The Pathfinder Landing site on Mars has boulders that may be cratered (Stim
py), split (Chimp), fragmented (Book End and Flat Top), or otherwise partly
destroyed (Yogi and Frog) by collisional processes. Atmospheric-entry calc
ulations show that centimeter-sized projectiles survive passage through the
martian atmosphere and encounter the surface of Mars at velocities of a fe
w kilometers per second. Craters Less than 1 meter in diameter may contribu
te to the evolution of the martian surface and its soils.