Caldicot Levels
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Caldicot Levels
The Caldicot and Wentloog Levels are two areas of low-lying estuarine alluvial wetland and intertidal mudflats adjoining the north bank of the Severn Estuary, either side of the River Usk estuary near Newport in south east Wales. They are also known collectively as the Monmouthshire Levels or Gwent Levels, and the name Wentloog is sometimes spelled Wentlooge in official publications. The Caldicot Level lies to the southeast of Newport between the River Usk and River Wye and consists of . It is home to Newport Wetlands Reserve. The Wentloog Level lies to the southwest between the River Usk and Rhymney River and consists of . The levels are formed from tidal deposits and alluvium, which have been recurrently inundated and reclaimed from the Severn Estuary by humans since Roman times. They have been patterns of settlement, enclosure and drainage systems belonging to successive periods of use, and are extremely rich archaeologically, with finds from the Mesolithic, Bronze Age ...
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Goldcliff Reen
Goldcliff ( cy, Allteuryn) is a village, parish and community to the south east of the city of Newport in South Wales. It lies within the Newport city boundaries in the historic county of Monmouthshire and the preserved county of Gwent. Administratively, the community of Goldcliff includes the village/parish of Whitson. The population in 2001 was 233; by 2011 it had risen to 329. Toponymy The name is said to have originated from the siliceous limestone cliff, standing about high, at Hill Farm, rising over a great bed of yellow mica which breaks the level at the shore and has a glittering appearance in sunshine, especially to ships passing in the Bristol Channel. Giraldus Cambrensis, who toured Wales in 1188 refers to the location as "Gouldclyffe" and describes it in Latin as "...glittering with a wonderful brightness". Bradney, Sir Joseph, ''A History of Monmouthshire, Vol 4 part 2: The Hundred of Caldicot'' (Part 2). pub 1914, reprinted 1994, Merton Priory Press. Charac ...
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Roman Britain
Roman Britain was the period in classical antiquity when large parts of the island of Great Britain were under occupation by the Roman Empire. The occupation lasted from AD 43 to AD 410. During that time, the territory conquered was raised to the status of a Roman province. Julius Caesar invaded Britain in 55 and 54 BC as part of his Gallic Wars. According to Caesar, the Britons had been overrun or culturally assimilated by other Celtic tribes during the British Iron Age and had been aiding Caesar's enemies. He received tribute, installed the friendly king Mandubracius over the Trinovantes, and returned to Gaul. Planned invasions under Augustus were called off in 34, 27, and 25 BC. In 40 AD, Caligula assembled 200,000 men at the Channel on the continent, only to have them gather seashells ('' musculi'') according to Suetonius, perhaps as a symbolic gesture to proclaim Caligula's victory over the sea. Three years later, Claudius directed four legi ...
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Redwick, Newport
Redwick ( cy, Y Redwig) is a small village and community (parish) to the south east of the city of Newport, in Wales, United Kingdom. It lies within the Newport city boundaries, in the historic county of Monmouthshire and the preserved county of Gwent. in 2011 the population was 206. Location Redwick is located 6 miles (9.5 km) south east of the centre of Newport and some 4 miles (6.5 km) south west of Caldicot, Monmouthshire on the flat coastal lands reclaimed from the Severn Estuary and Bristol Channel and part of the Caldicot and Wentloog Levels. The Church The ancient parish church of Church of St Thomas, Redwick is a Grade I listed building. It is notable for many unusual features. An earlier dedication, when it belonged to Tintern Abbey, appears to have been to St. Michael. It is held with Magor. The church is unusually large for a parish church on the Caldicot and Wentloog Levels, perhaps second only in its grandeur to that at Peterstone. The church has a full ...
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Nash, Newport
Nash ( cy, Trefonnen) is a village and community to the south of the city of Newport, South Wales, in the Lliswerry ward. Origin of the name The name is thought to originate from a contraction of "An Ash" (tree), meaning literally `place of the ash tree(s)'. This is supported by its appearance in deeds as "De Fraxino" (''fraxinus'' was the Latin name for the ash tree). The Welsh name is ''Trefonnen'', given in older sources as ''Tre'r onnen'', also meaning Town (''tref'') of the Ash (''onnen''). Nash and nearby Goldcliff, as Nash and Goldcliffe, are two of the few villages to appear on the Cambriae Typus map of 1573. Location Nash lies about to the south of the built-up area of the city of Newport, on the Caldicot levels, a large area of land reclaimed from the sea and crossed by drainage channels and reens. In addition to the village itself, the parish contains Uskmouth power stations and part of the Newport Wetlands nature reserve, including its Visitors Centre whi ...
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Salt Marsh
A salt marsh or saltmarsh, also known as a coastal salt marsh or a tidal marsh, is a coastal ecosystem in the upper coastal intertidal zone between land and open saltwater or brackish water that is regularly flooded by the tides. It is dominated by dense stands of salt-tolerant plants such as herbs, grasses, or low shrubs. These plants are terrestrial in origin and are essential to the stability of the salt marsh in trapping and binding sediments. Salt marshes play a large role in the aquatic food web and the delivery of nutrients to coastal waters. They also support terrestrial animals and provide coastal protection. Salt marshes have historically been endangered by poorly implemented coastal management practices, with land reclaimed for human uses or polluted by upstream agriculture or other industrial coastal uses. Additionally, sea level rise caused by climate change is endangering other marshes, through erosion and submersion of otherwise tidal marshes. However, recent ackn ...
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Magor, Monmouthshire
Magor (; cy, Magwyr) is a large village in Monmouthshire, south east Wales, about west of Chepstow and about east of Newport. It lies on the Caldicot Levels beside the Severn Estuary, and is in the community of Magor with Undy. Magor lies close to the M4 motorway. History The original Welsh language name ''Magwyr'', from which the English name is derived, is thought to originate from the Latin ''maceria'', meaning masonry walls or ruins. It may relate either to a now-lost Roman villa in the area, or alternatively to sea defences or a causeway built by the Romans. Magor and the surrounding area contain many Roman ruins and artefacts, and the village centre was originally located at the inner edge of salt marshes which the Romans began to reclaim as farmland. The local name "Whitewall" may relate to the same causeway, which would have connected the village to a small now-vanished harbour on the Severn Estuary known as Abergwaitha or Aberweytha. In 1994 the remains of a 13th-ce ...
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Wilcrick
Wilcrick ( cy, Chwilgrug) is a hamlet within the administrative boundary of the city of Newport, South Wales, just to the west of Magor and approximately southeast of Newport city centre. It is within the historic county of Monmouthshire. Etymology The name translates from the Welsh as a "bare hill" or "mound". Archaeology Willcrick is located on the B4245 road to the northwest of Magor. To the southeast of the village is Wilcrick Hill which has a hillfort on its summit, of which only the earthworks remain. Archaeological evidence of a small Iron Age settlement found preserved under peat at Barland's Farm suggests that the occupiers may have used the Caldicot and Wentloog Levels to pasture their cattle when conditions permitted, and may have moved into the hillfort when the Levels were too wet to be useable. Nearby, a nearly complete 3rd century Romano-British oak boat was found beside a buried stone and timber quay in 1993, during the building of a distribution depot a ...
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Romano-British
The Romano-British culture arose in Britain under the Roman Empire following the Roman conquest in AD 43 and the creation of the province of Britannia. It arose as a fusion of the imported Roman culture with that of the indigenous Britons, a people of Celtic language and custom. Scholars such as Christopher Snyder believe that during the 5th and 6th centuries – approximately from 410 when the Roman legions withdrew, to 597 when St Augustine of Canterbury arrived – southern Britain preserved an active sub-Roman culture that survived the attacks from the Anglo-Saxons and even used a vernacular Latin when writing. Arrival of the Romans Roman troops, mainly from nearby provinces, invaded in AD 43, in what is now part of England, during the reign of Emperor Claudius. Over the next few years the province of Britannia was formed, eventually including the whole of what later became England and Wales and parts of Scotland.Kinder, H. & Hilgemann W. ''The Penguin Atlas of World ...
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Uskmouth
Uskmouth ( cy, Aberwysg) is an area to the south of the city of Newport, South Wales. Location Uskmouth is effectively in the west of the village of Nash. It is at Uskmouth that the River Usk meets the Severn estuary. Amenities It includes part of the Newport Wetlands Reservebr> a notable wildlife reservebr> with reed beds and grasslands that attract breeding birds such as lapwings, redshanks, oystercatchers, little ringed plovers and ringed plovers, as well as visitors such as wigeons, shovelers, teals, shelducks and pintails, bitterns, hen harriers and short-eared owls. It is part of the Caldicot Levels. Following storms in the autumn of 1986, a track of human footprints was discovered eroding out of the clays in the intertidal zone in front of Uskmouth Power Station. The footprints were found to contain peat deposits, allowing them to be carbon dated to 4200BC. At the time they were the oldest known human footprints in Britain, but in 2013 footprints made about 800,0 ...
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Goldcliff
Goldcliff ( cy, Allteuryn) is a village, parish and community to the south east of the city of Newport in South Wales. It lies within the Newport city boundaries in the historic county of Monmouthshire and the preserved county of Gwent. Administratively, the community of Goldcliff includes the village/parish of Whitson. The population in 2001 was 233; by 2011 it had risen to 329. Toponymy The name is said to have originated from the siliceous limestone cliff, standing about high, at Hill Farm, rising over a great bed of yellow mica which breaks the level at the shore and has a glittering appearance in sunshine, especially to ships passing in the Bristol Channel. Giraldus Cambrensis, who toured Wales in 1188 refers to the location as "Gouldclyffe" and describes it in Latin as "...glittering with a wonderful brightness". Bradney, Sir Joseph, ''A History of Monmouthshire, Vol 4 part 2: The Hundred of Caldicot'' (Part 2). pub 1914, reprinted 1994, Merton Priory Press. Character ...
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Site Of Special Scientific Interest
A Site of Special Scientific Interest (SSSI) in Great Britain or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland is a conservation designation denoting a protected area in the United Kingdom and Isle of Man. SSSI/ASSIs are the basic building block of site-based nature conservation legislation and most other legal nature/geological conservation designations in the United Kingdom are based upon them, including national nature reserves, Ramsar sites, Special Protection Areas, and Special Areas of Conservation. The acronym "SSSI" is often pronounced "triple-S I". Selection and conservation Sites notified for their biological interest are known as Biological SSSIs (or ASSIs), and those notified for geological or physiographic interest are Geological SSSIs (or ASSIs). Sites may be divided into management units, with some areas including units that are noted for both biological and geological interest. Biological Biological SSSI/ASSIs may ...
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Iron Age
The Iron Age is the final epoch of the three-age division of the prehistory and protohistory of humanity. It was preceded by the Stone Age (Paleolithic, Mesolithic, Neolithic) and the Bronze Age (Chalcolithic). The concept has been mostly applied to Iron Age Europe and the Ancient Near East, but also, by analogy, to other parts of the Old World. The duration of the Iron Age varies depending on the region under consideration. It is defined by archaeological convention. The "Iron Age" begins locally when the production of iron or steel has advanced to the point where iron tools and weapons replace their bronze equivalents in common use. In the Ancient Near East, this transition took place in the wake of the Bronze Age collapse, in the 12th century BC. The technology soon spread throughout the Mediterranean Basin region and to South Asia (Iron Age in India) between the 12th and 11th century BC. Its further spread to Central Asia, Eastern Europe, and Central Europe is somewhat dela ...
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