Measurement of Be-10 and Al-26 concentrations produced by cosmic ray bombar
dment within the quartz mineral fraction of surficial deposits and exposed
bedrocks (in situ-production) is rapidly becoming an important quantitative
tool in geomorphology. Whereas conventional methods provide age control on
stratigraphic profiles, surface exposure dating using in situ-produced Be-
10 and Al-26 is particularly well-suited not only for continuous dating but
also for quantifying spatial variations and rates of geomorphic processes.