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The following is a list of tourist attractions on the Isle of Wight This is a dynamic list and may never be able to satisfy particular standards for completeness. You can help by adding missing items with reliable sources .
Pages in category "Tourist attractions on the Isle of Wight" The following 32 pages are in this category, out of 32 total. This list may not reflect recent changes .
Detailed map of the Isle of Wight. The Isle of Wight is situated between the Solent and the English Channel, is roughly rhomboid in shape, and covers an area of 150 sq mi (380 km 2). Slightly more than half, mainly in the west, is designated as the Isle of Wight Area of Outstanding Natural Beauty.
Sandown Bay is a broad open bay which stretches for much of the length of the Isle of Wight's southeastern coast. It extends 8 + 1 ⁄ 2 miles (13.7 km) from Culver Down, near Yaverland in the northeast of the Island, to just south of Shanklin, near the village of Luccombe in the southwest. [1]
Isle of Wight 50°40′12″N 1°05′49″W / 50.67000°N 1.09694°W / 50.67000; -1 Whitecliff Bay is a sandy bay near Foreland which is the easternmost point of the Isle of Wight , England, about two miles south-west of Bembridge and just to the north of Culver Down .
Monks Bay is situated on the southern coast of the Isle of Wight, England just to the east of the village of Bonchurch, it is around 1 ⁄ 3 mile (0.54 km) in length. [1] It is popular with visitors and is one of the natural highlights of the town, which has hosted such figures as Charles Dickens.
North Carolina portal Wikimedia Commons has media related to Visitor attractions in North Carolina . Note: Articles and subcategories in this category should also be included in at least one of this state's other categories.
The cliffs of Alum Bay, showing the steeply-dipping multi-coloured sands above the white Chalk, with shallower dips towards the northern end. Alum Bay is the location of a classic sequence of upper Paleocene and Eocene beds of soft sands and clays, separated by an unconformity from the underlying Cretaceous Chalk Formation that forms the adjoining headland of West High Down.
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