Water Mills Deriving from the Burton and Broadmead Brooks, the By Brook descends some 200m in 25km from its highest point to its confluence with the River Avon. The By Brook has powered at least Read more…
Our landscape, our history Land use is often determined by the underlying physical environment, especially geology, topography and hydrology. Here we take a high level view of the most important physical characteristics of Wiltshire, from Read more…
Elsewhere on this website, we have seen archaeological evidence of human activity in the Nettleton area, such as Neolithic burial mounds, Roman shrines and Medieval causeways. These are features either visible on the ground or Read more…
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