Sourlie, near Irvine (Fig. 1), is certainly one of the few and probably the only site in the whole of Scotland where, to date, irrefutable stratigraphical evidence demonstrates that during the Quaternary period the country was subjected to glaciation in both Late Devensian and pre-Late Devensian times (cf. [Mitchell et al. 1973][1]; [Lowe 1984][2]; [Bowen et al. 1986][3], pp. 320–3; [Bowen and Sykes 1988][4]). The relevant field evidence, preliminary results of laboratory analysis and some conclusions concerning the significance of the site at Sourlie are presented below. Temporary, open-cast coal excavations at Sourlie in 1986 exposed thin (to 0.6 m) lenses of organic-rich sediments (unit D1, Table 1 and Fig. 2) contained within local pockets on the upper surface of a layer of glacio-fluvial deposits (C). The latter sediments overlie an ablation deposit (B), which rests on a basal grey lodgement till (A) that contains clasts of (mainly) local sedimentary rocks. Units D1 and D2 are overlain by two distinctly different deposits. The lower of these, a thinly developed pink-brown diamicton (E), contains a mixture of clasts of local and far-travelled sedimentary, igneous and metamorphic rocks, together with occasional fragments and rare complete valves of marine molluscs. The overlying, thicker, upper grey lodgement till (F) is devoid of shell fragments. In grain-size characteristics, clay mineralogy and geochemistry its matrix closely resembles that of unit A, but, in addition to containing clasts of local sedimentary rocks, unit F contains basic igneous rock fragments that have been transported at least a . . . [1]: #ref-16 [2]: #ref-12 [3]: #ref-1 [4]: #ref-2