Scientists using an instrument on NASA’s Cassini orbiter have confirmed that at least one other body in our solar system has a liquid lake. The lake, probably composed of ethane, is 150 miles long and located near the south pole of Saturn’s moon, Titan.
The liquid lake was identified using Cassini’s visual and infrared mapping spectrometer (VIMS), an instrument run from The University Arizona which identifies the chemical composition of objects by the way matter reflects light. When VIMS observed the lake, named Ontario Lacus, it detected ethane. The ethane is in liquid solution with methane, nitrogen and other low-molecular weight hydrocarbons.
The ubiquitous hydrocarbon haze in Titan’s atmosphere hinders the view to Titan’s surface but there are transparent atmospheric “windows” at certain infrared light wavelengths through which Cassini’s VIMS can see to the ground. VIMS observed Ontario Lacus on Cassini’s 38th close flyby of Titan in December 2007.
The lake is roughly 7,800 square miles, just slightly larger than North America’s Lake Ontario. Infrared spectroscopy doesn’t indicate how deep the lake is, but the scientists speculate that it must be at least three-quarters of an inch deep.
Before the Cassini mission, scientists thought that Titan would be awash in global oceans of ethane and other light hydrocarbons, the byproducts of photolysis, or the action of ultraviolet light on methane over 4.5 billion years of solar system history. But 40 close flybys of Titan by the Cassini spacecraft show no such oceans exist.
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