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Kington Rural

Civil parishes in HerefordshireUse British English from July 2022
Hergest court geograph.org.uk 957989
Hergest court geograph.org.uk 957989

Kington Rural is a civil parish in west Herefordshire, England, and is approximately 17 miles (30 km) north-west from the city and county town of Hereford. The parish borders Wales at the west, and contains the hamlets and small settlements of Upper Hergest, Lower Hergest, Chickward, Bredward, and Kingswood at the south, and Bradnor Green and Rushok at the north. The nearest town is the market town of Kington which, with its parish, is to a large extent enclosed by Kington Rural. Significant landmarks of the parish are the Castle Twts motte and bailey earthwork, Hergest Court 15th-century manor house, and Hergest Ridge on the England–Wales border.

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

Kington Rural
Upper Hergest,

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Wikipedia: Kington RuralContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 52.1952 ° E -3.0713 °
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Address

Upper Hergest

Upper Hergest
HR5 3EN , Kington Rural
England, United Kingdom
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Hergest court geograph.org.uk 957989
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Nearby Places

Stanner Rocks

Stanner Rocks is a rounded hill, steep in parts, which lies close to the Wales border with England between Walton and Kington. A superb collection of wild plants can be found here. Where it faces south, warm sunshine and drying winds create an ideal environment for plants which are more likely to be seen around the Mediterranean. The most famous of Stanner Rocks’ specialties is the pretty and elusive Radnor Lily, having small, starry yellow flowers. The Stanner-Hanter Complex refers to the set of rocks which outcrop at Stanner Hill and the nearby Hanter Hill and Worsel Wood and which have long been considered to be the oldest in Wales, having been dated to around 700 million years BP using the rubidium-strontium dating method. They comprise gabbro, diorite and granite. Little modern research has been undertaken on the Complex. The rocks have been variously described as a hypersthene trap (Murchison 1867); an Archean ridge (Calloway1879); a Carboniferous laccolith (Raw 1904); a Tertiary igneous complex (Watts 1906); and a Carboniferous intrusion (Pocock & Whitehead 1935). Holgate & Knight-Hallowes (1941) suggested a Precambrian origin based on the occurrence of dolerite clasts associated with Longmyndian sediments in a nearby quarry. Much of the confusion must relate to the fault-bounded nature of the Complex which gives no direct stratigraphic control of its age of formation. In the late 1970s the general acceptance of the theory of plate tectonics resulted in a re-investigation of the Precambrian and Paleozoic igneous rocks of southern Britain. Thorpe et al. (1984) made the earliest developments by identifying the calc-alkaline nature of many of these exposures and interpreting this evidence as the product of Precambrian subduction. The Stanner - Hanter Complex was not part of this study, perhaps because of its considerable alteration or possibly owing to the limited range of rock types. In 1980 the publication of a Rb/Sr isotopic age of 702 ± 4 Ma by Pachett et al. confirmed the Neoproterozoic age of the Complex whilst establishing it as the oldest dated rock sequence in southern Britain. More extensive dating of Avalonian rocks both in southern Britain and Maritime Canada has allowed Avalonian subduction to be refined into several stages. Gibbons & Hõrak (1996) grouped the Stanner-Hanter Complex with the Malverns Complex placing both within Avalonian Event 1, the early arc-construction phase, which has been dated at 677Ma. Implicit in this interpretation, however, is the assumption that the Stanner-Hanter rocks have a calc-alkaline composition. Slightly older dolerites and gabbros in the Avalonian of Newfoundland have a more primitive oceanic affinity related to the rifting and formation of primitive oceanic crust.

Church of St Mary, Kington
Church of St Mary, Kington

The Church of St Mary, or St. Mary the Virgin Church, Kington, Herefordshire, England is a Grade I listed parish church. The church was established c. 1300, but is much-altered. It has a 12th-century tower, originally free-standing, and included in the church when the latter was extended in the 13th century. A double broach spire was added in the 18th century. The tower houses a six-bell ring. Five were made by Rudhall of Gloucester between 1736 and 1739, including the tenor, which weighs 11 long cwt 23 lb (1,255 lb or 569 kg) and is in the key of F-sharp. The other bell was made by William Evans of Chepstow in 1764. The bells were refurbished in 1978 by the Whitechapel Bell Foundry. The church also has an organ made by J. W. Walker & Sons Ltd, installed in the North chancel chamber in 1883 and improved and refurbished by Henry Willis & Sons in 1959. The lychgate is constructed from carved stone, dates from the 18th century, and has its own Grade II* listing. Its design is unusual, with a domed roof capped with a finial, and open arches set into each wall.Inside the church is an alabaster monument to Sir Thomas Vaughan (died 1469 at the Battle of Edgecote Moor) and his wife Elen Gethin.The church was Grade I listed in October 1953, giving it legal protection from unauthorised alteration or demolition. It is part of the Diocese of Hereford and is one of five (three in England, two in Wales) that are jointly administered as the "Kington Parishes"'.