Fifteen samples of dune sand, and three samples from a core taken in t
he beach face, were collected from a sand spit which protrudes into Di
ngle Bay in Southwest Ireland. The potassium-rich feldspar grains from
the samples were dated using a single aliquot luminescence protocol f
or infrared stimulated luminescence (IRSL) signals. No ages over 600 y
ears were obtained, which demonstrates the youth of the dune forms cur
rently observed. The youngest ages were about 150 years old, but for t
hese samples the scatter in the equivalent dose obtained as the mean o
f 18 measurements was higher than for the older samples.