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Whale Chine
Whale Chine is a geological feature near Chale on the south-west coast of the Isle of Wight, England (the Back of the Wight). One of a number of such chines on the island created by stream erosion of soft Cretaceous rocks, it is a narrow and steep coastal ravine dropping 140 feet through Lower Greensand rocks from clifftop farmland to Chale Bay. Its name probably originates from the Wavell family, owners of the nearby Atherfield Farm between 1557 and 1636. It is reached from a car park on the A3055 coastal road, where a stream running parallel to the cliff takes a right-angled bend to descend to the beach. In the past, descent to the beach at Whale Chine could be achieved by some 126 wooden steps, since their closure in 2005, these steps were washed away by the sea in the winter storms of 2013/14. As the beach is a popular fishing site, Local fisherman have constructed a new flight of stairs by carving steps down through the rock, although this is not recommended. Despite the o ... [...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] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...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] |
Whale Chine
Whale Chine is a geological feature near Chale on the south-west coast of the Isle of Wight, England (the Back of the Wight). One of a number of such chines on the island created by stream erosion of soft Cretaceous rocks, it is a narrow and steep coastal ravine dropping 140 feet through Lower Greensand rocks from clifftop farmland to Chale Bay. Its name probably originates from the Wavell family, owners of the nearby Atherfield Farm between 1557 and 1636. It is reached from a car park on the A3055 coastal road, where a stream running parallel to the cliff takes a right-angled bend to descend to the beach. In the past, descent to the beach at Whale Chine could be achieved by some 126 wooden steps, since their closure in 2005, these steps were washed away by the sea in the winter storms of 2013/14. As the beach is a popular fishing site, Local fisherman have constructed a new flight of stairs by carving steps down through the rock, although this is not recommended. Despite the o ... [...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] |
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] |
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] |
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] |
Lower Greensand
The Lower Greensand Group is a geological unit present across large areas of Southern England. It was deposited during the Aptian and Albian ages of the Early Cretaceous. It predominantly consists of sandstone and unconsolidated sand that were deposited in shallow marine conditions. Lithology The Lower Greensand typically comprises loose, unconsolidated sandstone (termed rubblestone/rubble in construction) and sands of varying grain size with subordinate amounts of siltstones, mudstones (containing smectites and similar) and limestones. The name "greensand" is derived from the presence of the green coloured mineral glauconite, which forms in shallow marine conditions. In the Weald of East Sussex the lowermost part of the group is recognised by green glauconitic clays with a basal bed of phosphate nodules. These clays are overlain by green sandy clays and silts and finally homogeneous fine grained sands.Lake, R.D. & Shepard-Thorn, E.R. (1987) ''Geology of the country around Ha ... [...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] |
Pyrite
The mineral pyrite ( ), or iron pyrite, also known as fool's gold, is an iron sulfide with the chemical formula Fe S2 (iron (II) disulfide). Pyrite is the most abundant sulfide mineral. Pyrite's metallic luster and pale brass-yellow hue give it a superficial resemblance to gold, hence the well-known nickname of ''fool's gold''. The color has also led to the nicknames ''brass'', ''brazzle'', and ''brazil'', primarily used to refer to pyrite found in coal. The name ''pyrite'' is derived from the Greek (), 'stone or mineral which strikes fire', in turn from (), 'fire'. In ancient Roman times, this name was applied to several types of stone that would create sparks when struck against steel; Pliny the Elder described one of them as being brassy, almost certainly a reference to what is now called pyrite. By Georgius Agricola's time, , the term had become a generic term for all of the sulfide minerals. Pyrite is usually found associated with other sulfides or oxides in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shepherd's Chine
Shepherd's Chine is a geological feature on the south west coast of the Isle of Wight, England. It lies to the west of the village of Little Atherfield. This chine is one of the largest on the Isle of Wight. It starts at the side of the A3055 road#Military Road, A3055 Military Road and runs west for about 500m to reach the beach at Brighstone Bay just to the north of Atherfield Point. This chine has much shallower sides than other chines on the Isle of Wight and is extensively covered with hardy bushes, scrub and rough grasses. The Chine drains water from the mainly flat agricultural land surrounding Little Atherfield. The resulting stream used to be collected behind a small dam and then pumped back onto the surrounding farm land. The remains of the reservoir and pump house, complete with pump, still stand about halfway along the chine. Similarly to Grange/Marsh Chine once the stream reaches the pebble beach it soaks in and disappears. To the west of Shepherd's Chine is the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
