1 00:00:02,970 --> 00:00:05,138 - Earth is constantly changing the way it looks, 2 00:00:05,138 --> 00:00:07,107 and there's more happening beneath our feet 3 00:00:07,107 --> 00:00:08,509 than you might expect. 4 00:00:08,509 --> 00:00:12,546 [dramatic music] 5 00:00:16,250 --> 00:00:19,620 Can you tell the difference between these two mountains? 6 00:00:19,620 --> 00:00:22,089 The difference is Earth-shattering. 7 00:00:22,089 --> 00:00:23,857 - The difference between a mountain and a volcano 8 00:00:23,857 --> 00:00:25,192 is that volcanoes 9 00:00:25,192 --> 00:00:26,793 are formed from lava, 10 00:00:26,793 --> 00:00:30,430 whereas mountains are not necessarily formed from lava. 11 00:00:30,430 --> 00:00:32,266 Volcanism changes and shapes our planet 12 00:00:32,266 --> 00:00:34,635 by giving us new landmasses such as Hawaii, 13 00:00:34,635 --> 00:00:36,136 such as Iceland, 14 00:00:36,136 --> 00:00:39,439 and it also builds these tall, mountain-like structures 15 00:00:39,439 --> 00:00:41,008 on the surface of our planet. 16 00:00:41,008 --> 00:00:42,609 And in many cases, it actually helps 17 00:00:42,609 --> 00:00:44,811 to make the ground more fertile for planting 18 00:00:44,811 --> 00:00:46,580 of different types of crops. 19 00:00:46,580 --> 00:00:50,984 - Volcanoes are places on the Earth or other planets 20 00:00:50,984 --> 00:00:54,555 where molten material from the inside comes up 21 00:00:54,555 --> 00:00:58,759 and flows out or explodes out onto the surface. 22 00:00:58,759 --> 00:01:00,227 Volcanoes will form anywhere 23 00:01:00,227 --> 00:01:02,095 that the material from the inside 24 00:01:02,095 --> 00:01:04,131 can make its way to the surface. 25 00:01:04,131 --> 00:01:06,667 Sometimes the material will just shove its way up 26 00:01:06,667 --> 00:01:08,235 and makes its own pathway. 27 00:01:08,235 --> 00:01:11,338 Other times, it'll follow a fracture or a crack 28 00:01:11,338 --> 00:01:13,473 through the rocks at the surface. 29 00:01:13,473 --> 00:01:15,876 - Faults are just cracks in Earth's crust 30 00:01:15,876 --> 00:01:18,111 that form the boundaries for Earth's tectonic plates. 31 00:01:18,111 --> 00:01:19,980 - One of the things you can actually tell right away 32 00:01:19,980 --> 00:01:23,350 from looking at a volcano is if you look at its slope, 33 00:01:23,350 --> 00:01:25,752 if you just look at the volcano as a whole, 34 00:01:25,752 --> 00:01:28,088 it's just the height divided by the width. 35 00:01:28,088 --> 00:01:31,625 A shallow-sloped volcano was one that was formed 36 00:01:31,625 --> 00:01:34,995 by magma that had a low viscosity, that was runny, 37 00:01:34,995 --> 00:01:36,496 and a steep-sloped volcano 38 00:01:36,496 --> 00:01:39,099 is one that was formed by a magma that was sticky. 39 00:01:39,099 --> 00:01:42,169 When magma moves around, it has to push the rocks around. 40 00:01:42,169 --> 00:01:43,337 And one way that we can measure that 41 00:01:43,337 --> 00:01:45,806 is through the breaking of the rocks 42 00:01:45,806 --> 00:01:47,107 using seismometers. 43 00:01:47,107 --> 00:01:49,877 - Volcanoes play a role in how Earth looks today, 44 00:01:49,877 --> 00:01:52,546 but did you know that volcanoes are on other worlds 45 00:01:52,546 --> 00:01:54,181 in our solar system? 46 00:01:54,181 --> 00:01:57,284 You didn't? Well, that's not your fault. 47 00:01:57,284 --> 00:01:58,919 - Mars has volcanoes. 48 00:01:58,919 --> 00:02:01,154 Actually, the largest volcano in our solar system, 49 00:02:01,154 --> 00:02:03,190 Olympus Mons, is on Mars. 50 00:02:03,190 --> 00:02:04,691 Venus has volcanoes, 51 00:02:04,691 --> 00:02:07,694 Jupiter's moon, Io, has lots and lots of volcanoes. 52 00:02:07,694 --> 00:02:09,696 And there are hundreds of volcanoes on Io's surface 53 00:02:09,696 --> 00:02:11,131 and they erupt daily. 54 00:02:11,131 --> 00:02:13,600 - Not all planetary bodies are made of rocks, 55 00:02:13,600 --> 00:02:15,068 and in fact, 56 00:02:15,068 --> 00:02:16,537 the outer solar system, 57 00:02:16,537 --> 00:02:18,539 the majority of the bodies out there are-- 58 00:02:18,539 --> 00:02:21,241 have an icy surface. 59 00:02:21,241 --> 00:02:24,478 And so through heating and other mechanisms, 60 00:02:24,478 --> 00:02:26,613 you can melt ice just like you can melt rocks. 61 00:02:26,613 --> 00:02:29,049 - And so when we have volcanism on these moons, 62 00:02:29,049 --> 00:02:31,685 instead of taking the form of hot rock or lava 63 00:02:31,685 --> 00:02:33,086 that erupts onto the surface, 64 00:02:33,086 --> 00:02:34,555 we have slush that erupts onto the surface. 65 00:02:34,555 --> 00:02:36,190 What we call this cold volcanism, 66 00:02:36,190 --> 00:02:39,359 or this icy volcanism, is cryovolcanism. 67 00:02:39,359 --> 00:02:42,062 You have a planet that has a very smooth surface, 68 00:02:42,062 --> 00:02:44,498 then you know that volcanoes or cryovolcanoes 69 00:02:44,498 --> 00:02:45,599 have been active. 70 00:02:45,599 --> 00:02:47,234 You know that there's been some fluid, 71 00:02:47,234 --> 00:02:48,468 whether that be lava, 72 00:02:48,468 --> 00:02:50,237 or when you're talking about icy volcanism, 73 00:02:50,237 --> 00:02:53,640 icy lava or a cryolava that's erupted onto the surface 74 00:02:53,640 --> 00:02:55,676 and it smoothed the surface out. 75 00:02:55,676 --> 00:02:58,312 - Cryovolcanoes? Cool. 76 00:02:58,312 --> 00:03:00,214 So there are different types of volcanoes 77 00:03:00,214 --> 00:03:02,916 and they can be found all over our solar system. 78 00:03:02,916 --> 00:03:04,818 But how do we know this? 79 00:03:04,818 --> 00:03:07,054 - So the technology that's used to explore volcanoes 80 00:03:07,054 --> 00:03:09,089 that I use the most is basically 81 00:03:09,089 --> 00:03:11,625 data that comes back from robotic spacecraft. 82 00:03:11,625 --> 00:03:13,560 So NASA has sent spacecraft 83 00:03:13,560 --> 00:03:14,895 to many planets and moons. 84 00:03:14,895 --> 00:03:16,797 From these pictures, we're able to determine 85 00:03:16,797 --> 00:03:19,399 how tall these volcanoes are, how wide they are. 86 00:03:19,399 --> 00:03:21,668 These spacecraft also have instruments that tell us about 87 00:03:21,668 --> 00:03:23,871 the composition of those volcanoes. 88 00:03:23,871 --> 00:03:25,939 What we're able to do with that information 89 00:03:25,939 --> 00:03:28,141 is we're able to use, then, computer models 90 00:03:28,141 --> 00:03:29,776 and mathematical equations 91 00:03:29,776 --> 00:03:32,513 to try to figure out how these volcanoes formed, 92 00:03:32,513 --> 00:03:34,615 how runny the lava was that formed them. 93 00:03:34,615 --> 00:03:37,484 - Other ways that we can monitor volcanoes include 94 00:03:37,484 --> 00:03:40,821 paying attention to gases coming out of fractures 95 00:03:40,821 --> 00:03:42,322 around the volcanoes. 96 00:03:42,322 --> 00:03:46,093 A really big volcanic eruption can have global effects. 97 00:03:46,093 --> 00:03:48,328 Something big like Mt. Pinatubo 98 00:03:48,328 --> 00:03:50,364 puts so much ash into the air 99 00:03:50,364 --> 00:03:51,465 that it actually cooled the Earth off 100 00:03:51,465 --> 00:03:53,333 for a little while. 101 00:03:53,333 --> 00:03:54,635 - It's important to study volcanoes 102 00:03:54,635 --> 00:03:56,003 because they teach us a lot 103 00:03:56,003 --> 00:03:58,839 about the interior properties of planets and moons. 104 00:03:58,839 --> 00:04:01,742 So, if we see volcanoes on the surface of a planet or a moon, 105 00:04:01,742 --> 00:04:03,377 we know at one time or another 106 00:04:03,377 --> 00:04:05,212 that the interior was warm enough 107 00:04:05,212 --> 00:04:06,780 to sustain that type of activity. 108 00:04:06,780 --> 00:04:09,216 When we think of our own planet, Earth, 109 00:04:09,216 --> 00:04:10,651 volcanism has been very important. 110 00:04:10,651 --> 00:04:12,920 We have this very nice atmosphere that, you know, 111 00:04:12,920 --> 00:04:15,155 full of nitrogen and oxygen that we breathe here. 112 00:04:15,155 --> 00:04:18,192 Early Earth's atmosphere was actually formed 113 00:04:18,192 --> 00:04:20,694 from gases that erupted from volcanoes. 114 00:04:20,694 --> 00:04:22,529 - It's important to study volcanoes 115 00:04:22,529 --> 00:04:23,864 no matter where they are, 116 00:04:23,864 --> 00:04:26,333 and thanks to NASA, we know more about volcanoes 117 00:04:26,333 --> 00:04:30,003 on our planet and in our solar system. 118 00:04:30,003 --> 00:04:32,806 Talk about explosive science. 119 00:04:32,806 --> 00:04:34,808 For "Real World," I'm Mishay.