On a Deposit of Interglacial Lœss, and some Transported Preglacial Freshwater Clays on the Durham Coast

Abstract

I. Introduction. The object of this paper is to describe some phenomena connected with the earlier Glacial deposits that are exposed on the Durham coast. The beds to which attention is more particularly directed form part of, or are connected with, a recently-discovered deposit of Scandinavian Drift. They comprise the following:—