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    "results": [
        {
            "id": 30215,
            "url": "https://svs.gsfc.nasa.gov/30215/",
            "result_type": "Hyperwall Visual",
            "release_date": "2019-03-15T18:00:00-04:00",
            "title": "Urban Growth in Las Vegas",
            "description": "The city of Las Vegas—meaning the meadows—was established in 1905. Its grassy meadows and artesian springs attracted settlers traveling across the arid Desert Southwest in the early 1800s. In the 1930s, gambling became legalized and construction of the Hoover Dam began, resulting in the city's first growth spurt. Since then, Las Vegas has not stopped growing. Population has reached nearly two million over the past decade, becoming one of the fastest growing metropolitan areas in the world. These false-color images show the rapid urbanization of Las Vegas between 1972 and 2018. The city streets and other impervious surfaces appear gray, while irrigated vegetation appears red. Over the years, the expansion of irrigated vegetation (e.g., lawns and golf courses) has stretched the city’s desert bounds. || ",
            "hits": 469
        },
        {
            "id": 30761,
            "url": "https://svs.gsfc.nasa.gov/30761/",
            "result_type": "Hyperwall Visual",
            "release_date": "2017-07-29T00:00:00-04:00",
            "title": "Cape Canaveral and Orlando Landsat timeseries",
            "description": "Kennedy Space Center and Orlando land cover change.Since December 1968, the John F. Kennedy Space Center (KSC) has been NASA's primary launch center of human spaceflight. The center is home to one Launch Complex (LC) with two pads: LC-39A and LC-39B. Built on a swamp, the two pads were originally constructed in the 1960s as clean pads and served as a starting point for Apollo and our journey to the moon.This pair of false-color images shows KSC and the adjacent Cape Canaveral Air Force Station in 1972 and 2016. Acquired with the Landsat series of satellites, the scenes are shown in green, red, and near-infrared light, a combination that helps differentiate components of the landscape. Vegetation is red, while urban areas are brown to gray. West of launch pads 39A and 39B, you can see the facility’s 525-foot-tall Vehicle Assembly Building (for stacking NASA's largest rockets), the 3-mile-long Shuttle Landing Facility, and the iconic Kennedy Space Center Visitor Complex.  As of 2017, only Launch Complex 39A is active, launching SpaceX's Falcon 9. Launch Complex 39B will serve as the launch site for the agency's Space Launch System rocket and Orion spacecraft on deep-space missions, including the journey to Mars. South of KSC, launch pads (active and inactive) line the coast of Cape Canaveral Air Force Station (CCAFS). || ",
            "hits": 83
        },
        {
            "id": 3509,
            "url": "https://svs.gsfc.nasa.gov/3509/",
            "result_type": "Visualization",
            "release_date": "2008-04-16T00:00:00-04:00",
            "title": "Las Vegas Growth from Landsat",
            "description": "This sequence of images from the earliest Landsat satellite to the present captures the dramatic growth of Las Vegas, Nevada. From 1973 to 2006, the population of Las Vegas grew from 358,000 to over 2 million. || ",
            "hits": 49
        },
        {
            "id": 3116,
            "url": "https://svs.gsfc.nasa.gov/3116/",
            "result_type": "Visualization",
            "release_date": "2005-03-02T12:00:00-05:00",
            "title": "Mount St. Helens Before, During, and After (WMS)",
            "description": "Mount St. Helens erupted on May 18, 1980, devastating more than 150 square miles of forest in southwestern Washington state. This animation shows Landsat images of the Mount St. Helens area in 1973, 1983, and 2000, illustrating the destruction and regrowth of the forest. The 1983 image clearly shows the new crater on the northern slope where the eruption occurred, the rivers and lakes covered with ash, and the regions of deforestation. The 2000 image, taken twenty years after the eruption, still shows the changed crater, but much of the devastated area is covered by new vegetation growth. || ",
            "hits": 139
        },
        {
            "id": 3112,
            "url": "https://svs.gsfc.nasa.gov/3112/",
            "result_type": "Visualization",
            "release_date": "2005-02-15T12:00:00-05:00",
            "title": "Aral Sea Evaporation (WMS)",
            "description": "The Aral Sea is actually not a sea at all, but an immense fresh water lake. In the last thirty years, more than sixty percent of the lake has disappeared because much of the river flow feeding the lake was diverted to irrigate cotton fields and rice paddies. Concentrations of salts and minerals began to rise in the shrinking body of water, leading to staggering alterations in the lake's ecology and precipitous drops in the Aral's fish population. Powerful winds that blow across this part of Asia routinely pick up and deposit the now exposed lake bed soil. This has contributed to a significant reduction in breathable air quality, and crop yields have been appreciably affected due to heavily salt laden particles falling on arable land. This series of Landsat images taken in 1973, 1987 and 2000 show the profound reduction in overall area at the north end of the Aral, and a commensurate increase in land area as the floor of the sea now lies exposed. || ",
            "hits": 47
        },
        {
            "id": 2911,
            "url": "https://svs.gsfc.nasa.gov/2911/",
            "result_type": "Visualization",
            "release_date": "2004-02-13T12:00:00-05:00",
            "title": "Urbanization around the Pearl River Estuary in China from 1973 through 2001 (WMS)",
            "description": "The region around the Pearl River Estuary in southern China experienced rapid urban growth in the 1980s and 1990s. This growth was spurred by the establishment of special government economic zones, particularly in Shenzhen, just to the east of the estuary. Urban areas increased by more than 300% between 1988 and 1996. This growth can be directly assessed by remote sensing measurements from space, particularly by comparing images from the Landsat sensors for the last thirty years. This animation shows nine such images in sequence, from the years 1973, 1975, 1977, 1979, 1988, 1992, 1995, 2000, and 2001. || ",
            "hits": 33
        },
        {
            "id": 2761,
            "url": "https://svs.gsfc.nasa.gov/2761/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "Landsat-7 20 Year Urbanization of Deep Bay near Shenzhen, China",
            "description": "The long operational history of the Landsat satellite allows a detailed study of urban growth around the world, as illustrated by this animation of urbanization around Shenzen, China. || ",
            "hits": 30
        },
        {
            "id": 2762,
            "url": "https://svs.gsfc.nasa.gov/2762/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "Landsat 7 20 Year Urbanization West of Shenzhen, China",
            "description": "The long operational history of the Landsat satellite allows a detailed study of urban growth around the world, as illustrated by this animation of urbanization around Shenzen, China. || ",
            "hits": 42
        },
        {
            "id": 2763,
            "url": "https://svs.gsfc.nasa.gov/2763/",
            "result_type": "Visualization",
            "release_date": "2003-06-23T12:00:00-04:00",
            "title": "Landsat-7 20-Year Urbanization of Shenzhen, China",
            "description": "The long operational history of the Landsat satellite allows a detailed study of urban growth around the world, as illustrated by this animation of urbanization around Shenzen, China. || ",
            "hits": 22
        },
        {
            "id": 2357,
            "url": "https://svs.gsfc.nasa.gov/2357/",
            "result_type": "Visualization",
            "release_date": "2002-02-05T12:00:00-05:00",
            "title": "Salt Lake City, Utah: Growth Over Time!",
            "description": "Growth over time, comparing two data sets from the Landsat satellite series. The first data set was collected on August 7, 1972. The second data set was collected on July 31, 2000. || ",
            "hits": 21
        },
        {
            "id": 2358,
            "url": "https://svs.gsfc.nasa.gov/2358/",
            "result_type": "Visualization",
            "release_date": "2002-02-05T12:00:00-05:00",
            "title": "Salt Lake, Utah: Growth Over Time!",
            "description": "Comparing two data sets for Salt Lake, Utah, from the Landsat satellite series. The first data set is from August 7, 1972; the second, from July 31, 2000. || ",
            "hits": 22
        },
        {
            "id": 2359,
            "url": "https://svs.gsfc.nasa.gov/2359/",
            "result_type": "Visualization",
            "release_date": "2002-02-05T12:00:00-05:00",
            "title": "Bingham Coppermine, Utah: Growth Over Time!",
            "description": "Comparing two data sets for Bingham Canyon Copper Mine, Utah, from the Landsat satellite series. The first data set is from August 7, 1972; the second, from July 31, 2000. || ",
            "hits": 8
        },
        {
            "id": 2323,
            "url": "https://svs.gsfc.nasa.gov/2323/",
            "result_type": "Visualization",
            "release_date": "2001-12-10T12:00:00-05:00",
            "title": "Dhaka, Bangladesh Urban Growth",
            "description": "The population of Dhaka, Bangladesh grew in size considerably between 1972 and 2001. This 'urban growth' can be easily seen through various Landsat satellite images over time. || ",
            "hits": 79
        },
        {
            "id": 2210,
            "url": "https://svs.gsfc.nasa.gov/2210/",
            "result_type": "Visualization",
            "release_date": "2001-08-02T12:00:00-04:00",
            "title": "Landsat Witnesses the Destruction of Mesopotamian Ecosystem",
            "description": "In one of the greatest ecological disasters of our time, the ancient marshlands of Mesopotamia are systematically being converted to dry salt flats as a result of human mismanagement of the region's water resources.Landsat satellite imagery reveals that in the last 10 years, wetlands that once covered as much as 20,000 square km in parts of Iraq and Iran have been reduced to a small fraction of their original size. The authors of a new report released by the United Nations Environment Programme (UNEP) at the 11th Stockholm Water Symposium on August 13, 2001, warn that the marshlands could completely disappear within the next 3-5 years unless dramatic steps are taken immediately to reverse the damage being done.The UNEP Executive Director described the wetlands' condition as 'a major environmental catastrophe that will be remembered as one of humanity's worst engineered disasters.' He noted that 'the tragic loss of this rare wetland has occurred in approximately the same period since world leaders pledged to safeguard the environment at the United Nations Conference on Environment and Development (the Earth Summit) held in Rio de Janeiro in 1992.' Regarded by historians as one of the cradles of civilization, the Mesopotamian Fertile Crescent has supported Marsh Arab society for millennia. But through the damming and siphoning off of waters from the Tigris and Euphrates Rivers, the countries of Iran, Iraq, Turkey, and Syria have decimated the ecosystem and, with it, a culture rooted in the dawn of human history (dating back to ancient Sumeria about 5,000 years ago). || ",
            "hits": 49
        },
        {
            "id": 2105,
            "url": "https://svs.gsfc.nasa.gov/2105/",
            "result_type": "Visualization",
            "release_date": "2001-04-19T12:00:00-04:00",
            "title": "Dramatic Evaporation of the Aral Sea",
            "description": "Disappearing Water: The Aral Sea Over Time (From 1973 to 2001) A time series is a powerful illustrative tool. Where in the case of Las Vegas we see the direct effects of people on the land, in the case of the Aral Sea, separating the countries of Kazakhstan and Uzbekistan, we see indirect, but no less dramatic effects on a different part of the world. The Aral Sea is actually not a sea at all. It is an immense lake, a body of fresh water, although that particular description of its contents might now be more a figure of speech than practical fact. In the last thirty years, more than sixty percent of the lake has disappeared. As you'll see in the visualization, the change over time is dramatic. In the 1970s, farmers and state offices opened significant diversions from the rivers supplying water to the lake, sending millions of gallons to irrigate cotton fields and rice paddies. So voluminous were these irrigation sluices that concentrations of salts and minerals began to rise in the shrinking body of water. That change in chemistry has led to staggering alterations in the lake's ecology, causing precipitous drops in the Aral's fish population. A secondary effect of this reduction in the Aral Sea's overall size is the rapid exposure of the lake bed. Powerful winds that blow across this part of Asia routinely pick up and deposit tens of thousands of tons of now exposed soil every year. This has not only contributed to significant reduction in breathable air quality for nearby residents, but also appreciably affected crop yields due to those heavily salt laden particles falling on arable land. In the following sequence of images, we see a series of Landsat scenes taken several years apart. As the years pass, we see the profound reduction in overall area covered by the Aral, and a commensurate increase in land area as the floor of the sea now lies exposed. || ",
            "hits": 123
        },
        {
            "id": 2117,
            "url": "https://svs.gsfc.nasa.gov/2117/",
            "result_type": "Visualization",
            "release_date": "2001-04-19T12:00:00-04:00",
            "title": "Dramatic Evaporation of the Aral Sea (With Dates)",
            "description": "Disappearing Water: The Aral Sea Over Time (From 1973 to 2001) A time series is a powerful illustrative tool. Where in the case of Las Vegas we see the direct effects of people on the land, in the case of the Aral Sea, separating the countries of Kazakhstan and Uzbekistan, we see indirect, but no less dramatic effects on a different part of the world. The Aral Sea is actually not a sea at all. It is an immense lake, a body of fresh water, although that particular description of its contents might now be more a figure of speech than practical fact. In the last thirty years, more than sixty percent of the lake has disappeared. As you'll see in the visualization, the change over time is dramatic. In the 1970s, farmers and state offices opened significant diversions from the rivers supplying water to the lake, sending millions of gallons to irrigate cotton fields and rice paddies. So voluminous were these irrigation sluices that concentrations of salts and minerals began to rise in the shrinking body of water. That change in chemistry has led to staggering alterations in the lake's ecology, causing precipitous drops in the Aral's fish population. A secondary effect of this reduction in the Aral Sea's overall size is the rapid exposure of the lake bed. Powerful winds that blow across this part of Asia routinely pick up and deposit tens of thousands of tons of now exposed soil every year. This has not only contributed to significant reduction in breathable air quality for nearby residents, but also appreciably affected crop yields due to those heavily salt laden particles falling on arable land. In the following sequence of images, we see a series of Landsat scenes taken several years apart. As the years pass, we see the profound reduction in overall area covered by the Aral, and a commensurate increase in land area as the floor of the sea now lies exposed. || ",
            "hits": 121
        },
        {
            "id": 2100,
            "url": "https://svs.gsfc.nasa.gov/2100/",
            "result_type": "Visualization",
            "release_date": "2001-04-09T12:00:00-04:00",
            "title": "Light Iceland Glacier Recession 1973 to 2000",
            "description": "This animation shows glacier recesion at the Breidamerkurjokull glacier in Iceland. The data from 1973 is taken from Landsat 1 and the 2000 data is from Landsat 7. The Breidamerkurjokull glacier in Iceland has been measured by Landsat to be receding since 1973. The glacierologists in Iceland and here at NASA's Goddard Space Flight Center have measured the recession throughout the entire glacier and found different rates of recession in different areas. In general, the glacier seems to be receding at about 2% annually.It is extremely controversial whether or not this recession is caused by global warming. || ",
            "hits": 8
        },
        {
            "id": 2101,
            "url": "https://svs.gsfc.nasa.gov/2101/",
            "result_type": "Visualization",
            "release_date": "2001-04-09T12:00:00-04:00",
            "title": "Iceland Glacier Recession 1973 to 2000, Glacier Terminus Contrast Emphasized",
            "description": "This animation shows glacier recesion at the Breidamerkurjokull glacier in Iceland. The data from 1973 is taken from Landsat 1 and the 2000 data is from Landsat 7. The Breidamerkurjokull glacier in Iceland has been measured by Landsat to be receding since 1973. The glacierologists in Iceland and here at NASA's Goddard Space Flight Center have measured the recession throughout the entire glacier and found different rates of recession in different areas. In general, the glacier seems to be receding at about 2% annually.It is extremely controversial whether or not this recession is caused by global warming. || ",
            "hits": 14
        },
        {
            "id": 2093,
            "url": "https://svs.gsfc.nasa.gov/2093/",
            "result_type": "Visualization",
            "release_date": "2001-04-05T12:00:00-04:00",
            "title": "Panda Habitat Deforestation: Highlighting Wolong Preserve",
            "description": "Zoom into China, highlighting the Wolong Preserve. || Animation highlighting the Wolong Preserve (China) || a002093.00350_print.png (720x480) [765.5 KB] || a002093_pre.jpg (320x242) [8.0 KB] || a002093.webmhd.webm (960x540) [2.7 MB] || a002093.dv (720x480) [47.5 MB] || a002093.mpg (352x240) [1.9 MB] || ",
            "hits": 20
        },
        {
            "id": 2094,
            "url": "https://svs.gsfc.nasa.gov/2094/",
            "result_type": "Visualization",
            "release_date": "2001-04-05T12:00:00-04:00",
            "title": "Panda Habitat Deforestation: Data",
            "description": "This animation uses a Landsat texture, USGS DEM data for elevation, and the Michigan State data for deforestation. Dissolve between 1965, 1974, and 1997 deforestation data sets. || ",
            "hits": 12
        },
        {
            "id": 2064,
            "url": "https://svs.gsfc.nasa.gov/2064/",
            "result_type": "Visualization",
            "release_date": "2001-02-26T12:00:00-05:00",
            "title": "Lake Chad Evaporation 1963 to 1997",
            "description": "Located on the edge of the Sahara and bordering four countries—Chad, Cameroon, Nigeria, and Niger—the immense area of this land locked lake has nearly disappeared in recent years. Persistent drought has caused the lake to drop from its former sixth place position in the list of world's largest lakes; it is now one tenth its former size.The basin of the lake is not naturally deep, so the surface area of the lake tended to spread out, keeping the total depth to little more 23 feet (7 meters). In recent years, rainfall patterns have begun to change, and tributaries to Lake Chad have not been refilling the basin as rapidly as they used to. The lush, productive flora and fauna fed by the wetlands of the shallow lake have suffered as a result.This has led to significant changes for various communities of people that live in the vicinity of the Lake. While for some the now exposed lake bed has enabled new land to be cultivated, much of the available fresh water that might have been used for irrigation is no longer dependable. As rainfall rates appear to be declining year after year, people living nearby develop even greater dependence on the lake, draining it even faster. || ",
            "hits": 44
        },
        {
            "id": 2065,
            "url": "https://svs.gsfc.nasa.gov/2065/",
            "result_type": "Visualization",
            "release_date": "2001-02-26T12:00:00-05:00",
            "title": "Lake Chad Evaporation 1973 to 1987",
            "description": "Located on the edge of the Sahara and bordering four countries—Chad, Cameroon, Nigeria, and Niger—the immense area of this land locked lake has nearly disappeared in recent years. Persistent drought has caused the lake to drop from its former sixth place position in the list of world's largest lakes; it is now one tenth its former size.The basin of the lake is not naturally deep, so the surface area of the lake tended to spread out, keeping the total depth to little more 23 feet (7 meters). In recent years, rainfall patterns have begun to change, and tributaries to Lake Chad have not been refilling the basin as rapidly as they used to. The lush, productive flora and fauna fed by the wetlands of the shallow lake have suffered as a result.This has led to significant changes for various communities of people that live in the vicinity of the Lake. While for some the now exposed lake bed has enabled new land to be cultivated, much of the available fresh water that might have been used for irrigation is no longer dependable. As rainfall rates appear to be declining year after year, people living nearby develop even greater dependence on the lake, draining it even faster. || ",
            "hits": 94
        },
        {
            "id": 23,
            "url": "https://svs.gsfc.nasa.gov/23/",
            "result_type": "Visualization",
            "release_date": "1994-01-14T12:00:00-05:00",
            "title": "Changes in Glacier Bay: Glacier Fly Up",
            "description": "Flying up Glacier Bays Muir Inlet, ending at the Muir Glacier || a000023.00005_web.png (720x480) [515.3 KB] || a000023_thm.png (80x40) [5.7 KB] || a000023_pre.jpg (320x238) [8.3 KB] || a000023_pre_searchweb.jpg (320x180) [60.0 KB] || a000023.webmhd.webm (960x540) [3.1 MB] || a000023.dv (720x480) [72.3 MB] || a000023.mp4 (640x480) [4.0 MB] || a000023.mpg (352x240) [2.5 MB] || ",
            "hits": 39
        },
        {
            "id": 24,
            "url": "https://svs.gsfc.nasa.gov/24/",
            "result_type": "Visualization",
            "release_date": "1994-01-14T12:00:00-05:00",
            "title": "Changes in Glacier Bay: Glacier Zoom In",
            "description": "Zooming in from a full image of Glacier Bay to a closeup of the Muir Glacier || a000024.00005_web.png (720x480) [698.7 KB] || a000024_thm.png (80x40) [7.1 KB] || a000024_pre.jpg (320x238) [15.0 KB] || a000024_pre_searchweb.jpg (320x180) [84.8 KB] || a000024.webmhd.webm (960x540) [3.6 MB] || a000024.dv (720x480) [54.0 MB] || a000024.mp4 (640x480) [3.1 MB] || a000024.mpg (352x240) [2.0 MB] || ",
            "hits": 29
        },
        {
            "id": 25,
            "url": "https://svs.gsfc.nasa.gov/25/",
            "result_type": "Visualization",
            "release_date": "1994-01-14T12:00:00-05:00",
            "title": "Changes in Glacier Bay: Muir Glacier",
            "description": "Changes in Glacier Bays Muir Glacier from 1973 to 1986 || a000025.00005_web.png (720x480) [553.5 KB] || a000025_thm.png (80x40) [6.0 KB] || a000025_pre.jpg (320x238) [10.6 KB] || a000025_pre_searchweb.jpg (320x180) [60.2 KB] || a000025.webmhd.webm (960x540) [3.6 MB] || a000025.dv (720x480) [122.0 MB] || a000025.mp4 (640x480) [6.9 MB] || a000025.mpg (352x240) [4.6 MB] || ",
            "hits": 50
        },
        {
            "id": 26,
            "url": "https://svs.gsfc.nasa.gov/26/",
            "result_type": "Visualization",
            "release_date": "1994-01-14T12:00:00-05:00",
            "title": "Changes in Glacier Bay: Riggs and McBride Glaciers",
            "description": "Changes in Glacier Bays Riggs and McBride Glaciers from 1973 to 1986 || a000026.00005_web.png (720x480) [425.4 KB] || a000026_thm.png (80x40) [5.5 KB] || a000026_pre.jpg (320x238) [11.1 KB] || a000026_pre_searchweb.jpg (320x180) [66.2 KB] || a000026.webmhd.webm (960x540) [3.5 MB] || a000026.dv (720x480) [123.5 MB] || a000026.mp4 (640x480) [7.0 MB] || a000026.mpg (352x240) [5.3 MB] || ",
            "hits": 38
        },
        {
            "id": 27,
            "url": "https://svs.gsfc.nasa.gov/27/",
            "result_type": "Visualization",
            "release_date": "1994-01-14T12:00:00-05:00",
            "title": "Changes in Glacier Bay: Casement Glacier",
            "description": "Changes in Glacier Bays Casement Glacier from 1973 to 1986 || a000027.00005_web.png (720x480) [607.8 KB] || a000027_thm.png (80x40) [5.7 KB] || a000027_pre.jpg (320x238) [10.3 KB] || a000027_pre_searchweb.jpg (320x180) [60.7 KB] || a000027.webmhd.webm (960x540) [2.3 MB] || a000027.dv (720x480) [79.0 MB] || a000027.mp4 (640x480) [4.4 MB] || a000027.mpg (352x240) [2.8 MB] || ",
            "hits": 40
        },
        {
            "id": 28,
            "url": "https://svs.gsfc.nasa.gov/28/",
            "result_type": "Visualization",
            "release_date": "1994-01-14T12:00:00-05:00",
            "title": "Changes in Glacier Bay: Brady Glacier",
            "description": "Changes in Glacier Bays Brady Glacier from 1973 to 1986 || a000028.00005_web.png (720x480) [654.2 KB] || a000028_thm.png (80x40) [5.9 KB] || a000028_pre.jpg (320x238) [11.0 KB] || a000028_pre_searchweb.jpg (320x180) [70.3 KB] || a000028.webmhd.webm (960x540) [2.6 MB] || a000028.dv (720x480) [68.7 MB] || a000028.mp4 (640x480) [3.9 MB] || a000028.mpg (352x240) [2.9 MB] || ",
            "hits": 35
        },
        {
            "id": 29,
            "url": "https://svs.gsfc.nasa.gov/29/",
            "result_type": "Visualization",
            "release_date": "1994-01-14T12:00:00-05:00",
            "title": "Changes in Glacier Bay: Reid and Lamplugh Glaciers",
            "description": "Changes in Glacier Bays Reid and Lamplugh Glaciers from 1973 to 1986 || a000029.00005_web.png (720x480) [704.3 KB] || a000029_thm.png (80x40) [6.2 KB] || a000029_pre.jpg (320x238) [11.2 KB] || a000029_pre_searchweb.jpg (320x180) [64.8 KB] || a000029.webmhd.webm (960x540) [2.6 MB] || a000029.dv (720x480) [79.0 MB] || a000029.mp4 (640x480) [4.5 MB] || a000029.mpg (352x240) [2.8 MB] || ",
            "hits": 35
        },
        {
            "id": 30,
            "url": "https://svs.gsfc.nasa.gov/30/",
            "result_type": "Visualization",
            "release_date": "1994-01-14T12:00:00-05:00",
            "title": "Changes in Glacier Bay: Margerie Glacier",
            "description": "Changes in Glacier Bays Margerie Glacier from 1973 to 1986 || a000030.00005_web.png (720x480) [423.5 KB] || a000030_thm.png (80x40) [6.4 KB] || a000030_pre.jpg (320x238) [12.6 KB] || a000030_pre_searchweb.jpg (320x180) [69.7 KB] || a000030.webmhd.webm (960x540) [5.0 MB] || a000030.dv (720x480) [140.6 MB] || a000030.mp4 (640x480) [8.0 MB] || a000030.mpg (352x240) [5.8 MB] || ",
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