- Canisp
Infobox Mountain
Name = Canisp
Photo = Canisp_from_Conival.jpg
Caption = Canisp seen fromConival , nine kilometres to the east.
Elevation = 847 m (2779 ft)
Location =Assynt , SCO
Range =Northwest Highlands
Prominence = 691 m Ranked 65th inBritish Isles
Parent peak =Ben More Assynt
Topographic
OS "Landranger" 15, OS "Explorer" 442
First ascent =
Easiest route =
Grid_ref_UK = NC203187
Listing = Corbett, Marilyn
Translation = White Mountain
Language =Old Norse
Pronunciation =Canisp (
Scottish Gaelic : "Canasp" [http://www.smo.uhi.ac.uk/gaidhlig/faclair/sbg/lorg.php?facal=Canasp&seorsa=Gaidhlig&tairg=Lorg&eis_saor=on] ) is a mountain in the far north west ofScotland , it is situated in the parish ofAssynt , in the county ofSutherland , 25 kilometres north of the town ofUllapool . Canisp reaches a height of 847 metres (2779 feet) and qualifies as a Corbett and Marilyn hill. The mountain's name translates from theOld Norse language as "“White Mountain”".Geography and Geology
Canisp is an isolated mountain that stands in the Glencanisp Forest, a large rock and water wilderness, it has a considerable
topographic prominence of 691 metres (2,280 feet) making the mountain a very good viewpoint. Canisp has very little vegetation, even on its lower slopes large areas ofGneiss (one of the oldest rocks in the world), are visible on the surface. Canisp is in the strange situation of being eclipsed by the nearby smaller mountain ofSuilven which stands five kilometres to the west and is 116 metres lower in altitude. Suilven is a much more popular and exciting hill with its jagged summit ridge. Canisp stands in a geologically important area, it is part of theMoine Thrust Belt and is typical of many of the Assynt hills in that it rises from a base of Lewisian Gneiss and is composed ofTorridonian sandstone capped byCambrian quartzite giving the hill a distinctive light grey crown. Its rocks also show signs of major abrasions left by the scouring of the landscape byglacier s of the lastice age .Canisp stands on the lands of the Glencanisp and Drumrunie Estates, a 44,000 acre (176 km²) tract of land which was bought in 2005 for £2,900,000 by the Assynt Foundation, a group of around 900 local residents, from the Vestey family. Compared to the other Assynt hills, Canisp does not show any distinct topographic qualities, it is a fairly uncomplicated mountain with a symmetrical profile with two main ridges running north west and south east. Its south western flank has crags and scree and falls steeply into Glen Canisp, while its north eastern slopes also fall precipitously to the loch studded moorland.
Ascents
The most popular ascent of Canisp starts at the north end of Loch Awe (gbm4ibx|NC249160) where there is car parking and a footbridge to cross the River Loanan as it leaves the loch. The route gains the summit by the south east ridge. This is the shortest and quickest route, but it is still 6km long, almost completely devoid of paths, and defended by stones, heather and bog. Another ascent from the east which also uses the SE ridge starts at Stronchrubie where there is also a footbridge over the Loanan. Longer ascents are also possible from
Lochinver and Ledmore Junction, both these routes utilise the path between the two places that traverses the length of Glen Canisp before leaving the glen to climb the mountain by either its north west ridge (from Lochinver) or south east ridge (from Ledmore). The route from Lochinver gains the NW ridge by a path from Loch na Gainimh and is regarded byHamish Brown as the most pleasing way up the mountain. The summit of Canisp is marked by a large stone built wind shelter. The view from the top of the mountain is regarded as one of the finest in Scotland giving all round views taking in the surrounding loch studded moorland,The Minch beyond Lochinver and most of the well known mountains of Assynt.References
* The Corbetts and Other Scottish Hill, (SMC Guide) ISBN 0-907521-29-0
* Climbing the Corbetts, Hamish Brown, ISBN 1-898573-08-5
* [http://news.bbc.co.uk/2/hi/uk_news/scotland/4605233.stm BBC News on purchase of Glen Canisp Estate]
* [http://aragorn.leeds.ac.uk/assyntgeology/geology/geoessay.pdf Geology of NW Scotland]
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