North West Highlands Geopark

Knockan Crag

The North West Highlands Geopark is a geopark in the Scottish Highlands. Awarded UNESCO geopark status in 2004,[1] it features some of the oldest rocks in Europe, around 3,000 million years old.[2][3] The park contains many notable geological features, such as the Moine Thrust Belt and Smoo Cave and covers an area of around 2,000 square kilometres (770 sq mi).[1]

Geography

The park is located in the extreme north-west of Scotland and includes parts of Sutherland and Wester Ross, including Cape Wrath. The area is one of the most sparsely inhabited in Europe,[4] and is largely treeless. The park's eastern boundary generally follows the Moine Thrust Belt, otherwise the park is generally bounded by the north and west coasts of Scotland, with a few islands included in the park, such as the Summer Isles.[5]

Notable features

Smoo Cave

The Moine Thrust Belt was formed between 430 and 500 million years ago. The belt includes Precambrian Moine rocks which have been pushed on top of younger Cambrian and Ordovician rocks, much to the surprise of Victorian geologists.[5][6] A debate ensued between prominent geologists of the time. Roderick Murchison and Archibald Geikie argued that the Moine rocks must in fact be younger than the rocks beneath them, a point of view opposed by James Nicol and Charles Lapworth. The controversy was resolved by Ben Peach and John Horne who found that the Moine rocks had been pushed some 70 kilometres east over the top of the younger rocks by tectonic action. This was the first thrust fault to be discovered.[7] A monument to the pair is located within the park. Its inscription reads: To Ben N Peach and John Horne who played the foremost part in unravelling the geological structure of the North West Highlands 1883-1897. An international tribute. Erected 1980.[8] The faultline can be seen most easily at a line of cliffs named Knockan Crag. This crag is where the Moine is where the apparent anomaly in the ages of the rocks was first seen, and is where the thrust belt was first identified. A visitor's centre is located here, as well as several pieces of sculpture created by modern artists.[9]

The area contains a number of limestone caves. The most well known of these is Smoo Cave, a large sea cave near Durness. This cave is unique within the UK in that its outer chamber was formed by the action of seawater, while the inner chambers were formed by fresh water.[10] Its entrance 15 metres high, is the largest entrance of any sea cave in the British Isles.[11] Archaeological excavations have found evidence of human habitation dating back to the Mesolithic period.[12] The cave became well known after Sir Walter Scott visited it in 1814. Another notable cave site is the Inchnadamph Bone Caves. At these caves, remains of Eurasian lynx, brown bear, Arctic fox, reindeer and polar bears have been found; as well as human remains dated between 4,515 and 4,720 years old.[13] Uamh an Claonaite, Scotland's longest cave is partly located below these Bone Caves.

Suilven, one of the park's mountains

Also located in the park is Cape Wrath, the northwesternmost point on the Scottish mainland, which features the highest vertical cliffs in mainland Britain.[5] Another feature is the Old Man of Stoer, a sandstone sea stack located off the Point of Stoer in Assynt.

Mountains

The Moine Thrust Belt is regarded as the northwest boundary of the Caledonian mountain belt.[14] However, a few mountains exist within the park, some of which are well known. The highly distinctive Suilven is perhaps the most notable mountain within the park, and its image is used in promotional material.[15] Other mountains to be found here include Stac Pollaidh, Canisp, Quinag, Foinaven and Arkle.

Geology

A large boulder of Lewisian Gneiss within the geopark

The park contains a wide variety of different types of rock:

See also

Footnotes

  1. 1 2 "Scotland's first Geopark". Sustainable Tourism. VisitScotland. 2004-11-18. Retrieved 2008-01-27.
  2. "North West Highlands Geopark: Scotland's first European Geopark" (pdf). Geopark Brochure. Retrieved 2008-01-25.
  3. "The geology of Scotland". VisitScotland website. Retrieved 2008-01-26.
  4. "Welcome to North West Highland Geopark". North West Highland Geopark Website. Retrieved 2008-01-26.
  5. 1 2 3 "The Geopark Story". North West Highlands Geopark website. Archived from the original on 2007-11-27. Retrieved 2008-01-25.
  6. "Overview of Moine Thrust". Gazetteer for Scotland. Retrieved 2008-01-25.
  7. Oldroyd, David R. (1990). The Highlands Controversy: Constructing Geological Knowledge through Fieldwork in Nineteenth-Century Britain. University of Chicago Press. ISBN 978-0-226-62634-5.
  8. Dryburgh, P. M. et al. (1995) Assynt: The Geologists' Mecca. Edinburgh Geological Society.
  9. "About Knockan Crag". Knockan Crag website. Retrieved 2008-01-25.
  10. "Geology". Smoo Cave. Retrieved 2008-01-25.
  11. "Data". Smoo Cave. Retrieved 2008-01-25.
  12. "Archaeology". Smoo Cave. Retrieved 2008-01-25.
  13. "Inchnadamph Bone Caves" (pdf). Scottish Natural Heritage. Retrieved 2008-01-25.
  14. "GCR block - Moine". Joint Nature Conservation Committee. Retrieved 2008-01-27.
  15. See the Geopark website and Brochure (pdf link).
  16. Lerner, K. Lee; Lerner, Brenda Wilmoth (Eds.), ed. (2003). "Europe". World of Earth Science. Farmington Hills, MI: Gale. ISBN 978-0-7876-7739-8. Retrieved 2008-01-26.
  17. "NWH Geology map" (PDF). British Geological Survey. Retrieved 2008-01-25.

External links

Wikimedia Commons has media related to North West Highlands Geopark.
Wikivoyage has a travel guide for North West Highlands Geopark.

Coordinates: 58°7′N 5°8′W / 58.117°N 5.133°W / 58.117; -5.133

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