Plate impact experiments have been performed on two igneous rocks of differ
ent grain size. Shock stresses have been measured using embedded manganin s
tress gauges, up to similar to 12 GPa. In the coarser grained material data
was obtained by impacting rock flyer plates onto previously characterized
targets. Results are compared and contrasted to the existing data for other
geological materials. In the finer-grained material lateral stress was als
o measured. In combination with the longitudinal stresses, these results ha
ve been used to obtain the materials shear strength under shock loading con
ditions. Results suggest that the material is deforming in an inelastic man
ner. (C) 2000 American Institute of Physics. [S0021-8979(00)06408-2].