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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 ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Isle Of Wight
The Isle of Wight ( ) is a county in the English Channel, off the coast of Hampshire, from which it is separated by the Solent. It is the largest and second-most populous island of 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, and is designated a UNESCO Biosphere Reserve. The island has been home to the poets Algernon Charles Swinburne and Alfred, Lord Tennyson. Queen Victoria built her summer residence and final home, Osborne House at East Cowes, on the Isle. It has a maritime and industrial tradition of boat-building, sail-making, the manufacture of flying boats, hovercraft, and Britain's space rockets. The island hosts annual music festivals, including the Isle of Wight Festival, which in 1970 was the largest rock music ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Back Of The Wight
Back of the 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 through steep gorges. Stretchi ... [...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 "ceole", 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 3 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 6 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 refers ... [...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 the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow 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 ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...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 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 sea-level ... [...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] |
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 and 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 .... The brook initially wound its way to the cliff face and its descent over the edge created Ladder Chi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 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 s ... and Walpen Chine. The brook initially wound its way to the cliff face and its descent over the edge created Ladde ... [...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 coa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
