River Yar Eastern Yar | |
---|---|
Location | |
Country | England |
Region | Isle of Wight |
Physical characteristics | |
Source | |
• location | Niton, Isle of Wight |
Mouth | The Solent |
• location | Bembridge Harbour, Isle of Wight |
Length | 20 km (12 mi) |
Basin features | |
Tributaries | |
• left | Scotchells Brook |
The River Yar on the Isle of Wight, England, rises in a chalk coomb in St. Catherine's Down near Niton, [1] close to the southern tip of the island. It flows across the Lower Cretaceous rocks of the eastern side of the island, through the gap in the central Upper Cretaceous chalk ridge of the Island at Yarbridge, then across the now drained Brading Haven to Bembridge Harbour in the northeast.
For most of its course, the river passes through rural areas. At Alverstone, a small weir uses water from the river to power a water mill.
The Yar is one of two rivers on the Isle of Wight with the same name. It is referred to as the Eastern Yar if it is necessary to distinguish between them with the other river being known as the Western Yar.
The Isle of Wight is an island, English county and unitary authority in the English Channel, 2 to 5 miles off the coast of Hampshire, across the Solent. It is the largest and second-most populous island in England. Referred to as "The Island" by residents, the Isle of Wight has resorts that have been popular holiday destinations since Victorian times. It is known for its mild climate, coastal scenery, and verdant landscape of fields, downland, and chines. The island is historically part of Hampshire. The island is designated a UNESCO Biosphere Reserve. With a land area of 380 km2 (150 sq mi), it is about half the size of Singapore.
The Solent is a strait between the Isle of Wight and mainland Great Britain; the major historic ports of Southampton and Portsmouth lie inland of its shores. It is about 20 miles long and varies in width between 2+1⁄2 and 5 mi, although the Hurst Spit which projects 1+1⁄2 mi (2.4 km) into the Solent narrows the sea crossing between Hurst Castle and Colwell Bay to just over 1 mi (1.6 km).
The Isle of Wight National Landscape is an Area of Outstanding Natural Beauty (AONB) on the Isle of Wight, England's largest offshore island.
The Chalk Group is the lithostratigraphic unit which contains the Upper Cretaceous limestone succession in southern and eastern England. The same or similar rock sequences occur across the wider northwest European chalk 'province'. It is characterised by thick deposits of chalk, a soft porous white limestone, deposited in a marine environment.
The River Yar on the Isle of Wight, England, rises near the beach at Freshwater Bay, on the south coast, and flows only a few miles north to Yarmouth where it meets the Solent. Most of the river is a tidal estuary. Its headwaters have been truncated by erosion of the south coast.
St Helens is a village and civil parish located on the eastern side of the Isle of Wight.
Devil's Dyke is a 100 metre (300') deep V-shaped dry valley on the South Downs in Sussex in southern England, 5 miles (8.0 km) north-west of Brighton. It is managed by the National Trust, and is also part of the Beeding Hill to Newtimber Hill Site of Special Scientific Interest. Devil's Dyke was a major local tourist attraction in the late 19th and early 20th centuries. It is now a popular viewpoint and site for walking, model aircraft flying and hang gliding. The South Downs Way passes the site.
Whitwell is a small village and former civil parish, now in the parish of Niton and Whitwell, on the south of the Isle of Wight, England, approximately 5 kilometres north-west of Ventnor, the village's nearest town. In addition to this, it is about five minutes away from its neighbouring small villages of Godshill and Niton. According to 2001 census data, the total population of the village was 578. There is a variety of stone and thatched housing, as well as some more modern housing, the most recent of which was completed in 2006.
Foreland or Forelands, and the adjacent Foreland Fields, is the easternmost point of the Isle of Wight, part of the village of Bembridge. It is located about 6.5 miles due south of the city of Portsmouth on the British mainland, separated by the eastern reaches of the Solent. It is characterised by a pub called the Crab and Lobster Inn and various beach huts plus a beach cafe and a coast guard lookout. In the sea are the reefs of Bembridge Ledge which is rich in edible crabs, lobsters and spider crabs and shoals of mackerel. In the Crab & Lobster Inn are photographs of the many shipwrecks, which included the submarine HMS Alliance, now a museum ship at Gosport and the First World War troopship the S.S. Mehndi carrying troops from South Africa, with great loss of life.
Compton Bay is a bay located on the southwest section of the Isle of Wight, England. Its northwestern edge is defined by the distinctive white chalk cliff of Freshwater Cliff, named after adjacent Freshwater Bay, which forms a small cove with the village of Freshwater situated just behind. Its northeastern edge is formed from the soft red and orange lower cretaceous rocks of Brook Bay, which are rapidly eroding.
Yarbridge is a hamlet on the Isle of Wight, England. It is at the southern tip of the parish of Brading.
Shide is a small settlement on the Isle of Wight, some of which is considered to be in the Newport conurbation.
Tennyson Down is a hill at the west end of the Isle of Wight just south of Totland. Tennyson Down is a grassy, whale-backed ridge of chalk which rises to 482 ft/147m above sea level. Tennyson Down is named after the poet Lord Tennyson who lived at nearby Farringford House for nearly 40 years. The poet used to walk on the down almost every day, saying that the air was worth 'sixpence a pint'.
Shide railway station was at Shide, on the southern fringes of Newport, Isle of Wight, off the south coast of England. It was an intermediate station on the line from Newport to Sandown, which was initially operated by the Isle of Wight Railway.
Calbourne and Shalfleet railway station, was an intermediate station of the Freshwater, Yarmouth and Newport Railway, incorporated in 1860, opened over a ten-month period between 1888 and 1889 and closed 65 years later. Situated between the two villages and serving a moderately populous rural area it was a "reasonably" successful station on an ultimately unprofitable line. Originally the station had a cottage style front but after absorption by the Southern a corrugated building from the acrimonious-split era was relocated to the site. The station itself, situated on the down side, has long been demolished and replaced with a modern bungalow; but the level-crossing keeper's cottage, a short distance away at Pounds Lane, is still visitable.
On the Isle of Wight, Morton is the area of Brading where Morton Marshes and the River Yar form a boundary to the extension of housing estates from Sandown.
The Hampshire Basin is a geological basin of Palaeogene age in southern England, underlying parts of Hampshire, the Isle of Wight, Dorset, and Sussex. Like the London Basin to the northeast, it is filled with sands and clays of Paleocene and younger ages and it is surrounded by a broken rim of chalk hills of Cretaceous age.
Brading Marshes to St. Helen's Ledges is a 488.5-hectare (1,207-acre) Site of special scientific interest which stretches from Brading along the Yar valley between Bembridge and St Helens, Isle of Wight through to the sea at Priory Bay on the north east coast of the Isle of Wight. It encompasses the Brading Marshes RSPB reserve, Bembridge harbour and the inter tidal sand, mud flats and rocky ledges exposed off the coast at low water, including the land around St Helens Fort which is not attached to the mainland. It is the second largest SSSI on the Isle of Wight. The site was notified in 1951 for both its biological and geological features.
Dorset is a county located in the middle of the south coast of England. It lies between the latitudes 50.512°N and 51.081°N and the longitudes 1.682°W and 2.958°W, and occupies an area of 2,653 km2. It spans 90 kilometres (56 mi) from east to west and 63 kilometres (39 mi) from north to south.
The geology of the Isle of Wight is dominated by sedimentary rocks of Cretaceous and Paleogene age. This sequence was affected by the late stages of the Alpine Orogeny, forming the Isle of Wight monocline, the cause of the steeply-dipping outcrops of the Chalk Group and overlying Paleogene strata seen at The Needles, Alum Bay and Whitecliff Bay.
Ordnance Survey One Inch Seventh Series sheet 180
50°41′32″N1°06′39″W / 50.69222°N 1.11083°W