Tor (rock formation)

A tor in Altai Krai, southern Siberia.

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

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 such word is crag (from Welsh craig "rock").

Formation

Tors are most common and most well known as a landform that was created by the erosion and weathering of granitic rocks. However, tors 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]

Kit-Mikayi, a celebrated tor near Kisumu, Kenya.

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.

An example is 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.

See also

• List of tors

References

Wikimedia Commons has media related to Tors.

Further reading

• 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.