Watching brief by S Porter and J McNicoll-Norbury of TVAS during the excavation of an irrigation lake to the south-west of the multivallate, Iron Age hillfort indicated that the site had been the subject of previous landscaping work, probably during the construction of the golf course removing any archaeological features that may have been present.
A watching brief by S Porter of TVAS following earlier evaluation revealed a range of archaeological deposits from the medieval through to late post-medieval periods. The earliest evidence was a medieval pit with sparse medieval pottery. More complex deposits of post-medieval date including walls, floors, a probable well and a cesspit were also revealed.
Evaluation by A Mundin of TVAS revealed that the natural gravel geology was overlain by alluvial clay deposits, which in turn were sealed by dumped rubble deposits in the late 19th century. A number of modern walls were present, but no evidence of earlier archaeological remains was recorded.
A watching brief by G Elliot of TVAS recorded a brick well of probable 19th century date and a brick wall running along the boundary of the site with Bishop’s Mead.
Watching brief and historic building recording by A Taylor and G Elliot of TVAS. Coombe Edge was noted as a good example of a small country house with a lodge and for its association with the family of Sir Ranulf Fiennes. Groundworks associated with a new house, pool and pond were monitored for remains connected with the route of the Roman road thought to run adjacent to the site, but no finds or features of archaeological interest were revealed.
Evaluation by J Pine of TVAS revealed two ditches, one undated and the other tentatively dated to the Roman period. A number of trenches were targeted over cropmarks, but no features that correlated with the cropmarks were revealed.