What did the 125th street fault line effect?
Some landforms associated with the San Andreas Fault include valleys (like the Carrizo Plain), mountains (such as the Tehachapi Mountains), and hills (like the Santa Cruz Mountains). These landforms result from the movement of tectonic plates along the fault line.
The largest and most famous earthquake fault in California is the San Andreas fault. It is 800 km long. It is significant because it runs through a heavily populated area (Los Angeles) and it is likely to do very serious damage some day. The San Andreas fault is a transform fault.
in addition to the concise answers given above, fault could also be recognize in sedimentary terrain from; OMISSION OF STRATA, REPETITION OF STRATA AND ABRUPT CHANGE IN MORPHOLOGY OF ON EARTH SURFACE .
The San Andreas Fault is a strike-slip fault where the motion is mainly horizontal, with the two sides moving past each other horizontally. It is a transform boundary between the Pacific Plate and the North American Plate.
The fault that caused the 1906 San Francisco earthquake has an estimated length of about 296 miles (477 km). Scientists determined this information by studying the surface rupture, seismic waves, and geologic features left behind by the earthquake, combined with geological mapping and trenching techniques along the fault trace.
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The San Andreas fault line was first identified in 1895 by Professor of geology Andrew Lawson. The San Andreas fault is approximately 800 miles long.
It depends on what subway line is closest to your starting point. The address 59 Canal Street is between Allen and Orchard Streets. If you're starting out on the B or D trains (of the B-D-F-M, the orange line), then take the Downtown B or D to Grand Street (at Chrystie Street). Then walk 2 blocks south on Chrystie Street to Canal Street: Grand Street ---> Hester Street ---> Canal Street. Turn left onto Canal, and walk 3.5 blocks east on Canal to #59. If you're starting out on the 4-5-6 (the dark green line), then take the Downtown 4, 5 or 6 to 14th Street-Union Square, and transfer there to the Downtown N-R-Q (the yellow line). Take the Downtown N, R or Q to Canal Street (at Lafayette Street). Then walk 10.5 blocks east on Canal to #59. They're short blocks, so this is not a long walk. The first block you should reach after Lafayette Street is Centre Street. If you walk 1 block and find yourself at Crosby Street, then you're going west, not east. If you're starting out on the 6 train, then you may wish to transfer to the 4 or 5 at 125th Street. The 6 is a local train, while the 4 and 5 are express, so you'll skip 10 local stops between 125th and 14th-Union Square.
In New York City, approximately 17 to 20 street blocks (north/south blocks) equals a mile, and about 5 to 10 avenue blocks (east/west blocks) equals a mile (the length of the avenue blocks varies considerably, depending on what neighborhood you're in. In Midtown, it's about 10 avenue blocks to a mile, but there are some avenue blocks on the Upper West Side that are close to half a mile long). So, it's approximately 3 miles straight north from 67th to 125th Street in Manhattan.
It is believed that the largest fault line is the San Andreas Fault in California, which is approximately 800 miles long and extends through much of the state. This fault is known for its ability to produce major earthquakes due to the movement of the tectonic plates along it.
According to wikipedia, the San Andreas Fault is roughly 810 miles long running partially through Baja California, Mexico.
It is in the Philippines, the countries main fault line. It runs from Sierra Madre to Tagaytay City. The Philippino fault system is a series of faults, most strips are long and narrow like the Zambales ophiolites which is at least 400 kms long
The largest fault line in the world is the Pacific Ring of Fire, which is approximately 40,000 kilometers long. It encircles the Pacific Ocean and is known for its frequent seismic and volcanic activity.
Impedance relays for transmission line fault detection can have several disadvantages. They are prone to misoperation during system changes, such as load variations or line outages, which can lead to incorrect fault detection. Additionally, their performance can be affected by the presence of series compensation or long transmission lines, where the measured impedance may not accurately represent the fault location. Finally, they may not effectively distinguish between different fault types, leading to challenges in selective tripping.
The Elysian Park fault is a fault that lies in the Los Angeles Basin. The fault is ten miles wide by twenty miles long.
A parade with a marching band or the holocaust all over again.
Yes, a country that is not on a fault line can still experience earthquakes. These earthquakes can be caused by other geological processes, such as volcanic activity, or by human activities like mining or reservoir-induced seismicity. Additionally, seismic waves can travel long distances and cause shaking in regions far from where the earthquake originated.