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Abstract

The Altar Stone at Stonehenge in Wiltshire, UK, is enigmatic in that it differs markedly from the other bluestones. It is a grey-green, micaceous sandstone and has been considered to be derived from the Old Red Sandstone sequences of South Wales. Previous studies, however, have been based on presumed derived fragments (debitage) that have been identified visually as coming from the Altar Stone. Portable X-ray fluorescence (pXRF) analyses were conducted on these fragments (ex situ) as well as on the Altar Stone (in situ). Light elements (Z

Keywords

Stonehenge; Altar Stone; sandstone; debitage; portable XRF; provenancing

Published in

Mineralogical Magazine
2022, volume: 86, number: 4, article number: PII S0026461X22000226
Publisher: MINERALOGICAL SOC

SLU Authors

UKÄ Subject classification

Geology
Archaeology

Publication identifier

  • DOI: https://doi.org/10.1180/mgm.2022.22

Permanent link to this page (URI)

https://res.slu.se/id/publ/116810