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Cwm Caseg
Cwm Caseg is a broad glacial valley in Snowdonia leading west from the Carneddau towards Bethesda. It is bordered by Carnedd Llewelyn to the southeast, Yr Elen to the west, and Foel Grach Foel Grach is a mountain in the Carneddau range. It is the eighth-highest summit in Snowdonia as well as Wales, and is included in the Welsh 3000s. It is located on a broad ridge extending northwards from Carnedd Llewelyn to Carnedd Gwenlli ... to the northeast. It contains a small lake, Ffynnon Caseg.Pearce, Horace. In the Tracks of Old Welsh Glaciers'. The Dublin University Magazine, Volume 84, 1874 References Bethesda, Gwynedd Llanllechid Valleys of Gwynedd Valleys of Snowdonia {{Wales-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Looking Across Afon Caseg Towards Cwm Caseg - Geograph
Looking is the act of intentionally focusing visual perception on someone or something, for the purpose of obtaining information, and possibly to convey interest or another sentiment. A large number of troponyms exist to describe variations of looking at things, with prominent examples including the verbs "stare, gaze, gape, gawp, gawk, goggle, glare, glimpse, glance, peek, peep, peer, squint, leer, gloat, and ogle".Anne Poch Higueras and Isabel Verdaguer Clavera, "The rise of new meanings: A historical journey through English ways of ''looking at''", in Javier E. Díaz Vera, ed., ''A Changing World of Words: Studies in English Historical Lexicography, Lexicology and Semantics'', Volume 141 (2002), p. 563-572. Additional terms with nuanced meanings include viewing, Madeline Harrison Caviness, ''Visualizing Women in the Middle Ages: Sight, Spectacle, and Scopic Economy'' (2001), p. 18. watching,John Mowitt, ''Sounds: The Ambient Humanities'' (2015), p. 3. eyeing,Charles John ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snowdonia
Snowdonia or Eryri (), is a mountainous region in northwestern Wales and a national park of in area. It was the first to be designated of the three national parks in Wales, in 1951. Name and extent It was a commonly held belief that the name is derived from ("eagle"), and thus means "the abode/land of eagles", but recent evidence is that it means ''highlands'', and is related to the Latin (to rise) as leading Welsh scholar Sir proved. The term first appeared in a manuscript in the 9th-century , in an account of the downfall of the semi-legendary 5th-century king (Vortigern). In the Middle Ages, the title ''Prince of Wales and Lord of Snowdonia'' () was used by ; his grandfather used the title ''Prince of north Wales and Lord of Snowdonia.'' The name ''Snowdonia'' derives from '' Snowdon'', the highest mountain in the area and the highest mountain in Wales at . Before the boundaries of the national park were designated, "Snowdonia" was generally used to refer to a s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carneddau
The (lit. 'the cairns'; is a Welsh plural form, and is sometimes anglicised to ''Carnedds'') are a group of mountains in Snowdonia, Wales. They include the largest contiguous areas of high ground (over or high) in Wales and England (although larger areas over 2,000 feet are found in Northern England), as well as six or seven of the highest peaks in the country—the Fifteen Peaks. The range also encloses a number of lakes such as Llyn Cowlyd and Llyn Eigiau, and the Aber Falls waterfall. It is delimited by the Irish Sea to the north, the Conwy valley to the east, and by the A5 road from Betws-y-Coed to Bethesda to the south and west. The area covers nearly , about 10% of the area of Snowdonia. The area is bordered by three main roads—the A55 (to the north), the A5 to the south and the A470 to the east. Geology In common with much of Snowdonia, the rocks forming the Carneddau originated largely during the Ordovician period between 485 and 444 Ma (million years ago). P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bethesda, Wales
Bethesda (; ) is a town and community on the River Ogwen and the A5 road on the edge of Snowdonia, in Gwynedd, north-west Wales. It is the fifth-largest community in Gwynedd. History The settlement's ancient name was Cilfoden, formerly known as Glanogwen. In 1823, the Bethesda Chapel was built and the town subsequently grew around and later named after it. The chapel was rebuilt in 1840. The town grew around the slate quarrying industries; the largest of the local quarries is the Penrhyn Quarry. At its peak, the town exported purple slate all over the world. Penrhyn Quarry suffered a three-year strike led by the North Wales Quarrymen's Union between 1900 and 1903 – the longest industrial dispute in British history. This led to the creation of the nearby village of Tregarth, built by the quarry owners, which housed the families of those workers who had not struck. It also led to the formation of three co-operative quarries, the largest of which Pantdreiniog dominated th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carnedd Llewelyn
Carnedd Llewelyn, also spelled Carnedd Llywelyn, is a mountain massif in the Carneddau range in Snowdonia, north-west Wales. It is the highest point of the Carneddau and the second highest peak by relative height in Wales, 49th in the British Isles and lies on the border between Gwynedd and Conwy. Topography and ascent routes Carnedd Llewelyn lies in the middle of the main north-east to south-west ridge of the Carneddau, between Carnedd Dafydd to the south-west and Foel Grach to the north. A short subsidiary ridge links it to Yr Elen to the north-west. It can be climbed from Gerlan, above Bethesda, taking the path following Afon Llafar then continuing to the summit of Yr Elen before following the short ridge to Carnedd Llewelyn. Another path starts from Helyg on the A5, taking the track to the reservoir then following the slopes above Craig yr Ysfa to the summit. An alternative is to reach it by following the main ridge, either from Pen yr Ole Wen or fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yr Elen
Yr Elen is a mountain in the Carneddau range in Snowdonia, Wales. It is the ninth highest mountain in Snowdonia. The average annual temperature of the peak is around . It lies on a short ridge running north-northwest off the main northeast-to-southwest ridge of the Carneddau, just over one kilometre from Carnedd Llewelyn. It is usually climbed from the main ridge of the Carneddau, as it is only a short walk from Carnedd Llywelyn. It can also be climbed from Gerlan, near Bethesda, following Afon Llafar then heading up the slopes of Yr Elen, but this involves walking through wet valleys and a number of rivers that are difficult to cross. In drier times, ascent can be made via the crossing of Afon Caseg and then up the "front edge" of the peak. The views from this point north-west, over to Bangor and Anglesey, are stunning on a clear day, especially with a summer's sunset. This is well worth the arduous ascent. The etymology of the name is unclear, with the personal name "Helen" ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foel Grach
Foel Grach is a mountain in the Carneddau range. It is the eighth-highest summit in Snowdonia as well as Wales, and is included in the Welsh 3000s. It is located on a broad ridge extending northwards from Carnedd Llewelyn to Carnedd Gwenllian (formerly Y Garnedd Uchaf) and Foel-fras. An emergency refuge has been built below the summit. Compared to the surrounding mountains, much deeper snow settles here due to its rather broad summit and high grassy slopes. On clear days the Isle of Man and even the Mourne Mountains in Northern Ireland Northern Ireland ( ga, Tuaisceart Éireann ; sco, label=Ulster-Scots, Norlin Airlann) is a part of the United Kingdom, situated in the north-east of the island of Ireland, that is variously described as a country, province or region. North ... can be seen from the summit.Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone. . References External linkswww. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bethesda, Gwynedd
Bethesda (; ) is a town and community on the River Ogwen and the A5 road on the edge of Snowdonia, in Gwynedd, north-west Wales. It is the fifth-largest community in Gwynedd. History The settlement's ancient name was Cilfoden, formerly known as Glanogwen. In 1823, the Bethesda Chapel was built and the town subsequently grew around and later named after it. The chapel was rebuilt in 1840. The town grew around the slate quarrying industries; the largest of the local quarries is the Penrhyn Quarry. At its peak, the town exported purple slate all over the world. Penrhyn Quarry suffered a three-year strike led by the North Wales Quarrymen's Union between 1900 and 1903 – the longest industrial dispute in British history. This led to the creation of the nearby village of Tregarth, built by the quarry owners, which housed the families of those workers who had not struck. It also led to the formation of three co-operative quarries, the largest of which Pantdreiniog dominated t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llanllechid
Llanllechid () is a village near Bethesda and a community in Gwynedd, Wales with a population of 889 as of the 2011 UK census and an area of . The community also includes Tal-y-Bont near Bangor, Gwynedd and a large part of the Carneddau range so is therefore sparsely populated. Eglwys St Llechid, Llanllechid St Llechid is the patron saint of the village, where she founded the parish church and a holy well (now lost). The church closed in 2002. Notable people * (1854–1911), writer, geographer, cartographer, journalist, editor, historian, inventor; born and grew up in Llanllechid * |
Valleys Of Gwynedd
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only local ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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