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Beinn Liath Mhor & Sgorr Ruadh

Oct 5

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Long day out in Glen Carron!

Approach track showing Sgorr Ruadh behind Fuar Tholl
Approach track showing Sgorr Ruadh behind Fuar Tholl

Introduction - Glen Carron

There isn't very much in Glen Carron. The A890 passes through the glen from Achnasheen to Lochcarron south west for 21 miles. The views are wonderful and there are 3 munros on the north and access to 10 munros to the south.


Facilities in the Achnasheen are limited. The Ledgowan Lodge Hotel is one mile (1.5 kilometres) west of the village, but the Achnasheen Hotel (by the railway station) burnt down in the early 1990s and has never been rebuilt. Despite the size of the village, Achnasheen is also the name of a postal district which covers several much larger communities including Kinlochewe, Poolewe and Laide. This dates from the time when the railway station was built in 1870, it was an important stop on the Kyle of Lochalsh Line. The railway still operates but all freight and mail, and most passengers, now travel by road.


Lochcarron is a larger community. The village stretches for almost two miles (three kilometres), meandering along the shore of Loch Carron ("Loch of rough water"). Lochcarron was formerly known as "Janetown" or "Jeantown", and consisted of only a few houses until 1813 when it expanded due to the arrival of the Parliamentary road from Contin to Strome Ferry. The ferry operated for many years until it ceased in the latter part of the 20th century. It has a shop and plenty of accommodation. Attadale Gardens are well worth a visit.


The geology of Glen Carron is very interesting and can be linked to the geology described in my blogs on Knoydart. In particular, it's relation to the Moine Thrust event and the creation of our dramatic landscapes in the North West Highlands.

The first mapping of the Moine Thrust Belt, NW Scotland: the progress of Peach, Horne and colleagues (1883–1936) Geological Society, London, Special Publications Author: Robert W. H. Butler
The first mapping of the Moine Thrust Belt, NW Scotland: the progress of Peach, Horne and colleagues (1883–1936) Geological Society, London, Special Publications Author: Robert W. H. Butler

As the geological map above clearly shows, the Moine Thrust Belt (turquoise) passes right through the two mountains I climbed and the geology is evident in the photos. I could write a blog on the Moine Thrust alone and not ever have enough space, and I would probably bore you, but just a wee note below on what it means and how old it is with a link to a superb article.


"The Moine Thrust was an integral part of a protracted period of mountain building from 475 to 405 million years ago, when three continental plates collided as the intervening Iapetus Ocean was consumed by subduction: Laurentia (now North America and Greenland), Baltica (Scandinavia and northern Europe), and Avalonia (southern England and east Newfoundland). The ancient mountain chain is called the Caledonides, the Roman name for all us unruly Celts. Remnants of these once lofty peaks can be traced from Scandinavia to northwest Scotland and Ireland, eastern Greenland, and the Appalachians of eastern North America." (Brian Ricketts Geological Digressions - The Moine Thrust: An idea that unravelled mountains - Geological Digressions)


Onto the main event then, below you'll find my stats, the route, and information you will hopefully enjoy and find useful.


Stats and stuff - munros; maps & timings


Munro number: 39 and 38 (to go)

Munro name(s): Beinn Liath Mhor 926m (3038ft) and Sgorr Ruadh 962m (3156ft)

Area: Glen Carron

Maps: Cape Wrath Trail North Map; OS Map of Glen Carron & West Monar | Explorer 429 Map | Ordnance Survey Shop

Distance: 11.60 miles (18.6km)

Ascent: 1,444m (4738ft)

Moving time: 5 hours

Total time: 8 hours 30 mins


Ratings


Bogginess ☹️

Effort 😅😅😅

Navigation 🤔🤔🤔

Enjoyment 😍😍😍


Local information


Eating: Coffee Shop in Achnasheen midgebitecafe@gmail.com 01445 720222 (information available on Facebook); Home | Ledgowan Lodge Hotel | Achnasheen Scotland

There are not very many places to eat in Glen Carron and actually anywhere along the A890. You may be better served staying in Lochcarron if you cannot get accomodation in Achnasheen.

Accommodation: Home | Ledgowan Lodge Hotel | Achnasheen Scotland - offers luxury accommodation but also has a bunkhouse. Ledgowan Bunkhouse is a small self-catering bunkhouse a short walk from Achnasheen railway station. It sleeps 5 guests in 5 rooms, so each guest has their own room with wash basin , with a pleasant communal dining area, kitchen and bathroom. The Bunk House is fully centrally heated, so warm and cosy. There is an onsite bar for drinks and coffee etc. and you can book a table in the restaurant in the Guesthouse if you prefer. Please note that all guests are required to bring their own bedding or sleeping bags, although pillows and pillow slips are provided.

Gerry's Hostel

Facilities: Very few! Petrol stations can be found at Contin, Kyle of Lochalsh and Kinlochewe, all have shops as well. Just don't forget anything! At the train station car park in Achnasheen there are public toilets and an electric car charging point.

Don't miss: The views! Attadale | open garden in Wester Ross | Attadale, Strathcarron IV54 8YX, UK


The route

The route for these two mountains begins at the train station in Achnashellac. You can park on the south side of the main road in an ample carpark. On the north side of the main road head up a track on the left to the station and a cross over the railway line. Once across there is a gate and a steep road up to your right, only follow this for 100m or so, then turn left following a good track up onto the moor through the trees.

Beinn Liath Mhor from the path emerging at the top of Coire Lair
Beinn Liath Mhor from the path emerging at the top of Coire Lair

After a stiff climb along the side of the River Lair the path emerges onto open moorland. Follow the path to the right. This is an old right of way from Achnashellac to Coulin and a wonderful long walk in itself.

The long ridge of Beinn Liath Mhor on the right and Sgorr Ruadh on the left
The long ridge of Beinn Liath Mhor on the right and Sgorr Ruadh on the left

At the high point of this path on the col at Drochaid Coire Lair, take a faint path on your left that develops into an excellent stalkers path, very steep and exposed in places. This is a hard pull but you quickly gain height and attain the ridge of Beinn Liath Mhor at a height of 876m (2874ft). The long 2km ridge stretches ahead of you. An undulating walk with some steep ascents and descents.

Sgorr Ruadh on the left and the first peak of the Beinn Liath Mhor ridge at 876m
Sgorr Ruadh on the left and the first peak of the Beinn Liath Mhor ridge at 876m
View back along the ridge of Beinn Liath Mhor with Beinn Alligan, Liathach and Beinn Eighe from left to right
View back along the ridge of Beinn Liath Mhor with Beinn Alligan, Liathach and Beinn Eighe from left to right
Summit
Summit Beinn Liath Mhor

I was glad to be on the summit of Beinn Liath Mhor. From here great care is required descending to Bealach Coire Lair, especially in misty conditions, as the route is not obvious. To be fair, it wasn't obvious in clear conditions! The descent is on boulders and scree followed by worn sandstone. Descend past a small lochan and continue climbing slightly to the col and a second lochan, this marks the crossing point of the col and the start of the route up Sgorr Ruadh. Remember to take time to look back at the geology of the ridge you have just traversed. It's very ancient and hugely important in understanding how the mountains here were formed. More in Claire's top tips below!

View to Sgorr Ruadh from the summit of Beinn Liath Mhor
View to Sgorr Ruadh from the summit of Beinn Liath Mhor
Great example of the varied geological terrain, quartz to sandstone
Great example of the varied geological terrain, quartz to sandstone
The path from the col is clear from the ascent of Sgorr Ruadh
The path from the col is clear from the ascent of Sgorr Ruadh

From the col the path up Sgorr Ruadh is clear, direct and steep in places. The summit affords wonderful views of the Torridon hills and of course, Beinn Liath Mhor.

Path to the summit of Sgorr Ruadh
Path to the summit of Sgorr Ruadh
Maol Chean-Dearg and Ben Damph - more examples of the vertical thrust that created the mountains
Maol Chean-Dearg and Ben Damph - more examples of the vertical thrust that created the mountains
Beinn Alligan, Liathach and Beinn Eighe from left to right
Beinn Alligan, Liathach and Beinn Eighe from left to right
Beinn Liath Mhor from the summit of Sgorr Ruadh
Beinn Liath Mhor from the summit of Sgorr Ruadh

The descent is straightforward south-east down a broad grassy slope past a number of small lochans. Once you have passed the largest lochan, Loch a Bhealaich Mhoir, keep descending heading for Fuar Tholl until you intercept a stalkers path and turn left (east) into Coire Lair. Drop down into Coire Lair and re-join the path you started on.

Final view of Beinn Liath Mhor before crossing the River Lair and returning to the station on the inward path
Final view of Beinn Liath Mhor before crossing the River Lair and returning to the station on the inward path

I thoroughly enjoyed this day out and was surprised how few people I met on the hill itself. I did meet walkers with huge rucksacks completing the Cape Wrath Trail which passes from Achnashellac to Kinlochewe past Coulin, and 6 mountain bikers completing the Torridon Achnashellac loop, also called the Torridon Lollipop! - a 40km off-road red mountain bike route with 1200m of climbing!


Each to their own.....

Claire's top tip....


Geology rocks!


The steep flanks of Beinn Liath Mhor are of national importance in that they show arguably the clearest large-scale examples of imbricate thrusts and associated folds anywhere in north-west Scotland. The spectacular structures are readily seen from distant viewpoints on account of extensive rock exposure and the marked colour contrast between the main rock types involved, red-brown Torridonian sandstones and white Cambrian quartzites.


Or, in other words, the different types of rock that are moved around when the earths geological forces are active, are very obvious on Beinn Liath Mhor. It clearly shows the trust of different rocks that have been forced upwards, and over each other over time.

In this picture you can clearly see the white bands of Cambrian quartzites and the intervening red (greyer at this distance) bands of Torridonian sandstone
In this picture you can clearly see the white bands of Cambrian quartzites and the intervening red (greyer at this distance) bands of Torridonian sandstone

In addition, there is amazing evidence of shear zones, where different rocks have moved over one another and left clear markings, showing tectonic processes that have been happening over millions of year!

Shear zone where different rocks have forced past each other over millions of years
Shear zone where different rocks have forced past each other over millions of years

This reminds me of runes and I can imagine some ancient Norse travellers passing over the mountains leaving messages for their followers!

Coming next......


Meall nan Ceapraichean & Edidh nan Clach Geala


Thank you for reading ❤️ xx



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