WEBVTT FILE 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]