1 00:00:00,330 --> 00:00:04,560 In a remote area of northwest Greenland, [music rises] 2 00:00:04,560 --> 00:00:08,750 an international team of scientists has 3 00:00:08,750 --> 00:00:12,990 made a stunning discovery, buried beneath a kilometer 4 00:00:12,990 --> 00:00:17,180 of ice. It’s an impact crater … 5 00:00:17,180 --> 00:00:21,400 300 meters deep … 31 km wide 6 00:00:21,400 --> 00:00:25,690 … much bigger than Washington, D.C., 7 00:00:25,690 --> 00:00:29,890 even bigger than Paris, and it’s probably 8 00:00:29,890 --> 00:00:34,150 one of the youngest large impact craters on Earth. 9 00:00:34,150 --> 00:00:38,480 The relentless spread of the Greenland Ice Sheet has covered the crater, obscuring 10 00:00:38,480 --> 00:00:42,700 obscuring it from view for thousands if not hundreds of thousands of years. 11 00:00:42,700 --> 00:00:46,910 Even so, scientists say it was essentially hiding in plain sight. 12 00:00:46,910 --> 00:00:51,180 So what finally revealed its presence? 13 00:00:51,180 --> 00:00:55,420 It all started with a rock … a map … 14 00:00:55,420 --> 00:00:59,610 and a connection made by scientists at the Natural History Museum in Copenhagen. 15 00:00:59,610 --> 00:01:03,920 Each day, scientists there pass by a large 16 00:01:03,920 --> 00:01:08,120 iron meteorite found in Greenland decades ago. 17 00:01:08,120 --> 00:01:12,330 One day, they got a new map of the bedrock topography beneath the ice sheet, 18 00:01:12,330 --> 00:01:16,550 mostly based on ice-penetrating radar data collected 19 00:01:16,550 --> 00:01:20,750 onboard NASA’s P-3 aircraft over two decades. [Sound of aircraft engine] 20 00:01:20,750 --> 00:01:24,950 This map gets more refined all the time, yet there are still areas open 21 00:01:24,950 --> 00:01:29,180 to interpretation, including the conspicuously semicircular 22 00:01:29,180 --> 00:01:33,360 edge of the ice sheet, drained by the Hiawatha Glacier. 23 00:01:33,360 --> 00:01:37,550 There, the data showed a circular depression in the bedrock, 24 00:01:37,550 --> 00:01:41,770 near the region where that courtyard meteorite had been found. 25 00:01:41,770 --> 00:01:45,990 In May of 2016, the team sent the German research plane 26 00:01:45,990 --> 00:01:50,200 Polar 6 to fly over Hiawatha Glacier with a powerful new 27 00:01:50,200 --> 00:01:54,490 ice-penetrating radar. 28 00:01:54,490 --> 00:01:58,750 Radar waves can travel through the ice, measuring its thickness 29 00:01:58,750 --> 00:02:03,080 and internal structure. Studying data from this airborne survey, 30 00:02:03,080 --> 00:02:07,340 the scientists confirmed the telltale bowl shape and central peaks 31 00:02:07,340 --> 00:02:11,590 beneath Hiawatha Glacier. They also found that the oldest ice 32 00:02:11,590 --> 00:02:15,820 in this crater was actually fairly young, by Greenland standards, 33 00:02:15,820 --> 00:02:19,930 and had experienced a great disturbance in its flow toward the end 34 00:02:19,930 --> 00:02:24,230 of the last ice age. [Sound of hammer on rock] 35 00:02:24,230 --> 00:02:28,470 The team then visited the area on foot, and in sediments deposited by a river 36 00:02:28,470 --> 00:02:32,690 draining out of the glacier, they found grains of the mineral quartz that showed signs 37 00:02:32,690 --> 00:02:36,950 of being physically shocked in a massive impact. 38 00:02:36,950 --> 00:02:41,130 Models suggest, the asteroid was more than a kilometer wide. 39 00:02:41,130 --> 00:02:45,320 The Hiawatha crater is one of the 25 largest known 40 00:02:45,320 --> 00:02:49,950 impact craters on Earth, and the first found under any of 41 00:02:49,950 --> 00:02:54,260 our planet’s ice sheets.Crucially, the Hiawatha impact 42 00:02:54,260 --> 00:02:58,550 crater still looks like an impact crater, even though it’s covered by ice 43 00:02:58,550 --> 00:03:02,750 and seems to be rapidly eroding. The data as a whole 44 00:03:02,750 --> 00:03:07,030 suggests it’s quite young – geologically speaking 45 00:03:07,030 --> 00:03:11,320 But we don’t know exactly when an asteroid sped 46 00:03:11,320 --> 00:03:15,550 toward Earth, through the atmosphere, and into the 47 00:03:15,550 --> 00:03:19,840 planet’s crust in Northwest Greenland. [Sound of impact] 48 00:03:19,840 --> 00:03:24,080 It was likely less than 3 million years ago. 49 00:03:24,080 --> 00:03:28,320 But it might have been as recently as during the last ice age, 50 00:03:28,320 --> 00:03:33,370 12 to 115 thousand years ago. 51 00:03:33,370 --> 00:03:37,560 The impact could have also occurred when ice already covered Greenland 52 00:03:37,560 --> 00:03:41,780 and it would have instantly vaporized billions of tons of ice and re-routed 53 00:03:41,780 --> 00:03:45,990 the flow of ice and water into the ocean. 54 00:03:45,990 --> 00:03:50,250 Whenever the impact happened, life on Earth at the time would have been profoundly affected. 55 00:03:50,250 --> 00:03:54,750 An impact of this size is unlikely 56 00:03:54,750 --> 00:03:58,920 to happen again soon, but evidence that it might have happened 57 00:03:58,920 --> 00:04:03,000 not so long ago, in Earth’s history is essential to assessing the risk today. 58 00:04:03,000 --> 00:04:07,100 This is the first study of the Hiawatha 59 00:04:07,100 --> 00:04:11,220 impact crater, but it still holds many secrets waiting to be discovered. 60 00:04:11,220 --> 00:04:15,300 61 00:04:15,300 --> 00:04:19,320 62 00:04:19,320 --> 00:04:23,390 63 00:04:23,390 --> 00:04:27,440 64 00:04:27,440 --> 00:04:29,567 [music fades]