Radnorshire is a sparsely populated area, one of thirteen historic and former administrative counties of Wales. It is represented by the Radnorshire area of Powys, which according to the 2011 census, had a population of 25,821. The historic county was bounded to the north by Montgomeryshire and Shropshire, to the east by Herefordshire, to the south by Brecknockshire and to the west by Cardiganshire.
The Gloucestershire Wildlife Trust is the Gloucestershire local partner in a conservation network of 46 Wildlife Trusts. The Wildlife Trusts are local charities with the specific aim of protecting the United Kingdom's natural heritage. The Gloucestershire Wildlife Trust is managed by a Board of Trustees elected from its membership who provide overall direction for the development of the Trust and there are Advisory Committees. The work of the trust is carried out through staff and volunteers.
The River Teifi in Wales forms the boundary for most of its length between the counties of Ceredigion and Carmarthenshire, and for the final 3 miles (4.8 km) of its total length of 76 miles (122 km), the boundary between Ceredigion and Pembrokeshire. Its estuary is northwest of Cardigan. Teifi has formerly been anglicised as "Tivy".
The Cotswold Water Park is the United Kingdom's largest marl lake system, straddling the Wiltshire–Gloucestershire border, northwest of Cricklade and south of Cirencester. There are 180 lakes, spread over 42 square miles (110 km2).
Radnor Forest in the county of Radnorshire, Wales is a rock dome composed of Silurian shales, mudstones and limestone in Mid Wales. It is a forest in the medieval sense of the word. It lies within the Welsh Marches region since Offa's Dyke lies nearby to the east.
The Wye Valley Area of Outstanding Natural Beauty is an internationally important protected landscape straddling the border between England and Wales.
Clyro is a village and community in Radnorshire, Powys, Wales, with 781 inhabitants as of the 2011 UK Census. The nearest town is Hay-on-Wye, some 1.5 miles (2.4 km) to the south-east.
Rhos Goch National Nature Reserve, located near Painscastle on the England/Wales border, is one of the largest raised bogs in mid and south Wales.
Gwent Wildlife Trust (GWT) is a wildlife trust covering the area between the lower Wye and Rhymney rivers which forms the vice county of Monmouthshire in south-east Wales. It is a registered charity and a member of the Wildlife Trusts Partnership.
The geology of Monmouthshire in southeast Wales largely consists of a thick series of sedimentary rocks of different types originating in the Silurian, Devonian, Carboniferous, Triassic and Jurassic periods.
Elenydd is an upland area of Mid Wales, extending across parts of northern and eastern Ceredigion and Powys between Aberystwyth and Rhayader. Elenydd is also a name given to the medieval commote of Cwmwd Deuddwr which covered approximately the same area.
Portrack Marsh Nature Reserve is a 50 acres (20 ha) reserve by the northern bank of the River Tees between the Tees Barrage and the Tees Viaduct, near Portrack housing estate in Stockton-on-Tees borough, County Durham. It is the last remaining wetland on the lower Tees. The site is bounded by Marston Road, a disused railway line, the Northumbrian Water's waste water treatment site, the River Tees, the Tees Barrage White Water Course, the grounds of The Talpore pub and a Tees Barrage access road.
Lower Wye Gorge is a 65-hectare (160-acre) biological and geological Site of Special Scientific Interest in Gloucestershire, notified in 1954 and renotified 1987. The site includes two Gloucestershire Wildlife Trust nature reserves being Ban-y-gor Wood and Lancaut. The Natural England citation states a revision for Lancaut inclusion.
Upper Wye Gorge is a Site of Special Scientific Interest (SSSI), noted for its biological and geological characteristics, around Symonds Yat in the Wye Valley on the Wales–England border. The site is listed in the 'Forest of Dean Local Plan Review' as a Key Wildlife Site (KWS).
Gwaunceste Hill is a 542-metre-high hill in the county of Powys in east Wales. It falls within the communities of Gladestry and Glascwm around 4 km east of the village of Hundred House and about 2 km north of the hamlet of Glascwm. The headwaters of the River Arrow gather on the eastern slopes of the hill. Drainage of its western slopes is into the River Edw, a tributary of the River Wye. Two subsidiary tops to the southeast and southwest are both known as ‘Little Hill’.
The Chafford Gorges Nature Park is a 200-acre (81 ha) nature reserve located in Chafford Hundred, England and managed by the Essex Wildlife Trust. It includes two Sites of Special Scientific Interest. Grays Thurrock Chalk Pit has been designated for its biological interest, and Lion Pit for geological interest.
Painscastle is a village and community in Powys, Wales which takes its name from the castle at its heart. It lies between Builth and Hay-on-Wye, approximately 3 miles from the Wales-England border today. The community also includes the villages and settlements of Rhosgoch, Bryngwyn, Llandeilo Graban and Llanbedr. The population as of the 2011 UK Census was 524. It is represented by the Painscastle and Rhosgoch Community Council, which comprises eight community councillors. It is included in the Glasbury electoral ward for Powys County Council elections.
The Begwns, or sometimes The Begwyns, is a small upland area in eastern Powys, Wales. They sit within the communities of Painscastle, Glasbury and Clyro, to the north of a great bend in the course of the Wye valley, west of Hay-on-Wye. ‘Begwns' is a cymricisation of the English ‘beacons’. The Begwns are 1293 acres of common land which was given to the National Trust by the Maesllwch Estate in 1992 and managed for grazing and quiet recreation. The common ranges in elevation from 250m at its lowest to 415m at ‘The Roundabout’, a hilltop wooded feature at the heart of the area. A trig point immediately outside of this enclosure is 1m lower. The trees were planted here to commemorate Queen Victoria’s Diamond Jubilee with a wall constructed around them in 1887 for protection.
The geology of Snowdonia National Park is dominated by sedimentary and volcanic rocks from the Cambrian and Ordovician periods with intrusions of Ordovician and Silurian age. There are Silurian and Cenozoic sedimentary rocks on the park's margins. The succession was intensely faulted and folded during the Caledonian Orogeny. The region was uplifted as the North Atlantic Ocean opened during the Cenozoic. The current mountainous landscape arises from repeated glaciations during the Quaternary period.
