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The River Dwyryd (), is a river in
Gwynedd Gwynedd () is a county in the north-west of Wales. It borders Anglesey across the Menai Strait to the north, Conwy, Denbighshire, and Powys to the east, Ceredigion over the Dyfi estuary to the south, and the Irish Sea to the west. The ci ...
, Wales which flows principally westwards; draining to the sea into Tremadog Bay, south of
Porthmadog Porthmadog (), originally Portmadoc until 1972 and known locally as "Port", is a coastal town and community (Wales), community in the Eifionydd area of Gwynedd, Wales, and the historic counties of Wales, historic county of Caernarfonshire. It li ...
.


Geography

The Dwyryd rises in the hills to the north of
Ffestiniog Ffestiniog (; ) is a community in Gwynedd, Wales, containing several villages, in particular the settlements of Llan Ffestiniog and Blaenau Ffestiniog. It has a population of 4,875. History Ffestiniog was a parish in Cantref Ardudwy; in 12 ...
. At its most northern extent, water draining from Moelwyn Mawr drains into Llyn Ystradau, the outflow of which forms the source of the Afon Goedol. This is joined by the River Bowydd at
grid reference A projected coordinate systemalso called a projected coordinate reference system, planar coordinate system, or grid reference systemis a type of spatial reference system that represents locations on Earth using Cartesian coordinate system, Car ...
: . At Rhyd-y-Sarn, the Afon Goedol is joined by the Afon Teigl (originating from Manod Mawr). Thereafter, the river is called the Afon Dwyryd. Below Rhyd y Sarn by Pont Dolymoch, the river is joined by the Afon Cynfal which flows from the east down a deep wooded
gorge A canyon (; archaic British English spelling: ''caƱon''), gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tend ...
which includes the spectacular Rhaeadr Cynfal (Cynfal
waterfall A waterfall is any point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in seve ...
) south of
Ffestiniog Ffestiniog (; ) is a community in Gwynedd, Wales, containing several villages, in particular the settlements of Llan Ffestiniog and Blaenau Ffestiniog. It has a population of 4,875. History Ffestiniog was a parish in Cantref Ardudwy; in 12 ...
. The main river then flows through a wide valley formed by
glaciation A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate be ...
, with a broad flat base formed from
glacial moraine A moraine is any accumulation of unconsolidated debris ( regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice s ...
s and riverine gravel deposits. The valley, the
Vale of Ffestiniog The Vale of Ffestiniog is a valley in the Snowdonia National Park in Gwynedd, North Wales. It stretches from Ffestiniog in the east and runs in a westerly direction towards Tremadog Bay, terminating near Porthmadog. The Afon Dwyryd runs thro ...
, has much agriculture but is subject to routine winter flooding. The Afon Tafarn-helyg has its
confluence In geography, a confluence (also ''conflux'') occurs where two or more watercourses join to form a single channel (geography), channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main ...
about further downstream. This tributary rises south of Gellilydan and just north of the reservoir of
Llyn Trawsfynydd Llyn Trawsfynydd is a large artificial reservoir situated near the village of Trawsfynydd in Gwynedd, North Wales. With a total surface area of the reservoir is slightly more extensive than Wales's largest natural lake, Bala Lake at . History ...
but does not receive any water from the reservoir. There are a number of small lakes and reservoirs in the woodlands north of Plas Tan y Bwlch which also drain south into the river. These lakes include Llyn y Garnedd, Llyn Hafod y Llyn and Llyn Mair. At
Maentwrog Maentwrog () is a village and community in the Welsh county of Merionethshire (now part of Gwynedd), lying in the Vale of Ffestiniog just below Blaenau Ffestiniog, within the Snowdonia National Park. The River Dwyryd runs alongside the vil ...
the Dwyryd becomes a long and sandy tidal
estuary An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime enviro ...
, flowing under the road and railway line at
Pont Briwet Pont Briwet refers to the road and railway bridges that cross the River Dwyryd, near Penrhyndeudraeth, Gwynedd in North Wales. The first bridge was a Victorian road and railway viaduct that was constructed entirely from timber by the Cambrian Ra ...
, before joining with the estuary of the
River Glaslyn is a river in Gwynedd, north-west Wales. While not of great significance in terms of its length (about ), it is one of Gwynedd's primary rivers, and has greatly influenced the landscape in which it flows. It has its source in Glaslyn, a ci ...
and then entering into Porthmadog Bay. The Afon y Glyn which drains the southwest catchment from Llyn Tecwyn Uchaf and Llyn Tecwyn Isaf enters the southern side of the Glaslyn estuary at the south end of a large extent of
salt marsh A salt marsh, saltmarsh or salting, also known as a coastal salt marsh or a tidal marsh, is a coastal ecosystem in the upper coastal intertidal zone between land and open saltwater or brackish water that is regularly flooded by the tides. I ...
known as Glastraeth (''green beach'') on its south bank and opposite the village of
Portmeirion Portmeirion (; ) is a folly* * * tourist village in Gwynedd, North Wales. It lies on the estuary of the River Dwyryd in the community (Wales), community of Penrhyndeudraeth, from Porthmadog and from Minffordd railway station. Portmeirion was d ...
. The whole of the river drains off igneous and ancient rocks of the
Cambrian The Cambrian ( ) is the first geological period of the Paleozoic Era, and the Phanerozoic Eon. The Cambrian lasted 51.95 million years from the end of the preceding Ediacaran period 538.8 Ma (million years ago) to the beginning of the Ordov ...
and
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 ...
which are all base-poor. Much of the catchment has also been used for commercial forestry during the last hundred years. As a consequence, many of the tributaries are highly acidic as a result of atmospheric
acidification Acidification may refer to: * Ocean acidification, decrease in the pH of the Earth's oceans * Freshwater acidification, atmospheric depositions and soil leaching of SOx and NOx * Soil acidification, buildup of hydrogen cations, which reduces the ...
. This has constrained the quality of the fishery and the
biodiversity Biodiversity is the variability of life, life on Earth. It can be measured on various levels. There is for example genetic variability, species diversity, ecosystem diversity and Phylogenetics, phylogenetic diversity. Diversity is not distribut ...
in many tributaries. Some of these problems have been exacerbated by past industrial activities including metal mining, slate mining, animal skin processing and the use by the
army An army, ground force or land force is an armed force that fights primarily on land. In the broadest sense, it is the land-based military branch, service branch or armed service of a nation or country. It may also include aviation assets by ...
of a gunnery range with large amounts of emplaced metal cartridge shells.


Afon Prysor

The Afon Prysor is the largest tributary of the Dwyryd, entering its left bank in the tidal section downstream of Maentwrog. It rises in the hills to the east of
Trawsfynydd Trawsfynydd (; Welsh language, Welsh for ) is a linear village in Gwynedd, Wales, near Llyn Trawsfynydd reservoir, and adjacent to the A470 road, A470 north of Bronaber and Dolgellau and 10 km (6 miles) south of Blaenau Ffestiniog. It als ...
and flows past the southern end of the village to enter
Llyn Trawsfynydd Llyn Trawsfynydd is a large artificial reservoir situated near the village of Trawsfynydd in Gwynedd, North Wales. With a total surface area of the reservoir is slightly more extensive than Wales's largest natural lake, Bala Lake at . History ...
, a large reservoir close to the
A470 The A470 (also named the Cardiff to Glan Conwy Trunk Road) is a trunk road in Wales. It is the country's longest road at and links the capital Cardiff on the south coast to Llandudno on the north coast. While previously one had to navigate th ...
. Prior to construction of the dam in the 1920s for hydroelectric power, the river had wandered across a broad upland marsh here known as Cors Goch. It is the only inland water in the UK that has been used as a source of cooling water for a nuclear power station. The Afon Prysor resumes its course below the dam, to flow down to the Dwyryd through the steeply wooded valley of Ceunant Llennyrch which is at the core of a national nature reserve. Most of the flow from the reservoir is channelled through the
hydro-electric power station Hydroelectricity, or hydroelectric power, is Electricity generation, electricity generated from hydropower (water power). Hydropower supplies 15% of the world's electricity, almost 4,210 TWh in 2023, which is more than all other Renewable energ ...
close to Maentwrog; the flow then re-joins the Prysor just before the confluence.


River traffic

At no point is the river deep enough to accommodate sea-going ships, but in the second half of the 18th century a number of quays were constructed west of Maentwrog from which small vessels took cargoes of timber and, increasingly, slate to be transferred to sea-going shipsSlate traffic on the Dwyryd
''Penmorfa'' in deeper water southwest of what would become
Porthmadog Porthmadog (), originally Portmadoc until 1972 and known locally as "Port", is a coastal town and community (Wales), community in the Eifionydd area of Gwynedd, Wales, and the historic counties of Wales, historic county of Caernarfonshire. It li ...
, transferring to Porthmadog itself when its harbour was opened in 1824. The river was and remains so shallow that viable cargoes could only be carried at
spring tide Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables ...
s. Some of the quays remain to this day, used by anglers. The opening of the
Ffestiniog Railway The Ffestiniog Railway () is a heritage railway based on Narrow-gauge railway, narrow-gauge, located in Gwynedd, Wales. It is a major tourist attraction located mainly within the Snowdonia#Snowdonia National Park, Snowdonia National Park. The ...
in 1836 dealt a mortal blow to the Dwyryd traffic, which ended completely by 1860.


References


Sources

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Further material

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External links


The river on navigable OS maps with satellite overlays
''National Library of Scotland'' {{authority control Dwyryd Dwyryd