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These are the user uploaded subtitles that are being translated: 1 00:00:01,240 --> 00:00:03,770 Mars. 2 00:00:03,776 --> 00:00:07,476 The red planet. 3 00:00:07,480 --> 00:00:12,418 Many scientists believe that the first person 4 00:00:12,418 --> 00:00:14,618 to set foot on its surface is alive today. 5 00:00:14,620 --> 00:00:18,990 Perhaps it's you. 6 00:00:18,991 --> 00:00:21,760 If it is you, then welcome to your ultimate travel guide. 7 00:00:21,760 --> 00:00:25,960 Using real images and data, 8 00:00:25,965 --> 00:00:27,995 we will take you to some of the most jaw-dropping landscapes 9 00:00:28,000 --> 00:00:30,500 discovered in our solar system 10 00:00:30,503 --> 00:00:33,733 right here on Mars. 11 00:00:33,739 --> 00:00:35,439 We don't have anything like this on earth. 12 00:00:35,441 --> 00:00:38,010 Places that may change 13 00:00:38,010 --> 00:00:39,840 the way you think about our own world... 14 00:00:41,680 --> 00:00:44,580 Is there life beyond the earth? 15 00:00:44,583 --> 00:00:47,013 This is probably one of the most profound questions 16 00:00:47,019 --> 00:00:49,519 that's ever been asked by the human mind. 17 00:00:49,522 --> 00:00:50,789 ...on a journey that will test the endurance 18 00:00:50,789 --> 00:00:52,919 of any traveler. 19 00:00:52,925 --> 00:00:56,195 Traveling to Mars is not for the faint of heart. 20 00:00:56,195 --> 00:01:00,495 At the dawn of the next golden age of exploration, 21 00:01:00,499 --> 00:01:01,567 here's your quintessential guide to the martian frontier. 22 00:01:01,567 --> 00:01:04,367 Oh, it's beautiful. 23 00:01:08,340 --> 00:01:09,909 Have you ever dreamed about traveling out of this world? 24 00:01:09,909 --> 00:01:12,539 My name is Mike Massimino, 25 00:01:12,545 --> 00:01:15,675 and I turned that fantasy into a reality 26 00:01:15,681 --> 00:01:18,611 when I space-walked to repair the Hubble space telescope. 27 00:01:18,617 --> 00:01:21,717 Great job, Mike. 28 00:01:21,720 --> 00:01:24,189 Now as we expand our knowledge of our solar system 29 00:01:24,189 --> 00:01:26,559 from Mercury to the cosmic unknowns, 30 00:01:28,527 --> 00:01:31,527 I want to take you on a personal journey to... 31 00:01:31,530 --> 00:01:34,600 -- Captions by vitac -- www.Vitac.Com 32 00:01:34,600 --> 00:01:36,400 captions paid for by discovery communications 33 00:01:36,402 --> 00:01:37,902 welcome to "the planets." 34 00:01:37,903 --> 00:01:40,072 I'm Mike Massimino. 35 00:01:40,072 --> 00:01:42,772 Ever since my space missions, 36 00:01:42,775 --> 00:01:44,075 I've thought about which planet in the solar system 37 00:01:44,076 --> 00:01:47,313 I'd like to visit. 38 00:01:47,313 --> 00:01:50,513 Hands down, it's Mars. 39 00:01:50,516 --> 00:01:52,016 So far, humans have only touched down on our moon, 40 00:01:52,017 --> 00:01:55,587 but that could change. 41 00:01:55,588 --> 00:01:57,256 NASA is planning on sending its first astronaut to Mars 42 00:01:57,256 --> 00:01:58,624 as soon as 2030, 43 00:01:58,624 --> 00:02:01,994 but there's a whole lot more 44 00:02:01,994 --> 00:02:05,264 we need to find out about our neighbor before we visit. 45 00:02:06,799 --> 00:02:10,836 The red glow of Mars 46 00:02:10,836 --> 00:02:13,066 is a constant feature in our night sky. 47 00:02:13,072 --> 00:02:17,172 But it's only when viewed up close 48 00:02:17,176 --> 00:02:19,906 that this rusty planet begins to reveal its secrets. 49 00:02:19,912 --> 00:02:22,542 It promises to wow any visitor 50 00:02:22,548 --> 00:02:26,548 who just traveled the seven months it would take 51 00:02:26,552 --> 00:02:29,052 to get there from the earth by spaceship. 52 00:02:29,054 --> 00:02:32,491 Other than our home planet, 53 00:02:32,491 --> 00:02:36,261 there is no world we know in such detail. 54 00:02:36,261 --> 00:02:40,061 That's thanks to the numerous satellites and rovers 55 00:02:40,065 --> 00:02:42,465 we've sent there over the past 50 years. 56 00:02:42,468 --> 00:02:45,537 And the landscapes they have looked down upon 57 00:02:45,537 --> 00:02:48,674 tell astonishing stories. 58 00:02:48,674 --> 00:02:54,244 Vast plains riddled with hundreds of thousands 59 00:02:54,246 --> 00:02:58,246 of craters, deep canyons, and strange rock formations, 60 00:02:58,250 --> 00:03:01,180 and views not seen anywhere on earth. 61 00:03:01,186 --> 00:03:06,925 We've photographed every corner of the planet, 62 00:03:06,925 --> 00:03:09,055 and plans are now under way to send the first humans to Mars. 63 00:03:09,061 --> 00:03:11,661 But what does it take to get there? 64 00:03:11,664 --> 00:03:15,294 How can we survive on the surface? 65 00:03:15,300 --> 00:03:17,000 And where are the best places to explore? 66 00:03:17,002 --> 00:03:22,072 For those ready for adventure, 67 00:03:22,074 --> 00:03:23,904 the best place to start is a well-known martian landmark -- 68 00:03:23,909 --> 00:03:26,178 Gale crater, 69 00:03:26,178 --> 00:03:31,248 a vast scar on the planet 70 00:03:31,250 --> 00:03:35,120 and home to NASA's flagship rover, curiosity, since 2012. 71 00:03:40,959 --> 00:03:44,929 The crater itself dwarfs any similar features here on earth. 72 00:03:44,930 --> 00:03:46,630 Every day, curiosity sends back detailed images 73 00:03:46,632 --> 00:03:49,432 from within the crater. 74 00:03:49,435 --> 00:03:52,035 This is one of them. 75 00:03:52,037 --> 00:03:56,207 And here, at the data science institute, 76 00:03:56,208 --> 00:03:58,177 professor Sanjeev Gupta is part of the team studying them. 77 00:03:58,177 --> 00:04:01,177 This is the crater rim over here. 78 00:04:01,180 --> 00:04:03,210 This is 150 kilometers in diameter. 79 00:04:03,215 --> 00:04:05,115 It's a really big feature. 80 00:04:05,117 --> 00:04:07,686 And there, in this view over here, 81 00:04:07,686 --> 00:04:10,355 what we can see is mount sharp. 82 00:04:10,355 --> 00:04:13,692 That's 5 kilometers high. 83 00:04:13,692 --> 00:04:15,592 That sits in the center of the crater, so it's really amazing 84 00:04:15,594 --> 00:04:18,694 'cause you really get a sense of this mountain 85 00:04:18,697 --> 00:04:21,734 that's sort of towering high above us. 86 00:04:21,734 --> 00:04:24,834 That's a mountain over 93 miles across 87 00:04:24,837 --> 00:04:30,807 and over 3 miles high. 88 00:04:30,809 --> 00:04:34,509 But professor Gupta isn't simply enjoying the view. 89 00:04:34,513 --> 00:04:38,413 Today, we know Mars as a dry, desolate world, 90 00:04:38,417 --> 00:04:41,954 but some images suggest that wasn't always the case. 91 00:04:41,954 --> 00:04:44,354 Gale crater was chosen as the landing site for curiosity 92 00:04:44,356 --> 00:04:46,956 after a very lengthy selection process. 93 00:04:46,959 --> 00:04:49,889 Orbiters had discovered evidence 94 00:04:49,895 --> 00:04:52,595 that the rocks at the base of mount sharp -- 95 00:04:52,598 --> 00:04:55,998 so, the rocks that we can see over here -- 96 00:04:56,001 --> 00:05:00,571 had evidence for hydration. 97 00:05:03,475 --> 00:05:05,444 Long before curiosity left earth, 98 00:05:05,444 --> 00:05:10,382 satellite images like this 99 00:05:10,382 --> 00:05:12,151 hinted there was more to this crater than meets the eye. 100 00:05:12,151 --> 00:05:14,381 And what's beautiful in this image 101 00:05:14,386 --> 00:05:16,655 is that you can see these canyons or valleys 102 00:05:16,655 --> 00:05:18,355 carved into the crater rim, 103 00:05:18,357 --> 00:05:22,494 and this is really suggestive 104 00:05:22,494 --> 00:05:24,694 that water flowed down the crater rim 105 00:05:24,696 --> 00:05:28,396 and eroded these canyons. 106 00:05:28,400 --> 00:05:30,369 Secondly, we can see all these beautiful layers here 107 00:05:30,369 --> 00:05:33,639 that form the base of mount sharp. 108 00:05:33,639 --> 00:05:37,176 These layers are enriched in hydrated minerals. 109 00:05:37,176 --> 00:05:39,144 So, those are minerals that contain water. 110 00:05:39,144 --> 00:05:42,781 Curiosity's mission? 111 00:05:42,781 --> 00:05:45,050 To follow the elusive trail of water on Mars. 112 00:05:45,050 --> 00:05:48,120 So, essentially, the orbital images 113 00:05:48,120 --> 00:05:50,550 provide us clues on where to go, 114 00:05:50,556 --> 00:05:54,793 but we really need to be on the ground, 115 00:05:54,793 --> 00:05:56,862 looking carefully at these rocks from a few meters away, 116 00:05:56,862 --> 00:05:59,531 and that's why we send rovers to Mars. 117 00:06:01,466 --> 00:06:04,503 Once the rover touched down, 118 00:06:04,503 --> 00:06:06,333 it quickly began picking up more clues. 119 00:06:06,338 --> 00:06:09,368 These are actually pebbles 120 00:06:09,374 --> 00:06:12,274 that are a few centimeters in diameter. 121 00:06:12,277 --> 00:06:15,377 What you can see when you look at the pebble outlines 122 00:06:15,380 --> 00:06:17,510 is that they have rounded shapes. 123 00:06:17,516 --> 00:06:19,716 So they've been, basically, rounded 124 00:06:19,718 --> 00:06:20,886 during a transport process. 125 00:06:20,886 --> 00:06:24,323 And they're too large 126 00:06:24,323 --> 00:06:28,023 to be moved and rounded by wind processes, 127 00:06:28,026 --> 00:06:30,756 and so the only way we can actually get this rounding 128 00:06:30,762 --> 00:06:32,362 is by water flow. 129 00:06:32,364 --> 00:06:35,094 I think it's irrefutable 130 00:06:35,100 --> 00:06:37,400 that there was once water flowing at the surface on Mars, 131 00:06:37,402 --> 00:06:39,732 based on the geological evidence. 132 00:06:39,738 --> 00:06:44,476 But even with its smooth surface, 133 00:06:44,476 --> 00:06:49,514 Gale crater wouldn't be the best landing site on Mars. 134 00:06:49,514 --> 00:06:54,152 So the question remains, where should you first touch down? 135 00:06:57,189 --> 00:07:01,426 This canyon is Valles Marineris, 136 00:07:01,426 --> 00:07:05,326 named after the mariner 9, the NASA mission that discovered it. 137 00:07:05,330 --> 00:07:10,068 The scale of the canyon is breathtaking. 138 00:07:10,068 --> 00:07:14,568 It is like the Grand Canyon on earth, but supersized. 139 00:07:14,573 --> 00:07:16,673 In places, its walls plunge 6 miles down, 140 00:07:16,675 --> 00:07:19,805 a unique geological formation 141 00:07:19,811 --> 00:07:23,911 not matched anywhere else on the planet. 142 00:07:23,916 --> 00:07:27,986 And it's thanks to this geology that this vast canyon system 143 00:07:27,986 --> 00:07:30,055 makes the ideal landing site for martian explorers. 144 00:07:35,027 --> 00:07:37,957 Astrogeologist Dr. Jim rice is confident in this conclusion. 145 00:07:37,963 --> 00:07:43,333 He's been involved in selecting Mars landing sites 146 00:07:43,335 --> 00:07:47,735 for every NASA mission since Mars pathfinder in 1994. 147 00:07:47,739 --> 00:07:50,369 You want something fairly flat, not too rocky, not too dusty. 148 00:07:50,375 --> 00:07:52,405 And because we use parachutes to help slow us down 149 00:07:52,411 --> 00:07:55,341 in the entry to the martian atmosphere, 150 00:07:55,347 --> 00:07:58,377 we're gonna be lower in elevation. 151 00:07:58,383 --> 00:08:00,152 And the views while landing would be jaw-dropping. 152 00:08:00,152 --> 00:08:02,621 Valles Marineris is a great spot 153 00:08:02,621 --> 00:08:04,121 because it's basically kind of like the Grand Canyon here. 154 00:08:04,122 --> 00:08:06,922 It's like someone has taken -- 155 00:08:06,925 --> 00:08:08,894 a giant surgeon with a scalpel making an incision 156 00:08:08,894 --> 00:08:10,824 and opened up the crust of the planet, 157 00:08:10,829 --> 00:08:13,966 allowing you to see deeper down, 158 00:08:13,966 --> 00:08:16,335 and deeper down in geology is further back in history. 159 00:08:16,335 --> 00:08:18,804 It's this view inside the planet 160 00:08:18,804 --> 00:08:21,504 that is the big draw for Dr. rice, 161 00:08:21,506 --> 00:08:23,336 but for most of us, the epic scale alone 162 00:08:23,342 --> 00:08:26,842 would be enticing enough. 163 00:08:26,845 --> 00:08:28,445 Now, that canyon is 10 times longer 164 00:08:28,447 --> 00:08:32,947 than the Grand Canyon here, 165 00:08:32,951 --> 00:08:34,820 it's four times deeper, and about 12 times wider. 166 00:08:34,820 --> 00:08:36,788 Another way to think about it is, 167 00:08:36,788 --> 00:08:40,425 the vast expanse of this canyon system, 168 00:08:40,425 --> 00:08:42,725 the length of it would be from New York City to Los Angeles. 169 00:08:42,728 --> 00:08:46,828 So that truly is the grand canyon of the solar system. 170 00:08:49,701 --> 00:08:51,570 Valles Marineris would provide the ultimate draw 171 00:08:51,570 --> 00:08:54,670 for any martian visitor. 172 00:08:54,673 --> 00:08:58,873 But it's not just the views that are attractive. 173 00:09:02,014 --> 00:09:04,383 Touching down inside Valles Marineris 174 00:09:04,383 --> 00:09:07,352 could help answer long-held questions 175 00:09:07,352 --> 00:09:09,882 about the chasm's formation. 176 00:09:09,888 --> 00:09:12,758 Images like this, taken from orbit, 177 00:09:12,758 --> 00:09:16,058 give us some clues to its history. 178 00:09:16,061 --> 00:09:17,729 Once theory is that ancient volcanoes 179 00:09:17,729 --> 00:09:22,868 ripped apart the surface, 180 00:09:22,868 --> 00:09:28,707 creating a rift that running water continued to carve. 181 00:09:28,707 --> 00:09:30,437 But only by landing there can we gather the conclusive proof. 182 00:09:30,442 --> 00:09:32,942 What you want to do as a geologist 183 00:09:32,944 --> 00:09:35,474 is get to outcrop like we see right here, 184 00:09:35,480 --> 00:09:39,650 a slab of rock you can get up and interrogate 185 00:09:39,651 --> 00:09:42,281 and kind of taste, so to speak, with your instruments. 186 00:09:42,287 --> 00:09:43,655 If you're a martian coming to earth, you'd probably come here, 187 00:09:43,655 --> 00:09:44,985 because you'd get a good idea 188 00:09:44,990 --> 00:09:47,259 of the geologic history of the earth 189 00:09:47,259 --> 00:09:49,127 from the rim all the way down to the floor. 190 00:09:49,127 --> 00:09:51,296 You know, most of these rocks 191 00:09:51,296 --> 00:09:52,664 record oceans that came and went, 192 00:09:52,664 --> 00:09:53,932 mountain chains that came and went, 193 00:09:53,932 --> 00:09:55,832 deserts that came and went. 194 00:09:55,834 --> 00:09:59,034 You know, on Mars, I think it'd be safe to say 195 00:09:59,037 --> 00:10:01,106 you'd go back 3, 3 1/2, maybe even 4 billion years 196 00:10:01,106 --> 00:10:04,443 at the floor of the canyon down there. 197 00:10:04,443 --> 00:10:07,973 I'd go in a heartbeat. 198 00:10:07,979 --> 00:10:11,716 Would you take the chance to travel to Mars? 199 00:10:11,716 --> 00:10:14,116 Visiting the red planet is not just about sightseeing. 200 00:10:14,119 --> 00:10:18,559 Once you get there, you'll have to survive 201 00:10:20,051 --> 00:10:23,321 some of the harshest conditions in the entire solar system. 202 00:10:25,356 --> 00:10:28,056 Years of hard work and planning 203 00:10:28,059 --> 00:10:31,759 went into my missions to the Hubble space telescope, 204 00:10:31,763 --> 00:10:33,793 but preparing to go to Mars is a whole other story. 205 00:10:33,798 --> 00:10:37,335 There'll be ice-cold temperatures 206 00:10:37,335 --> 00:10:39,035 and solar radiation coming at you from every angle. 207 00:10:39,037 --> 00:10:41,937 So to meet these challenges, 208 00:10:41,940 --> 00:10:43,940 scientists are coming up with some useful new tools 209 00:10:43,942 --> 00:10:46,242 to help us survive. 210 00:10:48,913 --> 00:10:53,913 Mars is a barren world, 211 00:10:53,918 --> 00:10:55,718 with its water and atmosphere long lost to the hands of time. 212 00:10:55,720 --> 00:10:59,590 For human space travelers, 213 00:10:59,591 --> 00:11:01,321 it would be an absolutely inhospitable environment. 214 00:11:01,326 --> 00:11:04,356 That is why researchers 215 00:11:04,362 --> 00:11:08,032 have descended upon the volcanoes of Hawaii, 216 00:11:08,032 --> 00:11:11,632 an environment on earth that closely matches Mars 217 00:11:11,636 --> 00:11:14,405 in terms of landscape, at least. 218 00:11:14,405 --> 00:11:17,105 They're trying to figure out how we can survive 219 00:11:17,108 --> 00:11:19,177 on the desolate and hostile planet. 220 00:11:22,213 --> 00:11:26,483 Michael lye and his team have designed a space suit 221 00:11:26,484 --> 00:11:30,254 to simulate Mars missions here on Hawaii. 222 00:11:30,254 --> 00:11:32,724 Once you land on Mars, you're basically living in a vacuum. 223 00:11:32,724 --> 00:11:34,754 It's got an atmosphere, but not much. 224 00:11:34,759 --> 00:11:37,259 And while you're there, 225 00:11:37,261 --> 00:11:39,661 you won't be able to go outside and breathe naturally. 226 00:11:42,734 --> 00:11:45,734 Temperature-wise, it's gonna be extremely cold many times. 227 00:11:45,737 --> 00:11:49,907 And it's generally a pretty hostile environment -- 228 00:11:49,907 --> 00:11:52,337 solar flares, U.V. radiation, Alpha particles, 229 00:11:52,343 --> 00:11:53,943 other kinds of radiation from the sun, 230 00:11:53,945 --> 00:11:57,215 as well as cosmic radiation 231 00:11:57,215 --> 00:11:59,115 that's coming from all over the solar system and beyond. 232 00:11:59,117 --> 00:12:01,817 You have to wear a space suit 233 00:12:01,819 --> 00:12:03,649 the entire time you're on the surface of Mars. 234 00:12:05,890 --> 00:12:11,860 Temperatures on Mars can plummet 235 00:12:11,863 --> 00:12:14,732 to below negative-195 degrees near the poles. 236 00:12:14,732 --> 00:12:19,270 Containing virtually no oxygen, 237 00:12:19,270 --> 00:12:23,270 the wispy atmosphere has a pressure of just 0.6% 238 00:12:23,274 --> 00:12:27,812 of what can be found at sea level here on earth. 239 00:12:27,812 --> 00:12:31,712 This is why space suits will be one of the critical components 240 00:12:31,716 --> 00:12:32,884 for any future human missions. 241 00:12:32,884 --> 00:12:35,084 So, you need something 242 00:12:35,086 --> 00:12:37,516 to protect you from essentially exploding 243 00:12:37,522 --> 00:12:39,422 or at least having your skin all stretched out 244 00:12:39,424 --> 00:12:41,254 and the blood boiling and getting the bends, 245 00:12:41,259 --> 00:12:43,689 things like that. 246 00:12:43,695 --> 00:12:46,564 The way space suits are designed now, 247 00:12:46,564 --> 00:12:49,164 they're mostly pressurized spacecraft. 248 00:12:49,167 --> 00:12:52,367 Essentially, they're almost like a mini spaceship. 249 00:12:56,941 --> 00:13:00,278 Oh, it's beautiful, Mike. It really is. 250 00:13:00,278 --> 00:13:03,008 Martian visitors will require a full face helmet, 251 00:13:03,014 --> 00:13:04,682 permanent oxygen supply, life support, 252 00:13:04,682 --> 00:13:08,982 and electrical systems 253 00:13:08,986 --> 00:13:11,923 just like astronauts on board the international space station. 254 00:13:11,923 --> 00:13:14,523 But you'll have to look beyond your space suit 255 00:13:14,525 --> 00:13:18,863 for safety and shelter. 256 00:13:18,863 --> 00:13:22,033 The next location in our Mars travel guide 257 00:13:22,033 --> 00:13:25,870 is one that could provide some much-needed refuge 258 00:13:25,870 --> 00:13:29,070 for the weary traveler -- the Tharsis region, 259 00:13:29,073 --> 00:13:31,743 home to some of the largest volcanoes in the solar system, 260 00:13:31,743 --> 00:13:34,873 including Pavonis Mons. 261 00:13:34,879 --> 00:13:38,149 This may not look like a typical home, 262 00:13:38,149 --> 00:13:41,819 but buried just beneath the surface of this volcano 263 00:13:41,819 --> 00:13:44,819 is a unique feature that offers protection from the elements, 264 00:13:44,822 --> 00:13:47,252 and, remarkably, similar features 265 00:13:47,258 --> 00:13:49,188 can be found right here on earth 266 00:13:49,193 --> 00:13:51,162 if you know where to look for them. 267 00:13:54,866 --> 00:13:58,336 We're out here on an A'a flow in Hawaii. 268 00:13:58,336 --> 00:14:00,236 This lava flow originated towards the summit of Mauna Loa 269 00:14:00,238 --> 00:14:02,268 and has flowed about 20 kilometers 270 00:14:02,273 --> 00:14:05,073 towards the ocean here. 271 00:14:05,076 --> 00:14:09,646 But what you don't see is that this lava flow 272 00:14:09,647 --> 00:14:11,517 is covering a vast network of lava tubes that is now below us, 273 00:14:14,452 --> 00:14:15,982 and that's what we want to get to. 274 00:14:15,987 --> 00:14:18,087 Volcanoes are cool 275 00:14:18,089 --> 00:14:20,858 'cause we find them all over the solar system. 276 00:14:20,858 --> 00:14:23,758 Volcanism is a fundamental process 277 00:14:23,761 --> 00:14:27,231 for shaping planetary bodies, for shaping moons, 278 00:14:27,231 --> 00:14:31,001 so the more we can learn about it, the more we can understand 279 00:14:31,002 --> 00:14:33,371 our solar system and our universe. 280 00:14:33,371 --> 00:14:36,440 The surface of Pavonis Mons 281 00:14:36,440 --> 00:14:38,570 is riddled with lava tubes like this, 282 00:14:38,576 --> 00:14:41,946 natural caverns that formed 283 00:14:41,946 --> 00:14:44,916 when the planet was still volcanically active. 284 00:14:44,916 --> 00:14:48,486 NASA volcanologist Dr. Brent Garry 285 00:14:48,486 --> 00:14:50,354 has dedicated his career to understanding these features. 286 00:14:50,354 --> 00:14:54,792 As a lava flow is coming down, 287 00:14:54,792 --> 00:14:57,192 these tube systems can form underneath a solid crust. 288 00:14:57,195 --> 00:14:59,063 So you'll have a hard crust on the outside, 289 00:14:59,063 --> 00:15:01,663 and the interior will be the lava, 290 00:15:01,666 --> 00:15:03,066 the liquid rock flowing through it. 291 00:15:03,067 --> 00:15:06,097 Think of the London underground. 292 00:15:06,103 --> 00:15:08,403 It's like a subway system of lava going through there. 293 00:15:08,406 --> 00:15:11,436 And as the lava drains out, 294 00:15:11,442 --> 00:15:13,242 that's when we're left with these giant cavern systems 295 00:15:15,513 --> 00:15:18,683 that we see here, that we're inside right now. 296 00:15:18,683 --> 00:15:21,652 Today, Dr. Garry is using light detection 297 00:15:21,652 --> 00:15:26,422 and ranging technology, or LiDAR, 298 00:15:26,424 --> 00:15:29,124 to create a 3-d model of this lava tube in Hawaii. 299 00:15:29,126 --> 00:15:31,156 What we're building with all the LiDAR scans 300 00:15:31,162 --> 00:15:33,262 is a map of a lava tube. 301 00:15:33,264 --> 00:15:34,964 LiDAR is an optimal system to use 302 00:15:34,966 --> 00:15:36,234 because it doesn't need its own light source. 303 00:15:36,234 --> 00:15:38,764 It can see in the dark. 304 00:15:38,769 --> 00:15:42,569 Until we land on the red planet, 305 00:15:42,573 --> 00:15:45,943 mapping lava tubes on earth is Dr. Garry's best chance 306 00:15:45,943 --> 00:15:47,343 of understanding their martian equivalents. 307 00:15:52,216 --> 00:15:53,684 This is a map created on one of his previous expeditions. 308 00:15:53,684 --> 00:15:54,884 Here, we're flying through 309 00:15:54,886 --> 00:15:56,486 one of the collapse pits, 310 00:15:56,487 --> 00:15:59,017 and what we're capturing 311 00:15:59,023 --> 00:16:02,093 is the shape, the dimensions, 312 00:16:02,093 --> 00:16:04,093 the morphology of the whole entire lava-tube system. 313 00:16:04,095 --> 00:16:05,495 But we're also capturing the details 314 00:16:05,496 --> 00:16:07,926 of all the different textures 315 00:16:07,932 --> 00:16:11,702 that are on the inside of the lava tube. 316 00:16:15,139 --> 00:16:19,409 Traveling to Mars is not for the fainthearted. 317 00:16:19,410 --> 00:16:22,079 You need to be prepared for a harsh, dynamic environment. 318 00:16:22,079 --> 00:16:25,249 Micrometeorites rain down, 319 00:16:25,249 --> 00:16:31,519 dust storms rage for weeks at a time, 320 00:16:31,522 --> 00:16:35,422 and radiation levels are up to 250 times higher than on earth. 321 00:16:35,426 --> 00:16:39,726 Lava tubes would provide much-needed sanctuary 322 00:16:39,730 --> 00:16:43,230 for any travelers weary of the ferocious martian climate. 323 00:16:46,837 --> 00:16:49,637 And for those willing to venture outside, 324 00:16:49,640 --> 00:16:52,270 the lava tubes provide the perfect base 325 00:16:52,276 --> 00:16:54,806 to explore the rest of the Tharsis region 326 00:16:54,812 --> 00:16:59,112 and its staggering volcanoes. 327 00:16:59,116 --> 00:17:02,686 Home to 12 volcanoes near the martian equator 328 00:17:02,687 --> 00:17:05,687 and stretching across 2,500 miles, 329 00:17:05,690 --> 00:17:10,528 the volcanoes here are record-breaking -- 330 00:17:10,528 --> 00:17:16,567 up to 100 times larger than anything on earth, 331 00:17:16,567 --> 00:17:18,997 including the largest volcano in our solar system, Olympus Mons. 332 00:17:23,441 --> 00:17:26,141 This would surely be one of the top tourist attractions 333 00:17:26,143 --> 00:17:31,482 for any traveler visiting Mars. 334 00:17:35,319 --> 00:17:37,388 No trip is complete without sharing these spectacular sights 335 00:17:37,388 --> 00:17:41,958 with your family and friends, 336 00:17:41,959 --> 00:17:46,529 but a postcard wouldn't make it home to earth. 337 00:17:46,530 --> 00:17:48,399 Instead, scientists are coming up with cutting-edge technology 338 00:17:48,399 --> 00:17:51,769 to make sure our loved ones 339 00:17:53,778 --> 00:17:56,347 never miss a moment of our martian adventure. 340 00:18:00,552 --> 00:18:02,482 Communication to mission control during space travel is vital. 341 00:18:02,487 --> 00:18:04,255 And for me, it was also essential 342 00:18:04,255 --> 00:18:05,655 to stay connected to my family. 343 00:18:05,657 --> 00:18:08,257 It was on my second mission 344 00:18:08,259 --> 00:18:11,196 that I sent the first tweet from space. 345 00:18:11,196 --> 00:18:12,864 And as we prepare for future missions to Mars, 346 00:18:12,864 --> 00:18:15,533 what about space texting? 347 00:18:15,533 --> 00:18:18,533 Researchers are suggesting that we try that, 348 00:18:18,536 --> 00:18:22,136 along with some other groundbreaking methods. 349 00:18:25,176 --> 00:18:30,076 With so many stunning images, 350 00:18:30,081 --> 00:18:34,681 it's easy to forget just how isolated Mars is from earth. 351 00:18:34,686 --> 00:18:38,423 Intrepid travelers will need a way to keep in touch with home. 352 00:18:38,423 --> 00:18:41,153 NASA engineer Dr. Kara Beaton is part of the team 353 00:18:41,159 --> 00:18:43,259 investigating how future Mars explorers 354 00:18:43,261 --> 00:18:44,429 will be able to communicate. 355 00:18:44,429 --> 00:18:45,697 The shortest journey 356 00:18:45,697 --> 00:18:47,227 that you would have for a Mars mission 357 00:18:47,232 --> 00:18:49,532 is close to three years. 358 00:18:49,534 --> 00:18:51,903 It's about six months of transit time there, 359 00:18:51,903 --> 00:18:54,072 and then you need to wait for about a year or year and a half 360 00:18:54,072 --> 00:18:56,202 on the surface before you can begin 361 00:18:56,207 --> 00:18:58,007 your return journey back to earth. 362 00:19:00,245 --> 00:19:02,575 Three years in isolation 363 00:19:02,580 --> 00:19:05,917 with a very small crew of just a couple people 364 00:19:05,917 --> 00:19:09,287 and limited communication with family and friends on earth 365 00:19:09,287 --> 00:19:13,787 is a big challenge that NASA is currently looking into. 366 00:19:15,693 --> 00:19:18,793 Today, Dr. Beaton and her colleagues 367 00:19:18,797 --> 00:19:20,927 are testing prototype communications backpacks. 368 00:19:22,767 --> 00:19:24,235 So, because of the very large distances 369 00:19:24,235 --> 00:19:28,035 between earth and Mars -- 370 00:19:28,039 --> 00:19:31,709 anywhere from 35 million to 225 million miles -- 371 00:19:31,709 --> 00:19:36,009 there is a communication delay between someone talking on earth 372 00:19:36,014 --> 00:19:38,244 to someone on Mars and vice versa. 373 00:19:38,249 --> 00:19:40,118 So if I were to have a conversation with you 374 00:19:40,118 --> 00:19:42,918 and I'm on Mars and you're on earth 375 00:19:42,921 --> 00:19:46,051 and I speak over a voice comm loop, 376 00:19:46,057 --> 00:19:47,287 it would take anywhere from 4 to 22 minutes to get to you, 377 00:19:47,292 --> 00:19:49,492 and then, for you to respond, 378 00:19:49,494 --> 00:19:51,863 it would take another 4 to 22 minutes 379 00:19:51,863 --> 00:19:54,663 for me to hear that response. 380 00:19:54,666 --> 00:19:56,496 By seeing how these sorts of delays 381 00:19:56,501 --> 00:20:00,501 impact real fieldwork, 382 00:20:00,505 --> 00:20:03,635 Dr. Beaton and her team are able to develop solutions. 383 00:20:03,641 --> 00:20:05,571 So, we've come up with different techniques 384 00:20:05,577 --> 00:20:07,107 for how to best communicate. 385 00:20:07,111 --> 00:20:09,441 So, obviously, voice is one way, 386 00:20:09,447 --> 00:20:12,047 and certainly, that's a viable option, 387 00:20:12,050 --> 00:20:13,680 but we've also found that text-messaging is good 388 00:20:13,685 --> 00:20:15,315 because that allows the crew members 389 00:20:15,320 --> 00:20:17,450 to do something else on the side 390 00:20:17,455 --> 00:20:19,385 while they're waiting to hear a response. 391 00:20:22,093 --> 00:20:26,130 But in a real Mars mission, 392 00:20:26,130 --> 00:20:29,067 how would you actually send and receive these messages? 393 00:20:29,067 --> 00:20:32,837 To begin, you'll need one of these -- 394 00:20:32,837 --> 00:20:35,837 a nearly 230-foot radio telescope. 395 00:20:35,840 --> 00:20:39,210 Richard Stephenson is a radio engineer 396 00:20:39,210 --> 00:20:41,880 here at the Canberra deep space communication complex 397 00:20:41,880 --> 00:20:44,980 in Australia. 398 00:20:44,983 --> 00:20:48,620 The deep space network is capable 399 00:20:48,620 --> 00:20:50,588 of sending and receiving high-frequency radio signals 400 00:20:50,588 --> 00:20:53,958 billions of miles away, 401 00:20:53,958 --> 00:20:59,228 even to the very edges of our solar system. 402 00:20:59,230 --> 00:21:03,130 The deep space network has three complexes around the globe, 403 00:21:03,134 --> 00:21:07,504 and they're spaced around about 120 degrees apart. 404 00:21:07,505 --> 00:21:10,575 So, as the earth rotates, we can provide 24/7 coverage 405 00:21:10,575 --> 00:21:14,075 to any of the missions that we're supporting. 406 00:21:14,078 --> 00:21:16,608 These radio dishes are our eyes and ears on the planet, 407 00:21:16,614 --> 00:21:18,483 and any information we get back from Mars 408 00:21:18,483 --> 00:21:20,051 is received right here. 409 00:21:20,051 --> 00:21:23,651 Well, this antenna -- 410 00:21:23,655 --> 00:21:26,055 deep space station 43 is our 70-meter antenna. 411 00:21:26,057 --> 00:21:29,157 It's a very heavy-duty antenna. 412 00:21:29,160 --> 00:21:32,930 We're looking at 4,000 tons of steerable metal. 413 00:21:32,931 --> 00:21:34,961 So regardless of wind, weather, we can support the spacecraft 414 00:21:34,966 --> 00:21:38,936 that need to communicate to earth. 415 00:21:38,937 --> 00:21:40,437 As we prepare to send the first human explorers 416 00:21:40,438 --> 00:21:43,168 to the red planet, 417 00:21:43,174 --> 00:21:44,404 building up a martian communication infrastructure 418 00:21:44,409 --> 00:21:47,839 is going to be key. 419 00:21:47,845 --> 00:21:49,675 The deep space network's motto is 420 00:21:49,681 --> 00:21:52,681 "don't leave earth without us." 421 00:21:52,684 --> 00:21:54,914 We're the traffic control of the solar system. 422 00:21:54,919 --> 00:21:57,219 Thanks to radio telescopes like these, 423 00:21:57,221 --> 00:22:00,221 strategically positioned around the globe, 424 00:22:00,224 --> 00:22:01,993 travelers to Mars won't be isolated from everyone 425 00:22:01,993 --> 00:22:03,493 back on earth. 426 00:22:03,494 --> 00:22:06,631 If you're one of them, 427 00:22:06,631 --> 00:22:11,001 you'll be able to communicate with your loved ones every day, 428 00:22:11,002 --> 00:22:13,972 waxing lyrical about the epic wonders you have seen. 429 00:22:13,972 --> 00:22:18,509 These telescopes will be the sorting offices 430 00:22:18,509 --> 00:22:22,809 for the most spectacular postcards in the universe. 431 00:22:22,814 --> 00:22:26,984 Despite its stunning landscapes, Mars has a dark secret, 432 00:22:26,985 --> 00:22:30,355 a history shrouded in mystery and destruction. 433 00:22:30,355 --> 00:22:33,525 If we are ever going to plan future expeditions to Mars, 434 00:22:35,031 --> 00:22:38,061 we've got to understand its violent past. 435 00:22:42,338 --> 00:22:44,868 For the past 50 years, unmanned spacecraft and rovers 436 00:22:44,874 --> 00:22:46,443 have gathered incredible images and data 437 00:22:46,443 --> 00:22:48,311 about our elusive neighbor. 438 00:22:48,311 --> 00:22:50,079 But even though Mars is the planet 439 00:22:50,079 --> 00:22:52,309 that we know the most about, 440 00:22:52,315 --> 00:22:54,245 there's still a lot to understand 441 00:22:54,250 --> 00:22:58,620 before we consider living there. 442 00:23:01,524 --> 00:23:04,154 This is Orcus Patera crater. 443 00:23:09,532 --> 00:23:11,362 Nearly 250 miles long, it dwarfs any features nearby. 444 00:23:15,472 --> 00:23:16,772 No one knows quite how this unusual teardrop crater 445 00:23:16,773 --> 00:23:18,441 was formed. 446 00:23:21,277 --> 00:23:25,815 The latest in a long line of mysteries, 447 00:23:25,815 --> 00:23:27,645 it will provide an intriguing stop on any martian adventure. 448 00:23:27,650 --> 00:23:29,580 Mars has a lot of craters. 449 00:23:29,586 --> 00:23:32,616 Most of them are circular. 450 00:23:32,622 --> 00:23:33,922 You can see these craters 40 or 50 kilometers across -- 451 00:23:33,923 --> 00:23:35,853 they tend to be circular. 452 00:23:35,859 --> 00:23:37,459 But there are some that are not. 453 00:23:37,460 --> 00:23:40,660 Now, if I were going to Mars, 454 00:23:40,663 --> 00:23:42,332 the one I would like to go to the most is the whopper. 455 00:23:42,332 --> 00:23:43,932 It looks like a whale. 456 00:23:43,933 --> 00:23:45,233 In fact, it's called Orcus Patera. 457 00:23:45,235 --> 00:23:46,635 "Orcus" means "whale." 458 00:23:46,636 --> 00:23:48,966 So, there's something odd. 459 00:23:48,972 --> 00:23:51,002 Look at all the other craters. They're round. 460 00:23:51,007 --> 00:23:52,475 What formed this? 461 00:23:52,475 --> 00:23:54,675 Coming down. 462 00:23:54,677 --> 00:23:56,777 Until we go there ourselves, 463 00:23:56,779 --> 00:24:00,179 our best shot at answering that question 464 00:24:00,183 --> 00:24:04,383 is to re-create the impact here on earth, 465 00:24:04,387 --> 00:24:05,887 and professor Peter Schultz has just the experiment. 466 00:24:05,889 --> 00:24:08,889 Going back. 467 00:24:08,892 --> 00:24:10,092 This is the NASA Ames vertical gun range, 468 00:24:10,093 --> 00:24:13,123 a unique facility 469 00:24:13,129 --> 00:24:14,998 that simulates high-speed celestial body impacts 470 00:24:14,998 --> 00:24:17,367 on a small scale. 471 00:24:19,135 --> 00:24:22,335 Today, professor Schultz 472 00:24:22,338 --> 00:24:24,807 is trying to re-create the Orcus Patera crater. 473 00:24:28,645 --> 00:24:31,275 This is a case of trying to simulate what happens 474 00:24:31,281 --> 00:24:34,511 when you have a giant projectile -- 475 00:24:34,517 --> 00:24:36,247 an asteroid or even a moon -- collide with Mars. 476 00:24:36,252 --> 00:24:38,652 So, we're gonna try that here. 477 00:24:38,655 --> 00:24:42,855 The target sits 478 00:24:42,859 --> 00:24:44,389 inside a large pressure- controlled impact chamber. 479 00:24:44,394 --> 00:24:46,262 So, at the chamber, 480 00:24:46,262 --> 00:24:47,962 we can control the atmospheric conditions. 481 00:24:47,964 --> 00:24:50,594 And we have a projectile 482 00:24:50,600 --> 00:24:52,030 that will be launched to go through this hole, 483 00:24:52,035 --> 00:24:56,435 this launch tube, 484 00:24:56,439 --> 00:25:00,439 maybe about eight times the velocity of a speeding bullet. 485 00:25:00,443 --> 00:25:02,412 So now all we have to do is really lock and load. 486 00:25:04,180 --> 00:25:08,050 Professor Schultz has rigged the gun 487 00:25:08,051 --> 00:25:11,421 so that it fires at just 15 degrees from the horizontal, 488 00:25:11,421 --> 00:25:13,289 simulating an oblique meteor strike. 489 00:25:13,289 --> 00:25:16,359 With everything in place, 490 00:25:16,359 --> 00:25:18,089 the final step is to fire the projectile. 491 00:25:24,567 --> 00:25:27,136 Rolling. 492 00:25:28,338 --> 00:25:30,006 Oh, good! 493 00:25:30,006 --> 00:25:31,336 We got it, we got it, we got it, we got it. 494 00:25:31,341 --> 00:25:33,441 Let me see, let me see, let me see. 495 00:25:33,443 --> 00:25:34,643 5.60 kilometers per second. 496 00:25:34,644 --> 00:25:35,644 Well done, sir. 497 00:25:41,784 --> 00:25:43,784 Whoa! 498 00:25:43,786 --> 00:25:46,316 It looks like it worked. 499 00:25:46,322 --> 00:25:47,690 So, instead of getting a round crater, 500 00:25:47,690 --> 00:25:49,258 we have an oblong crater, 501 00:25:49,258 --> 00:25:52,595 and we have an oblong crater 502 00:25:52,595 --> 00:25:57,665 that has multiple impacts downrange. 503 00:25:57,667 --> 00:26:01,537 There's a really low rim here, high rim there, and a shelf. 504 00:26:01,537 --> 00:26:03,667 And it requires a very low-angle impact, 505 00:26:03,673 --> 00:26:06,803 and I think that's what's happened on Mars. 506 00:26:10,480 --> 00:26:14,017 The crater is almost a mirror image of Orcus Patera, 507 00:26:14,017 --> 00:26:18,855 scoured lengthways across the landscape. 508 00:26:18,855 --> 00:26:20,755 And professor Schultz has a theory for how it was formed. 509 00:26:23,793 --> 00:26:26,093 A moon going around Mars is in an orbit, 510 00:26:26,095 --> 00:26:28,364 and eventually, that orbit decays, 511 00:26:28,364 --> 00:26:31,901 gets closer and closer to Mars. 512 00:26:31,901 --> 00:26:33,331 In fact, the moon Phobos going around Mars right now 513 00:26:33,336 --> 00:26:36,636 will collide with Mars 514 00:26:36,639 --> 00:26:37,769 in something like 28 million, maybe 30 million years. 515 00:26:37,774 --> 00:26:40,504 So, when that happens, 516 00:26:40,510 --> 00:26:44,347 it'll come in at an extremely low angle, 517 00:26:44,347 --> 00:26:46,677 grazing, just like a spacecraft trying to come in for a landing, 518 00:26:46,683 --> 00:26:47,883 except it's not gonna land so well. 519 00:26:47,884 --> 00:26:50,784 It's gonna collide 520 00:26:50,787 --> 00:26:55,487 and form a crater very similar to Orcus Patera. 521 00:26:55,491 --> 00:26:57,721 Mars has two potato-shaped moons -- 522 00:26:57,727 --> 00:26:59,657 Phobos and Deimos. 523 00:26:59,662 --> 00:27:04,801 But Peter's audacious thought 524 00:27:04,801 --> 00:27:09,101 is that there was once another lost moon orbiting the planet. 525 00:27:09,105 --> 00:27:11,274 The theory makes sense, but the jury remains out. 526 00:27:15,044 --> 00:27:18,014 Situated close to some of Mars' largest volcanoes, 527 00:27:18,014 --> 00:27:19,714 other scientists argue that volcanic forces 528 00:27:19,716 --> 00:27:22,585 could have created the crater 529 00:27:22,585 --> 00:27:25,015 by stretching and compressing the ground. 530 00:27:28,191 --> 00:27:30,191 If we are to discover the crater's true origins, 531 00:27:30,193 --> 00:27:33,262 we must go there ourselves, 532 00:27:33,262 --> 00:27:36,362 because it's only by studying landscapes up close 533 00:27:36,365 --> 00:27:39,702 that we can fully understand them. 534 00:27:39,702 --> 00:27:43,202 Imagine standing atop the crater rim 535 00:27:43,206 --> 00:27:47,243 rising a mile above the surrounding plains, 536 00:27:47,243 --> 00:27:50,780 looking into the depths of the crater below. 537 00:27:50,780 --> 00:27:53,680 What an incredible and enigmatic stop 538 00:27:53,683 --> 00:27:57,283 on your adventure across Mars. 539 00:27:57,286 --> 00:28:01,186 Just like preparing for a trip to a foreign land, 540 00:28:01,190 --> 00:28:04,527 smart packing will be a must for Mars. 541 00:28:04,527 --> 00:28:08,797 So what should you fill your suitcase with? 542 00:28:10,358 --> 00:28:13,688 For starters, you may want to bring a winter coat. 543 00:28:17,865 --> 00:28:19,333 Mars is nicknamed the red planet because of its crimson color. 544 00:28:19,333 --> 00:28:21,933 But take a closer look, 545 00:28:21,936 --> 00:28:24,736 and you'll see beautiful white swirls. 546 00:28:24,739 --> 00:28:27,539 Learning more about these mysterious white ribbons 547 00:28:27,542 --> 00:28:30,042 may unlock the secrets of how Mars formed 548 00:28:30,044 --> 00:28:32,144 and where it's headed. 549 00:28:34,582 --> 00:28:36,751 Your ultimate travel guide to Mars 550 00:28:36,751 --> 00:28:39,981 includes marvelous canyons, 551 00:28:39,987 --> 00:28:42,417 the most spectacular volcanoes in the solar system, 552 00:28:42,423 --> 00:28:43,723 and even underground caves. 553 00:28:43,724 --> 00:28:46,894 But there's no better place 554 00:28:46,894 --> 00:28:49,664 to explore the mysterious martian landscapes 555 00:28:49,664 --> 00:28:51,732 than at the southernmost reaches of the planet. 556 00:28:51,732 --> 00:28:56,632 It may be well off the beaten track, 557 00:28:56,637 --> 00:28:59,367 but the extra effort required to get there will be worthwhile. 558 00:28:59,373 --> 00:29:02,210 This is Mars' Southern polar cap, 559 00:29:02,210 --> 00:29:07,310 one of the coldest places on the planet. 560 00:29:07,315 --> 00:29:08,983 Temperatures here can drop below minus-248 degrees Fahrenheit. 561 00:29:08,983 --> 00:29:11,913 It's an icy destination 562 00:29:11,919 --> 00:29:14,589 that planetary scientist Dr. Meg Schwamb 563 00:29:14,589 --> 00:29:17,019 has long held a fascination. 564 00:29:17,024 --> 00:29:18,654 So, we're standing on a dormant volcano 565 00:29:18,659 --> 00:29:19,927 on the big island of Hawaii. 566 00:29:19,927 --> 00:29:21,657 And so, this is where we have 567 00:29:21,662 --> 00:29:23,292 some of the world-class telescopes 568 00:29:26,300 --> 00:29:29,570 that are observing the night sky. 569 00:29:29,570 --> 00:29:33,240 So, I'm really interested in the south pole of Mars, 570 00:29:33,241 --> 00:29:34,871 and so how that can tell us more about Mars' past 571 00:29:34,876 --> 00:29:37,044 and its current history. 572 00:29:39,714 --> 00:29:44,614 On a clear night, the poles of Mars 573 00:29:44,619 --> 00:29:46,519 can even be seen through small telescopes from here on earth. 574 00:29:48,656 --> 00:29:52,556 Amateur images like these 575 00:29:52,560 --> 00:29:55,830 show the bright ice caps against the red disk of the planet, 576 00:29:55,830 --> 00:29:59,930 but their true wonder is only truly revealed 577 00:29:59,934 --> 00:30:05,204 with images taken from orbit. 578 00:30:05,206 --> 00:30:08,406 At over 248 miles wide and almost 2 miles thick, 579 00:30:08,409 --> 00:30:13,009 the Southern polar cap is a freezing vision 580 00:30:13,014 --> 00:30:16,751 of swirling white on an otherwise rusty-colored planet. 581 00:30:16,751 --> 00:30:19,581 Though it may look much like the south pole on earth, 582 00:30:19,587 --> 00:30:21,055 it has one crucial difference. 583 00:30:21,055 --> 00:30:22,585 So, as you can see behind me, 584 00:30:22,590 --> 00:30:24,659 there's some white dotting the surface, 585 00:30:24,659 --> 00:30:26,789 and that's actually some snow left after 586 00:30:26,794 --> 00:30:28,994 from one of our recent snowfalls. 587 00:30:28,996 --> 00:30:32,166 But on Mars, in the south pole, 588 00:30:32,166 --> 00:30:34,435 there isn't water ice that's exposed, or snow. 589 00:30:34,435 --> 00:30:37,004 It actually snows carbon dioxide. 590 00:30:37,004 --> 00:30:40,141 Often referred to as dry ice, 591 00:30:40,141 --> 00:30:42,910 in the martian winter, this frozen carbon dioxide 592 00:30:42,910 --> 00:30:47,880 blankets the Southern reaches of the planet. 593 00:30:47,882 --> 00:30:50,012 Come spring, when it melts, it transforms straight into a gas, 594 00:30:50,017 --> 00:30:52,717 dramatically changing the landscape 595 00:30:52,720 --> 00:30:54,920 and creating a remarkable phenomenon. 596 00:30:54,922 --> 00:30:59,192 So, what happens on the south pole of Mars 597 00:30:59,193 --> 00:31:00,793 is that you have this layer of semitranslucent ice 598 00:31:00,795 --> 00:31:03,965 on top of the dirt, 599 00:31:03,965 --> 00:31:07,635 and when the sun comes up in the spring and summer, 600 00:31:07,635 --> 00:31:09,303 the sunlight penetrates through down to that dirt layer 601 00:31:09,303 --> 00:31:12,940 and heats up. 602 00:31:12,940 --> 00:31:14,440 Because it's warm, the carbon dioxide ice in contact with it 603 00:31:14,442 --> 00:31:16,842 starts to turn into gas. 604 00:31:16,844 --> 00:31:19,244 And so now you have a layer of gas 605 00:31:19,246 --> 00:31:23,446 trapped underneath a layer of ice. 606 00:31:23,451 --> 00:31:26,581 The consequences of this thaw are quite spectacular. 607 00:31:26,587 --> 00:31:29,557 So, when this gas is trapped underneath this ice sheet, 608 00:31:29,557 --> 00:31:33,027 it breaks through in any way it can through the ice. 609 00:31:33,027 --> 00:31:35,627 And when it gets to the surface, it creates these jets or geysers 610 00:31:35,629 --> 00:31:38,299 on the surface of the south pole of Mars. 611 00:31:38,299 --> 00:31:39,799 Gas is rushing out maybe a few meters -- 612 00:31:39,800 --> 00:31:44,170 not much further, we think. 613 00:31:44,171 --> 00:31:46,471 But it brings up this dust and dirt from below that ice sheet. 614 00:31:46,474 --> 00:31:49,474 If I was standing on the surface of Mars, 615 00:31:49,477 --> 00:31:50,945 you'd see these sort of dark jets coming up, 616 00:31:50,945 --> 00:31:54,715 and it's the local surface winds 617 00:31:54,715 --> 00:31:57,685 that blow these material into these dark streaks. 618 00:31:57,685 --> 00:31:59,785 And then, when there's no more carbon dioxide ice, 619 00:31:59,787 --> 00:32:01,517 it disappears. 620 00:32:01,522 --> 00:32:05,492 Seen from space, 621 00:32:05,493 --> 00:32:08,493 this windblown dust creates breathtaking landscapes. 622 00:32:08,496 --> 00:32:12,096 But these images aren't simply pretty. 623 00:32:12,099 --> 00:32:15,969 They tell us about the martian climate, too. 624 00:32:15,970 --> 00:32:20,170 If we can study how these geysers form, these jets, 625 00:32:20,174 --> 00:32:23,174 and how the wind sort of blows these material, 626 00:32:23,177 --> 00:32:24,977 we can learn more about the martian atmosphere. 627 00:32:24,979 --> 00:32:27,879 This process is completely alien. 628 00:32:27,882 --> 00:32:31,312 We don't have anything like this on earth. 629 00:32:34,522 --> 00:32:37,922 These features disappear each year, 630 00:32:37,925 --> 00:32:40,455 but they leave behind another wonder in their wake -- 631 00:32:40,461 --> 00:32:42,991 the real spiders from Mars. 632 00:32:42,997 --> 00:32:46,867 If we look a little deeper into these images, 633 00:32:46,867 --> 00:32:48,667 what we find, that when there's no carbon dioxide ice anymore, 634 00:32:48,669 --> 00:32:50,469 the fans go away. 635 00:32:50,471 --> 00:32:54,071 And what's left in many of these areas 636 00:32:54,075 --> 00:32:56,805 are these kind of dendritic, like, spider-like features, 637 00:32:56,811 --> 00:32:58,411 which actually has been informally dubbed spiders, 638 00:32:58,412 --> 00:33:01,342 or aranea forms. 639 00:33:04,718 --> 00:33:08,188 These erosion channels meet in a central pit 640 00:33:08,189 --> 00:33:11,289 resembling the body and long legs of a spider, 641 00:33:11,292 --> 00:33:16,262 legs that can stretch for hundreds of miles 642 00:33:16,263 --> 00:33:19,263 and can take more than 1,000 martian years to grow. 643 00:33:19,266 --> 00:33:20,634 Explorers lucky enough to stand at the south pole 644 00:33:20,634 --> 00:33:24,134 during a martian summer 645 00:33:24,138 --> 00:33:26,738 would gaze upon these alien spider-like features 646 00:33:26,740 --> 00:33:29,740 stretching across the landscape. 647 00:33:29,743 --> 00:33:31,212 They would be offered a taste of martian weather 648 00:33:31,212 --> 00:33:34,812 and witness the dramatic proof 649 00:33:34,815 --> 00:33:37,445 that Mars is far from the dead and unchanging planet 650 00:33:37,451 --> 00:33:41,188 that many people assumed. 651 00:33:41,188 --> 00:33:46,258 Mars' icy poles provide some respite 652 00:33:46,260 --> 00:33:48,690 from the desert landscapes that cover most of the planet. 653 00:33:48,696 --> 00:33:52,533 And the more adventurous traveler 654 00:33:52,533 --> 00:33:54,602 may also choose to follow the elusive trail of liquid water 655 00:33:54,602 --> 00:33:58,339 on the martian surface. 656 00:33:58,339 --> 00:34:00,169 In doing so, they will uncover the hidden story 657 00:34:00,174 --> 00:34:04,111 of ancient Mars. 658 00:34:04,111 --> 00:34:06,080 Thanks to the curiosity rover, 659 00:34:06,080 --> 00:34:09,280 we now know that Gale crater 660 00:34:09,283 --> 00:34:11,652 was once the site of an ancient lake. 661 00:34:11,652 --> 00:34:16,522 But where did all the water go? 662 00:34:16,524 --> 00:34:18,654 And how did it shape the landscape we see today? 663 00:34:18,659 --> 00:34:22,659 To see that, Dr. Gupta 664 00:34:22,663 --> 00:34:26,600 needs to look at Gale crater 3.8 billion years ago, 665 00:34:26,600 --> 00:34:29,170 just after it was formed by a meteor impact. 666 00:34:30,838 --> 00:34:32,968 So, this is really cool here. 667 00:34:32,973 --> 00:34:36,773 We've got an augmented reality sandbox, 668 00:34:36,777 --> 00:34:38,707 and so what I'm doing now is, I'm creating the crater rim. 669 00:34:38,712 --> 00:34:40,542 So, there would have been a mountain 670 00:34:40,548 --> 00:34:43,617 in the center of the crater 671 00:34:43,617 --> 00:34:46,487 formed during that impact process. 672 00:34:46,487 --> 00:34:48,556 That forms the core of mount sharp. 673 00:34:48,556 --> 00:34:52,326 When Gale crater first formed, 674 00:34:52,326 --> 00:34:56,696 it's thought Mars had a much more substantial atmosphere, 675 00:34:56,697 --> 00:34:59,297 making the planet warmer and, therefore, wetter than today. 676 00:34:59,300 --> 00:35:01,630 And the water fell across the planet's surface 677 00:35:01,635 --> 00:35:04,035 as rain and snow. 678 00:35:04,038 --> 00:35:07,338 We've got rain forming on the crater rim 679 00:35:07,341 --> 00:35:09,710 and then gushing out into the center of Gale crater 680 00:35:09,710 --> 00:35:11,679 and building up. 681 00:35:11,679 --> 00:35:15,679 As it poured down into the crater, 682 00:35:15,683 --> 00:35:17,952 its water shaped many of the features we see today. 683 00:35:20,054 --> 00:35:22,554 Imagine, if you have heavy rainfall, 684 00:35:22,556 --> 00:35:24,586 rainfall over hundreds of years, 685 00:35:24,592 --> 00:35:26,992 the landscape gets progressively eroded 686 00:35:26,994 --> 00:35:30,364 and carves deep canyons and valleys. 687 00:35:30,364 --> 00:35:33,194 The sediment eroded from those gullies 688 00:35:33,200 --> 00:35:36,100 would have washed into Gale crater, 689 00:35:36,103 --> 00:35:38,372 forming those river deposits that we can see so beautifully 690 00:35:38,372 --> 00:35:41,002 in the images that curiosity takes. 691 00:35:41,008 --> 00:35:45,546 And then the climate changed. 692 00:35:45,546 --> 00:35:47,915 It lost its atmosphere and became arid and hyper-cold, 693 00:35:47,915 --> 00:35:53,385 and all that water evaporated. 694 00:35:53,387 --> 00:35:57,257 And we were left with a crater infilled with sediment. 695 00:35:57,258 --> 00:36:00,358 The rusty, ancient surface of Mars 696 00:36:00,361 --> 00:36:05,631 has enigmatic landscapes at every turn, 697 00:36:05,633 --> 00:36:08,463 from towering sculpted peaks to hidden underground caverns. 698 00:36:08,469 --> 00:36:11,538 And if you are one of the first explorers, 699 00:36:11,538 --> 00:36:16,377 you will need to study every detail. 700 00:36:16,377 --> 00:36:18,577 Each landmark holds its own clues to Mars' mysteries, 701 00:36:18,579 --> 00:36:23,249 and there is no greater mystery 702 00:36:23,250 --> 00:36:25,780 than whether life exists beyond the earth. 703 00:36:25,786 --> 00:36:29,486 As a stranger from earth, 704 00:36:31,151 --> 00:36:34,181 will you be greeted by martian life when you arrive? 705 00:36:36,290 --> 00:36:38,390 When people meet me for the first time, 706 00:36:38,392 --> 00:36:40,822 the question I get asked the most is, 707 00:36:40,827 --> 00:36:42,857 "is there life somewhere else in the universe?" 708 00:36:42,863 --> 00:36:46,500 And while I don't know for sure, 709 00:36:46,500 --> 00:36:48,569 I love the possibility that life could exist on other planets. 710 00:36:48,569 --> 00:36:51,738 So how do we find this life, 711 00:36:51,738 --> 00:36:56,338 whether it be past, present, or future? 712 00:36:56,343 --> 00:36:59,173 There's one scientist that says the proof is in the salt. 713 00:37:02,082 --> 00:37:03,650 To stand a chance of finding life on Mars, 714 00:37:03,650 --> 00:37:05,250 it's thought travelers will need 715 00:37:05,252 --> 00:37:07,882 to journey to a region of the planet 716 00:37:07,888 --> 00:37:10,588 unexplored by landers or rovers. 717 00:37:10,591 --> 00:37:13,521 Perched in the remote Southern highlands, 718 00:37:13,527 --> 00:37:16,827 Terra Sirenum is a land of cratered terrain 719 00:37:16,830 --> 00:37:20,467 capped in crystalline mineral deposits. 720 00:37:20,467 --> 00:37:24,805 It's thought that if we're going to find signs of local wildlife, 721 00:37:24,805 --> 00:37:26,873 past or present, then this will be the best spot. 722 00:37:28,842 --> 00:37:32,112 Of all the questions astrobiology asks, 723 00:37:32,112 --> 00:37:36,182 probably its biggest one is, is there life beyond the earth? 724 00:37:36,183 --> 00:37:37,983 When we're assessing whether a planet is habitable, 725 00:37:37,985 --> 00:37:39,315 we're looking for some basic things. 726 00:37:39,319 --> 00:37:41,719 We need some liquid water 727 00:37:41,722 --> 00:37:45,292 for all those chemical reactions to happen in, 728 00:37:45,292 --> 00:37:46,922 we need a source of energy, like sunlight or chemical energy, 729 00:37:46,927 --> 00:37:49,157 and we also need some basic elements 730 00:37:49,162 --> 00:37:51,592 like carbon and phosphorus. 731 00:37:51,598 --> 00:37:55,768 All those things have to come together in one place 732 00:37:55,769 --> 00:37:58,099 for life as we know it, at least, to be able to grow. 733 00:38:01,508 --> 00:38:03,276 Before our first spacecraft arrived in the 1960s, 734 00:38:03,276 --> 00:38:05,776 the idea of visitors to Mars 735 00:38:05,779 --> 00:38:08,579 setting foot on a lush, living planet 736 00:38:08,582 --> 00:38:10,412 seemed like a perfectly reasonable idea. 737 00:38:10,417 --> 00:38:13,247 In the early history of Mars, 738 00:38:13,253 --> 00:38:15,322 the planet would have looked quite a lot like early earth. 739 00:38:15,322 --> 00:38:17,391 There would have been liquid water on the surface. 740 00:38:17,391 --> 00:38:19,391 Maybe it would have been warmer. 741 00:38:19,393 --> 00:38:21,893 Perhaps during that period of time, 742 00:38:21,895 --> 00:38:26,565 it could have sustained biology. 743 00:38:26,566 --> 00:38:28,966 But about 3 1/2 billion years ago, that water froze up, 744 00:38:28,969 --> 00:38:30,799 and the planet become what we know today -- 745 00:38:30,804 --> 00:38:34,141 pretty much a desert world. 746 00:38:34,141 --> 00:38:37,041 Because of that, it was never able 747 00:38:37,044 --> 00:38:38,674 to sustain the sort of evolutionary development 748 00:38:38,679 --> 00:38:41,448 that you can see around you here. 749 00:38:45,118 --> 00:38:49,288 So we need to look in places on Mars and on earth 750 00:38:49,289 --> 00:38:50,619 that could give primitive life a fighting chance. 751 00:38:50,624 --> 00:38:53,193 There are two types of places. 752 00:38:53,193 --> 00:38:55,023 We might look in briny, salty solutions. 753 00:38:55,028 --> 00:38:57,128 Those brines could still be liquid 754 00:38:57,130 --> 00:38:59,199 on the surface of Mars today. 755 00:38:59,199 --> 00:39:00,567 And we're looking at ancient salt deposits. 756 00:39:00,567 --> 00:39:03,497 In those salts, 757 00:39:03,503 --> 00:39:05,872 maybe we might try and look for signs of past life. 758 00:39:07,541 --> 00:39:10,441 With that in mind, 759 00:39:10,444 --> 00:39:14,114 astrobiologists like professor Cockell 760 00:39:14,114 --> 00:39:17,451 started searching for the perfect spot to hunt for life. 761 00:39:20,587 --> 00:39:25,287 And in time, images taken from orbit 762 00:39:25,292 --> 00:39:27,622 revealed more than 200 places in the Terra Sirenum region 763 00:39:27,627 --> 00:39:30,797 where thick salt layers exist. 764 00:39:32,999 --> 00:39:37,299 The Terra Sirenum region of Mars 765 00:39:37,304 --> 00:39:39,134 has salt deposits from ancient ponds and lakes 766 00:39:39,139 --> 00:39:41,839 that essentially evaporated -- 767 00:39:41,842 --> 00:39:43,510 the last remnants of liquid water on Mars. 768 00:39:45,645 --> 00:39:49,583 And these salts in Terra Sirenum 769 00:39:49,583 --> 00:39:52,413 could preserve or record the existence of life on Mars. 770 00:39:52,419 --> 00:39:53,887 And to support this theory, professor Cockell 771 00:39:53,887 --> 00:39:57,587 has been investigating some 772 00:39:57,591 --> 00:40:00,560 of the most remote and inhospitable places on earth. 773 00:40:00,560 --> 00:40:03,660 So, here we've got some samples from the Negev desert. 774 00:40:03,663 --> 00:40:07,533 Microbes that live in those environments are very tolerant 775 00:40:07,534 --> 00:40:10,234 of both high temperatures and extreme dryness. 776 00:40:10,237 --> 00:40:12,737 And then, these microbes are from a lake in Canada 777 00:40:12,739 --> 00:40:16,609 that has very high concentrations of sulfate, 778 00:40:16,610 --> 00:40:20,310 similar to the sorts of salts that we find on Mars. 779 00:40:20,313 --> 00:40:21,782 Finding living bacteria in places like this 780 00:40:21,782 --> 00:40:25,852 tells Cockell and his team 781 00:40:25,852 --> 00:40:28,352 that Mars-like environments here on earth can support life. 782 00:40:28,355 --> 00:40:30,985 But that's only half the picture. 783 00:40:30,991 --> 00:40:35,128 So, this is a sample from a very extreme environment. 784 00:40:35,128 --> 00:40:36,628 It comes from a kilometer underground in a salt mine. 785 00:40:36,630 --> 00:40:39,030 This is the sort of sample 786 00:40:39,032 --> 00:40:41,802 you might be able to find in Terra Sirenum 787 00:40:41,802 --> 00:40:44,802 if you dug down beneath the surface. 788 00:40:44,805 --> 00:40:48,905 The question is, could these microbes 789 00:40:48,909 --> 00:40:50,609 also survive under the conditions on present-day Mars? 790 00:40:50,610 --> 00:40:54,410 We've subjected these microbes 791 00:40:54,414 --> 00:40:57,344 to similar sorts of environments that you might find on Mars, 792 00:40:57,350 --> 00:40:59,820 so no oxygen, very low amounts of energy, 793 00:40:59,820 --> 00:41:02,120 very low concentrations of nutrients. 794 00:41:02,122 --> 00:41:05,759 And in those sorts of environments, 795 00:41:05,759 --> 00:41:07,489 these microbes can not only survive -- they can also grow. 796 00:41:07,494 --> 00:41:10,063 What these results show us 797 00:41:10,063 --> 00:41:12,263 is that some of these salty environments on Mars 798 00:41:12,265 --> 00:41:13,765 may well have been habitable. 799 00:41:13,767 --> 00:41:17,837 It may not look like much, 800 00:41:17,838 --> 00:41:21,538 but this is the closest thing to life on Mars anyone has seen. 801 00:41:21,541 --> 00:41:23,771 I often joke that if you send me to Terra Sirenum 802 00:41:23,777 --> 00:41:25,907 with a microscope and a shovel, 803 00:41:25,912 --> 00:41:28,112 I can tell you within a few hours 804 00:41:28,114 --> 00:41:30,644 whether there's life on Mars. 805 00:41:30,650 --> 00:41:33,520 Astrobiologists like professor Cockell 806 00:41:33,520 --> 00:41:35,720 are building a case that the salt plains on Mars 807 00:41:35,722 --> 00:41:38,652 are potentially habitable. 808 00:41:38,658 --> 00:41:41,188 The inquisitive traveler prepared to dig deep 809 00:41:41,194 --> 00:41:44,194 might just find some of the local wildlife 810 00:41:44,197 --> 00:41:47,867 sheltered beneath the subsurface. 811 00:41:47,868 --> 00:41:49,468 It would be the discovery of the century 812 00:41:49,469 --> 00:41:54,139 and proof that life probably exist elsewhere 813 00:41:54,140 --> 00:41:55,721 in the universe too, 814 00:41:56,297 --> 00:42:00,721 and it would be the perfect end to an epic journey. 61393

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