I’ve already done three residential schools with the OU [SXR103, SXR260 and SXR 208], each one better than the last, so this one had a lot to live up to! This time I didn’t have to travel far, it was only 2 hours north of me in Perthshire, near Pitlochry in a field centre in Kindrogan Wood. It was a fantastic place – a conservation ‘eco-centre’, with red squirrels, pine martins and Scottish wildcats amongst the wildlife in the wood. Each day we set out on the bus to a different location in order to study the geology and hopefully learn something about deformation and metamorphism. On the first day, Sunday, we went north of Lochnagar to Glen Gairn to have a look at a granite pluton.
I love how picturesque and beautiful rural Scotland is, all the little stone bridges and cottages, as well as old gothic castles and rolling mountains. I’m already dying to get back out there – I’m making learning to drive a priority now! Anyway, back to the geology…
The granite exposure at the side of the road. Billy Connolly drove past and gave us a wave! Not to let some rocks sat around untouched, we got stuck in…
My lovely room-mate Emma in the centre [young lady in the aquamarine jumper] studying her notes. I wish I could tell you something highly embarrassing about her, but she was a really nice girl!
We climbed up to the roof of the granite pluton to find the contact with the country rock, but hunger got the better of us – so we broke for some lunch. We found a little stone circular wall built up to waist height against the rock, some smart fellows had previously built themselves a shelter. We made use of this for lunch, camping out inside to have sandwiches and crisps.
Stood above the sandwich spot, looking down on Glen Gairn and the first two locations. We were lucky to get such great weather all week – with rain only coming down heavily the day we spent mostly indoors!
A pegmatite within the granite pluton. A pegmatite is an intrusive igneous rock with crystals > 2.5 cm in size, with a granitic composition.
This was a very old Scots Pine tree… although I didn’t note the age down in my field notebook so your guess is as good as mine.
This is a great little bit of structural geology. The country rock and the small quartz intrusions have been folded by some deformation event, however the pale granite intrusion that runs top to bottom along the left has not been folded, so it must have been intruded after the deformation event which caused the folds in the country rock. There is further evidence that the dyke is post-deformation in the apothesys – the smaller vein of granite running off perpendicular to the main one – to the top right, which cuts across the folds in the country rock, rather than being folded itself.
I’ll update with the pictures from the rest of the trip later, currently looking into some new walks to do with the family in the local area.