Green, C. and Young, D. (2014). RIVERSIDE STUDIOS AND QUEENS WHARF, HAMMERSMITH, LONDON BOROUGH OF HAMMERSMITH AND FULHAM: (NGR: TQ 2312 7811): A REPORT ON THE GEOARCHAEOLOGICAL FIELDWORK AND DEPOSIT MODELLING . University of Reading: Quaternary Scientific (Quest). https://doi.org/10.5284/1030911. Cite this using datacite

Title The title of the publication or report Title:	RIVERSIDE STUDIOS AND QUEENS WHARF, HAMMERSMITH, LONDON BOROUGH OF HAMMERSMITH AND FULHAM: (NGR: TQ 2312 7811): A REPORT ON THE GEOARCHAEOLOGICAL FIELDWORK AND DEPOSIT MODELLING
Series The series the publication or report is included in Series:	Quaternary Scientific (Quest) unpublished report series
Downloads Any files associated with the publication or report that can be downloaded from the ADS Downloads:	quaterna1-205939_1.pdf (2 MB) : Download
Licence Type ADS, CC-BY 4.0 or CC-BY 4.0 NC. Licence Type:	ADS Terms of Use and Access
DOI The DOI (digital object identifier) for the publication or report. DOI	https://doi.org/10.5284/1030911
Publication Type The type of publication - report, monograph, journal article or chapter from a book Publication Type:	Report (in Series)
Abstract The abstract describing the content of the publication or report Abstract:	Geoarchaeological monitoring and a programme of deposit modelling was carried out in order to clarify the nature of the sub-surface stratigraphy and to evaluate the potential of the sedimentary sequences for reconstructing the environmental history of the site and its environs. The site lies on the Kempton Park Terrace (Gibbard, 1994), where no alluvial floodplain is recorded. The results of the geoarchaeological deposit modelling are consistent with the existing BGS mapping, and confirm that the site is underlain by London Clay, the surface of which appears to fall eastwards and lies at between -0.45 and -0.41m OD, in turn overlain by the Kempton Park Gravel, deposit during the Middle to Late Devensian (30 to 80ka BP). The surface of this unit rises eastwards, recorded at between 0.50 and 3.95m OD, so that the gravel is thickest in the eastern part of the site (between 4.3 and 4.4m). The Gravel is notably thinner in the eastern part of the site, recorded at between 0.4 and 0.9m thick. No evidence was found for a unit of Langley Silt at the site (mapped elsewhere overlying the Kempton Park Gravel). Variable thicknesses of Made Ground cap the sequence, so that the modern surface of the site lies at between ca. 4.7 and 5.7m OD. No further investigations were recommended.
Author The authors of this publication or report Author:	Cheryl Green Daniel Young
Publisher The publisher of the publication or report Publisher:	Quaternary Scientific (Quest)
Other Person/Org Other people or organisations for this publication or report Other Person/Org:	Historic England (OASIS Reviewer) Greater London HER (OASIS Reviewer)
Year of Publication The year the book, article or report was published Year of Publication:	2014
Locations Any locations covered by the publication or report. This is not the place the book or report was published. Locations:	Site: RIVERSIDE STUDIOS AND QUEENS WHARF County: Greater London District: Hammersmith and Fulham Parish: HAMMERSMITH Country: England Grid Reference: 523120, 178110 (Easting, Northing)
Subjects / Periods Subjects / Periods associated with this record. Subjects / Periods:	PALAEOLITHIC (Historic England Periods) GRAVEL (Monus) EVALUATION (Event)
Identifiers Identifiers associated with the publication. These might include DOIs, site codes, Monument Identifiers etc. Identifiers:	OASIS Id: quaterna1-205939 OBIB: Project Number 217/13
Source Where the record has come from or which dataset it was orginally included in. Source:	OASIS (OASIS)
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Created Date The date the record of the pubication was first entered Created Date:	01 Feb 2018

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