A basaltic tephra layer consisting of brownish-olive glass shards, and
about 0.2 mm thick. was found in cores from four lakes in northwest G
ermany. According to pollen analysis it was deposited during the early
Boreal period (corresponding to about 8700 BP). The petrographic prop
erties, the geochemical composition and the age agree with those of th
e Saksunarvatn tephra, which was first found on the Faroe Islands. The
position of the tephra layer in the pollen stratigraphy and in the ab
solute time-scale is discussed. Procedures for locating the tephra in
other cores are suggested.