Moel Y Gaer, Rhosesmor
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Moel Y Gaer, Rhosesmor
Moel y Gaer (Welsh for "bald hill of the fortress") is an Iron Age hillfort located on a summit at the southern end of Halkyn Mountain, overlooking the village of Rhosesmor, Flintshire, Wales. It is a well-preserved hillfort overlooking the Dee Estuary. Excavations in the early 1970s revealed a sequence of defensive structures made of timber and several phases of building work inside the ramparts. The hillfort Excavations suggest that the site was occupied, perhaps sporadically, from the Neolithic period to sometime before the Roman conquest of the area. Remains of a timber long house on the hill summit have been dated to the third millennium BC and may represent the earliest human occupation of the region. Defensive construction at the site began around the late seventh century BC, and at first consisted of a timber palisade enclosing a settlement of timber roundhouses. The palisade was later replaced by a stone-and-earth rampart and a ditch. Much of the archaeological work ...
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Moel Y Gaer, Rhosesmor
Moel y Gaer (Welsh for "bald hill of the fortress") is an Iron Age hillfort located on a summit at the southern end of Halkyn Mountain, overlooking the village of Rhosesmor, Flintshire, Wales. It is a well-preserved hillfort overlooking the Dee Estuary. Excavations in the early 1970s revealed a sequence of defensive structures made of timber and several phases of building work inside the ramparts. The hillfort Excavations suggest that the site was occupied, perhaps sporadically, from the Neolithic period to sometime before the Roman conquest of the area. Remains of a timber long house on the hill summit have been dated to the third millennium BC and may represent the earliest human occupation of the region. Defensive construction at the site began around the late seventh century BC, and at first consisted of a timber palisade enclosing a settlement of timber roundhouses. The palisade was later replaced by a stone-and-earth rampart and a ditch. Much of the archaeological work ...
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Welsh Language
Welsh ( or ) is a Celtic language family, Celtic language of the Brittonic languages, Brittonic subgroup that is native to the Welsh people. Welsh is spoken natively in Wales, by some in England, and in Y Wladfa (the Welsh colony in Chubut Province, Argentina). Historically, it has also been known in English as "British", "Cambrian", "Cambric" and "Cymric". The Welsh Language (Wales) Measure 2011 gave the Welsh language official status in Wales. Both the Welsh and English languages are ''de jure'' official languages of the Welsh Parliament, the Senedd. According to the 2021 United Kingdom census, 2021 census, the Welsh-speaking population of Wales aged three or older was 17.8% (538,300 people) and nearly three quarters of the population in Wales said they had no Welsh language skills. Other estimates suggest that 29.7% (899,500) of people aged three or older in Wales could speak Welsh in June 2022. Almost half of all Welsh speakers consider themselves fluent Welsh speakers ...
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British Iron Age
The British Iron Age is a conventional name used in the archaeology of Great Britain, referring to the prehistoric and protohistoric phases of the Iron Age culture of the main island and the smaller islands, typically excluding prehistoric Ireland, which had an independent Iron Age culture of its own. The parallel phase of Irish archaeology is termed the Irish Iron Age. The Iron Age is not an archaeological horizon of common artefacts but is rather a locally-diverse cultural phase. The British Iron Age followed the British Bronze Age and lasted in theory from the first significant use of iron for tools and weapons in Britain to the Romanisation of the southern half of the island. The Romanised culture is termed Roman Britain and is considered to supplant the British Iron Age. The tribes living in Britain during this time are often popularly considered to be part of a broadly-Celtic culture, but in recent years, that has been disputed. At a minimum, "Celtic" is a linguistic ter ...
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Hillfort
A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roman period. The fortification usually follows the contours of a hill and consists of one or more lines of earthworks, with stockades or defensive walls, and external ditches. Hillforts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC, and were used in many Celtic areas of central and western Europe until the Roman conquest. Nomenclature The spellings "hill fort", "hill-fort" and "hillfort" are all used in the archaeological literature. The ''Monument Type Thesaurus'' published by the Forum on Information Standards in Heritage lists ''hillfort'' as the preferred term. They all refer to an elevated site with one or more ramparts made of earth, stone and/or wood, with an external ditch. Many ...
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Halkyn Mountain
Halkyn ( cy, Helygain ; Flintshire Welsh: ''Lygian '') is a village and community in Flintshire, north-east Wales and situated between Pentre Halkyn, Northop and Rhosesmor. At the 2001 Census the population of the community was 2,876, increasing slightly to 2,879 at the 2011 Census. Pentre Halkyn is in the community. History Halkyn is one of the ancient parishes of Flintshire, originally comprising the townships of Hendrefigillt, Lygan y Llan and Lygan y Wern. The area was notable during the Roman occupation for the mining of lead. The village was recorded in the ''Domesday Book'' of 1086 as ''Alchene'', when it was then part of Cheshire, in England. Halkyn had many public houses in the early 19th century. These public houses included the Crown Inn, (now known as Crown Cottages) which was situated on the left-hand side as you go towards Rhes-y-cae from the Old Halkyn Post Office. The Royal Oak (now a private house known as the Old Royal Oak), directly opposite the Blue Bel ...
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Rhosesmor
Rhosesmor is a small village near Mold, Flintshire, in north-east Wales. The village lies near the parishes of Halkyn and Rhes-y-cae. The hamlet of Wern-y-Gaer is encompassed by the boundaries of the village. The hill fort site affords views across the Clwydian Hills to the west and the whole sweep of Wirral to the Sefton coastline and Liverpool and further east. History The new parish of Caerfallwch (the traditional Welsh placename for the village) was created on 23 October 1876, from part of the township of Caerfallwch, which until that time had been in the parish of Northop. The ''London Gazette'' of the 27 October 1876 defined the boundaries of the new parish: :"''All that part of the parish of Northop in the county of Flint and in the diocese of Saint Asaph which is comprised within and is co-extensive with the limits of that portion of the township of Caerfallwch wherein the present incumbent of the said parish of Northop now possesses the exclusive cure of souls, o ...
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Flintshire
, settlement_type = County , image_skyline = , image_alt = , image_caption = , image_flag = , image_shield = Arms of Flintshire County Council.svg , shield_size = 100px , shield_alt = , shield_link = , image_blank_emblem = , blank_emblem_alt = , image_map = File: Flintshire UK location map.svg , map_alt = , map_caption = Flintshire shown within Wales , coordinates = , subdivision_type = Sovereign state , subdivision_name = , subdivision_type1 = Constituent country , subdivision_type2 = Preserved county , subdivision_name1 = , subdivision_name2 = Clwyd , established_title ...
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Wales
Wales ( cy, Cymru ) is a Countries of the United Kingdom, country that is part of the United Kingdom. It is bordered by England to the Wales–England border, 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 2021 of 3,107,500 and has a total area of . Wales has over of coastline and is largely mountainous with its higher peaks in the north and central areas, including Snowdon (), its highest summit. The country lies within the Temperateness, north temperate zone and has a changeable, maritime climate. The capital and largest city is Cardiff. Welsh national identity emerged among the Celtic Britons after the Roman withdrawal from Britain in the 5th century, and Wales was formed as a Kingdom of Wales, kingdom under Gruffydd ap Llywelyn in 1055. Wales is regarded as one of the Celtic nations. The Conquest of Wales by Edward I, conquest of Wales by Edward I of England was completed by 1283, th ...
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Dee Estuary
The Dee Estuary ( cy, Aber Dyfrdwy) is a large estuary by means of which the River Dee flows into Liverpool Bay. The estuary starts near Shotton after a five-mile (8 km) 'canalised' section and the river soon swells to be several miles wide forming the boundary between the Wirral Peninsula in north-west England and Flintshire in north-east Wales. The Dee Estuary's largest towns along it include Hollywell, Flint, Connah's Quay, Shotton, Queensferry, Saltney Ferry, Chester (City), Heswall, West Kirby and Neston as well as other villages and towns alongside it. The A548 also passes along the estuary in Wales and parts of Cheshire West and Chester and Merseyside in England. The North Wales Coast Line follows the course of the Dee Estuary between Prestatyn and Chester. Geology The estuary is unusual in that comparatively little water occupies so large a basin. One theory is that larger rivers such as the Severn and/or Mersey once flowed into the Dee. The current view is ...
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Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in th ...
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Roman Conquest Of Britain
The Roman conquest of Britain refers to the conquest of the island of Britain by occupying Roman forces. It began in earnest in AD 43 under Emperor Claudius, and was largely completed in the southern half of Britain by 87 when the Stanegate was established. Conquest of the far north and Scotland took longer with fluctuating success. The Roman army was generally recruited in Italia, Hispania, and Gaul. To control the English Channel they used the newly formed fleet. The Romans under their general Aulus Plautius first forced their way inland in several battles against British tribes, including the Battle of the Medway, the Battle of the Thames, and in later years Caratacus's last battle and the Roman conquest of Anglesey. Following a widespread uprising in AD 60 in which Boudica sacked Camulodunum, VerulamiumChurchill, ''A History of the English-Speaking Peoples'', p. 7 and Londinium, the Romans suppressed the rebellion in the Defeat of Boudica. They went on eventually to ...
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Neolithic Long House
The Neolithic long house was a long, narrow timber dwelling built by the first farmers in Europe beginning at least as early as the period 5000 to 6000 BC. They first appeared in central Europe in connection with the early Neolithic cultures such as the Linear Pottery culture or Cucuteni culture. This type of architecture represents the largest free-standing structure in the world in its era. Long houses are present across numerous regions and time periods in the archaeological record. The long house was a rectangular structure, 5.5 to 7.0 m wide, of variable length, around 20 m up to 45 m. Outer walls were wattle and daub, sometimes alternating with split logs, with pitched, thatched roofs, supported by rows of poles, three across.The numbers are from Gimbutas (1991) pages 39–41. However, they are approximately the same as the numbers given by other researchers and can therefore be taken as true measurements within a tolerance. The exterior walls would have been quite short be ...
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