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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.
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.[citation needed] 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. Stretching out from this coast are three ledges of resistant rock, the Brook, Brighstone and Atherfield ledges, on which many ships have been wrecked over the years.
Past Compton and Brighstone, the coast is wild and there are only four access points inland, Whale, Walpen and Ladder Chine and the greatest of them all, Blackgang Chine, which was once a home of smugglers and experienced a massive landslide during the early-20th century, leaving a much larger chine in its place. Blackgang Chine is home to a theme park of the same name, which was the first theme park to be constructed in the United Kingdom.
The most obvious natural features on land are the downs that enclose the area and cut it off from the rest of the island; parts of these are protected as a Site of Special Scientific Interest and large stretches owned by the National Trust. Brighstone Forest, which covers the top of Brighstone Down, is the largest on the island.
At St. Catherine's Point, the Back of the Wight ends and the Undercliff of Ventnor begins.
Like the geology of the Isle of Wight as a whole the geology of the area is varied; at Freshwater the Upper Cretaceous Chalk is exposed resulting in substantial cliffs until Compton, at this point other geological types begin to occur including clays, these formations are unique for the way the layers have been tilted exposing ancient, fossil bearing strata of the Vectis Formation overlaid with the Wessex Formation. These Wealden rocks date from around 120 million years ago, thus younger than similar rocks elsewhere in the UK.
Most of the settlements in the area are villages or hamlets that have evolved around farms or water courses. Settlement in the area has never been great and the villages are mostly old in construction.[citation needed] Many exist because of medieval churches and manors such as Mottistone Manor. The main settlements are:
There is little evidence of the region having been settled in prehistory; apart from the Longstone at Mottistone there are few artefacts. That there were once dinosaurs is proved by the numerous types of bones and fossils that have been excavated from the cliffs, including some species unique to the island. At the time the fossils were laid down, between 125 and 110 million years ago, the island was at a latitude similar to that of North Africa. There is an abundance of fossils on the island, especially of crustaceans and nautiloids such Ammonites.
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Back of the Wight AI simulator
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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.
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.[citation needed] 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. Stretching out from this coast are three ledges of resistant rock, the Brook, Brighstone and Atherfield ledges, on which many ships have been wrecked over the years.
Past Compton and Brighstone, the coast is wild and there are only four access points inland, Whale, Walpen and Ladder Chine and the greatest of them all, Blackgang Chine, which was once a home of smugglers and experienced a massive landslide during the early-20th century, leaving a much larger chine in its place. Blackgang Chine is home to a theme park of the same name, which was the first theme park to be constructed in the United Kingdom.
The most obvious natural features on land are the downs that enclose the area and cut it off from the rest of the island; parts of these are protected as a Site of Special Scientific Interest and large stretches owned by the National Trust. Brighstone Forest, which covers the top of Brighstone Down, is the largest on the island.
At St. Catherine's Point, the Back of the Wight ends and the Undercliff of Ventnor begins.
Like the geology of the Isle of Wight as a whole the geology of the area is varied; at Freshwater the Upper Cretaceous Chalk is exposed resulting in substantial cliffs until Compton, at this point other geological types begin to occur including clays, these formations are unique for the way the layers have been tilted exposing ancient, fossil bearing strata of the Vectis Formation overlaid with the Wessex Formation. These Wealden rocks date from around 120 million years ago, thus younger than similar rocks elsewhere in the UK.
Most of the settlements in the area are villages or hamlets that have evolved around farms or water courses. Settlement in the area has never been great and the villages are mostly old in construction.[citation needed] Many exist because of medieval churches and manors such as Mottistone Manor. The main settlements are:
There is little evidence of the region having been settled in prehistory; apart from the Longstone at Mottistone there are few artefacts. That there were once dinosaurs is proved by the numerous types of bones and fossils that have been excavated from the cliffs, including some species unique to the island. At the time the fossils were laid down, between 125 and 110 million years ago, the island was at a latitude similar to that of North Africa. There is an abundance of fossils on the island, especially of crustaceans and nautiloids such Ammonites.