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Peter Walker: Track/2636 in area near Loch Maree to Loch Broom (Britain)
Slioch
Ascent: 1190m,
Length: 21.1km,
Creator time taken: 7h39m
Descent: 1161m,
Time predicted from Naismith's rule: 6h 12m + breaks
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PlacesStart at NH03754 62384, Slioch Trig Point, Slioch, Sgurr an Tuill Bhain, Meall Each, end at Start
Track Rating ..
[RWD version 1 ]
Slioch seen across Loch Maree
This is the 'standard' route to Slioch, the huge mountain visible across Loch Maree in the NW Highlands of Scotland, and is a fair indicator of the difference between walking in that area and walking in Ireland. While actually pretty straightforward compared to nearby peaks such as the Torridonian giants (brutal steepness, exposed scrambling) or the summits in the Great Wilderness of which it commands magnificent views (hilariously vast distances to cover), it should be born in mind that this route involves a walk of the best part of 7km to reach the bottom of the mountain, and once you're there it's a long grind from practically sea level to almost 1000m (although there is a path for most of it).
Looking down the south ridge of Slioch
Still, highly recommended and a good introduction (assuming decent fitness!) to one of the finest hillwalking areas in these islands.
Looking to the fabled summits of A'Mhaighdean and Ruadh Stac Mor from Slioch
Editing Details for track/2636
NOTE: ALL information such as Ascent, Length and Creator time taken etc should be regarded as approximate. The creator's comments are opinions and may not be accurate or still correct.
Your time to complete will depend on the speed of the slowest plus break time and your mode of transport.
NOTE: It is up to you to ensure that your route is appropriate for you and your party to follow bearing in mind all factors such as safety, weather conditions, experience and access permission.
Uploaded on: Sun, 20 Jul 2014 (19:04:30), Linkback: https://mountainviews.ie/track/2636/
* Note: A GPS Height in the elevation profile is sourced from the device that recorded the track. An "SRTM" height is derived from a model of elevations for parts of the earth. More detail
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