Airborne radar images of part of the Greenland ice sheet reveal icy te
rrain whose radar properties are unique among radar-studied terrestria
l surfaces but resemble those of Jupiter's icy Galilean satellites. Th
e 5.6- and 24-centimeter-wavelength echoes from the Greenland percolat
ion zone, like the 3.5- and 13-centimeter-wavelength echoes from the i
cy satellites, are extremely intense and have anomalous circular and l
inear polarization ratios. However, the detailed subsurface configurat
ions of the Galilean satellite regoliths, where heterogeneities are th
e product of prolonged meteoroid bombardment, are unlikely to resemble
that within the Greenland percolation zone, where heterogeneities are
the product of seasonal melting and refreezing.