Essex erratic boulders: a gazetteer Fig. 1. A distribution of erratic boulders referred to in the gazetteer The gazetteer is obviously biased towards boulders visible from the road. Almost all of these have been moved by humans to their present positions, many of them moved in antiquity without mechanical assistance. The boulders in farmyards and by farm gates were discovered in fields during ploughing but it is reasonable to assume that most boulders discovered in this way would simply be moved to the edge of the field and left there. Hundreds of examples, therefore, remain to be rediscovered on farm land in ditches and hedgerows. History of Research One of the first to record information about Essex erratic boulders was John Brown of Stanway in the 1830s (Brown 1837) but it was the Essex Field Club in the late 19th and early 20th centuries that regularly recorded the existence of erratic boulders in the pages of the Essex Naturalist. The first paper was by the Rev. A.W. Rowe in 1887 entitled Some Essex boulders. In the same year, Rowe produced a remarkably detailed analysis of Essex erratics in the Quarterly Journal of the Geological Society entitled On the rocks of the Essex drift. This was followed in 1893 by a paper in the Transactions of the Essex Archaeological Society by the Rev. H.T. Armfield, Rector of Colne Engaine, entitled On some ancient boulders scattered in the district of the Colnes. However, it was head teacher and amateur geologist Dr. A.E. Salter, who, in 1914, produced the most comprehensive list in a paper in the Essex Naturalist entitled Sarsen, basalt and other boulders in Essex. This paper has been an invaluable source of reference for all those interested in Essex boulders since then. In the 1950s E.A. Rudge revived interest in puddingstone with his numerous articles and papers on the alignment of boulders which he claimed represented the route of a prehistoric trackway. Rudge made no distinction between puddingstone and ferricrete and lumped them together under the geological name of 'conglomerate'. Much has been written about boulders in churchyards. These were present before the church was constructed and it is possible that in some cases they were part of a prehistoric burial chamber or monument. It is common to find church walls built upon erratic boulders which has led to the Essex Naturalist (New Series) 20 (2003) 117