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River Wheelock

Cheshire geography stubsEngland river stubsRivers of CheshireRivers of StaffordshireStaffordshire geography stubs
Weaver catchment
Woods and Stream geograph.org.uk 155178
Woods and Stream geograph.org.uk 155178

The River Wheelock is a small river in Cheshire in north west England. It drains water from the area between Sandbach and Crewe, and joins the River Dane at Middlewich (grid reference SJ693669), and then the combined river flows into the River Weaver in Northwich. Alternative names for the river have were recorded in 1619 as Sutton Watter, Sutton Brooke, and Lawton Brooke.Early recorded variations of the name Wheelock have included Quelok, Qwelok, Whelok, Whelocke, with later forms using Wheelock Watter and Wheelock Brooke. The name is said to mean "winding river" and it is reported to have based on the Old Welsh word chwylog, the chwyl part of which means "a turn, a rotation, a course", with an adjective suffix of og. The river has given its name to the large village of Wheelock.

Excerpt from the Wikipedia article River Wheelock (License: CC BY-SA 3.0, Authors, Images).

River Wheelock
Beechfield Drive,

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Latitude Longitude
N 53.19747 ° E -2.4586 °
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Beechfield Drive

Beechfield Drive
CW10 9QE
England, United Kingdom
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Woods and Stream geograph.org.uk 155178
Woods and Stream geograph.org.uk 155178
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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.