Piospheres, that is, zones of attenuating stocking impact extending out from watering places, are a feature of arid pastoral regions. The present authors studied, for the first time, the initial developtnent of a piosphere in respect of a number of variables of the soil surface. The site was near-pristitie chenopod shrubland, part of a paddock of 1340 ha near Whyalla, South Australia, stocked with ca. 200 sheep on a new watering point. Soil features monitored over the first 2.5 years were dung deposition, sheep track developtnent and surface erosion, the soil lichen crust, cotnpaction of the soil surface and dustfall, usitig fenced plots of at least 550 m-as controls,Piosphere patterns (i.e. patterns reflecting the concetitricity of stocking pressure around water) were tnanifest within the first 3 months for sheep dung deposition, sheep track development, and lichen cover. Soil compaction, which was confined to sheep tracks and then largely to the surface 5 ctn, displayed a piosphere pattern when it was first recorded 6 months after stocking. Bulk density of this layer was elevated by up to 20%. There was only a weak piosphere pattern in dustfall. The piosphere patterns tn sheep track development and destruction of the lichen crust became more pronounced in time.