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Encyclopedia > River Teifi

The River Teifi (Welsh: Afon Teifi) is a river in West Wales flowing into the sea below Cardigan town. The catchment of the river is estimated to be 1,008 square kilometres yielding an average flow at Glan Teifi of 31.026 m³/s. The maximum recorded flow (up till 1970 ) was 269.7 m³/s on December 17, 1965. The average rainfall varies from 1552 mm in the upper catchment to 1176 mm in the lower catchment. Welsh redirects here, and this article describes the Welsh language. ... This article is about the country. ... Cardigan (Welsh: Aberteifi) is the traditional county town of Cardiganshire (Ceredigion) in west Wales. ... December 17 is the 351st day of the year (352nd in leap years) in the Gregorian Calendar. ... 1965 (MCMLXV) was a common year starting on Friday (the link is to a full 1965 calendar). ...


Geography

The Teifi has its source in Llyn Teifi, one of several lakes known collectively as Teifi Pools. These are situated in mid Wales toward the north of the administrative area of Ceredigion. This wide area, with a very sparse population, is part of the desert of Wales. The river flows past Strata Florida Abbey and then through Pontrhydfendigaid before reaching the main river valley floor. Here it passes through one of the great raised mires of Britain, Gors Goch Glan Teifi, also known as Tregaron Bog. Over the next 30 miles the Teifi meanders generally south-west in a gentle arc, passing through the villages and towns of Tregaron, Llanddewi Brefi, Cwmann, Lampeter, Llanybydder, Llandysul, Newcastle Emlyn, Cenarth, Llechryd and finally Cardigan town. The river becomes tidal below Llechryd and descends into Cardigan town through the steep sided Cilgerran Gorge. Below Cardigan town the river broadens into a wide estuary, passing the seaside resort of Poppit Sands before finally entering the sea in Cardigan Bay. This article is about the country. ... For other uses please see Ceredigion (disambiguation) Ceredigion is a county in Wales. ... The Desert of Wales is a large area in central Wales so called because of its lack of roads and towns and its general inaccessibility. ... The remains of Strata Florida Abbey as depicted in the 1851 Illustrated London Reading Book Strata Florida (in Welsh: Ystrad Fflur) is a former Cistercian abbey situated just outside Pontrhydfendigaid, near Tregaron in the county of Ceredigion, Wales. ... Pontrhydfendigaid is a village in Ceredigion, Wales, lying on the River Teifi. ... Tregaron is a market town in Ceredigion (Cardiganshire), mid Wales, lying on the River Teifi. ... Llanddewi Brefi is a small village in Ceredigion (Cardiganshire), Wales. ... Cwmann is a small village near Lampeter, just on the border with Carmartenshire. ... Lampeter (Welsh: Llanbedr Pont Steffan, or more informally, Llambed) is a town in Ceredigion, Wales, United Kingdom, lying at the confluence of the River Teifi and the River Dulas. ... Llanybydder is a village straddling the River Teifi in Carmarthenshire, Wales, with a population of 1,423. ... Llandysul is a market town in the Welsh county of Ceredigion, with the twin community of Pont Tyweli, which lies directly across the Teifi River in Carmarthenshire. ... Newcastle Emlyn (Welsh: Castell Newydd Emlyn) is a town, straddling Ceredigion (Cardiganshire) and Carmarthenshire in west Wales (though officially it is in Carmarthenshire), lying on the River Teifi. ... Cenarth is a village on the border of Ceredigion and Carmarthenshire in Wales, lying on the River Teifi. ... Llechryd is a parish in the lower division of the hundred of Troedyraur, county of Ceredigion in South Wales. ... Cardigan (Welsh: Aberteifi) is the traditional county town of Cardiganshire (Ceredigion) in west Wales. ... The term Cardigan Bay, when used by itself, can refer to: A horse called Cardigan Bay A bay in Wales called Cardigan Bay A bay in Prince Edward Island called Cardigan Bay This is a disambiguation page — a navigational aid which lists other pages that might otherwise share the...


Geology and landscape

The Teifi and its tributaries are underlain by ancient Ordovician and Silurians mudstones which have been extensively glaciated during the ice ages. The resultant landform is one of gently rolling hills supporting a range of agriculture in which dairying and sheep rearing dominate. Cardiganshire (now Ceredigion) had the reputation of supplying London with its milk in the 19th century . The landscapes of the Teifi valley are very attractive and the Teifi is considered by many to be one of the most beautiful rivers in Wales. The Ordovician period is the second of the six (seven in North America) periods of the Paleozoic era. ... The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 443. ... Cardiganshire (Sir Aberteifi in Welsh) was a traditional county in Wales that existed between 1282 and 1974. ... This article is about the capital of England and the United Kingdom. ...


Teifi pools, the source of the Teifi are a series of small lakes left by past glacial activity. The lakes are upland and acid in nature. Some have been enlarged by damming and now provide a source of drinking water. The very extensive raised mire above Tregaron acts as a huge sponge at the head of the river evening out extremes in flow. Rapids and waterfalls are uncommon but the examples at Henllan and especially at Cenarth are noteworthy and have been extensively photographed and painted because of the beauty of the landscape. The gorge between Llechryd and Cilgerran has a special brooding quality. Few visitors stray into the gorge and the river winds its way almost silently between the densely wooded sides with their distinctive under-storey flora of sedges. Genera See text The family Cyperaceae, or the Sedge family, is a taxon of monocot flowering plants that superficially resemble grasses or rushes. ...


Culture and history

The Teifi valley has been inhabited since pre-history. There are many remains of Iron Age and Stone age man including Cromlechs ( burial chambers) and standing stones. The remains of a medieval abbey stand at Strata Florida with some excellent examples of encaustic tiles on the floors. The river flows near to the University of Wales, Lampeter which was the oldest university established in Wales. Between Cenarth and Cardigan there is an ancient tradition of fishing and travel using coracles – very simple light-weight boats made of bent sticks covered with waterproofed hide or skins,. These are paddled by a single oar used at the front of the craft which requires great skill. The principal use for coracles is in salmon fishing using nets. This form of fishing is now very tightly controlled and the right to fish in this way is passed down from father to son. There is also an age-old tradition of illegal salmon and sea-trout fishing in the lower Teifi. Iron Age Axe found on Gotland This article is about the archaeological period known as the Iron Age, for the mythological Iron Age see Iron Age (mythology). ... Stone Age fishing hook. ... T shaped Hunebed D27 in Borger-Odoorn, Netherlands, recent. ... Standing stones, orthostats, liths or more commonly, megaliths because of their large and cumbersome size, are solitary stones set vertically in the ground. ... The Middle Ages formed the middle period in a traditional schematic division of European history into three ages: the classical civilization of Antiquity, the Middle Ages, and modern times. ... University of Wales, Lampeter Prifysgol Cymru, Llanbedr Pont Steffan   University of Wales, Lampeter (Welsh: Prifysgol Cymru, Llanbedr Pont Steffan) is a university in Lampeter, Wales, the oldest degree awarding institution in Wales, and the third oldest in England and Wales after Oxford and Cambridge. ... Coracle: Ku-Dru or Kowa of Tibet—Field Museum of Natural History, Chicago A coracle is a primitive type of boat. ... For other uses, see Poaching (disambiguation). ...


  Results from FactBites:
 
River Teifi - Wikipedia, the free encyclopedia (668 words)
The catchment of the river is estimated to be 1,008 square kilometres yielding an average flow at Glan Teifi of 31.026 m³/s.
The Teifi and its tributaries are underlain by ancient Ordovician and Silurians mudstones which have been extensively glaciated during the ice ages.
Teifi pools, the source of the Teifi are a series of small lakes left by past glacial activity.
  More results at FactBites »


 

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