1 00:00:00,000 --> 00:00:02,000 Hi, we're the Treehouse Detectives. 2 00:00:02,000 --> 00:00:06,000 Dr. D said that you might be able to help us learn about how crustal movement is monitored. 3 00:00:06,000 --> 00:00:09,000 I sure can. I use GPS to measure crustal movements. 4 00:00:09,000 --> 00:00:13,000 I've heard of GPS, but I'm not sure what it is or how it works. 5 00:00:13,000 --> 00:00:16,000 GPS stands for Global Positioning System. 6 00:00:16,000 --> 00:00:19,000 It's a satellite navigation system consisting of 24 satellites. 7 00:00:19,000 --> 00:00:22,000 Pilots and boaters use it to plot their course. 8 00:00:22,000 --> 00:00:26,000 Geologists use it to accurately measure the position of monitoring stations. 9 00:00:27,000 --> 00:00:31,000 Here in Southern California, we have a network of 250 GPS stations. 10 00:00:31,000 --> 00:00:35,000 How does knowing the position of these stations help you to understand earthquakes? 11 00:00:35,000 --> 00:00:39,000 It shows us the stretching, warping, and movement of the crust that's not really noticeable. 12 00:00:39,000 --> 00:00:41,000 How accurate is it? 13 00:00:41,000 --> 00:00:46,000 We can measure the positions of points on the Earth to 3 millimeters horizontally and 7 millimeters vertically. 14 00:00:46,000 --> 00:00:50,000 That's small. How does that differ from what a seismograph does? 15 00:00:50,000 --> 00:00:53,000 A seismograph measures earthquakes when they happen. 16 00:00:53,000 --> 00:00:56,000 With GPS, we can actually measure the quiet motions of the Earth. 17 00:00:56,000 --> 00:01:00,000 That means we can measure the strain buildup as well as the earthquakes themselves. 18 00:01:00,000 --> 00:01:03,000 It is particularly useful in identifying active blind faults. 19 00:01:03,000 --> 00:01:05,000 What's a blind fault? 20 00:01:05,000 --> 00:01:09,000 A blind fault is a break in the crust that doesn't break through the surface anywhere. 21 00:01:09,000 --> 00:01:14,000 Naturally, these faults are not easy to locate or study and might go unnoticed without GPS technology. 22 00:01:14,000 --> 00:01:18,000 That's pretty impressive. I'm glad we have the ability to see these faults. 23 00:01:18,000 --> 00:01:21,000 Would this technology help us to predict earthquakes? 24 00:01:21,000 --> 00:01:25,000 We are integrating data from a lot of different sources into computer simulations. 25 00:01:25,000 --> 00:01:28,000 These simulations should help us understand the earthquake process. 26 00:01:28,000 --> 00:01:31,000 We hope to eventually be able to do short-term forecasting. 27 00:01:31,000 --> 00:01:33,000 Can you give us an example? 28 00:01:33,000 --> 00:01:37,000 By monitoring all the stations, we can find out which faults have the greatest slip rate. 29 00:01:37,000 --> 00:01:43,000 The slip rate, typically measured in millimeters per year, is how fast the two sides of a fault are moving past each other. 30 00:01:43,000 --> 00:01:47,000 These faults that have the greatest slip rates may be the locations of future earthquakes. 31 00:01:47,000 --> 00:01:49,000 I wish you were able to make a prediction now. 32 00:01:49,000 --> 00:01:53,000 Can GPS help us to know if we experience an earthquake in Virginia? 33 00:01:53,000 --> 00:01:58,000 We can use GPS to measure displacements from earthquakes, but we don't measure the shaking part from an earthquake. 34 00:01:58,000 --> 00:02:02,000 A seismometer is used to measure this, and it will be better able to answer your question. 35 00:02:02,000 --> 00:02:04,000 Thank you very much, Dr. Donilon. 36 00:02:04,000 --> 00:02:08,000 You're welcome. Email me if you have any questions, and say hello to Dr. D for me.