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Snowdon (/ ˈ s n oʊ d ən /), or Yr Wyddfa (Welsh: [ər ˈʊɨ̞̯ðva] ⓘ), is a mountain in Snowdonia in North Wales.It has an elevation of 1,085 metres (3,560 ft) above sea level, which makes it both the highest mountain in Wales and the highest in the British Isles south of the Scottish Highlands.
Snowdonia, or Eryri (Welsh: ⓘ), is a mountainous region and national park in North Wales. It contains all 15 mountains in Wales over 3000 feet high, including the country's highest, Snowdon (Yr Wyddfa), which is 1,085 metres (3,560 ft) tall.
The Snowdon Massif, Snowdon Range, or Yr Wyddfa massif, is one of the three mountain groups in Snowdonia (Eryri), north Wales, to include mountains over 3,000 feet (914 m) high. It occupies the area between Beddgelert , Pen-y-Pass and Llanberis .
Clogwyn Du'r Arddu (Welsh pronunciation: [ˈklɔɡwɨ̞n ˈdɨːr ˈarðɨ̞], translates as the "black cliff of the black height"), [2] is a north-facing rhyolite set of cliffs located on the northern flank of Snowdon mountain.
Date/Time Thumbnail Dimensions User Comment; current: 21:27, 29 October 2010: 1,025 × 1,305 (1.28 MB): Nilfanion {{Information |Description=Map of Snowdonia National Park, UK with the following information shown: *National Park boundary *Administrative borders *Coastline, lakes and rivers *Roads and railways *Urban areas Equirectangular map projecti
Location of Arkansas in the United States. Arkansas is located in the southeastern United States, in the West South Central Census Bureau division. Arkansas covers an area of 53,179 square miles (137,733 km²) and ranks as the 29th largest state by size. [7]
Aran Fawddwy is a mountain in southern Snowdonia, Wales, United Kingdom. It is the highest point ( county top ) of the historic county of Merionethshire (for local government purposes, it lies within the current council area of Gwynedd ).
Panorama of part of the Snowdon Massif including Snowdon (centre right) taken from Mynydd Mawr.The Glyderau are visible in the distance.. The bedrock geology of Snowdonia is largely formed from a sequence of sedimentary and igneous rocks originating during the early Palaeozoic (the Cambrian, Ordovician and Silurian periods, lasting between 539 and 419 million years ago).
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