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Display PDF in Separate -Qnuthprn E n v ir o n m e n t A g e n c y Environment Agency - a better organisation works for the public and environment in England and Wales has specific duties and powers. for present and future generations. Nationally, around 15 million hectares The Environment Agency is one of the of land are managed by the Agency world's most powerful environmental along with 36,000km of rivers and watchdogs, regulating air, land and 5,000km of coastline, including more water. As 'guardians of the than 2 million hectares of coastal environment' the Agency has legal waters. duties to protect and improve the There are eight regional offices, which environment throughout England and are split into 26 area offices. Southern Wales and in doing so contributes Region covers the counties of Kent, towards 'sustainable development' - Sussex, Hampshire and the Isle of meeting the needs of today without Wight. harming future generations. Created by the 1995 Environment Act, the Agency started work in 1996. It is officially a 'non-departmental public body', which means that the Front cover photographs: Main picture ■ Eastern Yar Top inset - Codshill Church Bottom inset - Sea defences Freshwater Bay Nettlestone Bembridge Rivers of the Isle of Wight History and Geology Popular as a holiday destination with clay contain Europe's most abundant an 'abroad feel' to it, the Isle of Wight dinosaur fossil beds. is the largest Island off the English There are three distinct rock coast. It is separated from Hampshire formations, the Tertiary Clays and by the Solent and bounded by the Sands to the north, the central chalk English Channel on its south side. ridge that once connected The Evidence suggests that the first settlers, Needles to the chalk of the Isle of the New Stone Age communities, Purbeck and the Greensands, Gault arrived on the Island sometime after and Wealden Clays to the south of the 4,000 BC. As the population expanded island. These rocks were laid down large areas of woodland were cleared over a period of time dating back to for agriculture and by the Middle Ages the Cretaceous (1 35 million years ago) the Island had become a mixed and the Tertiary (65 million years ago) agricultural landscape. timescales. The last two million years (Quaternary) complete the geological By Tudor times seven deer parks had story of the island. been created. Queen Victoria and Prince Albert added their royal seal of The Island's topography reflects the approval when they made Osbourne geology and forms distinctive areas of House their Island home, causing a the landscape: large development of Victorian villas • high central ridge of chalk downs and gardens to spring up. and the Southern Chalk Downs The Island formed part of the • the Creensand ridge mainland until well after the last ice • northern clay pastures age. Despite its small size - 381 km2 • intensively managed southern (155 square miles) - the Isle of Wight coastal plains, river valleys and has a varied geology and its rocks and dramatic coastline Main picture: South Wight coast Rivers of the Isle of Wight Until well after the last ice age the Isle dismembered by the sea breaking into of Wight was part of the mainland. A the main channel between Purbeck major trunk stream, the Solent River, and the Island. flowed eastwards from the River Frome This breach occurred as a result of a in Dorset along the line of the Solent depression of the land, or rise in sea and Spithead, to outfall to the sea in level, which lasted until about 2000 BC the Littlehampton area. Its northern and also led to the submergence of tributaries would have included the the downstream reaches of the North Avon, Test and Itchen and its southern flowing rivers, giving them their well tributaries would have been the marked estuaries. The Harbours of streams which drained from the Yarmouth, Newtown, Cowes and northern slopes of Purbeck and the Isle Wootton Creek owe their origins to of Wight. The drainage system was this movement. Wootton Creek O Rivers Calboume Mill Apart from a few small brooks on the woodlands. The Island's estuaries are south coast, all the Island's streams the remnants of once large valley flow northwards. Included among systems that carried rivers into the these are the Western Yar, Newtown great Solent estuary. River (Caul Bourne) and the Palmer's, Rivers not fed from the chalk aquifer Blackbridge and Monktonmead like the Merstone Stream or Thorley Brooks. Brook tend to have a 'flashy' response There are five main estuary systems - to rainfall and suffer from naturally low the Eastern Yar, Western Yar, flows in the summer. However, rivers Newtown, Medina and Wootton fed by springs from the chalk like Creek. All share common features of Lukely Brook do not tend to react tidal mudflats and shingle, saltmarsh rapidly to rainfall except when coupled and varying amounts of fringing with urban run off. 9 Rivers of the Isle of Wight Medina The Isle of Wight's major rivers are the Medina and the Eastern Yar. The Medina rises as chalk springs from St Catherine's Down on the south side of the Island. Medina is a latinised form of its Saxon name Medene meaning Middle River. The Medina is 1 7km long, with a catchment area of 71 sq km, and flows due north collecting the Merstone Stream at Blackwater before intersecting the ridge at Shide. It is a linear estuary enclosed by a low valley with plenty of industry and shipping and little marginal vegetation. The Medina's tributary, the Lukely Brook rises in the Bowcombe Valley and joins the river at the head of the estuary in Newport - the Island's capital. Lukely Brook is also subject to tides and forms the northern boundary of medieval Newport. It cuts through the chalk at Carisbrooke where, to the east of the valley, sits the famous castle. From Newport to the sea at Cowes the river is tidal. Rivers of the Isle of Wight Eastern Yar The Eastern Yar is 27 km long and for agriculture. Bembridge Harbour flows north east from springs at St and the Yar were extensively modified Catherine's Down collecting the in historic times by the construction of Wroxall Stream, Scotchell's Brook and causeways, with land reclamation and a number of small tributaries before drainage above the causeway to St cutting through the central chalk ridge Helen's. The dunes of the Duver are a at Brading. Until the 16th century the marked contrast to the seafront and Eastern Yar flowed into the sea at both harbour, while the embankment of the Sandown and Bembridge. The whole Yar upstream provides an unusual and of this saltmarsh has been reclaimed attractive landscape of wet grazing. Eastern Yar - Longbridge o Yarmouth Mill Western Yar at Freshwater Nature Reserve Thorley Brook Western Yar The Western Yar was once a river with of the river. Afton Marsh reed beds a well developed system of tributaries, dominate the upper reach. but the erosion of the channel coast Creation of the harbour and has destroyed its upper catchment. breakwater in 1843 - seven at Protection works now prevent the sea Yarmouth did much to change the flowing into the Western Yar at shape of the lower reaches of the Freshwater Bay - the source of the estuary, as did the building of a tide- river. The river must once have been mill and sluice gates in 1 793 across one of the largest on the Island but is the Thorley Brook - the Western Yar's now no more than a brook with a main tributary. The bridge and disproportionately large estuary. A harbour dominate the estuary mouth. balanced landscape of fields, saltmarsh and woods all add to the attractiveness o Rivers of the Isle of Wight Water Resources The Environment Agency balances Greensand Groundwater Scheme and carefully demands for water and the the Medina Yar Transfer Scheme which needs of the environment through an takes groundwater from the Lower abstraction licensing system. Greensand and transfers it to the Medina. Water is abstracted from the Island's rivers and groundwater for a range of Water is then transferred from the uses including public water supply, Medina to the Yar to allow abstraction agriculture and industry. Conditions from the Yar at Sandown. may be attached to the licence to In 1988 the Island was chosen as the protect the rights of existing users and ensure that the water environment, largest pilot scheme area for metering water. Since the installation of water such as river flows and wetlands, are not unacceptably affected. meters at more than 51,000 homes, demand has reduced by 20%. The major aquifers on the Island are the Chalk, the Upper Greensand and Water Quality the Lower Greensand. Abstractions for The Environment Agency has a public water supply are from the two largest rivers, the Eastern Yar and responsibility for the water quality of Medina. all controlled inland waters and coastal waters up to a limit of three nautical Demand for public supply is the miles offshore. greatest stress on water resources with Water quality is assessed by taking 86% of all licensed groundwater samples of water and measuring the abstraction for public supply. Nearly 57% of surface water abstraction is also for public supply. In the past the Isle of Wight suffered water supply problems due to its limited surface water sources and high summer population. New sources of supply were developed including the Cross-Solent Main, which involves pumping water from Testwood Reservoir in Hampshire. The Lower Spray irrigation Southern Water - Seaclean Wight concentration of chemical pollutants water service companies have agreed which they contain.
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