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Preliminary results on a case study : Ridgeway Mass Grave, Dorset

The InterArchive Project is a multi-disciplinary investigation into the hidden archive of archaeological human interment. The aim of the project is to assess the nature of the archaeological and historical burial record preserved at the micro-scale within grave soils, particularly where physical remains can no longer be recognised visually. The methodology will also assess the effects of taphonomic processes in burials from different environments. This will be achieved by developing a sampling and analytical protocol to maximise the retrieval of this cultural archive, integrating the complimentary techniques of soil micromorphology, inorganic geochemistry and trace organic analyses. The purpose is to unlock both the physical and chemical archive of archaeological and forensic information, which can then be used to aid in cultural reconstruction. The study will investigate a wide range of soil types and inhumations from prehistory through to the early ninetieth century and thus will improve our understanding of the role of the burial environment in the preservation and movement of grave residues such as hair, funerary goods and textiles. This poster focuses on Ridgeway Hill, in Weymouth, Dorset, which is the site of a mass grave currently being assessed through the interdisciplinary InterArchive methods. This site was excavated in 2009, by Oxford Archaeology, and contains around 51 decapitated skeletons, dating from AD 890-AD 1030. A lack of clothing associated finds suggests that the bodies were naked when buried. The InterArchive project, therefore intends to examine the Ridgeway Hill grave soils for unseen archaeological evidence.

InterArchive Project Preliminary results on a case study : Ridgeway Mass Grave, Dorset C. A. Lang1, B. J. Keely2, H. R. Stokes1, M. R. Usai1, C.A. Wilson3 & D. R. Brothwell1 1 Depart e t of Archaeology, U i ersity of York, Ki g’s Ma or, York YO 7EP 2 Department of Chemistry, University of York, Heslington Campus, York, YO10 5DD 3 School of Biological and Environmental Science, University of Stirling, Stirling FK9 4LA [email protected] 3. Preliminary results: 1.1 Aims of the project: Initial results have been obtained through micromorphological analysis of the thin sections, in cross-polarised (XPL)and plain polarized light (PPL). From this initial analysis environmental conditions affecting the burial pit can be obtained. Figure 3.1 shows eluviation of clay minerals from the upper horizons of the soil profile. Through the established analytical methods of soil micromorphology the InterArchive project aims to recover cultural and environmental information from archaeological graves. This will involve determining the role of the soil in in burials and how it effects decomposition. 3.1 Pedological Features cc cc A A gm gm 1 2 cc cc gm Figure 1.1: The site is situated north of Weymouth next to the A354 relief road, the construction of which is the reason for finding the remains 3 Ridgeway Hill, in Weymouth , Dorset, is the site of a 8901030 AD mass burial pit The site is currently being assessed by the InterArchive team. Ridgeway was excavated in 2009, by Oxford Archaeology, the site was found to contain 51 skulls and what is believed to be the associated skeleton 1 Figure 1.2: The burial pit illustrating the complexity of the site 2. Methodology 2 (3)Hand/Arm (4) Feet Three skeletons were sampled at Ridgeway, due to the complexity of the site, a full set of samples from each skeleton could not be obtained 3 2.2 Micromorphology: •Soil samples were orientated to attain the maximum detection of features. • U disturbed soil sa ples where i preg ated (crystic resi ), 3 μ thi sectio s ere produced •Thin section description: Zeiss AxioVision Rel 4.8 using terminology of Bullock (1985) and Stoops (2003) 4 There are no observed extinction lines within the clay coating sand so this might indicates a possibility that the hydromorphic condition had not altered. From this we can hypothesis that the site may not have seen disturbance at lower levels. 3.2 Coarse material: The majority of biologically derived coarse material found at the Ridgeway site, is bone(Figure 3.2). The degree of weathering is lower on the bones of the pelvic area than those around the skull. It is not possible, on either thin sections, to identify specific features of the bone such as the haversian canals. There is evidence for stronger diagenesis of the skull bone with movement of the depletion calcite into the soil matrix. 1 3 2 4 Figure 3.2: Fine bone fragments (coarse biologically derived material) 1(XPL) & 2(PPL): from the pelvis area. 3(XPL)& 4(PPL) : from the skull area 4. Discussion: 2.1 Sampling areas: (1) Beside the skull (2) Pelvic Area cc gm Figure 3.1: The development of textural dusty clay coatings (CC) on void walls with greater contrast to the groundmass (gm) 1(XPL) & 2 (PPL) :heel, 3 (XPL) & 4 (PPL): pelvic area. 1.2 The site: Systematic sampling strategies were adopted to maximise information retrieval : 4 sampling areas are normally obtained cc The unsorted textural clay and silt material coating the channel, vughs and packing voids is the result of high energy water movement through the soil (Figure 3.1) The XPL images give a clearer indication of the level of deposition, as the coatings contrast in XPL to a greater extent than PPL. Fine polymorphic amorphous organic matter possibly formed through the movement colloidal scan be seen in (1) & (2) 4 Although the project is still in the early stages, it is clear that there is the potential to reveal significant aspects of human burials contained in grave soil. Through initial reconnaissance of the thin sections encouraging information has been gleaned. The natural processes that have taken place in the surrounding environment have been seen through the development of coatings in the soil, indicating the movement of mineral and organic particles . Further analysis must look at the movement of material from the bodies for evidence of; pre and post-burial treatments, dietary evidence, and organic matter. This will help to establish patterns of dispersal through voids and fluids as a result of the decomposition processes. SEM (scanning electron microscopy) analysis will also be employed on the thin sections to analyse elemental composition of pedological features, and image analysis software will help in establishing spatial patterns. Acknowledgements: The research has received funding from the European Research Council under the European Community's Seventh Framework Programme (FP7/2007-2013) / ERC grant agreement n° 230193 References: Bullock, P., Fedoroff, N., Jongerius, A., Stoops, G., Turina, T. and Babel, U. 1985. Handbook for Soil Thin Section Description. Waine Research Publication, England Stoops, G. 2003. Guidelines for Analysis and Description of Soil and Regolith Thin Section. Soil Society of America, Inc. USA