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Twinhills Woods and Meadows

Forests and woodlands of SomersetMeadows in SomersetSites of Special Scientific Interest in SomersetSites of Special Scientific Interest notified in 1990Use British English from July 2014
Woodland Sites of Special Scientific Interest
Twinhillswood
Twinhillswood

Twinhills Woods and Meadows (grid reference ST558432) is a 21.2 hectare (52.4 acre) biological Site of Special Scientific Interest on the Monarch's Way south of Dulcote in Somerset, notified in 1990. Twinhills Woods and Meadows comprise a complex of ancient, semi-natural woodland, neutral and calcareous grassland with associated mature hedges and areas of shrub growth. Further interest is added by the presence of numerous butterfly species on the site. A total of 26 species have been recorded including grizzled skipper (Pyrgus malvae), white-letter hairstreak (Satyrium w-album), green-veined white (Pieris napi), brown argus (Aricia agestis), marbled white (Melangargia galthea), silver-washed fritillary (Argynnis paphia) and marsh fritillary (Eurodryas aurinia).The site is crossed by the Monarch's Way long distance footpath.

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Twinhills Woods and Meadows
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N 51.18631 ° E -2.6338 °
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Dulcote Quarry
Dulcote Quarry

Dulcote Quarry is a disused limestone quarry at Dulcote, near Wells on the Mendip Hills, Somerset, England. The quarry measures around 600 metres (2,000 ft) from West to East and around 350 metres (1,150 ft) from North to South, with an area of 18 acres (7.3 ha), which is surrounded by 80 acres (32 ha) of woodland.The site has been used for quarrying since the mid-19th century. The Foster Yeoman Company was founded at Dulcote, in 1923, and later became part of Aggregate Industries. The site achieved an output of approximately 0.25M tonnes per year of Carboniferous Limestone, for general purpose construction aggregates. Much of the stone was moved on the Cheddar Valley Line (a branch line of the Great Western Railway) by an independent company which became known as Mendip Rail.A Geodiversity audit of the site was carried out in 2004, which highlighted the limestone strata and fossils identified. These include Carboniferous Limestone overlain by Triassic Mercia Mudstones and Sandstones with geodes, which were formed by siliceous mineral replacement.In 2007 the quarry was bought by the Kilbride group, a subsidiary of Kilmartin Holdings which itself became part of Hansteen Holdings. When the parent company went into receivership the part owning Dulcote survived and put the worked-out quarry site up for commercial redevelopment with outline planning permission for a price of £1.5 million. In 2016 the site was bought for development as a food production site for Charlie Bigham's, which opened in 2017. In March 2022, a multi-user path (part of the Strawberry Line) connecting the end of the Wells-Dulcote railway path at Dulcote underpass to the quarry entrance was officially opened.

St John's Priory, Wells
St John's Priory, Wells

St John's Priory in Wells, Somerset, England, from the 14th century. Along with its boundary walls and railings it has been designated as a Grade I listed building.The initial development was as a hospital for poor, aged and sick men by 1210. The original foundation was by Jocelin of Wells, after his consecration in 1204, along with his brother Hugh of Wells.It was made into a priory in 1350 providing accommodation for a prior, chaplain and ten brothers, which lasted until the dissolution of the monasteries when it had an income of £40 per year. It then became crown property until 1575 when it was given to Sir Christopher Hatton and later became the property of Baron Brooke.Land was donated to St John's in both 1667 and 1716.The former priory building may also have been used as a guest house for visitors to Wells Cathedral and the Bishop's Palace. There was a cemetery associated with the building. The history of the buildings is set out in 33 deeds including one from 1738 which is displayed in the dining room.The land surrounding the priory was disturbed and remaining archaeological remains destroyed around 1850 when new roads and a school were built on the site. This also involved demolition of some of the building. In the 1860s the building was owned by the Lovell family.The two-storey stone building was an open hall but a first floor corridor and bedrooms have been added. The roof is supported by cruck trusses and purlins. Dendochronology has shown the wood used for the roof was felled in the winter of 1313 to 1314.