edinburgh ██, ███–███.Google Scholar
Ballantyne, C. K. & Stone, J. O. 2004. The Beinn Alligin rock avalanche, NW Scotland: cosmogenic 10Be dating, interpretation and significance. The Holocene 14, 461–466.Google Scholar
Ballantyne, C. K. & Stone, J. O. 2009. Rock-slope failure at Baosbheinn, Wester Ross, NW Scotland: age and interpretation. Scottish Journal of Geology 45, 177–181.Google Scholar
Ballantyne, C. K. & Stone, J. O. 2012. Did large ice caps persist on low ground in north-west Scotland during the Lateglacial Interstade? Journal of Quaternary Science 27, 297–306.Google Scholar
Ballantyne, C. K. & Stone, J. O. 2013. Timing and periodicity of paraglacial rock-slope failures in the Scottish Highlands. Geomorphology 186, 150–161.Google Scholar
Ballantyne, C. K. & Whittington, G. W. 1987. Niveo-aeolian sand deposits on An Teallach, Wester Ross, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 78, 51–63.Google Scholar
Ballantyne, C. K. & Whittington, G. W. 1999. Late Holocene alluvial fan formation and floodplain incision, Central Grampian Highlands, Scotland. Journal of Quaternary Science 14, 651–671.Google Scholar
Bateman, M. D. 1995. Thermoluminescence dating of the British coversand deposits. Quaternary Science Reviews 14, 791–798.Google Scholar
Bayfield, N. G. 1984. The dynamics of heather (Calluna vulgaris) stripes in the Cairngorm Mountains, Scotland. Journal of Ecology 72, 515–527.Google Scholar
Benedict, J. B. 1970. Downslope soil movement in a Colorado alpine region: rates, processes and climatic significance. Arctic and Alpine Research 2, 165–226.Google Scholar
Benn, D. I. 1989. Debris transport by Loch Lomond Readvance glaciers in northern Scotland: basin form and the within-valley asymmetry of lateral moraines. Journal of Quaternary Science 4, 243–254.Google Scholar
Benn, D. I. 1992. The genesis and significance of ‘hummocky moraine': evidence from the Isle of Skye, Scotland. Quaternary Science Reviews 11, 781–799.Google Scholar
Bennett, M. R. 1999. Paraglacial and periglacial slope adjustment of a degraded lateral moraine in Glen Torridon. Scottish Journal of Geology 35, 79–83.Google Scholar
Birse, E. L. 1980. Suggested amendments to the world soil classification to accommodate Scottish aeolian and mountain soils. Journal of Soil Science 31, 117–124.Google Scholar
Bishop, P., Hoey, T. B., Jansen, J. D. & Lexartza Artza, I. 2005. Knickpoint recession rate and catchment area: the case of uplifted rivers in Eastern Scotland. Earth Surface Processes and Landforms 30, 767–778.Google Scholar
Blundell, A. & Barber, K. E. 2005. A 2800-year palaeoclimatic record from Tore Hill Moss, Strathspey, Scotland: the need for a multi-proxy approach to peat-based climatic reconstructions. Quaternary Science Reviews 24, 1261–1277.Google Scholar
Boston, C. M. & Lukas, S. 2017. Evidence for restricted Loch Lomond Stadial plateau ice in Glen Turret and implications for the age of the Turret Fan. Proceedings of the Geologists' Association 128, 42–53.Google Scholar
Bradwell, T., Stoker, M. S., Golledge, N. R., Wilson, C. K., Merritt, J. W., Long, D., Everest, J. D., Hestvik, O. B., Stevenson, A. G., Hubbard, A. L., Finlayson, A. G. & Mathers, H. E. 2008. The northern sector of the last British Ice Sheet: maximum extent and demise. Earth-Science Reviews 88, 207–226.Google Scholar
Brazier, V. 1987. Late Quaternary alluvial fans, debris cones and talus cones in the Grampian Highlands, Scotland. Unpublished PhD Thesis, University of St Andrews, UK.Google Scholar
Brazier, V., Whittington, G. W. & Ballantyne, C. K. 1988. Holocene debris cone evolution in Glen Etive, western Grampian Highlands, Scotland. Earth Surface Processes and Landforms 13, 525–531.Google Scholar
Brazier, V., Kirkbride, M. P. & Werritty, A. 1993. The River Clyde-Medwin meanders. Scottish Geographical Magazine 109, 45–59.Google Scholar
Brazier, V., Kirkbride, M. P. & Gordon, J. E. 1998. Active ice-sheet deglaciation and ice-dammed lakes in the northern Cairngorm Mountains, Scotland. Boreas 27, 297–310.Google Scholar
Brazier, V. & Ballantyne, C. K. 1989. Late Holocene debris cone evolution in Glen Feshie, western Cairngorm Mountains, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 80, 17–24.Google Scholar
Briffa, K. R. & Atkinson, T. C. 1997. Reconstructing Late-glacial and Holocene climates. In Hulme, M. & Barrow, E. (eds) Climates of the British Isles: Present, Past and Future, 84–111. London: Routledge. 454 pp.Google Scholar
Bromley, G. R., Putnam, A. E., Rademaker, K. M., Lowell, T. V., Schaefer, J. M., Hall, B., Winckler, G., Birkel, S. D. & Borns, H. W. 2014. Younger Dryas deglaciation of Scotland driven by warming summers. Proceedings of the National Academy of Sciences 111, 6215–6219.Google Scholar
Brooks, S. J., Matthews, I. P., Birks, H. H. & Birks, H. J. B. 2012. High resolution Lateglacial and early-Holocene summer air temperature records from Scotland inferred from chironomid assemblages. Quaternary Science Reviews 41, 67–82.Google Scholar
Brooks, S. J. & Birks, H. J. B. 2000. Chironomid-inferred late-glacial air temperatures at Whitrig Bog, south-east Scotland. Journal of Quaternary Science 15, 759–764.Google Scholar
Brooks, S. M., Anderson, M. G. & Collinson, A. J. C. 1995. Modelling the role of climate, vegetation and pedogenesis in shallow translational hillslope failure. Earth Surface Processes and Landforms 20, 231–242.Google Scholar
Brown, A. G., Keough, M. K. & Rice, J. 1994. Floodplain evolution in the East Midlands, United Kingdom: the lateglacial and Flandrian alluvial record from the Soar and Nene Valleys. Philosophical Transactions of the Royal Society, London 348A, 261–293.Google Scholar
Bryant, R. H. & Carpenter, C. P. 1987. Ramparted ground ice depressions in Britain and Ireland. In Boardman, J. (ed.) Periglacial Processes and Landforms in Britain and Ireland, 183–190. Cambridge: Cambridge University Press. 308 pp.Google Scholar
Castillo, M., Bishop, P. & Jansen, J. D. 2013. Knickpoint retreat and transient bedrock channel morphology triggered by base-level fall in small bedrock river catchments: the case of the Isle of Jura, Scotland. Geomorphology , 1–9.Google Scholar
Cave, J. A. S. & Ballantyne, C. K. 2016. Catastrophic rock-slope failures in NW Scotland: quantitative analysis and implications. Scottish Geographical Journal 132, 185–209.Google Scholar
Chandler, R. J., Kellaway, G. A., Skempton, A. W. & Wyatt, R. J. 1976. Valley slope sections in Jurassic strata near Bath, Somerset. Philosophical Transactions of the Royal Society, London, Series A 283, 527–556.Google Scholar
Chiverrell, R. C., Harvey, A. M. & Foster, G. C. 2007. Hillslope gullying in the Solway Firth – Morecambe Bay region, Great Britain: responses to human impact and/or climate deterioration? Geomorphology 84, 317–343.Google Scholar
Christiansen, H. H. 2004. Windpolished boulders and bedrock in the Scottish Highlands: evidence and implications of Late Devensian wind activity. Boreas 33, 82–94.Google Scholar
Church, M., Kellerhals, R. & Day, T. J. 1989. Regional clastic sediment yield in British Columbia. Canadian Journal of Earth Sciences 26, 31–45.Google Scholar
Church, M., Wolcott, J. & Maizels, J. 1990. Palaeovelocity: a parsimonious proposal. Earth Surface Processes and Landforms 15, 475–480.Google Scholar
Church, M. & Slaymaker, O. 1989. Disequilibrium of Holocene sediment yield in glaciated British Columbia. Nature 337, 452–454.Google Scholar
Clark, C. D., Hughes, A. L. C., Greenwood, S. L., Jordan, C. & Sejrup, H. P. 2012. Pattern and timing of retreat of the last British-Irish Ice Sheet. Quaternary Science Reviews 44, 112–146.Google Scholar
Connell, E. R. & Hall, A. M. 1987. The periglacial history of Buchan, north east Scotland. In Boardman, J. (ed.) Periglacial Processes and Landforms in Britain and Ireland, 277–285. Cambridge: Cambridge University Press. 308 pp.Google Scholar
Cornish, R. 2017. The gravel fans of upper Glen Roy, Lochaber, Scotland: their importance for understanding glacial, proglacial and glaciolacustrine dynamics during the Younger Dryas cold period in an Atlantic margin setting. Proceedings of the Geologists' Association 128, 83–109.Google Scholar
Curry, A. M. 1999a. Paraglacial modification of drift-mantled hillslopes. Unpublished PhD Thesis, University of St Andrews, UK.Google Scholar
Curry, A. M. 1999b. Paraglacial modification of slope form. Earth Surface Processes and Landforms 24, 1213–1228.Google Scholar
Curry, A. M. 2000a. Holocene reworking of drift-mantled hillslopes in the Scottish Highlands. Journal of Quaternary Science 15, 529–541.Google Scholar
Curry, A. M. 2000b. Holocene reworking of drift-mantled hillslopes in Glen Docherty, Northwest Highlands, Scotland. The Holocene 10, 509–518.Google Scholar
Curry, A. M. & Morris, C. J. 2004. Lateglacial and Holocene talus slope development and rockwall retreat on Mynydd Du, UK. Geomorphology 58, 85–106.Google Scholar
Davenport, C. A. & Ringrose, P. S. 1987. Deformation of Scottish Quaternary sediment sequences by strong earthquake motions. Geological Society, London, Special Publications, 29, 299–314.Google Scholar
Dawson, A. G. 2009. So Foul and Fair a Day: a History of Scotland's Weather and Climate. Edinburgh: Birlinn, 230 pp.Google Scholar
Densmore, A. L. & Hovius, N. 2000. Topographic fingerprints of bedrock landslides. Geology 28, 371–374.Google Scholar
Dickson, J. H., Jardine, W. G. & Price, R. J. 1976. Three late-Devensian sites in west-central Scotland. Nature 262, 43–44.Google Scholar
Douglas, T. D. & Harrison, S. 1987. Late Devensian periglacial slope deposits in the Cheviot Hills. In Boardman, J. (ed.) Periglacial Processes and Landforms in Britain and Ireland, 237–244. Cambridge: Cambridge University Press. 308 pp.Google Scholar
Dykes, A. P. & Warburton, J. 2008. Characteristics of the Shetland Islands (UK) peat slides of September 2003. Landslides 5, 213–226.Google Scholar
Everest, J. D. & Kubik, P. W. 2006. The deglaciation of eastern Scotland: cosmogenic 10Be evidence for a Lateglacial stillstand. Journal of Quaternary Science 21, 95–104.Google Scholar
Fabel, D., Ballantyne, C. K. & Xu, S. 2012. Trimlines, blockfields, mountain-top erratics and the vertical dimensions of the last British-Irish Ice Sheet in NW Scotland. Quaternary Science Reviews, 55, 91–102.Google Scholar
Ferguson, R. I. & Ashworth, P. 1991. Slope-induced changes in channel character along a gravel-bed stream: the Allt Dubhaig, Scotland. Earth Surface Processes and Landforms 16, 65–82.Google Scholar
Ferguson, R. I. & Werritty, A. 1983. Bar development and channel changes in the gravelly River Feshie. International Association of Sedimentologists, Special Publication 6, 181–193.Google Scholar
Finlayson, A., Golledge, N., Bradwell, T. & Fabel, D. 2011. Evolution of a Lateglacial mountain icecap in northern Scotland. Boreas 40, 536–554.Google Scholar
Firth, C. R. & Stewart, I. S. 2000. Postglacial tectonics of the Scottish glacio-isostatic uplift centre. Quaternary Science Reviews 19, 1469–1493.Google Scholar
FitzPatrick, E. A. 1956. An indurated soil horizon formed by permafrost. Journal of Soil Science 7, 248–254.Google Scholar
FitzPatrick, E. A. 1969. Some aspects of soil evolution in north-east Scotland. Soil Science 107, 403–408.Google Scholar
FitzPatrick, E. A. 1987. Periglacial features in the soils of north east Scotland. In Boardman, J. (ed.) Periglacial Processes and Landforms in Britain and Ireland, 153–162. Cambridge: Cambridge University Press. 308 pp.Google Scholar
Foster, G. C., Chiverrell, R. C., Harvey, A. M., Dearing, J. A. & Dunsford, H. 2008. Catchment hydro-geomorphological responses to environmental change in the Southern Uplands of Scotland. The Holocene 18, 935–950.Google Scholar
Foulds, S. A. & Macklin, M. G. 2006. Holocene land-use change and its impact on river basin dynamics in Great Britain and Ireland. Progress in Physical Geography 30, 589–604.Google Scholar
Galloway, R. W. 1961. Ice wedges and involutions in Scotland. Biuletyn Peryglacjalny 10, 169–193.Google Scholar
Gemmell, A. M. D. & Ralston, I. B. M. 1984. Some recent discoveries of ice-wedge cast networks in north-east Scotland. Scottish Journal of Geology 20, 115–118.Google Scholar
Gilvear, D. J. & Harrison, D. J. 1991. Channel change and the significance of floodplain stratigraphy: 1990 flood event, Lower River Tay, Scotland. Earth Surface Processes and Landforms 16, 753–761.Google Scholar
Gilvear, D. J. & Winterbottom, S. J. 1992. Channel change and flood events since 1783 on the regulated River Tay, Scotland: implications for flood hazard management. Regulated Rivers: Research and Management 7, 247–260.Google Scholar
Golledge, N. R. 2007. Sedimentology, stratigraphy, and glacier dynamics, western Scottish Highlands. Quaternary Research 68, 79–95.Google Scholar
Golledge, N. R. 2010. Glaciation of Scotland during the Younger Dryas Stadial: a review. Journal of Quaternary Science 25, 550–566.Google Scholar
Golledge, N. R., Hubbard, A. & Sugden, D. E. 2008. High-resolution numerical simulation of Younger Dryas glaciation in Scotland. Quaternary Science Reviews 27, 888–904.Google Scholar
Goodfellow, B. W. 2007. Relict non-glacial surfaces in formerly glaciated landscapes. Earth-Science Reviews 80, 47–73.Google Scholar
Goodfellow, B. W., Skelton, A., Martel, S. J., Stroeven, A. P., Jansson, K. N. & Hättestrand, C. 2014. Controls on tor formation, Cairngorm Mountains, Scotland. Journal of Geophysical Research: Earth Surface 119, F002862.Google Scholar
Gray, J. M. 1975. The Loch Lomond Readvance and contemporaneous sea levels in Loch Etive and neighbouring areas of western Scotland. Proceedings of the Geologists' Association 86, 227–238.Google Scholar
Gray, J. M. & Sutherland, D. G. 1977. The ‘Oban-Ford' moraine: a reappraisal. In Gray, J. M. & Lowe, J. J. (eds) Studies in the Scottish Lateglacial Environment, 33–44. Oxford: Pergamon Press. 212 pp.Google Scholar
Gugliemi, Y. & Cappa, F. 2010. Regional-scale relief evolution and large landslides: insights from geomechanical analyses in the Tinée Valley (southern French Alps). Geomorphology 117, 121–129.Google Scholar
Hall, A. M. 1991. Pre-Quaternary landscape evolution in the Scottish Highlands. Transactions of the Royal Society of Edinburgh: Earth Sciences 82, 1–26.Google Scholar
Hall, A. M., Binnie, S. A., Sugden, D. E., Dunai, T. J. & Wood, C. 2016. Late readvance and rapid final deglaciation of the last ice sheet in the Grampian Mountains, Scotland. Journal of Quaternary Science 31, 869–878.Google Scholar
Hallet, B. 2013. Stone circles: form and soil kinematics. Philosophical Transactions of the Royal Society A371, 20120357.Google Scholar
Harbor, J. & Warburton, J. 1993. Relative rates of glacial and nonglacial erosion in alpine environments. Arctic and Alpine Research 25, 1–7.Google Scholar
Harkness, D. D. & Wilson, H. W. 1979. Scottish Universities Research and Reactor Centre radiocarbon measurements III. Radiocarbon 21, 203–256.Google Scholar
Harris, C. 2013. Slope deposits and forms. In Elias, S. A. & Mock, C. J. (eds) Encyclopedia of Quaternary Science, Second Edition, Volume 3, 481–489. Amsterdam: Elsevier. 3888 pp.Google Scholar
Harris, C., Kern-Luetschg, M., Murton, J. B., Font, M., Davies, M. & Smith, F. 2008. Solifluction processes on permafrost and non-permafrost slopes: results of a large-scale laboratory simulation. Permafrost and Periglacial Processes 19, 359–378.Google Scholar
Harrison, S. 1996. Paraglacial or periglacial? The sedimentology of slope deposits in upland Northumberland. In Anderson, M. G. & Brooks, S. M. (eds) Advances in Hillslope Processes, 1197–1218. Chichester: Wiley. 1340 pp.Google Scholar
Harrison, S. 2002. Lithological variability of Quaternary slope deposits in the Cheviot Hills, U.K. Proceedings of the Geologists' Association 113, 121–138.Google Scholar
Harrison, S., Whalley, W. B. & Anderson, E. 2008. Relict rock glaciers and protalus lobes in the British Isles: implications for Late Pleistocene mountain geomorphology and palaeoclimate. Journal of Quaternary Science 23, 287–304.Google Scholar
Harrison, S., Bailey, R. M., Anderson, E., Arnold, L. & Douglas, T. 2010. Optical dates from British Isles ‘solifluction sheets' suggest rapid landscape response to Late Pleistocene climate change. Scottish Geographical Journal 126, 101–111.Google Scholar
Harrison, S., Rowan, A.V., Glasser, N. F., Knight, J., Plummer, M. A. & Mills, S. C. 2014. Little Ice Age glaciers in Britain: glacier-climate modelling in the Cairngorm Mountains. The Holocene 24, 135–140.Google Scholar
Harvey, A. M. 1986. Geomorphic effects of a 1000-year storm in the Howgill Fells, Northwest England. Zeitschrift für Geomorphologie 30, 71–91.Google Scholar
Hinchliffe, S. 1999. Timing and significance of talus slope reworking, Trotternish, Skye, northwest Scotland. The Holocene 9, 483–494.Google Scholar
Hinchliffe, S., Ballantyne, C. K. & Walden, J. 1998. The structure and sedimentology of relict talus, Trotternish, northern Skye, Scotland. Earth Surface Processes and Landforms 23, 545–560.Google Scholar
Hinchliffe, S. & Ballantyne, C. K. 1999. Talus accumulation and rockwall retreat, Trotternish, Isle of Skye, Scotland. Scottish Geographical Journal 115, 53–70.Google Scholar
Hinchliffe, S. & Ballantyne, C. K. 2009. Talus structure and evolution on sandstone mountains in NW Scotland. The Holocene 19, 477–486.Google Scholar
Hippolyte, J-C., Bourlès, D., Léanni, L., Braucher, R., Chauvet, F. & Lebatard, A. E. 2012. 10Be ages reveal >12 ka of gravitational movement in a major sackung of the western Alps (France). Geomorphology , 139–153.12+ka+of+gravitational+movement+in+a+major+sackung+of+the+western+Alps+(France).+Geomorphology+,+139–153.>Google Scholar
Holmes, G. 1984. Rock slope failure in parts of the Scottish Highlands. Unpublished PhD Thesis, University of Edinburgh, UK.Google Scholar
Hopkinson, C. & Ballantyne, C. K. 2014. Age and origin of blockfields on Scottish mountains. Scottish Geographical Journal 130, 116–141.Google Scholar
Hovius, N. & Meunier, P. 2012. Earthquake-induced landsliding and patterns of seismically-induced landsliding. In Clague, J. J. & Stead, D. (eds) Landslides: Types, Mechanisms and Modelling, 24–36. Cambridge: Cambridge University Press. 436 pp.Google Scholar
Hubbard, A., Bradwell, T., Golledge, N., Hall, A. M., Patton, H., Sugden, D. E., Cooper, R. & Stoker, M. 2009. Dynamic cycles, ice streams and their impact on the extent, chronology and deglaciation of the British-Irish ice sheet. Quaternary Science Reviews 28, 758–776.Google Scholar
Huijzer, B. & Vandenberghe, J. 1998. Climatic reconstruction of the Weichselian Pleniglacial in northwestern and central Europe. Journal of Quaternary Science 13, 391–417.Google Scholar
Huisink, M. 2000. Changing river styles in response to Weichselian climate changes in the Vecht valley, eastern Netherlands. Sedimentary Geology 133, 115–134.Google Scholar
Hutchinson, J. N. 2010. Relict sand wedges in soliflucted London Clay at Wimbledon, London, UK. Proceedings of the Geologists' Association 121, 444–454.Google Scholar
Innes, J. L. 1983. Lichenometric dating of debris-flow deposits in the Scottish Highlands. Earth Surface Processes and Landforms 8, 579–588.Google Scholar
Innes, J. L. 1986. Textural properties of regoliths on vegetated steep slopes in upland regions. Transactions of the Royal Society of Edinburgh: Earth Sciences 77, 241–250.Google Scholar
Isarin, R. F. B. 1997. Permafrost distribution and temperatures in Europe during the Younger Dryas. Permafrost and Periglacial Processes 8, 313–333.Google Scholar
Jansen, J. D., Codilean, A. T., Bishop, P. & Hoey, T. B. 2010. Scale dependence of lithological control on topography: bedrock channel geometry and catchment morphology in Western Scotland. Journal of Geology 118, 223–246.Google Scholar
Jansen, J. D., Fabel, D., Bishop, P., Xu, S., Schnabel, C. & Codilean, A. T. 2011. Does decreasing paraglacial sediment supply slow knickpoint retreat? Geology 39, 543–546.Google Scholar
Jarman, D. 2006. Large rock-slope failures in the Highlands of Scotland: characterisation, causes and spatial distribution. Engineering Geology 83, 161–182.Google Scholar
Jarman, D. 2007. Introduction to the mass movements in the older mountain areas of Great Britain. In Cooper, R. G. (ed.) Mass Movements in Great Britain. Geological Conservation Review Series 33, 33–56. Peterborough: Joint Nature Conservation Committee.Google Scholar
Jarman, D., Wilson, P. & Harrison, S. 2013. Are there any relict rock glaciers in the British mountains? Journal of Quaternary Science 28, 131–143.Google Scholar
Jarman, D. & Ballantyne, C. K. 2002. Beinn Fhada, Kintail: a classic example of paraglacial rock-slope deformation. Scottish Geographical Journal 118, 59–68.Google Scholar
Jenkins, A., Ashworth, P. J., Ferguson, R. I., Grieve, I. C., Rowling, P. & Stott, T. A. 1988. Slope failures in the Ochil Hills, Scotland, November 1984. Earth Surface Processes and Landforms 13, 69–76.Google Scholar
Kääb, A. & Kneisel, C. 2006. Permafrost creep within a recently deglaciated glacier foreland: Muragl, Swiss Alps. Permafrost and Periglacial Processes 17, 79–85.Google Scholar
Kasse, C., Vandenberghe, D., De Corte, F. & Van Den Haute, P. 2007. Late Weichselian fluvio-aeolian sands and coversands of the type locality Grubbenvorst (southern Netherlands): sedimentary environments, climate record and age. Journal of Quaternary Science 22, 695–708.Google Scholar
Kelletat, D. 1970. Rezente Periglazialerscheinungen im Schottischen Hochland. Göttinger Geographische Abhandlungen 51, 67–140.Google Scholar
Kinnard, C. & Lewkowicz, A. G. 2006. Frontal advance of turf-banked solifluction lobes, Kluane Range, Yukon Territory, Canada. Geomorphology 73, 261–276.Google Scholar
Kirkbride, M. P., Everest, J., Benn, D. I., Gheorghiu, D. & Dawson, A. G. 2014. Late-Holocene and Younger Dryas glaciers in the northern Cairngorm Mountains, Scotland. The Holocene 24, 141–148.Google Scholar
Kotarba, A. 1984. Slope features in areas of high relief in maritime climate (with the Island of Rhum as example). Studia Geomorphologica Carpatho-Balcanica 17, 77–88.Google Scholar
Lamb, H. H. 1991. Historic Storms of the North Sea, British Isles and Northwest Europe. Cambridge: Cambridge University Press. 228 pp.Google Scholar
Langdon, D. G. & Barber, K. E. 2005. The climate of Scotland over the last 5000 years inferred from multiproxy peatland records: inter-site correlations and regional variability. Journal of Quaternary Science 20, 549–566.Google Scholar
Lauder, T. D. 1830. An Account of the Great Floods of August 1829 in the Province of Moray and Adjoining Districts. Edinburgh: Adam Black. 316 pp.Google Scholar
Lewkowicz, A. G. 2007. Dynamics of active-layer detachment failures, Fosheim Peninsula, Ellesmere Island, Nunavut, Canada. Permafrost and Periglacial Processes 18, 89–103.Google Scholar
Lewkowicz, A. G. & Harris, C. 2005. Morphology and geotechnique of active-layer detachment failures in discontinuous and continuous permafrost, northern Canada. Geomorphology 69, 275–297.Google Scholar
Lewin, J., Macklin, M. G. & Johnstone, E. 2005. Interpreting alluvial archives: sedimentological factors in the British Holocene alluvial record. Quaternary Science Reviews 24, 1873–1889.Google Scholar
Lewin, J. & Macklin, M. G. 2003. Preservation potential for Late Quaternary river alluvium. Journal of Quaternary Science 18, 107–120.Google Scholar
Lewin, J. & Weir, M. J. C. 1977. Morphology and recent history of the lower Spey. Scottish Geographical Magazine 93, 45–51.Google Scholar
Lowe, J. J., Palmer, A. P., Carter-Champion, A., Macleod, A., Ramirez-Rojas, I. & Timms, R. G. O. 2017. Stratigraphy of a Lateglacial lake basin sediment sequence at Turret Bank, upper Glen Roy, Lochaber: implications for the age of the Turret Fan. Proceedings of the Geologists' Association 128, 110–124.Google Scholar
Luckman, B. H. 1992. Debris flows and snow avalanche landforms in the Lairig Ghru, Cairngorm Mountains, Scotland. Geografiska Annaler 74A, 109–121.Google Scholar
Macklin, M. G., Jones, A. F. & Lewin, J. 2010. River response to rapid Holocene environmental change: evidence and explanation in British catchments. Quaternary Science Reviews 29, 1555–1576.Google Scholar
Macklin, M. G., Lewin, J. & Jones, A. F. 2013. River entrenchment and terrace formation in the UK Holocene. Quaternary Science Reviews 76, 194–206.Google Scholar
MacLeod, A., Palmer, A. P., Lowe, J. J., Rose, J., Bryant, C. & Merritt, J. 2011. Timing of glacier response to Younger Dryas climatic cooling in Scotland. Global and Planetary Change 79, 264–274.Google Scholar
Maizels, J. K. 1983a. Channel changes, palaeohydrology and deglaciation: evidence from some Lateglacial sandur deposits of northeast Scotland. Quaternary Studies in Poland 4, 171–187.Google Scholar
Maizels, J. K. 1983b. Proglacial channel systems: change and thresholds for change over long, intermediate and short time-scales. Special Publications of the International Association of Sedimentologists 6, 251–266.Google Scholar
Maizels, J. K. & Aitken, J. 1991. Palaeohydrological change during deglaciation in upland Britain: a case study from northeast Scotland. In Starkel, L., Gregory, K. J. & Thornes, J. B. (eds) Temperate Palaeohydrology: Fluvial Processes in the Temperate Zone during the last 15,000 years, 105–145. Chichester: Wiley. 568 pp.Google Scholar
Marren, P. M. 2001. Sedimentology of proglacial rivers in eastern Scotland during the Late Devensian. Transactions of the Royal Society of Edinburgh: Earth Sciences 92, 149–171.Google Scholar
Matsuoka, N. 2001. Solifluction rates, processes and landforms: a global review. Earth-Science Reviews 55, 107–134.Google Scholar
Matthews, J. A. & Briffa, K. R. 2005. The ‘Little Ice Age': re-evaluation of an evolving concept. Geografiska Annaler 87A, 17–36.Google Scholar
McColl, S. T. 2012. Paraglacial rock-slope stability. Geomorphology , 1–16.Google Scholar
McEwen, L. J. 1989. River channel changes in response to flooding in the upper River Dee catchment, Aberdeenshire, over the last 200 years. In Beven, K. & Carling, P. (eds) Floods: Hydrological, Sedimentological and Geomorphological Implications, 219–238. Chichester: Wiley. 290 pp.Google Scholar
McEwen, L. J. 1994. Channel pattern adjustment and streampower variations on the middle River Coe, Western Grampian Highlands. Catena 21, 357–374.Google Scholar
McEwen, L. J. 1997. Geomorphological change and fluvial landscape evolution in Scotland during the Holocene. In Gordon, J. E. (ed.) Reflections on the Ice Age in Scotland: an update on Quaternary studies, 116–129. Glasgow: Scottish Association of Geography Teachers and Scottish Natural Heritage. 188 pp.Google Scholar
McEwen, L. J. & Werritty, A. 1988. The hydrology and long-term geomorphic significance of a flash flood in the Cairngorm Mountains, Scotland. Catena 21, 357–374.Google Scholar
McEwen, L. J. & Werritty, A. 2007. ‘The Muckle Spate of 1829': the physical and societal impact of a catastrophic flood on the River Findhorn, Scottish Highlands. Transactions of the Institute of British Geographers 32, 66–89.Google Scholar
Mercier, D. 2011. La Géomorphologie Paraglaciaire. Saarbrücken: Éditions Universitaires Européennes, 256 pp.Google Scholar
Merritt, J. W., Auton, C. A., Connell, E. R., Hall, A. M. & Peacock, J. D. 2003. Cainozoic Geology and Landscape Evolution of North-East Scotland. Edinburgh: Memoir of the British Geological Survey.Google Scholar
Meunier, P., Hovius, N. & Haines, A. J. 2008. Topographic site effects and the location of earthquake-induced landslides. Earth and Planetary Science Letters 275, 221–232.Google Scholar
Milne, F. D., Werritty, A., Davies, M. C. R. & Brown, M. J. 2009. A recent debris flow event and implications for hazard management. Quarterly Journal of Engineering Geology and Hydrogeology 42, 51–60.Google Scholar
Milne, F. D., Brown, M. J. & Werritty, A. 2010. A hazardous channelized debris flow in Glen Ogle, Stirlingshire. Scottish Journal of Geology 46, 181–189.Google Scholar
Milne, F. D., Brown, M. J., Davies, M. C. R. & Cameron, G. 2015. Some key topographic and material controls on debris flows in Scotland. Quarterly Journal of Engineering Geology and Hydrogeology 48, 218–223.Google Scholar
Mitchell, W. A. 2008. Quaternary geology of part of the Kale Water catchment, western Cheviot Hills, Scotland. Scottish Journal of Geology 44, 51–63.Google Scholar
Moore, R., Carey, J., Mills, A., Martin, S., Irinder, S., Kerry, L., Leask, G. & Simmons, A. 2006. Recent landslide impacts on the UK Scottish road network: investigation into the mechanisms, causes and management of landslide risk. In Ashaari, M. (ed.) Proceedings of the International Conference on Slopes, Malaysia, 2006, 223–237. Kuala Lumpur: Public Works Department.Google Scholar
Morrocco, S. M., Ballantyne, C. K., Spencer, J. Q. & Robinson, R. A. J. 2007. Age and significance of aeolian sediment reworking on high plateaux in the Scottish Highlands. The Holocene 17, 349–360.Google Scholar
Mottershead, D. 1978. High altitude solifluction and postglacial vegetation, Arkle, Sutherland. Transactions of the Botanical Society of Edinburgh 43, 17–24.Google Scholar
Murton, J. B. 2013. Ice wedges and ice-wedge casts. In Elias, S. A. & Mock, C. J. (eds) Encyclopedia of Quaternary Science, Second Edition, Volume 3, 436–451. Amsterdam: Elsevier. 3888 pp.Google Scholar
Murton, J. B. & Ballantyne, C. K. 2017. Periglacial and permafrost ground models for Great Britain. Geological Society, London, Engineering Group Special Publications 28, 501–597.Google Scholar
Murton, J. B. & French, H. M. 1993a. Thaw modification of frost–fissure wedges, Richards Island, Pleistocene Mackenzie Delta, western Arctic Canada. Journal of Quaternary Science 8, 185–196.Google Scholar
Murton, J. B. & French, H. M. 1993b. Thermokarst involutions, Summer Island, Pleistocene Mackenzie Delta, western Canadian Arctic. Permafrost and Periglacial Processes 4, 217–229.Google Scholar
Murton, J. B. & Kolstrup, E. 2003. Ice-wedge casts as indicators of palaeotemperatures: precise proxy or wishful thinking? Progress in Physical Geography 27, 155–170.Google Scholar
Nichol, D. 2009. A peat slide at Glenfiddich, East Grampian Highlands. Scottish Journal of Geology 45, 183–186.Google Scholar
Nielsen, P. R., Dahl, S. O., Jansen, H. L. & Støren, E. N. 2016. Holocene aeolian sedimentation and episodic mass-wasting events recorded in lacustrine sediments on Langøya in Vesterålen, northern Norway. Quaternary Science Reviews 148, 146–162.Google Scholar
Palmer, A. P. & Lowe, J. J. 2017. Dynamic landscape changes in Glen Roy and vicinity, west Highland Scotland, during the Younger Dryas and early Holocene: a synthesis. Proceedings of the Geologists' Association 128, 2–25.Google Scholar
Peacock, J. D. 1986. Alluvial fans and an outwash fan in upper Glen Roy, Lochaber. Scottish Journal of Geology 22, 347–366.Google Scholar
Peacock, J. D. & May, F. 1993. Pre-Flandrian slope deformation in the Scottish Highlands: examples from Glen Roy and Glen Gloy. Scottish Journal of Geology 29, 183–189.Google Scholar
Pennington, W., Haworth, E. Y., Bonny, A .P. & Lishman, J. P. 1972. Lake sediments in northern Scotland. Philosophical Transactions of the Royal Society B264, 191–294.Google Scholar
Phillips, W. M., Hall, A. M., Mottram, R., Fifield, L. K. & Sugden, D. E. 2006. Cosmogenic 10Be and 26Al exposure ages of tors and erratics, Cairngorm Mountains, Scotland: timescales for the development of a classic landscape of selective linear erosion. Geomorphology 73, 222–245.Google Scholar
Plug, L. J. & Werner, B. T. 2008. Modelling of ice-wedge networks. Permafrost and Periglacial Processes 19, 63–69.Google Scholar
Reid, E., Thomas, M. F. & Tipping, R. M. 2003. Holocene alluvial fan and fluvial activity in upper Glen Licht, Kintail. In Tipping, R. M. (ed.) The Quaternary of Glen Affric and Kintail: Field Guide, 157–164. London: Quaternary Research Association. 217 pp.Google Scholar
Reid, E. & Thomas, M. F. 2006. A chronostratigraphy of mid- and late-Holocene slope evolution: Creagan a'Chaorainn, Northern Highlands, Scotland. The Holocene 16, 429–444.Google Scholar
Reimer, P. J., Bard, E., Bayliss, A. et al. 2013. IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP. Radiocarbon 55, 1869–1887.Google Scholar
Rhind, D. W. 1969. The Terraces of the Tweed Valley. Unpublished PhD Thesis, University of Edinburgh, UK.Google Scholar
Riddell, K. J. & Fuller, T. W. 1995. The Spey Bay geomorphological study. Earth Surface Processes and Landforms 20, 671–686.Google Scholar
Ringrose, P. S. 1989a. Palaeoseismic (?) liquifaction event in late Quaternary lake sediments at Glen Roy, Scotland. Terra Nova 1, 57–62.Google Scholar
Ringrose, P. S. 1989b. Recent fault movement and palaeoseismicity in western Scotland. Tectonophysics 163, 305–314.Google Scholar
Robertson-Rintoul, M. 1986. A quantitative soil-stratigraphic approach to the correlation and dating of post-glacial river terraces in Glen Feshie, Western Cairngorms. Earth Surface Processes and Landforms 11, 606–617.Google Scholar
Rose, J. 1975. Raised beach gravels and ice-wedge casts at Old Kilpatrick, near Glasgow. Scottish Journal of Geology 11, 15–21.Google Scholar
Rumsby, B., McVey, R. & Brasington, J. 2001. The potential for high resolution fluvial archives in braided rivers: quantifying historic reach-scale channel and floodplain development in the River Feshie, Scotland. In Maddy, D., Macklin, M. G. & Woodward, J. (eds) Basin Sediment Systems: Archives of Environmental Change, 445–467. Rotterdam: Balkema. 530 pp.Google Scholar
Rumsby, B. T., Brasington, J., Langham, J. A., McLelland, S. J., Middleton, R. & Rollinson, G. 2008. Monitoring and modelling particle and reach-scale morphological change in gravel-bed rivers: applications and challenges. Geomorphology 93, 40–54.Google Scholar
Russell, A. J. 1995. Late Devensian meltwater movement and storage within the Ochil Hills, Scotland. Scottish Journal of Geology 31, 65–78.Google Scholar
Russell, A. J., Tweed, F. S. & Harris, T. 2003. High-energy sedimentation, Creag Aoil, Spean Bridge, Scotland: implications for meltwater movement and storage during Loch Lomond Stadial (Younger Dryas) ice retreat. Journal of Quaternary Science 18, 415–430.Google Scholar
Russell, A. J. & Marren, P. W. 1998. A Younger Dryas (Loch Lomond Stadial) jökulhlaup deposit, Fort Augustus, Scotland. Boreas 27, 231–242.Google Scholar
Rydval, M., Loader, N. J., Gunnarson, B. E., Druckenbrod, D. L., Linderholm, H. W., Moreton, S. G., Wood, C. V. & Wilson, R. 2017. Reconstructing 800 years of summer temperatures in Scotland from tree rings. Climate Dynamics 49, 2951–2974.Google Scholar
Salt, K. E. & Ballantyne, C. K. 1997. The structure and sedimentology of relict talus, Knockan, Assynt, NW Scotland. Scottish Geographical Magazine 113, 82–89.Google Scholar
Sanchez, G., Rolland, Y., Corsini, M., Broucher, R., Bourlès, D., Arnold, M. & Aumaître, G. 2010. Relationships between tectonics, slope instability and climate change: cosmic ray exposure dating of active faults, landslides and glacial surfaces in the French Alps. Geomorphology 117, 1–13.Google Scholar
Sissons, J. B. 1977. Former ice-dammed lakes in Glen Moriston, Inverness-shire, and their significance in upland Britain. Transactions of the Institute of British Geographers 2, 224–242.Google Scholar
Sissons, J. B. 1979a. The later lakes and associated fluvial terraces of Glen Roy, Glen Spean and vicinity. Transactions of the Institute of British Geographers 4, 12–29.Google Scholar
Sissons, J. B. 1979b. Catastrophic lake drainage in Glen Spean and the Great Glen, Scotland. Journal of the Geological Society, London 136, 215–224.Google Scholar
Sissons, J. B. 1982. A former ice-dammed lake and associated glacier limits in the Achnasheen area, central Ross-shire. Transactions of the Institute of British Geographers 7, 98–116.Google Scholar
Sissons, J. B. & Cornish, R. 1983. Fluvial landforms associated with ice-dammed lake drainage in upper Glen Roy, Scotland. Proceedings of the Geologists' Association 94, 45–52.Google Scholar
Sletten, K., Blikra, L. H., Ballantyne, C. K., Nesje, A. & Dahl, S. O. 2003. Holocene debris flows recognised in a lacustrine sedimentary succession: sedimentology, chronostratigraphy and cause of triggering. The Holocene 13, 907–990.Google Scholar
Small, D. & Fabel, D. 2016. Was Scotland deglaciated during the Younger Dryas? Quaternary Science Reviews 145, 259–263.Google Scholar
Smith, D. E., Stewart, I. S., Harrison, S. & Firth, C. R. 2009. Late Quaternary neotectonics and mass movement in South East Raasay, Inner Hebrides, Scotland. Proceedings of the Geologists' Association 120, 145–154.Google Scholar
Smith, D. E., Barlow, N. L. M., Bradley, S., Firth, C. R., Hall, A. M., Jordan, J. T. & Long, D. 2018. Quaternary sea level change in Scotland. Earth and Environmental Science Transactions of the Royal Society of Edinburgh ██, ███–███.Google Scholar
Spink, T. W. 1991. Periglacial discontinuities in Eocene Clay near Denham, Buckinghamshire. Geological Society, London, Engineering Geology Special Publications 7, 389–396.Google Scholar
Stewart, I. S., Firth, C. R., Rust, D. J., Collins, P. E. F. & Firth, J. A. 2001. Postglacial fault movement and palaeoseismicity in western Scotland: a reappraisal of the Kinloch Hourn fault, Kintail. Journal of Seismology 6, 307–328.Google Scholar
Strachan, G. J. 2015. Debris flow activity and gully propagation: Glen Docherty, Wester Ross. Scottish Journal of Geology 51, 69–80.Google Scholar
Strachan, G. J. 2017. A peaty-debris flow in Glen Docherty, Wester Ross. Scottish Geographical Magazine 133, 54–68.Google Scholar
Stuiver, M., Reimer, P. J. & Reimer, R. W. 2016. CALIB 7.1. http://calib.org (accessed June 2017).Google Scholar
Sugden, D. E. 1971. The significance of periglacial activity on some Scottish mountains. Geographical Journal 137, 388–392.Google Scholar
Thom, A. S. & Ledger, D. C. 1976. Rainfall, runoff and climatic change. Proceedings of the Institution of Civil Engineers 61, 633–652.Google Scholar
Tipping, R. 1992. The determination of the cause in the generation of major prehistoric valley fills in the Cheviot Hills, Anglo-Scottish border. In Needham, S. & Macklin, M. G. (eds) Alluvial Archaeology in Britain. Oxbow Monograph 27, 111–121. Oxford: Oxbow Books. 280 pp.Google Scholar
Tipping, R. 1994. Fluvial chronology and valley floor evolution of the upper Bowmont Valley, Borders Region, Scotland. Earth Surface Processes and Landforms 19, 641–657.Google Scholar
Tipping, R. 1995a. Holocene landscape change at Carn Dubh, near Pitlochry, Perthshire, Scotland. Journal of Quaternary Science 10, 59–75.Google Scholar
Tipping, R. 1995b. Holocene evolution of a lowland Scottish landscape: Kirkpatrick Fleming. Part III, fluvial history. The Holocene 5, 184–195.Google Scholar
Tipping, R. 1998. The chronology of Late Quaternary fluvial activity in part of the Milfield Basin, northeast England. Earth Surface Processes and Landforms 23, 845–856.Google Scholar
Tipping, R. 1999. Moffat Basin: Holocene fluvial stratigraphy and chronology. In Tipping, R. (ed.) The Quaternary of Dumfries and Galloway: Field Guide, 153–159. London: Quaternary Research Association. 204 pp.Google Scholar
Tipping, R. 2007. Multidisciplinary approaches to defining historic period coastal and fluvial changes at Dunglass Burn, south east Scotland. Scottish Geographical Journal 123, 16–32.Google Scholar
Tipping, R., Carter, S. & Haggart, B. A. 1994. Late Quaternary valley floor evolution in the vicinity of Carradale. Kintyre. Scottish Journal of Geology 30, 131–145.Google Scholar
Tipping, R., Milburn, P. & Halliday, S. 1999. Fluvial processes and land-use change 2000 years ago in upper Annandale, southern Scotland. In Brown, A. G. & Quine, T. A. (eds) Fluvial Processes and Environmental Change, 311–327. Chichester: Wiley. 426 pp.Google Scholar
Tipping, R., Jones, A. P., Carter, S., Holden, T. & Cressey, M. 2008. The chronology and long-term dynamics of a low energy river system: the Kelvin Valley, central Scotland. Earth Surface Processes and Landforms 33, 910–922.Google Scholar
Tipping, R. & Halliday, S. P. 1994. The age of alluvial fan deposition at a site in the Southern Uplands of Scotland. Earth Surface Processes and Landforms 19, 333–348.Google Scholar
Van Vliet, B. & Langohr, R. 1981. Correlations between fragipans and permafrost with special reference to silty Weichselian deposits in Belgium and northern France. Catena 8, 137–154.Google Scholar
Vandenberghe, J. 2003. Climate forcing of fluvial system development: an evolution of ideas. Quaternary Science Reviews 22, 2053–2060.Google Scholar
Vandenberghe, J. 2008. The fluvial cycle at warm–cold–warm transitions in lowland regions: a refinement of theory. Geomorphology 98, 275–284.Google Scholar
Vandenberghe, J. 2013. Cryoturbation structures. In Elias, S. A. & Mock, C. J. (eds) Encyclopedia of Quaternary Science, Second Edition, Volume 3, 430–435. Amsterdam: Elsevier. 3888 pp.Google Scholar
Veyret, Y. & Coque-Delhuille, B. 1993. Réflexions prélimininaires sur les phénomènes catastrophiques affectant la tourbière-couverture aux îles Shetland. Norois 40, 653–664.Google Scholar
Wanner, H., Solomina, O., Grosjean, M., Ritz, S.P. & Jetel, M. 2011. Structure and origin of Holocene cold events. Quaternary Science Reviews 30, 3109–3123.Google Scholar
Ward, R. G. W. 1985. Geomorphological evidence of avalanche activity in Scotland. Geografiska Annaler 67A, 247–256.Google Scholar
Ward, R. G. W., Langmuir, E. D. G. & Beatty, B. 1985. Snow profiles and avalanche activity in the Cairngorm Mountains, Scotland. Journal of Glaciology 31, 18–27.Google Scholar
Watters, R. J. 1972. Slope stability in the metamorphic rocks of the Scottish Highlands. Unpublished PhD Thesis, University of London, UK.Google Scholar
Wells, S. G. & Harvey, A. M. 1987. Sedimentologic and geomorphic variations in storm-generated alluvial fans, Howgill Fells, northwest England. Geological Society of America Bulletin 98, 182–194.Google Scholar
Werritty, A. 1984. Stream response to flash floods in Scotland. In Burt, T. P. & Walling, D. E. (eds) Catchment experiments in Fluvial Geomorphology, 537–560. Norwich: Geobooks. 592 pp.Google Scholar
Werritty, A. & Ferguson, R. I. 1980. Pattern changes on a Scottish braided river over 1, 30 and 200 years. In Cullingford, R. A., Davidson, D. A. & Lewin, J. (eds) Timescales in Geomorphology, 53–68. Chichester: Wiley. 370 pp.Google Scholar
Werritty, A. & Hoey, T. 2003. Geomorphological changes and trends in Scotland: river channels and processes. Scottish Natural Heritage Commissioned Report F00AC107B. 90 pp.Google Scholar
Werritty, A. & Leys, K. 2001. The sensitivity of Scottish rivers and upland valley floors to recent environmental change. Catena 49, 251–273.Google Scholar
Werritty, A. & McEwen, L. J. 1997. The fluvial geomorphology of Scotland. In Gregory, K. J. (ed.) Fluvial Geomorphology of Great Britain. Geological Conservation Review Series 13, 21–32. London: Chapman & Hall.Google Scholar
Whitbread, K., Jansen, J., Bishop, P. & Attal, M. 2015. Substrate, sediment and slope controls on bedrock channel geometry in postglacial streams. Journal of Geophysical Research: Earth Surface 120, 779–798.Google Scholar
Whittington, G. 1985. The Little Ice Age and Scotland's weather. Scottish Geographical Magazine 101, 174–178.Google Scholar
Wilson, P. 1993. Ploughing-boulder characteristics and associated soil properties in the Lake District and southern Scotland. Scottish Geographical Magazine 109, 18–26.Google Scholar
Winter, M. G., Heald, A. P., Parsons, J. A., Macgregor, F. & Shackman, L. 2006. Scottish debris-flow events of August 2004. Quarterly Journal of Engineering Geology and Hydrogeology 39, 73–78.Google Scholar
Winterbottom, S. J. 2000. Medium and short-term channel planform changes on the Rivers Tay and Tummel, Scotland. Geomorphology 34, 195–208.Google Scholar
Worsley, P. 2014. Ice-wedge growth and casting in a Late Pleistocene periglacial, fluvial succession at Baston, Lincolnshire. Mercian Geologist 18, 159–170.Google Scholar
Young, J. A. T. 1976. The terraces of Glen Feshie, Inverness-shire. Transactions of the Royal Society of Edinburgh 69, 501–512.Google Scholar
Young, J. A. T. 1977. Glacial geology of the Dulnain Valley, Inverness-shire. Scottish Journal of Geology 13, 59–74.Google Scholar
Young, J. A. T. 1978. The landforms of upper Strathspey. Scottish Geographical Magazine 94, 76–94.Google Scholar
Zerathe, S., Lebourg, T., Braucher, R. & Bourlès, D. 2014. Mid-Holocene cluster of large-scale landslides revealed in the Southwestern Alps by 36Cl dating. Insight on an Alpine-scale landslide activity. Quaternary Science Reviews 90, 106–127.Google Scholar