{
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    "next": null,
    "previous": null,
    "results": [
        {
            "id": 2882,
            "url": "https://svs.gsfc.nasa.gov/2882/",
            "result_type": "Visualization",
            "release_date": "2004-05-02T12:00:00-04:00",
            "title": "Zoom down to the Gale Crater on Mars",
            "description": "This is a zoom down to the Gale Crater on MARS as seen by Viking and the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC).  These images show a very large area of sedimentation inside the Gale Crater.  The origin of the sedimentary material remains unanswered. Studying these layers of rocks could answer many questions about the history of MARS. || ",
            "hits": 24
        },
        {
            "id": 2864,
            "url": "https://svs.gsfc.nasa.gov/2864/",
            "result_type": "Visualization",
            "release_date": "2004-04-22T12:00:00-04:00",
            "title": "Earth-Mars Volcano Comparisons: Final Composite",
            "description": "Despite the 2:1 relative size difference between Earth and Mars, the Martian volcano, Olympus Mons, still dwarfs Earth's Mauna Loa, Hawaii volcano. When measured from the ocean floor, Mauna Loa is 10km. high compared to Olympus Mons at 23km. This post-produced animation composite was created using various elements from animations #2865 through #2872. || ",
            "hits": 128
        },
        {
            "id": 2868,
            "url": "https://svs.gsfc.nasa.gov/2868/",
            "result_type": "Visualization",
            "release_date": "2004-04-22T12:00:00-04:00",
            "title": "Earth-Mars Volcano Comparisons: True Color Mars",
            "description": "Despite the 2:1 relative size difference between Earth and Mars, the Martian volcano, Olympus Mons, dwarfs Earth's Mauna Loa, Hawaii volcano. When measured from the ocean floor, Mauna Loa is approximately 10km. high compared to Olympus Mons at 23km. This animation is one element of the Earth-Mars comparison, showing Mars in it's true color beauty. The beginning of this animation is match-framed to animations #2864 through #2872. || ",
            "hits": 51
        },
        {
            "id": 2869,
            "url": "https://svs.gsfc.nasa.gov/2869/",
            "result_type": "Visualization",
            "release_date": "2004-04-22T12:00:00-04:00",
            "title": "Earth-Mars Volcano Comparisons: Elevation Color-Mapped Mars",
            "description": "Despite the 2:1 relative size difference between Earth and Mars, the Martian volcano, Olympus Mons, dwarfs Earth's Mauna Loa, Hawaii volcano.  When measured from the ocean floor, Mauna Loa is approximately 10km. high compared to Olympus Mons at 23km.  This animation is one element of the Earth-Mars comparison.  It shows Mars' differing terrain via an elevation color map.  Yellow indicates the mean elevation.  Green, blue, and purple are low lying areas.  Red, brown, and white are the highest elevations.  This animation is match-framed to animations #2864 through #2872 and uses the same color map as animation #2866. || ",
            "hits": 468
        },
        {
            "id": 2870,
            "url": "https://svs.gsfc.nasa.gov/2870/",
            "result_type": "Visualization",
            "release_date": "2004-04-22T12:00:00-04:00",
            "title": "Earth-Mars Volcano Comparisons: True Color Olympus Mons over Elevation Color-Mapped Earth Bathymetry with True Color Land Features",
            "description": "Despite the 2:1 relative size difference between Earth and Mars, the Martian volcano, Olympus Mons, dwarfs Earth's Mauna Loa, Hawaii volcano. When measured from the ocean floor, Mauna Loa is approximately 10km. high compared to Olympus Mons at 23km. In this animation, Olympus Mons obstructs the view of Mauna Loa, but gives the viewer a good perspective of the overall size of this giant volcano. This animation is match-framed to animations #2864 through #2872. || ",
            "hits": 118
        },
        {
            "id": 2871,
            "url": "https://svs.gsfc.nasa.gov/2871/",
            "result_type": "Visualization",
            "release_date": "2004-04-22T12:00:00-04:00",
            "title": "Earth-Mars Volcano Comparisons: Transparent Olympus Mons over Elevation Color-Mapped Earth with True Color Land",
            "description": "Despite the 2:1 relative size difference between Earth and Mars, the Martian volcano, Olympus Mons, dwarfs Earth's Mauna Loa, Hawaii volcano. When measured from the ocean floor, Mauna Loa is approximately 10km. high compared to Olympus Mons at 23km. In this animation, a transparent Olympus Mons is juxtaposed over Mauna Loa, allowing the viewer to better see the size differences between these land masses. This animation is match-framed to animations #2864 through #2872. || ",
            "hits": 108
        },
        {
            "id": 2872,
            "url": "https://svs.gsfc.nasa.gov/2872/",
            "result_type": "Visualization",
            "release_date": "2004-04-22T12:00:00-04:00",
            "title": "Earth-Mars Volcano Comparisons: Mars Inside a Transparent Earth",
            "description": "Despite the 2:1 relative size difference between Earth and Mars, the Martian volcano, Olympus Mons, dwarfs Earth's Mauna Loa, Hawaii volcano. When measured from the ocean floor, Mauna Loa is approximately 10km. high compared to Olympus Mons at 23km. This animation not only shows the relative size differences between Mauna Loa and Olympus Mons, but also shows the size difference between these 2 planets. The equatorial radius of Mars is approximately 3397 km. compared to Earth's equatorial radius of 6378.1 km. This animation is match-framed to animations #2864 through #2872. || ",
            "hits": 81
        },
        {
            "id": 2778,
            "url": "https://svs.gsfc.nasa.gov/2778/",
            "result_type": "Visualization",
            "release_date": "2003-07-03T12:00:00-04:00",
            "title": "Mars Odyssey: Mars' Northern Hemisphere",
            "description": "NASA's Mars Odyssey detected water ice in the northern hemisphere. During the winter months, the icy soil is covered by a thick layer of carbon dioxide ('dry ice') frost obscuring the water ice signature. This animation is match-framed to animation 2779 and animation 2780. Its purpose is to establish a frame of reference using a true color data set. In this case, that data is from Viking. || ",
            "hits": 36
        },
        {
            "id": 2779,
            "url": "https://svs.gsfc.nasa.gov/2779/",
            "result_type": "Visualization",
            "release_date": "2003-07-03T12:00:00-04:00",
            "title": "Mars Odyssey: Water Ice/Winter Observations",
            "description": "NASA's Mars Odyssey detected water ice in the northern hemisphere. During the winter months, the icy soil is covered by a thick layer of carbon dioxide ('dry ice') frost obscuring the water ice signature.This animation is match-framed to animation #2778 and animation #2780. It shows the areas of ice during a martian winter. || ",
            "hits": 48
        },
        {
            "id": 2780,
            "url": "https://svs.gsfc.nasa.gov/2780/",
            "result_type": "Visualization",
            "release_date": "2003-07-03T12:00:00-04:00",
            "title": "Mars Odyssey: Water Ice/Summer Observations",
            "description": "NASA's Mars Odyssey detected water ice in the northern hemisphere. During the winter months, the icy soil is covered by a thick layer of carbon dioxide ('dry ice') frost obscuring the water ice signature.This animation is match-framed to #2778 and #2779. It shows the areas of ice during a martian summer. || ",
            "hits": 35
        },
        {
            "id": 764,
            "url": "https://svs.gsfc.nasa.gov/764/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "Mars Polar Lander Landing Site: Global View to False Color MOLA Inset",
            "description": "This is one of a series of visualizations showing false-colored renderings of the Martian topography measured by MOLA in the vicinity of the Mars Polar Lander landing site. Blue tones represent elevations of less than 2 kilometers, while reddish tones are greater than about 2.8 kilometers, relative to the mean equatorial height of Mars. The elevation of the landing site is about 2.4 km, midway into the polar layered terrain. The  400 meters (1/4 mile) resolution of the MOLA data gives a smoothed but vertically exaggerated view of the topography. At this scale it is impossible to ascertain the actual roughness at the lander's destination, forcing project directors to make their best guesses based on available data. || ",
            "hits": 12
        },
        {
            "id": 765,
            "url": "https://svs.gsfc.nasa.gov/765/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "Close Up Fly Over of Mars Polar Lander Landing Area in True Color",
            "description": "This is one of a series of visualizations showing false-colored renderings of the Martian topography measured by MOLA in the vicinity of the Mars Polar Lander landing site. Blue tones represent elevations of less than 2 kilometers, while reddish tones are greater than about 2.8 kilometers, relative to the mean equatorial height of Mars. The elevation of the landing site is about 2.4 km, midway into the polar layered terrain. The 400 meters (1/4 mile) resolution of the MOLA data gives a smoothed but vertically exaggerated view of the topography. At this scale it is impossible to ascertain the actual roughness at the lander's destination, forcing project directors to make their best guesses based on available data. || ",
            "hits": 8
        },
        {
            "id": 766,
            "url": "https://svs.gsfc.nasa.gov/766/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "Close Up Fly Over of Mars Polar Lander Landing Area in False Color",
            "description": "This is one of a series of visualizations showing false-colored renderings of the Martian topography measured by MOLA in the vicinity of the Mars Polar Lander landing site. Blue tones represent elevations of less than 2 kilometers, while reddish tones are greater than about 2.8 kilometers, relative to the mean equatorial height of Mars. The elevation of the landing site is about 2.4 km, midway into the polar layered terrain. The 400 meters (1/4 mile) resolution of the MOLA data gives a smoothed but vertically exaggerated view of the topography. At this scale it is impossible to ascertain the actual roughness at the lander's destination, forcing project directors to make their best guesses based on available data. || ",
            "hits": 2
        },
        {
            "id": 767,
            "url": "https://svs.gsfc.nasa.gov/767/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "A Comparison of Visible and Topographic Data for the Martian South Pole: Version 1",
            "description": "This is one of a series of visualizations showing false-colored renderings of the Martian topography measured by MOLA in the vicinity of the Mars Polar Lander landing site. Blue tones represent elevations of less than 2 kilometers, while reddish tones are greater than about 2.8 kilometers, relative to the mean equatorial height of Mars. The elevation of the landing site is about 2.4 km, midway into the polar layered terrain. The 400 meters (1/4 mile) resolution of the MOLA data gives a smoothed but vertically exaggerated view of the topography. At this scale it is impossible to ascertain the actual roughness at the lander's destination, forcing project directors to make their best guesses based on available data. || ",
            "hits": 11
        },
        {
            "id": 768,
            "url": "https://svs.gsfc.nasa.gov/768/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "A Comparison of Visible and Topographic Data for the Martian South Pole: Version 2",
            "description": "This is one of a series of visualizations showing false-colored renderings of the Martian topography measured by MOLA in the vicinity of the Mars Polar Lander landing site. Blue tones represent elevations of less than 2 kilometers, while reddish tones are greater than about 2.8 kilometers, relative to the mean equatorial height of Mars. The elevation of the landing site is about 2.4 km, midway into the polar layered terrain. The 400 meters (1/4 mile) resolution of the MOLA data gives a smoothed but vertically exaggerated view of the topography. At this scale it is impossible to ascertain the actual roughness at the lander's destination, forcing project directors to make their best guesses based on available data. || ",
            "hits": 6
        },
        {
            "id": 769,
            "url": "https://svs.gsfc.nasa.gov/769/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "A Rotating True Color View of the Martian South Pole",
            "description": "This is one of a series of visualizations showing false-colored renderings of the Martian topography measured by MOLA in the vicinity of the Mars Polar Lander landing site. Blue tones represent elevations of less than 2 kilometers, while reddish tones are greater than about 2.8 kilometers, relative to the mean equatorial height of Mars. The elevation of the landing site is about 2.4 km, midway into the polar layered terrain. The 400 meters (1/4 mile) resolution of the MOLA data gives a smoothed but vertically exaggerated view of the topography. At this scale it is impossible to ascertain the actual roughness at the lander's destination, forcing project directors to make their best guesses based on available data. || ",
            "hits": 19
        },
        {
            "id": 770,
            "url": "https://svs.gsfc.nasa.gov/770/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "A Rotating False Color View of the Martian South Pole from MOLA",
            "description": "This is one of a series of visualizations showing false-colored renderings of the Martian topography measured by MOLA in the vicinity of the Mars Polar Lander landing site. Blue tones represent elevations of less than 2 kilometers, while reddish tones are greater than about 2.8 kilometers, relative to the mean equatorial height of Mars. The elevation of the landing site is about 2.4 km, midway into the polar layered terrain. The 400 meters (1/4 mile) resolution of the MOLA data gives a smoothed but vertically exaggerated view of the topography. At this scale it is impossible to ascertain the actual roughness at the lander's destination, forcing project directors to make their best guesses based on available data. || ",
            "hits": 23
        },
        {
            "id": 771,
            "url": "https://svs.gsfc.nasa.gov/771/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "A Rotating False Color View of the Martian South Pole from MOLA: New Color Map",
            "description": "This is one of a series of visualizations showing false-colored renderings of the Martian topography measured by MOLA in the vicinity of the Mars Polar Lander landing site. || ",
            "hits": 12
        },
        {
            "id": 773,
            "url": "https://svs.gsfc.nasa.gov/773/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "Push in South of the Hellas Basin Showing Topography from MOLA",
            "description": "Zoom into the region of Mars just south of the Hellas Basin showing topography data from MOLA.  Blue tones represent elevations of less than 2 kilometers, while reddish tones are greater than about 2.8 kilometers, relative to the mean equatorial height of Mars. || a000773.00010_print.png (720x480) [508.9 KB] || a000773_pre.jpg (320x238) [7.8 KB] || a000773.webmhd.webm (960x540) [3.7 MB] || a000773.dv (720x480) [145.1 MB] || a000773.mp4 (640x480) [8.9 MB] || a000773.mpg (352x240) [5.7 MB] || ",
            "hits": 17
        },
        {
            "id": 774,
            "url": "https://svs.gsfc.nasa.gov/774/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "Push in South of the Hellas Basin Showing Topography from MOLA: New Color Map",
            "description": "Zoom into the region of Mars just south of the Hellas Basin showing topography data from MOLA.  This animation uses a color table designed to highlight the topography at the south pole.  White colors indicate elevations in excess of 3012 meters, red shows elevations between 2500 and 3012 meters, yellow shows elevations from 2450 to 2500 meters, dark cyan shows elevations from 2150 to 2450 meters, dark violet shows elevations from 320 to 2150 meters. || a000774.00010_print.png (720x480) [401.1 KB] || a000774_pre.jpg (320x238) [6.0 KB] || a000774.webmhd.webm (960x540) [5.6 MB] || a000774.dv (720x480) [151.6 MB] || a000774.mp4 (640x480) [8.9 MB] || a000774.mpg (352x240) [1.8 MB] || ",
            "hits": 4
        },
        {
            "id": 776,
            "url": "https://svs.gsfc.nasa.gov/776/",
            "result_type": "Visualization",
            "release_date": "1999-11-22T12:00:00-05:00",
            "title": "Mars Southern Hemisphere Rotation in False Color from MOLA",
            "description": "Blue represents low topography and red or white represent areas of high topography. || Watching MOLA topography data of the southern hemisphere of Mars on a rotating globe || a000776.00010_print.png (720x480) [512.4 KB] || a000776_pre.jpg (320x238) [7.8 KB] || a000776.webmhd.webm (960x540) [3.9 MB] || a000776.dv (720x480) [122.5 MB] || a000776.mp4 (640x480) [7.0 MB] || a000776.mpg (352x240) [4.9 MB] || ",
            "hits": 62
        }
    ]
}