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 If the site above is broken or not responding, you can report that fact to OneLook.com below: Clarendon Linden Fault - New York maps Click on the Clarendon Linden Fault to view it full screen. File Type: jpg, File size: 18364 bytes (17.93 KB), Map Dimensions: 512px x 394px (16777216 colors) The shape of the rock is due to the weathering and erosion of a softer dolostone layer sandwiched between two harder layers. >     Pages 61 - 69. Videos. OSTI.GOV Conference: Remote sensing study on the Clarendon-Linden fault system in Allegany County, New York 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. 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. 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 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. Insurance Agent. If you would like to participate, you can choose to edit this article, or visit the project page for more information. This fault does not pose a strong threat to this area. The most recent event was on May 25, 1995. The data sets utilized include detailed *FREE* shipping on eligible orders. Many of the major northerly‐striking fault systems, such as the Clarendon‐Linden Fault System, are reactivated intra‐Grenvillian suture systems. 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. 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. Demographics [ edit ] Historical population The rock is a glacial erratic, being carried to its present location by glacial transportation most likely during the last ice age. 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. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. Clarendon, South Australia. The changeover has started and we have our first wet flakes of the season in Jamestown! The system is named in part for the town of Clarendon, New York. In the late 1960’s the bottom half of the rock was buried during the reconstruction of Route 5. According to one version of the legend, the Devil was caught napping beside this large boulder. 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. Ellen Fenton & Company, LLC. Clarendon Vale TAS. We have snow!!! The rock derives its name from a legend that the Devil was once chained to it. 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 … The chain that held him gradually wore a deep grove in the boulder resulting in the rocks interesting mushroom shape. Rushford (Caneadea) Dam Park Located in Allegany County Image courtesy of Gerald Smith. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. The May 31, 1897 event was the strongest in Virginia's history. Ellen Fenton & Company, LLC. If you don't have earthquake coverage on your homeowners policy we'd be happy to help! 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. Copy and past this code into your website. Type: Park (Public). 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. - DH.    |    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. 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. 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. It extends from Lake Ontario to Allegheny County and is still active to vertical displacements, periodically causing minor earthquakes in the area. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. 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. 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). 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. 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. By comparison, a 6.5 magnitude quake struck Sylmar, California, in 1971, causing a hospital wing to collapse. It extends through Orleans, Genesee, Wyoming, and into Allegany counties and is responsible for much of the seismic activity in the region. I11 Advances in analysis of geotechnical instabilities, SM study No. Autores: Robert Jacobi, John Fountain Localización: Géographie physique et quaternaire, ISSN 0705-7199, Vol. 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 fault system has no more than 100 meters (328 feet) of total displacement across The rock originally had a height of about 20 feet (6.1m), with a base diameter of probably 25 feet (7.6 m). Feature Type: Structural. 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). 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. 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 Linden Fault - New York maps Click on the Clarendon Linden Fault to view it full screen. 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. See All. "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. 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. More. Structural instability features in the vicinity of the Clarendon-Linden fault system, western New York and Lake Ontario. environments that were frequently impacted by storms; Syndepositional fault activity.