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Walmore Common

Ramsar sites in EnglandSites of Special Scientific Interest in GloucestershireSpecial Protection Areas in England
Walmore Common geograph.org.uk 350415
Walmore Common geograph.org.uk 350415

Walmore Common (grid reference SO740162 & grid reference SO745150) is a 57.78-hectare (142.8-acre) nature reserve on the flood-plain of the River Severn, west of the city of Gloucester in England and north of the village of Chaxhill. It was notified as a biological Site of Special Scientific Interest in 1966. The site is listed in the 'Forest of Dean Local Plan Review' as a Key Wildlife Site (KWS).The common is recognised as a wetland area of international importance and is designated as a Ramsar site. The common is recognised as a Special Protection Area (SPA) under the EC Directive on the conservation of Wild Birds.

Excerpt from the Wikipedia article Walmore Common (License: CC BY-SA 3.0, Authors, Images).

Walmore Common
A48, Gloucester Westbury-on-Severn

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Geographical coordinates (GPS)

Latitude Longitude
N 51.833476 ° E -2.370743 °
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Address

Walmore Hill Primary School

A48
GL2 8LA Gloucester, Westbury-on-Severn
England, United Kingdom
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Phone number

call+441452750373

Website
walmorehillschool.co.uk

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Walmore Common geograph.org.uk 350415
Walmore Common geograph.org.uk 350415
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River Frome, Stroud
River Frome, Stroud

The River Frome, once also known as the Stroudwater, is a small river in Gloucestershire, England. It is to be distinguished from another River Frome in Gloucestershire, the Bristol Frome, and the nearby River Frome, Herefordshire. The river is approximately 25 miles (40 km) long.It flows broadly westwards, from its source high up on the Cotswold escarpment, initially through a narrow, steep-sided valley, which it shares with the Thames and Severn Canal and the Golden Valley line railway. Below Stroud, the main town on the river, it is swelled by flows from several tributaries, and the valley opens out, with the channel splitting into two before reuniting into a single channel. The river, as well as its tributaries, has been used for milling since the time of the Domesday Book. Some early mills were used for milling corn but subsequently the river was important for the woollen industry, until that experienced a series of depressions in the early 19th century. The area then became known for the production of walking sticks and umbrella sticks, an industry that lasted into the mid-20th century. Steam engines were installed from the 1810s onwards, but were often used to assist when water power was insufficient, rather than to replace water power. Despite the demise of milling, many mill buildings survive along the course of the river, a significant number of which are listed buildings, in recognition of their architecture. The river has undergone modification over the years, not least to power the mills. There was an early attempt to make it navigable as far as Stroud, using cranes to move containers from boats at one level to those at another level, at places where a mill dam prevented through navigation. The scheme was abandoned before it was completed, due to the cost of construction and the time taken to tranship the containers. Communication was later provided by the Stroudwater Navigation, a separate canal which followed the route of the river from the River Severn to Wallbridge and opened in 1779. This was later extended through to the River Thames by the construction of the Thames and Severn Canal, which opened in 1789. Both are now part of the Cotswold Canals Trust, and are being restored. A small part of both canals near their junction is classified as a main river, because three of the tributaries of the Frome were diverted into them in the 1950s as part of a flood prevention scheme. Despite the number of historical weirs and modern flood defence structures, the river is not classified as heavily modified, although the modification of its channel, together with the volume of water abstracted to supply the canals and for the drinking water industry, mean that its water quality is only rated moderate under the terms of the Water Framework Directive, as both factors affect the ability of fish to move freely along the river.

Severn bore
Severn bore

The Severn bore is a tidal bore seen on the tidal reaches of the River Severn in south western England. It is formed when the rising tide moves into the funnel-shaped Bristol Channel and Severn Estuary and the surging water forces its way upstream in a series of waves, as far as Gloucester and beyond. The bore behaves differently in different stretches of the river; in the lower, wider parts it is more noticeable in the deep channels as a slight roller, while the water creeps across the sand and mudflats. In the narrower, upper reaches, the river occupies the whole area between its banks and the bore advances in a series of waves that move upstream. Near Gloucester, the advancing water overcomes two weirs, and sometimes one in Tewkesbury, before finally petering out. Bores are present on about 130 days in the year, concentrated on the days immediately following the new and full moon. The size and precise timing of the bore depend on such things as the time of high tide, the barometric pressure, the wind speed and direction, the amount of water coming down the river and how well scoured the main drainage channels are. There are a number of viewpoints from which the bore can be seen, or viewers can walk along the river bank or floodbanks. Historically, the bore has been of importance to shipping visiting the docks at Gloucester, but this was alleviated by the construction of an alternative route, the Gloucester and Sharpness Canal, which opened in 1827. Nowadays the bore is of interest to surfers and canoeists who attempt to ride the waves.