Water on the Moon?

More than 50 separate images have been summed together over one lunar day in these composite Clementine orbital images of the poles of the Moon. Areas of near permanent illumination are white and areas of near permanent darkness are black. The south pole (B) is about 10 times darker, and colder, than the north pole (A). The scale bar is 100 km.
 
Orbital geometry of
the Clementine
radar experiment.
Area sampled.
Science magazine published an article where the authors report the possible presence of water ice in the permanently shadowed region at the south pole of the Moon. 

Is only a possibility, already suggested in 1961. Volatiles degassed from the primitive Moon or deposited on the lunar surface by cometary and asteroidal impacts might migrate and collect in permanently shadowed cold traps near the lunar poles, where they could be stable over geologic time. 

The Mariner 10 spacecraft make a flyby over the Mercury south pole in 1974-1975. Years later, water ice was detected there with the Arecibo radiotelescope. The same technique used with Mercury data at Arecibo (1993) has been used now to estimate the extent of the area of putative south pole ice deposits: 90 to 135 square km.