(Dolerite Chip in the
Alexander Keiller Museum - Tim Daw)
The discovery of Stonehenge bluestone fragments from the top
of Silbury Hill has provoked enduring debate, amid stratigraphic and
petrological ambiguities. In the latest WANHM, Wiltshire Archaeological and
Natural History Magazine, Ixer, Bevins, and Pollard (2025), https://www.academia.edu/144003051/Slbury_Hill_lithics
, provide a meticulous reappraisal,
synthesising archival data with advanced microscopy to affirm these as
deliberate human-transported debitage. A pivotal contribution lies in
clarifying the corpus's fraught discovery history, particularly the discrepancy
between Atkinson's published account—mentioning only a volcanic tuff—and the
separate archival identification of a spotted dolerite via a museum label, a
mismatch that has long muddled interpretations.
Five fragments comprise the corpus: four flaked spotted
dolerites ('preselite') and one volcanic tuff (initially termed 'volcanic
ash'). Atkinson's 1970 Antiquity note records just one find from an
"undisturbed" summit context: the tuff fragment (Wilts 391),
macroscopically identified as akin to Stonehenge's volcanic ash bluestone and
recovered from clean chalk rubble ~0.7 m below the surface (Atkinson 1970,
314). Its pairing with a 'Windmill Hill ware' sherd—later deemed likely
Anglo-Saxon—hinted at disturbance, undermining claims of Neolithic integrity.
Unmentioned in Atkinson’s account but documented via a bag label in the
Alexander Keiller Museum archive, is a second fragment from the 1969 topsoil: a
spotted dolerite specimen. Three additional spotted dolerites surfaced from
2007 subsoil excavations, all lacking secure prehistoric associations (Ixer
2013). This selective reporting—overlooking the labelled dolerite—has sown
confusion, with the tuff often conflated with the dolerite or dismissed as
intrusive, as noted in subsequent syntheses (Field & Leary 2010, 60–61).
Post-excavation analyses amplified uncertainties. Wilts 391,
the thin section derived from Atkinson's tuff fragment and prepared in the
1970s for the South West Implement Petrology Collection, was erroneously
identified by R. V. Davis as Cornish hornblende schist, emphasising 'decomposed
feldspar' (misread sparry calcite) while disregarding its clastic tuff fabric
and Atkinson's macroscopic assessment (Clough & Cummins 1988, 162). The
original rock specimen vanished, likely consumed in sectioning, prompting
further conflations. Such lapses, compounded by incomplete documentation,
invited speculation of post-Neolithic intrusion—via antiquarian activity or
medieval remodelling (Field & Leary 2010, 60–61).
Ixer et al. (2025) disentangles this 'conundrum' through
rigorous petrography, confirming all five as Stonehenge-sourced debitage and
explicitly resolving the Atkinson-label disconnect by cross-referencing museum
records with fieldwork archives. Wilts 391 exemplifies calcite-bearing Andesite
Group A tuff, with limonite-stained 'rhyolite' clasts (fine-grained white
mica-albite-chlorite-quartz intergrowths), vesicular lava inclusions, and
tension gashes—hallmarks matching buried orthostat 32c from north Pembrokeshire's
Fishguard Volcanic Group (Ixer et al. 2023). The dolerites, including the
labelled 'Museum' piece, exhibit ophitic textures, epidotisation, and spinel
spots diagnostic of 'preselite'. This validates Atkinson's intuition while
exposing Davis's oversights, attributing the sherd to localised disturbance
rather than wholesale rejection of Neolithic deposition.
Crucially, the authors dismiss glacial transport—once
invoked for bluestone dissemination (e.g., Ixer 2009)—citing the flakes'
knapped morphology, sub-centimetre scale, and orthostat-specific matches, which
preclude Ice Age entrainment. Instead, they propose intentional Late Neolithic
conveyance and deposition during Silbury's final phases (~late 24th/early 23rd
century BC; Marshall et al. 2013), likely by Beaker-period groups effecting
ritual fragmentation. This echoes Darvill and Wainwright's (2009) model for
Stonehenge and parallels Cheviot granodiorite at West Kennet palisade (Ixer et
al. 2022), suggesting token exotics as apotropaic or mnemonic elements in a
networked monumental landscape (Richards et al. 2020).
As a review, Ixer et al. excels in transforming archival
detritus into interpretive clarity, elevating these four small dolerite chips
and single tuff flake to evidence of modest Wessex-wide mobility—chiefly by
demystifying the Atkinson-dolerite enigma. Whether the fragments derive from a
single larger piece or multiple orthostats remains unresolved, though their
petrological affinities suggest the four dolerite chips are all off one block.
Only Wilts 391 enjoys unambiguous Neolithic security, however, tempering
conclusions.
My own speculative thought experiment based on the overland
bluestone transport hypothesis positing an A40-aligned route from Preseli, with
a River Severn crossing near Gloucester (Parker Pearson et al. 2015) the
Avebury landscape lies on this natural route to Stonehenge. Are the chips from Stonehenge or souvenirs of a
passing monolith, maybe from initial shaping nearby?
References
Atkinson, R.J.C., 1970. Silbury Hill, 1969–70. Antiquity,
44, pp.313–314. Available at: https://doi.org/10.1017/S0003598X00104582
Clough, T.H.McK. & Cummins, W.A. (eds.), 1988. Stone
Axe Studies Volume 2: The petrology of prehistoric stone implements from the
British Isles. Council for British Archaeology Research Report 67, London.
ISBN: 0-906780-52-7. Available at: https://www.cambridge.org/core/journals/antiquity/article/reviews-t-h-mck-clough-w-a-cummins-ed-stone-axe-studies-2-the-petrology-of-prehistoric-stone-implements-from-the-british-isles-279-pages-42-figures-240-tables-3-maps-1988-london-council-for-british-archaeology-research-report-67-isbn-0906780527-paperback-35/4D955A236D2703A06740E01B2E4C44AE
Darvill, T. & Wainwright, G., 2009. Stonehenge
excavations 2008. The Antiquaries Journal, 89, pp.1–19. DOI:
10.1017/S000358150900002x. Available at: https://eprints.bournemouth.ac.uk/11797/
Field, D. & Leary, J., 2010. The Story of
Silbury Hill. English Heritage, Swindon. ISBN: 9781848020467. Available
at: https://books.google.nl/books/about/The_Story_of_Silbury_Hill.html
Ixer, R.A., 2013. The spotted dolerite fragments. In: Leary,
J., Field, D., & Campbell, G. (eds.) Silbury Hill: the largest
prehistoric mound in Europe, pp.60–61. English Heritage, Swindon.
Ixer, R.A., Bevins, R.E., Pirrie, D. & Power, M., 2023.
Treasures in the Attic: Testing Cunnington's assertion that Stone 32c is the
‘type’ sample for Andesite Group A. Wiltshire Archaeological and
Natural History Magazine, 116, pp.40–52. https://pure.southwales.ac.uk/en/publications/treasures-in-the-attic-testing-cunningtons-assertion-that-stone-3
Ixer, R, Bevins, R, Pearce, N, Pirrie, D, Pollard, J,
Finlay, A, Power, M & Patience, I 2025, 'Exotic granodiorite lithics from
Structure 5 at West Kennet, Avebury World Heritage Site, Wiltshire, UK', Wiltshire
Archaeological and Natural History Magazine, vol. 118, pp. 1-18. Available
at: https://www.academia.edu/125773662/West_Kennet_Granodiorites [
Ixer, R.A., Bevins, R.E. & Pollard, J., 2025. Bluestones
from Silbury Hill. Wiltshire Archaeological & Natural History
Magazine, 118, pp.269–278. Available at: https://www.academia.edu/144003051/Slbury_Hill_lithics
Marshall, P., Bayliss, A., Leary, J., Pollard, J.,
Vallender, J. & Young, G., 2013. The Silbury chronology. In: Leary, J.,
Field, D. & Campbell, G. (eds.), Silbury Hill: the largest
prehistoric mound in Europe, pp.97–116. English Heritage, Swindon.
Parker Pearson, M. et al. (2015) ‘Craig
Rhos-y-felin: a Welsh bluestone megalith quarry for Stonehenge’, Antiquity,
89(348), pp. 1331–1352. https://www.cambridge.org/core/journals/antiquity/article/craig-rhosyfelin-a-welsh-bluestone-megalith-quarry-for-stonehenge/D1E66A287D494205D22881CBF1F6DDE8
.
Richards, C., Bayliss, A., Beadsmoore, L., Bronk Ramsey, C.,
Card, N., Dunbar, E., et al., 2009. The date of the Greater Stonehenge
Cursus. Antiquity, 83(319): pp.40–53. DOI:
10.1017/S0003598X00099363. Available at: https://www.researchgate.net/publication/233882913_The_Date_of_the_Greater_Stonehenge_Cursus
have you no knowledge of the Moon Maidens who used to dance naked at Stonehenge the dance atop Silbury on a summer solstice? They bought their offerings from far and wide. :)
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