Lilburn, Northumberland
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Lilburn, Northumberland
Lilburn is a small village in Northumberland, England. It is located in the on the edge of the Cheviots. The local farming estate is centred on Lilburn Tower. The area is noted for its large number of earthworks and remains of prehistoric settlements. Governance Lilburn is in the parliamentary constituency of Berwick-upon-Tweed Berwick-upon-Tweed (), sometimes known as Berwick-on-Tweed or simply Berwick, is a town and civil parish in Northumberland, England, south of the Anglo-Scottish border, and the northernmost town in England. The 2011 United Kingdom census reco .... References Villages in Northumberland {{Northumberland-geo-stub ...
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Alnwick
Alnwick ( ) is a market town in Northumberland, England, of which it is the traditional county town. The population at the 2011 Census was 8,116. The town is on the south bank of the River Aln, south of Berwick-upon-Tweed and the Scottish border, inland from the North Sea at Alnmouth and north of Newcastle upon Tyne. The town dates to about AD 600 and thrived as an agricultural centre. Alnwick Castle was the home of the most powerful medieval northern baronial family, the Earls of Northumberland. It was a staging post on the Great North Road between Edinburgh and London. The town centre has changed relatively little, but the town has seen some growth, with several housing estates covering what had been pasture and new factory and trading estate developments along the roads to the south. History The name ''Alnwick'' comes from the Old English ''wic'' ('dairy farm, settlement') and the name of the river Aln. The history of Alnwick is the history of the castle and its ...
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Northumberland
Northumberland () is a county in Northern England, one of two counties in England which border with Scotland. Notable landmarks in the county include Alnwick Castle, Bamburgh Castle, Hadrian's Wall and Hexham Abbey. It is bordered by land on three sides; by the Scottish Borders region to the north, County Durham and Tyne and Wear to the south, and Cumbria to the west. The fourth side is the North Sea, with a stretch of coastline to the east. A predominantly rural county with a landscape of moorland and farmland, a large area is part of Northumberland National Park. The area has been the site of a number of historic battles with Scotland. Name The name of Northumberland is recorded as ''norð hẏmbra land'' in the Anglo-Saxon Chronicle, meaning "the land north of the Humber". The name of the kingdom of ''Northumbria'' derives from the Old English meaning "the people or province north of the Humber", as opposed to the people south of the Humber Estuary. History ...
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Berwick-upon-Tweed (UK Parliament Constituency)
Berwick-upon-Tweed () is a parliamentary constituency in Northumberland represented in the House of Commons of the UK Parliament since 2015 by Anne-Marie Trevelyan, a Conservative. It was a parliamentary borough in the county of Northumberland of the House of Commons of England from 1512 to 1706, then of the House of Commons of Great Britain from 1707 to 1800 and of the House of Commons of the United Kingdom from 1801 to 1885. It returned two Members of Parliament (MPs), elected by the bloc vote system. It has been a county constituency since 1885, electing one MP under the first-past-the-post system. Profile The constituency of Berwick-upon-Tweed is in the county of Northumberland. It includes as its northernmost point the town of Berwick-upon-Tweed and stretches south to include the towns of Alnwick and Amble — the Northumberland coast forms its long eastern boundary. Its length is roughly 50 miles (80 km) and its area is 2,310 square kilometres. Predominantly r ...
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Cheviots
The Cheviot Hills (), or sometimes The Cheviots, are a range of uplands straddling the Anglo-Scottish border between Northumberland and the Scottish Borders. The English section is within the Northumberland National Park. The range includes The Cheviot (the highest hill), plus Hedgehope Hill to the east, Windy Gyle to the west, and Cushat Law and Bloodybush Edge to the south. The hills are sometimes considered a part of the Southern Uplands of Scotland as they adjoin the uplands to the north. Since the Pennine Way runs through the region, the hills are also considered a part of the northern Pennines although they are separated from the Cheviot Hills by the Tyne Gap, part of which lies within the southern extent of the Northumberland National Park. The Cheviot Hills are primarily associated with geological activity from approximately 480 to 360 million years ago, when the continents of Avalonia and Laurentia collided, resulting in extensive volcanic activity (the Caledonian or ...
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Lilburn Tower
Lilburn Tower is a privately owned 19th-century mansion house at Lilburn, near Wooler, Northumberland. The property is a Grade II* listed building and forms part of the Lilburn Estate. A number of discrete buildings and monuments are scattered across the grange, including the Hurlestone, Hurlestone Tower and an astronomical observatory. The ancient manors of East and West Lilburn were united when both were purchased separately by John Clennell of the Clennel family of Clennell Hall about 1700. The ruinous remains of the old 15th-century manor house, known as West Lilburn Tower, which incorporated a pele tower, are scheduled as an Ancient Monument and protected by Grade II listed building status. On the death of Thomas Clennel, the estate devolved to his nephew, Henry Collingwood, who was High Sheriff of Northumberland in 1793. The estate was bequeathed to Henry John William Collingwood of Cornhill in the 1820s, and in 1828 he began the construction of the imposing new Elizabet ...
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Earthworks (engineering)
Earthworks are engineering works created through the processing of parts of the earth's surface involving quantities of soil or unformed rock. Shoring structures An incomplete list of possible temporary or permanent geotechnical shoring structures that may be designed and utilised as part of earthworks: *Mechanically stabilized earth *Earth anchor * Cliff stabilization *Grout curtain *Retaining wall *Slurry wall *Soil nailing *Tieback (geotechnical) *Trench shoring * Caisson *Dam *Gabion *Ground freezing Gallery File:Mechanically stabilized earth diagram.gif, Mechanically stabilized earth File:GroutCurtain.gif, Grout curtain File:Retaining Wall Type Function.jpg, Retaining wall types File:Soil Nail.jpg, Soil nailing File:FEMA - 6044 - Photograph by Larry Lerner taken on 03-15-2002 in New York.jpg, Tieback File:Sbh s600.JPG, Trench shoring File:Caisson Schematic.svg, Caisson File:Vyrnwy dam.JPG, Dam File:Gabion 040.jpg, Gabions File:Cross section of a ground freezing pipe as u ...
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Prehistoric
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. T ...
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British House Of Commons
The House of Commons is the lower house of the Parliament of the United Kingdom. Like the upper house, the House of Lords, it meets in the Palace of Westminster in London, England. The House of Commons is an elected body consisting of 650 members known as members of Parliament (MPs). MPs are elected to represent constituencies by the first-past-the-post system and hold their seats until Parliament is dissolved. The House of Commons of England started to evolve in the 13th and 14th centuries. In 1707 it became the House of Commons of Great Britain after the political union with Scotland, and from 1800 it also became the House of Commons for Ireland after the political union of Great Britain and Ireland. In 1922, the body became the House of Commons of the United Kingdom of Great Britain and Northern Ireland after the independence of the Irish Free State. Under the Parliament Acts 1911 and 1949, the Lords' power to reject legislation was reduced to a delaying power. The gov ...
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