It seems surprising that the number of entrances that Durrington Walls originally had is uncertain.
1, 2, 4 and even 3 have been suggested.
It seems surprising that the number of entrances that Durrington Walls originally had is uncertain.
1, 2, 4 and even 3 have been suggested.
The route that the great sarsens were brought from the Marlborough Downs to Stonehenge is still debated. This blog was started to investigate it and it is still of interest.
I am using 40 tonnes as the maximum weight of an untrimmed sarsen that was moved. The raft or sledge it was moved on then adds to this weight.
The idea that they were brought down the River Avon from Upavon to Amesbury is still popular despite the impossibility of it.
The River Avon we see now isn't the same as it was in Neolithic times, the main difference is that it has historically been dredged, over-widened and impounded in many places due to past river management.
It would have been a multichannel meandering stream in a marshy valley bottom with trees and bushes growing over and in it.
1) They weren't slid on the frozen river.
The River Avon is largely fed from ground water along its route, water that is referred to as warm during the winter as it stays at near constant temperature all year round. The river doesn't freeze solid and according to Gold's Formula the ice would need to be over 500mm thick
The River at Amesbury has a normal maximum depth of 700mm and is usually half of that, and at Upavon it is a lot less.
2) They weren't loaded onto rafts and floated down.
To float 40 tonnes of stone 40 cubic metres of water must be displaced. If we had a weightless box to load the stone on it would need to be 4 metres wide, 20 metres long and 500mm deep, the depth of the river being a limiting factor here.
A wooden raft made of logs would need to be much larger. Wood has a specific gravity of 500 - 800 kg per m3 . The photo shows how only half of a log raft is out of the water. At the lightest end the raft would need to weigh another forty tonnes to displace enough water, at a more realistic weight for hardwoods of 750kg/m3 it nearly 100 tonnes. A forty five meter by five meter wide raft at 500 mm deep. The river is not big enough.
Only by using hollowed logs or canoes could the weight and size of the raft be reduced but would they be strong enough for the massive stones?
Dragging heavy stones through an overgrown bog didn't happen, they went overland away from the river.
A very detailed look at the Bluestone quarries and the associated stone tools discovered there.
Abstract: Excavations at two of the sources of Stonehenge’s bluestones in Mynydd Preseli, west Wales, have led to the discovery of stone tools associated with megalith quarrying in the final centuries of the fourth millennium BC, shortly before the suspected date of the bluestones’ erection at Stonehenge, 240 km away. Among the most plentiful of these tools are stone wedges, three of which were found in situ at the rhyolite bluestone quarry of Craig Rhos-y-felin. Two of these were positioned in the joints of a rhyolite pillar adjacent to a recess left by a removed pillar. Geochemical analysis reveals that these and the third wedge are of compositions different to the rock on either side of the cracks into which they had been driven, confirming their identification as quarrying tools. This research sheds new light on the methods used to extract the stones for Stonehenge.
Mike Parker Pearson, Richard Bevins, Nick Pearce, Rob Ixer, Josh Pollard, Colin Richards, Kate Welham
Journal of Archaeological Science: Reports,
Volume 46,
2022,
103697,
ISSN 2352-409X,
https://doi.org/10.1016/j.jasrep.2022.103697
(https://www.sciencedirect.com/science/article/pii/S2352409X22003601)
Keywords: Megalith quarries; Dolerite; Rhyolite; Stonehenge; Mynydd Preseli; Neolithic
Mythical rings? Waun Mawn and Stonehenge Stage 1 by Timothy Darvill
"In a recent
Antiquity article, Parker Pearson
and colleagues (2021) presented
results from excavations at Waun
Mawn in south-west Wales, interpreting the site
as a dismantled stone circle and source
for some of the Bluestone
pillars used in the Aubrey Holes at Stonehenge. Here, the author examines the evidence, showing that alternative
interpretations are possible. Waun Mawn is argued to represent a series of smaller
stone settings, typical of ceremonial sites in
south- west Wales. Meanwhile
the Aubrey Holes are shown to reflect a well-established regional
sequence in which post circles are followed by pit circles. A Welsh
‘source-circle’ for
Stonehenge cannot be excluded but, the author
argues, the claim is unsupported by the current evidence."
Darvill plan showing the recorded stones
and stone-sockets at Waun Mawn,
Pembrokeshire (figure by G. Belmont
after Grimes 1964: fig. 36 and Parker Pearson
et
al. 2021: fig. 4a).
|
Name |
Longitude |
Latitude |
|
|
1 |
Castle Hill, Blunsdon St Andrew |
-1.77441 |
51.61914 |
|
2 |
Bury Hill Camp, Purton |
-1.9183 |
51.60967 |
|
3 |
Nuns Walk, Malmesbury. |
-2.09482 |
51.58369 |
|
4 |
Ringsbury Camp |
-1.89333 |
51.57961 |
|
5 |
Liddington Castle |
-1.70066 |
51.51583 |
|
6 |
Bincknoll Castle |
-1.84618 |
51.51221 |
|
7 |
Barbury Castle |
-1.78635 |
51.48527 |
|
8 |
Membury Camp |
-1.56636 |
51.47567 |
|
9 |
Bury Wood Camp |
-2.2632 |
51.46427 |
|
10 |
Nash Hill |
-2.09702 |
51.42346 |
|
11 |
Oldbury Castle |
-1.93037 |
51.42246 |
|
12 |
Chisbury Camp |
-1.60051 |
51.39205 |
|
13 |
Oliver's Castle |
-1.99994 |
51.38113 |
|
14 |
Rybury Camp |
-1.88173 |
51.37463 |
|
15 |
Martinsell Hill Camp |
-1.7514 |
51.37447 |
|
16 |
Giant's Grave |
-1.76244 |
51.36796 |
|
17 |
Budbury |
-2.25754 |
51.34854 |
|
18 |
Godsbury |
-1.68904 |
51.31853 |
|
19 |
Fosbury Camp |
-1.54311 |
51.30692 |
|
20 |
Broadbury Banks |
-1.86838 |
51.29888 |
|
21 |
Castle Combe |
-2.14601 |
51.29561 |
|
22 |
Sunton |
-1.65939 |
51.28765 |
|
23 |
Chisenbury Camp |
-1.78358 |
51.28374 |
|
24 |
Casterley Camp |
-1.83531 |
51.28101 |
|
25 |
Bratton Castle |
-2.14302 |
51.26376 |
|
26 |
Sidbury Camp |
-1.6913 |
51.25365 |
|
27 |
Battlesbury Camp |
-2.14668 |
51.20994 |
|
28 |
Cley Hill Camp |
-2.23204 |
51.20298 |
|
29 |
Scratchbury Camp |
-2.1262 |
51.19727 |
|
30 |
Knook Castle |
-2.05856 |
51.19553 |
|
31 |
Vespasian's Camp |
-1.79108 |
51.17399 |
|
32 |
Codford Circle |
-2.02644 |
51.16419 |
|
33 |
Yarnbury Castle |
-1.95097 |
51.16271 |
|
34 |
Ludgershall Castle |
-1.37222 |
51.15252 |
|
35 |
Ogbury Camp |
-1.79669 |
51.14368 |
|
36 |
Bilbury Rings |
-1.98711 |
51.12541 |
|
37 |
Grovely Castle |
-1.93238 |
51.12132 |
|
38 |
Ebsbury Hill |
-1.91339 |
51.11762 |
|
39 |
Park Hill Camp |
-2.33901 |
51.11122 |
|
40 |
White Sheet Castle |
-2.28097 |
51.11032 |
|
41 |
Figsbury Ring |
-1.73232 |
51.10337 |
|
42 |
Kenwalch's Castle |
-2.36163 |
51.10056 |
|
43 |
Old Sarum |
-1.80464 |
51.09337 |
|
44 |
Wick Ball Camp |
-2.00071 |
51.08687 |
|
45 |
Castle Ditches, Tisbury |
-2.0533 |
51.05463 |
|
46 |
Chiselbury |
-1.97559 |
51.05239 |
|
47 |
Great Woodbury |
-1.79653 |
51.04969 |
|
48 |
Odstock Copse |
-1.79517 |
51.02569 |
|
49 |
Castle Rings, Donhead St Mary |
-2.16153 |
51.02501 |
|
50 |
Clearbury Ring |
-1.78401 |
51.01836 |
|
51 |
Winklebury Camp |
-2.06945 |
50.99478 |
|
52 |
The Earldoms |
-1.64684 |
50.99299 |

That pigs, cattle, humans and even a dog came to the Stonehenge area from distant parts in prehistory has been one of the more interesting scientific discoveries of recent times. The links to Orcadian culture has also been speculated on.
Behind the headlines and speculation there is solid research - some links to start from:
Evans, J., Parker Pearson, M., Madgwick, R. et al. Strontium and oxygen isotope evidence for the origin and movement of cattle at Late Neolithic Durrington Walls, UK. Archaeol Anthropol Sci 11, 5181–5197 (2019). https://doi.org/10.1007/s12520-019-00849-wThere seems to be some confusion as to what the latest scientific consensus by the relevant experts in glaciation is with regards to Stonehenge.
TL;DR summary: They acknowledge their models aren't quite working with how far the ice spread out into the Celtic sea, but when they tweak the current model to correct that it brings ice down into the south west of England where there is no evidence for it apart from a hypothesis of glacial erratics at or on their way to Stonehenge. They prefer the hypothesis that they are missing an input in their model and if that was corrected the model would match the reality better, which doesn't include glaciers in the south west of England.
An egregious mismatch occurred at 26 ka, where the modelled grounding line position of the Irish Sea Ice Stream fell 150 km behind that indicated by the geological evidence (minimum reconstruction, Fig. 6; Scourse et al. 2021). We experimented with various nudges to the model to try and prevent this underrun but they resulted in significant overruns of other parts of the ice sheet, notably with the SW Peninsula of England (Cornwall and Devon) and much of the English Midlands becoming glaciated. The final choice of model run (Fig. 6) is therefore a compromise that mostly fits the wider empirical limits, but underruns in the Celtic Sea. The alternative choice of accepting a model run that reached the shelf edge in the Celtic Sea but also glaciated the SW Peninsula and parts of the English Midlands would have interesting implications for the long-standing hypothesis that some of the stones of Stonehenge may have been transported, at least partway as glacial erratics (e.g. Judd 1902; Scourse 1997; John 2018; Pearson et al. 2019). Although this may indeed be accommodated by earlier more extensive glaciations, we suggest however, that a process, forcing, or feedback is missing in the numerical modelling we present here and that once discovered would enable sufficient ice advance in the Celtic Sea without exceeding ice limits elsewhere. For example, Scourse et al. (2021) suggest that a non-steady oscillation (surge) arose as a release from the build-up of ice behind a topographic constriction in the Irish Sea. We further speculate that the drainage of lakes on the ice stream surface, or floods from subglacial lakes, may have temporarily facilitated faster ice flow and ‘over-extension’ of the ice margin by locally increasing basal lubrication.
From:
https://onlinelibrary.wiley.com/share/T7PBKPTRFPBVRJJCXSJU?target=10.1111/bor.12594
Clark, C.D., Ely, J.C., Hindmarsh, R.C.A., Bradley, S., Ignéczi, A., Fabel, D., Ó Cofaigh, C., Chiverrell, R.C., Scourse, J., Benetti, S., Bradwell, T., Evans, D.J.A., Roberts, D.H., Burke, M., Callard, S.L., Medialdea, A., Saher, M., Small, D., Smedley, R.K., Gasson, E., Gregoire, L., Gandy, N., Hughes, A.L.C., Ballantyne, C., Bateman, M.D., Bigg, G.R., Doole, J., Dove, D., Duller, G.A.T., Jenkins, G.T.H., Livingstone, S.L., McCarron, S., Moreton, S., Pollard, D., Praeg, D., Sejrup, H.P., Van Landeghem, K.J.J. and Wilson, P. (2022), Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE-CHRONO reconstruction. Boreas. https://doi.org/10.1111/bor.12594