The Berw Fault is a SW NE trending Fault geology fault in North Wales . It forms part of the Menai Straits fault System, with the Dinorwic Fault and the Aber Dinlle Fault . It has a long history of movement with early ductile fabrics preserved from a sinistral left lateral strike slip sense shear zone active at the end of the Precambrian and in to the early Cambrian . Any Caledonian deformation is unclear but the fault zone was reactivated in the Carboniferous as a NW throwing normal fault with Reflection seismology seismic reflection data showing the formation of a Graben Half graben half graben in its hanging wall. There are no indications of inversion during the Variscan Orogeny , but the fault was reactivated in a normal sense during the Permian and Triassic and again during the Cenozoic with a sinistral strike slip sense. ref name Tim cite journal last Needham first T. coauthors Morgan R. year 1997 title The East Irish Sea and adjacent basins new faults or old? journal Journal of the Geological Society volume 154 issue 1 pages 145 150 doi 10.1144 gsjgs.154.1.0145 url http jgs.lyellcollection.org cgi content abstract 154 1 145 accessdate 18 December 2010 ref See also List of geological faults of Wales References Reflist coord 53.22 4.34 display title Category Geology of Wales geology stub Wales geo stub ... more details
The Serra Fault is the northernmost Fault geology fault in a zone of northwest striking range front thrust faults adjacent to and northeast of the San Francisco Peninsula segment of the San Andreas Fault , in eastern San Mateo County, California San Mateo County , California . ref name kennedy Kennedy, 2005 . ref The Serra Fault is positioned approximately convert 1.5 3 km mi sp us northeast of the San Andreas Fault moreover the Serra Fault extends for more than convert 20 km mi abbr on from Hillsborough, California the town of Hillsborough to a point near Daly City, California Daly City . Serra geology According to Kennedy Three angular unconformities within the Merced and overlying Colma Formation s have formed on the steeply dipping fold forelimb . ref name kennedy Mid to later Holocene fluvial channel deposits inset into the Merced Formation along the forelimb of the fold seem to be deformed, illustrating that the folding is active. The Serra Fault is a low angle imbricate fault that has ... Formation. The Serra Fault was originally zoned as potentially active by the State of California ref California, 1974 ref under the mandated special studies for surface fault rupture. 1980s studies ... the Serra Fault is lacking. ref Earth Metrics, 1989 ref The Serra Fault is, therefore, not zoned for Special Studies by the State of California and is classified as Quaternary in age that is, fault ..., generating uncertainty about the depositional history of these units as well as the timing of fault ... deposits, as well as younger Holocene inset channel deposits, show fault propagation fold growth and tilting related to activity on the Serra Fault itself. ref Yi, 2005 ref See also Crystal Springs Reservoir Hillside Fault Reference notes Reflist Kennedy, Drew G., LATE PLEISTOCENE TO HOLOCENE FOLD GROWTH ABOVE THE SERRA FAULT, NORTHERN SAN FRANCISCO PENINSULA, CALIFORNIA , Sanders & Associates ..., Special Studies Zone Serra Fault , 1974 Sacramento, California Earth Metrics, 1989 Marc. Papineau ... more details
The Tintina Fault is a large fault geology strike slip fault in western North America , extending from northwestern British Columbia , Canada to the U.S. state of central Alaska . It represents the northern extension of the Rocky Mountain Fault in the northern United States . ref http www.blm.gov pgdata etc medialib blm ak jrmic usbm rpts.Par.31547.File.tmp OFR 88 78.pdf Mineral deposits of the Tanana Yukon Uplands A Summary Report ref See also Denali Fault Rocky Mountain Trench Northern Cordilleran Volcanic Province References reflist coord missing British Columbia Faults Category Seismic faults of Canada Category Seismic faults of the United States Category Geology of British Columbia Category Geology of Yukon Category Geology of Alaska BritishColumbia geo stub Yukon geo stub Alaska geo stub Geology stub ... more details
Oaxaca Fault lang es Falla de Oaxaca is a seismic fault that runs near Oaxaca, Oaxaca Oaxaca city, Oaxaca , Mexico . It runs north on the east side of the city from Etla Valley . Donaji Fault is a nearby fault that runs roughly perpendicular to Oaxaca Fault at its southern end. ref http redalyc.uaemex.mx pdf 568 56840401.pdf ref References reflist External links http redalyc.uaemex.mx pdf 568 56840401.pdf Geofisica International Univserity Autonoma de Mexico Central America plates Category Geology of Mexico Category Seismic faults ... more details
Image Fault breccia Keystone Thrust Red Rock Canyon NV.jpg thumb right Fault breccia of the Keystone Thrust, Red Rock Canyon National Conservation Area , Nevada. Fault breccia IPAc en icon b r t i or IPAc en b r i Italian for breach , or tectonic breccia , is a breccia a rock geology rock type consisting of angular clast s that was formed by tectonics tectonic forces. Fault breccia is a tectonite formed by localized zone of brittle deformation a fault geology fault zone in a rock. Origin Fault breccias are tectonites formed primarily by tectonic movement along a localized zone of brittle deformation a fault geology fault zone in a rock formation or province. The grinding and milling occurring when the two sides of the fault zone moving along each other results in a material that is made of loose fragments. Because of this fragmentation fault zones are easily infiltrated by groundwater . Secondary minerals such as calcite , epidote , quartz or talc can precipitation chemistry precipitate from the circulating groundwater filling the voids and cementing the rock. However, when the tectonic movement along the fault zone continues the cement itself can be fragmented leading to a new gouge material containing neoformed clasts. Deeper in the Earth s crust geology crust , where temperatures and pressures are higher, the rocks in the fault zone can still brecciate, but they keep their internal cohesion. The resulting type of rock is called a cataclasite . Properties Fault ... type, unless cementation took place at a later stage. Sometimes a distinction is made between fault gouge and fault breccia, the first has a smaller grain size . ref Twiss, R.J. & Moores, E.M., 2000 6th edition Structural Geology , W.H. Freeman & co, ISBN 0 7167 2252 6 p. 55 ref Zones of fault breccia and fault gouge in rocks can be a hazard for the construction of tunnel s and Mining mines , as the non ... Breccia Cataclasite Fault geology References reflist 30em Category Rocks Category Tectonics Category ... more details
Unreferenced auto yes date December 2009 A fault model is an engineering model of something that could go wrong in the construction or operation of a piece of equipment. From the model, the designer or user can then predict the consequences of this particular fault. Fault models can be used in almost all branches of engineering. Basic fault models in digital circuit s include the stuck at fault model. A signal, or gate output, is stuck at a 0 or 1 value, independent of the inputs to the circuit. the bridging fault model. Two signals are connected together when they should not be. Depending on the logic circuitry employed, this may result in a wired OR or wired AND logic function. Since there are O n 2 potential bridging faults, they are normally restricted to signals that are physically adjacent in the design. The open fault model. Here a wire is assumed broken, and one or more inputs are disconnected from the output that should drive them. As with bridging faults, the resulting behavior depends on the circuit implementation. The delay fault model, where the signal eventually assumes the correct value, but more slowly or rarely, more quickly than normal. A fault model in an Aerospace context is a set of structured information which helps users or systems to identify and isolate a problem that occurs on an engine, Line replaceable unit LRU , or Auxiliary power unit APU during a flight. Associated with this fault model may be a suggested repair procedure along with references to Aircraft maintenance manuals Light maintenance manual . See also Automatic test pattern generation Single Stuck Line Fault coverage DEFAULTSORT Fault Model Category Digital electronics Category Electronic design Engineering stub de Fehler in elektronischen Schaltungen fr Mod le de faute ... more details
Unreferenced date December 2009 Merge Single stuck line date February 2010 A stuck at fault is a particular fault model used by fault simulators and automatic test pattern generation ATPG tools to mimic a manufacturing defect within an integrated circuit . Individual signals and pins are assumed to be stuck at Logical 1 , 0 and X . For example, an output is tied to a logical 1 state during test generation to assure that a manufacturing defect with that type of behavior can be found with a specific test pattern. Likewise the output could be tied to a logical 0 to model the behavior of a defective circuit that cannot switch its output Not all faults can be analyzed using the stuck at fault model. Compensation for static hazards, namely branching signals, can render a circuit untestable using this model. Also, redundant circuits cannot be tested using this model, since by design there is no change in any output as a result of a single fault. See also Design For Test Single stuck line DEFAULTSORT Stuck At Fault Category Digital electronics Category Electronic design automation ... more details
Image Flat eq map anotated.png thumb right 300px Map showing major faults in the San Francisco Bay Area The Maacama Fault is a right lateral moving dextral geologic fault located in the Pacific Coast Ranges Coast Ranges of northwestern California . It is considered to be the northernmost segment of the Hayward Fault subsystem of the San Andreas Fault zone. Aseismic creep Creep along the Maacama is about 8 mm per year, consistent with the steady movement along the rest of the Hayward Fault system. It is also capable of producing large earthquakes. ref cite web title Paleoseismic Investigation Of The Maacama Fault At The Haehl Creek Site, Willits, California author LARSEN, Mort, PRENTICE, Carol S., KELSEY, Harvey M., ZACHARIASEN, Judith, and ROTBERG, Gabriel L. url http gsa.confex.com gsa 2005CD finalprogram abstract 85295.htm accessdate 12 December 2008 date 2005 publisher The Geological Society of America ref The Maacama Fault runs just east of Ukiah, California Ukiah and just west of Willits, California Willits . References reflist http gldims.cr.usgs.gov webapps cfusion Sites qfault qf web search res.cfm USGS Database Maacama Fault http www.storage.water.ca.gov docs o reg geo plate faulting.pdf storage.water.ca.gov geo plate faulting California Faults Category Seismic faults of California Category Natural history of Sonoma County, California Category Natural history of Mendocino County, California ... more details
The Christchurch Fault is an active fault active seismic fault running under the city of Christchurch in the middle of New Zealand s South Island . It runs from an area close to Riccarton, New Zealand Riccarton , under the Christchurch Central City Central City , through the eastern suburbs off the coast of New Brighton, New Zealand New Brighton . It runs parallel to the more destructive Port Hills Fault that lies 5 km to the south of the Christchurch Fault. ref name Stuff.co.nz 4819335 cite news url http www.stuff.co.nz national christchurch earthquake 4819335 Second Christchurch fault much better behaved title Second Christchurch fault much better behaved last Gorman first Paul date 29 March 2011 newspaper The Press accessdate 24 September 2011 ref The Christchurch fault is believed to have been responsible for a series of earthquakes that rocked the city on Boxing Day of 2010. It may have been responsible for a 1869 Christchurch earthquake moderate earthquake that shook the city in 1869. ref cite web title 5 JUNE 1869 CHRISTCHURCH EARTHQUAKE url http www.geonet.org.nz content download 5878 26262 file geonet news issue 2 feb 03.pdf publisher Geonet accessdate 20 October 2011 page 5 format PDF month February year 2003 ref References reflist colwidth 30em Seismic faults of New Zealand Category Seismic faults of New Zealand ... more details
Image Closeup of Grand Tetons.JPG thumb East face of the Teton Range. The Teton fault is located at the base of these mountains. The Teton fault is a normal fault located in northwestern Wyoming . The fault ... movement on the fault has caused the dramatic topography of the Teton Range. ref name Byrd Byrd, J.O.D., Smith, R.B., Geissman, J.W. 1994 The Teton fault, Wyoming Topographic signature, neotectonics ... The Teton fault is located in a unique geologic setting. The fault is on the boundary of four major .... This province adds tension perpendicular to the fault line causing the fault blocks to move apart. The Idaho Wyoming Thrust belt is located south of the Teton fault and is a region of thick and deformed crust that prevents the fault from extending farther south. The Rocky Mountain Foreland is located east of the Teton fault and is a region of thicker crust. This section of crust is heavier and adds to the vertical downward force on the hanging wall of fault. The Yellowstone volcanic plateau ... fault. ref name Byrd The Teton fault is unique in that it strike and dip dips or slopes to the east ... fault can be explained by the subsidence of the Snake River Plain . The Snake River Plain is located to the west of the Teton fault and was formed by the migration of the Yellowstone caldera across southern Idaho. As this section of crust cools it tends to subside causing the footwall of the fault to tilt down toward the west. ref name Byrd ref name Pickering The Teton fault is also an important ... name Smith Smith, R.B., Byrd, O.D., 1993 . The Teton fault, Wyoming seismotectonics, Quaternary history ... 667. ref Geologic history The development of the Teton fault has been influenced by many past geologic ... province beginning 20 17 million years ago. ref name Smith The age of the Teton fault is somewhat ... on the fault occurred within the last 2 million years. ref name Pickering ref name Smith Rates of movement on the fault have changed throughout time. At the end of the Pinedale glaciation ... more details
The Hosgri Fault also Hosgri Fault Zone , San Gregorio Hosgri Fault Zone is an offshore fault geology fault zone located near the Central Coast of California in San Luis Obispo County, California San Luis Obispo County . The main fault stretches for about convert 140 km mi sing on , and the coastal communities closest to it are Cambria, California Cambria , San Simeon, California San Simeon and Morro Bay, California Morro Bay , Baywood Los Osos, California Baywood Park Los Osos , and Avila Beach, California Avila Beach . ref name SCEDC http www.data.scec.org fault index hosgri.html Hosgri Fault .... 12 Oct. 2009. ref The fault system including branches is some 420 km long, and is a right lateral strand of the San Andreas fault system. ref http gsa.confex.com gsa 2010CD finalprogram abstract 173206.htm Geological Society of America STRUCTURAL ANALYSIS OF THE SAN SIMEON FAULT ZONE, CALIFORNIA IMPLICATIONS FOR TRANSFORM TECTONICS ref Fault Information The Hosgri Fault is a component of the San Andreas Fault system. ref Graham, S. A., and W. R. Dickinson. Evidence for 115 Kilometers of Right Slip on the San Gregorio Hosgri Fault Trend. Science 199.4325 1978 179 181. Print. ref Its movement is primarily reverse thrust fault thrust , as well as exhibiting right lateral slip, and is thought ... Lompoc earthquake magnitude 7.1 is thought to have occurred on this fault. ref http www.data.scec.org ... ref Seismology Seismologists monitor activity on the Hosgri fault constantly because of its physical proximity to the nuclear Diablo Canyon Power Plant . In fact, the fault lies only 2 miles offshore ... 214.4520 1981 528 529. Print. ref More recently in 2008, yet another even closer fault was discovered, the Shoreline Fault 1 mile from the NPP. Coord 35 07 N 119 39 W source enwiki plaintext parser display title References reflist California Faults DEFAULTSORT Hosgri Fault Category Seismic faults ... Andreas Fault sk San Andreas sh Rasjed San Andreas fi San Andreasin siirros sv San Andreasf rkastningen ... more details
Image Guatemala1976EarthquakeMap.jpg thumb right 250px Motagua fault The Motagua Fault also, Motagua Fault Zone is a major, active left lateral moving transform fault which cuts across Guatemala , continuing offshore along the southern Pacific coast of Mexico , returning onshore along the southernmost tip of Oaxaca , then continuing offshore until it merges with the Middle America Trench near Acapulco . It forms part of the tectonic boundary between the North American Plate and the Caribbean Plate . It is considered the onshore continuation of the Cayman Trench which runs under the Caribbean Sea . The Motagua Fault is regarded by some geologists as part of a system of faults designated the Motagua Polochic system rather than as a discrete single boundary. The Chixoy Polochic Fault Polochic fault also referred to as the Chixoy Polochic Fault lies north and parallel to the Motagua Fault and shares some of the motion between the North American and Caribbean Plates. The Motagua Fault has been responsible for several major earthquakes in Guatemala s history, including the one which occurred on February 4, 1976. ref http earthquake.usgs.gov regional world events 1976 02 04.php Historic Earthquakes Bot generated title ref See also Chixoy Polochic Fault Guatemala 1976 earthquake Earthquakes in Guatemala References reflist External links http search.datapages.com data doi 10.1306 A1ADD9A1 0DFE 11D7 8641000102C1865D Datapages, Volume 28 1978 http libraryphoto.cr.usgs.gov cgi bin show picture.cgi?ID ID. 20GUATEMALA 20EARTHQUAKE 2052ct USGS Map coord missing Guatemala Central America plates Category Earthquakes in Guatemala Category Geographic areas of seismological interest Category Seismic faults of Guatemala de Motagua Polochic Verwerfung es Falla de Motagua lt Motagvos l is ... more details
every 350 years somewhere along one of the central segments of the Wasatch Fault. The segments that underlie ... segments around 2,100 years ago. Experts note that the fault is overdue for another major earthquake ... in the region have been undergoing extensive seismic retrofitting , reservoirs on the fault have ... acts as quicksand . An earthquake on the Wasatch Fault could severely damage gas, electric, water ... Utah Geological Survey Public Information Series 40 The Wasatch Fault http uk.youtube.com watch?v owJ6bbHou8I Utah Geological Survey presentation about the fault Utah Faults Category Geology of Utah ... more details
The Atacama Fault is major geological fault in Chile an Atacama desert that runs a length of roughly 800 km in a north south direction and exhibits current seismicity. The fault extends roughly from Iquique in the north to Copiap in the south. Parts of the Chile Highway 5 Pan American Highway run trough the main trace of the fault. coord missing Chile Category Seismic faults of Chile Category Geography of Atacama Region Category Geography of Antofagasta Region Category Geography of Tarapac Region tectonics stub Chile geo stub Tectonics of South America ... more details
nihongo Fuk zu Fault Fuk zu Dans is a fault in Aichi Prefecture of Japan, which was responsible for the 1945 Mikawa earthquake . It extends some 28 km 10 km submarine to Nishio City. ref http www.journalarchive.jst.go.jp english jnlabstract en.php?cdjournal zisin1948&cdvol 25&noissue 1&startpage 44 ref It flows into the Yokosuka fault which extends another 20 km. External links http www.kyouiku.nrc.gamagori.aichi.jp mikawajisin wasureji htm photo photo04c.htm Fukozu Fault pic References reflist East Asia plates Category Seismic faults of Japan Category Geography of Aichi Prefecture ja ... more details
Wikify date April 2012 context date November 2011 A bridging fault consists of two signals that are connected when they should not be. Depending on the logic circuitry employed, this may result in a wired OR or wired AND logic function. Since there are O n 2 potential bridging faults, they are normally restricted to signals that are physically adjacent in the design. References http books.google.com books?id JeMz2QOtjUIC&pg PA3 Bridging Fault Model from Test and Diagnosis for Small Delay Defects http books.google.com books?id XmVJGbl4O3wC&pg PA67 Bridging Fault from Integrated circuit test engineering modern techniques http docs.lib.purdue.edu cgi viewcontent.cgi?article 1012&context ecepubs A bridging fault model where undetectable faults imply logic redundancy from Design Automation and Test in Europe Category Electronic engineering ... more details
Urasoko fault nihongo Urasoko Dans or Urasoko fault system is a seismic fault system running for 39 kilometers near Tsuruga , Japan. Combined with the faults of the system, there are an additional 25 km of faults. It is notable in that it runs beneath a nuclear power plant, Tsuruga Nuclear Power Plant . It was determined that it is capable of triggering a 7.4 magnitude quake. ref cite web url http mdn.mainichi.jp mdnnews news 20120306p2g00m0dm081000c.html title Fault under Tsuruga nuclear plant could trigger M7.4 quake research The Mainichi Daily News publisher Mdn.mainichi.jp date accessdate 2012 03 08 ref References reflist East Asia plates Category Seismic faults of Japan ... more details
Unreferenced date December 2009 about the CPU error the tennis term serve tennis On the x86 architecture, a double fault exception occurs if the central processing unit processor encounters a problem while trying to service a pending interrupt or Exception handling exception . An example situation when a double fault would occur is when an interrupt is triggered but the segment in which the interrupt handler resides is invalid. If the processor encounters a problem when calling the double fault handler, a triple fault is generated and the processor shuts down. As double faults can only happen due to kernel computing kernel bugs, they are rarely caused by user space programs in a modern protected mode operating system , unless the program somehow gains kernel access some virus computing virus es and also some low level DOS programs . Other processors like PowerPC or SPARC generally save state to predefined and reserved machine registers. A double fault will then be a situation where another exception happens while the processor is still using the contents of these registers to process the exception. SPARC processors have four levels of such registers, i.e. they have a Register window 4 window register system . See also Triple fault DEFAULTSORT Double Fault Category Computer errors Category Central processing unit ... more details
Use dmy dates date September 2011 The Chaman Fault is a major, active Fault geology geological fault ..., primarily Transform fault transform , Sinistral and dextral left lateral strike slip fault. The slippage rate along the Chaman fault system as the Indo Australian Plate moves northward relative ... transform aspect, the Chaman fault system has a Convergent boundary compressional component as the Indian ... Survey ref From the south, the Chaman fault starts at the triple junction where the Arabian ... Coast of Pakistan. The fault tracks northeast across Balochistan Pakistan Balochistan and then north ... lateral slip Herat fault, up to where it merges with the Pamir fault system north of the 38 parallel. ref Fig.2 Chaman fault System associated with Indian Plate Boundary April 2008 http www.neduet.edu.pk Civil 2008 1.pdf Chaman Fault System CFS a Prominent Seismo tectonic Feature In Pakistan Cowasjee ... are often included as part of the Chaman fault system. South of the triple junction, where the fault ... Zone . While there is general agreement that the fault is slipping at a rate of at least 10 mm yr ..., T. 1992 Chaman fault, Pakistan Afghanistan In Bucknam, R. C. and Hancock, P. L. eds. 1992 ... 223 ref Offsets have been described throughout the fault in Pakistan that are young enough that only ... and Nakata, T. 1992 Chaman fault, Pakistan Afghanistan In Bucknam, R. C. and Hancock, P. L. eds. 1992 ... of the compressional plate boundary and are aligned parallel to the Chaman fault movement. The fault itself is west of these ranges. Significant earthquakes along the fault 1505, 5 July or 6th An earthquake created a 60 km long surface rupture along a transverse fault in the Chaman system with several meters of vertical offset. This transverse fault is sometimes called the Paghman fault. ref ... w math 1935 Balochistan earthquake along the Ghazaband portion of the fault system killed upwards of 35,000 ... amount of vertical slip as the eastern wall of the fault dropped down. ref Yeats, R. S. Lawrence ... more details
File TibetanPlateauTectonics.png thumb 280px Tectonic map of the Tibetan Plateau showing location of the Kunlun fault The Kunlun fault is a strike slip fault to the north side of Tibet . Slippage along the convert 1500 km long fault has occurred at a constant rate for the last 40,000 years. This has resulted in a cumulative offset of more than convert 400 m . ref cite web title The Kunlun Fault url http earthobservatory.nasa.gov IOTD view.php?id 871 work Earth Observatory publisher NASA date 2000 10 10 accessdate 2010 04 15 ref The fault is seismically active, most recently causing the moment magnitude scale magnitude 7.8 2001 Kunlun earthquake . ref name Klinger cite journal last Klinger first Y. coauthors Xu X., Taponnier P., Vand der Woierd J., Lasserre C. & King G. year 2005 title High Resolution Satellite Imagery Mapping of the Surface Rupture and Slip Distribution of the Mw 7.8, 14 November 2001 Kokoxili Earthquake, Kunlun Fault, Northern Tibet, China journal Bulletin of the Seismological Society of America volume 95 issue 5 pages 1970 1987 doi 10.1785 0120040233 url http www.ipgp.fr king DownloadsVarious 2005 KlingerBSSA2005.pdf accessdate 15 June 2010 Dead link date October 2010 bot H3llBot ref References reflist BR regional geology stub Category Geology of Tibet Category Geology of China ... more details
Image Tanna Fault in Japan 2010 May.jpg right thumb 200px Tanna Fault surface rupture File Tanna Fault 20120325.jpg thumb 200px Ravine of Tanna Fault viewed from N nihongo Tanna Fault Tanna Dans is a left lateral fault which runs along the northeast side of Izu Peninsula south 30 km to Izu, Shizuoka Izu City. It was responsible for the 1930 North Izu earthquake, magnitude 7.0 Kita Izu Earthquake ja . ref http www.bssaonline.org cgi content abstract 69 5 1343 Seismological Society of America Static and dynamic parameters of the Izu Oshima, Japan earthquake of January 14, 1978 ref References reflist External links http www.town.kannami.shizuoka.jp hp page000001300 hpg000001270.htm Kannami official website Japanese http sk01.ed.shizuoka.ac.jp koyama public html tanna tanna.html Masato Koyama s Home Page Shizuoka University Japanese Commonscat Tanna Fault East Asia plates coord 35 05 47 N 139 01 04 E source kolossus jawiki display title Category Seismic faults of Japan ja ... more details
Image Neodani fault.JPG thumb right 250px This fault can be seen as a step portion in the center of the photo. nihongo Neodani Fault Neodani Dans is a left lateral slip fault in Central Japan, Gifu Prefecture, which ruptured causing the 1891 Mino Owari earthquake Otherwise known as the Nobi Earthquake in 1891. It caused a 6m vertical offset and 8m left lateral offset, and ruptured over 80 km. ref http mahabghodss.net NewBooks www web digital nashrieh bssa 2008 BSSA 20 20Oct 202008 20 Vol. 2098 20, 20Issue 205 20 6 2170.pdf ref The quake was the largest ever recorded in inland Japan. External Sites http www.glgarcs.net topics neodani.html Neodani fault & museum http mahabghodss.net NewBooks www web digital nashrieh bssa 2008 BSSA 20 20Oct 202008 20 Vol. 2098 20, 20Issue 205 20 6 2170.pdf Long Term Seismic Behavior of a Fault Involved in a Multiple Fault Rupture Insights from Tectonic Geomorphology along the Neodani Fault, Central Japan References reflist East Asia plates coord 35 37 00 N 136 37 11 E source kolossus jawiki display title Category Seismic faults of Japan ja ... more details
File Cobequid fault zone near Clarke Head.JPG thumb 260px Part of the Cobequid fault zone exposed in cliffs to the west of Clarke Head, near Parrsboro , Nova Scotia , juxtaposing Lower Carboniferous Windsor Group against Upper Triassic to Lower Jurassic Blomidon group . The Cobequid Fault is a fault that is the extension of the Chedabucto Fault . This fault runs from Truro, Nova Scotia Truro to Cape Chignecto south of the Cobequid Hills . Both the Cobequid fault and the Chedabucto Fault form the Minas Fault zone splitting Nova Scotia into the Avalon Zone and the Meguma Zone. Movement on the Cobequid Fault started before 400 million years ago and end around 40 million years ago. Between that time around 350 million years violent volcanic eruptions at Spicers Cove north Cape Chignecto Provincial Park and 50 Million years after Grey sandstone rich in fossil plants were deposited. At Five Islands Provincial Park at Red Rocks there are red rocks formed by the large accumulation of mud, sand and gravel around 210 Million years ago. References http gsc.nrcan.gc.ca marine scotianmargin go e.php Geology of the Scotian Margin http www.capechignecto.net overview history.htm Cape Chignecto Park George Pe piper, David J.W. Piper, http journals.hil.unb.ca index.php ag article view 1259 1652 A synopsis of the geology of the Cobequid Highlands, Nova Scotia , Atlantic Geology , 2003 Coord 45.38 64.07 display title type landmark dim 120000 region CA NS Category Landforms of Nova Scotia NovaScotia geo stub ... more details
Orphan date November 2010 The Sawtooth Fault is an east dipping normal fault vertical motion which runs along the eastern base of the Sawtooth Mountains in the state of Idaho in the United States. In 2010, scientists from the Idaho State University mapped the recently discovered Sawtooth Fault near the base of the mountains and found that it could produce an earthquake measuring up to magnitude 7.5 on the Richter scale . Two past large earthquakes likely took place on the fault around 7,000 and 4,000 years before present b.p . The fault stretches convert 40 mi km abbr on long, and runs near Stanley, Idaho and Redfish Lake , and the potential future earthquake would also be felt in Boise . ref cite news last US & Canada first BBC News title Scientists find new seismic fault in Rocky Mountains url http www.bbc.co.uk news world us canada 11790298 accessdate 20 November 2010 newspaper British Broadcasting Corporation date 18 November 2010 ref ref cite news last Wall first Tim title Large Seismic Fault Found in the Rockies url http news.discovery.com earth large seismic fault found in the rockies.html accessdate 20 November 2010 newspaper Discovery News date November 19, 2010 ref External links http www.localnews8.com news 25257306 detail.html Possible New Fault Line Found In Central Idaho , Associated Press report, KIFI LocalNews8.com, October 2, 2010 References reflist http geology.isu.edu dml thesis Johnson Eric 2010 ISU.pdf Lacustrine Evidence of Seismic Events on the Sawtooth Fault in the Redfish Lake Drainage, Sawtooth Mountains, Central Idaho , Eric M. Johnson, Thesis, Idaho State University, April 2010 Category Geology of Idaho Category Landforms of Custer County, Idaho tectonics stub ... more details
Shoreline Fault is a 25 km long vertical strike slip fault ref http www.sciencedaily.com releases 2010 06 100602215239.htm ScienceDaily Revised Seismotectonic Model for California Central Coast More Complex Than Previously Thought ref discovered in 2008 that lies less than a mile from the Diablo Canyon Nuclear Power Plant in California . It is thought to be able to produce quakes up to 6.5 magnitude, and along with the Hosgri fault are thought to pose a threat to the nuclear plant despite the operator, Pacific Gas and Electric claiming the facility to be able to withstand a 7.5 magnitude quake. ref http www.santamariatimes.com news local govt and politics article 8c1f14cc 2c11 11df b385 001cc4c03286.html Santa Maria Times Supervisors request delay for Diablo relicensing ref References reflist External sites http diablocanyonpge.com home resources shoreline fault zone report with plates.html PG&E Shoreline Fault Zone Report geology stub Category Seismic faults of California California Faults ... more details
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