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I got blisters on the soles of my feet

Rebecca likes walking...on paths. I like walking a little bit of the beaten track. I had a day off today so decided to head for the Mournes on a solo ascent of Slieve Bernagh. Solo ascent is my little joke, the mountain is only 750m high, but I think it's the third highest peak in Northern Ireland behind Donard and Commedagh...I may be wrong however. I used to walk here a lot with my old boy when I was young, we used to climb in the Mournes every Sunday, I think we managed all the peaks, well all the decent ones anyway.It's a shame his fitness is not what it was, I'd love to have his companionship on these walks again.
These photos are a bit duff, I was using an old rattlebox of a camera, and the mist was pretty bad. I felt like a real intrepid explorer using the old map and compass when the mist closed in at the top of Bernagh.
Hopefully Stephen knows something about the geology of Bernagh, the Tors are very impressive, rocks the size of my house, must have been some serious 'geological activity' on the go up there.

Comments

Almost looks like "The Great Wall". Nice pics.

If Tristan reads your weblog he's a better man to answer this.

Bernagh is part of a series of igneous injections into high level crust, a collapsing caldera was the theory when I was in school. So you have this big chamber of magma in the crust, where magma is supposed to be, but it collapses, and the magma gets squirted upwards, it doesn't reach the surface but gets high enough for an ice age or two to reveal the Moutains of Mourne, hard granite the ice couldn't shift.

This happen in about 5 stages, creating 5 types of granite, Bernagh is G2 as you can maybe see on this map ( if you're lost look from right to left: Bloody Bridge > Slieve Donard > Slieve Bernagh):
http://green.carisenda.com/photos/mournes.gif

regardless of how they're formed, it looks like amazing hiking to me.

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