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The Brevard Fault Zone is a part of a much larger system of faults at the base of the Appalachian thrust sheet [1] that played a key role in uplifting the Appalachian Mountains. The extent of its role remains uncertain because most of the fault is buried beneath Quaternary sediment. [ 7 ]
Normal fault: Longmen Shan Fault: Sichuan, China: Thrust fault: Active: 2008 Sichuan (M8.0) Lost River Fault: Idaho, United States: Normal: Active: 1983 Borah Peak (M6.9) Lusatian Fault: Germany: Thrust fault: Macquarie Fault Zone >400: South Pacific Ocean: Fault (geology)#Strike-slip faults: Active: 1989 Maquarie Isl. (8.2), 2008 Macquarie ...
A newly discovered fault line shows why New York City was hit harder by an April earthquake than its epicenter in New Jersey. This discovery could really shake up the Big Apple.
The New Madrid seismic zone (NMSZ), sometimes called the New Madrid fault line (or fault zone or fault system), is a major seismic zone and a prolific source of intraplate earthquakes (earthquakes within a tectonic plate) in the Southern and Midwestern United States, stretching to the southwest from New Madrid, Missouri.
The 800-mile San Andreas Fault is one of the largest fault lines in the world. ... ancient Lake Cahuilla affected the fault line, and discovered two primary impacts. First, ...
--in Nashville notation, the chord chart for both would be notated as 1 4 5 1. By convention, Nashville notation eliminates the slashes and bar lines that denote the beats in the measure: "With the number system it’s understood that each number written on your chart is given the value of one measure of music. In 4/4 time, that’s a total of ...
A fault off the Pacific coast could devastate Washington, Oregon and Northern California with a major earthquake and tsunami. Researchers mapped it comprehensively for the first time.
The earthquake lasted between 25 and 30 seconds and had an estimated magnitude of 6.75 on the surface-wave magnitude scale. The calculated focal mechanism is consistent with slightly oblique dextral (right lateral) strike-slip on a NW-SE trending fault plane, matching the orientation of other fault planes measured in the area and a marked bathymetric lineament.