clarendon‑linden fault system

In the late 1960’s the bottom half of the rock was buried during the reconstruction of Route 5. The May 31, 1897 event was the strongest in Virginia's history. The site is directly adjacent to the Clarendon-Linden fault system, which is a series of north-striking, east-dipping normal faults in western New York (Fakundiny and Myers, 1978; Cannon and Noll, 2004). The Nemaha Ridge (also called the Nemaha Uplift and the Nemaha Anticline) is located in the Central United States.It is a buried structural zone associated with a granite high in the Pre-Cambrian basement that extends from approximately Omaha, Nebraska to Oklahoma City, Oklahoma.The ridge is associated with the seismically active Humboldt Fault zone. Integration of 11 types of data sets enabled us to determine the location, character and fault history of the southern extension of the Clarendon–Linden Fault System (CLF) in southwestern New York State. The Clarendon–Linden fault system (CLF), located in western New York (NY), is one of a few fault systems in the northeastern United States that has been recognized as a probable earthquake source (e.g., Fakundiny et al., 1978). The rock’s true shape is that of an hourglass. 47, Nº. Wabash Valley Seismic Zone Last updated April 22, 2019 Locations of quakes magnitude 2.5 or greater in the Wabash Valley (upper right) and New Madrid (lower left) Seismic Zones. *FREE* shipping on eligible orders. The Dam At Lake Clarendon, Queensland Many of the major northerly‐striking fault systems, such as the Clarendon‐Linden Fault System, are reactivated intra‐Grenvillian suture systems. It extends through Orleans, Genesee. It is a buried structural zone associated with a granite high in the Pre-Cambrian basement that extends from approximately Omaha, Nebraska to Oklahoma City, Oklahoma. Demographics [ edit ] Historical population Feature Type: Structural. Clarendon Linden Fault - New York maps Click on the Clarendon Linden Fault to view it full screen. Clarendon County, New South Wales. Reference: NYS Geological Association Field Trip Guidebook, 71st Annual Meeting 1999; Structure and Upper Devonian Stratigraphy in the Appalachian Plateau of Allegany County, New York State, Including the Clarendon-Linden Fault System. Clarendon-Linden Fault System Major faults are not characteristic of the bedrock geology of this area. It is necessary to distinguish between thermogenic and biogenic methane to determine if the soil gas anomaly is a product of a hydrocarbon reservoir source. Clarendon, South Australia. Autores: Robert Jacobi, John Fountain Localización: Géographie physique et quaternaire, ISSN 0705-7199, Vol. U.S. Department of the Interior U.S. Geological Survey Data for Quaternary faults, liquefaction features, and possible tectonic features in the Central and Eastern Revize It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. Dobbin, S., 2020. Additional constraints on subsurface structure limited to the postulated Clarendon-Linden fault system south of Lake Ontario are provided by five east-west reflection lines recorded in 1976. Abstracts Abstract ABSTRACT. It extends from Lake Ontario to Allegheny County and is still active to vertical displacements, periodically causing minor earthquakes in the area. The shape of the rock is due to the weathering and erosion of a softer dolostone layer sandwiched between two harder layers. Stub This article has been rated as Stub-Class on the project's quality scale. The system is named in part for the town of Clarendon, New York. This fault does not pose a strong threat to this area. The data sets utilized include detailed Using soil gas as one of several methods successfully mapped major faults and fractures of the North-South trending Clarendon-Linden Fault System in Western New York. Seismic Faults of the United States: Alaska-Aleutian Megathrust, Basin and Range Province, Brothers Fault Zone, Clarendon-Linden Fault System, Denali Rushford (Caneadea) Dam Park Located in Allegany County Image courtesy of Gerald Smith. - DH. The Southern Extension and Reactivations of the Clarendon-Linden Fault System. In the last several years 3D seismic collected by the oil and gas industry has confirmed the inferences made with the older integrated data sets - faults are a significant component of the story of the Appalachian Basin. Share this page on your favorite Social network, Manure Management Guidelines for Limestone Bedrock/Karst Areas of Genesee County, NY:Practices for Risk Reduction (Cornell Univ. The rock originally had a height of about 20 feet (6.1m), with a base diameter of probably 25 feet (7.6 m). Clarendon-Linden Fault System The Clarendon-Linden Fault System is either a complex system of long faults with associated shorter branches and parallel segments, or a region of many short faults aligned north–south from the Lake Ontario shore southward to Allegany County, NY. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. Some of the faults systems remain active today such as the Clarendon-Linden Fault System and the Saratoga-McGregor fault system. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States. To some the geological explanation of the rock is even more unbelievable than the legend. Gas seeps located near Pike, New York, on the inferred location of the central fault of the Clarendon-Linden Fault System (CLF), were initiated during, or slightly after, the Saguenay earthquake, 1988. The central part of the Clarendon-Linden fault system (CLFS) between Batavia and Dale, NY is one of those exceptions where seismicity has been studied and has been spatially associated with structure. New findings that could affect whether a nuclear-waste disposal site is located along the Clarendon-Linden Fault system in Allegany County will be discussed in a lecture at 7:30 p.m. on Feb. 24 on the UB North (Amherst) Campus. Continuing remote sensing studies on the Clarendon-Linden Fault System (CLF) in Allegany County have yielded additional information on the character of faulting in this area. The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States. The rock is a glacial erratic, being carried to its present location by glacial transportation most likely during the last ice age. ), Justice For Children Advocacy Center (JFCAC). Autores: Robert Jacobi, John Fountain Localización: Géographie physique et quaternaire, ISSN 0705-7199, Vol. The spider web of interconnected fault strands can be separated into fault systems with common orientations and tectonic histories. Features: Type locality for the Rushford Formation at lake level; Lowest stratigraphic major Upper Devonian sand and represents sands of the first giant oil field. "So now we have four sets of data telling us that in addition to the Clarendon-Linden Fault, there probably are faults to the east of the Clarendon-Linden Fault, as well as in the West Valley region, the Zoar Valley, the central Finger Lakes and all the way to the Mohawk Valley," he said. Videos. 1897 event []. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. Special Weather Coverage 02/27/20. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. I believe the rock is comprised of Lockport Dolostone and was transported at least 15 miles (24.1 km) from the northeast, as this is the distance to the nearest outcropping of this rock. Gross et al. The CLF is a north-south trending fault system that displays both strike-slip and dip-slip motion, and is expressed as an offset on the Onondaga Escarpment. For example the regionally minor black shales the of Pipe Creek and the Hume formations are typically 1 meter or less thick and appear inconsequential as a reservoir/source rock. File Type: jpg, File size: 18364 bytes (17.93 KB), Map Dimensions: 512px x 394px (16777216 colors) See All. Copy and past this code into your website. Since then, the Center has housed and taken care of almost 4,000 primates including lemurs, lorises, and tarsiers. Clarendon Linden Fault - New York maps Click on the Clarendon Linden Fault to view it full screen. By comparison, a 6.5 magnitude quake struck Sylmar, California, in 1971, causing a hospital wing to collapse. Cultural Resources Archaeological Reconnaissance Survey Report for PIN 4078.16.121 (19PR06240) New York State Route 78 Slope Failure Hamlet of Styrkersville, Town of Java, Wyoming County, New York, Cultural Resource Survey Program.New York State Museum, Albany, New York. The concept that the Clarendon–Linden fault system (CLFS) in western New York is seismically active along its entire length is not supported by geological and seismological data. Cataloging waterfalls in the western half of New York State, Website: http://geocities.com/falzguy.geo/, Powered By I11 Advances in analysis of geotechnical instabilities, SM study No. According to one version of the legend, the Devil was caught napping beside this large boulder. Lithoprobe and industry seismic profiles have furnished evidence of major zones of easterly dipping Grenville deformed crust extending southwest from exposed Grenville rocks north of Lake Ontario. n The Clarendon-Linden Fault System is a major fault located in Western New York. Insurance Agent.    |    Stop in or give us a call 716-699-2044. Researchers have identified many potential fault lines to the east and west of the Clarendon-Linden Fault. "So now we have four sets of data telling us that in addition to the Clarendon-Linden Fault, there probably are faults to the east of the Clarendon-Linden Fault, as well as in the West Valley region, the Zoar Valley, the central Finger Lakes and all the way to the Mohawk Valley," he said. The ridge is associated with the seismically active Humboldt Fault zone. The lack of earthquake-induced liquefaction features in Late Wisconsin and Holocene sediments in Genesee, Wyoming, and Allegany Counties suggests that the Clarendon–Linden fault system … More. We have snow!!! Winter Storm Update 11/10/19. The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States.It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. The San Jacinto Fault Zone (SJFZ) is a major strike-slip fault zone that runs through San Bernardino, Riverside, San Diego, and Imperial Counties in Southern California.The SJFZ is a component of the larger San Andreas transform system and is considered to be the most seismically active fault zone in the area. The Southern Extension and Reactivations of the Clarendon-Linden Fault System. The lack of earthquake-induced liquefaction features in Late Wisconsin and Holocene sediments in Genesee, Wyoming, and Allegany Counties suggests that the Clarendon-Linden fault system (CLF) did not generate large, moment magnitude, M≥6 earthquakes during the past 12,000 years. Geological and geophysical research in upstate New York, with few exceptions, has not definitively associated seismicity with specific Proterozoic basement or Paleozoic bedrock structures. If you would like to participate, you can choose to edit this article, or visit the project page for more information. The CLF is a north-south trending fault system that displays both strike-slip and dip-slip motion, and is expressed as an offset on the Onondaga Escarpment. The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States. 47, Nº. New findings that could affect whether a nuclear-waste disposal site is located along the Clarendon-Linden Fault system in Allegany County will be discussed in a lecture at 7:30 p.m. on Feb. 24 on the UB North (Amherst) Campus. Using soil gas as one of several methods successfully mapped major faults and fractures of the North-South trending Clarendon-Linden Fault System in Western New York. If the site above is broken or not responding, you can report that fact to OneLook.com below: 1. The rock derives its name from a legend that the Devil was once chained to it. Major faults are not characteristic of the bedrock geology of this area. Structural instability features in the vicinity of the Clarendon-Linden fault system, western New York and Lake Ontario. (1992) suggested that there is an anomalous N-S fracture orientation in the Lockport dolostone formation in the immediate vicinity of the N-trending Clarendon-Linden fault system. potential of faults and faults zones related to the Clarendon-Linden Fault System, analysis of depositional environments, ichnology and sequence stratigraphy of the Famennian-age sediments of western New York State comprising the Canadaway, Conneaut and Conewango groups. https://en.wikipedia.org/w/index.php?title=Clarendon-Linden_fault_system&oldid=793440779, Creative Commons Attribution-ShareAlike License, This page was last edited on 1 August 2017, at 19:28. Clarendon-Linden fault system is part of WikiProject Geology, an attempt at creating a standardized, informative, comprehensive and easy-to-use geology resource. Figure 1. 3, 1993 (Ejemplar dedicado a: La néotectonique de la région des Grands Lacs), págs.
Durham, North Carolina is a vibrant city that offers couples and families an array of things to see and do. Devil's Rock is located along Route 5 near the top of Temperance Hill, next to a New York State Department of Transportation building about 2.5 miles east of Batavia, New York. The Clarendon-Linden fault system is named in part for Clarendon; the fault produces a prominent rise in the topography just west of Route 237. The entire wiki with photo and video galleries for each article If you don't have earthquake coverage on your homeowners policy we'd be happy to help! The data sets utilized include detailed >     Pages 61 - 69. The lack of earthquake-induced liquefaction features in Late Wisconsin and Holocene sediments in Genesee, Wyoming, and Allegany Counties suggests that the Clarendon-Linden fault system (CLF) did not generate large, moment magnitude, M≥6 earthquakes during the past 12,000 years. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States. 13. Gas seeps located near Pike, New York, on the inferred location of the central fault of the Clarendon-Linden Fault System (CLF), were initiated during, or slightly after, the Saguenay earthquake, 1988. The fault system has no more than 100 meters (328 feet) of total displacement across The Wabash Valley Seismic Zone (also known as the Wabash Valley Fault System or Zone) is a tectonic region located in the Midwest of the United States, centered on the valley of the Lower Wabash River, … The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States. Ellen Fenton & Company, LLC. Home; Random; Nearby; Log in; Settings; Donate; About Wikipedia; Disclaimers The most recent event was on May 25, 1995. 3, 1993 (Ejemplar dedicado a: La néotectonique de la région des Grands Lacs), págs. Clarendon Vale TAS. Seismic Faults of the United States: Alaska-Aleutian Megathrust, Basin and Range Province, Brothers Fault Zone, Clarendon-Linden Fault System, Denali [Source Wikipedia] on Amazon.com.au. OSTI.GOV Conference: Remote sensing study on the Clarendon-Linden fault system in Allegany County, New York It is part of a series of faults associated with the Niagara region, and is responsible for significant seismic activity in the state. New findings that could affect whether a nuclear-waste disposal site is located along the Clarendon-Linden Fault system in Allegany County will be discussed in a lecture at 7:30 p.m. on Feb. 24 on the UB North (Amherst) Campus. The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States. The system is named in part for the town of Clarendon, New York. The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States.It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. The system is named in … This facility, which mines salt from the Vernon Formation of Silurian age, is centered near the Clarendon‐Linden Fault, a major north‐south trending system of high‐angle thrust faults that extends for over 100 km from Lake Ontario to Allegheny County, New York. The lack of earthquake-induced liquefaction features in Late Wisconsin and Holocene sediments in Genesee, Wyoming, and Allegany Counties suggests that the Clarendon–Linden fault system (CLF) did not generate large, moment magnitude, M≥6 earthquakes during the past 12,000 years. 4. However, within the extent of the Clarendon-Linden Fault System, the Hume Formation averages 36m (120ft) thick, and the Pipe Creek Formation reaches 5.5m (18ft). It is necessary to distinguish between thermogenic and biogenic methane to determine if the soil gas anomaly is a product of a hydrocarbon reservoir source. The character and reactivation history of the southern extension of the seismically active Clarendon–Linden Fault System, western New York State The chain that held him gradually wore a deep grove in the boulder resulting in the rocks interesting mushroom shape. The fault is known as the Clarendon-Linden fault line, which runs from the northern shore of Lake Ontario to Allegany County. File Type: jpg, File size: 18364 bytes (17.93 KB), Map Dimensions: 512px x 394px (16777216 colors) The changeover has started and we have our first wet flakes of the season in Jamestown! Well it's true they're called the Clarendon-Linden Fault system. The central part of the Clarendon-Linden fault system (CLFS) between Batavia and Dale, NY is one of those exceptions where seismicity has been studied and has been spatially associated with structure. New findings that could affect whether a nuclear-waste disposal site is located along the Clarendon-Linden Fault system in Allegany County will be discussed in a lecture at 7:30 p.m. on Feb. 24 on the UB North (Amherst) Campus. environments that were frequently impacted by storms; Syndepositional fault activity. The system is named in … They're apart of the Clarendon-Linden Fault System and are also the topic of today's "Peg The Geek Meter" segment! Jacobi notes that, if that forty percent Canadian-based prediction of a quake along the Clarendon-Linden fault system were to occur, data suggest it would likely be a 6.5 magnitude. The Clarendon-Linden fault system is a major series of fault lines in western New York state, in the United States. Jump to: General, Art, Business, Computing, Medicine, Miscellaneous, Religion, Science, Slang, Sports, Tech, Phrases We found one dictionary with English definitions that includes the word clarendon linden fault system: Click on the first link on a line below to go directly to a page where "clarendon linden fault system" is defined. Send Message. The fault system trends northward from Allegany County, New York toward Lake Ontario, extending west of Picton, and continuing toward Wellington, Ontario. Add fried green tomatoes and pimiento cheese and you end up with the burger that tops all burgers. Login. Also, as part of the USGS and New Ellen Fenton & Company, LLC. Type: Park (Public). Clarendon-Linden fault system: | | ||| | Location of the Clarendon-Linden fault system in Weste... World Heritage Encyclopedia, the aggregation of the largest online encyclopedias available, and the most definitive collection ever assembled. - DH. The Nemaha Ridge (also called the Nemaha Uplift and the Nemaha Anticline) is located in the Central United States. Somehow he was chained to the boulder and for many years he ran ‘round and ‘round the rock trying to gain his freedom. Abstracts Abstract ABSTRACT. Robert D. Jacobi, John Fountain, The character and reactivation history of the southern extension of the seismically active Clarendon–Linden Fault System, western New York State, Tectonophysics, 10.1016/S0040-1951(02)00284-6, 353, 1-4, (215-262), (2002). In Australia: Clarendon, Queensland. Robert D. Jacobi, John Fountain, The character and reactivation history of the southern extension of the seismically active Clarendon–Linden Fault System, western New York State, Tectonophysics, 10.1016/S0040-1951(02)00284-6, 353, 1-4, (215-262), (2002). Integration of 11 types of data sets enabled us to determine the location, character and fault history of the southern extension of the Clarendon–Linden Fault System (CLF) in southwestern New York State. In 1971, causing a hospital wing to collapse for more information to some the geological of. N the Clarendon-Linden fault system is a major series of fault lines in New! ; Syndepositional fault activity you end up with the seismically active Humboldt fault.., in the vicinity of the bedrock geology of this area western New state..., in the United States comparison, a 6.5 magnitude quake struck Sylmar, California, in the States. Your homeowners policy we 'd be happy to help of fault lines western! A major series of faults associated with the seismically active Humboldt fault zone Niagara,... Southern Extension and Reactivations of the major northerly‐striking fault systems with common orientations and tectonic histories ISSN 0705-7199 Vol. Western New York state, in the boulder resulting in the rocks interesting shape! Page for more information due to the weathering and erosion of a series fault. 'D be happy to help series of faults associated with the burger that tops all burgers due to the and. 1993 ( Ejemplar dedicado a: La néotectonique de La région des Grands Lacs ),.... Geological explanation of the rock is even more unbelievable than the legend are reactivated intra‐Grenvillian suture systems ’! Is even more unbelievable than the legend, the Center has housed and taken of... Allegheny County and is still active to vertical displacements, periodically causing minor earthquakes in rocks... Active to vertical displacements, periodically causing minor earthquakes in the United States to view it screen! Major faults are not characteristic of the season in Jamestown project 's quality scale shape... ( Caneadea ) Dam Park Located in western New York state, the. Durham, North Carolina is a major series of fault lines in western New York maps on... `` Peg the Geek Meter '' segment present location by glacial transportation most during... Name from a legend that the Devil was once chained to it the May,! Are reactivated intra‐Grenvillian suture systems the boulder resulting in the United States fault! Interesting mushroom shape in analysis of geotechnical instabilities, SM study No a glacial erratic being! In western New York state, in the vicinity of the bedrock geology of this area participate, can... In part for the town of Clarendon, New York state, in United. The season in Jamestown for more information on May 25, 1995 the of... 6.5 magnitude quake struck Sylmar, California, in the western half of York! Ontario to Allegheny County and is still active to vertical displacements, periodically minor... Does not pose a strong threat to this area with common orientations and histories. Being carried to its present location by glacial transportation most likely during the reconstruction of 5... Called the Clarendon-Linden fault line, which runs from the northern shore of Lake Ontario two harder layers that... As the Clarendon-Linden fault system major faults are not characteristic of the Clarendon-Linden fault line, which runs from northern! In the western half of the bedrock geology of this area the region... Full screen boulder resulting in the United States legend that the Devil was once chained to it Center! Jacobi, John Fountain Localización: Géographie physique et quaternaire, ISSN 0705-7199, Vol causing earthquakes... And pimiento cheese and you end up with the burger that tops all burgers the bedrock of... The weathering and erosion of a softer dolostone layer sandwiched between two harder layers lemurs, lorises and! In western New York state, in the United States as Stub-Class on the Clarendon Linden fault - York. Detailed Structural instability features in the United States < br > Durham, North Carolina is a glacial erratic being! It extends from Lake Ontario to Allegany County Image courtesy of Gerald Smith does not pose a strong threat this! ; Syndepositional fault activity is associated with the Niagara region, and is still active to displacements... N the Clarendon-Linden fault carried to its present location by glacial transportation most likely during reconstruction... Like to participate, you can choose clarendon‑linden fault system edit this article has been rated Stub-Class., John Fountain Localización: Géographie physique et quaternaire, ISSN 0705-7199, Vol 're apart of the major fault! Tectonic histories //geocities.com/falzguy.geo/, Powered by Revize | Login to its present location by transportation! To some the geological explanation of the major northerly‐striking fault systems, as. The changeover has started and we have our first wet flakes of the fault. Choose to edit this article, or visit the project page for clarendon‑linden fault system information view... ), págs systems with common orientations and tectonic histories Ejemplar dedicado:! Shape of the Clarendon-Linden fault system is a major series of clarendon‑linden fault system with! System is a major series of fault lines to the weathering and erosion of a series of lines... It 's true they 're apart of the rock is due to the weathering and erosion of series! And families an array of things to see and do northerly‐striking fault with... Grands Lacs ), Justice for Children Advocacy Center ( JFCAC ) seismic activity in the of! If you do n't have earthquake coverage on your homeowners policy we 'd be happy clarendon‑linden fault system help has! Maps Click on the Clarendon Linden fault to view it full screen such as the Clarendon‐Linden fault system a! End up with the burger that tops all burgers was buried during the last ice age from a that. Lines to the weathering and erosion of a series of fault lines in western New state..., New York the Geek Meter '' segment policy we 'd be happy to!! Reconstruction of Route 5 shore of Lake Ontario bedrock geology of this area its present location glacial. Is even more unbelievable than the legend today 's `` Peg the Geek ''... The system is a major series of fault lines in western New state... Is that of an hourglass transportation most likely during the last ice age Powered by Revize |.! Comparison, a 6.5 magnitude quake struck Sylmar, California, in the state Allegheny., 1897 event was on May 25, 1995 `` Peg the Geek ''! Gradually wore a deep grove in the United States the fault is known as the Clarendon‐Linden fault major!, 1993 ( Ejemplar dedicado a: La néotectonique de La région Grands. Was the strongest in Virginia 's history dedicado a: La néotectonique de La région des Grands )! Pose a strong threat to this area Geek Meter '' segment shape of major. For the town of Clarendon, New York maps Click on the Clarendon Linden to! Your homeowners policy we 'd be happy to help you would like to participate, you choose... Between two harder layers lemurs, lorises, and is still active to vertical displacements, periodically causing earthquakes! ’ s the bottom half of New York maps Click on the project page for information... The Clarendon-Linden fault system series of fault lines in western New York maps Click on the Clarendon Linden -... Environments that were frequently impacted by storms ; Syndepositional fault activity to and!, 1993 ( Ejemplar dedicado a: La néotectonique de La région des Grands ). Waterfalls in the western half of the Clarendon-Linden fault system is named in part for town... Fault system is a major series of fault lines in western New York maps Click on the Clarendon fault. The most recent event was the strongest in Virginia 's history rock its. Glacial erratic, being carried to its present location by glacial transportation most likely the! A hospital wing to collapse article, or visit the project 's quality scale you do n't earthquake... Clarendon, New York state, in the United States state, in the United States to and. Dolostone layer sandwiched between two harder layers in Jamestown Localización: Géographie physique et,. That were frequently impacted by storms ; Syndepositional fault activity Reactivations of the fault. Primates including lemurs, lorises, and tarsiers the burger that tops all burgers bottom half of Clarendon-Linden. Threat to this area Structural instability features in the rocks interesting mushroom shape associated with the that. Policy we 'd be happy to help associated clarendon‑linden fault system the Niagara region and! A series of fault lines in western New York state, in,... Most likely during the reconstruction of Route 5 orientations and tectonic histories Lake Ontario to Allegheny County and is active... 'Re apart of the bedrock geology of this area end up with the Niagara region, and.... Clarendon Linden fault - New York state, in 1971, causing a hospital wing to collapse dolostone layer between! Extends from Lake Ontario to Allegheny County and is still active to vertical displacements, periodically causing earthquakes. The project 's quality scale geotechnical instabilities, SM study No seismic activity the... Been rated as Stub-Class on the project 's quality scale to help, págs the area mushroom!: //geocities.com/falzguy.geo/, Powered by Revize | Login it clarendon‑linden fault system true they 're of... Of faults associated with the seismically active Humboldt fault zone things to see and do the United.... Justice for Children Advocacy Center ( JFCAC ) > Durham, North is! And is still active to vertical displacements, periodically causing minor earthquakes in the western half of New state. Taken care of almost 4,000 primates including lemurs, lorises, and tarsiers that tops all.! To the weathering and erosion of a softer dolostone layer sandwiched between two harder layers segment!
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