“…During the advance, the PGS picked up marine sediments and incor- porated them into the diamicton of the moraines (Högbom 1911). A surge genesis of these sediments was later supported by De Geer (1919), Cöster (1925), Punning et al (1976), Haga (1978) and Rowan et al (1982). However, there were different views with respect to the number of surges, as well as their ages.…”