Showing 1-50 of 135 posts. Most recent first | Next 50 
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Haven't been able to find out any history of this one yet. It stands, set in a rough stone base, so may well be of modern origin, although it may be re(z)erected.
A tall thin stone, over 10ft tall, it leans or points quite heavily. Views over towards The Cheviots to the West and Hepburn Woods to the East.
Of notable mention is a bit of modern architecture just oevr the hill - The Hurlstone Tower was built in 2000 by the local landowner and is a round 3 storey castle looking folly.
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Do not underestimate the trip to the Giants Graves. walk along a track for about 1/2 a mile and then the ascent begins, and goes on, and on, and on. Through the woods, the hillside has steps all the way to the summit, but it is a real steep climb.
Expect to take some rest stops (and on the way back down travellers plaintively asking "is it much further?") Once you reach the top of the steps, you might think you are there. Oh, no, continue along the hilltop, climbing still slightly, through the woods - watch out, we expected Orcs to come running at us at any moment.
When you reach the clearing, you will not be disappointed. What a great place! As others have said, the views must have been breathtaking - a burial for kings!
Only one thing spoilt our restful period at the top.... a phone call from work! don't take your mobile.
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On the approach to Machrie Moor from the A841 you will walk past this burial cairn, the historic Scotland plaque seems unsure of what it is....
"Is it a stone circle with a later burial cairn built inside it or is it simply a cairn with a permanent stone kerb?"
I think the latter, but you can correct me on that.
Whatever it is, it augments the approach to the amphitheatre of Machrie Moor - watch carefully as you approach, other standing stones will become evident on the way to the main sites.
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HOW TO GET THERE
From Berwick Upon Tweed Head towards the A1 (Southwards) Before you reach the A1, turn left towards the village of Scremerston. Immediately turn left again and follow the road round. At Borewell Farm (offering farm shop etc) take another left. cross the railway and continue along the road until it falls away into disrepair. park up below the "pill box" and walk through the nature reserve part of the dunes. you will come to a fence, climb it and follow the path down to the beach. It is pretty rough and steep going, but soon you will be on a sandy beach. Keep close to the dunes and look out for rocks that are submerged at high tide. These are the ones you need to examine.
Apologies if the grid reference is not 100% correct.
If you have any problems finding it - give me a shout!
Moey
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ART IMITATES LIFE
This area was something that caught me by surprise. On the beach at Cocklawburn near Berwick-Upon-Tweed Lie some excellent rock formations that look similar to cup and ring marks.
I used to walk my dogs here a lot and had never noticed them beforee, but one day I was walking with my head down and say one of the ring formations. I couldn't believe it - didn't know if they were natural or man made.
I looked around and there were loads of them. Some qute large, but many were huddled together on rocky outcrops like so many limpets hanging on for dear life. Many are flat to the surface of the sand, but others are vertical on the rocks.
I formulated a theory about sandstone and volcanic rock fusing, but this doesn't seem to be quite right.
Through the wonders of the community that is Head Heritage, I got talking to Fitzcoraldo about rock art, I sent him the pics and he showed them to the resident geologists on his oil rig. I hope Fitz doesn't mind me reprinting his reply, but this is the current thinking on the formations.
"I have a name for your bizarre rock formation and can tell you that your half baked theory was only a quarter baked.
I've consulted the afternoon shift geologists and the consensus seems to be that they are a phenomena called MUD VOLCANOES, in fossil form of course.
Apparently you get mud volcanoes in areas like large river deltas, where you get a large amount of sediment deposited quickly, this mud is then overlain by slower deposited sands which compress the mud causing it to flow upwards inna volcano stylee. So there you go."
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