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1999 Winsford railway accident

Railway accidents and incidents in CheshireRailway accidents in 1999Train collisions in England

On 23 June 1999, a Virgin Trains electric express train from London Euston to Glasgow Central, hauled by Class 87 No 87027 Wolf of Badenoch, ran into an empty First North Western four-carriage Pacer unit, injuring 27 people. The express had been travelling at about 110 mph (180 km/h), but driver Roy Eccles noticed the Pacer on the line and was able to decelerate to about 50 mph (80 km/h) at the time of impact. Eccles was awarded a medal for his prompt action, which averted a much more serious accident. The driver of the Pacer train helped passengers from the Glasgow Central train despite his injuries.The Pacer had passed a signal at danger and run through a set of points, coming to a stand on the line on which the express was approaching. Its rear cab was destroyed in the crash along with a section of the passenger accommodation, and the coach bodies were displaced from their underframes. The incident report stated that the accident was most likely to have been human error of the Pacer driver as the investigation showed no faults with either the signalling system or the brakes of the Pacer train. Due to the severe level of damage sustained by the Pacer train, the safety of the units were investigated as part of the inquiry into the accident.

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1999 Winsford railway accident
Clive Back Lane,

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N 53.18501 ° E -2.48963 °
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Clive Back Lane

Clive Back Lane
CW7 3NX
England, United Kingdom
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Cheshire Plain
Cheshire Plain

The Cheshire Plain is a relatively flat expanse of lowland within the county of Cheshire in North West England but extending south into Shropshire. It extends from the Mersey Valley in the north to the Shropshire Hills in the south, bounded by the hills of North Wales to the west and the foothills of the Pennines to the north-east. The Wirral Peninsula lies to the north-west whilst the plain merges with the South Lancashire Plain in the embayment occupied by Manchester to the north. In detail, the plain comprises two areas with distinct characters, the one to the west of the Mid Cheshire Ridge and the other, larger part, to its east. The plain is the surface expression of the Cheshire Basin, a deep sedimentary basin that extends north into Lancashire and south into Shropshire. It assumed its current form as the ice-sheets of the last glacial period melted away between 20,000 and 15,000 years ago leaving behind a thick cover of glacial till and extensive tracts of glacio-fluvial sand and gravel. The primary agricultural use of the Cheshire Plain is dairy farming, creating the general appearance of enclosed hedgerow fields. Meteorologists use the term Cheshire Gap when referring to the lowlands of the Cheshire Plain, providing as they do a passage between the Clwydian Hills, in Wales on the one hand and the Peak District and South Pennines on the other. Weather systems are often guided down this "gap", penetrating much further inland than elsewhere along the coast of the Irish Sea.