MadSci Network: Earth Sciences |
First, let me apologize for taking so long to respond to your question. I was out of town when it arrived and just returned. As far as earthquakes, in general, go, you can have them due to compression, tension, lateral motion, or a combination. You'll see quakes due to compression in places like the Himalaya, where the Indian subcontinent is pushing into Asia and compressing the crust in the collision zone. In these cases, one block of rock will ride up and over another. You see this a lot in most mountain ranges because this is how most mountains form. Tensional faults occur where the crust is pulling apart. This sort of faulting happened, for example, Europe, Africa, and the Americas split apart to form the Atlantic Ocean. Currently we see this sort of faulting in the Red Sea and the African Rift Valley. Lateral movement occurs near what are called transform faults. This is where one tectonic plate is moving alongside another, but the motion takes place in fits and starts. We see this in California, where the western-most part of the state is moving northward on the Pacific Plate and the rest of the state is on the North American Plate. So ground on the west side of the San Andreas Fault is slowly moving to the north in small jumps of a few meters or so at a time. In the case of Turkey, it's in a seismically active area. Typically, as you can guess from the mountains, the stress is compressional because the mountains are still building. For more information about earthquakes and faulting you should try the WWW page of the United States Geological Survey (USGS) at http://www.usgs.gov - they have a lot of good information. You can also try to contact a local college or university (for example, in the Boston area, MIT has some excellent geophysicists) and the USGS may have an office, too.
Try the links in the MadSci Library for more information on Earth Sciences.