Global fall-out from atmospheric testing of thermonuclear weapons prod
uced horizon markers corresponding to the initiation of testing in 195
3 and the maximum fall-out in 1963. The radioactive isotope Cs-137 ass
ociated with these events has a half-life of 30.2 years. Therefore, wi
th the appropriate radiation detectors, this fall-out can be used as a
long-term temporal indicator in glaciers and snowpack. A prototype ga
mma-ray detector system was successfully tested and was used to make i
n-situ measurements of the Cs-137 marker in a borehole at Summit, Gree
nland. The system consisted of a 7.6 cm by 7.6 cm NaI (Tl) scintillati
on crystal/photomultiplier detector, commercial pre-amplifier, amplifi
er and power supplies, and a microcomputer-based pulse-height analyzer
. The measurements were made in boreholes of 25.4 cm and 12.7 cm diame
ter to depths of 22 m. Based on the results reported here, the gamma-r
ay detection technique promises to be a powerful way to locate quickly
horizon markers in the field.