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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 and 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 Mya. The J ... 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 cl ... [...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 Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era 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. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...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] |
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 and 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 Mya. The J ... 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 cl ... [...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] |
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] |
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] |
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] |
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 stages 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] |
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] |
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 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 Atherfield Bay Holi ... [...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] |
