Young, D. and Batchelor, C. R. (2018). LAND ADJACENT TO PEARSON HOUSE, EDINBURGH GATE, HARLOW, ESSEX Environmental Archaeological Assessment Report. University of Reading: Quaternary Scientific (Quest). https://doi.org/10.5284/1076665. Cite this using datacite

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Title:
LAND ADJACENT TO PEARSON HOUSE, EDINBURGH GATE, HARLOW, ESSEX Environmental Archaeological Assessment Report
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Series:
Quaternary Scientific (Quest) unpublished report series
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quaterna1-317077_2.pdf (3 MB) : Download
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DOI
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DOI
https://doi.org/10.5284/1076665
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Publication Type:
Report (in Series)
Abstract
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Abstract:
A programme of environmental archaeological assessment was undertaken at the Pearson House site. The results of the deposit modelling indicate that the site lies towards the edge of the floodplain and the edge of a former channel, the main axis of which probably traverses the north-western area of the site. Overlying the bedrock is a sequence of probably Late Devensian Gravel, Holocene alluvium and modern Made Ground. The alluvial sequence consists of a tripartite sequence of sandy Lower Alluvium, Organic Clay, and the clay-rich Upper Alluvium. Significantly, the organic unit at the site is indicative of a transition towards semi-terrestrial (marshy) conditions. It is generally present at elevations between ca. 38.5 and 35.5m OD, in thicknesses of between 2.6 and 0.18m. Radiocarbon dating of the base of the Organic Clay in borehole WS16 has provided a Late Roman/Early Medieval age for the onset of organic accumulation. The results of the pollen assessment are consistent with this age for the sequence; an open environment dominated by herbaceous taxa is indicated, with limited trees and shrubs and indications of human activity in the form of disturbance and/or cultivation indicators, including cereals. The floodplain environment is likely to have been relatively damp, dominated by sedge fen or reed swamp type vegetation. The pollen assemblage is relatively consistent throughout the Organic Clay and is poorly preserved. In addition, no identifiable macrofossil remains were found within the organic unit in WS16. On this basis, no further palaeoenvironmental analysis of the sequence is recommended. As stated in Young (2018), from an archaeological perspective, the site's location towards the margins of the floodplain (and potentially a former channel) suggest that the archaeological potential is considered to be limited to where the Gravel surface lies above ca. 37m OD.
Author
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Author:
Daniel Young ORCID icon
C R Batchelor
Publisher
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Publisher:
Quaternary Scientific (Quest)
Other Person/Org
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Other Person/Org:
Historic England (OASIS Reviewer)
Essex County Council Historic Environment (OASIS Reviewer)
Year of Publication
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Year of Publication:
2018
Locations
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Locations:
Site: Land adjacent to Pearson House
County: Essex
District: Harlow
Parish: HARLOW
Country: England
Grid Reference: 544908, 211265 (Easting, Northing)
Subjects / Periods
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Subjects / Periods:
EARLY MEDIEVAL (Historic England Periods) PEAT (Monus)
ROMAN (Historic England Periods) PEAT (Monus)
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OASIS Id: quaterna1-317077
OBIB: Quaternary Scientific (QUEST) Unpublished Report July 2018; Project Number 044/18 ©
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Created Date
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Created Date:
30 Apr 2020