Woking

Goldsworth playing fields, Parley Brook, Woking

Fieldwork carried out by W Mills with volunteer assistance under the overall direction of R Savage of SyAS to investigate any surviving contexts related to the discovery during fieldwalking in the 1920s and 30s of the Late Upper Palaeolithic flint blades now held in the British Museum as the Lawson Collection. Two transects of auger holes indicated the survival in parts of the site of late Ice Age soil horizons, but not close to the site of the flint discoveries.

Land at Egley Road, Woking

Evaluation by D Britchfield of WA identified evidence for prehistoric activity on or in the vicinity of the site in the form of residual burnt flint and a flint blade of Mesolithic or early Neolithic date. A small quantity of medieval pottery was recovered from a tree-throw hollow but a small pit contained no datable material. Features such as a grubbed-out hedgerow and an infilled ditch indicated that the landscape had been altered in the recent past.

Woking Palace, Old Woking

The seventh season of community excavations, and the third and final year of a Heritage Lottery funded project called ‘Woking Palace and its Park’, at the Scheduled moated site by The Friends of Woking Palace, SyAS and SCAU, under the direction of R Poulton of SCAU.

Sheerwater, Woking

Geoarchaeological survey by E Stafford of OA to inform the proposed Sheerwater Regeneration scheme. Twenty hand-augered samples across the northern part of the site provided baseline data on the nature of sedimentary sequences and recorded a shallow topsoil and a humic silty sandy subsoil over Bagshot Bed deposits. Charcoal fragments from the base of the sequence were radiocarbon dated to the Middle Bronze Age (1500–1320 cal BC) and may be indicative of human activity in the vicinity during this period.

Water main replacement, White Rose Lane, Old Woking

Watching brief by H Archer of CA during trenching and other groundworks revealed a series of alluvial deposits ranging from fairly uniform silty sand at the upper levels to lower deposits of fine clayey silt with some organic material continuing below the level of excavation. Residual finds recovered from the topsoil were, with the exception of six prehistoric flints, almost entirely post-medieval in date.

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