1 00:00:00,000 --> 00:00:04,000 Hi, Dr. D. Hi, kids. 2 00:00:04,000 --> 00:00:06,000 Is this the seismograph you're building? 3 00:00:06,000 --> 00:00:08,000 That's right. I'm almost finished. 4 00:00:08,000 --> 00:00:13,000 This seismograph is not very sensitive, but it does work. 5 00:00:13,000 --> 00:00:15,000 It measures horizontal motion. 6 00:00:15,000 --> 00:00:18,000 So you actually use a peanut can and an old brick? 7 00:00:18,000 --> 00:00:21,000 Yeah, sure. Let me start from the beginning. 8 00:00:21,000 --> 00:00:23,000 The seismograph measures the shaking of the Earth. 9 00:00:23,000 --> 00:00:26,000 To measure the shaking, we take advantage of Newton's first law. 10 00:00:26,000 --> 00:00:29,000 I think I remember. Isn't it also called inertia? 11 00:00:29,000 --> 00:00:32,000 I'm impressed. So what is inertia? 12 00:00:32,000 --> 00:00:35,000 It means that when an object is at rest, it stays at rest. 13 00:00:35,000 --> 00:00:37,000 And when an object is in motion, it remains in motion. 14 00:00:37,000 --> 00:00:41,000 That's right. This brick has a lot of inertia, so it's hard to get moving. 15 00:00:41,000 --> 00:00:46,000 When the Earth shakes, the base of the seismograph will also shake. 16 00:00:46,000 --> 00:00:49,000 But the brick, which is not tied to the base, will not. 17 00:00:49,000 --> 00:00:51,000 The can over there records the vibration. 18 00:00:51,000 --> 00:00:53,000 Can we try it? 19 00:00:53,000 --> 00:00:55,000 Sure. Let's make an earthquake by shaking the table. 20 00:00:56,000 --> 00:01:00,000 It really works. Look at the waves. Did we do that? 21 00:01:00,000 --> 00:01:02,000 You sure did. 22 00:01:02,000 --> 00:01:06,000 Here's a different kind of seismograph. It measures vertical motion. 23 00:01:06,000 --> 00:01:09,000 It looks really different. 24 00:01:09,000 --> 00:01:16,000 Because it has inertia, this magnet hanging on the spring tends to stand still when the table moves up and down. 25 00:01:16,000 --> 00:01:20,000 A magnet moving through a coil of wire produces electricity, which this meter records. 26 00:01:20,000 --> 00:01:22,000 Can we try this one too? 27 00:01:22,000 --> 00:01:24,000 Sure. 28 00:01:25,000 --> 00:01:29,000 All right. But here's a sense of the seismometer that hooked up to this computer. 29 00:01:29,000 --> 00:01:33,000 That graph looks a lot like the seismogram that Mr. Lau showed us. 30 00:01:41,000 --> 00:01:45,000 The harder I hit the table, the larger the signal. This is really cool. 31 00:01:45,000 --> 00:01:48,000 And look at how it vibrates up and down. 32 00:01:48,000 --> 00:01:51,000 Because it produces an electric signal, it is easy to amplify. 33 00:01:51,000 --> 00:01:54,000 Even a small vibration can be shown on the computer. 34 00:01:54,000 --> 00:01:57,000 Now, I can't loan you this device. 35 00:01:57,000 --> 00:02:03,000 But why don't you take my wooden seismograph back to the treehouse and see if it can record another tremor? 36 00:02:03,000 --> 00:02:07,000 I have a friend at NASA's Jet Propulsion Laboratory in Pasadena, California. 37 00:02:07,000 --> 00:02:10,000 He uses satellites to measure the motion of the Earth's crust. 38 00:02:10,000 --> 00:02:14,000 You might want to talk to her in your quest to become earthquake experts.