{
    "id": 4097,
    "url": "https://svs.gsfc.nasa.gov/4097/",
    "page_type": "Visualization",
    "title": "Greenland's Mega-Canyon beneath the Ice Sheet",
    "description": "Subglacial topography plays an important role in modulating the distribution and flow of meltwater beneath the ice known as basal water flow. This animation portrays topographic data of the bedrock under the Greenland ice sheet derived from ice-penetrating radar data. Clearly evident in the topography is a 750-km-long subglacial canyon in northern Greenland that is likely to have influenced basal water flow from the ice sheet interior to the margin. The authors suggest that the mega-canyon predates ice sheet inception and has influenced basal hydrology in Greenland over past glacial cycles. (See reference under \"Science Paper\" below)Starting with a view of the surface of Greenland, the animation zooms closer to the surface as the ice sheet is stripped away to reveal the false-color topography of the bedrock that lies beneath. Regions above sea level are shown in shades of green while areas below zero are colored by shades of brown. Yellow indicates the area near sea level. The topography is exaggerated from 12 to 40 times in order to accentuate the topographic relief. Visible in the topography from about the midpoint of Greenland to its Northwest coast is the 750-km-long subglacial canyon described by the authors. || ",
    "release_date": "2013-08-29T14:00:00-04:00",
    "update_date": "2023-05-03T13:51:53.780411-04:00",
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        "alt_text": "Animation of Greenland's mega-canyon.This video is also available on our YouTube channel.",
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        "filename": "canale_grande_V05_p30_1080.mp4",
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        "alt_text": "Animation of Greenland's mega-canyon.This video is also available on our YouTube channel.",
        "width": 1920,
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    "main_credits": {
        "Visualizations by": [
            {
                "name": "Cindy Starr",
                "employer": "Global Science and Technology, Inc."
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    "progress": "Complete",
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            "description": "Subglacial topography plays an important role in modulating the distribution and flow of meltwater beneath the ice known as basal water flow. This animation portrays topographic data of the bedrock under the Greenland ice sheet derived from ice-penetrating radar data. Clearly evident in the topography is a 750-km-long subglacial canyon in northern Greenland that is likely to have influenced basal water flow from the ice sheet interior to the margin. The authors suggest that the mega-canyon predates ice sheet inception and has influenced basal hydrology in Greenland over past glacial cycles. (See reference under \"Science Paper\" below)<p><p>Starting with a view of the surface of Greenland, the animation zooms closer to the surface as the ice sheet is stripped away to reveal the false-color topography of the bedrock that lies beneath. Regions above sea level are shown in shades of green while areas below zero are colored by shades of brown. Yellow indicates the area near sea level. The topography is exaggerated from 12 to 40 times in order to accentuate the topographic relief. Visible in the topography from about the midpoint of Greenland to its Northwest coast is the 750-km-long subglacial canyon described by the authors.",
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        "<p><p>Bamber, J.L., Siegert, M.J., Griggs, J.A., Marshall, S., Spada, G. Paleofluvial canyon drains subglacial water from northern Greenland, Science, 2013.<p>Bamber, J. L., Griggs, J. A., Hurkmans, R. T. W. L., Dowdeswell, J. A., Gogineni, S. P., Howat, I., Mouginot, J., Paden, J., Palmer, S., Rignot, E., and Steinhage, D.: A new bed elevation dataset for Greenland, The Cryosphere, 7, 499-510, 10.5194/tc-7-499-2013, 2013. (<a href=\"http://www.the-cryosphere.net/7/499/2013/doi:10.5194/tc-7-499-2013\">Available here.</a>)",
        "<p><p>Bamber, J.L., Siegert, M.J., Griggs, J.A., Marshall, S., Spada, G. Paleofluvial canyon drains subglacial water from northern Greenland, Science, 2013.<p>Bamber, J. L., Griggs, J. A., Hurkmans, R. T. W. L., Dowdeswell, J. A., Gogineni, S. P., Howat, I., Mouginot, J., Paden, J., Palmer, S., Rignot, E., and Steinhage, D.: A new bed elevation dataset for Greenland, The Cryosphere, 7, 499-510, 10.5194/tc-7-499-2013, 2013. (<a href=\"http://www.the-cryosphere.net/7/499/2013/doi:10.5194/tc-7-499-2013\">Available here.</a>)"
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            "page_type": "Produced Video",
            "title": "Megacanyon",
            "description": "Ice has blanketed Greenland for millions of years. In some places it can be almost two miles thick. Scientists now know that hidden beneath the ice is a canyon that extends hundreds of miles north from near the center of the ice sheet. By combining more than four years’ worth of ice-penetrating radar measurements from NASA’s Operation IceBridge mission with other data sets, researchers created a topographic map of Greenland’s bedrock. The map shed light on the existence of a canyon that measures at least 460 miles in length and a half-mile deep. At greater than 1.5 times the length of the Grand Canyon, it is longer than any known canyon on Earth. Watch the visualization for a tour of Greenland’s massive, under-ice canyon. In the visualization the terrain elevation is shown using color, where greens indicate areas above sea level, browns indicate areas below sea level, and yellows indicate areas at or near sea level. || ",
            "release_date": "2013-09-17T00:00:00-04:00",
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