During the investigation of the erosional effects of the rainstorm on 30-31
August 1997 on Mount Fulufjallet, two samples have been radiocarbon age de
termined. The results give a maximum age of events occurring earlier. One s
ample of an exposed Picea trunk in the sandur of the stream St Goljan was r
adiocarbon dated to 1320+/-120 C-14 years BP. The lowermost part of a peat
sequence in a soligenous mire in the valley of the stream Tangan was radioc
arbon dated to 1455+/-70 C-14 years.