Site Data from a Ridge and Furrow Survey at DIRFT III, Northamptonshire 2016

Cotswold Archaeology, 2022. https://doi.org/10.5284/1095483. How to cite using this DOI

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Cotswold Archaeology (2022) Site Data from a Ridge and Furrow Survey at DIRFT III, Northamptonshire 2016 [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1095483

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Digital Object Identifiers

Digital Object Identifiers (DOIs) are persistent identifiers which can be used to consistently and accurately reference digital objects and/or content. The DOIs provide a way for the ADS resources to be cited in a similar fashion to traditional scholarly materials. More information on DOIs at the ADS can be found on our help page.

Citing this DOI

The updated Crossref DOI Display guidelines recommend that DOIs should be displayed in the following format:

https://doi.org/10.5284/1095483
Sample Citation for this DOI

Cotswold Archaeology (2022) Site Data from a Ridge and Furrow Survey at DIRFT III, Northamptonshire 2016 [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1095483

Introduction

Working shot
Working shot

Thiis collection comprises site data (images and CAD) from a geoarchaeological investigation of the medieval/early post-medieval ridge and furrow earthworks and later field boundaries at the site of Daventry International Rail Freight Terminal (DIRFT III), Northamptonshire. The work was carried out During March and April 2016, by Cotswold Archaeology. Five hand-dug test pits and twenty-one machine-excavated trenches were excavated across the northern half of the site. The trenches were targeted on remnant ridge and furrow and other earthwork features shown on a LiDAR survey of the site, with the aim of investigating the development of the medieval agricultural landscape. On the floodplain, a buried soil horizon was encountered beneath the mineralised medieval ploughsoil. This deposit had some of the characteristics of a Boreal soil (i.e. Mesolithic/Neolithic), but pollen analysis suggests that it was probably a cultivated soil. The soil horizon overlay a variety of vegetation features (tree throw hollows etc.), suggesting that the floodplain supported some degree of tree cover prior to clearance for agricultural use. There was no suitable organic material for radiocarbon dating, so the age of the buried soil is uncertain. However, small ditches were also identified beneath the buried soil, probably forming part of an agricultural ditch system of Late Iron Age or Roman date. It is therefore probable that the buried soil horizon dates to the first millennium AD. Investigation of the medieval ridge and furrow earthworks identified some changes to its organisation during its period of active use, but dating these changes was constrained by the lack of dateable artefactual material and the homogeneity of the subsoil that formed the earthwork features.


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