Swift Wind Farm, Churchover, Warwickshire. Archaeological Evaluation (OASIS ID: cotswold2-260961)

Cotswold Archaeology, 2016. https://doi.org/10.5284/1039952. How to cite using this DOI

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Cotswold Archaeology (2016) Swift Wind Farm, Churchover, Warwickshire. Archaeological Evaluation (OASIS ID: cotswold2-260961) [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1039952

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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/10.5284/1039952
Sample Citation for this DOI

Cotswold Archaeology (2016) Swift Wind Farm, Churchover, Warwickshire. Archaeological Evaluation (OASIS ID: cotswold2-260961) [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1039952

Introduction

Swift Wind Farm, Churchover, Warwickshire. Archaeological Evaluation (OASIS ID: cotswold2-260961)

An archaeological evaluation was undertaken by Cotswold Archaeology in March 2014 at Swift Wind Farm, Churchover. Six trenches were excavated. The evaluation revealed a small number of features of possible archaeological origin on either side of the River Swift (within Areas B and C). However, the predominant archaeological features identified comprised evidence for ridge and furrow cultivation, with furrows being recorded in all trenches except Trench 1.

A probable ditch or pit, 202 identified in Trench 2 (Area C) remains artefactually undated. However, this feature does correlate with geophysical anomaly 2 which may represent a curvilinear enclosure.

To the east of the River Swift, two ditches identified at the northern limit of Trench 6 (Area B) are suggestive of ditches flanking a trackway. It remains undetermined they are associated with nearby geophysical anomalies that are interpreted as later prehistoric/Roman enclosures and field systems immediately to the west, or whether they form a trackway that is broadly contemporary with the ridge and furrow.


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