We report on an initial attempt to apply luminescence dating to a sample fr
om a fossil alluvial channel bar deposit situated on a terrace similar to 5
0 m above the present course of the Orange River approximately 7 km west of
Aliwal North on Rotondo farm. Our findings show that such alluvium is with
in the range of luminescence dating, and that the alluvial terrace gravels
may be younger than was previously speculated.