Detailed topographic maps of the lunar poles have been obtained by Earth-ba
sed radar-interferometry with the 3.5-centimeter wavelength Goldstone Solar
System Radar. The interferometer provided maps 300 kilometers by 1000 kilo
meters of both polar regions at 150-meter spatial resolution and 50-meter h
eight resolution. Using ray tracing, these digital elevation models were us
ed to locate regions that are in permanent shadow from solar illumination a
nd may harbor ice-deposits. Estimates of the total extent of shadowed areas
poleward of 87.5 degrees latitude are 1030 and 2550 square kilometers for
the north and south poles, respectively.