Search results
Results From The WOW.Com Content Network
Ryde School with Upper Chine (referred to as “Ryde School”) is a co-educational independent day and boarding school in Ryde, on the Isle of Wight. The school, founded in 1921, is a member of the HMC (Headmasters’ and Mistresses’ Conference).
File:Ryde Pier, Isle of Wight.jpg. Add languages. Page contents not supported in other languages. ... Co-sited: Date and time of digitizing: 16:43, 5 March 2017:
Ryde Pier is an early 19th century pier serving the town of Ryde, on the Isle of Wight, off the south coast of England.It is the world's oldest seaside pleasure pier. [1] [2] Ryde Pier Head railway station is at the sea end of the pier, and Ryde Esplanade railway station at the land end, both served by Island Line trains.
Ryde is an English seaside town and civil parish on the north-east coast of the Isle of Wight. The built-up area had a population of 24,096 according to the 2021 Census . [ 1 ] Its growth as a seaside resort came after the villages of Upper Ryde and Lower Ryde were merged in the 19th century, as can still be seen in the town's central and ...
Ryde Esplanade railway station serves the town of Ryde on the Isle of Wight, and forms part of the Ryde Transport Interchange. Located on the sea front, it is the most convenient station for the majority of the town. Ryde Esplanade is also the location of the principal ticket office and all lost property facilities for the Island Line.
Gregory Avenue, Pondwell. Pondwell is an area between Nettlestone and Ryde on the Isle of Wight, off the southern coast of England.According to the Post Office the population for the area at the 2011 Census was included in the civil parish of Nettlestone and Seaview.
Haylands is an area just to the south of Ryde on the Isle of Wight, off the south coast of England. At the time of the 2011 Census the population etc. of Haylands is listed under Ryde. Located to the east, it is a short walk away from housing estates at Pell and Binstead. [1]
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.