1.
London
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London /ˈlʌndən/ is the capital and most populous city of England and the United Kingdom. Standing on the River Thames in the south east of the island of Great Britain and it was founded by the Romans, who named it Londinium. Londons ancient core, the City of London, largely retains its 1. 12-square-mile medieval boundaries. London is a global city in the arts, commerce, education, entertainment, fashion, finance, healthcare, media, professional services, research and development, tourism. It is crowned as the worlds largest financial centre and has the fifth- or sixth-largest metropolitan area GDP in the world, London is a world cultural capital. It is the worlds most-visited city as measured by international arrivals and has the worlds largest city airport system measured by passenger traffic, London is the worlds leading investment destination, hosting more international retailers and ultra high-net-worth individuals than any other city. Londons universities form the largest concentration of education institutes in Europe. In 2012, London became the first city to have hosted the modern Summer Olympic Games three times, London has a diverse range of people and cultures, and more than 300 languages are spoken in the region. Its estimated mid-2015 municipal population was 8,673,713, the largest of any city in the European Union, Londons urban area is the second most populous in the EU, after Paris, with 9,787,426 inhabitants at the 2011 census. The citys metropolitan area is the most populous in the EU with 13,879,757 inhabitants, the city-region therefore has a similar land area and population to that of the New York metropolitan area. London was the worlds most populous city from around 1831 to 1925, Other famous landmarks include Buckingham Palace, the London Eye, Piccadilly Circus, St Pauls Cathedral, Tower Bridge, Trafalgar Square, and The Shard. The London Underground is the oldest underground railway network in the world, the etymology of London is uncertain. It is an ancient name, found in sources from the 2nd century and it is recorded c.121 as Londinium, which points to Romano-British origin, and hand-written Roman tablets recovered in the city originating from AD 65/70-80 include the word Londinio. The earliest attempted explanation, now disregarded, is attributed to Geoffrey of Monmouth in Historia Regum Britanniae and this had it that the name originated from a supposed King Lud, who had allegedly taken over the city and named it Kaerlud. From 1898, it was accepted that the name was of Celtic origin and meant place belonging to a man called *Londinos. The ultimate difficulty lies in reconciling the Latin form Londinium with the modern Welsh Llundain, which should demand a form *lōndinion, from earlier *loundiniom. The possibility cannot be ruled out that the Welsh name was borrowed back in from English at a later date, and thus cannot be used as a basis from which to reconstruct the original name. Until 1889, the name London officially applied only to the City of London, two recent discoveries indicate probable very early settlements near the Thames in the London area
2.
Dam
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A dam is a barrier that impounds water or underground streams. Reservoirs created by not only suppress floods but also provide water for activities such as irrigation, human consumption, industrial use, aquaculture. Hydropower is often used in conjunction with dams to generate electricity, a dam can also be used to collect water or for storage of water which can be evenly distributed between locations. Dams generally serve the purpose of retaining water, while other structures such as floodgates or levees are used to manage or prevent water flow into specific land regions. The word dam can be traced back to Middle English, and before that, from Middle Dutch, the first known appearance of dam occurs in 1165. However, there is one village, Obdam, that is mentioned in 1120. The word seems to be related to the Greek word taphos, so the word should be understood as dike from dug out earth. The names of more than 40 places from the Middle Dutch era such as Amsterdam and Rotterdam, early dam building took place in Mesopotamia and the Middle East. Dams were used to control the level, for Mesopotamias weather affected the Tigris. The earliest known dam is the Jawa Dam in Jordan,100 kilometres northeast of the capital Amman and this gravity dam featured an originally 9-metre-high and 1 m-wide stone wall, supported by a 50 m-wide earth rampart. The structure is dated to 3000 BC, the Ancient Egyptian Sadd-el-Kafara Dam at Wadi Al-Garawi, located about 25 km south of Cairo, was 102 m long at its base and 87 m wide. The structure was built around 2800 or 2600 BC as a dam for flood control. During the Twelfth Dynasty in the 19th century BC, the Pharaohs Senosert III, Amenemhat III, two dams called Ha-Uar running east-west were built to retain water during the annual flood and then release it to surrounding lands. The lake called Mer-wer or Lake Moeris covered 1,700 km2 and is today as Berkat Qaroun. One of the wonders of the ancient world was the Great Dam of Marib in Yemen. Repairs were carried out during various periods, most important around 750 BC and these extensive works were not actually finalized until 325 AD and allowed the irrigation of 25,000 acres. By the mid-late 3rd century BC, an intricate water-management system within Dholavira in modern-day India was built, the system included 16 reservoirs, dams and various channels for collecting water and storing it. Eflatun Pınar is a Hittite dam and spring temple near Konya and it is thought to be from the time of the Hittite empire between the 15th and 13th century BC
3.
Metre
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The metre or meter, is the base unit of length in the International System of Units. The metre is defined as the length of the path travelled by light in a vacuum in 1/299792458 seconds, the metre was originally defined in 1793 as one ten-millionth of the distance from the equator to the North Pole. In 1799, it was redefined in terms of a metre bar. In 1960, the metre was redefined in terms of a number of wavelengths of a certain emission line of krypton-86. In 1983, the current definition was adopted, the imperial inch is defined as 0.0254 metres. One metre is about 3 3⁄8 inches longer than a yard, Metre is the standard spelling of the metric unit for length in nearly all English-speaking nations except the United States and the Philippines, which use meter. Measuring devices are spelled -meter in all variants of English, the suffix -meter has the same Greek origin as the unit of length. This range of uses is found in Latin, French, English. Thus calls for measurement and moderation. In 1668 the English cleric and philosopher John Wilkins proposed in an essay a decimal-based unit of length, as a result of the French Revolution, the French Academy of Sciences charged a commission with determining a single scale for all measures. In 1668, Wilkins proposed using Christopher Wrens suggestion of defining the metre using a pendulum with a length which produced a half-period of one second, christiaan Huygens had observed that length to be 38 Rijnland inches or 39.26 English inches. This is the equivalent of what is now known to be 997 mm, no official action was taken regarding this suggestion. In the 18th century, there were two approaches to the definition of the unit of length. One favoured Wilkins approach, to define the metre in terms of the length of a pendulum which produced a half-period of one second. The other approach was to define the metre as one ten-millionth of the length of a quadrant along the Earths meridian, that is, the distance from the Equator to the North Pole. This means that the quadrant would have defined as exactly 10000000 metres at that time. To establish a universally accepted foundation for the definition of the metre, more measurements of this meridian were needed. This portion of the meridian, assumed to be the length as the Paris meridian, was to serve as the basis for the length of the half meridian connecting the North Pole with the Equator
4.
Floodplain
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In other words, a floodplain is an area near a river or a stream which floods when the water level reaches flood stage. Flood plains are made by a meander eroding sideways as it travels downstream, when a river breaks its banks and floods, it leaves behind layers of alluvium. These gradually build up to create the floor of the flood plain, floodplains generally contain unconsolidated sediments, often extending below the bed of the stream. These are accumulations of sand, gravel, loam, silt, and/or clay, and are often important aquifers, geologically ancient floodplains are often represented in the landscape by fluvial terraces. These are old floodplains that remain relatively high above the present floodplain and it is probable that any section of such an alluvial plain would show deposits of a similar character. The floodplain during its formation is marked by meandering or anastomotic streams, oxbow lakes and bayous, marshes or stagnant pools, and is occasionally completely covered with water. When the drainage system has ceased to act or is diverted for any reason. The floodplain differs, however, because it is not altogether flat and it has a gentle slope downstream, and often, for a distance, from the side towards the center. The floodplain is the place for a river to dissipate its energy. Meanders form over the floodplain to slow down the flow of water, in terms of flood management the upper part of the floodplain is crucial as this is where the flood water control starts. Artificial canalisation of the river here will have a impact on wider flooding. This is the basis of flood management. Floodplains can support particularly rich ecosystems, both in quantity and diversity, tugay forests form an ecosystem associated with floodplains, especially in Central Asia. They are a category of riparian zones or systems, a floodplain can contain 100 or even 1,000 times as many species as a river. Microscopic organisms thrive and larger species enter a rapid breeding cycle, opportunistic feeders move in to take advantage. The production of nutrients peaks and falls away quickly, however the surge of new growth endures for some time and this makes floodplains particularly valuable for agriculture. River flow rates are undergoing change following suit with climate change and this change is a threat to the riparian zones and other flood plain forests. These forests have over time synced their seedling deposits after the peaks in flow to best take advantage of the nutrient rich soil generated by peak flow
5.
Greater London
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London, or Greater London, is a region of England which forms the administrative boundaries of London. It is organised into 33 local government districts, the 32 London boroughs, the Greater London Authority, based in Southwark, is responsible for strategic local government across the region and consists of the Mayor of London and the London Assembly. The county of Greater London was created on 1 April 1965 through the London Government Act 1963, administratively, Greater London was first established as a sui generis council area under the Greater London Council between 1963 and 1986. The area was re-established as a region in 1994, and the Greater London Authority formed in 2000, the region covers 1,572 km2 and had a population of 8,174,000 at the 2011 census. In 2012, it had the highest GVA per capita in the United Kingdom at £37,232, the Greater London Built-up Area—used in some national statistics—is a measure of the continuous urban area of London, and therefore includes areas outside of the administrative region. The term Greater London has been and still is used to different areas in governance, statistics, history. In terms of ceremonial counties, London is divided into the small City of London, outside the limited boundaries of the City, a variety of arrangements has governed the wider area since 1855, culminating in the creation of the Greater London administrative area in 1965. The Greater London Arterial Road Programme was devised between 1913 and 1916, one of the larger early forms was the Greater London Planning Region, devised in 1927, which occupied 1,856 square miles and included 9 million people. The LCC pressed for an alteration in its boundaries soon after the end of the First World War, noting that within the Metropolitan, a Royal Commission on London Government was set up to consider the issue. The LCC proposed a vast new area for Greater London, with a boundary somewhere between the Metropolitan Police District and the home counties, protests were made at the possibility of including Windsor, Slough and Eton in the authority. The Commission made its report in 1923, rejecting the LCCs scheme, two minority reports favoured change beyond the amalgamation of smaller urban districts, including both smaller borough councils and a central authority for strategic functions. The London Traffic Act 1924 was a result of the Commission, Greater London originally had a two-tier system of local government, with the Greater London Council sharing power with the City of London Corporation and the 32 London Borough councils. The GLC was abolished in 1986 by the Local Government Act 1985 and its functions were devolved to the City Corporation and the London Boroughs, with some functions transferred to central government and joint boards. Greater London was used to form the London region of England in 1994, a referendum held in 1998 established a public will to recreate an upper tier of government to cover the region. The Greater London Authority, London Assembly and the directly elected Mayor of London were created in 2000 by the Greater London Authority Act 1999, in 2000, the outer boundary of the Metropolitan Police District was re-aligned to the Greater London boundary. The 2000 and 2004 mayoral elections were won by Ken Livingstone, the 2008 and 2012 elections were won by Boris Johnson. The 2016 election was won by Sadiq Khan, Greater London continues to include the most closely associated parts of the Greater London Urban Area and their historic buffers. Thus it includes, in five boroughs, significant parts of the Metropolitan Green Belt which protects designated greenfield land in a way to the citys parks
6.
Tide
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Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon and the Sun and the rotation of the Earth. Some shorelines experience a semi-diurnal tide—two nearly equal high and low tides each day, other locations experience a diurnal tide—only one high and low tide each day. A mixed tide—two uneven tides a day, or one high, Tides vary on timescales ranging from hours to years due to a number of factors. To make accurate records, tide gauges at fixed stations measure water level over time, gauges ignore variations caused by waves with periods shorter than minutes. These data are compared to the level usually called mean sea level. Tidal phenomena are not limited to the oceans, but can occur in other systems whenever a gravitational field varies in time. For example, the part of the Earth is affected by tides. Tide changes proceed via the following stages, Sea level rises over several hours, covering the intertidal zone, the water rises to its highest level, reaching high tide. Sea level falls over several hours, revealing the intertidal zone, the water stops falling, reaching low tide. Oscillating currents produced by tides are known as tidal streams, the moment that the tidal current ceases is called slack water or slack tide. The tide then reverses direction and is said to be turning, slack water usually occurs near high water and low water. But there are locations where the moments of slack tide differ significantly from those of high, Tides are commonly semi-diurnal, or diurnal. The two high waters on a day are typically not the same height, these are the higher high water. Similarly, the two low waters each day are the low water and the lower low water. The daily inequality is not consistent and is small when the Moon is over the equator. From the highest level to the lowest, Highest Astronomical Tide – The highest tide which can be predicted to occur, note that meteorological conditions may add extra height to the HAT. Mean High Water Springs – The average of the two high tides on the days of spring tides, mean High Water Neaps – The average of the two high tides on the days of neap tides. Mean Sea Level – This is the sea level
7.
North Sea
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The North Sea is a marginal sea of the Atlantic Ocean located between Great Britain, Scandinavia, Germany, the Netherlands, Belgium, and France. An epeiric sea on the European continental shelf, it connects to the ocean through the English Channel in the south and it is more than 970 kilometres long and 580 kilometres wide, with an area of around 570,000 square kilometres. The North Sea has long been the site of important European shipping lanes as well as a major fishery, the North Sea was the centre of the Vikings rise. Subsequently, the Hanseatic League, the Netherlands, and the British each sought to dominate the North Sea and thus the access to the markets, as Germanys only outlet to the ocean, the North Sea continued to be strategically important through both World Wars. The coast of the North Sea presents a diversity of geological and geographical features, in the north, deep fjords and sheer cliffs mark the Norwegian and Scottish coastlines, whereas in the south it consists primarily of sandy beaches and wide mudflats. Due to the population, heavy industrialization, and intense use of the sea and area surrounding it. In the southwest, beyond the Straits of Dover, the North Sea becomes the English Channel connecting to the Atlantic Ocean, in the east, it connects to the Baltic Sea via the Skagerrak and Kattegat, narrow straits that separate Denmark from Norway and Sweden respectively. In the north it is bordered by the Shetland Islands, and connects with the Norwegian Sea, the North Sea is more than 970 kilometres long and 580 kilometres wide, with an area of 570,000 square kilometres and a volume of 54,000 cubic kilometres. Around the edges of the North Sea are sizeable islands and archipelagos, including Shetland, Orkney, the North Sea receives freshwater from a number of European continental watersheds, as well as the British Isles. A large part of the European drainage basin empties into the North Sea including water from the Baltic Sea, the largest and most important rivers flowing into the North Sea are the Elbe and the Rhine – Meuse watershed. Around 185 million people live in the catchment area of the rivers discharging into the North Sea encompassing some highly industrialized areas, for the most part, the sea lies on the European continental shelf with a mean depth of 90 metres. The only exception is the Norwegian trench, which extends parallel to the Norwegian shoreline from Oslo to a north of Bergen. It is between 20 and 30 kilometres wide and has a depth of 725 metres. The Dogger Bank, a vast moraine, or accumulation of unconsolidated glacial debris and this feature has produced the finest fishing location of the North Sea. The Long Forties and the Broad Fourteens are large areas with uniform depth in fathoms. These great banks and others make the North Sea particularly hazardous to navigate, the Devils Hole lies 200 miles east of Dundee, Scotland. The feature is a series of trenches between 20 and 30 kilometres long,1 and 2 kilometres wide and up to 230 metres deep. Other areas which are less deep are Cleaver Bank, Fisher Bank, the International Hydrographic Organization defines the limits of the North Sea as follows, On the Southwest
8.
London Borough of Newham
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It is 5 miles east of the City of London, north of the River Thames. Newham was one of the six host boroughs for the 2012 Summer Olympics, the local authority is Newham London Borough Council. The boroughs motto, from its Coat of Arms, is Progress with the People, the Coat of Arms was derived from that of the County Borough of West Ham, while the motto is a translation of the County Borough of East Hams Latin Progressio cum Populo. Green Street and Boundary Road mark the boundary between the two. North Woolwich also became part of the borough along with an area west of the River Roding which had previously been part of the Municipal Borough of Barking. Newham was devised for the borough as a new name. Unlike most English districts, its council is led by an elected mayor of Newham. From 2002 to 2009 one of the councillors had been appointed as the ambassador and performed the civic. The borough is considered part of Outer London for purposes such as funding and this is because the majority of Newham was not part of the 1889–1965 County of London. The council is actively campaigning to have Newham officially considered part of Inner London in order to increase its level of government grant by £60 million, at the borough elections held in 2014, the Labour Party won all 60 of the seats on the Council. Sir Robin Wales was re-elected as the boroughs Executive Mayor with 61% of the first preference votes cast, Newham has the youngest overall population and one of the lowest White British populations in the country according to the 2011 Census. The borough has the second highest percentage of Muslims in Britain, after the London Borough of Tower Hamlets, at 32%. When using Simpsons Diversity Index on 10 aggregated ethnic groups, the 2001 census identified Newham as the most ethnically diverse district in England and Wales, Newham has the lowest percentage of White British residents of all of Londons boroughs. The joint-lowest wards with White British population are Green Street East and Green Street West, East Ham North is closely followed, at 4. 9%. People of White British ancestry nevertheless remain the largest single group in the borough. The largest non-White British ethnic groups are Indian, African, Bangladeshi, Newham has had for many decades a large Indian community. The ethnic group to increase the most in number since 1991 is the Bangladeshi community, the Borough is the education authority for the district providing education in a mix of Foundation, community and voluntary aided schools. The Essex Primary School in Sheridan Road with over 900 pupils is one of the biggest primary schools in London and this is currently based on the UEL Stratford campus, but is planned to move to its own facilities
9.
Elizabeth II
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Elizabeth II has been Queen of the United Kingdom, Canada, Australia, and New Zealand since 6 February 1952. Elizabeth was born in London as the eldest child of the Duke and Duchess of York, later King George VI and Queen Elizabeth and her father acceded to the throne on the abdication of his brother Edward VIII in 1936, from which time she was the heir presumptive. She began to undertake duties during the Second World War. Elizabeths many historic visits and meetings include a visit to the Republic of Ireland. She has seen major changes, such as devolution in the United Kingdom, Canadian patriation. She has reigned through various wars and conflicts involving many of her realms and she is the worlds oldest reigning monarch as well as Britains longest-lived. In October 2016, she became the longest currently reigning monarch, in 2017 she became the first British monarch to commemorate a Sapphire Jubilee. Elizabeth has occasionally faced republican sentiments and press criticism of the family, however, support for the monarchy remains high. Elizabeth was born at 02,40 on 21 April 1926, during the reign of her paternal grandfather and her father, Prince Albert, Duke of York, was the second son of the King. Her mother, Elizabeth, Duchess of York, was the youngest daughter of Scottish aristocrat Claude Bowes-Lyon, 14th Earl of Strathmore and she was delivered by Caesarean section at her maternal grandfathers London house,17 Bruton Street, Mayfair. Elizabeths only sibling, Princess Margaret, was born in 1930, the two princesses were educated at home under the supervision of their mother and their governess, Marion Crawford, who was casually known as Crawfie. Lessons concentrated on history, language, literature and music, Crawford published a biography of Elizabeth and Margarets childhood years entitled The Little Princesses in 1950, much to the dismay of the royal family. The book describes Elizabeths love of horses and dogs, her orderliness, others echoed such observations, Winston Churchill described Elizabeth when she was two as a character. She has an air of authority and reflectiveness astonishing in an infant and her cousin Margaret Rhodes described her as a jolly little girl, but fundamentally sensible and well-behaved. During her grandfathers reign, Elizabeth was third in the line of succession to the throne, behind her uncle Edward, Prince of Wales, and her father, the Duke of York. Although her birth generated public interest, she was not expected to become queen, many people believed that he would marry and have children of his own. When her grandfather died in 1936 and her uncle succeeded as Edward VIII, she became second-in-line to the throne, later that year, Edward abdicated, after his proposed marriage to divorced socialite Wallis Simpson provoked a constitutional crisis. Consequently, Elizabeths father became king, and she became heir presumptive, if her parents had had a later son, she would have lost her position as first-in-line, as her brother would have been heir apparent and above her in the line of succession
10.
Teddington Lock
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Teddington Lock is a complex of three locks and a weir on the River Thames in England at Ham in south west London. The lock is on the side of the river. The river downstream of the lock, known as the Tideway, is tidal, though Teddington marks the tidal limit, in periods of very high fluvial flow the tidal influence can be seen as far upstream as East Molesey, location of the second lock on the Thames. The Teddington lock complex consists of three locks, a launch lock, a very large barge lock and a small skiff lock. The barge lock has a set of gates in the middle so it can operate in two sizes. The large bow shaped weir stretches across to Teddington from an island upstream of the lock which also acts as the point for the two bridges making up Teddington Lock Footbridge. Stephen Leach took over the post of Clerk of Works for the First District in 1802, just before his retirement, Truss has proposed locks at Molesey and Teddington, each having a weir with long tumbling bays, similar to modern practice. John Rennie had suggested a series of cuts in 1794. Rennie and William Jessop again proposed four long cuts in 1805, each about 1.5 miles long, zacchary Allnutt, by then Surveyor for the Second and Third Districts, stretching from Staines to Mapledurham, suggested locks at Chertsey, Sunbury and Teddington in 1805. Rennie submitted new proposals in 1809, with nine locks between Staines and Twickenham, two would be without weirs, while the other seven would require large weirs to be built in the river. An Act of Parliament was obtained by the City of London Corporation in June 1810, each would be 150 by 20 feet with the associated weir having ample capacity for flood conditions. Rennie, Leach and the Navigation Committee visited the sites in July, Leach then took charge of the work, which was undertaken by contractors Joseph Kimber and John Dows who also built Sunbury Lock. Work at Teddington started in September 1810, but there were delays caused by flooding in November and December, the lock was finished and opened in June 1811, but the weir was incomplete. The lock was further upstream than the present lock complex at the point where the footbridge now crosses and it comprised three pairs of gates as stipulated in the act. Total cost for lock, cut, weir, ballast and ground was £22,035 10s, 7 1⁄2d. of which the land from Lord Dysarts estate cost £282 10s. The lock was, at first, highly unpopular with the fishermen and bargemen. After attempts to smash it, the keeper was granted permission to keep a blunderbuss with bayonet attached thereto to ward off attacks on the lock. By 1827 the timber lock needed considerable repair and in 1829 the weir was destroyed by an accumulation of ice and it is noted that in 1843 the lock-keeper prevented a steam vessel from coming through the lock
11.
North Sea flood of 2007
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Cyclone Tilo was preceded by the extratropical remains of ex-Hurricane Noel on 7 November, which paved the way for the stronger upstream storm Tilo. The jet stream was diverted to the north by a ridge of high pressure to the west of Ireland in the Atlantic Ocean forcing the jet stream over the north of Greenland. In combination with a tide, the tidal level was expected to exceed 3 metres above normal sea levels. The flood and waves were expected to overwhelm sea defences and cause flooding, in particular. However, in the event, the surge was 20 centimetres less than forecast. However, in the Norfolk village of Walcott, storms breached the sea wall, also, the water level came to just 10 cm below the top of the sea wall surrounding Great Yarmouth. Flood warnings were issued for the east coast of Britain and the entire Dutch coast, the Maeslantkering in the port city of Rotterdam was closed for the first time since its construction in 1997. Denmark and Germany issued severe gale warnings for winds gusts up to 125 km/h, oil platforms off the coast of Norway were also closed for the duration of the storm. Felixstowe docks were closed and trains services were suspended between Lowestoft and Norwich due to flooding of the line, in Scotland all schools in Orkney were closed with some closures also in Caithness and Sutherland. Wind gusts as high as 100 miles per hour were reported, the Northlink ferry company cancelled sailings between the Northern Isles. Caledonian MacBrayne also cancelled a dozen routes to the Western Isles,4000 homes lost power in Grampian, there were also reports of trees and roofs being blown down. A rescue tug was called on to stand by a 240-foot cargo ship struggling in the sea off Shetland, the A90 road was closed between Aberdeen and Peterhead after a lorry was blown over. A double-decker bus was blown off the road near Mintlaw in Aberdeenshire, there were also reports of a roof blown off in Fraserburgh. North Norfolk District Council were left seeking to apply for compensation from the governments Bellwin scheme for natural disasters, replacing damaged promenade handrails was estimated to cost £20,000, while council-owned beach chalets were estimated to cost more than £40,000 to mend. Inspections were also undertaken of the steel under Cromer pier, where waves had damaged the floor of the Pavilion Theatre, national Oceanography Centre movie model of surge Parker and Foden High-resolution Measurement of a North Sea Storm Surge. Storm Surge, Seaham, County Durham, YouTube
12.
Thames Diamond Jubilee Pageant
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The Thames Diamond Jubilee Pageant was a parade on 3 June 2012 of 670 boats on the Tideway of the River Thames in London as part of the celebrations of the Diamond Jubilee of Elizabeth II. The Queen, Prince Philip and other members of the Royal Family were aboard vessels that took part in the parade, the parade was organised by the Thames Diamond Jubilee Foundation, and funded by private donations and sponsorship. The pageant master was Adrian Evans, the vessels that took part included military, commercial, and pleasure craft. According to Guinness World Records, this was the largest ever parade of boats, surpassing the record of 327 vessels set in Bremerhaven, Germany. Sailing vessels and others too tall to pass under the bridges were moored as an Avenue of Sail downstream of London Bridge with smaller craft in St Katherine Docks, British media organisations estimated that one million spectators watched from the banks of the Thames. The pageant was broadcast live by the BBC and Sky News, more than 10 million tuned into the BBCs four-and-a-half-hour coverage, with an audience average of 10.3 million. The organisers of the pageant were the Thames Diamond Jubilee Foundation, chaired by Lord Salisbury, with Michael Lockett as the Chief Executive of the Pageant and Pageant Master, Adrian Evans. Other bodies involved in the organisation included the Port of London Authority, the RNLI, the Metropolitan Police, the Maritime and Coastguard Agency, the pageant was planned with inspiration from a painting by the 18th-century Venetian painter, Canaletto. The painting Lord Mayors Day on the Thames depicts a flotilla against a background of London, the painting was loaned for an exhibition at the National Maritime Museum, Greenwich from the Lobkowicz Collections, Prague. The pageant took a route from Wandsworth to Tower Bridge, the Thames was closed to normal navigation. The flotilla proceeded in sections preceded by Music Herald Barges, The Royal Jubilee Bells Man-powered boats Academy of Ancient Music The Royal Squadron, the royal barge was further decorated for the occasion with thousands of flowers and plants, and hung with drapery with the arms of Commonwealth countries. The Queen was attended by Lady Susan Hussey, her lady-in-waiting for more than 50 years, her deputy secretary, Edward Young, her equerry, Lieutenant Colonel Dan Rex. The Queen wore an ensemble designed by royal couturier Angela Kelly, comprising dress, coat, hat, the coat, which had a pleated frill at the front and neck, was of ivory boucle, decorated with gold, silver and ivory paillettes and Swarovski crystals. The matching hat had a cockade of feathers in gold, silver and ivory. Her jewels were the diamond starburst Jardine brooch, a pearl necklace. The Duchess of Cornwall wore an ensemble with sleeves decorated with gold paillettes, by Anna Valentine. Her jewellery was a pearl and diamond choker. She wore a brooch with two dolphins, a gift of the Royal Submarines, the Countess of Wessex wore a printed dress by Emilia Wickstead
