Moel Ysgyfarnogod
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Moel Ysgyfarnogod
Moel Ysgyfarnogod (''Bare hill of the hares'' in Welsh) is a mountain in Snowdonia, North Wales and is the northernmost of the Rhinogydd. Rhinog Fawr lies directly south. It overlooks Llyn Trawsfynydd, and from the summit it is possible to see the towns of Porthmadog and Blaenau Ffestiniog. It may be climbed from Trawsfynydd in the east, or from Talsarnau in the west. To the north-west of the summit, on an area of moorland and rocky outcrops, lies Bryn Cader Faner, an ancient stone circle. It is one of the finest examples of a Bronze Age cairn in Britain, and has rocky standing stones A menhir (from Brittonic languages: ''maen'' or ''men'', "stone" and ''hir'' or ''hîr'', "long"), standing stone, orthostat, or lith is a large human-made upright stone, typically dating from the European middle Bronze Age. They can be foun ... along its circumference. References {{reflist External links www.geograph.co.uk : photos of Moel Ysgyfarnogod and surrounding area Talsarnau ...
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Rhinog Fawr
''Rhinog Fawr'' is a mountain in Snowdonia, North Wales and forms part of the Rhinogydd range. It is the third highest summit of the Rhinogydd, losing out to Y Llethr and Diffwys respectively. Its smaller cousin Rhinog Fach lies to the south, separated by the pass of Bwlch Drws Ardudwy, while its other neighbour, Moel Ysgyfarnogod lies to the north. In common with most of the range, the terrain is characterised by hard sedimentary rock Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles ... covered with heather, making progress on foot difficult. At 510m, nestled in crags, lies ''Llyn Du'', a small tarn beneath the summit. The ascent is most easily made from the north-east or north-west, via the ''Roman Steps'' pass.Nuttall, John & Anne (1999). ''The Mountains of England & Wales'' - ...
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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 Ffestiniog, north of Dolgellau and south of Caernarfon. The community population of 4,185 in the 2011 census was put at 4,134 in 2019. It grew in the 19th century as a port for local slate, but as the trade declined, it continued as a shopping and tourism centre, being close to Snowdonia National Park and the Ffestiniog Railway. The 1987 National Eisteddfod was held there. It includes nearby Borth-y-Gest, Morfa Bychan and Tremadog. History Porthmadog came about after William Madocks built a sea wall, the ''Cob'', in 1808–1811 to reclaim much of Traeth Mawr from the sea for farming use. Diversion of the Afon Glaslyn caused it to scour out a new natural harbour deep enough for small ocean-going sailing ships,John Dobson and Roy Woods, ''Ffe ...
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Mountains And Hills Of Snowdonia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Mountains And Hills Of Gwynedd
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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Bryn Cader Faner Stone Circle - Geograph
Bryn is a Welsh word meaning hill. It may also refer to: Places United Kingdom See also UK location England * Bryn, Greater Manchester ** Bryn (ward), an electoral ward in Wigan ** Bryn railway station * Cornwall Wales * Bryn, an electoral division of Conwy County Borough Council * Bryn, Llanelli in Carmarthenshire * Bryn, Neath Port Talbot * The Bryn, a village in Monmouthshire Elsewhere * Bryn, Akershus, Bærum, Norway * Bryn, Oslo, Norway ** Bryn Station * Bryn, Ukraine, a village in Ivano-Frankivsk Oblast, Ukraine Other uses * Bryn (given name), includes a list of people with the given name * Bryn (surname), includes a list of people with the surname * ''Bryn'', a 2003 album by Welsh bass-baritone Bryn Terfel * "Bryn", a 2008 song by Vampire Weekend from ''Vampire Weekend'' See also * Bryn Athyn, Pennsylvania, U.S. * Bryn Mawr, Pennsylvania, U.S. * Brin (other) * Bryne (other) * Brynn (other) Brynn is an Anglicised spelling of the Welsh give ...
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Standing Stones
A menhir (from Brittonic languages: ''maen'' or ''men'', "stone" and ''hir'' or ''hîr'', "long"), standing stone, orthostat, or lith is a large human-made upright stone, typically dating from the European middle Bronze Age. They can be found individually as monoliths, or as part of a group of similar stones. Menhirs' size can vary considerably, but they often taper toward the top. They are widely distributed across Europe, Africa and Asia, but are most numerous in Western Europe; particularly in Ireland, Great Britain, and Brittany, where there are about 50,000 examples, and northwestern France, where there are some 1,200 further examples. Standing stones are usually difficult to date. They were constructed during many different periods across pre-history as part of the larger megalithic cultures in Europe and near areas. Some menhirs stand next to buildings that have an early or current religious significance. One example is the South Zeal Menhir in Devon, which formed th ...
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Bronze Age
The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age system proposed in 1836 by Christian Jürgensen Thomsen for classifying and studying ancient societies and history. An ancient civilization is deemed to be part of the Bronze Age because it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from production areas elsewhere. Bronze is harder and more durable than the other metals available at the time, allowing Bronze Age civilizations to gain a technological advantage. While terrestrial iron is naturally abundant, the higher temperature required for smelting, , in addition to the greater difficulty of working with the metal, placed it out of reach of common use until the end o ...
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Bryn Cader Faner
Bryn Cader Faner is a Bronze Age round cairn which lies to the east of the small hamlet of Talsarnau in the Ardudwy area of Gwynedd in Wales Wales ( cy, Cymru ) is a country that is part of the United Kingdom. It is bordered by England to the east, the Irish Sea to the north and west, the Celtic Sea to the south west and the Bristol Channel to the south. It had a population in .... The diameter is and there are 18 thin jagged pillars which jut upwards from the low cairn. It is thought to date back to the late third millennium BC. The site was disturbed by 19th-century treasure-seekers, who left a hole in the centre indicating the position of a cist or a grave. Originally there may have been about 30 pillars, each some long. However, before the Second World War, the British army used the site for gunnery practice and damaged many of the stones on the east side. ''Bryn Cader Faner'' is thought to mean 'the hill with the chair with the flag' or 'the hill of the throne ...
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Talsarnau
Talsarnau () or Talsamau is a village and community in the Ardudwy area of Gwynedd in Wales. Its population was 525 in 2001, and had increased to 550 at the 2011 Census. The village of Talsarnau is situated on the A496 coastal road between Maentwrog and Harlech, close to the hamlets of Eisingrug and Llandecwyn. It has one primary school and one pub, "The Ship Aground", which starts serving food from 18:00 (6pm). Talsarnau railway station on the Cambrian Line serves the village. The community also includes Ynys Gifftan and Soar, Gwynedd. Notable people * Mary Evans (1735 – 1789 in Talsarnau), leader of a short-lived religious cult. * Ann Harriet Hughes (1852–1910) a Welsh language novelist * Sir Alfred Charles Glyn Egerton, FRS (1886–1959), chemist, he pioneered the use of liquid methane Methane ( , ) is a chemical compound with the chemical formula (one carbon atom bonded to four hydrogen atoms). It is a group-14 hydride, the simplest alkane, and the main co ...
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Trawsfynydd
Trawsfynydd (; Welsh for "across hemountain") is a linear village in Gwynedd, Wales, near Llyn Trawsfynydd reservoir, and adjacent to the A470 north of Bronaber and Dolgellau and 10 km (6 miles) south of Blaenau Ffestiniog. The total community area is 12,010 hectares (46.4 square miles) with a population of only 973. The area is sparsely populated with each hectare (acre) inhabited by an average 0.07 (0.03) persons. The village is typical of many Welsh villages. There is one grocery shop, one public house, a newsagent, a chemist, garage, petrol service station, and a branch of a large agricultural merchants. The community includes Bronaber. History Prehistoric people lived in the area in scattered groups of circular huts near the river, Afon Crawcwellt, about two miles south of today's village. A substantial Romano-British fort and settlement was established at Tomen y Mur in the first century CE. The area continued to be inhabited during sub Roman Britain. An example ...
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Blaenau Ffestiniog
Blaenau Ffestiniog is a town in Gwynedd, Wales. Once a slate mining centre in historic Merionethshire, it now relies much on tourists, drawn for instance to the Ffestiniog Railway and Llechwedd Slate Caverns. It reached a population of 12,000 at the peak development of the slate industry, but fell with the decline in demand for slate. The population of the community, including the nearby village Llan Ffestiniog, was 4,875 in the 2011 census: the fourth most populous in Gwynedd after Bangor, Caernarfon and Llandeiniolen. The population not including Llan is now only about 4,000. Etymology and pronunciation The meaning of Blaenau Ffestiniog is "uplands of Ffestiniog". The Welsh word ' is the plural of ' "upland, remote region". Ffestiniog here is probably "territory of Ffestin" (Ffestin being a personal name) or could possibly mean "defensive place". The English pronunciation of Blaenau Ffestiniog suggested by the ''BBC Pronouncing Dictionary of British Names'' is , but the f ...
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