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Aberglaslyn
The Afon Glaslyn (English, ''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 cirque lake on the flanks of Snowdon. It is joined by Nant Traswnant which drains Pen-y-Pass and by Nant Cynnyd before entering the beautiful lake, Llyn Gwynant. The river then flows through Llyn Dinas before entering the village of Beddgelert. In the middle of the village it is joined by the substantial tributary, the River Colwyn which drains the south-western flank of Snowdon. The much enlarged river flows down past Gelert's grave before tumbling down into the Aberglaslyn Pass. This is a small rocky gorge close to the main road which provides easy public access to a most picturesque piece of Snowdonian scenery. Passing through Pont Aberglaslyn, the river emerges from the gorge into the relatively ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aberglaslyn Hall
Aberglaslyn Hall is an outdoor learning centre near Beddgelert, North Wales on the edge of the Snowdonia National Park. The hall was purchased by Leicestershire County Council in 1962. It offers dormitory style accommodation for up to 48 people and serves as a residential centre for groups wishing to participate in outdoor activities and environmental education. Early history In 1873 the land was used as a copper mine run by John Greaves. Aberglaslyn Hall was originally built in 1880 as a private dwelling by John Ernest Greaves. In 1891 Aberglaslyn was sold to John Albert Alexander Williams (born 1863) of Glangwna; he enlarged and improved the property, including installing an organ in the current dining room which was powered by a generator from the stream. Williams resided at Aberglaslyn Hall and was Sheriff of Carnarvonshire in 1895. His musical compositions included the march "Cambria" which was played at the investiture of the Prince of Wales at Carnarvon in 1911. In 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pont Aberglaslyn
Pont Aberglaslyn is a stone arch bridge over the Afon Glaslyn and the surrounding hamlet, located near Beddgelert and Nantmor in Gwynedd, north-west Wales. A well-known beauty spot, according to Peter Bishop it was "one of the most visited sites in north Wales" at the end of the eighteenth century; an 1883 guidebook wrote that it "has occupied the artist's pencil perhaps more than any other". Location Pont Aberglaslyn is located near the downstream end of the Aberglaslyn Pass. While the location is rocky with the river running through rapids just upstream, it is not far above sea level. The river was tidal and navigable up to around Pont Aberglaslyn until the early nineteenth century, when the construction of the Cob seawall near Porthmadog prevented the tide from reaching it. Below the bridge is Llyn Glas (Blue Lake), a former harbour site used for loading copper mined nearby. The bridge was formerly on the border between Caernarfonshire on the west side of the river and Meri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aberglaslyn Pass
The Aberglaslyn Pass ( cy, Bwlch Aberglaslyn) is a narrow gorge of considerable beauty in Snowdonia, Gwynedd, north Wales. The A498 road/ A4085 road follows a relatively level route along the Afon Glaslyn through the pass from Beddgelert to Prenteg and then continues at the edge of the Traeth Mawr via Tremadog to Porthmadog. River pass As recently as the early 19th century, the river Glaslyn was navigable for small boats at high tide as far as Pont Aberglaslyn, which is just south of Beddgelert, where a sixth-century monastery was succeeded in the twelfth by an Augustinian priory. In the Middle Ages Beddgelert was seen as a safe resting place before travelling further. The route from the coast via Beddgelert and overland to Caernarfon or Bangor via Llyn Cwellyn was often considered preferable to the long voyage round the Llŷn Peninsula. Edmund Vale: Snowdonia, National Park Guide Number 2 HMSO 1958/1960 (page 75) Pont Aberglaslyn is in the parish of Nantmor. From here t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
RSPB
The Royal Society for the Protection of Birds (RSPB) is a charitable organisation registered in England and Wales and in Scotland. It was founded in 1889. It works to promote conservation and protection of birds and the wider environment through public awareness campaigns, petitions and through the operation of nature reserves throughout the United Kingdom. In 2020/21 the RSPB had an income of £117 million, 2,000 employees, 12,000 volunteers and 1.1 million members (including 195,000 youth members), making it one of the world's largest wildlife conservation organisations. The RSPB has many local groups and maintains 222 nature reserves. As founders, chief officers and presidents, women have been at the helm of the RSPB for over 85 years. History The origins of the RSPB lie with two groups of women, both formed in 1889: * The Plumage League was founded by Emily Williamson at her house in Didsbury, Manchester, as a protest group campaigning against the use of great creste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osprey
The osprey (''Pandion haliaetus''), , also called sea hawk, river hawk, and fish hawk, is a diurnal, fish-eating bird of prey with a cosmopolitan range. It is a large raptor reaching more than in length and across the wings. It is brown on the upperparts and predominantly greyish on the head and underparts. The osprey tolerates a wide variety of habitats, nesting in any location near a body of water providing an adequate food supply. It is found on all continents except Antarctica, although in South America it occurs only as a non-breeding migrant. As its other common names suggest, the osprey's diet consists almost exclusively of fish. It possesses specialised physical characteristics and exhibits unique behaviour to assist in hunting and catching prey. As a result of these unique characteristics, it has been given its own taxonomic genus, ''Pandion'', and family, Pandionidae. Taxonomy The osprey was described by Carl Linnaeus under the name ''Falco haliaeetus'' in his ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Dwyryd
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, south of Porthmadog. Geography The Dwyryd rises in the hills to the north of Ffestiniog. 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: . 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) south of Ffestiniog. The main river then flows through a wide valley formed by glaciation, with a broad flat base formed from glacial moraines and riverine gravel deposits. The valley, the Vale of Ffestiniog, has much agriculture but is subject to routine winter flooding. The Afon Tafarn-helyg has its confluence about further downstream. This ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, the main market town of the Llŷn Peninsula, together with the historic towns of Harlech and Criccieth, and Abersoch Abersoch is a village in the community of Llanengan in Gwynedd, Wales. It is a popular coastal seaside resort, with around 800 residents, on the east-facing south coast of the Llŷn Peninsula at the southern terminus of the A499. It is about ..., a popular location for water sports, all lie on its shores. External links Overview of its marine biology* Cardigan Bay {{Gwynedd-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsh
A marsh is a wetland that is dominated by herbaceous rather than woody plant species.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p Marshes can often be found at the edges of lakes and streams, where they form a transition between the aquatic and terrestrial ecosystems. They are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs, and the marsh is sometimes called a carr. This form of vegetation is what differentiates marshes from other types of wetland such as swamps, which are dominated by trees, and mires, which are wetlands that have accumulated deposits of acidic peat. Marshes provide habitats for many kinds of invertebrates, fish, amphibians, waterfowl and aquatic mammals. This biological productivity means that marshes contain 0.1% of global sequestered terrestrial carbon. Moreover, they have an outsized influence on clima ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meander
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as bay ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Traeth Mawr
Traeth Mawr (Welsh for "large beach") is a polder near Porthmadog in Gwynedd in Wales. The area was formerly the large tidal estuary of the Afon Glaslyn. It was created after large-scale land reclamation occurred in the late 18th century and the early 19th century. A large embankment, called the Cob, separates the area from the sea and carries a road and railway line. History Early years The original estuary of the ''Afon Glaslyn'' was a dangerous place; many people were said to have died in the quicksands trying to cross the Traeth Mawr. In the late 18th century, various landowners around the edge of the estuary began to systematically reclaim land of between and . Between 1770 and 1800 this resulted in the creation of about of new land. Around 1798, William Madocks bought the Tan-yr-Allt estate near Penmorfa Marsh. Soon afterwards he reclaimed an area of sand from the sea and the river by building a earthen bank from Prenteg to Clog-y-Berth (now Porthmadog). The tow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
