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Scientists are particularly interested in Saturn's moon Titan because it's one of the few known moons with its own dense atmosphere. Titan's atmosphere is also thought to be very similar to what Earth's atmosphere was a long time ago. By learning about Titan, we'll learn about our own planet.
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For current information about the NASA Astrobiology Program, please visit http://astrobiology.nasa.gov/


2003-12-30 | MISSIONS
Destination: Gusev Crater

On January 3, Spirit, NASA’s 400-pound rover, is scheduled to land on what may be a dried-up lake bed on Mars. “There’s not much doubt: this site contained a body of liquid water, at least for some amount of time,” says Jim Garvin, NASA’s Lead Scientist for Mars Exploration. The site is Gusev Crater, a 90-mile wide hole in the ground that probably formed three to four billion years ago when an asteroid crashed just south of Mars’ equator. There’s a channel system that drains into it, which probably carried liquid water, or water and ice, into the crater.

NASA's Mars Exploration Rovers are quickly approaching Mars. Once there, the twin rovers will examine separate sites for geological information about the history of water on Mars. Because life as we know it requires water to survive, understanding the history of liquid water on Mars is vital for determining the potential for past or present life on the planet.


More on this story Full text of original item from NASA, Dec 30, 2003

Related news stories

Dec 13, 2004 | MISSIONS
Mars Rovers Spot Water-Clue Mineral, Frost, Clouds
(NASA - JPL) - Scientists have identified a water-signature mineral in bedrock examined by Spirit in the "Colombia Hills."

Nov 11, 2004 | MISSIONS
Mars Exploration Rover Mission Status
(NASA - JPL) - Operators for the Opportunity rover are choosing a path for exiting Endurance Crater.

Aug 18, 2004 | MISSIONS
Bedrock in Mars' Gusev Crater Hints at Watery Past
(NASA - JPL) - Spirit has found evidence that water thoroughly altered some rocks in Mars' Gusev Crater.


The preceding news links are provided as a public service for interested users. The views and claims expressed in external internet sites are not necessarily those of NASA.

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