What is a fault line?
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(m)\n\nIn geology, faults are discontinuities (cracks) in the Earth's crust that are the result of differential motion within the crust. Faults are the source of many earthquakes that are caused by slippage vertically or laterally along the fault. The largest examples are at tectonic plate boundaries, but many small faults are known to exist that are far from active plate boundaries.
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What kind of lines ... manufacturing, drawing???\nConcurrent means the same or in agreement, so the lines, whatever type they are either look the same, are running the same or mirror each other in some way.
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Fault level is the current expected to flow into a short circuit at a stated point on a system.\n\nIt is defined as: Fault level = Open-circuit voltage x Short-circuit current [VA/phase]\n\nTry Google Book Search, pal.
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Normal fault: hanging wall moves down relative to the footwall.\n\nReverse fault: hanging wall moves up relative to the footwall.\n\nSorry don't have time to search for fault diagrams...\n\nwriting lesson plans right now\n\nyou really should do your own homework. :P
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Try: http://earthquake.usgs.gov/research/monitoring/anss/ for definitions.
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Depending on the (source + cable) impedance, approx .01 ohms and figuring that this is a 3phase line then:\n\nFault Current is approx 365,000 amps in less than a second.\n\nCheck out the following; Type in Fault Current in search.
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Shear Wave: A wave in which the disturbance is an elastic deformation perpendicular to the direction of motion of the wave. (Shear waves are also called 'transverse waves.')\n\nShear-wave splitting due to the alignment of vertical cracks in the crust has been widely observed in a variety of tectonic settings and data gathering experiments, from earthquake recordings to controlled-source seismic data. It has also been recognized that the polarization of the fast split shear wave is usually parallel to the local strike of cracks (or direction of the maximum horizontal stress), and that the time delay between fast and slow shear waves is closely related to the intensity of crack-induced anisotropy in the medium.\n\nif you wanna see an image of ahear wave aplit then click on the link below.\nhttp://www.missouri.edu/~sandvole/split.html
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Drive Interstate Highway 5 from just south of Gilroy California to L.A. and you'll be right on the fault line. The fault also extends into the Pacific where it meets the bottom of the ocean north of San Fransisco. All of these places are of course in California.
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de·mar·ca·tion also de·mar·ka·tion    ( P )  Pronunciation Key  (dmär-kshn)\nn. \nThe setting or marking of boundaries or limits. \nA separation; a distinction: a line of demarcation between two rock strata. \n \n\ndemarcation\n\nn 1: the boundary of a specific area [syn: limit, demarcation line] 2: a conceptual separation or demarcation; "there is a narrow line between sanity and insanity" [syn: line, dividing line, contrast]
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think about looking at the horizon, its a line that runs from side to side , sky line in the horizon(horizontal line)
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The Geological definition would be a fracture along which there has been displacement relative to one another parallel to the fracture plane
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Apparently, there are fault lines running through New York City (see sources #1 and #2) and throughout upstate New York state (see source #3). \n\nI was surprised about this as well, because I had assumed (incorrectly) that the fault lines were all Western.
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"Fault-block mountains are produced when normal (near vertical) faults fracture a section of continental crust. Vertical motion of the resulting blocks, sometimes accompanied by tilting, can then lead to high escarpments. These mountains are basically formed by the earth's crust being stretched and extended. Tilted blocks are common in the Basin and Range region of the western United States. Level blocks lead to the horst and graben terrain seen in northern Europe. Fault block mountains commonly accompany rifting and are indicators of tensional tectonic forces."
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The dividing line is the use of the scientific method: observation, hypothysis and experiment.\n\nOne of the earliest was Galileo's experiment with falling bodies using the Tower of Pisa.  \n\nSee below.
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Usually a flowline refers to a pipe that transfers fluid from an oil or gas well to a processing facility. It might also transfer fluid from a smaller facility to a larger one with a given oil field. \n\nA pipeline usually refers to a pipe that transfers gas, crude oil, gasoline or other finished product from a processing facility or storage facility to another location be it another processing facility, refinery,  chemical plant or end user
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A fault is merely a fracture in the rock along which movement has occurred.  Faults can occur on the scale of the very small, where you can measure the movement of rock on each side in millimetres, to the very large, such as the san andreas fault in the USA.  Each side of this fault has very different rock to the other as the fault has moved kilometres.  Since the rock within faults has been fractured and broken, it is generally softer than the surrounding rock causing it to preferentially erode.  Landforms such as valleys and rivers quite often follow old faults as a result of this.
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anticlines and synclines are down folds