WEBVTT FILE 1 00:00:01.500 --> 00:00:06.090 In early 2015, Earth saw the birth of a new island 2 00:00:06.090 --> 00:00:09.370 ...the first of its explosive type in 53 years. 3 00:00:09.370 --> 00:00:09.500 4 00:00:09.500 --> 00:00:14.800 The blast was so large that nearby tourists caught the explosion on camera. 5 00:00:14.800 --> 00:00:18.210 The new island, unofficially known as Hunga Tonga - Hunga Ha'apai, 6 00:00:18.210 --> 00:00:20.870 is located in the remote South Pacific, 7 00:00:20.870 --> 00:00:24.060 nestled between two other islands in the Kingdom of Tonga. 8 00:00:24.060 --> 00:00:25.330 9 00:00:25.330 --> 00:00:29.690 It's the first island of its kind to erupt and persist in the modern satellite era, 10 00:00:29.690 --> 00:00:34.540 giving scientists an unprecedented view from space of its erosional evolution. 11 00:00:34.540 --> 00:00:37.050 12 00:00:37.050 --> 00:00:40.120 The event immediately caught the attention of Dr. Jim Garvin, 13 00:00:40.120 --> 00:00:46.020 Chief Scientist at NASA's Goddard Space Flight Center, geomorphologist, and Mars expert. 14 00:00:46.020 --> 00:00:47.690 15 00:00:47.690 --> 00:00:50.660 [Garvin] It should be a pile of basaltic anticidic rocks. 16 00:00:50.660 --> 00:00:54.800 That’s what you expect in this kind of setting...but there’s more. 17 00:00:54.800 --> 00:00:55.120 18 00:00:55.120 --> 00:01:00.350 [narrator] What does a Mars expert see in the island that the rest of us don't? 19 00:01:00.350 --> 00:01:05.770 [Garvin] I think these small islands, small volcanic islands, freshly made, evolving rapidly 20 00:01:05.770 --> 00:01:11.400 are windows into the role of surface waters on Mars as they have effected 21 00:01:11.400 --> 00:01:14.860 small land forms like volcanoes. And we see fields of them on Mars! 22 00:01:14.860 --> 00:01:18.720 23 00:01:18.720 --> 00:01:22.660 [narrator] The island dramatically changed shape and size every day for the first few months 24 00:01:22.660 --> 00:01:26.250 About six months in, it finally stabilized. 25 00:01:26.250 --> 00:01:26.960 26 00:01:26.960 --> 00:01:30.450 [Garvin] We watched this island change. And it got more and more exciting. 27 00:01:30.450 --> 00:01:36.680 It didn’t wash away. While there was massive erosion, there was redeposition, protecting the island. 28 00:01:36.680 --> 00:01:38.690 29 00:01:38.690 --> 00:01:44.170 Similar processes seen on Earth may have been at work two or three billion years ago 30 00:01:44.170 --> 00:01:48.360 on Mars - persistent surface waters that may have fashioned 31 00:01:48.360 --> 00:01:51.770 the Martian terrain that is evident there today. 32 00:01:51.770 --> 00:01:52.960 33 00:01:52.960 --> 00:01:56.900 [narrator] The truth is the two systems are actually cosmically related 34 00:01:56.900 --> 00:01:59.960 Our understanding of landforms on distant planets 35 00:01:59.960 --> 00:02:04.970 is directly informed by studying the evolution of similar features on Earth. 36 00:02:04.970 --> 00:02:05.960 37 00:02:05.960 --> 00:02:10.460 [Garvin] Earth is a magical place because, really, it’s our point of departure for everything 38 00:02:10.460 --> 00:02:14.010 And we come to realize in the last hundred years or so 39 00:02:14.010 --> 00:02:18.480 that it’s a far more dynamic world than we ever thought. 40 00:02:18.480 --> 00:02:28.979