Everything about Wye Valley totally explained
» This article is about the river valley along the Anglo-Welsh border. For other rivers named "Wye", see River Wye (disambiguation)
The
Wye Valley Area of Outstanding Natural Beauty (AONB) is an internationally important protected landscape straddling the border between
England and
Wales. It is one of the most dramatic and scenic landscape areas in southern Britain.
The
River Wye (
Welsh:
Afon Gŵy) is the
fifth-longest river in the
United Kingdom. The upper part of the river passes through the settlements of
Rhayader,
Builth Wells and
Hay-on-Wye, but the area designated as an AONB surrounds only the 72-mile stretch lower down the river, from just south of the city of
Hereford to
Chepstow.
This area covers parts of the counties of
Gloucestershire,
Herefordshire and
Monmouthshire, and is recognised in particular for its
limestone gorge scenery and dense native woodlands, as well as its wildlife, archaeological and industrial remains. It is also historically important as one of the birthplaces of the modern
tourism industry. The area is predominantly rural, and many people make a living from tourism, agriculture or forestry.
Ross-on-Wye is the only town within the AONB itself, but Hereford,
Monmouth,
Coleford and Chepstow lie just outside its boundaries.
Geology
The varied landscapes of the Wye Valley can be explained by underlying rocks and structures, and how ice and then the river and tributary streams have acted upon them through time.
Close to Hereford, the geology of the area around the village of
Woolhope is largely made up of
Silurian limestones,
shales and
sandstones. To the south of this, the Herefordshire lowlands are largely underlain by red
mudstones and
sandstones, producing a redder soil. These rocks are softer than the limestones elsewhere, so the river created more
meanders, a wider
floodplain, and a gentler and more rolling landscape. Around
Symonds Yat, limestones and red sandstones meet. This leads to a landscape of hills and plains, as well as substantial meanders which have formed impressive river cliffs.
The Lower Wye landscape was formed by the river acting on a series of layers of rock that dip towards the
Forest of Dean. Here the river has incised into the margins of the
Old Red Sandstone plateau to form a gorge with substantial river cliffs. The steepest parts of the Wye gorge are cut through the
Carboniferous Limestone. Here the combined action of the river, natural joints in the rocks and quarrying have exposed many vertical faces, particularly between
Tintern and Chepstow.
Geological interest extends underground, and there are many
rock shelters and solution
caves in the area. These include King Arthur's Cave and many others in the area of Symonds Yat. At
St Arvans, near Chepstow, the underground watercourses have carved out long cave systems, which exit at
Otter Hole at the base of Piercefield cliffs — the only cave system in England or Wales which has to be reached through a tidal sump, making it a
mecca for experienced cavers.
Wildlife
The Wye Valley is important for its rich wildlife habitats. The area has three sites of international importance, designated as candidate
Special Areas of Conservation (cSACs) under the
European Union's
Habitats Directive. In national terms, the area is particularly important for
Lesser Horseshoe Bats,
Peregrine Falcons,
ravens, rare
whitebeam,
nightjar and lesser known fish like the
shad and
thwaite.
In September 2006 it was reported that one colony of lesser horseshoe bats in the area had reached record numbers, with some 890 bats in a small stone barn. This is believed to be the largest colony of lesser horseshoe bats in England, and one of the largest in Europe.
Archaeology
The valley has been inhabited for at least 12,000 years. Caves near
Symonds Yat and
Chepstow provide evidence of settlement dating from
Palaeolithic times, and finds from later stone ages have also been found. These have yielded evidence of how prehistoric human populations lived as nomadic hunters and traders.
Standing stones at
Huntsham,
Staunton, and
Trellech all have origins dating back to the
Bronze Age. Later,
Iron Age forts along the lower Wye Valley, and in the Woolhope area, took advantage of the natural hilltops and promontories to form well-defended settlements. It is likely that many of these marked the edges of disputed tribal pre-Roman territories.
Watling Street ran through the
Roman settlements of Ariconium (just north of Ross on Wye) and
Blestium (Monmouth), and a number of other small Roman settlements are known. The first evidence of the exploitation of iron and coal in the valley is found in the Roman period, with iron working known from sites at
Monmouth,
Trellech and elsewhere, as well as in the adjoining
Forest of Dean. The medieval boroughs of
Goodrich and Chepstow, at each end of the Wye Gorge, may have originally been established at this time.
Closely following the River Wye,
Offa's Dyke was built in the 8th century under
King Offa to mark out the boundary between England and Wales and is, today, the longest archaeological monument in Britain.
Offa's Dyke Path long distance footpath today traces the route through the Wye valley.
The medieval period
When the
Normans conquered the region in the eleventh century they immediately built major
castles at
Chepstow and
Monmouth to defend the territory. Smaller castles were built at
Goodrich and
St Briavels.
Tintern Abbey was founded in 1131 by
Cistercian monks, and largely rebuilt in the thirteenth century. It is the best-preserved
medieval abbey in
Wales and an outstanding example of
Gothic architecture.
Many of the smaller villages in the area probably date from the Middle Ages, and much of this expansion was probably associated with the early
iron industry. The medieval iron industry consumed large quantities of
charcoal and much of the woodland was
coppiced for this purpose.
Trellech was one of the largest communities in Wales during this period.
The development of industry
The Lower Wye Valley can claim to be a birthplace of the
Industrial Revolution.
Iron has been made in the Wye Valley since
Roman times, using the ready supply of timber, good quality ore and abundant
charcoal from the
Forest of Dean. The river provided transport for the raw materials and finished product, and with the introduction of the
blast furnace in the 1500s, its tributaries began to be used for water power.
The first
brass made in Britain was founded at
Tintern in 1566.
Wire-making followed, with water mills situated on all the tributaries of the lower Wye. The area resounded to the noise and smoke of heavy industry for the next 400 years and gave rise to many pioneering industries. For instance,
Whitebrook became famous for paper milling, when
wallpaper became a fashionable way to decorate houses. At
Redbrook,
copper works were established by 1691, and a century later the village became one of the world's major
tinplate manufacturing centres. This industry survived until the 1960's and was renowned for producing the thinnest, highest quality plate in the world. The
Lydbrook valley was also a thriving centre for metal industries, such as the manufacture of telegraph cables.
The valley woodlands were carefully managed to produce mature trees for
shipbuilding, or by coppicing for
charcoal, and to provide bark for
tanning. The valley industries were also massive consumers of timber. A ship of 150 tons, for example, required 3,000 wagonloads of timber to complete — and in 1824, 13 ships were launched at
Brockweir alone.
The river was the economic backbone of the region, providing an important means of transport, trade and communication. In late medieval times,
salmon weirs hindered free passage on the river, but the Wye Navigation Act in 1662 enabled the river's potential to be developed. By 1727 shallow draught boats could get upstream beyond Hereford, and a significant shipbuilding industry developed at Monmouth,
Llandogo, Brockweir and Chepstow. However, by 1835 it was stated that the Wye
"can scarcely be considered a commercial highway" above Monmouth, and by the 1880s Brockweir bridge was the effective upper limit of navigation.
As the 19th century progressed, the valley's industries gradually declined, and management of the woodlands lessened when there was no longer a ready market for their products.
The origins of British tourism
The Wye Valley witnessed the birth of British
tourism in the eighteenth century. The earliest known appreciation of the area's spectacular beauty can be dated to the beginning of the century, when
John Kyrle developed the 'Prospect' at
Ross-on-Wye, and it was later mentioned in verse by
Alexander Pope.
In 1745,
John Egerton, later
Bishop of Durham, started taking friends on boat trips down the valley from the rectory at Ross. The area became more widely known following the publication of works by the poet
Thomas Gray, and, in particular,
Observations on the River Wye by the Reverend
William Gilpin, published in 1782. The first illustrated tour guide to be published in Britain, it helped travellers locate and enjoy the most "
Picturesque" aspects of the countryside. Regular excursions began to be established from Ross, the boat journey to
Chepstow taking two days.
Some of the most famous poets, writers and artists of the day made the pilgrimage to the great sights of
Goodrich,
Tintern and
Chepstow — among them
Coleridge,
Thackeray and
Turner.
Wordsworth was also captivated by the area, writing
Lines Written a Few Miles Above Tintern Abbey in 1798.
The first of Britain's great landscapes to be 'discovered', the Wye Valley's particular attraction was its river scenery, and the many guidebooks, engravings and paintings ensured a continuing steady stream of visitors. Viewpoints were specially constructed, including the
Kymin above
Monmouth, with its round house giving panoramic views across the town. Another highlight for travellers was the cliff ascent and walks at
Piercefield. However, most of the truly 'Picturesque' scenes were sketched from river level, with the shimmering water as the foreground for the forests and cliffs behind, and the castle and abbey ruins.
Transport
In 1813 the Monmouth Tramroad linked
Coalway (near
Coleford),
Redbrook and
Monmouth. This was the world's first railed-way to make specific powers in its Act of Parliament to allow for the charging of fares to passengers.
The standard gauge railway line between Chepstow, Monmouth and Ross opened much later, in 1876. This made the valley more accessible and popular to tourists. In the early 1900s, crowds of up to 1300 would travel on a special train journey to see
Tintern Abbey on the night of the harvest moon. The line closed to passengers in 1959, although sections remain as bridleways and footbridges.
The road network in the lower Wye valley remained essentially undeveloped during the rise of the Valley's industrialisation, until a series of
Turnpike trusts were authorised during the 18th century. It wasn't until 1828 that the current Wye Valley road, the
A466, was first constructed.
The area became more accessible to much of the country with the building of the
M50 between the
M5 and Ross-on-Wye, and the opening of the
Severn Bridge (now part of the
M48) in 1966.
Management of the area
The Wye Valley Area of Outstanding Natural Beauty (
AONB) was first designated in 1971. The designation indicates the importance of recognising and preserving the area's distinctive qualities, for the benefit of present and future generations.
Administratively the area is very complex, being the only protected landscape to straddle the border between England and Wales. The Counties of Herefordshire, Monmouthshire and Gloucestershire are each in a different government region.
Co-ordination of conservation across these political boundaries is undertaken by an AONB unit and Joint Advisory Committee. A Management Plan for the AONB enlists a range of partners in conserving and enhancing its beauty for the benefit of present and future generations.
The navigation of the tidal part of the Wye (below
Bigsweir) comes under the control of the
Gloucester Harbour Trustees as Competent Harbour Authority.
Further Information
Get more info on 'Wye Valley'.
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