How much do we know about Stonehenge? Less than we think. And what has Stonehenge got to do with the Ice Age? More than we might think. This blog is mostly devoted to the problems of where the Stonehenge bluestones came from, and how they got from their source areas to the monument. Now and then I will muse on related Stonehenge topics which have an Ice Age dimension...
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Tuesday, 19 August 2014
Those mysterious pink erratics
Where did these mysterious pink granite erratics come from? The one in the top photo is on the island of Flat Holm in the Bristol Channel, and the one in the bottom pic is from Saunton in Devon. Both are quite close to sea level, and both are resting on wave-cut platforms. The mobile phone in the lower photo gives the scale.
I assume nobody has ever done any petrography on these.... but there are a number of possible sources of pink granite erratics in the UK -- some in Wales, some in Ireland. But the main possible source is in northern England, where the Shap granite outcrops. Could that really be the source? Here is a close-up:
Over to the geologists.......
Hate to say this but it is not unlike the Shap adamellite.
ReplyDeleteThere are no small dark heathens in it?
M
Why do you hate to say that? Thought you were an impartial scientist free of all encumbrances?!!
ReplyDeleteNo idea what either granite looks like close up. But hoping to get over to Flat Holm before long, to take a look.....
Brian,
ReplyDeleteMany great posts here! Keep up the good work you are doing. Invaluable contributions for both professionals and laypersons alike! I appreciate the lessons!
I have one small curiosity. How did that pink granite erratic get wedged under that sizable bedrock strata in the photo? What can this tell us about the ice that deposited it there and not on top of the bedrock strata?
Kostas
Kostas -- the pink erratic is resting on a coastal rock platform cut at a time of higher sea-level. How much time elapsed between the erosion of the platform and the arrival of the boulder is currently not known. later on, other sediments began to accumulate and covered the boulder. For many thousands of years the boulder was sealed away, out of sight -- then recent coastal erosion cut the "drift cliff" back and exposed the boulder again. Straightforward sedimentology.....
ReplyDeleteI hate to pontificate but someone has to do it.
ReplyDeleteM
Message for Kostas
ReplyDeleteComment rejected. Not going there again -- the topic of giant erratics on the SW England coastal platform is well covered already on this blog. Please search and thou shalt find.
The Shap adamellite is highly recognisable and if it Shap I am surprised that that has not been noted before. In addition Ixer and Vince looked at the use of Shap erratics in AS pottery and needed to look at the ice directions moving the erratics. I don't think they mentioned north to south moving ice entraining Shap, but as they were dealing with NE England may have missed it.
ReplyDeleteM