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Lea Hall, Wimboldsley

Cheshire building and structure stubsCountry houses in CheshireGrade II* listed buildings in CheshireGrade II* listed housesHouses completed in the 18th century
United Kingdom listed building stubs
Wimboldsley Lea Hall geograph.org.uk 574470
Wimboldsley Lea Hall geograph.org.uk 574470

Lea Hall is a former country house standing to the northwest of the village of Wimboldsley, Cheshire, England. It dates from the early part of the 18th century, and was built for the Lowndes family. During the 19th century the house was owned by Joseph Verdin. Additions, including dormer windows, were made in the 19th century. During the 20th century the house was divided into three flats. The house is constructed in red brick with ashlar dressings and a tiled roof. It is in two storeys, with an attic and a basement. The roof is large and hipped, with a viewing platform. The entrance front is symmetrical, in five bays, the central bay protruding slightly forward. This bay contains a doorway with a swan's nest pediment decorated with scrolls, and containing a crest with the initials J V (for Joseph Verdin). The authors of the Buildings of England series describe the house as a "perfect brick box, delightful if just a little funny to look at". It is recorded in the National Heritage List for England as a designated Grade II* listed building.

Excerpt from the Wikipedia article Lea Hall, Wimboldsley (License: CC BY-SA 3.0, Authors, Images).

Geographical coordinates (GPS)

Latitude Longitude
N 53.17346 ° E -2.47968 °
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Address

Stanthorne and Wimboldsley


, Stanthorne and Wimboldsley
England, United Kingdom
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Wimboldsley Lea Hall geograph.org.uk 574470
Wimboldsley Lea Hall geograph.org.uk 574470
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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.