numerous other tumuli and long barrows in the area surrounding Scratchbury Camp, including some located on the adjacent and co-joined Cotley Hill to the southeast, and on Middle Hill to the west. On the crown of Cotley Hill is a further Bronze Age tumulus surrounded by an Iron Age enclosure. Nearby to the northwest, on the side of Middle Hill, is the site of the deserted medieval village of Middleton, whose surviving earthworks consist of building platforms cut into lynchets and enclosed by a boundary bank and ditch, and a hollow-way. There are also signs of strip lynchets immediately to the north of Scratchbury Camp on the side of the hill. A Roman bronze spoon was found on or near Scratchbury Camp in 1804, and a Roman urn was found in the surrounding area before 1856 Geography Scratchbury is on the edge of the chalk plateau of Salisbury Plain, and within the area of Norton Bavant Chalk Downland Edge, as described by the West Wiltshire Landscape Character Assessment. The hill has extensive views overlooking the Wylye valley to the south. The Salisbury Plain chalk massif is part of a system of chalk downlands throughout eastern and southern England formed by the rocks of the Chalk Group; the landscape is underlain by a combination of Lower, Middle and Upper Chalk supporting shallow well drained calcareous silty soils over chalk on slopes and crests. Escarpments are often formed where layers of chalk have been compressed to form a fold, or where the chalk has been faulted, resulting in accelerated erosion along the line of the weakness. For the Norton Bavant Chalk Downland Edge, the 'character' of this area encompasses three distinctive, steeply sloping hills (Middle Hill, Scratchbury Hill, and Cotley Hill), which form a distinct and somewhat isolated unit of Chalk Downland Edge. The hills are covered with long fields, which are predominantly arable, with occasional patches of rough remnant chalk grassland and scrub on the tops of the hills. Many chalk grassland slopes in England show the mark of centuries of grazing by sheep, the slopes bearing a stepped or striped appearance formed by a mixture of soil creep and sheep paths, and such erosion is visible on the slopes of Scratchbury Hill. Regular patches and belts of mixed woodland populate parts of the lower slopes. Imber military range perimeter paths run across the top of the hills, providing public access