Abstract
The Southern Uplands form a tract of rolling, dissected tableland, underlain by steeply dipping sedimentary and metasedimentary rocks of Ordovician and Silurian age, into which several granitic plutons were intruded during the Devonian. The landscape is one of selective glacial erosion, but the effects of successive Pleistocene glaciations are muted: deep glacial troughs and cirques are largely restricted to the Galloway Hills in the southwest and the Tweedsmuir Hills in the centre of the region. Moraines are mainly limited to those deposited by Loch Lomond Stadial glaciers in the same areas, but meltwater channels are widespread and outwash terraces deposited during retreat of the last ice sheet flank the floodplains of both trunk and tributary rivers. Frost-weathered regolith covers summits and plateaux, suggesting that these were occupied by cold-based glacier ice during the last glacial cycle. Lateglacial solifluction of regolith and till has produced smooth valley-side slopes and contributed to the accumulation of periglacial valley fills; active solifluction is represented by lobes and ploughing boulders on some of the highest ground. Rock-slope failures occur mainly in clusters and exhibit a variety of forms conditioned by the underlying geological structure and lithology. There is evidence that settlement expansion and associated land-use impacts have caused gullying of hillslopes during the Late Holocene, resulting in the deposition of alluvial fans and debris cones, and transient floodplain aggradation due to increased sediment supply to rivers.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Similar content being viewed by others
References
Ballantyne CK (2001) The sorted stone stripes of Tinto Hill. Scot Geogr J 117:313–324
Ballantyne CK (2018) Periglacial geomorphology. Wiley, Chichester
Ballantyne CK (2019) After the ice: Lateglacial and Holocene landforms and landscape evolution in Scotland. Earth Env Sci Trans R Soc Edinb 110:133–171
Ballantyne CK, Harris C (1994) The periglaciation of Great Britain. Cambridge University Press, Cambridge
Ballantyne CK, Small D (2019) The last Scottish Ice Sheet. Earth Env Sci Trans R Soc Edinb 110:93–131
Ballantyne CK, Rinterknecht V, Gheorghiu DM (2013) Deglaciation chronology of the Galloway Hills ice centre, SW Scotland. J Quat Sci 28:412–420
Bishop WW, Coope GR (1977) Stratigraphical and faunal evidence for Lateglacial and early Flandrian environments in south-west Scotland. In: Gray JM, Lowe JJ (eds) Studies in the Scottish Lateglacial environment. Pergamon, Oxford, pp 61–88
Brooks SJ, Birks HJB (2000) Chironomid-inferred late-glacial air temperatures at Whitrig Bog, south-east Scotland. J Quat Sci 15:759–764
Chiverrell RC, Harvey AM, Foster GC (2007) Hillslope gullying in the Solway Firth—Morecambe Bay region, Great Britain: responses to human impact and/or climate deterioration? Geomorphology 84:317–343
Chiverrell RC, Smedley RK, Small D et al (2018) Ice margin oscillations during deglaciation of the northern Irish Sea Basin. J Quat Sci 33:739–762
Clark CD, Hughes ALC, Greenwood SL et al (2012) Pattern and timing of retreat of the last British-Irish Ice Sheet. Quat Sci Rev 44:112–146
Cornish R (1981) Glaciers of the Loch Lomond Stadial in the western Southern Uplands of Scotland. Proc Geol Assoc 92:105–114
Cornish R (1982) Glacier flow at a former ice divide in SW Scotland. Trans R Soc Edinb: Earth Sci 73:31–41
Cornish R (1983) Glacial erosion in an ice-divide zone. Nature 301:413–415
Evans DJA (2004) Classics in Scottish physical geography revisited: Sissons JB (1958) Supposed ice-dammed lakes in Britain with particular reference to the Eddleston Valley, southern Scotland. Scot Geogr J 120:219–226
Evans DJA, Livingstone SJ, Vieli A, Ó Cofaigh C (2009) The palaeoglaciology of the central sector of the British-Irish Ice Sheet: reconciling glaciology and preliminary ice-sheet modelling. Quat Sci Rev 28:739–757
Everest JD, Bradwell T, Golledge NR (2005) Subglacial landforms of the Tweed palaeo-ice stream. Scot Geogr J 121:163–173
Fabel D, Ballantyne CK, Xu S (2012) Trimlines, blockfields, mountain-top erratics and the vertical dimensions of the last British-Irish Ice Sheet in NW Scotland. Quat Sci Rev 55:91–102
Foster GC, Chiverrell RC, Harvey AM et al (2008) Catchment hydro-geomorphological responses to environmental change in the Southern Uplands of Scotland. The Holocene 18:935–950
Harrison S (2002) Lithological variability of Quaternary slope deposits in the Cheviot Hills, UK. Proc Geol Assoc 113:121–138
Harrison S, Bailey RM, Anderson E et al (2010) Optical dates from British Isles ‘solifluction sheets’ suggest rapid landscape response to Late Pleistocene climate change. Scot Geogr J 126:101–111
Hopkinson C, Ballantyne CK (2014) Age and origin of blockfields on Scottish mountains. Scot Geogr J 130:116–141
Livingstone SJ, Evans DJA, Ó Cofaigh C et al (2012) Glaciodynamics of the central sector of the last British-Irish Ice Sheet in northern England. Earth-Sci Rev 111:25–55
Livingstone SJ, Ó Cofaigh C, Evans DJA (2008) Glacial geomorphology of the central sector of the last British-Irish Ice Sheet. J Maps 4:358–377
Livingstone SJ, Roberts DH, Davies BJ et al (2015) Late Devensian deglaciation of the Tyne Gap palaeo-ice stream, northern England. J Quat Sci 30:790–804
Mitchell WA (2008) Quaternary geology of part of the Kale Water catchment, western Cheviot Hills, Scotland. Scot J Geol 44:51–63
Pearce D (2014) Reconstruction of Younger Dryas glaciation in the Tweedsmuir Hills, Southern Uplands, Scotland: style, dynamics and palaeo-climatic implications. PhD thesis, University of Worcester
Pearce D, Rea BR, Bradwell T, McDougall D (2014) Glacial geomorphology of the Tweedsmuir Hills, central Southern Uplands, Scotland. J Maps 10:457–465
Price RJ (1960) Glacial meltwater channels in the upper Tweed basin. Geogr J 126:483–489
Ragg JM, Bibby JS (1966) Frost weathering and solifluction products in southern Scotland. Geogr Annlr 48A:12–23
Salt KE, Evans DJA (2004) Superimposed subglacial streamlined landforms of southwest Scotland. Scot Geogr J 120:133–147
Sissons JB (1958) Supposed ice-dammed lakes in Britain with particular reference to the Eddleston Valley, southern Scotland. Geogr Annlr 40:159–187
Sissons JB (1961) A subglacial drainage system by the Tinto Hills, Lanarkshire. Trans Edinb Geol Soc 18:175–193
Stone P, McMillan AA, Floyd JD et al (2012) British regional geology: south of Scotland. British Geological Survey, 4th edn. Keyworth
Tipping R (1992) The determination of cause in the generation of major prehistoric valley fills in the Cheviot Hills, Anglo-Scottish border. In: Needham S, Macklin MG (eds) Alluvial archaeology in Britain: Oxbow Monograph 27. Oxbow Books, Oxford, pp 111–121
Tipping R (1994) Fluvial chronology and valley floor evolution of the upper Bowmont Valley, Borders Region, Scotland. Earth Surf Proc Landf 19:641–657
Tipping R, Halliday SP (1994) The age of alluvial fan deposition at a site in the Southern Uplands of Scotland. Earth Surf Proc Landf 19:333–348
Tipping R, Milburn P, Halliday S (1999) Fluvial processes and land-use change 2000 years ago in upper Annandale, southern Scotland. In: Brown AG, Quine TA (eds) Fluvial processes and environmental change. Wiley, Chichester, pp 311–327
Wilson P (1993) Ploughing boulder characteristics and associated soil properties in the Lake District and southern Scotland. Scot Geogr J 109:18–26
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2021 Springer Nature Switzerland AG
About this chapter
Cite this chapter
Ballantyne, C.K. (2021). Upland Landscapes and Landforms of the Southern Uplands. In: Ballantyne, C.K., Gordon, J.E. (eds) Landscapes and Landforms of Scotland. World Geomorphological Landscapes. Springer, Cham. https://doi.org/10.1007/978-3-030-71246-4_27
Download citation
DOI: https://doi.org/10.1007/978-3-030-71246-4_27
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-030-71245-7
Online ISBN: 978-3-030-71246-4
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)