Stonehenge and the Ice Age
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...
Some of the ideas discussed in this blog are published in my new book called "The Stonehenge Bluestones" -- available by post and through good bookshops everywhere. Bad bookshops might not have it....
To order, click HERE
Sunday, 27 April 2025
Sunday, 20 April 2025
Inaugural Rhosygilwen Easter Lecture: The Bluestone Mystery
I'm honoured to be invited to give the inaugural Easter Lecture at Rhosygilwen tomorrow evening (7.30 pm) -- on the subject of the Stonehenge bluestones.
I'll talk about the modern mythology invented by Prof MPP and others, and scrutinize the science of the stones, some of which is I think pretty sound and some of which is distinctly dodgy.
I'm hoping for a good turnout, and I'll be using the evening to raise money for my favourite charity -- which is SHELTER.
If you live in West Wales, feel free to come along and join the fun........
Monday, 7 April 2025
Another Welsh Triad: the Three Great Preseli Bluestone Disputations
The bluestone quarrying myth: three sites and three detailed rebuttals
Brian John (2025). Carn Goedog on Mynydd Preseli Was Not the Site of a Bluestone Megalith Quarry. Archaeology in Wales, March 2025, 14 pp
John, B S, Elis-Gruffydd, D & Downes, J, 2015b, Observations on the supposed Neolithic Bluestone Quarry at Craig Rhos-y-felin, Pembrokeshire, Archaeology in Wales 54, 139-148.
https://www.researchgate.net/publication/286775899_OBSERVATIONS_ON_THE_SUPPOSED_NEOLITHIC_BLUESTONE_QUARRY_AT_CRAIG_RHOSYFELIN_PEMBROKESHIRE
John, B S, 2024a, The Stonehenge bluestones did not come from Waun Mawn in West Wales, The Holocene, 34 (7), 20 March 2024.
https://www.researchgate.net/publication/379121966_The_Stonehenge_bluestones_did_not_come_from_Waun_Mawn_in_West_Wales
Thursday, 20 March 2025
Archaeological mythology and the Welsh Triads
- One of the Three Fantastical Places of
- Powerful Stone.........
In Wales, things come in threes. To quote from the Prydain Wiki:The Welsh Triads (Welsh Trioedd Ynys Prydein, literally "Triads of the Island of Britain") are a group of related texts in medieval manuscripts which preserve fragments of Welsh folklore, mythology and traditional history in groups of three. The triad is a rhetorical form whereby objects are grouped together in threes, with a heading indicating the point of likeness.
https://prydain.fandom.com/wiki/Welsh_Triads
According to Wikipedia:
Some triads simply give a list of three characters with something in common (such as "the three frivolous bards of the island of Britain" while others include substantial narrative explanation. The triad form probably originated amongst the Welsh bards or poets as a mnemonic aid in composing their poems and stories, and later became a rhetorical device of Welsh literature. The Medieval Welsh tale Culhwch and Olwen has many triads embedded in its narrative.
https://en.wikipedia.org/wiki/Welsh_Triads
I remember reading the classic work of Rachel Bromwich many years ago, and being greatly intrigued by it. What's not to like about the three princes of the Court of Arthur, or the three bulls of battle of the Island of Prydain, or the three arrogant ones, or the three atrocious assassinations, or the three great illusions?
See also:
https://www.maryjones.us/ctexts/triads2.html
Bearing in mind that tales and myths are not necessarily old, and they they continue to be created, we come to the three Great Fabricators, Michael of the East, Robert of the Middle and Richard of the West. And behold the tale of the Three Fantastical Places of Powerful Stone, known as Rhosyfelin, Carn Goedog and Waun Mawn..........
Sunday, 9 March 2025
Monolith extraction pits at Stonehenge?
There has been some discussion lately, on social media, on the possible occurrence of one or more deep pits at Stonehenge, in amongst the stone settings -- indicative of the extraction of use of large stones. This is not a new idea -- indeed, I had a discussion with Nick Snashall about this some years ago.
https://brian-mountainman.blogspot.com/2016/08/extraction-pits-solution-hollows-post.html
In that discussion, I was not at all convinced by the argument that genuine extraction pits are genuinely different in kind (ie in morphological features) to other pits that are man-made either as sockets or to accommodate packing stones etc...........
See also:
https://brian-mountainman.blogspot.com/2013/08/where-did-stonehenge-sarsens-come-from.html
https://brian-mountainman.blogspot.com/2018/03/stonehenge-always-was-bit-of-mess.html
https://brian-mountainman.blogspot.com/2019/02/were-some-stonehenge-sarsens.html
The honeycomb characteristics of the chalky ground surface beneath the Stonehenge layer and other accumulations of detritus have always suggested to me that at least some of the surface indentations and elongated hollows might mark the places from which noth sarsens and bluestones have been extracted and rearranged. There is the matter of the "stone 16 pit"......... or a pit that might have held stone 56......
In other words, there is a strong possibility that Stonehenge was simply built where it is because that is where the stones (or the bulk of them) were found...........
Some recent discussion has centred on a large "mystery pit" at the centre of Stonehenge, which has shown up in various excavations. Prof MPP thinks it is very intriguing, but Tim Daw thinks it is a genuine extraction pit, used for taking away the Lake House meteorite, which he speculates was found here. I'm not sure what the basis for that speculation might be. But why could the pit not have been an extraction pit once occupied by one of the larger sarsens or even by one or more bluestones?
To quote Mike Pitts in "Digging Deeper":
https://brian-mountainman.blogspot.com/2018/04/pitts-and-very-ancient-sarsens.html
The idea is that there are two great pits at Stonehenge, larger than any other and both difficult to explain. One of these I partly excavated in 1979, where we found the impression of a standing stone on the bottom, and Atkinson excavated part of it in 1956 (thinking at the time it was the erection ramp for the Heelstone).The other is near the centre of Stonehenge. It was written about by Mike Parker Pearson and colleagues in Antiquity 2007, as part of their study of the site’s phasing. It’s a problematic thing, as Parker Pearson argues, excavated partly by Gowland in 1901 and partly by Atkinson on two occasions, in 1956 and 1958. There are two radiocarbon dates from samples that appear to be from the pit, but context details are missing and we can’t be sure exactly where they came from, and whether or not they were in pits dug into the filled larger pit; I don’t think we can trust these to age the big pit, which like that by the Heelstone, remains undated.
Both of these could be explained as filled natural hollows that once contained larger local sarsens. To the north-east, we may be looking at the stone that was dug out and raised, the Heelstone. To the south-west, we can only guess. It’s such a large pit, it might have held the tallest stone, trilithon Stone 56 which now stands at the end of the pit. I suggested Stone 16 as a possible candidate, because of its odd shape.
Thursday, 6 March 2025
The last glaciers of the Wicklow Mountains
This is an interesting article which looks at the evidence for the last small glaciers in the Wicklow Mountains, in Younger Dryas / Zone III / Loch Lomond / NS times, around 12,000 years ago. There are interesting comparisons with other Irish mountain areas and with Scotland, where the extent of this new glacierisation was much more dramatic.
These small glaciers -- just seven of them -- can be classified as cirque glaciers, and the authors incorporate evidence of three types of associated moraines, each one dependent upon certain glaciological conditions. Three of the studied glaciers do not look much like cirque glaciers at all, but more like elongated snowpatches or snowfields on NE-facing steep slopes where snowdrift accumulations occurred. Were these really small glaciers (with flowing ice capable of transporting detritus) or were they small firn fields fronted by pro-talus ramparts or ridges of frost-shattered debris that simply slid down the snow surface from exposed cliff edges? I would have liked something in the article about stone and boulder shapes in the three moraine types, which might have given us a clue........
But these are small matters, and the cosmogenic dating evidence presented by the authors (based on the sampling of morainic boulder surfaces) is rather convincing.
Lauren Knight, Clare M. Boston, Harold Lovell, Timothy T. Barrows, Eric A. Colhoun, David Fink, Nicholas C. Pepin. 05 March 2025Restricted cirque glaciers in the Wicklow Mountains, Ireland, during the Nahanagan Stadial (Greenland Stadial-1/Younger Dryas).
In Ireland, the Nahanagan Stadial (NS) was characterised by cirque glacier, plateau icefield and mountain ice cap expansion and is named after the cirque glacier type-site of Lough Nahanagan in the Wicklow Mountains. This period is broadly equivalent to the Younger Dryas Stadial and Greenland Stadial-1 (GS-1: ~12.9–11.7 ka). Here, we provide the first evaluation of the full extent of NS glaciation in the Wicklow Mountains by combining solar radiation modelling, mapping of glacial geomorphology, 10Be and 26Al cosmogenic surface exposure dating, 3D glacier reconstructions and analysis of snowblow and avalanching potential. We identify seven sites that hosted cirque glaciers at this time. Glacier extent was very restricted, with most glaciers only partially filling their cirques. Equilibrium line altitudes (ELAs) ranged from 470 ± 5 m a.s.l. (Lough Nahanagan) to 721 ± 5 m a.s.l. (Lough Cleevaun), with an average ELA of 599 m a.s.l. Higher snowblow and avalanching contributions at sites with lower ELAs demonstrate local topoclimatic influence on glacier growth and preservation alongside regional climate. The Wicklow Mountains provides a good example of marginal cirque glaciation during GS-1 and the importance of local topography and microclimate for sustaining glaciers in some mountain areas of Britain and Ireland.
Tuesday, 4 March 2025
The hunt for the Morvil Scottish erratic.....
Reference: Burt, C., Aspden, J., Davies, J., Hall, M., Schofield, D., Sheppard, T., Waters, R., Wilby, P., Williams, M. (2012). Geology of the Fishguard district: a brief explanation of the geological map Sheet 210 Fishguard. British Geological Survey.
https://webapps.bgs.ac.uk/memoirs/docs/B06909.html