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Pendleton Fault

The Pendleton Fault, sometimes called the Irwell Valley Fault, stretches for about 20 miles (32 km) from Bolton in Greater Manchester along the Irwell Valley through Pendleton to Poynton in Cheshire, running northwest–southeast. The fault throws the beds of the Middle Coal Measures of the Manchester Coalfield by 1,000 feet (300 m) on its western side. The fault is active, and movement has caused earthquakes.

Pendleton, Greater ManchesterPendleton, Greater ManchesterPendleton is an inner-city district of Salford, Greater Manchester, England. The A6 dual carriageway skirts the east of the district. Historically in Lancashire, Pendleton experienced rapid urbanisation during the Industrial Revolution. HistoryThe township has been variously recorded as Penelton in 1199, Pennelton in 1212, Penilton in 1236, Penhulton in 1331, Penulton in 1356 and Pendleton from about 1600. In the Middle Ages the manor was held by the Hultons of Hulton Park.Manchester CoalfieldManchester CoalfieldThe Manchester Coalfield is part of the South Lancashire Coalfield, the coal seams of which were laid down in the Carboniferous Period. Some easily accessible seams were worked on a small scale from the Middle Ages, and extensively from the beginning of the Industrial Revolution in the early 19th century until the last quarter of the 20th century. The Coal Measures lie above a bed of Millstone Grit and are interspersed with sandstones, mudstones, shales, and fireclays.Irwell ValleyIrwell ValleyThe Irwell Valley in North West England extends from the Forest of Rossendale through the cities of Salford and Manchester. The River Irwell runs through the valley, along with the River Croal.Fault (geology)Fault (geology)In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes.EarthquakeEarthquakeSudden movement of the Earth's crustEarthquake epicenters occur mostly along tectonic plate boundaries, especially on the Pacific Ring of Fire.An earthquake, also called a quake, tremor, or temblor, is the shaking of the Earth's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves.BoltonBoltonTown in Greater Manchester, EnglandTown in EnglandBolton ( , locally ) is a town in Greater Manchester in England. In the foothills of the West Pennine Moors, Bolton is between Manchester, Blackburn, Wigan, Bury and Salford. It is surrounded by several towns and villages that form the wider borough, of which Bolton is the administrative centre. The town is within the historic county boundaries of Lancashire.PoyntonPoyntonPoynton is a town in the civil parish of Poynton-with-Worth, in the Cheshire East district and the ceremonial county of Cheshire, England; from 1974 to 2009 it was in Macclesfield district. It is located on the easternmost fringe of the Cheshire Plain, 11 miles (18 km) south-east of Manchester, 7 miles (11 km) north of Macclesfield and 5 miles (8 km) south of Stockport. The first mention of the manor of Poynton was in 1289.Coal measuresCoal measuresIn lithostratigraphy, coal measures are coal-bearing strata, with the term typically applied to European units of the Upper Carboniferous System. In the United Kingdom, the term is equivalent to regional components of the Westphalian-age Coal Measures Group. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal.Coal miningCoal miningCoal mining is the process of extractingcoal from the ground or from a mine. Coal is valued for its energy content and since the 1880s has been widely used to generate electricity. In the United Kingdom and South Africa, a coal mine and its structures are a colliery, a coal mine is called a "pit", and above-ground mining structures are referred to as a "pit head". In Australia, "colliery" generally refers to an underground coal mine.Richter scaleThe Richter scale (), also called the Richter magnitude scale, Richter's magnitude scale, and the Gutenberg–Richter scale, is a measure of the strength of earthquakes, developed by Charles Richter in collaboration with Beno Gutenberg, and presented in Richter's landmark 1935 paper, where he called it the "magnitude scale". This was later revised and renamed the local magnitude scale, denoted as ML or ML.

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