River Dwyryd
   HOME

TheInfoList



OR:

The River Dwyryd ( cy, Afon Dwyryd, meaning a river of two fords) is a river in Gwynedd, Wales which flows principally westwards; draining to the sea into
Tremadog Bay Tremadog Bay is a large inlet of Cardigan Bay, defined by the north Cambrian Coast and the Llŷn Peninsula of north Wales. The Afon Glaslyn flows into the north of the bay and Saint Tudwal's Islands lie at the western end of the bay. Pwllheli, ...
, south of
Porthmadog Porthmadog (; ), originally Portmadoc until 1974 and locally as "Port", is a Welsh coastal town and community in the Eifionydd area of Gwynedd and the historic county of Caernarfonshire. It lies east of Criccieth, south-west of Blaenau Ff ...
.


Geography

The Dwyryd rises in the hills to the north of
Ffestiniog Ffestiniog () is a community in Gwynedd in 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 1284 ...
. At its most northern extent, water draining from Moelwyn Mawr drains into the Tanygrisiau Reservoir, the outflow of which forms the source of the Afon Goedol. This is joined by the River Bowydd at
grid reference A projected coordinate system, also known as a projected coordinate reference system, a planar coordinate system, or grid reference system, is a type of spatial reference system that represents locations on the Earth using cartesian coordin ...
: . Below Rhyd y Sarn, the river is joined by the Afon Cynfal which flows from the east down a deep wooded gorge which includes the spectacular Rhaeadr Cynfal (Cynfal
waterfall A waterfall is a 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 severa ...
) south of
Ffestiniog Ffestiniog () is a community in Gwynedd in 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 1284 ...
. 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 she ...
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 throug ...
, has much agriculture but is subject to routine winter flooding. The Afon Tafarn-helyg has its confluence about further downstream. This tributary rises south of Gellilydan and just north of the reservoir of Llyn Trawsfynydd 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 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 environm ...
, 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 R ...
, before joining with the estuary of the River Glaslyn and then entering into
Porthmadog Bay Porthmadog (; ), originally Portmadoc until 1974 and locally as "Port", is a Welsh coastal town and community in the Eifionydd area of Gwynedd and the historic county of Caernarfonshire. It lies east of Criccieth, south-west of Blaenau Ffesti ...
. 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 or saltmarsh, 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. It is domin ...
known as Glastraeth (''green beach'') on its south bank and opposite the village of
Portmeirion Portmeirion is a tourist village in Gwynedd, North Wales. It was designed and built by Sir Clough Williams-Ellis between 1925 and 1975 in the style of an Italian village, and is now owned by a charitable trust. The village is located in the co ...
. The whole of the river drains off igneous and ancient rocks of the Cambrian and
Ordovician The Ordovician ( ) is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. T ...
which are all
base-poor In ecology, base-richness is the level of chemical bases in water or soil, such as calcium or magnesium ions. Many organisms prefer base-rich environments. Chemical bases are alkalis, hence base-rich environments are either neutral or alkaline ...
. 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. This has constrained the quality of the fishery and the
biodiversity Biodiversity or biological diversity is the variety and variability of life on Earth. Biodiversity is a measure of variation at the genetic (''genetic variability''), species (''species diversity''), and ecosystem (''ecosystem diversity'') l ...
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 (from Old French ''armee'', itself derived from the Latin verb ''armāre'', meaning "to arm", and related to the Latin noun ''arma'', meaning "arms" or "weapons"), ground force or land force is a fighting force that fights primarily on ...
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 and flows past the southern end of the village to enter Llyn Trawsfynydd, 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 navigat ...
. 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 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 1974 and locally as "Port", is a Welsh coastal town and community in the Eifionydd area of Gwynedd and the historic county of Caernarfonshire. It lies east of Criccieth, south-west of Blaenau Ff ...
, 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 ca ...
s. Some of the quays remain to this day, used by anglers. The opening of the Ffestiniog Railway in 1836 dealt a mortal blow to the Dwyryd traffic, which ended completely by 1860.


References


Sources

* *


Further material

* * * * * *


External links


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