1 00:00:00,010 --> 00:00:08,980 [ Sound effect ] 2 00:00:09,000 --> 00:00:11,880 [ Music ] 3 00:00:11,900 --> 00:00:17,230 My name is Lynn Carter. I'm a research space scientist, and I work with the Planetary Geodynamics group here at Goddard. 4 00:00:17,250 --> 00:00:22,230 I study the geology of planetary surfaces: the Earth, Moon, Mars, Venus. 5 00:00:22,250 --> 00:00:24,880 There's a lot of things you can learn about the Earth by studying other planets. 6 00:00:24,900 --> 00:00:28,100 For example on the Earth we have a lot of erosive processes. 7 00:00:28,120 --> 00:00:33,480 You know, it rains, it washes parts of the surface away, we have plate tectonics, which recycles the crust. 8 00:00:33,500 --> 00:00:36,230 But on other planets those processes don't necessarily occur. 9 00:00:36,250 --> 00:00:40,160 So, for example, when we look at the Moon we're seeing a surface that's much older. 10 00:00:40,180 --> 00:00:44,130 We can use impact cratering on the Moon, to sort of understand how many impacts happened, 11 00:00:44,150 --> 00:00:48,010 the size of the objects that were hitting each other in the in the early solar system. 12 00:00:48,030 --> 00:00:50,930 Generally what I would do every day is a variety of things. 13 00:00:50,950 --> 00:00:56,530 Like I might come in and do some image analysis, and then do some writing about our scientific results. 14 00:00:56,550 --> 00:00:59,100 Sometimes I do field work in Hawaii or Arizona. 15 00:00:59,120 --> 00:01:03,450 We take a ground-penetrating radar out and we learn more about lava flows on the Earth. 16 00:01:03,470 --> 00:01:06,180 One of my favorite things is to use radar remote sensing. 17 00:01:06,200 --> 00:01:10,650 For example, on Mars we can use radars to sound all the way to the bottom of Mars' polar caps 18 00:01:10,670 --> 00:01:13,450 and see all this layering within the polar caps. 19 00:01:13,470 --> 00:01:16,820 And on the Moon we're using it to study impact cratering. 20 00:01:16,840 --> 00:01:20,610 Sometimes when an impact crater is formed a huge sheet of melt is thrown out. 21 00:01:20,630 --> 00:01:26,120 This melted rock flows across the surface, but then over time it's covered over by stuff from other impacts. 22 00:01:26,140 --> 00:01:28,310 But with the radar it just blows right through all of that 23 00:01:28,330 --> 00:01:32,580 and you can see this beautiful image of the melt flow coming out of the crater. 24 00:01:32,600 --> 00:01:34,880 Looking ahead to the future there are so many different things that we could learn 25 00:01:34,900 --> 00:01:36,980 about planetary science that would be interesting. 26 00:01:37,000 --> 00:01:42,660 One of my favorites is Venus, actually, because it's about the same size and it's very close to the Earth in the solar system. 27 00:01:42,680 --> 00:01:46,780 And why has there been this divergent evolution between these two worlds that are very similar? 28 00:01:46,800 --> 00:01:49,750 And I think understanding that problem will be very interesting.