Skip to main content

Sarsens—The Maker of Upland Scenery of Southern England: From Mid-Cenozoic Gravel Plains to Neolithic Landscapes

  • Chapter
  • First Online:

Part of the book series: World Geomorphological Landscapes ((WGLC))

Abstract

Sarsens are somewhat enigmatic rocks present in southern England, mainly scattered as boulders of metric dimensions across the Chalk uplands of Wiltshire and Dorset. They are remnants of mid-Cenozoic silcretes and the majority originated due to silicification of primary fluvial and lacustrine deposits, in an environment typified by low relief and general geomorphic stability. The vast majority of sarsens does not occur in situ which limits their value as palaeomorphological indicators. In-valley boulder trains are the most spectacular natural occurrences of sarsens and a few examples from the Marlborough Downs and Dorset Chalklands are presented in more detail. They are interpreted either as a result of solifluction transport from the interfluves and slopes towards the valley floors under periglacial conditions or as remnants of drainage-line silcretes inherited from the mid-Cenozoic. Sarsens were extensively used by Neolithic societies and the famous megalithic structures of Stonehenge, Avebury and others are built of huge sarsen blocks.

This is a preview of subscription content, log in via an institution.

Buying options

Chapter
USD   29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD   169.00
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD   219.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD   219.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Learn about institutional subscriptions

References

  • Ballantyne CK, Harris C (1994) The Periglaciation of great Britain. Cambridge University Press, Cambridge, p 330

    Google Scholar 

  • Cleal R (2011) Avebury. Monuments and landscape. National Trust, Swindon, p 32

    Google Scholar 

  • Curry D (1992) Tertiary. In: Duff PMD, Smith AJ (eds) Geology of England and Wales. Geol Soc, London, pp 389–411

    Google Scholar 

  • Gibbard PL, Lewin J (2003) The history of the major rivers of southern Britain during the Tertiary. J Geol Soc London 160:829–845

    Article  Google Scholar 

  • Goudie AS (1973) Duricrusts in tropical and subtropical landscapes. Clarendon, Oxford, p 174

    Google Scholar 

  • Green CP (1997a) Stonehenge: geology and prehistory. Proc Geol Assoc 108:1–10

    Article  Google Scholar 

  • Green CP (1997b) The provenance of rocks used in the construction of Stonehenge. Proc Brit Acad 92:257–270

    Google Scholar 

  • Green C (2016) The exploitation of silcretes (sarsen and puddingstone) in England and Normandy since Stonehenge. Proc Geol Assoc 127:349–358

    Article  Google Scholar 

  • Hepworth JV (1998) Aspects of the English silcretes and comparison with some Australian occurrences. Proc Geol Assoc 109:271–288

    Article  Google Scholar 

  • Huggett J (2016) Puddingstones and related silcretes of the Anglo-Paris Basin – an overview. Proc Geol Assoc 127:297–300

    Article  Google Scholar 

  • Jones DKC (1980) The Tertiary evolution of south-east England with particular reference to the Weald. In: Jones DKC (ed) The shaping of Southern England. Institute of British Geographers, Spec Publ 11. Academic Press, London, pp 13–47

    Google Scholar 

  • Jones DKC (1999) Evolving models of the Tertiary evolutionary geomorphology of southern England, with special reference to the Chalklands. In: Smith BJ, Whalley WB, Warke PA (eds) Uplift, erosion and stability: perspectives on long-term landscape development. Spec Publ 162. Geol Soc, London, pp 1–23

    Google Scholar 

  • Nash DJ (2004) Silcrete. In: Goudie A (ed) Encyclopedia of geomorphology. Routledge, London, pp 959–960

    Google Scholar 

  • Nash DJ, Shaw PA, Ullyott JS (1998) Drainage-line silcretes of the Middle Kalahari: an analogue for Cenozoic sarsen trains? Proc Geol Assoc 109:241–254

    Article  Google Scholar 

  • Pain CF, Ollier CD (1995) Inversion of relief—a component of landscape evolution. Geomorphology 12:151–165

    Article  Google Scholar 

  • Parker Pearson M (2016) The sarsen stones of Stonehenge. Proc Geol Assoc 127:363–369

    Article  Google Scholar 

  • Pollard J, Reynolds A (2002) Avebury. The biography of a landscape. Tempus, Stroud, p 288

    Google Scholar 

  • Small RJ (1980) The Tertiary geomorphological evolution of south-east England: an alternative interpretation. In: Jones DKC (ed) The shaping of Southern England. Institute of British Geographers, Spec Publ 11. Academic Press, London, pp 49–70

    Google Scholar 

  • Small RJ, Clark MJ, Lewin J (1970) The periglacial rock-stream at Clatford Bottom, Marlborough Downs, Wiltshire. Proc Geol Assoc 81:87–98

    Article  Google Scholar 

  • Summerfield MA, Goudie AS (1980) The sarsens of southern England: their palaeoenvironmental interpretation with reference to other silcretes. In: Jones DKC (ed) The shaping of Southern England, vol 11. Institute of British Geographers, Spec Publ. Academic Press, London, pp 71–100

    Google Scholar 

  • Summerfield MA, Whalley WB (1980) Petrographic investigations of sarsens (Cainozoic silcretes) from southern England. Geol Mijnb 59:145–153

    Google Scholar 

  • Thiry M (1999) Diversity of continental silicification features: examples from the Cenozoic deposits in the Paris Basin and neighbouring basement. In: Thiry M, Simon-Coinçon R (eds) Palaeoweathering, Palaeosurfaces and related continental deposits, vol 27. Int Assoc Sedimentol Spec Publ, Blackwell, Oxford, pp 87–127

    Google Scholar 

  • Ullyott JS, Nash DJ (2016) Distinguishing pedogenic and non-pedogenic silcretes in the landscape and geological record. Proc Geol Assoc 127:311–319

    Article  Google Scholar 

  • Ullyott JS, Nash DJ, Shaw PA (1998) Recent advances in silcrete research and their implications for the origin and palaeoenvironmental significance of sarsens. Proc Geol Assoc 109:255–270

    Article  Google Scholar 

  • Ullyott JS, Nash DJ, Whiteman CA, Mortimore RN (2004) Distribution, petrology and mode of development of silcretes (Sarsens and Puddingstones) on the eastern South Downs, UK. Earth Surf Proc Landf 29:1509–1539

    Article  Google Scholar 

  • Whalley WB, Chartres C (1976) Preliminary observations on the origin and sedimentological nature of sarsen stones. Geol Mijnb 55:68–72

    Google Scholar 

  • Worsley P (2019) Geology of the Clatford Bottom catchment and its sarsen stones on the Marlborough Downs. Mercian Geol 19:242–252

    Google Scholar 

Download references

Acknowledgements

I am grateful to Filip Duszyński who executed all line diagrams accompanying this chapter.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Piotr Migoń .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2020 Springer Nature Switzerland AG

About this chapter

Check for updates. Verify currency and authenticity via CrossMark

Cite this chapter

Migoń, P. (2020). Sarsens—The Maker of Upland Scenery of Southern England: From Mid-Cenozoic Gravel Plains to Neolithic Landscapes. In: Goudie, A., Migoń, P. (eds) Landscapes and Landforms of England and Wales. World Geomorphological Landscapes. Springer, Cham. https://doi.org/10.1007/978-3-030-38957-4_18

Download citation

Publish with us

Policies and ethics