Matches in SemOpenAlex for { <https://semopenalex.org/work/W3037083839> ?p ?o ?g. }
- W3037083839 endingPage "105188" @default.
- W3037083839 startingPage "105188" @default.
- W3037083839 abstract "The Altar Stone at Stonehenge is a greenish sandstone thought to be of Late Silurian-Devonian (‘Old Red Sandstone’) age. It is classed as one of the bluestone lithologies which are considered to be exotic to the Salisbury Plain environ, most of which are derived from the Mynydd Preseli, in west Wales. However, no Old Red Sandstone rocks crop out in the Preseli; instead a source in the Lower Old Red Sandstone Cosheston Subgroup at Mill Bay to the south of the Preseli, has been proposed. More recently, on the basis of detailed petrography, a source for the Altar Stone much further to the east, towards the Wales-England border, has been suggested. Quantitative analyses presented here compare mineralogical data from proposed Stonehenge Altar Stone debris with samples from Milford Haven at Mill Bay, as well as with a second sandstone type found at Stonehenge which is Lower Palaeozoic in age. The Altar Stone samples have contrasting modal mineralogies to the other two sandstone types, especially in relation to the percentages of its calcite, kaolinite and barite cements. Further differences between the Altar Stone sandstone and the Cosheston Subgroup sandstone are seen when their contained zircons are compared, showing differing morphologies and U-Pb age dates having contrasting populations. These data confirm that Mill Bay is not the source of the Altar Stone with the abundance of kaolinite in the Altar Stone sample suggesting a source further east, towards the Wales-England border. The disassociation of the Altar Stone and Milford Haven undermines the hypothesis that the bluestones, including the Altar Stone, were transported from west Wales by sea up the Bristol Channel and adds further credence to a totally land-based route, possibly along a natural routeway leading from west Wales to the Severn estuary and beyond. This route may well have been significant in prehistory, raising the possibility that the Altar Stone was added en route to the assemblage of Preseli bluestones taken to Stonehenge around or shortly before 3000 BC. Recent strontium isotope analysis of human and animal bones from Stonehenge, dating to the beginning of its first construction stage around 3000 BC, are consistent with the suggestion of connectivity between this western region of Britain and Salisbury Plain.This study appears to be the first application of quantitative automated mineralogy in the provenancing of archaeological lithic material and highlights the potential value of automated mineralogy in archaeological provenancing investigations, especially when combined with complementary techniques, in the present case zircon age dating." @default.
- W3037083839 created "2020-07-02" @default.
- W3037083839 creator A5018629884 @default.
- W3037083839 creator A5023609308 @default.
- W3037083839 creator A5027188683 @default.
- W3037083839 creator A5027563352 @default.
- W3037083839 creator A5034746928 @default.
- W3037083839 creator A5050210839 @default.
- W3037083839 creator A5077855027 @default.
- W3037083839 date "2020-08-01" @default.
- W3037083839 modified "2023-10-13" @default.
- W3037083839 title "Constraining the provenance of the Stonehenge ‘Altar Stone’: Evidence from automated mineralogy and U–Pb zircon age dating" @default.
- W3037083839 cites W1215896481 @default.
- W3037083839 cites W1596067340 @default.
- W3037083839 cites W1978253086 @default.
- W3037083839 cites W1978862323 @default.
- W3037083839 cites W1988392743 @default.
- W3037083839 cites W1991476194 @default.
- W3037083839 cites W1995831403 @default.
- W3037083839 cites W2006600330 @default.
- W3037083839 cites W2007105153 @default.
- W3037083839 cites W2031889172 @default.
- W3037083839 cites W2067260877 @default.
- W3037083839 cites W2070566812 @default.
- W3037083839 cites W2083475744 @default.
- W3037083839 cites W2120210793 @default.
- W3037083839 cites W2136958428 @default.
- W3037083839 cites W2195708234 @default.
- W3037083839 cites W2342124398 @default.
- W3037083839 cites W2534787226 @default.
- W3037083839 cites W2550093689 @default.
- W3037083839 cites W2805222059 @default.
- W3037083839 cites W2838875940 @default.
- W3037083839 cites W2915981654 @default.
- W3037083839 cites W2953842340 @default.
- W3037083839 doi "https://doi.org/10.1016/j.jas.2020.105188" @default.
- W3037083839 hasPublicationYear "2020" @default.
- W3037083839 type Work @default.
- W3037083839 sameAs 3037083839 @default.
- W3037083839 citedByCount "16" @default.
- W3037083839 countsByYear W30370838392020 @default.
- W3037083839 countsByYear W30370838392021 @default.
- W3037083839 countsByYear W30370838392022 @default.
- W3037083839 countsByYear W30370838392023 @default.
- W3037083839 crossrefType "journal-article" @default.
- W3037083839 hasAuthorship W3037083839A5018629884 @default.
- W3037083839 hasAuthorship W3037083839A5023609308 @default.
- W3037083839 hasAuthorship W3037083839A5027188683 @default.
- W3037083839 hasAuthorship W3037083839A5027563352 @default.
- W3037083839 hasAuthorship W3037083839A5034746928 @default.
- W3037083839 hasAuthorship W3037083839A5050210839 @default.
- W3037083839 hasAuthorship W3037083839A5077855027 @default.
- W3037083839 hasBestOaLocation W30370838392 @default.
- W3037083839 hasConcept C107832698 @default.
- W3037083839 hasConcept C109007969 @default.
- W3037083839 hasConcept C127313418 @default.
- W3037083839 hasConcept C142362112 @default.
- W3037083839 hasConcept C151730666 @default.
- W3037083839 hasConcept C166957645 @default.
- W3037083839 hasConcept C17409809 @default.
- W3037083839 hasConcept C205649164 @default.
- W3037083839 hasConcept C2778849375 @default.
- W3037083839 hasConcept C2779650180 @default.
- W3037083839 hasConcept C2780049196 @default.
- W3037083839 hasConcept C2781063710 @default.
- W3037083839 hasConcept C52119013 @default.
- W3037083839 hasConcept C59235061 @default.
- W3037083839 hasConceptScore W3037083839C107832698 @default.
- W3037083839 hasConceptScore W3037083839C109007969 @default.
- W3037083839 hasConceptScore W3037083839C127313418 @default.
- W3037083839 hasConceptScore W3037083839C142362112 @default.
- W3037083839 hasConceptScore W3037083839C151730666 @default.
- W3037083839 hasConceptScore W3037083839C166957645 @default.
- W3037083839 hasConceptScore W3037083839C17409809 @default.
- W3037083839 hasConceptScore W3037083839C205649164 @default.
- W3037083839 hasConceptScore W3037083839C2778849375 @default.
- W3037083839 hasConceptScore W3037083839C2779650180 @default.
- W3037083839 hasConceptScore W3037083839C2780049196 @default.
- W3037083839 hasConceptScore W3037083839C2781063710 @default.
- W3037083839 hasConceptScore W3037083839C52119013 @default.
- W3037083839 hasConceptScore W3037083839C59235061 @default.
- W3037083839 hasFunder F4320311690 @default.
- W3037083839 hasFunder F4320320275 @default.
- W3037083839 hasLocation W30370838391 @default.
- W3037083839 hasLocation W30370838392 @default.
- W3037083839 hasLocation W30370838393 @default.
- W3037083839 hasLocation W30370838394 @default.
- W3037083839 hasLocation W30370838395 @default.
- W3037083839 hasOpenAccess W3037083839 @default.
- W3037083839 hasPrimaryLocation W30370838391 @default.
- W3037083839 hasRelatedWork W1625501688 @default.
- W3037083839 hasRelatedWork W1964660227 @default.
- W3037083839 hasRelatedWork W2004879873 @default.
- W3037083839 hasRelatedWork W2022262407 @default.
- W3037083839 hasRelatedWork W2072607489 @default.
- W3037083839 hasRelatedWork W2077818555 @default.
- W3037083839 hasRelatedWork W2091666877 @default.
- W3037083839 hasRelatedWork W2112470756 @default.