Avening Valley
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Avening Valley
The Avening Valley is located in the South Cotswolds in England, running roughly east from Nailsworth and through the village of Avening. During the 17th century, the cloth industry developed in the Avening Valley, with mills powered by the Avening Stream. One of the larger cloth mills was named the Holcombe Mill (an old "gig" mill), which was adapted in 1879 for manufacture of bedding. Another is at Longfords Mills, Minchinhampton Minchinhampton is an ancient Cotswolds market town in the Stroud District in Gloucestershire, South West England. The town is located on a hilltop, south-east of Stroud. The common offers wide views over the Severn Estuary into Wales and furth .... References Valleys of Gloucestershire Cotswolds {{Gloucestershire-geo-stub ...
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Village Stream - Geograph
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church.
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Cotswolds
The Cotswolds (, ) is a region in central-southwest England, along a range of rolling hills that rise from the meadows of the upper Thames to an escarpment above the Severn Valley and Evesham Vale. The area is defined by the bedrock of Jurassic limestone that creates a type of grassland habitat rare in the UK and that is quarried for the golden-coloured Cotswold stone. The predominantly rural landscape contains stone-built villages, towns, and stately homes and gardens featuring the local stone. Designated as an Area of Outstanding Natural Beauty (AONB) in 1966, the Cotswolds covers making it the largest AONB. It is the third largest protected landscape in England after the Lake District and Yorkshire Dales national parks. Its boundaries are roughly across and long, stretching southwest from just south of Stratford-upon-Avon to just south of Bath near Radstock. It lies across the boundaries of several English counties; mainly Gloucestershire and Oxfordshire, and parts ...
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England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ...
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Nailsworth
Nailsworth is a town and civil parish in Gloucestershire, England, lying in one of the Stroud Valleys in the Cotswolds, on the A46 road (the Roman Fosse Way), south of Stroud and about north-east of Bristol and Bath. The parish had a population of 5,794 at the 2011 census. History Nailsworth in ancient times was a settlement at the confluence of the Avening Valley and the Woodchester Valley, on the Nailsworth Stream, and from the 1st or 2nd centuries CE on the Roman Fosse Way. Among many notable historic medieval buildings in the area are Beverston Castle and Owlpen Manor. In the modern era, Nailsworth was a small mill town and centre for brewing. It was connected directly to the UK national rail network between 1867 and 1947, as the terminus of the Stonehouse and Nailsworth Railway. Amenities These days Nailsworth is visited in the summer by walkers. It holds a farmers' market every fourth Saturday in the month. Local events such as the market and the Nailsworth Festival ...
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Minchinhampton
Minchinhampton is an ancient Cotswolds market town in the Stroud District in Gloucestershire, South West England. The town is located on a hilltop, south-east of Stroud. The common offers wide views over the Severn Estuary into Wales and further into the Cotswolds. Toponymy The place-name 'Minchinhampton' is first attested as ''Hantone'' in the Domesday Book of 1086. It appears as ''Minchenhamtone'' in the Assize Rolls of 1221. The name was originally the Old English ''Heatun'', meaning "high town or settlement". The additional element is the Old English ''mynecen'', meaning a nun, which is related to the modern word "monk". Minchinhampton at one time belonged to the nunnery in Caen in Normandy, France. Thus the name means "the nuns' high town or settlement". . On a map of 1825 (published 1828) the town is labelled "Minching-Hampton" (see external links). Amenities and features The main square has a war memorial, and a 17th-century Market House, given to the town in 1919 by t ...
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Valleys Of Gloucestershire
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ...
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