strike-slip faults where they move laterally
247 faults or fault systems as of December 30, 2008.
features
The movement of the Pacific and North American plates produced California's major geological features. These features include faults, volcanoes, mountain ranges, and basins.
one is the San Andreas Fault in California.
Deep furrows in the ground or ocean floor are faults. San Andreas fault in California is a prime example, having displacement hundreds of kilometers long. Two kinds of faults are dip-slip faults and strike-slip faults.
Geological faults are planar fractures. More information can be found on sites such as Wikipedia, as well as the California Geological Survey website.
Deep furrows in the ground or ocean floor are faults. San Andreas fault in California is a prime example, having displacement hundreds of kilometers long. Two kinds of faults are dip-slip faults and strike-slip faults.
Transform boundaries produce strike-slip faults. These faults occur when two tectonic plates slide past each other horizontally. Examples of transform boundaries include the San Andreas Fault in California.
No, California will not sink into the ocean. While some parts of California are at risk of flooding due to rising sea levels and potential earthquakes, the entire state sinking into the ocean is not a realistic scenario.
Perhaps the most famous is the San Andreas fault in California in the US.
There are many faults in California. The two most significant faults are the San Andreas Fault and the Hayward Fault.
Transform boundaries like the one on the California cost cause strike slip faults. As the two plates move in opposite direction the earthquake occurs.