A Saturday afternoon lecture by Richard Bevins at the Wiltshire Museum. 21st November 2015
Stonehenge is arguably one of the most famous prehistoric monuments in the World. It is renowned for the enormous size of the sarsen monoliths used in its construction which comprise the Outer Circle and Outer Horseshoe. It is generally agreed that these stones were sourced from the Marlborough Downs area, some 30 km to the north of Stonehenge. However, a set of smaller stones, comprising the Inner Circle, the Inner Horseshoe and the Altar Stone, are exotic to the Salisbury Plain area; these are the so-called bluestones, and have been the subject of investigations since the latter part of the 19th Century. Early petrographical studies recognised that the bluestones largely comprise a range of altered volcanic, intrusive and tuffaceous rocks with rarer sandstones but could not provide a definitive source.
However, it was the seminal paper by H.H. Thomas in 1923 that persuasively demonstrated that the spotted dolerite component of the bluestones could be sourced to outcrops exposed towards the eastern margin of Mynydd Preseli in southwest Wales, citing the tors Carn Meini and Cerrigmarchogion as the most likely sources. Thomas also argued that other lithologies in the bluestone assemblage, notably the rhyolites and the ‘calcareous ash’, could be sourced in the same locale, in particuar from Carn Alw and the northern slopes of Foel Drygarn respectively.
The first major investigation of the geochemistry of bluestone assemblage was by Richard Thorpe and team who compared whole rock wavelength-dispersive X-ray fluorescence spectrometry analyses from both orthostats and debitage at Stonehenge with whole rock analyses from Mynydd Preseli
Using petrography, mineral chemistry and whole rock geochemistry Richard Bevins and Rob Ixer have re-examined the proposed source of the bluestone rhyolites and determined that Carn Alw, as proposed by Thomas, is not the source of bluestone rhyolite; instead they argued that the majority of the rhyolite debitage from the Stonehenge Landscape (but not the four rhyolitic/dacitic standing or recumbent orthostats) comes instead from a prominent outcrop called Craig Rhos y felin, located on low ground to the north of the Mynydd Preseli range in the vicinity of Brynberian. More recently they have re-examined the spotted and non-spotted dolerites and concluded that a large % of the dolerite fragments and cored samples from Stonehenge come from Carn Goedog rather than Carn Meini.
Dr Richard Bevins as Keeper and Head of the Department of Natural Sciences at the National Museum Wales in Cardiff is responsible for Strategic leadership for collections and research related activities within the Department.
Qualifications, memberships and relevant positions:
BSc (Hons) Geology (Aberystwyth University), PhD (Keele), Fellow (Geological Society of London), Chartered Geologist (CGeol), Fellow (Society of Antiquaries of London), Honorary Lecturer (School of Earth & Ocean Sciences, Cardiff University), Chair, Geological Society of London’s Geoconservation Committee, Member of the Geological Society of London’s External Relations Committee, Chair of the British Geological Survey’s National Geological Repository Advisory Committee.
Primary research area is centred on the the Caledonian igneous history of Wales and related areas, as well as on their low-grade metamorphism. More recent work has focussed on extending the petrology and geochemistry of altered igneous rocks from Pembrokeshire into a re-examination of the source of the Stonehenge bluestones.
Saturday afternoon lectures start at 2.30pm and last approx. one hour.
Our Lecture Hall is accessible via a lift if required, has a hearing loop and air conditioning.
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