Eastern Yar

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River Yar
Eastern Yar
River Yar - geograph.org.uk - 120713.jpg
The Eastern Yar at Brading marshes
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
Length20 km (12 mi)
Basin features
Tributaries 
  left Scotchells Brook
River Yar at Alverstone River Yar, Alverstone, IW, UK.jpg
River Yar at Alverstone
Riverside scene in early spring, near Alverstone Eastern Yar River, Isle of Wight, UK.jpg
Riverside scene in early spring, near Alverstone

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.

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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.

<span class="mw-page-title-main">The Solent</span> Strait separating the Isle of Wight from the mainland of England

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+12 and 5 mi, although the Hurst Spit which projects 1+12 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.

<span class="mw-page-title-main">Chalk Group</span> Stratigraphic Unit in England

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.

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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.

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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.

<span class="mw-page-title-main">Geology of the Isle of Wight</span>

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.

References

  1. "River Yar Trail - Source to Sea". WightCam. Archived from the original on 23 April 2009. Retrieved 17 June 2009.

Ordnance Survey One Inch Seventh Series sheet 180

50°41′32″N1°06′39″W / 50.69222°N 1.11083°W / 50.69222; -1.11083