Monument record MHG29867 - Mesolithic flint-working site at Oliclett, near Wick

Scatter of flints flakes found during forestry preparation works near Oliclett, Caithness. All the flakes were within a fairly well defined area no more than 6m x 6m. Paul Humphreys attended and took digital photos as well as locating the grid reference using a GPS.The flakes were located on the interface between the peat layer and the underlying clay.
The site will not be planted but instead incorporated within the adjoining clearing.
The flakes are currently in the landowner's possession. <1>

Preliminary excavation was carried out of a lithic scatter revealed by forestry ploughing in an area of blanket peat below the Hill of Oliclett. The ploughing had uncovered buried soils in areas where the peat appears to have been extensively cut in the past. Over 1200 lithics (flint and quartzite) were recovered from these soils, mostly undiagnostic debitage. However, the assemblage does contain 61 narrow blade microliths and a number of microburins and bladelets, indicating a Mesolithic date for the site. A single barbed-and-tanged arrowhead was also recovered from the base of the peat.
The site is located on a gentle E-facing slope at 100m OD, in the vicinity of a number of small burns and around 6km from the modern coastline. There appear to be two main concentrations of lithics, located approximately 100m apart on small knolls. Only one of these was thoroughly investigated, revealing that here the scatter was composed of several epicentres surrounded by areas of reduced lithic density. Environmental sampling was undertaken in the vicinity of the site. <2><3>

Radiocarbon analysis of peat samples from this area has revealed that the blanket peat began to form at c.6575 BC, which strongly suggests that the peats are concurrent with the later Mesolithic use of the hillside. This indicates strong potential for the survival of well-preserved, stratified occupation evidence within or beneath the peat. <4>

Further excavations took place at this site in 2002, expanding the original survey area. Further Mesolithic material was recovered, as well as a considerable amount of burnt flint. Some possible stake holes were discovered in association with an ard mark, but no datable material was recovered from the features. <5>