Find link

language: af: Afrikaans als: Alemannisch [Alemannic] am: አማርኛ [Amharic] an: aragonés [Aragonese] ar: العربية [Arabic] arz: مصرى [Egyptian Arabic] as: অসমীয়া [Assamese] ast: asturianu [Asturian] az: azərbaycanca [Azerbaijani] azb: تۆرکجه [Southern Azerbaijani] ba: башҡортса [Bashkir] bar: Boarisch [Bavarian] bat-smg: žemaitėška [Samogitian] be: беларуская [Belarusian] be-tarask: беларуская (тарашкевіца) [Belarusian (Taraškievica)] bg: български [Bulgarian] bn: বাংলা [Bengali] bpy: বিষ্ণুপ্রিয়া মণিপুরী [Bishnupriya Manipuri] br: brezhoneg [Breton] bs: bosanski [Bosnian] bug: ᨅᨔ ᨕᨘᨁᨗ [Buginese] ca: català [Catalan] ce: нохчийн [Chechen] ceb: Cebuano ckb: کوردیی ناوەندی [Kurdish (Sorani)] cs: čeština [Czech] cv: Чӑвашла [Chuvash] cy: Cymraeg [Welsh] da: dansk [Danish] de: Deutsch [German] el: Ελληνικά [Greek] en: English eo: Esperanto es: español [Spanish] et: eesti [Estonian] eu: euskara [Basque] fa: فارسی [Persian] fi: suomi [Finnish] fo: føroyskt [Faroese] fr: français [French] fy: Frysk [West Frisian] ga: Gaeilge [Irish] gd: Gàidhlig [Scottish Gaelic] gl: galego [Galician] gu: ગુજરાતી [Gujarati] he: עברית [Hebrew] hi: हिन्दी [Hindi] hr: hrvatski [Croatian] hsb: hornjoserbsce [Upper Sorbian] ht: Kreyòl ayisyen [Haitian] hu: magyar [Hungarian] hy: Հայերեն [Armenian] ia: interlingua [Interlingua] id: Bahasa Indonesia [Indonesian] io: Ido is: íslenska [Icelandic] it: italiano [Italian] ja: 日本語 [Japanese] jv: Basa Jawa [Javanese] ka: ქართული [Georgian] kk: қазақша [Kazakh] kn: ಕನ್ನಡ [Kannada] ko: 한국어 [Korean] ku: Kurdî [Kurdish (Kurmanji)] ky: Кыргызча [Kirghiz] la: Latina [Latin] lb: Lëtzebuergesch [Luxembourgish] li: Limburgs [Limburgish] lmo: lumbaart [Lombard] lt: lietuvių [Lithuanian] lv: latviešu [Latvian] map-bms: Basa Banyumasan [Banyumasan] mg: Malagasy min: Baso Minangkabau [Minangkabau] mk: македонски [Macedonian] ml: മലയാളം [Malayalam] mn: монгол [Mongolian] mr: मराठी [Marathi] mrj: кырык мары [Hill Mari] ms: Bahasa Melayu [Malay] my: မြန်မာဘာသာ [Burmese] mzn: مازِرونی [Mazandarani] nah: Nāhuatl [Nahuatl] nap: Napulitano [Neapolitan] nds: Plattdüütsch [Low Saxon] ne: नेपाली [Nepali] new: नेपाल भाषा [Newar] nl: Nederlands [Dutch] nn: norsk nynorsk [Norwegian (Nynorsk)] no: norsk bokmål [Norwegian (Bokmål)] oc: occitan [Occitan] or: ଓଡ଼ିଆ [Oriya] os: Ирон [Ossetian] pa: ਪੰਜਾਬੀ [Eastern Punjabi] pl: polski [Polish] pms: Piemontèis [Piedmontese] pnb: پنجابی [Western Punjabi] pt: português [Portuguese] qu: Runa Simi [Quechua] ro: română [Romanian] ru: русский [Russian] sa: संस्कृतम् [Sanskrit] sah: саха тыла [Sakha] scn: sicilianu [Sicilian] sco: Scots sh: srpskohrvatski / српскохрватски [Serbo-Croatian] si: සිංහල [Sinhalese] simple: Simple English sk: slovenčina [Slovak] sl: slovenščina [Slovenian] sq: shqip [Albanian] sr: српски / srpski [Serbian] su: Basa Sunda [Sundanese] sv: svenska [Swedish] sw: Kiswahili [Swahili] ta: தமிழ் [Tamil] te: తెలుగు [Telugu] tg: тоҷикӣ [Tajik] th: ไทย [Thai] tl: Tagalog tr: Türkçe [Turkish] tt: татарча/tatarça [Tatar] uk: українська [Ukrainian] ur: اردو [Urdu] uz: oʻzbekcha/ўзбекча [Uzbek] vec: vèneto [Venetian] vi: Tiếng Việt [Vietnamese] vo: Volapük wa: walon [Walloon] war: Winaray [Waray] yi: ייִדיש [Yiddish] yo: Yorùbá [Yoruba] zh: 中文 [Chinese] zh-min-nan: Bân-lâm-gú [Min Nan] zh-yue: 粵語 [Cantonese]

jump to random article

Longer titles found: Flores Back Arc Thrust Fault (view), Northridge Blind Thrust Fault (view), Mount Diablo Thrust Fault (view)

searching for Thrust fault 124 found (451 total)

alternate case: thrust fault

Golconda Thrust (206 words) [view diff] exact match in snippet view article find links to article

Permian and the late Jurassic. It is considered equivalent to the Tobin thrust fault. It contains the Havallah sequence. The time of the Golconda Thrust is

on the planet, Beagle Rupes marks the surface expression of a large thrust fault believed to have formed as Mercury cooled and the entire planet shrank

Canada. It was formed as a result of the Lewis Overthrust, a geologic thrust fault resulted in the overlying of younger Cretaceous rocks by older Proterozoic

Coyote Hills segment of the Puente Hills Thrust Fault System. The Puente Hills Fault is a blind thrust fault that runs north and west from Orange County

northern Taiwan. It is also regarded as the northern part of "Western Thrust Fault Mountains" (西部衝上斷層山地) by Tomita Yoshirou and Lin Chaoqi. Although it

construction of the new section of US 23 in 1998, the "Pine Mountain Pound Gap Thrust Fault" was exposed. "The collision of the North American continent with Africa

Purchase Ridge syncline. It lies between the Clinchport Thrust Fault and the Hunter Valley Thrust Fault, on the Hunter Valley Thrust Sheet. The tunnel itself

Geologically, it is a breached anticline formed by a deep subsurface thrust fault. Most of the rocks at the surface are Cretaceous in age, including the

The Omagh Thrust Fault is a geological fault in County Tyrone. It is of one of the most important structural discontinuities in Northern Ireland and an

designated SSSI because of its geological interest for the Carmel Head Thrust fault where Precambrian rocks have been pushed over younger Ordovician rocks

the east. This is roughly the riverbed of the Krka. It is a sinistral thrust-fault that runs along the southern limb of the Krško Syncline. The movements

observations that support the idea that the STD can also be a north-directed thrust fault. The main problem that the South Tibetan detachment is expected to help

Silurian Sambre et. Meuse Trough that is bound by the Condroz Thrust Fault The Condroz Thrust Fault that extends from northern France to Aachen in Germany The

fault of the Midland Valley Terrane, the Castle Archdale Fault-Omagh Thrust Fault zone, while in the south is the Clogher Valley Fault. Carboniferous rocks

main shock. Blind thrust earthquake, an earthquake which occurs along a thrust fault that does not show signs on the Earth's surface. Cryoseism, a seismic

naturally through a big crack in the rock called the Sulphur Mountain Thrust Fault. The source of the water is located at higher elevations on either Sulphur

range: Ordovician Rome Formation over Moccasin Formation (Copper Creek Thrust Fault, Tennessee) Type Formation Lithology Primary limestone Location Region

As a result, forming the Greater Caucasus Range. The Main Caucasus Thrust Fault, a north-dipping fault, accommodates most of the plate interaction. Subduction

November 3, nucleating 22 km (14 mi) east of the foreshock, was on a thrust fault segment, the previously unknown Susitna Glacier thrust, to the south

is also known in English as the Harz North Rim Fault or Harznordrand Thrust (Fault). The northern edge of the Harz is oriented in a Hercynian (WNW-ESE)

2008) The disastrous 2003 Boumerdès earthquake led to the discovery of a thrust fault; it was subsequently named after the town. The fault has since been incorporated

located on the edge of Cerničko polje (karstic field) floor, at the thrust fault zone (overthrust), where eocene flysch and limestone make tectonic contact

Mountains due to its east-west trend of tectonic features, including thrust fault zones, anticlines, and domes. The area of tectonic activity experienced

The source fault, identified as the Hoshab Fault, was likely an old thrust fault due to its shallow dip angle. It formed within an accretionary wedge

is a Laramide uplift defined by a normal fault on the west side and a thrust fault on the east side. The northern part of the uplift is covered by sedimentary

the Tanlu fault belt extended to the north and was transformed into a thrust fault. Afterwards, although the Tan-Lu Faults was once restored to a strike-slip

Journal, 1996, 122–130. Shear-wave polarizations in the Peter the First Range indicating crack-induced anisotropy in a thrust-fault regime[dead link] v t e

up the crust and causing the extensional reactivation of an ancient thrust fault. Slip along a low-angle segment of the fault caused a slight ground deformation

[8] Tobe Thrust Fault 砥部衝上断層 Tobe shōjō dansō Tobe 33°43′58″N 132°47′44″E / 33.73272°N 132.79560°E / 33.73272; 132.79560 (Tobe thrust fault) 3.1,3,5

John E.; Tanaka, Sachiko (2004-11-12). "Earth Tides Can Trigger Shallow Thrust Fault Earthquakes". Science. 306 (5699): 1164–1166. Bibcode:2004Sci...306.1164C

earthquake, and instead showed oblique movement on a steeply-dipping thrust fault, with the eastern side of the fault rising relative to the western side

Paleoseismological investigations near Agsu, across the trace of the frontal thrust fault have found evidence for two earthquakes that may represent the events

3,000 meters (6,600 to 9,800 ft) high formed along the Main Boundary Thrust fault zone, with a steep southern face and gentler northern slopes. The range

(2008). "The 1998 Mw 5.7 Zhangbei-Shangyi earthquake revisited: a buried thrust fault revealed with interferometric synthetic aperture radar". Geochemistry

in turn is overlain by quartzite klippe features, a form of remnant thrust fault terrain, that contains itabirite. Based on similarities between the Gibi

down to Costa Rica for over 2,750 km. The subduction zone is a large thrust fault that has produced devastating earthquakes in human history. Subduction

presentation of a 17 km (11 mi) rupture on the west-dipping Gordon Valley blind thrust fault that could have produced the felt intensities that were specific to the

with a maximum displacement of 1 m on a 20 km long 32°-dipping blind thrust fault. Severe damage was observed in the epicentral area (I≥VII MSK). In Aïn

Haiyuan Fault between the Laohushan segment in the west and Liupanshan Thrust Fault to the east. The earthquake's epicenter is also likely near Haiyuan which

buteos such as the red-tailed hawk. Mt. Philo sits atop the Champlain Thrust fault of Middle Ordivician age. It is a Klippe made up of difficult to weather

underlying basement rocks date to the Jurassic period. The Los Lobos thrust fault complex demarcates the western boundary of the field. The Texas Company

place due to the steep grades formed by the geological feature called a thrust-fault. Kentucky portal “Visit Bad Branch Nature Preserve.” The Nature Conservancy

point where it may end, or merge with the east–west trending Pleito thrust fault. The White Wolf Fault (as illuminated by the aftershocks) was found to

Masao Inoue, stage actor, director Konpirasan Park Rishoin Temple Tobe Thrust Fault "Tobe town official statistics" (in Japanese). Japan. Tobe climate data

anticlinal structure with a sharp southern boundary defined by the Morales Thrust Fault, along which runs the Cuyama River. The Cuyama Valley separates the Caliente

igneous and metamorphics to Pre-Cretaceous metamorphics. The Vincent Thrust Fault, the oldest major fault in the range, dating to the Mesozoic, passes

Anna helped defined the Martic Line. They believed it to be a major thrust fault in Pennsylvania. Her ideas were often considered to be incomprehensible

Palaeocene, an Eocene strike-slip fault, an Oligocene northwest-verging thrust fault, and a south-east dipping normal fault inverted in the Neogene. Research

and chlorite. Sulphurets - This deposit is centered on the Sulphurets Thrust Fault where volcanic activity helped to form it (portions previously exposed

30–40 km west of Vienna, in a flat dipping and north–south striking thrust fault that is part of the Vienna Transform fault zone. This moderately-active

Hills at its northern termination. The fault continues north and joins a thrust fault system associated with the Assam Valley. the Mogang segment, the most

the Glärnisch (2,910 meters (9,550 ft)). The canton contains part of a thrust fault that was declared a geologic UNESCO World Heritage Site, under the name

permeability, and in sedimentary units which end abruptly at the Oak Ridge Thrust Fault; oil migrating upwards within permeable units, in this case, encounters

Highlands of Scotland, was crucial in the understanding of this, the first thrust fault to be discovered anywhere in the world. The monument's inscription reads:

mountain and the Turret Towers range immediately to the south lying on a thrust fault. Consequently, the eastern approach is more gradual, while the western

out across its face. Mount John Laurie is the result of the McConnell Thrust Fault, which put the resistive, cliff-forming Cambrian carbonate rock of the

length of 6 km (3.7 mi). Trenching studies revealed a northwest-dipping thrust fault measuring at least 75 km (47 mi) long which last moved between 1856 and

seen from Fil de Cassons (which is from southeast) showing the "Glarus thrust" fault in its peak. The photo is taken standing on the same line, indicated

boundary of the range is marked by the Santa Ynez Fault, the massive thrust fault that uplifted the mountains since approximately 5 million years ago starting

waves. Aftershock – follows larger earthquake. Blind thrust – along a thrust fault that does not show on the Earth's surface. Foreshock – precedes larger

Meadow Grounds syncline. This structure consists of a complex set of up-thrust fault blocks of Silurian and Devonian rocks bounded on all sides by north-trending

estimate slip rates from terrace rotation above an offshore, listric thrust fault, Kaikōura, New Zealand". Tectonophysics. 786: 228460. doi:10.1016/j.tecto

defined"- for example the 1994 Northridge earthquake occurred on a blind thrust fault not zoned by the act because of a lack of surface evidence. Living Where

rocks on top of younger units. In the northwest, the Luning-Fencemaker thrust fault developed in the Jurassic and thrust the Jungo terrane to the east, forming

other small synclines and anticlines in the Valley and Ridge province. A thrust fault, forced the rocks of the Blue Ridge on top of the Shenandoah Valley.

wholly within its limits. The mountains of the canton include part of a thrust fault that was declared a geologic UNESCO World Heritage Site, under the name

the north-central Smokies. As the elevation increases to the south, a thrust fault known as the Greenbrier Fault separates the Roaring Fork sandstone from

northern Tremp Formation. The main phase of movement of another major thrust fault, the Montsec to the south of the Tremp Basin, happened not before the

movements tilted the strata in the north to east and in the south a thrust fault pushed old Late Paleozoic rocks over the younger Purilactis Group. Salar

Plate and Eurasian Plate in the Cenozoic. In the latter deformation, a thrust fault belt running from east to west, the Flaming Mountains, was formed in

Falls, Montana. Nearby Mount Kidd marks the northern end of the Lewis Thrust Fault. Based on the Köppen climate classification, Mount James Walker is located

mechanism of the earthquake on May 21 corresponds to a northeast-striking thrust fault named Zemmouri fault which was identified for the first time after this

million years ago. During this time, the Ramapo fault, originally a thrust fault active during the creation of the Appalachian Mountains, was reactivated

southeastern British Columbia and southwestern Alberta, west of the Lewis Thrust Fault and south of about 49° 45". It overlies the Hollebeke Formation, and

southeastern British Columbia and southwestern Alberta, west of the Lewis Thrust Fault and south of about 50°N latitude. It unconformably overlies Ordovician

Little River Fault. Trenching of the Little River Fault indicate it is a thrust fault. This west-northwest–east-southeast striking fault is located within

outcrop in an area about 4 mi (6.4 km) long, adjacent to the McKittrick Thrust Fault, which defines the southwestern boundary of the oil field. They are found

Volcanics. The caldera is truncated on the north by a north-dipping thrust fault and is probably tilted to the south. Several other prominent gravity

defines the boundary between the Indian Plate and Eurasian Plate. This thrust fault is the source of most of Nepal's earthquakes. The earthquake of 1833

Glarus Thrust fault at Piz Dolf (right) and Piz Segnes as seen from Fil de Cassons

are folded into monoclines by several faults, including the Redlands Thrust Fault. List of national monuments of the United States "Listing of acreage

collision between the two plates and the so-called alpine orogeny. The major thrust fault of the Tectonic Arena Sardona in the eastern Glarus Alps gives a visible

Great Falls, Montana. Mount Kidd marks the northern end of the Lewis Thrust Fault. Based on the Köppen climate classification, Mount Kidd is located in

foothills along the south side of the valley as well. The large Morales Thrust Fault separates the abruptly-rising block of the Caliente Range from the valley

portion of the Ventura anticline, bounded on the north by the Grubb Thrust Fault, where the fault has pushed another closed anticline above the end of

foothills along the south side of the valley as well. The large Morales Thrust Fault separates the abruptly-rising block of the Caliente Range from the valley

Hill and south of Minehead. The Lynmouth-East Lyn Fault is a reverse or thrust fault dipping south at about 45 degrees which brings Lynton Slates over the

such as to the west the Rewhiti-Haupai Fault and to the east the Okura Thrust Fault. To the east, these continue until they reach the North-South aligned

to the south. Between these two geological areas is the Hunter-Mooki Thrust fault. At one time this fault was very geologically active and gave rise to

Chino Hills earthquake. The Northridge earthquake occurred on a blind-thrust fault directly underneath the San Fernando Valley, which until the earthquake

San Andreas is at some distance. Locally, the Sulphur Springs Valley Thrust Fault and Southampton Fault are found. No quaternary seismic activity along

et al., 2006). Site 808 is located in the front section of the main thrust fault, while site 1173 is located approximately 11 km from the frontal thrust

many parts of northern Armenia. The earthquake occurred along a known thrust fault with a length of 60 kilometers (37 mi). Its strike was parallel to the

be classified into three types. They are normal fault, reverse fault (thrust fault) and strike-slip fault. These different faulting behaviours accommodate

Cascadia subduction zone. While the focal mechanism indicated slip on a thrust fault striking N.10°W with a shallow dip of 13° to the east-northeast, the

were established during various periods (1920s, 1950s, 1960s). Meade Thrust Fault principle structure underlying basin. Cretaceous rocks underlie Willow

Discovery Rupes, photographed during the first flyby. Representation of the thrust fault at Discovery Rupes Australia region Aurora region Caduceata region The

overlap between the two sections was very narrow. They also noted that a thrust fault at Oyuklu artificially lengthens B−, the magnetozone containing the Norian-Rhaetian

Park. In its northern part, the mountains were formed as part of the thrust fault that was in 2008 declared a geologic UNESCO World Heritage Site, under

two smaller sub-events that initiated along the deeper portion of a thrust fault, but ruptured up-dip. Shortly afterwards, a 8.16 Mw  quake ruptured the

miles eastward into Massachusetts Bay. The west-dipping Northern Border thrust fault is marked by a rocky slope near Massachusetts Route 60 and forms the

researchers interpreted the rocks as a product of the Himalayan Main Central Thrust fault. In 1984 Heuberger et al. identified their actual origin in a giant landslide

further prospecting, which located commercial orebodies along the Chester thrust fault of Laramide age. The deposits are about six-mile east of Sargents. The

devastated many parts of the country. The earthquake occurred along a known thrust fault with a length of 60 kilometers (37 mi). Its strike was parallel to the

Shaw, John H.; Shearer, Peter M. (March 5, 1999). "An Elusive Blind-Thrust Fault Beneath Metropolitan Los Angeles". Science. 283 (5407): 1516–1518. Bibcode:1999Sci

located on the hanging wall of the regional, northwest-trending Cochise thrust fault. The movement of this fault transported Jurassic units of collapse-breccia

located on the hanging wall of the regional, northwest-trending Cochise thrust fault. The movement of this fault transported Jurassic units of collapse-breccia

further north the high Himalaya abruptly rise along the Main Central Thrust fault zone above the snow line at 5,000 to 5,500 metres (16,400 to 18,000 ft)

American Legion/Cabin John Bridge; Plummers Island (MD) Plummers Island Thrust Fault (inactive) Dead Run Dead Run Rapids Turkey Run (Potomac River) Cabin

DD Pollard, 2010, Structural geometry of Raplee Ridge monocline and thrust fault imaged using inverse Boundary Element Modeling and ALSM data, Journal

Millard F. (2005). "Influence of cumulative convergence on lithospheric thrust fault development and topography along the Australian-Pacific plate boundary

north end to near Livermore. These strike-slip faults and the Diablo thrust fault near Danville are all considered capable of significantly destructive

principal faults in the region are of the strike-slip type, a significant thrust fault (with no surface trace) is found on the mountain's southwest flank. The

(December 15, 2001). "Geologists trace fault zone under S.F. / Serra Thrust Fault is active, they say". San Francisco Chronicle. Retrieved 11 August 2023

chert and pyroclastic rocks, divided in half by the Trinity ophiolite. A thrust fault, known as the Trinity or Bully Choop thrust, separates the Eastern Klamath

from seismic inversion suggest rupture occurred along an east-dipping thrust fault, and produced a maximum displacement of 0.9 m (2 ft 11 in). It was reported

eastern boundaries of the Saltville Valley are located near the Saltville Thrust Fault, and the northwestern areas are bordered by the Upper Mississippian Little

the earthquake to shallow crustal faulting associated with a back-arc thrust fault running along the island. The Barbiris Fault which runs east–west south

like Shahr-e-Babak and Abadeh, and to the south-southwest by the main thrust fault of Zagros. A striking feature of this zone is the presence of immense

movement of the Earth's crust Blind thrust earthquake – Movement along a thrust fault that is not visible at the surface Intraplate earthquake – Earthquake

(Vivid Film) No Man's Land 20 (Video Team) Pornogothic (Wicked Pictures) Thrust Fault (VCA Platinum Plus) Words of Lust (Klimaxxx Productions) Best Overall

right figure shows a classic thrust belt and foreland basin system, the thrust fault carries overlying rocks to the surface and rocks of various lithology

by repeating southwest- to northeast-trending ridges and valleys. A thrust fault just east of Fairview indicates where younger rocks from the Ordovician

Seismic Zone being the most active. In 2012 he and his colleagues "found a thrust fault east of Knoxville that displaced bedrock for about one meter over Quaternary