By Robert Roy Britt, explorezone.com . 11.30.99
A new space-based technique for mapping earthquakes views Earth's surface from an angle, instead of from directly above, to map horizontal movement as little as a few millimeters. The resulting data are critical to understanding what the ground under your feet might do in the future.
When an earthquake strikes, seismologists use myriad tools and techniques to map the displaced fault and glean clues about whether the temblor might have added or removed stress to adjacent faults -- all hints of possible future seismic activity.
The new method overcomes limitations of the Global Positioning System, which requires ground sensors coupled with satellites to measure movement in selected spots. With GPS subtle but important changes can go unnoticed.
The emerging satellite technique is fast improving how researchers review an earthquake. The novel approach is all in the angle of view. Satellite-based radar can already accurately measure altitude differences from above -- a vertical component seen from directly overhead. By changing the angle of view to 23 degrees off vertical, adding the element of time, and then applying a little math, researchers can see how far the ground moved horizontally during an earthquake.
When a magnitude 7.1 earthquake moved the ground in Southern California
on Oct. 16 this year, two plates of Earth's crust slid past each other
in what researchers call a strike-slip fault. Like cars on a road moving
in the opposite direction, the two plates moved a total of 17 feet
in relation to each other -- each plate moving roughly half that distance.
Traditional methods can measure the overall movement, but undetectably
small variations at critical points can reveal important information about
what the fault might do next, or what adjacent faults might do, Peltzer
said. Stress and strain builds and recedes in neighboring faults each time
a surrounding batch of rock snaps under the pressure of Earth's continuously
moving plates.
informatin adapted from Satellites Get a New Angle on EarthQuakes