It covers the moon's
leading hemisphere — the side that faces forward as it moves in its orbit — which suggests that the black material has been swept up from space as the moon moves around Saturn.
Cassini also resolved a longstanding mystery about why one half of the moon's surface is 10 times as bright as the other:
The leading hemisphere of the moon picks up dark debris that is warmed by the sun, while brighter ices condense on the colder, trailing hemisphere.
The left - hand panel shows the moon's
leading hemisphere and the right - hand panel shows the moon's trailing side.
The pervasive magnesium - bearing mineral might also be what makes up the nonwater ice detected on
the leading hemisphere's surface.
The leading hemisphere has a yellowish appearance, while the trailing hemisphere seems to be splattered and streaked with a red material.
Some of the brighter, round markings might be recent impact craters, including a bright feature with rays apparently extending from it near longitude 130 degrees on
the leading hemisphere of Titan.
This view looks toward
the leading hemisphere of Enceladus.