Hay-on-Wye, known locally as Hay, is a market town and community in Powys, Wales, in the historic county of Brecknockshire. With over twenty bookshops, it is often described as a "town of books"; it is both the National Book Town of Wales and the site of the annual Hay Festival.
The Welsh Marches is an imprecisely defined area along the border between England and Wales in the United Kingdom. The precise meaning of the term has varied at different periods.
Until 1974, Brecknockshire, also formerly known as the County of Brecknock, Breconshire, or the County of Brecon, was an administrative county in the south of Wales, later classed as one of the thirteen historic counties of Wales. Named after its county town of Brecon, the county was mountainous and primarily rural.
Old Red Sandstone, abbreviated ORS, is an assemblage of rocks in the North Atlantic region largely of Devonian age. It extends in the east across Great Britain, Ireland and Norway, and in the west along the eastern seaboard of North America. It also extends northwards into Greenland and Svalbard. These areas were a part of the paleocontinent of Euramerica (Laurussia). In Britain it is a lithostratigraphic unit to which stratigraphers accord supergroup status and which is of considerable importance to early paleontology. The presence of Old in the name is to distinguish the sequence from the younger New Red Sandstone which also occurs widely throughout Britain.
The known history of Herefordshire starts with a shire in the time of King Athelstan, and Herefordshire is mentioned in the Anglo-Saxon Chronicle in 1051. The first Anglo-Saxon settlers, the 7th-century Magonsætan, were a sub-tribal unit of the Hwicce who occupied the Severn valley. The Magonsætan were said to be in the intervening lands between the Rivers Wye and Severn. The undulating hills of marl clay were surrounded by the Welsh mountains to the west; by the Malvern Hills to the east; by the Clent Hills of the Shropshire borders to the north, and by the indeterminate extent of the Forest of Dean to the south. The shire name first recorded in the Anglo-Saxon Chronicle may derive from "Here-ford", Old English for "army crossing", the location for the city of Hereford.
The Black Mountains are a group of hills spread across parts of Powys and Monmouthshire in southeast Wales, and extending across the England–Wales border into Herefordshire. They are the easternmost of the four ranges of hills that comprise the Brecon Beacons national park, and are frequently confused with the westernmost, which is known as the Black Mountain. The Black Mountains may be roughly defined as those hills contained within a triangle defined by the towns of Abergavenny in the southeast, Hay-on-Wye in the north and the village of Llangors in the west. Other gateway towns to the Black Mountains include Talgarth and Crickhowell. The range of hills is well known to walkers and ramblers for the ease of access and views from the many ridge trails, such as that on the Black Hill in Herefordshire, at the eastern edge of the massif. The range includes the highest public road in Wales at Gospel Pass, and the highest point in southern England at Black Mountain.
Archenfield is the historic English name for an area of southern and western Herefordshire in England. Since the Anglo-Saxons took over the region in the 8th century, it has stretched between the River Monnow and River Wye, but it derives from the once much larger Welsh kingdom of Ergyng.
The River Frome is a river in Herefordshire, England. It flows through Bromyard, and Bishops Frome. Immediately below the depopulated village of Stretton Grandison its tributary, the river or brook named the Lodon, joins it. It then flows west, past Yarkhill and the farmstead or locality of Prior's Frome before its confluence with the Lugg at Hampton Bishop about 2 miles (3.2 km) before the latter joins the Wye.
The Golden Valley is the name given to the valley of the River Dore in western Herefordshire, England. The valley is a picturesque area of gently rolling countryside. It lies in the lee of the Black Mountains, Wales.
The Wye Valley is a valley in Wales and England. The River Wye is the fourth-longest river in the United Kingdom.
Dorstone Castle was in the village of Dorstone in Herefordshire, England, located 6 miles to the east of Hay-on-Wye.
Ewyas Harold Castle was a castle in the village of Ewyas Harold in Herefordshire, England.
The geology of Wales is complex and varied; its study has been of considerable historical significance in the development of geology as a science. All geological periods from the Cryogenian to the Jurassic are represented at outcrop, whilst younger sedimentary rocks occur beneath the seas immediately off the Welsh coast. The effects of two mountain-building episodes have left their mark in the faulting and folding of much of the Palaeozoic rock sequence. Superficial deposits and landforms created during the present Quaternary period by water and ice are also plentiful and contribute to a remarkably diverse landscape of mountains, hills and coastal plains.
Herbert Rowse Armstrong TD MA was an English solicitor and convicted murderer, the only solicitor in the United Kingdom ever hanged for murder. He was living in Cusop Dingle, Herefordshire, England, and practising in Hay-on-Wye, on the border of England and Wales, from 1906 until his arrest on 31 December 1921 for the attempted murder of a professional rival by arsenic poisoning. He was later also charged with, and convicted of, the murder of his wife, the crime for which he was executed.
Ewyas was a possible early Welsh kingdom which may have been formed around the time of the Roman withdrawal from Britain in the 5th century. The name was later used for a much smaller commote or administrative sub-division, which covered the area of the modern Vale of Ewyas and a larger area to the east including the villages of Ewyas Harold and Ewyas Lacy.
The Bishop's Frome Limestone is a rock unit within the Raglan Mudstone Formation of the Old Red Sandstone occurring in the border region between England and South Wales. This limestone is a calcrete, that is to say it originated as a soil during a break in deposition rather than being an original marine deposit. It is perhaps the most significant of all of the calcretes which occur within the uppermost Silurian and lower Devonian sequence of rocks which constitute the Old Red Sandstone of the Anglo-Welsh Basin. It defines the boundary within the basin between the Silurian and the Devonian periods. The rock was formerly known as the Psammosteus Limestone after a characteristic fossil fish recorded from it; Psammosteus anglicus. The fossil remains were subsequently shown to have been wrongly identified and belong in fact to Traquairaspis symondsi. Its modern name derives from the Herefordshire village of Bishop's Frome. Its thickness is variable ranging from 2m up to 8m.
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.
Hay Bluff is a prominent hill at the northern tip of the Black Mountains, an extensive upland massif which straddles the border between south-east Wales and England. The mountain sits at the point where the main northeast-facing escarpment of the Black Mountains meets the northwest facing escarpment, the next peak to the west being Twmpa. The flat summit of Hay Bluff which is marked by a triangulation pillar at a height of 677 metres (2,221 ft) overlooks the middle Wye Valley and the book town of Hay-on-Wye.
Clifford is a village and civil parish in Herefordshire, England, and 2.5 miles (4.0 km) to the north of Hay-on-Wye. It lies on the south bank of the River Wye, which here forms the border between Wales and England. The village sits on the B4350 road. The civil parish includes the hamlets of Priory Wood and Hardwicke.
This article describes the geology of the Brecon Beacons National Park in mid/south Wales. The area gained national park status in 1957 with the designated area of 1,344 km2 (519 sq mi) including mountain massifs to both the east and west of the Brecon Beacons proper. The geology of the national park consists of a thick succession of sedimentary rocks laid down from the late Ordovician through the Silurian and Devonian to the late Carboniferous period. The rock sequence most closely associated with the park is the Old Red Sandstone from which most of its mountains are formed. The older parts of the succession, in the northwest, were folded and faulted during the Caledonian orogeny. Further faulting and folding, particularly in the south of the park is associated with the Variscan orogeny.
