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There are some earthquakes that are so slow they are almost ceptable, but important when they happen. So canly tell us about why they're so slow? Absolutely. In the year two thousand we discover a new type of false slip style called slow slip. They've been detected at lots of places around the world, not just it subduction zones and other fault areas. We see them in greece too as well as elsewhere on Earth. What does it mean for scientists to get rid of these types of faults by using technology like Google's G p s networks? The answer is pretty simple: It means you don't have to go very far out into the subsurface or
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