Thursday, 6 February 2025

The source of the quartz at Newgrange

I gather that misinformation about the stones of Newgrange is being strewn across the interweb.

So quickly here is the present state of knowledge:

"Newgrange, a Neolithic monument built around 3200 BCE,in Ireland's Boyne Valley, is renowned for its intricate architecture and the variety of stones used in its construction.  The stones that make up Newgrange were sourced from diverse locations, reflecting the builders' ability to transport and utilize materials from across the region.

The Newgrange mound is primarily composed of thousands of water-rolled stones gathered from the nearby River Boyne. These stones, weighing approximately 200,000 tonnes, form the bulk of the cairn. The inner passageway and outer kerbstones are made of greywacke, a type of stone that was likely collected from the rocky beach at Clogherhead, County Louth, about 20 km to the northeast.

The exterior of Newgrange features a striking array of decorative stones, including:

White Quartz Cobbles: These were transported from the Wicklow Mountains, approximately 50 km to the south. The quartz stones were used to create a facade that has been reconstructed in modern times.

Dark Speckled Granodiorite Cobbles: Originating from the Mourne Mountains, about 50 km to the north, these stones add a distinctive element to the monument's design.

Dark Gabbro Cobbles: Sourced from the Cooley Mountains, these stones contribute to the complex's visual appeal.

Inside the chambers, granite basins were used, which were brought from the Mournes. These basins are significant not only for their material but also for their role in the structure's function, possibly as repositories for the remains of the dead." 

From: https://www.perplexity.ai/search/write-a-blog-post-with-referen-53n66lYrS06qukqxIX0kqQ#0



Click to enlarge - from: Notes on Some Non-Local Cobbles at the Entrances to the Passage-Graves at Newgrange and Knowth, County Meath Frank Mitchell The Journal of the Royal Society of Antiquaries of Ireland, Vol. 122 (1992), pp. 128-145 (18 pages) https://www.jstor.org/stable/25509025 


And supporting this there is, for the academics with access, the magisterial: 

Meighan, I.G., Simpston, D.D.A., Hartwell, B.N., Fallick, A.E. and Kennan, P.S. (2003) Sourcing the quartz at Newgrange, Bru na Boinne, Ireland. In: Burenhult, G. and Westergaard, S. (eds.) Stones and Bones: Formal Disposal of the Dead in Atlantic Europe During the Mesolithic-Neolithic Interface 6000-3000 BC: Archaeological Conference in Honour of the Late Professor Michael J. O'Kelly. Series: BAR international series (1201). Archaeopress: Oxford, UK, pp. 247-251. ISBN 9781841715667

There is no evidence to show that any quartz stones were brought onto the site during the reconstruction. O'Kelly excavated the "numerous angular fragments" he used from in front of the monument. Whether his reconstruction is in any way accurate is another matter. 

O’Kelly, M.J. (1979) ‘The restoration of Newgrange’, Antiquity, 53(209), pp. 205–210. doi:10.1017/S0003598X00042538.




Sunday, 2 February 2025

The Combined Viewshed of the Tor and Cuckoo Stones.

 The new paper on the Tor and Cuckoo Stone* posits that: "The intervisibility of the two stones is likely to have been an essential feature of their locations, near the boundaries of their respective overlapping viewsheds,... the DTM indicates that a transect drawn between the two stones  passes close to the apex of a meander in the River Avon at a point where it is approximately equidistant from each stone and potentially intervisible, both from and towards both stones.

The paper has shows their individual viewsheds but not them combined. Simply overlaying the two figures and tweaking the colours gives the combined viewshed. 


Click to enlarge - all rights remain with the original paper


The mustard colour shows where both stones would be visible from, I thought they might have acted as pillars visible either side from the route through the landscape but that doesn't seem to be. But the apex of the river meander could be important. More to ponder on.

*HARDING, P. et al. (2025) ‘Earliest Movement of Sarsen Into the Stonehenge Landscape: New Insights from Geochemical and Visibility Analysis of the Cuckoo Stone and Tor Stone’, Proceedings of the Prehistoric Society, pp. 1–23. doi:10.1017/ppr.2024.13.

Friday, 31 January 2025

None of the Stonehenge Stones are Local

The new paper on the Cuckoo and Tor stones (*) posits that they are not local to Salisbury Plain and were brought from West Woods. It goes further and claims that no large numbers of large sarsens with a chemistry the same as those at West Woods are likely to have originated near Stonehenge.

This is surprising. They debate the obvious question here:

https://www.cambridge.org/core/journals/proceedings-of-the-prehistoric-society/article/earliest-movement-of-sarsen-into-the-stonehenge-landscape-new-insights-from-geochemical-and-visibility-analysis-of-the-cuckoo-stone-and-tor-stone/C7C6D363A6E59D0BBF5C3158077ABB24#s4

Geological implications

Our inference that the Cuckoo Stone and Tor Stone probably originated in the West Woods area directly challenges the suggestion made by Richards (Reference Richards and Parker2020) that both stones were either already situated at, or close to, their source locations when they were monumentalised. There is, however, a potential counter argument that would support Richards’ view: rather than the two stones being moved from West Woods, could it be that large sarsen boulders with a geochemistry similar to those at West Woods were already present in the Stonehenge landscape near the sites where the two stones were raised?

Their answer is no and I find their reasoning compelling.




* HARDING, P. et al. (2025) ‘Earliest Movement of Sarsen Into the Stonehenge Landscape: New Insights from Geochemical and Visibility Analysis of the Cuckoo Stone and Tor Stone’, Proceedings of the Prehistoric Society, pp. 1–23. doi:10.1017/ppr.2024.13.

Thursday, 30 January 2025

Earliest Movement of Sarsen Into the Stonehenge Landscape:

Earliest Movement of Sarsen Into the Stonehenge Landscape: New Insights from Geochemical and Visibility Analysis of the Cuckoo Stone and Tor Stone


Abstract: This paper presents the results of new research on two sarsen stones, known as the Cuckoo Stone and Tor Stone, both former standing stones that lie on opposite banks of the River Avon and straddle the eastern border of the Stonehenge and Avebury World Heritage Site. Geochemical analysis indicates that both stones were probably transported to their present site from West Woods on the Marlborough Downs in north Wiltshire, a source that likely also supplied the large sarsen monoliths at Stonehenge. The paper examines the geological conditions necessary for the formation of sarsen across the site of the present-day Salisbury Plain to address the apparent absence of natural sarsen in the area. The results are integrated with those of archaeological fieldwork from nearby contemporaneous sites to suggest that the Cuckoo Stone and Tor Stone were probably introduced into the Stonehenge landscape in the early part of the Late Neolithic period, ie, contemporary with Phase 1 of Stonehenge and some 400–500 years before the construction of the principal sarsen settings at the monument. Visibility analysis indicates that the two stones were probably intervisible and likely to have formed part of a planned landscape and were positioned to create a formal portal to the Stonehenge area on either bank of the River Avon.




HARDING, P. et al. (2025) ‘Earliest Movement of Sarsen Into the Stonehenge Landscape: New Insights from Geochemical and Visibility Analysis of the Cuckoo Stone and Tor Stone’, Proceedings of the Prehistoric Society, pp. 1–23. doi:10.1017/ppr.2024.13.


Wednesday, 22 January 2025

Stonehenge and its Altar Stone: the significance of distant stone sources

The long awaited MPP article on Stonehenge has arrived:



Locations of stone sources for Stonehenge (red) and Brú na Bóinne passage tombs (green). The location of the source of the Altar Stone is only approximate. Other sites mentioned in the text are in grey


Abstract

Geological research reveals that Stonehenge’s stones come from sources beyond Salisbury Plain, as recently demonstrated by the Altar Stone’s origins in northern Scotland more than 700 km away. Even Stonehenge’s huge sarsen stones come from 24 km to the north, while the bluestones can be sourced to the region of the Preseli Hills some 225 km away in west Wales. The six-tonne Altar Stone is of Old Red Sandstone from the Orcadian Basin, an area that extends from the Northern Isles of Orkney and Shetland to Inverness and eastwards to Banff, Turriff and Rhynie. Its geochemical composition does not match that of rocks in the Northern Isles, so it can be identified as coming from the Scottish mainland. Its position at Stonehenge as a recumbent stone within the southwest arc of the monument, at the foot of the two tallest uprights of the Great Trilithon, recalls the plans of recumbent stone circles of north-east Scotland. Unusually strong similarities in house floor layouts between Late Neolithic houses in Orkney and the Durrington Walls settlement near Stonehenge also provide evidence of close connections between Salisbury Plain and northern Scotland. Such connections may be best explained through Stonehenge’s construction as a monument of island-wide unification, embodied in part through the distant and diverse origins of its stones.


Parker Pearson, M., Bevins, R., Bradley, R., Ixer, R., Pearce, N. & Richards, C., (2025) “Stonehenge and its Altar Stone: the significance of distant stone sources”, Archaeology International 27(1). doi: https://doi.org/10.14324/AI.27.1.13

Sunday, 19 January 2025

The Altar Stone Source - the essential points

The research paper provides key evidence indicating that the Stonehenge Altar Stone likely originated from a Laurentian rock source. Here's a breakdown of the significant points:

Mineral Composition and Age

The researchers analyzed three types of mineral grains found in the Altar Stone fragments:

1. Detrital zircon: Largely composed of Mesoproterozoic and Archaean sources (very old, ranging from about 1 to 3.5 billion years) [1][3].

2. Rutile and apatite: Dominated by a mid-Ordovician source (approximately 460 million years old) [1][3].

Laurentian Origin

The ages of these grains strongly suggest derivation from a Laurentian crystalline source region [1][3]. Laurentia refers to the ancient continental craton that formed the core of North America and Greenland[2]. This is significant because:

- The presence of very old zircon grains (Mesoproterozoic and Archaean) matches igneous events in Laurentia [2].

- These events did not occur in other terranes like Gondwana, Ganderia, Meguma, or East Avalonia, which now form most of England and Wales[2].

Grampian Overprint

The mid-Ordovician ages (around 460 million years ago) of the rutile and apatite grains indicate that the Laurentian source region was overprinted by Grampian magmatism [1][3]. This refers to a phase of the Caledonian orogeny, a major mountain-building event that affected what is now Scotland.

Similarity to Orcadian Basin

Detrital age comparisons with sedimentary rocks throughout Britain and Ireland revealed a remarkable similarity between the Altar Stone and the Old Red Sandstone of the Orcadian Basin in northeast Scotland [1][3]. This basin includes parts of northeastern Scotland, Orkney, and Shetland [2].

This evidence collectively points to a Scottish origin for the Altar Stone, specifically from an area north of the Iapetus Suture, where rocks with Laurentian characteristics are found [2]. 

But not Orkney 

However, a follow-up study published in September 2024 in the Journal of Archaeological Science: Reports specifically examined megaliths from Orkney and concluded that the Altar Stone was not sourced from Mainland Orkney. This research used portable X-rays to analyze stones at the Stones of Stenness and the Ring of Brodgar, comparing their composition to that of the Altar Stone [4].

.

Citations:

[1] https://www.nature.com/articles/s41586-024-07652-1

[2] https://www.megalithic.co.uk/article.php?sid=2146415628

[3] https://research.aber.ac.uk/en/publications/a-scottish-provenance-for-the-altar-stone-of-stonehenge

[4] https://doi.org/10.1016/j.jasrep.2024.104738

Saturday, 18 January 2025

Unearthing Britain's Darkest Chapter: The Early Bronze Age Massacre at Charterhouse Warren

A recent study has shed light on one of prehistoric Britain’s most gruesome episodes: the massacre of at least 37 individuals at Charterhouse Warren, Somerset, around 4,000 years ago. This discovery, led by Professor Rick Schulting of the University of Oxford, challenges the notion of the Early Bronze Age as a peaceful era and reveals a chilling narrative of violence and dehumanization.

The Discovery


The remains—over 3,000 bone fragments—were first unearthed in the 1970s but largely overlooked until now. Found in a 15-meter-deep natural shaft, these bones belonged to men, women, and children, with nearly half being adolescents. The evidence indicates that the victims were killed, dismembered, and possibly cannibalized before their remains were discarded.

Gruesome Evidence


Analysis revealed cut marks, shattered skulls, and signs of defleshing and marrow extraction. Some bones even bore human bite marks. Researchers believe this brutality was not driven by survival needs but as an act of ritualistic "othering" or vengeance. The attackers likely sought to dehumanize their victims and send a powerful message to others.

Significance


This massacre represents the largest known act of interpersonal violence in Early Bronze Age Britain. It starkly contrasts with the era’s typical archaeological focus on trade, farming, and burial practices. The findings highlight how prehistoric communities were capable of extreme violence akin to modern atrocities

Schulting RJ, Fernández-Crespo T, Ordoño J, et al. ‘The darker angels of our nature’: Early Bronze Age butchered human remains from Charterhouse Warren, Somerset, UK. Antiquity. Published online 2024:1-17. doi:10.15184/aqy.2024.180