Tor (rock formation)

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Birch Tor, on Dartmoor

A tor, which is also known by geomorphologists as either a castle koppie or kopje, is a large, free-standing rock outcrop that rises abruptly from the surrounding smooth and gentle slopes of a rounded hill summit or ridge crest. In the South West of England, the term is commonly also used for the hills themselves – particularly the high points of Dartmoor in Devon and Bodmin Moor in Cornwall.[1]

Name[edit]

Mushroom-shaped tors on Colonels Mountain, Canada (IR Walker 1986)

The word tor (Cornish: tor, Old Welsh: twrr, Welsh: tŵr, Scottish Gaelic: tòrr), meaning hill,[2] is notable for being one of the very few Celtic loanwords to be borrowed into vernacular English before the modern era – such borrowings are mainly words of a geographic or topographical nature. Another word is crag (from Welsh craig "rock").

Formation[edit]

Tors are most common and most well known as a landform that was created by the erosion and weathering of granitic rocks. However, tor have also developed by the erosion and weathering of schists, dacites, dolerites, and coarse sandstones among other rock types. Tors are mostly less than 5 meters (16 ft) high. A variety of hypotheses have been proposed to explain the origin of tors and their origin remains a topic of continuing discussion among geologists and geomorphologists, and physical geographers. It is considered likely that tors were created by geomorphic processes that differed widely in type and duration according to regional and local differences in climate and rock types.[1][3]

For example the Dartmoor granite was emplaced around 280 million years ago, with the cover rocks stripped off soon afterwards, exposing it to chemical and physical weathering processes.[4] Where joints are closely spaced, the large crystals in the granite readily disintegrate to form a sandy regolith known locally as growan. This is readily stripped off by solifluction or surface wash when not protected by vegetation, notably during prolonged cold phases during the Quaternary ice ages - periglaciation. Where joints happen to be unusually widely spaced, core blocks can survive and escape above the weathering surface, developing into tors. These can be monolithic, as at Haytor and Blackingstone Rock, but are more usually subdivided into stacks, often arranged in avenues. Each stack can comprise several tiers or pillows, which may become separated: rocking pillows are called logan stones. These stacks are vulnerable to frost action, often collapsing, with trails of blocks called clitter down the slopes. Weathering has also given rise to circular "rock basins" formed by the accumulation of water and the repeated freezing and thawing – a fine example is to be found at Kes Tor on Dartmoor. Dating of 28 Dartmoor tors shows that most are surprisingly young, less than 100,000 years old, with none over 200,000 years old.[5] They probably emerged at the start of the last big ice age (Devensian). By contrast in the Scottish Cairngorms, the other classic granite tor concentration in Britain, the oldest tors dated are between 200 and 675,000 years old, with even glacially-modified ones having dates of 100-150,000 years.[6] This may reflect a dryer, more arctic climate.

Tors in Great Britain[edit]

Dartmoor[edit]

For more details on Dartmoor's tors, see List of Dartmoor tors and hills.
Panorama of some of Dartmoor's tors in the snow

Dartmoor represents one of the largest areas of exposed granite in the United Kingdom, covering an area of 368 square miles (954 square kilometres).[7] It is part of a chain of granite stretching through Cornwall, as far as the Isles of Scilly.

Some of the more durable granite survived to form the rocky crowns of Dartmoor tors. One of the best known is at Haytor, on the eastern part of the moor, whose granite is of unusually fine quality and was quarried from the hillside below the tor during the 19th and early 20th centuries. Its stone was used to construct the pillars outside the British Museum in London, and to build London Bridge. The last granite to be quarried there was used to build Exeter War Memorial in 1919.

Ten Tors is an annual weekend hike on Dartmoor.

Hawk's Tor, Bodmin Moor, Cornwall

Cornwall[edit]

Peak District[edit]

There are many tors in this area, notably in the Dark Peak where the host rock is Millstone Grit:

  • Back Tor, Derwent Edge (538m)
  • Carl Wark, Hathersage Moor
  • Dovestone Tor, Derwent Edge (505m)
  • Great Tor, Bamford
Higger Tor

In addition there are hills which incorporate 'tor' in their name but yet do not feature the geomorphological feature described in this article. Examples include Mam Tor and Shining Tor.[8]

Pennines[edit]

Scotland[edit]

There are numerous tors developed in the Cairngorm granite in the Scottish Highlands:

Other areas[edit]

Tor Bay, one of the sandy beaches near Oxwich Bay on the Gower Peninsula in south Wales, is so-called because the beach is framed by a huge outcrop of Carboniferous Limestone.

Tors in other countries[edit]

Externsteine, Germany

Germany[edit]

India[edit]

Tors are very commonly found in the Telangana and the Rayalaseema regions of Andhra Pradesh

North America[edit]

Part of the Angel Rocks formation in Alaska

Africa[edit]

Kit-Mikayi, a celebrated tor near Kisumu, Kenya

See also[edit]

References[edit]

  1. ^ a b Ehlen, J. (2004) Tor in Goudie, A., ed., pp. 1054-1056. Encyclopedia of Geomorphology. Routledge. London, England.
  2. ^ Crossing's Guide to Dartmoor, 1912 Edition, 1965 Reprint (David & Charles, Newton Abbot)
  3. ^ Twidale, C.R., and J.R.V. Romani (2005) Landforms and Geology of Granite Terrains. A.A. Balkema Publishers Leiden, The Netherlands. 359 pp. ISBN 978-0415364355
  4. ^ "Dartmoor Factsheet: Tor Formation". Dartmoor National Park. 2002. Retrieved 21 December 2011. 
  5. ^ Gunnell, Y., Jarman, D. and 8 others, 2013. The granite tors of Dartmoor, Southwest England: rapid and recent emergence revealed by Late Pleistocene cosmogenic apparent exposure ages. Quaternary Science Reviews 612, 62-76
  6. ^ Adrian Hall, New perspectives on a classic landscape of selective linear glacial erosion, The history of the Cairngorms: granite, landscape and processes, British Geological Survey
  7. ^ Dartmoor National Park Authority website. Retrieved 12 October 2008
  8. ^ Ordnance Survey 1:25,000 scale Explorer map sheets OL1 Dark Peak area & OL24 White Peak area

Further reading[edit]

  • Mercer, Ian (2009). "The Physical Anatomy of Dartmoor". Dartmoor – A Statement of its Time. London: Collins. pp. 30–78. ISBN 978-0-00-718499-6.