WEBVTT FILE 1 00:00:00.530 --> 00:00:04.060 In 2015, Earth saw the birth of a new island, 2 00:00:04.080 --> 00:00:07.170 the first of its explosive type in 53 years. 3 00:00:07.190 --> 00:00:12.020 The blast was so large that nearby tourists caught the explosion on camera. 4 00:00:12.040 --> 00:00:17.630 Despite raging volcanic activity above and below the Earth’s crust, an event like this is pretty rare. 5 00:00:17.650 --> 00:00:20.940 Which is why it immediately caught the attention of Dr. Jim Garvin - 6 00:00:20.960 --> 00:00:24.800 Chief Scientist at NASA's Goddard Space Flight Center and Mars expert. 7 00:00:24.820 --> 00:00:27.500 It should be a pile of basaltic andesite rocks. 8 00:00:27.520 --> 00:00:30.310 That’s what you expect in this kind of setting 9 00:00:30.330 --> 00:00:32.210 But there’s more. 10 00:00:32.230 --> 00:00:36.310 What answers does a Mars expert see in the island that the rest of don’t? 11 00:00:36.330 --> 00:00:40.360 12 00:00:40.380 --> 00:00:44.340 The new island unofficially known as Hunga Tonga-Hunga Ha'apai 13 00:00:44.360 --> 00:00:46.760 is located in the remote Southwest Pacific, 14 00:00:46.780 --> 00:00:49.940 nestled between two other islands in Kingdom of Tonga. 15 00:00:49.960 --> 00:00:54.310 It’s the first island of its kind to erupt and persist in the modern satellite era, 16 00:00:54.330 --> 00:00:59.250 giving scientists an unprecedented view from space of its evolution. 17 00:00:59.270 --> 00:01:02.290 There are other islands being formed including one’s near Japan. 18 00:01:02.310 --> 00:01:04.430 Very nice, lava eruptions, classic. 19 00:01:04.450 --> 00:01:09.710 But this one was special because there was this explosive element that reminded us at first glance 20 00:01:09.730 --> 00:01:13.040 – not exactly – of the kind of eruption at Surtsey. 21 00:01:13.060 --> 00:01:15.660 This is the eruption Jim is talking about 22 00:01:15.680 --> 00:01:20.960 – an island born from a similar explosive eruption in 1963 and one of only 23 00:01:20.980 --> 00:01:25.230 three volcanic islands that have survived in the past 150 years. 24 00:01:25.250 --> 00:01:25.620 25 00:01:25.640 --> 00:01:31.490 Very early in Jim's career, Surtsey was the first newly-formed oceanic island he ever studied. 26 00:01:31.510 --> 00:01:34.260 27 00:01:34.280 --> 00:01:37.000 Years later, he went on to become NASA’s Chief Scientist 28 00:01:37.020 --> 00:01:42.210 pushing the agency’s priorities towards Mars exploration that eventually led to the creation of 29 00:01:42.230 --> 00:01:45.750 the Mars Exploration Rovers, the Mars Reconnaissance Orbiter 30 00:01:45.770 --> 00:01:48.090 and the Mars Science Laboratory. 31 00:01:48.110 --> 00:01:53.920 So why is a scientist clearly fixated on Mars intrigued by new land on Earth? 32 00:01:53.940 --> 00:01:58.250 The truth is, the two systems are actually cosmically related. 33 00:01:58.270 --> 00:02:01.390 I think these small islands, small volcanic islands, 34 00:02:01.410 --> 00:02:08.040 freshly made, evolving rapidly, are windows into the role of surface waters on Mars 35 00:02:08.060 --> 00:02:10.980 as they have effected small land forms like volcanoes. 36 00:02:11.000 --> 00:02:12.750 And we see fields of them on Mars! 37 00:02:12.770 --> 00:02:14.380 There’s a lot to unpack there, 38 00:02:14.400 --> 00:02:17.760 but before you can understand the major significance of this on Mars, 39 00:02:17.780 --> 00:02:20.720 you have to understand why it’s a big deal on Earth. 40 00:02:20.740 --> 00:02:22.350 41 00:02:22.370 --> 00:02:28.970 It really felt like we were witnessing something that nobody else had seen. 42 00:02:28.990 --> 00:02:30.940 That’s the voice Dr. Vicki Ferrini 43 00:02:30.960 --> 00:02:36.740 – one of the first pairs of eyes to see the new island from the deck of her research vessel. 44 00:02:36.760 --> 00:02:41.500 It’s this crazy, huge land mass that’s sticking up out of the water 45 00:02:41.520 --> 00:02:44.840 where we know there wasn’t one before. 46 00:02:44.860 --> 00:02:47.090 We watched this island change. 47 00:02:47.110 --> 00:02:50.480 And it got more and more exciting. It didn’t wash away. 48 00:02:50.500 --> 00:02:55.650 While there was massive erosion, there was redeposition protecting the island. 49 00:02:55.670 --> 00:02:58.740 The initial mass above sea level was eroding very quickly 50 00:02:58.760 --> 00:03:02.010 over the first three to six months and then it leveled off. 51 00:03:02.030 --> 00:03:03.310 So you kind of see a curve – 52 00:03:03.330 --> 00:03:09.000 a logarithmic fall off in change in that mass above sea level. 53 00:03:09.020 --> 00:03:12.770 Basically, the island dramatically changed shape and size every day 54 00:03:12.790 --> 00:03:14.360 for the first few months. 55 00:03:14.380 --> 00:03:18.960 About six months in, it finally stabilized. 56 00:03:18.980 --> 00:03:22.430 Vicki’s initial measurements and observations were crucial, 57 00:03:22.450 --> 00:03:27.860 but their research ship couldn’t get close to the island without risking a collision. 58 00:03:27.880 --> 00:03:31.290 Two French explorers who were sailing past the islands on their worldwide 59 00:03:31.310 --> 00:03:34.940 voyage became NASA’s eyes and ears, collecting some of the very first 60 00:03:34.960 --> 00:03:37.950 images and samples of the interior island. 61 00:03:37.970 --> 00:03:38.930 62 00:03:38.950 --> 00:03:41.120 This is the Earth at its best. 63 00:03:41.140 --> 00:03:45.300 Because new land, new life, new landscapes 64 00:03:45.320 --> 00:03:46.900 and new patterns. 65 00:03:46.920 --> 00:03:49.110 How do they all work together? 66 00:03:49.130 --> 00:03:51.250 67 00:03:51.270 --> 00:03:55.250 The combined observations, satellite images, samples 68 00:03:55.270 --> 00:03:58.030 and three-dimensional topographical maps lead Jim and the team 69 00:03:58.050 --> 00:04:00.930 to make some pretty stunning preliminary conclusions 70 00:04:00.950 --> 00:04:03.020 Scientists think that, in this case, 71 00:04:03.040 --> 00:04:06.570 warmed seawater interacted with ash after the eruption, 72 00:04:06.590 --> 00:04:10.370 chemically altering the fragile rock into a tougher material. 73 00:04:10.390 --> 00:04:16.330 But studying the life and death of land on Earth also has much broader implications. 74 00:04:16.350 --> 00:04:19.440 This island may give us insights into if – 75 00:04:19.460 --> 00:04:23.830 and how – life formed on Mars in its early history. 76 00:04:23.850 --> 00:04:25.960 Islands like this might have worked on Mars. 77 00:04:25.980 --> 00:04:30.980 Two or three billion years ago, lakes and small seas, filling depressions, 78 00:04:31.000 --> 00:04:35.620 persistent surface waters – the stuff we really strive to understand 79 00:04:35.640 --> 00:04:41.020 because it could have produced the conditions necessary for microbial life – or not! 80 00:04:41.040 --> 00:04:43.970 While the verdict is still out on whether or not liquid water 81 00:04:43.990 --> 00:04:46.150 on the surface of Mars may have produced life, 82 00:04:46.170 --> 00:04:51.060 scientists are currently running detailed chemical analysis of the island rock samples 83 00:04:51.080 --> 00:04:54.640 that will hopefully provide more answers in the months to come. 84 00:04:54.660 --> 00:04:57.150 Earth is a magical place because, really, 85 00:04:57.170 --> 00:04:59.360 it’s our point of departure for everything. 86 00:04:59.380 --> 00:05:02.610 And we come to realize in the last hundred years or so 87 00:05:02.630 --> 00:05:06.770 that it’s a far more dynamic world than we ever thought. 88 00:05:06.790 --> 00:05:08.120 Which begs the question, 89 00:05:08.140 --> 00:05:11.670 what new secrets will this planet we think we understand so well 90 00:05:11.690 --> 00:05:13.950 reveal in the next 100 years? 91 00:05:13.970 --> 00:05:27.574