Guildford Castle, Guildford

Evaluation and excavation by R Poulton of SCAU prior to the installation of a new floor and external staircase to the castle keep. Material examined from within the keep suggested that a fairly substantial 19th century deposit extended to at least 0.5m below the current ground surface. This material was not excavated to its full depth. A trench in the area of the proposed staircase produced similar results to the investigations in 2001, where it was found that possible medieval deposits relating to the construction of the castle exist very close to the current ground surface.

Rear of 10–10a Downside, and front of Copperstones, Downside, Epsom

Excavation by A Hall of SyAS of two trenches and a test pit along the alignment of Stane Street suggested by S E Winbolt produced no evidence of the road. A further test pit along an alternative alignment suggested by I D Margary revealed no archaeological finds or features of interest and that the ground had been heavily disturbed. (375) Excavation by A Hall and F Pemberton of SyAS of three trenches and a test pit on I D Margary’s postulated line of Stane Street revealed a layer of closely packed flints considered to be the remains of the road. (380) Not clear where this latter excavation was

The Durdans, Woodcote End, Epsom

Historic building survey of the Riding School Building, which is part of The Durdans building complex and a Grade II Listed Building, by R Martin of SIHG. Designed by George Devey for the 5th Earl of Rosebery as a place to train horses under cover, the building is a large open barn structure nine-bays long with a projecting porch at the south side and a cant bay at the east end, and is dated to 1881 by a stone in the gable end of the porch. (SIHG 139)

Hampton Court Station, Hampton Court

Geoarchaeological evaluation by ArchaeoScape consisting of recording lithostratigraphy from three geotechnical boreholes and twelve geotechnical probe holes to provide a profile of sediment sequence, and assess the potential of the site for environmental evidence. The lower part of the sequence comprises sand and gravel of the Shepperton Gravel, a deposit widely recognised in the Middle Thames Valley and laid down at the end of the last glacial episode between c 20,000 and 10,000 years ago.

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