The loose material-regolith-on the surfaces of asteroids is thought to repr
esent ballistically emplaced ejecta from impacts(1,2) but the identificatio
n of source craters and the detailed study of the regolith modification hav
e been hampered by the limited spatial resolution and area coverage of the
few asteroids imaged by spacecraft. Here we report the results of global ma
pping of the asteroid 433 Eros from high-resolution images obtained by the
NEAR-Shoemaker spacecraft. Based on the images and ejecta-emplacement model
s, we suggest that most large ejecta blocks on Eros originate from a relati
vely young 7.6-km-diameter crater. A large fraction of the ejecta from impa
cts pre-dating that crater has apparently been buried or eroded. The images
also show evidence for the action of a variety of sorting environments for
regolith particles after they are deposited on the surface.