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Migneint
The Migneint () is a large expanse of moorland in central Snowdonia, north-west Wales. It is part of the ''Migneint-Arenig-Dduallt'' Special Area of Conservation, along with the mountains Arenig Fawr, Arenig Fach and Dduallt, covering a range of nearly . It is either the largest area of blanket bog in Wales, or the second largest, after the Berwyn range, further to the east. The area includes a few small lakes, including Llyn Conwy, the source of the River Conwy, and is bisected by the B4407 road from Ffestiniog to Ysbyty Ifan Ysbyty Ifan (formerly anglicised as ''Yspytty Ifan'') is a small, historic village and community (Wales), community in the Conwy County Borough of Wales. The population in 2011 was 196 in 76 households (29 household spaces had no usual resident .... Plans have been suggested to hold water on the Migneint for longer, to help prevent flooding in the Conwy valley; but local farmers have voiced concern that this could be harmful to livestock. Referen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llyn Conwy
Llyn Conwy (SH780462) is a lake in the county borough of Conwy County Borough, Conwy in central North Wales, north Wales. It is the source of the River Conwy which, on flowing south out of the lake, swings round to then generally flow in a northerly direction for a distance of some to its discharge in Conwy Bay. Llyn Conwy lies at a height of about 1,488 ft, with a maximum depth of 16 feet, and is by far the biggest lake of the Migneint moors, an extensive area of blanket mire with high rainfall - about 260 cm p.a. There is a view of Arenig Fawr. Geology This is an area of Ordovician rocks, lending its name to the "Llyn Conwy Formation", which is identified by its yellowish rhyolitic tuffs. This Formation also reappears in Afon Tryweryn to the south-east, where the hard rock was utilized in the construction of Llyn Celyn dam. Water quality and soil Llyn Conwy is owned by the National Trust for Places of Historic Interest or Natural Beauty, National Trust and, whilst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snowdonia
Snowdonia, or Eryri (), is a mountainous region and National parks of the United Kingdom, national park in North Wales. It contains all 15 mountains in Wales Welsh 3000s, over 3000 feet high, including the country's highest, Snowdon (), which is tall. These peaks are all part of the Snowdon Massif, Snowdon, Glyderau, and Carneddau ranges in the north of the region. The shorter Moelwynion and Moel Hebog ranges lie immediately to the south. The national park has an area of (the fourth-largest in the UK), and covers most of central and southern Gwynedd and the western part of Conwy County Borough. This is much larger than the area traditionally considered Snowdonia, and in addition to the five ranges above includes the Rhinogydd, Cadair Idris, and Aran Fawddwy, Aran ranges and the Dyfi hills, Dyfi Hills. It also includes most of the coast between Porthmadog and Aberdyfi. The park was the first of the three national parks of Wales to be designated, in October 1951, and the third i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conwy Valley
The River Conwy (; ) is a river in north Wales. From its source to its discharge in Conwy Bay it is long and drains an area of 678 square km. "Conwy" was formerly anglicised as "Conway." The name 'Conwy' derives from the old Welsh words ''cyn'' (chief) and ''gwy'' (water), the river being originally called the 'Cynwy'. It rises on the Migneint moor where a number of small streams flow into Llyn Conwy, then flows in a generally northern direction, being joined by the tributaries of the rivers Machno and Afon Lledr before reaching Betws-y-coed, where it is also joined by Llugwy. From Betws-y-coed the river continues to flow north through Llanrwst, Trefriw (where it is joined by the Afon Crafnant) and Dolgarrog (where it is joined by Afon Porth-llwyd and Afon Ddu) before reaching Conwy Bay at Conwy. A local quay, Cei Cae Gwyn, is located on its bank. During spring tides the river is tidal as far as Tan-lan, near Llanrwst. Tributaries of the River Conwy This is a l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ysbyty Ifan
Ysbyty Ifan (formerly anglicised as ''Yspytty Ifan'') is a small, historic village and community (Wales), community in the Conwy County Borough of Wales. The population in 2011 was 196 in 76 households (29 household spaces had no usual residents); over 79% of the population were able to speak Welsh language, Welsh. It has one of the smallest populations of any Welsh community, the smallest being Ganllwyd. It is in the electoral ward of Uwch Conwy. History Ysbyty Ifan, until about 1190, was known as . Then, it came to the attention of the Knights of St John, Knights of St John, the Order of Hospitallers, who set up a hospital to care for pilgrims and also to be a hostel for them on their journeys (Ysbyty Ifan means ''hospital of St John''). Ysbyty Ifan was on the ancient pilgrimage routes, for example, from Bangor Is Coed (Bangor-on-Dee) to Caer Gybi (fort), Holyhead and Bardsey Island and the Cistercian Way (Wales), Cistercian Way between Aberconwy Abbey, Aberconwy and Cymer Ab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moorland
Moorland or moor is a type of Habitat (ecology), habitat found in upland (geology), upland areas in temperate grasslands, savannas, and shrublands and the biomes of montane grasslands and shrublands, characterised by low-growing vegetation on Soil pH, acidic soils. Moorland today generally means uncultivated hill land (such as Dartmoor in South West England), but also includes low-lying wetlands (such as Sedgemoor, also South West England). It is closely related to heath, although experts disagree on the exact distinction between these types of vegetation. Generally, moor refers to Highland (geography), highland and high rainfall areas, while heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats are found mainly in Tropics, tropical Africa, Northern Europe, northern and western Europe, and South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arenig Fach
Arenig Fach is a mountain in southern Snowdonia, north Wales. It is a peak in the Arenig range and lies to the north of its parent peak Arenig Fawr. It lies close to Llyn Celyn alongside the A4212 between Trawsfynydd and Bala. Carnedd y Filiast and Foel Goch (Arenigs) is to the east, while Moel Llyfnant, Gallt y Daren and Arenig Fawr are to the south. The summit itself is known as Carnedd Bachgen, named after the ancient cairn, ''Carnedd y Bachgen'' (which lies just north-east of the summit), and is the highest point at the north end of a wide plateau. There is a trig point and a substantial shelter cairn. The mountain rises from the Migneint moorland and looks like a bulky heathery "lump" from most directions. However, its north-eastern face has steep cliffs with a small corrie lake, Llyn Arenig Fach, at their bottom. The last glacier occupation of this corrie is thought to have happened during the Loch Lomond Stadial The Younger Dryas (YD, Greenland Stadial GS-1) was a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arenig Fawr
is a mountain in Snowdonia, North Wales, close to Llyn Celyn reservoir, alongside the A4212 road, A4212 between Trawsfynydd and Bala, Gwynedd, Bala. Location Arenig Fawr is the highest member of the Arenigs, Arenig range, with , a smaller neighbouring mountain, lying to the north. It is surrounded by Moel Llyfnant to the west, Rhobell Fawr to the south and Mynydd Nodol to the east. Ascent The easy-to-moderate climb to the summit takes about 2½ hours from Llyn Celyn. There are no readily identifiable footpaths but the route is marked by an old wire boundary fence. Beneath the mountain is Llyn Arenig Fawr, a reservoir providing drinking water to Bala, Gwynedd, Bala and the surrounding villages. The summit, which is also known as , has a trig point and a memorial to eight American aircrew who died when their Flying Fortress bomber B-17F #42-3124 crashed on 4 August 1943. Some of the crash wreckage is still scattered across the hillside 300 m (330 yds) from the memorial locatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wetland Sites Of Special Scientific Interest
A wetland is a distinct semi-aquatic ecosystem whose groundcovers are flooded or soil saturation, saturated in water, either permanently, for years or decades, or only seasonally. Flooding results in oxygen-poor (anoxic waters, anoxic) processes taking place, especially in the soils. Wetlands form a transitional zone between waterbodies and dry lands, and are different from other terrestrial ecosystem, terrestrial or aquatic ecosystems due to their vegetation's roots having adapted to oxygen-poor hydric soil, waterlogged soils. They are considered among the most biologically diverse of all ecosystems, serving as habitats to a wide range of aquatic and semi-aquatic plants and animals, with often improved water quality due to plant removal of nutrient pollution, excess nutrients such as nitrates and phosphorus. Wetlands exist on every continent, except Antarctica. The water in wetlands is either freshwater, brackish or seawater, saltwater. The main types of wetland are defined bas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Gwynedd
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
