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Mars Rover Curiosity Finds Evidence of Stream

JPL scientists gave an update on Thursday about the Mars mission from the rover Curiosity

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    NEWSLETTERS

    NASA's Curiosity rover mission has found evidence a stream once ran vigorously across the area on Mars where the rover is driving, NASA scientists said on Thursday. Whit Johnson reports for the NBC4 News at 5 p.m. on Sept. 27, 2012.

    NASA's Curiosity rover mission has found evidence a stream once ran vigorously across the area on Mars where the rover is driving, NASA scientists said on Thursday.

    There is earlier evidence for the presence of water on Mars, but this evidence -- images of rocks containing ancient streambed gravels -- is the first of its kind.

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    Dr. Tyler Nordgren contributed to the Mars Rover Curiosity by designing its sundial, designed to help the rover's camera take color photos to better illustrate what Mars really looks like. Jacob Rascon reports from Redlands for the NBC4 News at 5 p.m. on August 6, 2012.

    Details about the mission were unveiled on Thursday at a press conference at the Jet Propulsion Laboratory, a division of Caltech, which built Curiosity and manages the Mars Science Laboratory Project for NASA.

    Scientists are studying the images of stones cemented into a layer of conglomerate rock. The sizes and shapes of stones offer clues to the speed and distance of a long-ago stream's flow.

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    Scientists say the Mars Rover Curiosity is doing exactly what it was designed to do and NASA engineers are ecstatic. The science laboratory is designed to pull samples from Mars' surface to determine if life may have existed on the red planet. Images have already started coming in. Conan Nolan reports from La Canada Flintridge for the NBC4 News at 4 p.m. on August 6, 2012.

    "From the size of gravels it carried, we can interpret the water was moving about 3 feet per second, with a depth somewhere between ankle and hip deep," said Curiosity science co-investigator William Dietrich of the University of California, Berkeley. "Plenty of papers have been written about channels on Mars with many different hypotheses about the flows in them. This is the first time we're actually seeing water-transported gravel on Mars. This is a transition from speculation about the size of streambed material to direct observation of it."

    The finding site lies between the north rim of Gale Crater and the base of Mount Sharp, a mountain inside the crater.

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    The orbiter flew over NASA's Jet Propulsion Laboratory in La Cañada Flintridge Friday where employees gathered on the roof of a parking lot to watch the shuttle's final flight. Patrick Healy reports from JPL at La Cañada Flintridge for the NBC4 News at 6 p.m. on Sept. 21, 2012.

    Earlier imaging of the region from Mars orbit allows for additional interpretation of the gravel-bearing conglomerate. The imagery shows an alluvial fan of material washed down from the rim, streaked by many apparent channels, sitting uphill of the new finds.

    The science team may use Curiosity to learn the elemental composition of the material, which holds the conglomerate together, revealing more characteristics of the wet environment that formed these deposits. The stones in the conglomerate provide a sampling from above the crater rim, so the team may also examine several of them to learn about broader regional geology.

    The slope of Mount Sharp in Gale Crater remains the rover's main destination. Clay and sulfate minerals detected there from orbit can be good preservers of carbon-based organic chemicals that are potential ingredients for life.

    "A long-flowing stream can be a habitable environment," said Grotzinger. "It is not our top choice as an environment for preservation of organics, though. We're still going to Mount Sharp, but this is insurance that we have already found our first potentially habitable environment."

    During the two-year prime mission of the Mars Science Laboratory,esearchers will use Curiosity's 10 instruments to investigate whether areas in Gale Crater have ever offered environmental conditions favorable for microbial life.

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