
The Tanat Valley (
Welsh
Welsh may refer to:
Related to Wales
* Welsh, of or about Wales
* Welsh language, spoken in Wales
* Welsh people, an ethnic group native to Wales
Places
* Welsh, Arkansas, U.S.
* Welsh, Louisiana, U.S.
* Welsh, Ohio, U.S.
* Welsh Basin, during t ...
: ) is a large valley in northern
Powys
Powys ( , ) is a Principal areas of Wales, county and Preserved counties of Wales, preserved county in Wales. It borders Gwynedd, Denbighshire, and Wrexham County Borough, Wrexham to the north; the English Ceremonial counties of England, ceremo ...
, Wales, formed by the course of the
River Tanat
The River Tanat, also known as , is a river in northern Powys, Wales. Its source is close to the Cyrniau Nod mountain, to the north of Lake Vyrnwy. The river flows in a generally east-south-east direction until it joins the River Vyrnwy near L ...
and its tributaries. Situated south of the
Berwyn range
The Berwyn range (Welsh (language), Welsh: ''Y Berwyn'' or ''Mynydd y Berwyn'') is an isolated and sparsely populated area of moorland in the northeast of Wales, roughly bounded by Llangollen in the northeast, Corwen in the northwest, Bala, Gw ...
, the valley forms from at
Llangynog
Llangynog (; ) is a village and community at the confluence of the Afon Eirth and the Afon Tanat at the foot of the Berwyn range in north Powys (previously Montgomeryshire), Wales.
It lies at the foot of the Milltir Cerrig mountain pass ...
from the merger of two narrow valleys, the Cwm Pennant and Cwm Rhiwarth. Various historic sites, including the Iron Age hillfort
Llwyn Bryn-Dinas and the medieval
St Melangell's Church
St Melangell's Church () is a Grade I Listed building, listed medieval building of the Church in Wales located in the former village of Pennant Melangell, in the Tanat Valley, Powys, Wales. The church was founded around the 8th century to comm ...
are located along the valley. Largely agrarian,
sheep farming
Sheep farming or sheep husbandry is the raising and breeding of domestic sheep. It is a branch of animal husbandry. Sheep are raised principally for their meat (lamb and mutton), milk (sheep's milk), and fiber (wool). They also yield sheepskin ...
has formed a major industry in the region for several centuries. Large-scale
slate
Slate is a fine-grained, foliated, homogeneous, metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade, regional metamorphism. It is the finest-grained foliated metamorphic ro ...
and
lead
Lead () is a chemical element; it has Chemical symbol, symbol Pb (from Latin ) and atomic number 82. It is a Heavy metal (elements), heavy metal that is density, denser than most common materials. Lead is Mohs scale, soft and Ductility, malleabl ...
mining in the region lasted from the 16th to late 20th century, although earlier mines possibly existed during the
Iron Age
The Iron Age () is the final epoch of the three historical Metal Ages, after the Chalcolithic and Bronze Age. It has also been considered as the final age of the three-age division starting with prehistory (before recorded history) and progre ...
.
Geology
The
alluvial
Alluvium (, ) is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is ...
valley is primarily composed of
Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years f ...
sedimentary rocks such as
mudstone
Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from ''shale'' by its lack of fissility.Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, ...
and
shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of Clay mineral, clay minerals (hydrous aluminium phyllosilicates, e.g., Kaolinite, kaolin, aluminium, Al2Silicon, Si2Oxygen, O5(hydroxide, OH)4) and tiny f ...
, with smaller amounts of
tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock co ...
and
calcareous rocks
Calcareous () is an adjective meaning "mostly or partly composed of calcium carbonate", in other words, containing lime or being chalky. The term is used in a wide variety of scientific disciplines.
In zoology
''Calcareous'' is used as an adjec ...
. Mineral deposits in the valley include
galena
Galena, also called lead glance, is the natural mineral form of lead(II) sulfide (PbS). It is the most important ore of lead and an important source of silver.
Galena is one of the most abundant and widely distributed sulfide minerals. It crysta ...
,
sphalerite
Sphalerite is a sulfide mineral with the chemical formula . It is the most important ore of zinc. Sphalerite is found in a variety of deposit types, but it is primarily in Sedimentary exhalative deposits, sedimentary exhalative, Carbonate-hoste ...
,
chalcopyrite
Chalcopyrite ( ) is a copper iron sulfide mineral and the most abundant copper ore mineral. It has the chemical formula CuFeS2 and crystallizes in the tetragonal system. It has a brassy to golden yellow color and a Mohs scale, hardness of 3.5 to 4 ...
,
barite
Baryte, barite or barytes ( or ) is a mineral consisting of barium sulfate (Ba S O4). Baryte is generally white or colorless, and is the main source of the element barium. The ''baryte group'' consists of baryte, celestine (strontium sulfate), ...
, and
witherite
Witherite is a barium carbonate mineral, Ba C O3, in the aragonite group. Witherite crystallizes in the orthorhombic system and virtually always is twinned. The mineral is colorless, milky-white, grey, pale-yellow, green, to pale-brown. The spec ...
. The soils are
podzolic
Podzols, also known as podosols, spodosols, or espodossolos, are the typical soils of coniferous or Taiga, boreal forests and also the typical soils of eucalypt forests and heathlands in southern Australia. In Western Europe, podzols develop on he ...
and rich in
clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolinite, ). Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impuriti ...
.
Geography
The tributary streams of the
Afon Tanat
The River Tanat, also known as , is a river in northern Powys, Wales. Its source is close to the Cyrniau Nod mountain, to the north of Lake Vyrnwy. The river flows in a generally east-south-east direction until it joins the River Vyrnwy near Lla ...
have their sources in the
Aran
Aran may refer to:
Places Azerbaijan
Villages and municipalities:
* Aran, Aghjabadi
* Aran, Lerik
* Aran, Shaki
* Aran, Tovuz
* Aran, Yevlakh
Iran
* Aran, Alborz, a village in Alborz Province
* Aran, Nain, a village in Isfahan Province
* Ar ...
and
Berwyn range
The Berwyn range (Welsh (language), Welsh: ''Y Berwyn'' or ''Mynydd y Berwyn'') is an isolated and sparsely populated area of moorland in the northeast of Wales, roughly bounded by Llangollen in the northeast, Corwen in the northwest, Bala, Gw ...
s along the northwestern borders of
Powys
Powys ( , ) is a Principal areas of Wales, county and Preserved counties of Wales, preserved county in Wales. It borders Gwynedd, Denbighshire, and Wrexham County Borough, Wrexham to the north; the English Ceremonial counties of England, ceremo ...
. The western extent of the valley is divided into two main valleys: the Cwm Pennant, following the upper Tanat; and the Cwm Rhiwarth, following the
Afon Eirth. The two river valleys merge at the village of
Llangynog
Llangynog (; ) is a village and community at the confluence of the Afon Eirth and the Afon Tanat at the foot of the Berwyn range in north Powys (previously Montgomeryshire), Wales.
It lies at the foot of the Milltir Cerrig mountain pass ...
.
The Berwyn range lies to the north of the valley, rising up to 500 meters above the valley floor, with the rolling Montgomery Hills to the south.
The valley floor is generally between
O.D.
Cwm Pennant

The Cwm Pennant is a narrow valley following the upper course of the Afon Tanat, prior to its merger with the Afon Eirth at
Llangynog
Llangynog (; ) is a village and community at the confluence of the Afon Eirth and the Afon Tanat at the foot of the Berwyn range in north Powys (previously Montgomeryshire), Wales.
It lies at the foot of the Milltir Cerrig mountain pass ...
.
Pennant Melangell
St Melangell's Church () is a Grade I listed medieval building of the Church in Wales located in the former village of Pennant Melangell, in the Tanat Valley, Powys, Wales. The church was founded around the 8th century to commemorate the rep ...
, a former village and medieval church, is located in the valley. A small, narrow valley, the Cwm Llêch, emerges from the south of the Cwm Pennant, following the course of the Afon Goch.
Cwm Blowty
The Cwm Blowty follows the
Afon Rhaeadr upstream of
Llanrhaeadr-ym-Mochnant
Llanrhaeadr-ym-Mochnant () is a village and Community (Wales), community in Powys, Wales; about 9 miles west of Oswestry and 12 miles south of Llangollen, on the B4580 road. It lies near the foothills of the Berwyn range, Berwyn mountains on the r ...
. A large waterfall, the
Pistyll Rhaeadr
Pistyll Rhaeadr (, meaning "waterfall (of) Rhaeadr") is a waterfall from the village of Llanrhaeadr-ym-Mochnant in Powys, Wales, and west of Oswestry.
Description
Pistyll Rhaeadr is formed by the Afon Disgynfa (''disgynfa'' also means "wate ...
, lies at the head of the valley.
History
Prehistoric and ancient settlements
The earliest evidence of human presence in the Tanat Valley dates to the
Upper Palaeolithic
The Upper Paleolithic (or Upper Palaeolithic) is the third and last subdivision of the Paleolithic or Old Stone Age. Very broadly, it dates to between 50,000 and 12,000 years ago (the beginning of the Holocene), according to some theories ...
; a barbed point from indicates temporary hunting settlements in the area.
Hunter-gatherer
A hunter-gatherer or forager is a human living in a community, or according to an ancestrally derived Lifestyle, lifestyle, in which most or all food is obtained by foraging, that is, by gathering food from local naturally occurring sources, esp ...
seasonal settlements likely existed in the
Mesolithic
The Mesolithic (Ancient Greek language, Greek: μέσος, ''mesos'' 'middle' + λίθος, ''lithos'' 'stone') or Middle Stone Age is the Old World archaeological period between the Upper Paleolithic and the Neolithic. The term Epipaleolithic i ...
and
Neolithic
The Neolithic or New Stone Age (from Ancient Greek, Greek 'new' and 'stone') is an archaeological period, the final division of the Stone Age in Mesopotamia, Asia, Europe and Africa (c. 10,000 BCE to c. 2,000 BCE). It saw the Neolithic Revo ...
. Permanent settlements were likely established in the
Late Neolithic
In the Near Eastern archaeology, archaeology of Southwest Asia, the Late Neolithic, also known as the Ceramic Neolithic or Pottery Neolithic, is the final part of the Neolithic period, following on from the Pre-Pottery Neolithic and preceding th ...
or
Bronze Age
The Bronze Age () was a historical period characterised principally by the use of bronze tools and the development of complex urban societies, as well as the adoption of writing in some areas. The Bronze Age is the middle principal period of ...
.
Although no settlements from the Late Neolithic period are known, several Bronze Age funerary sites are located around the valley, including
henges
A henge can be one of three related types of Neolithic Earthworks (archaeology), earthwork. The essential characteristic of all three is that they feature a ring-shaped bank and ditch, with the ditch inside the bank. Because the internal ditches ...
,
burial mounds
A tumulus (: tumuli) is a mound of earth and stones raised over a grave or graves. Tumuli are also known as barrows, burial mounds, mounds, howes, or in Siberia and Central Asia as ''kurgans'', and may be found throughout much of the world. ...
, and
cairns
Cairns (; ) is a city in the Cairns Region, Queensland, Australia, on the tropical north east coast of Far North Queensland. In the , Cairns had a population of 153,181 people.
The city was founded in 1876 and named after William Cairns, Sir W ...
.
The
Rhos-y-Beddau stone circle
A stone circle is a ring of megalithic standing stones. Most are found in Northwestern Europe – especially Stone circles in the British Isles and Brittany – and typically date from the Late Neolithic and Early Bronze Age, with most being ...
sits in the
hanging valley
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a ve ...
of the Rhaeadr, upstream of the Pistyll Rhaeadr.
Two
Iron Age
The Iron Age () is the final epoch of the three historical Metal Ages, after the Chalcolithic and Bronze Age. It has also been considered as the final age of the three-age division starting with prehistory (before recorded history) and progre ...
hillfort
A hillfort is a type of fortification, fortified refuge or defended settlement located to exploit a rise in elevation for defensive advantage. They are typical of the late Bronze Age Europe, European Bronze Age and Iron Age Europe, Iron Age. So ...
s,
Llwyn Bryn-Dinas and
Craig Rhiwarth, lie above the valley. These may have been a center of early
metallurgy
Metallurgy is a domain of materials science and engineering that studies the physical and chemical behavior of metallic elements, their inter-metallic compounds, and their mixtures, which are known as alloys.
Metallurgy encompasses both the ...
, due to abundant iron ore deposits in the region. An Iron Age hut circle has been found at Garnedd Wen, east of
Craig Rhiwarth.
Mining likely took place at the lead mines of Cwm Orog and Crag y Mwyn during the
Roman period
The Roman Empire ruled the Mediterranean and much of Europe, Western Asia and North Africa. The Roman people, Romans conquered most of this during the Roman Republic, Republic, and it was ruled by emperors following Octavian's assumption of ...
.

Medieval period
Pennant Melangell and Llanrhaeadr, the principal settlements of the largely rural agrarian valley, were both founded as ecclesiastical sites in the medieval period. Pennant Melangell is associated with
Saint Melangell, who supposedly founded a nunnery in the area, and
the shrine dedicated to her. Llanrhaeadr was formed as a
clas dedicated to
Saint Dogfan.
Sheep farming
Sheep farming or sheep husbandry is the raising and breeding of domestic sheep. It is a branch of animal husbandry. Sheep are raised principally for their meat (lamb and mutton), milk (sheep's milk), and fiber (wool). They also yield sheepskin ...
has been a major industry in the area since the 16th century.
Cattle farming also takes place in the valley.
Modern period
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science) ...
quarries have long been used in the region.
Slate
Slate is a fine-grained, foliated, homogeneous, metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade, regional metamorphism. It is the finest-grained foliated metamorphic ro ...
quarries and
lead
Lead () is a chemical element; it has Chemical symbol, symbol Pb (from Latin ) and atomic number 82. It is a Heavy metal (elements), heavy metal that is density, denser than most common materials. Lead is Mohs scale, soft and Ductility, malleabl ...
mines also emerged in the 16th century, continuing into the 20th century.
The 18th and 19th centuries were the period of greatest mining activity, mainly centered at the Llangynog mine. Five smaller mines surrounded Llangynog, alongside two at Cwm Hirnant. Although metal mining largely stopped after the closure of the Llangynog mine in 1899, activity at Cwm Orog continued until 1912, alongside slate and
rhyolite
Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture (geology), texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained matri ...
quarrying throughout the early 20th century. Mining operations at Llangynog led to large-scale
heavy metal contamination
A toxic heavy metal is a common but misleading term for a metal-like element noted for its potential toxicity. Not all heavy metals are toxic and some toxic metals are not heavy. Elements often discussed as toxic include cadmium, mercury and l ...
across the whole of the valley.
The
Tanat Valley Light Railway
The Tanat Valley Light Railway (TVLR) was a long standard gauge light railway. It ran westwards from Llanyblodwel in Shropshire, about 5 miles or 8 km southwest of Oswestry. It crossed the Wales–England border and continued up the Tanat Va ...
was opened in 1904 to serve the communities in the region, continuing operations until 1964.
References
Citations
Bibliography
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*
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{{coord, 52, 48, 45, N, 3, 17, 35, W, type:landmark_region:GB_dim:20000, display=title
Valleys of Powys