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            "id": 11374,
            "url": "https://svs.gsfc.nasa.gov/11374/",
            "result_type": "Produced Video",
            "release_date": "2013-11-05T00:00:00-05:00",
            "title": "Craterology",
            "description": "To better understand how Earth evolved, scientists are pointing cameras toward impact craters on the moon. Impact craters are giant surface depressions that form in the aftermath of collisions by asteroids, meteoroids and comets. Exposure to wind, water and geologic activity slowly degrades impact craters found on Earth. But by knowing how a crater has changed over time, scientists can piece together clues of what conditions were like on the planet long ago. Now, NASA’s Lunar Reconnaissance Orbiter spacecraft is collecting images of impact craters on the moon’s surface. Unlike on Earth, these craters aren’t prone to weathering because the moon has practically no atmosphere. As a result, some have remained untouched since the day they were born. Scientists will use the images to determine how natural disasters and the climates of Earth’s past have shaped how its craters look today. Watch the video to learn more. || ",
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            "id": 11113,
            "url": "https://svs.gsfc.nasa.gov/11113/",
            "result_type": "Produced Video",
            "release_date": "2012-10-17T09:00:00-04:00",
            "title": "Planetary Scientist Profile: Lynn Carter",
            "description": "NASA scientist Lynn Carter talks about her work in the Planetary Geodynamics Laboratory. || ",
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            "id": 10915,
            "url": "https://svs.gsfc.nasa.gov/10915/",
            "result_type": "Produced Video",
            "release_date": "2012-02-20T11:00:00-05:00",
            "title": "NASA Spacecraft Reveals Recent Geological Activity on the Moon",
            "description": "New images acquired by NASA's Lunar Reconnaissance Orbiter (LRO) spacecraft show that the moon's crust is being slightly stretched, forming small valleys - at least in some small areas. High-resolution images obtained by the Lunar Reconnaissance Orbiter Camera (LROC) provide evidence that these valleys are very young, suggesting the moon has experienced relatively recent geologic activity. || ",
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        {
            "id": 40063,
            "url": "https://svs.gsfc.nasa.gov/gallery/lunar-reconnaissance-orbiter/",
            "result_type": "Gallery",
            "release_date": "2010-03-04T00:00:00-05:00",
            "title": "Lunar Reconnaissance Orbiter",
            "description": "The Lunar Reconnaissance Orbiter, or LRO, is a multipurpose NASA spacecraft launched in 2009 to make a comprehensive atlas of the Moon’s features and resources. Since launch, LRO has measured the coldest temperatures in the solar system inside the Moon’s permanently shadowed craters, detected evidence of water ice at the Moon’s south pole, seen hints of recent geologic activity on the Moon, found newly-formed craters from present-day meteorite impacts, tested spaceborne laser communication technology, and much more.",
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            "url": "https://svs.gsfc.nasa.gov/3574/",
            "result_type": "Visualization",
            "release_date": "2009-01-15T00:00:00-05:00",
            "title": "Methane Plume on Mars",
            "description": "The first definitive detection of methane in the atmosphere of Mars indicates the planet is alive in the sense that it still has geologic activity powered by heat from its interior, according to a team of NASA and university scientists. The team used spectrometer instruments attached to several telescopes to detect plumes of methane that were emitted from specific sites during the warmer seasons - spring and summer. Though nothing conclusive can yet be determined, it is possible that the detected methane was either produced by geologic processes such as the oxidation of iron (serpentinization) or by microscopic Martian life below the planet's surface. The methane released today could be produced currently, or it could be ancient methane trapped in ice 'cages' called clathrates or as gas below a sub-surface ice layer. || ",
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