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