Palaeolithic artifacts were recorded from a terrace on the Great Ouse, near St. Neots, Huntingdonshire, in 1927, the chief source being a group of pits dug in what was formerly part of Paxton Park, on the left bank of the river in the parish of Little Paxton. Mr Tebbutt has since recovered many more artifacts from this site. Taken together, the material constitutes a working industry, which will be described in this paper.

A twelve-foot section, fig. 1, shows a basal layer (1) of boulders and large pebbles resting upon undisturbed Oxford Clay. One boulder of limestone measured two feet in length, and many other erratics showed the derivation of this layer from drift deposits of a preceding glacial stage. Bones and teeth of Elephas primigenius, Rhinoceros antiquitatis, Rangifer tarandus, and Equus caballus were found here. This basal bed is not a solifluxion level in place, though it may represent a solifluxion layer which has been re-washed and sorted. Certainly the Oxford Clay has not been caught up into it, and the elements are uniformly water-laid, passing up, without break, into nine feet of compact, well-bedded, fluviatile gravels.