Radiocarbon activities and uranium isotopic disequilibria were measure
d in water samples from both the sandy Pleistocene coastal aquifer and
within the upper Cretaceous Judea Group carbonate aquifer of northwes
tern Israel. The samples in both aquifers exhibit a decrease in C-14 a
ctivity that is concomitant to the growth in U-234-excess. This sugges
ts that under specific conditions, U-234-excess dating of groundwater
can be used to corroborate C-14 dates, while offering the possibility
of extending the range of dating of groundwater beyond that of C-14.