Irregular, dark green to black, glassy-looking boulders are locally co
mmon in the northwest portion of the rim of the Roter Kamm impact crat
er in southern Namibia. Their smooth surfaces, flow-like textures, pre
sence of folds, and their similarity to melt bombs have led to the int
erpretation that these are molten impact ejecta. However, the samples
we have examined are all fine-grained breccias composed of angular fra
gments that show no evidence of melting. Meltlike surface textures of
these rim breccias are largely a consequence of surface wind polishing
of fine-grained rocks in a desert environment. These monomict breccia
s were produced by impact-related brecciation of Gariep sediments (car
bonaceous, siliceous shales) previously modified by low-grade Damaran
metamorphism. Secondary quartz within the breccias is attributed to fl
uid activity that postdates the impact.