To evaluate the reliability of K-Ar ages on fresh basaltic rocks, various fractions and whole rocks were dated. The samples were chosen to obtain a variety of petrographic types representing several petrologic kindred and cooling environments. The dates provided no evidence of argon leakage. One sample of an unusual rock type (a troctolite) gave an anomalously high age, suggesting excess radiogenic argon. Nepheline separates from two rocks yielded ages equivalent to the ages of biotite and pyroxene. Introduction. Basaltic rocks have been dated by means of the potassium-argon method by numerous workers. Erickson and Kulp [1961] obtained encouraging but erratic results from measurements on the Palisades diabase and Watchung basalt. Since this initial work, numerous ages have been determined on basaltic rocks [e.Most of the previous work has been done on basalt flows. or diabases. Our investigation includes very diverse petrographic rock types of basaltic composition representing a number of cooling environments. We have made at least two argon analyses on each of eighteen rocks and mineral fractions of essentially known age in order to evaluate the method. Our results indicate that whole-rock determinations onpetrographically suitable mafic rocks are as reliable as any mineral fraction that can be dated. Analytical techniques. The radiogenic argon is measured by the isotope dilution method using Ar • spikes. These spikes are prepared in large batches on a manifold, so that they all have the same pressure. This pressure is determined by calibration against a spike of highly purified commercial air argon. Samples are fused by induction heating in tungsten or columbium crucibles. Purification involves the following steps: 1. Dry ice trap. 2. Copper oxide at 600øC. 3. Liquid nitrogen trap. 4. Calcium at 900øC. 5. Adsorption on charcoal at liquid nitrogen temperature in a break seal for transfer to the mass spectrometer. The typical blank is •10 -• tool of atmospheric argon; the best are about 3 X 10 -•2 mol. The mass spectrometer is a Reynolds [1956] type with Faraday cup collector. Flow runs are used for the larger samples and static runs for the smaller ones. Corrections for fractionation are made in both cases. POTASSIUM-ARGON DATING OF BASALTIC ROCKS 1083 flame measurements. Details of both flame tech-