Barron, H. F., Browne, M. A. E. and Finlayson, A. 2005. West Lothian Geodiversity. British Geological Survey Commissioned Report, CR/06/008N. 190pp.
3.4.8 Alkali-dolerite sills
Alkali-dolerite sills comprise approximately 1,268 hectares, or 2.9% of the surface area of West Lothian. They outcrop principally in the east of the district and mainly intrude Strathclyde Group rocks
3.4.8.1 Soils, habitats and land use
The alkali-dolerite sills are variable in their topographic expression. Most are intruded into Strathclyde Group rocks and have little or no impact on landform and are till-covered, except the Auchnoon Sill which forms the till-free Auchinoon Hill. The sills intruding the Inverclyde Group between the Linhouse Water and Kirknewton also form positive landforms — Selms Top
122). These till-free soils have developed mainly brown forest, peaty gleys and peaty podzol soils with drainage varying from free to imperfect. As might be expected, the till covered sills develop mainly non-calcareous gleys and gleyed brown forest soils
3.4.8.2 Biodiversity
Conservation biodiversity interest is concentrated in: the mixed biological and geological SSSIs at Firth of Forth (also Ramsar site and SPA) and Skolie Burn
3.4.8.3 West Lothian Geodiversity Sites
Given the very limited coverage of alkali-dolerite sills, the three sites described below are considered to adequately represent these rocks.