River SevernThe River Severn (Afon Hafren, ˈavɔn ˈhavrɛn), at long, is the longest river in Great Britain. It is also the river with the most voluminous flow of water by far in all of England and Wales, with an average flow rate of at Apperley, Gloucestershire. It rises in the Cambrian Mountains in mid Wales, at an altitude of , on the Plynlimon massif, which lies close to the Ceredigion/Powys border near Llanidloes. The river then flows through Shropshire, Worcestershire and Gloucestershire.
Wye ValleyThe Wye Valley Area of Outstanding Natural Beauty (AONB; Dyffryn Gwy) is an internationally important protected landscape straddling the border between England and Wales. The River Wye (Afon Gwy) is the fourth-longest river in the United Kingdom. The upper part passes through Rhayader, Builth Wells and Hay-on-Wye, but the area designated as an AONB covers surrounding a stretch lower down the river, from just south of Hereford to Chepstow.
Welsh peopleThe Welsh (Cymry) are an ethnic group native to Wales. "Welsh people" applies to those who were born in Wales (Cymru) and to those who have Welsh ancestry, perceiving themselves or being perceived as sharing a cultural heritage and shared ancestral origins. Wales is one of the four countries of the United Kingdom. The majority of people living in Wales are British citizens. In Wales, the Welsh language (Cymraeg) is protected by law.
MonmouthMonmouth (ˈmɒnməθ , ˈmʌn- ; Trefynwy meaning "town on the Monnow") is a town and community in Wales. It is situated where the River Monnow joins the River Wye, from the Wales–England border. Monmouth is northeast of Cardiff, and west of London. It is within the Monmouthshire local authority, and the parliamentary constituency of Monmouth. The population in the 2011 census was 10,508, rising from 8,877 in 2001. Monmouth is the historic county town of Monmouthshire although Abergavenny is now the county town.
Forest of DeanThe Forest of Dean is a geographical, historical and cultural region in the western part of the county of Gloucestershire, England. It forms a roughly triangular plateau bounded by the River Wye to the west and northwest, Herefordshire to the north, the River Severn to the south, and the City of Gloucester to the east. The area is characterised by more than of mixed woodland, one of the surviving ancient woodlands in England. A large area was reserved for royal hunting before 1066, and remained as the second largest crown forest in England, after the New Forest.
Bristol ChannelThe Bristol Channel (Môr Hafren, literal translation: "Severn Sea") is a major inlet in the island of Great Britain, separating South Wales (from Pembrokeshire to the Vale of Glamorgan) and South West England (from Devon, Somerset to North Somerset). It extends from the smaller Severn Estuary of the River Severn (Afon Hafren) to the North Atlantic Ocean. It takes its name from the English city and port of Bristol Long stretches of both sides of the coastline are designated as Heritage Coast.
Carboniferous LimestoneCarboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian Epoch of the Carboniferous Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup.
CaerwentCaerwent (Caer-went) is a village and community in Monmouthshire, Wales. It is located about five miles west of Chepstow and 11 miles east of Newport. It was founded by the Romans as the market town of Venta Silurum, an important settlement of the Brythonic Silures tribe. The modern village is built around the Roman ruins, which are some of the best-preserved in Europe. It remained prominent through the Roman era and Early Middle Ages as the site of a road crossing between several important civic centres.
Offa's DykeOffa's Dyke (Clawdd Offa) is a large linear earthwork that roughly follows the border between England and Wales. The structure is named after Offa, the Anglo-Saxon king of Mercia from AD 757 until 796, who is traditionally believed to have ordered its construction. Although its precise original purpose is debated, it delineated the border between Anglian Mercia and the Welsh kingdom of Powys. The earthwork, which was up to wide (including its flanking ditch) and high, traversed low ground, hills and rivers.
Welsh toponymyThe place-names of Wales derive in most cases from the Welsh language, but have also been influenced by linguistic contact with the Romans, Anglo-Saxons, Vikings, Anglo-Normans and modern English. Toponymy in Wales reveals significant features of the country's history and geography, as well as the development of the Welsh language. Its study is promoted by the Welsh Place-Name Society (Cymdeithas Enwau Lleoedd Cymru).
