1 00:00:12,170 --> 00:00:04,040 Music 2 00:00:12,190 --> 00:00:16,240 Andy: ...deposits left behind. This entire area, thousands of years ago, 3 00:00:16,260 --> 00:00:20,300 during the last ice age was covered by thick glaciers. Every year one of the 4 00:00:20,320 --> 00:00:24,350 major components of the Lunar and Planetary Science Academy internship 5 00:00:24,370 --> 00:00:28,390 program is a field study to an analog site, a planetary analog 6 00:00:28,410 --> 00:00:32,410 site. So this year we selected the Channeled Scablands of eastern 7 00:00:32,430 --> 00:00:36,420 Washington state. The topographic features 8 00:00:36,440 --> 00:00:40,480 and the geomorphological features here are similar to a lot of things that we're seeing on Mars 9 00:00:40,500 --> 00:00:44,560 we're seeing huge river valleys cut by massive floods of water 10 00:00:44,580 --> 00:00:48,630 And we also see columnar jointed basalts, which is something 11 00:00:48,650 --> 00:00:52,670 that was recently discovered on Mars with the HiRISE aerial camera on 12 00:00:52,690 --> 00:00:56,730 the Mars Reconnaissance Orbiter. To look at these basalts, we took 13 00:00:56,750 --> 00:01:00,760 hand measurements. We measured their widths and a few other features to make 14 00:01:00,780 --> 00:01:04,790 inferences about their cooling history, and then we took aerial 15 00:01:04,810 --> 00:01:08,820 photographs using an RC plane, provided by a program called 16 00:01:08,840 --> 00:01:12,850 R-Step, and a hexacopter, which is a six-propellered helicopter 17 00:01:12,870 --> 00:01:16,900 and our goal was to achieve the same resolution in these photos as we're seeing 18 00:01:16,920 --> 00:01:20,940 in the HiRISE images of the Martian columnar basalts. 19 00:01:20,960 --> 00:01:25,020 It's really convenient when we can find somewhere on Earth that's similar to something 20 00:01:25,040 --> 00:01:29,100 we're seeing on another planet because it's a whole heck of a lot cheaper to study here than to 21 00:01:29,120 --> 00:01:33,160 study there. So we learn what's going on here and then we can sort of extrapolate our findings