Saturn's large moon Titan is unique among planetary satellites in that it p
ossesses a thick atmosphere and a haze layer that is opaque to visible ligh
t. This haze is believed to be composed of organic compounds produced by th
e photolysis of methane. It has been suggested that the photochemical produ
cts of methane photolysis, primarily ethane, would "rain out" over time and
may produce reservoirs of liquid hydrocarbons on Titan's surface. Such mat
erial would appear very dark, with an albedo less than or equal to 0.02 (Kh
are et al. 1990, Bull. Am. Astron, Sec. 22, 1033). Such low-albedo regions
have not been previously detected on Titan's surface. Here we report observ
ations of Titan at a resolution of 0.04 arcsec (0.02 arcsec/pixel) using th
e technique of speckle imaging from the 10-m Keck I Telescope. By observing
Titan at specific infrared wavelengths which are windows through its atmos
phere, we have made both an albedo map of Titan's surface at 1.6 and 2.1 mu
m and an estimate of Titan's haze optical depth at these wavelengths. We c
learly distinguish low-albedo features (reflectance <0.05) on Titan's surfa
ce. (C) 1999 Academic Press.