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Brighton and London - May 1997

Some days off in southern England.

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The West Pier is a pier in Brighton, England. It was built in 1866 by Eugenius Birch and has been closed and deteriorating since 1975, awaiting renovation. It was Brighton's second pier, joining The Royal Suspension Chain Pier of 1823, and it is one of only two Grade I listed piers in the UK, the other being Clevedon Pier. Plans by the charity the West Pier Trust, which now owns the pier, to renovate it with help from the Heritage Lottery Fu [...]
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The West Pier is a pier in Brighton, England. It was built in 1866 by Eugenius Birch and has been closed and deteriorating since 1975, awaiting renovation. It was Brighton's second pier, joining The Royal Suspension Chain Pier of 1823, and it is one of only two Grade I listed piers in the UK, the other being Clevedon Pier. Plans by the charity the West Pier Trust, which now owns the pier, to renovate it with help from the Heritage Lottery Fu [...]
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The Brighton Marine Palace and Pier is a pleasure pier in Brighton, England. It is generally known as the Palace Pier for short, but has been informally renamed Brighton Pier since 2000 by its owners, the Noble Organisation, in an attempt to suggest that it is Brighton's only pier. The West Pier was its rival but was closed in 1975 and was subsequently severely damaged by fires and storms, with the remaining iron structure being partially de [...]
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On the beach, with always changing weather. The seafront has bars, restaurants, nightclubs and amusement arcades, principally between the piers. Being less than an hour from London by train has made the city a popular destination. Brighton beach has a nudist area (south of the easterly part of Kemptown). Brighton's beach, which is a shingle beach up to the mean low tide mark, has been awarded a blue flag. The Monarch's Way long-distance [...]
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The Royal Pavilion is a former royal residence located in Brighton, England. It was built in three campaigns, beginning in 1787, as a seaside retreat for George, Prince of Wales, from 1811 Prince Regent. It is often referred to as the Brighton Pavilion. It is built in the Indo-Saracenic style prevalent in India for most of the 19th century, with the most extravagant chinoiserie interiors ever executed in the British Isles.
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The Royal Pavilion is a former royal residence located in Brighton, England. It was built in three campaigns, beginning in 1787, as a seaside retreat for George, Prince of Wales, from 1811 Prince Regent. It is often referred to as the Brighton Pavilion. It is built in the Indo-Saracenic style prevalent in India for most of the 19th century, with the most extravagant chinoiserie interiors ever executed in the British Isles.
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Outside view of the the typical early 19th century pub with a tiled fireplace, an overkill of dark wood, mirrors, clocks, ship's bells, and barrels enjoying a new lease of life as a table. Rebuilt in 1824 to commemorate the victory at the Battle of Trafalgar, The Victory Inn is named after Captain Hardy’s HMS Victory, the flagship of the British fleet and therefore the vessel on which the Admiral would have sailed.
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Of geological interest and a tourist attraction, the bay is noted for its multi-coloured sand cliffs. Alum Bay is the location of a classic sequence of 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. Due to geological folding of the Alpine orogeny, the strata in the main section of the bay are vertical, with younger rocks to the w [...]
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Alum Bay is the location of a classic sequence of 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. Due to geological folding of the Alpine orogeny, the strata in the main section of the bay are vertical, with younger rocks to the west. The sands are coloured due to oxidised iron compounds formed under different conditions.
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Alum Bay is the location of a classic sequence of 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. Due to geological folding of the Alpine orogeny, the strata in the main section of the bay are vertical, with younger rocks to the west. The sands are coloured due to oxidised iron compounds formed under different conditions.
size on server: 850*567px. Orignal size available on request: 3030*2022px, 2921kB. link photo page.
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Alum Bay is the location of a classic sequence of 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. Due to geological folding of the Alpine orogeny, the strata in the main section of the bay are vertical, with younger rocks to the west. The sands are coloured due to oxidised iron compounds formed under different conditions.
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The Needles is a row of three distinctive stacks of chalk that rise out of the sea off the western extremity of the Isle of Wight, England, close to Alum Bay. The Needles lighthouse stands at the end of the formation. Built in 1859, it has been automated since 1994. The formation takes its name from the former fourth needle-shaped pillar called Lot's Wife that used to stand in its midst until it collapsed in a storm in 1764. The remaining ro [...]
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At the southwestern side of the Circus, moved after World War II from its original position in the centre, stands the Shaftesbury Monument Memorial Fountain, erected in 1892-1893 to commemorate the philanthropic works of Lord Shaftesbury, who was a famous Victorian politician and philanthropist. The monument is topped by Alfred Gilbert's winged nude statue of an archer, sometimes referred to as The Angel of Christian Charity and popularly kn [...]
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The bridge consists of two towers which are tied together at the upper level by means of two horizontal walkways which are designed to withstand the horizontal forces exerted by the suspended sections of the bridge on the landward sides of the towers. The vertical component of the forces in the suspended sections and the vertical reactions of the two walkways are carried by the two robust towers. The bascule pivots and operating machinery are hou [...]
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The founder of Twinings, Thomas Twining, opened the first known tea room, at 216 Strand, London, in 1706, still operating today. The firm's logo, created in 1787, is one of the world's oldest in continuous use. Holder of a Royal Warrant, Twinings has been owned by Associated British Foods since 1964. Twinings sells a variety of regional and flavoured teas such as Lapsang Souchong, Lady Grey and Darjeeling, as well as infusions, coffee, [...]
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Docklands is the semi-official name for an area in northeast and southeast London, England. It forms part of the boroughs of Southwark, Tower Hamlets, Newham and Greenwich. The docks were formerly part of the Port of London, at one time the world's largest port. They have now been redeveloped principally for commercial and residential use. The name London Docklands was used for the first time in a government report on redevelopment plans in [...]
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The Shepherd Gate Clock is the clock mounted on the wall outside the gate of the Royal Greenwich Observatory building in Greenwich, London. The clock, an early example of an electric clock, was a slave mechanism controlled by electric pulses transmitted by a master clock inside the main building. The 'network' of master and slave clocks was constructed and installed by Charles Shepherd in 1852. The clock by the gate was probably the fir [...]
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British astronomers have long used the Royal Observatory as a basis for measurement: four separate meridians have been drawn through the building. The basis of longitude, the Prime Meridian, established in 1851 and adopted at an international conference in 1884, passes through the Airy transit circle of the observatory. It was long marked by a brass strip in the courtyard, now upgraded to stainless steel, and, since 16 December 1999, has been mar [...]
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The Seven Sisters are a series of chalk cliffs by the English Channel. They form part of the South Downs in East Sussex, between the towns of Seaford and Eastbourne in southern England. They are within the Seven Sisters Country Park. They are the remnants of dry valleys in the chalk South Downs, which are gradually being eroded by the sea.
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The Seven Sisters are a series of chalk cliffs by the English Channel. They form part of the South Downs in East Sussex, between the towns of Seaford and Eastbourne in southern England. They are within the Seven Sisters Country Park. They are the remnants of dry valleys in the chalk South Downs, which are gradually being eroded by the sea.
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The River Cuckmere rises near Heathfield in East Sussex, England on the southern slopes of the Weald. The name of the river probably comes from an Old English word meaning fast-flowing, since it descends over 100 m (328 ft) in its initial four miles (6.4 km). Eventually flowing into the English Channel, it is the only undeveloped river mouth on the Sussex coast.
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