Hypervelocity impact can produce unique effects in materials, includin
g crystal structures, microstructures, and properties. Examples includ
e impact-driven shock waves to synthesize novel materials 1 mm and 1 m
um thin shocked to pressures up to 100 GPa (1 Mbar), preferential crys
tallographic alignment achieved by taking into account the shape and s
ize of powder particles, and high-pressure phase transitions quenched
in geological materials. Thin specimens are used to achieve the highes
t quench rates. Methods are described which show that the experiments
can be performed by precooling or preheating specimens in the range -1
70-degrees to +1000-degrees-C. Calculational results for the quartz ex
periments show the importance of computational simulations to determin
e the pressure history m the specimen.