The shallower western end of the loch
Location in Lochaber
|Type||freshwater loch, dimictic, oligotrophic|
|Primary inflows||River Meoble|
|Primary outflows||River Morar|
|Catchment area||168 square kilometres (65 sq mi)|
|Max. length||18.8 km (11.7 mi)|
|Surface area||26.7 km2 (10.3 sq mi)|
|Average depth||87 metres (284 ft)|
|Max. depth||310 m (1,017 ft)|
|Water volume||2.3073 cubic kilometres (81,482,000,000 cu ft)|
|Surface elevation||9 metres (30 ft)|
Loch Morar (Scottish Gaelic: Loch Mhòrair) is a freshwater loch in Lochaber, Highland, Scotland. It is the fifth-largest loch by surface area in Scotland, at 26.7 km2 (10.3 sq mi), and the deepest freshwater body in the British Isles with a maximum depth of 310 m (1,017 ft). The loch was created by glacial action around 10,000 years ago, and has a surface elevation of 9 metres (30 ft) above sea levels.
Loch Morar is 18.8 kilometres (11.7 mi) long, has a surface area of 26.7 km2 (10.3 sq mi), and is the deepest freshwater body in the British Isles with a maximum depth of 310 m (1,017 ft). In 1910, John Murray and Laurence Pullar found it to have a mean depth of 87 metres (284 ft) and a total volume of 2.3073 cubic kilometres (81,482,000,000 cu ft) during their survey of Scottish lochs. The bottom is deepened below the United Kingdom Continental Shelf, and until 1943, when a depth of 324 metres (1,062 ft) was observed in the Sound of Raasay, it was believed to be the deepest water in the United Kingdom. The surface of the loch is 9 metres (30 ft) above sea level.
The water of the loch is clear and oligotrophic, with a minimal intake of nutrients, making it a Site of Special Scientific Interest (SSSI). The main inflow is the River Meoble at the southern end, which drains from Loch Beoraid, although there are three other major inflows at the eastern end of the loch and a stream draining a complex of lochans to the north-west of Loch Morar. The outflow is the River Morar at the western end, which at a few hundred metres long is one of the shortest rivers in the British Isles. At the shallower eastern end of the loch, there are a number of sizeable forested islands.
Swordland Lodge, on the northern shore of the loch, was used as training school STS 23b during the Second World War by the Special Operations Executive. A 750 KW hydroelectric power station with a hydraulic head of 5.5 metres (18 ft) was built on the River Morar in 1948.
At the western end of the loch is the village of Morar, which is between Arisaig and Mallaig on the coastal A830 road. The settlements of Bracorina and Bracara are located along the northern shore of the loch, but there is no road along the southern shore. Tarbet, on the shore of Loch Nevis, is a short distance from Loch Morar.
During the period of the Highland Clearances, many residents emigrated to Canada. Boats left in 1790, 1802, and 1826, carrying people to Quebec, Glengarry in Ontario, and the Strait of Canso in Nova Scotia respectively.
The loch occupies a basin produced by the overdeepening of the valley by glacial erosion, along an east-west fault line. It is not a sea loch due to isostatic rebound that raised the rock sill at the end of the loch.
Based on estimates of erosion of between 2–4 mm (0.079–0.157 in) per year, the deep basin was created over a period of 67,000 – 150,000 years of glacial action, which occurred intermittently during the last million years of the Quaternary glaciation. An outwash fan made up of sand and gravels at the western end of the loch marks the limit of the re-advance in the Morar valley. Subsequently colonised by vegetation and known as Mointeach Mhòr (the mossy plain), these deposits blocked the outflow of the loch to the south, so that it drained from the north-west corner instead.
The catchment area of the loch is 168 square kilometres (65 sq mi), and the geology is base-poor. A site to the north of the loch was selected in 2011 as a SSSI for its characteristic rock exposures of the Moine group by the Geological Conservation Review, replacing the area around Mallaig harbour, which had been previously regarded as the most representative site.
The loch is surrounded by a mix of natural woodland, open hillside, sheep and cattle pasture and planted mixed coniferous and broadleaf woodlands. Only around 0.7% of the surface of the loch can be colonised by plants.
Loch Morar's fish population is believed to be limited to Atlantic Salmon, brown trout and sea trout, Arctic char, eel, stickleback, and minnow. Trout average around 0.75 pounds (0.34 kg) in size, but ferox trout of up to 15 pounds (6.8 kg) have been caught. The loch is also known to contain eels, although none were caught in a recent survey of eel populations in Lochaber, suggesting that they prefer the loch to the tributaries surveyed. Catches of salmon and sea trout declined dramatically between the 1970's and 1980's, in commons with other catchments on the west coast. Artificial stocking of the River Morar with salmon and sea trout was suspended in 2007 after the hatchery was closed.
The main salmonid spawning grounds are the River Meoble and the smaller burns that feed into the loch. The hydroelectric power station, which contain one of only two fish counters in Lochaber, is shut down during the smolt run, following a study on smolt mortality in 1992.
The catchment is managed by the Morar District Salmon Fishery Sub-board, which employs a full-time fisheries manager. Poaching in the form of netting has been known to occur at the mouth of the River Morar.
- Martin, Paula (2005). Lochaber: a historical guide. Birlinn. p. xix. ISBN 978-1-84158-241-2.
- Reed, Michael (2002). The Landscape of Britain. Routledge. p. 21. ISBN 978-1-134-72804-6.
- "Bathymetrical Survey of the Fresh-Water Lochs of Scotland, 1897–1909". maps.nls.uk. Retrieved 11 July 2014.
- Robinson, A. H. W. (1949). "Deep clefts in the inner sound of Raasay". Scottish Geographical Magazine 65: 20. doi:10.1080/00369224908735399.
- Mort, Frederick (2013) . The British Isles. Cambridge University Press. p. 58. ISBN 978-1-107-63281-3.
- Shine, Adrian (17 February 1983). "The Biology of Loch Ness". New Scientist (Reed Business Information) 80 (1345): 462–467. ISSN 0262-4079.
- Walker, Andrew (1996). A Repeat Survey of Salmon and Trout Stocks in the Loch Morar System (Report). Fisheries Research Service. http://www.scotland.gov.uk/Uploads/Documents/Coll1496.pdf.
- Google Inc. "Loch Morar". Google Maps (Map). Cartography by Google, Inc. https://firstname.lastname@example.org,-5.6298173,12z. Retrieved 13 July 2014.
- "Morar, River". scottish-places.info. Retrieved 13 July 2014.
- National Library of Scotland. Loch Morar (Map). http://maps.nls.uk/view/74422165. Retrieved 13 July 2014.
- Rigden, Denis (2004). How to be a Spy: The World War II SOE Training Manual. Dundurn. p. 4. ISBN 978-1-55488-191-8.
- David Harrison. "Special Operations". her.highland.gov.uk. Retrieved 14 July 2014.
- "Morar Power Station". scottish-places.info. Retrieved 13 July 2014.
- "Morar Dam, Hydro-electric Power Scheme". scotlandsplaces.gov.uk. Retrieved 13 July 2014.
- The People's Clearance: Highland Emigration to British North America, 1770-1815. University of Manitoba Press. 1982. p. 74. ISBN 978-0-88755-382-0.
- Johnson, J.K.; Wilson, Bruce G. (1989). Historical Essays on Upper Canada: New Perspectives. McGill-Queen's Press. p. 172. ISBN 978-0-7735-7354-3.
- Campey, Lucille H. (2007). After the Hector: The Scottish Pioneers of Nova Scotia and Cape Breton, 1773-1852. Dundurn. p. 118. ISBN 978-1-55002-770-9.
- "Geology of Loch Morar" (PDF). lochmorar.org.uk. Retrieved 12 July 2014.
- N. H. Trewin (2002). The Geology of Scotland. Geological Society of London. p. 411. ISBN 978-1-86239-126-0.
- Bernard E. Leake (2011). The Life and Work of Professor J. W. Gregory FRS (1864-1932): Geologist, Writer and Explorer. Geological Society of London. p. 145. ISBN 978-1-86239-323-3.
- Hambrey, M. J. (1994). Glacial Environments. UBC Press. p. 90. ISBN 978-0-7748-0510-0.
- McCann, S.B. (1966). "The limits of the Late-glacial Highland, or Loch Lomond, Readvance along the West Highland seaboard from Oban to Mallaig". Scottish Journal of Geology (The Geological Society) 2. Synopsis.
- "4. Mointeach Mhòr". Road to the Isles. Lochaber Geopark. Retrieved 20 July 2014.
- Bailey-Watts, A. E.; Duncan, P. (1981). "Chemical characterisation — A one-year comparative study". "The Ecology of Scotland's Largest Lochs". Monographiae Biologicae 44. p. 67. doi:10.1007/978-94-009-8635-0_3. ISBN 978-94-009-8637-4.
- "News from Mallaig Harbour April 2011". West Word. Retrieved 20 July 2014.
- "Wildlife Around Loch Morar". lochmorar.org.uk. Retrieved 11 July 2014.
- "Fish Populations". lochmorar.org.uk. Retrieved 11 July 2014.
- "Fishing on Loch Morar". lochmorar.org.uk. Retrieved 11 July 2014.
- Baum, Diane; Smith, Lucy (2010) (PDF). [1.pdf ] (Report). Lochaber Fisheries Trust. http://www.lochaberfish.org.uk/cust_images/Lochaber_eel_report_2010.pdf.
- Maclean, J. C.; Walker, A. F. (2002). The Status of Salmon and Sea Trout Stocks in the West Coast of Scotland (Report). Freshwater Fisheries Laboratory. http://scotland.gov.uk/Uploads/Documents/Coll0102.pdf.
- Campbell, Elizabeth Montgomery; Solomon, David John (1972). The Search for Morag. Tom Stacey. ISBN 0-85468-093-4.
- "Cryptozoology". lochmorar.org.uk. Retrieved 13 July 2014.
|Wikimedia Commons has media related to Loch Morar.|
- Map of Loch Morar from soundings performed by John Murray and Laurence Pullar
- Murrary and Puller's description of the loch