1 00:00:00,020 --> 00:00:03,100 2 00:00:03,120 --> 00:00:06,290 3 00:00:06,310 --> 00:00:09,360 4 00:00:09,380 --> 00:00:12,390 5 00:00:12,410 --> 00:00:14,510 To me, Volcanism is important to study 6 00:00:14,530 --> 00:00:17,700 because it is one of the most common and fundamental geologic 7 00:00:17,720 --> 00:00:19,890 processes that occurs in our solar system. 8 00:00:19,910 --> 00:00:21,930 It's a window into 9 00:00:21,950 --> 00:00:24,110 the history of our own planet, 10 00:00:24,130 --> 00:00:25,120 of the moon, 11 00:00:25,140 --> 00:00:27,880 and the other planets and moons in our solar system. 12 00:00:27,900 --> 00:00:32,090 My name is Brent Garry, and I am a Geologist at NASA Goddard Space Flight Center. 13 00:00:32,110 --> 00:00:34,130 I specialize in planetary volcanology, 14 00:00:34,150 --> 00:00:38,270 so it's my job to study the evolution of volcanoes and lava flows 15 00:00:38,290 --> 00:00:42,410 in our solar system – primarily on the Earth, the Moon, and Mars. 16 00:00:42,430 --> 00:00:47,590 What we're trying to answer is: How did these volcanoes evolve over time? 17 00:00:47,610 --> 00:00:48,700 When did they erupt? 18 00:00:48,720 --> 00:00:52,810 And kind of, what went on during the eruption process itself? 19 00:00:52,830 --> 00:00:54,910 When we get images back 20 00:00:54,930 --> 00:00:59,960 from the moon of these long, meandering depressions, called Sinuous Rilles, 21 00:00:59,980 --> 00:01:04,010 that look like rivers here on Earth – you know, we want to understand: 22 00:01:04,030 --> 00:01:06,220 Are these the remnants of collapsed lava tubes? 23 00:01:06,240 --> 00:01:12,380 Did the lava carve its way into the surface of the moon to leave these giant channels? 24 00:01:12,400 --> 00:01:14,570 Or in the case of Mars, the debate is whether or not 25 00:01:14,590 --> 00:01:23,400 these were carved by water, or fluvial activity, or if they were carved by lava flows, or volcanic activity. 26 00:01:23,420 --> 00:01:25,550 One of the best ways to answer these questions is by 27 00:01:25,570 --> 00:01:29,590 comparing the information and data we get back from the Moon and Mars to 28 00:01:29,610 --> 00:01:31,750 geologic features that we have right here on Earth. 29 00:01:31,770 --> 00:01:35,900 One of the exciting parts of my job is I get to travel around the world. 30 00:01:35,920 --> 00:01:39,980 I get to go to New Mexico, Hawaii, even Iceland to do my research. 31 00:01:40,000 --> 00:01:43,160 I love this part of my job because I get to I hike up volcanoes all day, 32 00:01:43,180 --> 00:01:46,270 we're hiking around desolate, you know, fields of lava, 33 00:01:46,290 --> 00:01:49,450 we're taking helicopter rides over these flow fields, 34 00:01:49,470 --> 00:01:52,530 we're looking at active lava flows that are going on, 35 00:01:52,550 --> 00:01:56,760 and even collecting samples of these features to study. 36 00:01:56,780 --> 00:02:01,050 "Taadaa! Don't try this at home kids." 37 00:02:01,070 --> 00:02:04,260 Our field team uses a wide range of instruments to do our work. 38 00:02:04,280 --> 00:02:07,360 We use things like a Differential GPS, 39 00:02:07,380 --> 00:02:10,550 which gives us the topography of the lava flows. 40 00:02:10,570 --> 00:02:12,740 We use a Ground-penetrating radar, 41 00:02:12,760 --> 00:02:16,920 which allows us to see in the subsurface of the flow field. 42 00:02:16,940 --> 00:02:18,930 And we also use a thermal imaging camera 43 00:02:18,950 --> 00:02:23,430 which allows us to see the differences in temperature across an active lava flow. 44 00:02:23,450 --> 00:02:27,430 A lot of people might think that studying geology is just looking at boring rocks all day. 45 00:02:27,450 --> 00:02:31,780 But my job here at NASA proves that geology is an adventure. 46 00:02:31,800 --> 00:02:32,810 It takes you around the world 47 00:02:32,830 --> 00:02:36,840 and also to the surfaces of other planets and moons in our solar system. 48 00:02:36,860 --> 00:02:47,281