Seismic faults Seismic faults The Alpine Fault is a geological fault, known as a right-lateral strike-slip fault, that runs almost the entire length of New Zealand's South Island. It forms a transform boundary between the Pacific Plate and the Indo-Australian Plate. Earthquakes along the fault, and the associated earth movements, have formed the Southern Alps. ...more on Wikipedia about "Alpine Fault"
The Clarendon-Linden fault system is a major series of fault lines in western New York state, USA. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. ...more on Wikipedia about "Clarendon-Linden fault system"
The Garlock Fault Line is a fault line running approximately northwest- southeast marking the northern boundary of the area known as the Mojave Block, as well as the southern ends of the Sierra Nevada and the valleys of the westernmost Basin and Range province. It intersects the (perhaps better known) San Andreas Fault in Antelope Valley, California. The motion of the Garlock causes deflection in the San Andreas, and deforms it slightly into a curve. The Garlock is the second largest fault in California behind the San Andreas. ...more on Wikipedia about "Garlock Fault"
Geologic faults or simply faults are planar rock fractures which show evidence of relative movement. Large faults within the Earth's crust are the result of shear motion and active fault zones are the causal locations of most earthquakes. Earthquakes are caused by energy release during rapid slippage along faults. The largest examples are at tectonic plate boundaries, but many faults occur far from active plate boundaries. Since faults usually do not consist of a single, clean fracture, the term fault zone is used when referring to the zone of complex deformation associated with the fault plane. ...more on Wikipedia about "Geologic fault"
The Hayward Fault Zone is located in northern California in the San Francisco Bay Area. It is parallel to and east of its more famous (and much longer) sister fault, the San Andreas Fault. To the east of the Hayward Fault lies the Calaveras Fault and beyond that the Clayton-Marsh Creek-Greenvile Fault and their northern and southern extensions via other faults. These four fault structures are the major faults in California at the latitude of San Francisco. ...more on Wikipedia about "Hayward Fault Zone"
The New Madrid Seismic Zone, also known as the Reelfoot Rift or the New Madrid Fault Line, is a major seismic zone located in the Midwestern United States. The New Madrid fault system was responsible for the 1812 New Madrid Earthquake and has the potential to produce damaging earthquakes in coming decades. ...more on Wikipedia about "New Madrid Seismic Zone"
The North Anatolian Fault ( Turkish: Kuzey Anadolu Fayı) is one of the most energetic earthquake zones in the world. Turkey is set on a minor tectonic plate which is being squeezed westwards as the Arabian and the Eurasian plates move together. The North Anatolian Plate is grinding past the two plates at a rate between 1cm and 20cm a year. ...more on Wikipedia about "North Anatolian Fault"
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San Andreas Fault is a geological fault that spans a length of roughly 800 miles (1287 kilometers) through California, United States. The fault, a right-lateral strike-slip fault, marks a transform boundary between the Pacific Plate and the North American Plate. It is well-known for the large and destructive earthquakes that have occurred along it. ...more on Wikipedia about "San Andreas Fault"
The Seattle Fault is a geologic fault in the North American Plate that runs from the Issaquah Alps to Hood Canal in Washington. It passes through Seattle, Washington just south of Downtown and is believed to be capable of generating an earthquake of at least 7.0 on the Richter scale. The Seattle Fault therefore has the potential to cause extensive damage to the city, as much of Pioneer Square and the Industrial District is built on fill, as is the downtown waterfront, which is supported by the Alaskan Way Seawall. ...more on Wikipedia about "Seattle Fault"
Þingvellir ( Icelandic " Þing": parliament, "vellir": plains) is a place in the southwest of Iceland near the peninsula of Reykjanes and the Hengill volcanic area. ...more on Wikipedia about "Þingvellir"
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