Clun and Chapel Lawn

Clun (Welsh: Colunwy) is a town in south west Shropshire, England, and the Shropshire Hills Area of Outstanding Natural Beauty. The 2011 census recorded 680 people living in the town. Research by the Campaign for the Protection of Rural England suggests that Clun is one of the most tranquil locations in England.

Clun Town Hall is a municipal building in The Square in Clun, Shropshire, England. The building, which is now used as a museum, is a Grade II* listed building.

Clun Castle is a medieval ruined castle in Clun, Shropshire, England. Clun Castle was established by the Norman lord Robert de Say after the Norman invasion of England and went on to become an important Marcher lord castle in the 12th century, with an extensive castle-guard system. Owned for many years by the Fitzalan family, Clun played a key part in protecting the region from Welsh attack until it was gradually abandoned as a property in favour of the more luxurious Arundel Castle. The Fitzalans converted Clun Castle into a hunting lodge in the 14th century, complete with pleasure gardens, but by the 16th century the castle was largely ruined. Slighted in 1646 after the English Civil War, Clun remained in poor condition until renovation work in the 1890s. Today the castle is classed as a Grade I listed building and as a Scheduled Monument. It is owned by the Duke of Norfolk, who also holds the title of Baron Clun, and is managed by English Heritage.

The 1990 Bishop's Castle earthquake occurred near the town of Bishop's Castle, Shropshire, England on 2 April.

Radnor Wood is a small forest east of the small town of Clun, Shropshire, England covering an area of 1.5 km2. The wood can be easily accessed via the B4368 which passes through Clun and to the south of the forest. It is located on top of a hill which reaches 326 metres above sea level. This point is one of the highest areas in the valley formed by the River Clun. The hill is mainly limestone and this abundance of limestone was discovered by the Romans. Early quarries have been found on the top of the hill and two recent disused quarries can be found at the base of the hill. Once part of one vast forest (the Clun Forest), Radnor Wood is considered small in comparison to the nearby woods such as: Hoar Wood Withins Wood

Bicton (or previously sometimes Bickton) is a hamlet in southwest Shropshire, England, one mile north of Clun. The short River Unk passes through the hamlet. In previous centuries it was a township in the Clun division of the hundred of Clun.The Bicton Burial Circle is a prehistoric stone circle, located south of the settlement between the River Unk and River Clun. Two barrows are seen as circular crop marks. The cremation at the burial site is suspected to belong to the Beaker period.The hamlet has been in existence for centuries. Although not listed in the 1086 Domesday Book, it is mentioned in county court papers dating from 1221, in which the county ruled that John Fitzalan I, Lord of Clun, was right to claim that Bicton belonged to his fiefdom.Little remains of Bicton Castle, also known as Bicton Motte, a motte and bailey dating from the 11th or 12th century. The motte's height is 2.2 metres today, as parts have been dug away during gravel extraction. Originally it was circular, with a diameter of 30 metres. The small bailey measured 14 by 25 metres. The castle is classified as E3: "feeble or damaged earthworks". Its location on the River Unk, like its counterpart in Newcastle on the River Clun, suggest it served as a forward defence of Clun Castle against the Welsh, rather than as an instrument of exploitation. When after the Norman Conquest Picot de Say was Lord of Clun, other nearby minor castles such as Hopton and Acton provided him with military service, so it is assumed that the same applied to Bicton Castle.Records show that agricultural work took place at Bicton at least in the 14th century. Its fields were among the most fertile in the Clun Valley. They were occupied by Welsh bondsmen, unfree tenants farming open fields. It was the location of a demesne sheep stint for 300 animals owned by the Fitzalans in the early 14th century. In 1354 a worker was paid four bushels of rye for spreading dung for seven weeks; and there is a later account of the same activity in 1372. In 1355 sixty Welshmen provided mowing services to the manor at Bicton. In 1373 240 sheared sheep were sent from nearby Clunton and Kempton to the reeve of Bicton. Swapping flocks of sheep between the locations of Bicton, Newton, Kempton, and Clunton was a recurring event throughout the second half of the 14th century. Bicton Farm has been farmed by the same family for centuries. The farm has one of the four water mills on the River Unk. Records from 1919 show activities of agroforestry.A 14th century court known as "hallmoot of the Welsh" is presumed to have met at times at Bicton. The unfree tenants of the Lord of Clun's demesne were tried here.

Coalbrookdale Formation, earlier known as Wenlock Shale or Wenlock Shale Formation and also referred to as Herefordshire Lagerstätte in palaeontology, is a fossil-rich deposit (Konservat-Lagerstätte) in Powys and Herefordshire at the England–Wales border in UK. It belongs to the Wenlock Series of the Silurian Period within the Homerian Age (about 430 million years ago). It is known for its well-preserved fossils of various invertebrate animals many of which are in their three-dimensional structures. Some of the fossils are regarded as earliest evidences and evolutionary origin of some of the major groups of modern animals.Roderick Murchison first described the geological setting of Coalbrookdale Formation by which he gave the name Silurian in 1935, referring to the Silures, a Celtic tribe of Wales. It is assigned to the Wenlock Group in 1978 based on the age of crustacean fossils found around the region. Robert J. King of the University of Leicester discovered the first unique fossil in 1990. The fossil, an arthropod was reported in 1996 and described in 2000 as Offacolus kingi. Since then, over 30 species of arthropods, polychaete worms, sponges, mollusks, echinoderms, and lobopods have been described; with about 30 species in store yet to be identified.

Acton is a village in Shropshire, England, south of Bishop's Castle.

Whitcott Keysett is a hamlet in south Shropshire, England. It is located two miles northwest of the small town of Clun. The west half of the settlement lies in the civil parish of Newcastle-on-Clun whilst the east half lies in Clun.

The Redlake is a minor river in southwest Shropshire, England. Its headwaters are to the south of Newcastle, on the other side of Spoad Hill (alternatively Springhill).It flows through Treverward, Purlogue, New Invention, Chapel Lawn, Bucknell and Coxall, before discharging into the River Clun at Jay. The last part of the river, through Adley Moor, is in Herefordshire.

Chapel Lawn is a small village in southwest Shropshire, England, located within the Redlake Valley, some three miles south of the small town of Clun. Chapel Lawn lies in an Area of Outstanding Natural Beauty bounded to the north by Bryneddin Wood, an ancient deciduous wood containing extensive plantings of Sessile Oak. On Caer Caradoc, a 399-metre (1,309 ft) hill less than 1 kilometre south of the village, can be found an Iron Age fort with mounds and ditches well defined and scheduled by English Heritage.

Caer Caradoc (Chapel Lawn) (Welsh – Caer Caradog) is an Iron Age hill fort and Scheduled Monument in the south-west of the English county of Shropshire, near the town of Clun. It overlooks the village of Chapel Lawn. It is located within an area of Open Access land and can be reached via a public footpath between the farms of Wax Hall to the west and Bryncambric to the east. This hill fort has the same name as another, Caer Caradoc near Church Stretton, also in Shropshire but 16 miles (26 km) to the north-east.