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New Chine
New Chine is a geological feature on the south west coast of the Isle of Wight, England (the Back of the Wight). It is west of the village of Chale. It is a sandy coastal ravine, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks. It leads from the 190 foot high clifftop to a knickpoint approximately one third of way down the cliff face above Chale Bay beach. The Chine is one of three chines that have been eroded by a small unnamed brook that descends from Chale that drains rainwater from the west side of St. Catherine's Hill. The other two chines are Ladder Chine and Walpen Chine. The brook initially wound its way to the cliff face and its descent over the edge created Ladder chine. As the cliff eroded, the brook found a shorter path to the sea and started creating Walpen Chine to the east of Ladder chine. As the cliff eroded further, the brook moved east again and is currently eroding an unnamed chine labelled New Chine. New Chin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Isle Of Wight
The Isle of Wight (Help:IPA/English, /waɪt/ Help:Pronunciation respelling key, ''WYTE'') is an island off the south coast of England which, together with its surrounding uninhabited islets and Skerry, skerries, is also a ceremonial county. The county is bordered by Hampshire across the Solent strait to the north, and is otherwise surrounded by the English Channel. Its largest settlement is Ryde, and the administrative centre is Newport, Isle of Wight, Newport. Wight has a land area of and had a population of 140,794 in 2022, making it the List of islands of England#Largest islands, largest and List of islands of England#Most populous islands, second-most populous English island. The island is largely rural, with the largest settlements primarily on the coast. These include Ryde in the north-east, Shanklin and Sandown in the south-east, and the large villages of Totland and Freshwater, Isle of Wight, Freshwater in the west. Newport is located inland at the point at which the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a Countries of the United Kingdom, country that is part of the United Kingdom. It is located on the island of Great Britain, of which it covers about 62%, and List of islands of England, more than 100 smaller adjacent islands. It shares Anglo-Scottish border, a land border with Scotland to the north and England–Wales border, another land border with Wales to the west, and is otherwise surrounded by the North Sea to the east, the English Channel to the south, the Celtic Sea to the south-west, and the Irish Sea to the west. Continental Europe lies to the south-east, and Ireland to the west. At the 2021 United Kingdom census, 2021 census, the population was 56,490,048. London is both List of urban areas in the United Kingdom, the largest city and the Capital city, capital. The area now called England was first inhabited by modern humans during the Upper Paleolithic. It takes its name from the Angles (tribe), Angles, a Germanic peoples, Germanic tribe who settled du ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Back Of The Wight
Back of the Wight (also known as West Wight) is an area on the Isle of Wight in England. The area has a distinct historical and social background, and is geographically isolated by the chalk hills, immediately to the North, as well as poor public transport infrastructure. Primarily agricultural, the Back of the Wight is made up of small villages spread out along the coast, including Brighstone, Shorwell and Mottistone. Geography The geographical boundaries of the Back of the Wight are imprecise and vary according to interpretation, however roughly speaking it comprises all the land located South of the Downs and East of Freshwater Bay until the curve in the Downs meets the sea near St. Catherine's Point. The main part of the Back of the Wight is formed of a large bay 18 miles long. The shore is edged by cliffs averaging around 300 feet high from Freshwater to Compton, broken at two points, Grange Chine and Brook Chine, which provide the only easy, natural access to the sea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chale
Chale is a village and civil parish on the Isle of Wight of England, in the United Kingdom. It is located three kilometres from Niton in the south of the Island in the area known as the Back of the Wight. The village of Chale lies at the foot of St. Catherine's Down. History Chale is recorded in the Domesday book as "Cela", which probably derives from the Old English word , meaning "throat". This is thought to refer to the nearby ravine or chine at Blackgang. The name was also recorded as "Chele" or "Chielle", but it has been "Chale" since the 12th century. There were three manors in Chale at the time of the Domesday Book: Chale, Gotten and Walpen. The Parish Church of St Andrew was founded by Hugh Gendon in Chale in 1114. However, the present church dates from the 14th century. It has six bells in its tower. One might have been made about 1360. It has some fine stained glass windows. The Chale Abbey farm has a window that dates from the 14th century. The name Abbey refe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chine
A chine () is a steep-sided coastal gorge where a river flows to the sea through, typically, soft eroding cliffs of sandstone or clays. The word is still in use in central Southern England—notably in East Devon, Dorset, Hampshire and the Isle of Wight—to describe such topographical features. The term 'bunny' is sometimes used to describe a chine in Hampshire. The term chine is also used in some Vancouver suburbs in Canada to describe similar features. Formation and features Chines appear at the outlet of small river valleys when a particular combination of geology, stream volume, and coastal recession rate creates a knickpoint, usually starting at a waterfall at the cliff edge, that initiates rapid erosion and deepening of the stream bed into a gully leading down to the sea. All chines are in a state of constant change due to erosion. The Blackgang Chine on the Isle of Wight, for example, has been destroyed by landslides and coastal erosion during the 20th century. As t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Knickpoint
In geomorphology, a knickpoint or nickpoint is part of a river or channel where there is a sharp change in channel bed slope, such as a waterfall or lake. Knickpoints reflect different conditions and processes on the river, often caused by previous erosion due to glaciation or variance in lithology. In the cycle of erosion model, knickpoints advance one cycle upstream, or inland, replacing an older cycle. A knickpoint that occurs at the head (furthest upstream extent) of a channel is called a headcut. Headcuts resulting in headward erosion are hallmarks of unstable expanding drainage features such as actively eroding gullies. Knickpoints also occur on other planetary bodies that previously had or currently have surface liquids, namely Mars and Titan. On Mars, the knickpoints have a common elevation that suggest a common sea level for a former Martian ocean. On Titan, mountain valleys adjacent to the present-day hydrocarbon seas show evidence of knickpoints and recent se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chale Bay
Chale Bay is a bay on the south-west coast of the Isle of Wight, England. It lies to the west of the village of Chale from which it takes its name. It faces south-west towards the English Channel, its shoreline is in length and is gently curving. It stretches from Artherfield Point in the north-west to Rocken End in the south-east. The bay is best viewed from the car park on the A3055 above Blackgang Chine or anywhere along the Isle of Wight Coastal Path which follows the whole coastline along the clifftop. Since the closure of the steps at Whale Chine, the beach at Chale Bay has become somewhat inaccessible, with no way down from the clifftop anywhere along its three miles. Parts of the beach are sometimes used by naturists, who are known locally as "Blackgang Bares". Geography The beach is predominantly shingle and is bordered by tall cliffs which are made of sandstone, chalk and clay and so are often subject to erosion. There are a number of coastal chines and ravines ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ladder Chine
Ladder Chine is a geological feature on the south west coast of the Isle of Wight, England ( the Back of the Wight). It is west of the village of Chale. It is a sandy coastal ravine, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks. It leads from the 190 foot high clifftop to a knickpoint approximately halfway down the cliff face above Chale Bay beach. The Chine is the first and largest of three chines that have been eroded by a small unnamed brook that descends from Chale that drains rainwater from the west side of St. Catherine's Hill. The other two chines are Walpen Chine and New Chine. The brook initially wound its way to the cliff face and its descent over the edge created Ladder chine. As the cliff eroded, the brook found a shorter path to the sea, creating the two other chines to the east of Ladder chine. Ladder Chine is now dry. The Isle of Wight Coastal Path runs along the cliff top above this chine. Many Southern Vec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Walpen Chine
Walpen Chine is a geological feature on the south west coast of the Isle of Wight, England. It is west of the village of Chale. It is a sandy coastal ravine, one of a number of such chines on the island created by stream erosion of soft Cretaceous rocks. It leads from the 190 feet high clifftop next to the Isle of Wight coastal path to a knickpoint approximately halfway down the cliff face above Chale Bay beach. The chine is one of three that have been eroded by a small unnamed brook that descends from Chale that drains rainwater from the west side of St. Catherine's Hill. The other two chines are Ladder Chine Ladder Chine is a geological feature on the south west coast of the Isle of Wight, England ( the Back of the Wight). It is west of the village of Chale. It is a sandy coastal ravine, one of a number of such chines on the island created by stre ... and New Chine. The brook initially wound its way to the cliff face and its descent over the edge created Ladder Ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Isle Of Wight Coastal Path
The Isle of Wight Coastal Path (or Coastal Footpath) is a circular long-distance footpath of 70 miles (113 km) around the Isle of Wight, UK. It follows public footpaths and minor lanes, with some sections along roads. Route The path is waymarked in both directions and can be started at any point, but is described here clockwise from the pier at Ryde (). Ryde to Sandown Ryde to Bembridge (7.5 miles) From the bus station by Ryde Pier, the path follows the Esplanade close to the beach. It passes Appley Tower and Puckpool Point before rejoining the coast road to Seaview. It then climbs inland on footpaths, skirting Priory Woods, before returning to sea level at The Duver near St Helen's Old Church. Then the path crosses the edge of Bembridge Harbour on the old mill wall, using Embankment Road to pass the houseboats in the harbour. The path then continues into Bembridge and to the Lifeboat Station. Bembridge to Sandown (5.5 miles) The path follows the coast ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
