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Conwy Mountain
Mynydd y Dref (Welsh : ''"Mountain of the Town"'') or Conwy Mountain is a hilly area to the west of the town of Conwy, in North Wales. To the north it overlooks the sea of Conwy Bay, and to the south lie the foothills of the Carneddau range of mountains, of which it forms a part. Mynydd y Dref is the remains of an ancient volcano that erupted about 450 million years ago. At the summit of Conwy Mountain are the Neolithic Hut Circles and the Iron Age hillfort of Castell Caer Seion (sometimes called Castell Caer Lleion). Castell Caer Seion comprised a stone walled fort, and remains show this to have been an extensive site, incorporated more than 50 hut circles and levelled platform houses, and with a citadel and outposts. Limited excavations were undertaken in 1951. No datable remains were found, only slingstones, querns and stone pestles and mortars, which suggests that, unlike many hillforts in north Wales, this site was not reoccupied in the late Roman period. Millstones w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conwy
Conwy (, ), previously known in English as Conway, is a walled market town, community and the administrative centre of Conwy County Borough in North Wales. The walled town and castle stand on the west bank of the River Conwy, facing Deganwy on the east bank. The town formerly lay in Gwynedd and prior to that in Caernarfonshire. The community, which also includes Deganwy and Llandudno Junction, had a population of 14,753 at the 2011 census. Although the community of Conwy straddles the River Conwy, for postal purposes the areas on the east bank form part of the post town of Llandudno Junction, with the Conwy post town being confined to west bank of the river. The ward on the west bank of the river had a population of 4,065 at the 2011 census. The resident population of the wider Conwy County Borough was estimated to be 116,200 in an ONS-estimate. The name 'Conwy' derives from the old Welsh words ''cyn'' (chief) and ''gwy'' (water), the river being originally called the 'Cynwy'. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quern-stone
Quern-stones are stone tools for hand-grinding a wide variety of materials. They are used in pairs. The lower stationary stone of early examples is called a saddle quern, while the upper mobile stone is called a muller, rubber or handstone. The upper stone was moved in a back-and-forth motion across the saddle quern. Later querns are known as rotary querns. The central hole of a rotary quern is called the eye, and a dish in the upper surface is known as the hopper. A handle slot contained a handle which enabled the rotary quern to be rotated. They were first used in the Neolithic era to grind cereals into flour. Uses of quern-stones An old Gaelic proverb is "The quern performs best when the grindstone has been pitted." Design of quern-stones The upper stones were usually concave while the lower ones were convex. Quern-stones are frequently identifiable by their grooved working surfaces which enabled the movement of flour. Sometimes a millrind was present as a piece of wood (or o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of Wales
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Conwy County Borough
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Category:Hillforts In Conwy County Borough ...
{{Commons category, Hill forts in Conwy County Borough Hillforts Conwy Conwy (, ), previously known in English as Conway, is a walled market town, community and the administrative centre of Conwy County Borough in North Wales. The walled town and castle stand on the west bank of the River Conwy, facing Deganwy on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Hillforts In Wales
This is a list of hillforts in Wales. Anglesey *Bwrdd Arthur, Din Sylwy (Bwrdd Arthur) (), contour fort *Caer Idris Hillfort (), promontory fort *Caer y Twr (), partial contour fort *Dinas Gynfor (), promontory fort *Dinas Porth Ruffydd (), promontory fort *Mynydd Llwydiarth (Anglesey), Mynydd Llwydiarth (), promontory fort *Parciau hill fort (), promontory fort *Tan-y-graig, Llanffinan (), contour fort *Twyn-y-Parc (), promontory fort *Y Werthyr hillfort (), marsh fort *Y Werthyr, Llanddeusant (), contour fort *Ynys-y-Fydlyn (), promontory fort Bridgend County Borough *Cae Summerhouse Camp (), partial contour fort *Chapel Hill Camp, Merthyr Mawr House (), contour fort *Coed-y-Mwstwr (), contour fort *Cwm Llwyd (), partial contour fort *Mynydd Twmpathyddaer (), contour fort *Mynydd y Gaer hillfort, Mynydd y Gaer (), partial contour fort *Pen y Castell, Kenfig Hill (), contour fort *Y Bwlwarcau (), multiple enclosure hillfort *Y Bwlwarcau, Eastern Enclosure (), hillslope fort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bangor, Gwynedd
Bangor (; ) is a cathedral city and community A community is a social unit (a group of living things) with commonality such as place, norms, religion, values, customs, or identity. Communities may share a sense of place situated in a given geographical area (e.g. a country, village, ... in Gwynedd, North Wales. It is the oldest city in Wales. Historic counties of Wales, Historically part of Caernarfonshire, it had a population of 18,322 in 2019, according to the Office for National Statistics. Landmarks include Bangor Cathedral, Bangor University, Garth Pier, and the Menai Suspension Bridge and Britannia Bridge which connect the city to the Anglesey, Isle of Anglesey. History The origins of the city date back to the founding of a monastic establishment on the site of Bangor Cathedral by the Celtic saint Deiniol in the early 6th century AD. itself is an old Welsh word for a wattled enclosure, such as the one that originally surrounded the cathedral site. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prestatyn
Prestatyn is a seaside town and community in Denbighshire, Wales. Historically a part of Flintshire, it is located on the Irish Sea coast, to the east of Rhyl. Prestatyn has a population of 19,085, History Prehistory There is evidence that the current town location has been occupied since prehistoric times. Prehistoric tools found in the caves of Graig Fawr, in the nearby village of Meliden, have revealed the existence of early human habitation in the area. Roman The Roman bathhouse is believed to be part of a fort on the road from Chester to Caernarfon. However, much of "Roman Prestatyn" has been destroyed as houses have been built over unexcavated land. Medieval The name Prestatyn derives from the Old English ''prēosta'' ("priests, the genitive plural of ''prēost'') and ''tūn'' ("town"), and was recorded in the ''Domesday Book'' as ''Prestetone''. Unlike similarly derived names in England, which generally lost their penultimate syllable and became Preston, this villag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Wales Path
The North Wales Path ( cy, Llwybr y Gogledd) is a long-distance walk of some that runs close to the coast of northern Wales between Prestatyn in the east and Bangor in the west. Parts of it overlap with the Wales Coast Path. The path runs along parts of the Clwydian Range and Dee Valley Area of Outstanding Natural Beauty (AONB). The path was devised, implemented and maintained by the then Countryside Council for Wales (merged to form Natural Resources Wales) and the three councils of: Gwynedd, Conwy, and Denbighshire. Route The route mostly follows existing public footpaths and is waymarked with its own logo. The path can easily be broken up into smaller, accessible sections, and many of these are well used. Popular sections include the Prestatyn–Dyserth Way, a former railway trackbed, the Great Orme and Little Orme at Llandudno, Mynydd y Dref (Conwy Mountain) between Conwy and Sychnant Pass, and Aber Falls. Interconnecting paths The Wales Coast Path, an long-distanc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sychnant Pass
Sychnant Pass (Welsh: ''Bwlch Sychnant'', "Dry-stream Pass") in Conwy County Borough, Wales, links Conwy to Penmaenmawr via Dwygyfylchi. Much of the pass is in Snowdonia National Park, and a large area of land within it has been designated a Site of Special Scientific Interest. At the bottom is the village of Capelulo, which lends its name to the community of Penmaenmawr. Before the coming of the railway to the North Wales coast, the road through Sychnant Pass was the route of choice for mail coaches at high tide, when the faster and safer route along the sands was unusable. After leaving Conwy, the route runs westward through the valley on the south side of Mynydd y Dref (Conwy Mountain), which is topped by the hillfort of Castell Caer Seion. There are parallel tracks and footpaths (including the North Wales Path) on Mynydd y Dref for most of the way. Also Allt-Wen () and Penmaenbach () can be climbed from here. At the western end of the valley, the Sychnant Pass Road runs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Napoleonic Wars
The Napoleonic Wars (1803–1815) were a series of major global conflicts pitting the French Empire and its allies, led by Napoleon I, against a fluctuating array of European states formed into various coalitions. It produced a period of French domination over most of continental Europe. The wars stemmed from the unresolved disputes associated with the French Revolution and the French Revolutionary Wars consisting of the War of the First Coalition (1792–1797) and the War of the Second Coalition (1798–1802). The Napoleonic Wars are often described as five conflicts, each termed after the coalition that fought Napoleon: the Third Coalition (1803–1806), the Fourth (1806–1807), the Fifth (1809), the Sixth (1813–1814), and the Seventh (1815) plus the Peninsular War (1807–1814) and the French invasion of Russia (1812). Napoleon, upon ascending to First Consul of France in 1799, had inherited a republic in chaos; he subsequently created a state with stable financ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hut Circle
In archaeology, a hut circle is a circular or oval depression in the ground which may or may not have a low stone wall around it that used to be the foundation of a round house. The superstructure of such a house would have been made of timber and thatch. They are numerous in parts of upland Britain and most date to around the 2nd century BC. Hut circles are usually around in internal diameter, the rocks themselves being wide and around high. Hut circles were also almost certainly covered by conical rounded roofs and supported by posts that were internal and sometimes external. Wales There are more than 100 registered hut circles and enclosures in Wales. They are to be found in areas which have not been ploughed and the stones have not been disturbed. They are quite common in the north. Remains of a hut circle on Tre'r Ceiri - geograph.org.uk - 1571421.jpg, Tre'r Ceiri Celtic Iron Age hut circle Cytiau Celtaidd - Celtic Iron Age Huts at Mynydd Twr, Caergybi (Holyhead), Wale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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