Loch Ness

For other uses, see Loch Ness (disambiguation).
Loch Ness

With Urquhart Castle in the foreground
Location Highland, Scotland
Coordinates 57°18′N 4°27′W / 57.300°N 4.450°W / 57.300; -4.450Coordinates: 57°18′N 4°27′W / 57.300°N 4.450°W / 57.300; -4.450
Type freshwater loch, oligotrophic, dimictic[1]
Primary inflows River Oich/Caledonian Canal, River Moriston, River Foyers, River Enrick, River Coiltie
Primary outflows River Ness/Caledonian Canal
Catchment area 1,770 km2 (685 sq mi)
Basin countries Scotland
Max. length 36.2 km (22.5 mi)
Max. width 2.7 km (1.7 mi)
Surface area 56 km2 (21.8 sq mi)
Average depth 132 m (433 ft)
Max. depth 226.96 m (744.6 ft)
Water volume 7.5 km3 (1.8 cu mi)
Surface elevation 15.8 m (52 ft)
Islands 1 (Cherry Island)
Settlements Fort Augustus, Invermoriston, Drumnadrochit, Abriachan, Lochend; Whitebridge, Foyers, Inverfarigaig, Dores.
Loch Ness
Location in Scotland

Loch Ness (/ˌlɒx ˈnɛs/; Scottish Gaelic: Loch Nis, [l̪ˠɔxˈniʃ]) is a large, deep, freshwater loch in the Scottish Highlands extending for approximately 23 miles (37 km) southwest of Inverness. Its surface is 52 ft (16 m) above sea level. Loch Ness is best known for alleged sightings of the cryptozoological Loch Ness Monster, also known affectionately as "Nessie". It is connected at the southern end by the River Oich and a section of the Caledonian Canal to Loch Oich. At the northern end there is the Bona Narrows which opens out into Loch Dochfour, which feeds the River Ness and a further section of canal to Inverness. It is one of a series of interconnected, murky bodies of water in Scotland; its water visibility is exceptionally low due to a high peat content in the surrounding soil.

Loch Ness is the second largest Scottish loch by surface area at 22 sq mi (56 km2) after Loch Lomond, but due to its great depth, it is the largest by volume in the British Isles. Its deepest point is 755 ft (230 m),[2][3] making it the second deepest loch in Scotland after Loch Morar. A 2016 survey claimed to have discovered a crevice that pushed the depth to 889 ft (271 m) but further research determined it to be a sonar anomaly.[4] It contains more fresh water than all the lakes in England and Wales combined,[3] and is the largest body of water on the Great Glen Fault, which runs from Inverness in the north to Fort William in the south.

Villages and places

Places on Loch Ness
North
Shores Western Eastern
South

At Drumnadrochit is the "Loch Ness Centre and Exhibition"[5] which examines the natural history and legend of Loch Ness. Boat cruises operate from various locations on the loch shore, giving visitors the chance to look for the "monster".

Urquhart Castle is located on the western shore, 1 mile (1.6 km) east of Drumnadrochit.

Lighthouses are located at Lochend (Bona Lighthouse) and Fort Augustus.

Monster

Main article: Loch Ness Monster

Loch Ness is thought by some to be the home of the Loch Ness Monster (also known as "Nessie"), a cryptid, reputedly a large unknown animal. It is similar to other supposed lake monsters in Scotland and elsewhere, though its description varies from one account to the next. Popular interest and belief in the animal's existence has varied since it was first brought to the world's attention in 1933.[6]

Fish species

Urquhart Bay and Loch Ness viewed from Grant's Tower at Urquhart Castle.

The following fish species are native to Loch Ness. A number of others such as perch and roach have been introduced in the Loch or Caledonian Canal with various levels of success.[7]

European eel Anguilla anguilla
Northern pike Esox lucius
European sea sturgeon Acipenser sturio (unconfirmed in the Loch, but known from BeaulyMoray Firth, which is connected via the River Ness)
Three-spined stickleback Gasterosteus aculeatus
Brook lamprey Lampetra planeri
Eurasian minnow Phoxinus phoxinus
Atlantic salmon Salmo salar
Sea trout Salmo trutta
Brown trout (ferox trout) Salmo trutta (Salmo ferox)
Arctic char Salvelinus alpinus

Island

The only island on Loch Ness is Cherry Island, visible at its southwestern end, near Fort Augustus. It is a crannog, which is a form of artificial island.[8] Most crannogs were constructed during the Iron Age.

There was formerly a second island (Dog Island) which was submerged when the water level was raised during the construction of the Caledonian Canal.[8]

Hydroelectricity

Loch Ness serves as the lower storage reservoir for the Foyers pumped-storage hydroelectric scheme, which was the first of its kind in the United Kingdom. The turbines were originally used to provide power for a nearby aluminium smelting plant, but now electricity is generated and supplied to the National Grid. Another scheme, the 100 MW Glendoe Hydro Scheme near Fort Augustus, began generation in June 2009 producing 76 gigawatt hours in its first months of operation[9], It was out of service between 2009 and 2012 for repair of the tunnels connecting the reservoir to the turbines[10][11]

Geology

Loch Ness lies along the Great Glen Fault, which forms a line of weakness in the rocks which has been excavated by glacial erosion, forming the Great Glen and the basins of Loch Lochy, Loch Oich and Loch Ness.[12]

Loch Ness records

John Cobb died in an attempt at the water speed record when his boat Crusader struck an unexplained wake on the surface of the loch in 1952. His accident was recorded by the BBC reporters on site at the time.[13] Nearby, there is a memorial to him erected by the people of Glenurquhart

On 31 August 1974, David Scott Munro, of Ross-shire Caberfeidh Water Ski Club, became the first person in the world to water ski (mono ski) the length of Loch Ness. From Lochend to Fort Augustus and back, he covered the 48 miles (77 km) in 77 minutes at an average speed of 37 miles per hour (60 km/h).[14]

Brenda Sherratt was the first person to swim 22 12 miles (36.2 km) along the length of Loch Ness in Scotland in 31 hours and 27 minutes in July 1966.

References

  1. Dill, W.A. (1993). Inland Fisheries of Europe, p. 227. EIFAC FAO Techinical Report 52 suppl.
  2. "Bathymetrical Survey of the Fresh-Water Lochs of Scotland, 1897–1909". National Library of Scotland. Archived from the original on 2007-02-08.
  3. 1 2 "Ness, Loch". The Gazetteer for Scotland. Retrieved 2010-02-09.
  4. "A new hideaway for the Loch Ness monster? Skipper claims to have uncovered deepest crevice yet". The Telegraph. Retrieved 2016-03-04.
  5. "The Loch Ness Centre".
  6. Nessie, Legend of. "The Legend of Nessie the Ultimate Loch Ness Monster Site". www.nessie.co.uk. Retrieved 2016-02-28.
  7. Loch Ness Information site: The Fish and Invertebrates of Loch Ness. Retrieved 24 March 2015.
  8. 1 2 Blundell, O. (1909). Proceedings of the Society of Antiquaries of Scotland (PDF). 43. pp. 159–164.
  9. "Glendoe Hydro scheme". Scottish and Southern Energy. Retrieved 2007-08-28.
  10. "Hydro-electric scheme's dam close". BBC. 2008-09-01. Retrieved 2010-02-09.
  11. "SSE Glendoe".
  12. Piccardi, Luigi (2014). "Post-glacial activity and earthquakes of the Great Glen Fault (Scotland)" (PDF). Memorie Descrittive della Carta Geologica d’Italia. 96: 431–446.
  13. Gallacher, Terry. "Loch Ness 1966". Retrieved 24 May 2012.
  14. Press & Journal newspaper. Inverness edition. 2 September 1974.
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