To quote Stephenson and Gould in British regional geology: the Grampian Highlands, fourth edition, 2007 when discussing the features you might expect to see in this part of Scotland,
'Metagreywackes, siliceous psammites and fine-grained quartzites are interbedded with the predominant well-foliated green schists containing abundant chlorite, epidote, biotite and albite porphyroblasts.'
When I was young we lived in London and I would often head in the school holidays to the museums in South Kensington. The big draw these days is the Natural History museum but back then dinosaurs weren't quite as popular as they are today and much of the ground floor was a series of somewhat lacklustre dioramas that were populated with a cast of vaguely unsettling stuffed animals.
Around the corner in Exhibition Road was the Science museum which became a big favourite with me mainly due to the number of interactive displays. The joy of finding a button on the front of a mahogany case which when pressed would lead (if it was working) to some magnificent mechanical contraption demonstrating how a bessemer converter worked (I mean who cares? - but just look at that vessel lighting up deep red!) or maybe they would be charging up the vast Van de Graaff generator to emulate a lightning strike. I could go on at length about the variety and interest of these displays but they made the Science museum a must-see.
A bit further along the road was the Geology museum (now part of the Natural History museum) and here there were exciting displays of various types of volcanic eruptions and earthquakes, there was even a floor that vibrated like an earthquake. In order to cool the passions, on the upper floors were halls of table height cases filled with displays of rocks from across the world. For those explorers about to scour the world for mineral wealth I have no doubt that this was a valuable resource. However, I believe that it was in these rooms that I lost enthusiasm for becoming conversant with geology.
So if my geological knowledge is a bit rudimentary, I apologise. Basically to understand what is going on geologically in Scotland I would probably need a PhD. But then if I was successful I would end writing sentences like the one above. All we need to know is that at this moment we are walking over a mixed bag of rocks that's known as the Southern Highland group and this forms part of the Dalradian supergroup. You might be interested to know that the Southern Highland group crosses Northern Ireland and ends on the eastern edges of Scotland between Stonehaven and Aberdeen. Too much? Let's skip on.
What goes up... |
The high and low paths came together before Inversnaid and now there is only one path and it's pretty rugged. The eastern loch side is steep and the Way is unable to contour beside it.
... must come down |
A lot of our fellow walkers have brought walking poles, which in this terrain are more of a hindrance than a help. In retrospect I believe that the majority of walkers who brought poles ended up carrying them. We don't use poles as they require a specific style of walking to be beneficial.
I did use poles at one time when I had a knee problem. Over eighteen months the problem resolved itself and I came to the conclusion that the poles were mainly a danger to fellow walkers, so I gave up with them.
Most hikers on the Way seemed to have poles because they thought they would protect their knees, which they would if used correctly. However I never saw one walker along the whole route who could have been said to have mastered the 'Nordic Walking' technique.
Free of Loch Lomond at last |
A Japanese Garden at Beinglas? - Scottish style |
Don't ask for credit |
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