1686 In England
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1686 In England
Events from the year 1686 in England. Incumbents * Monarch – James II * Parliament – Loyal Events * 21 June – judgement in the case of ''Godden v. Hales'' affirms the king's power to exercise his dispensing powers granting exemptions from anti-Catholic legislation. Heneage Finch is dismissed as Solicitor General for his refusal to defend the king's case. * 10 July – Court of Ecclesiastical Commission created. * 17 July – King James appoints four Catholics to the Privy Council of England. * 5 November – Bar Convent in York established, making it the oldest surviving active Catholic convent in England. Undated * A group of conspirators meet at Charborough House in Dorset to plan the overthrow of James II by Parliamentarians and the Dutch Stadtholder William III of Orange-Nassau (James's son-in-law). Publications * Edmond Halley presents a systematic study of the trade winds and monsoons and identifies solar heating as the cause of atmospheric motions. * John Pl ...
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1686
Events January–March * January 3 – In Madras (now Chennai) in India, local residents employed by the East India Company threaten to boycott their jobs after corporate administrator William Gyfford imposes a house tax on residences within the city walls. Gyfford places security forces at all entrances to the city and threatens to banish anyone who fails to pay their taxes, as well as to confiscate the goods of merchants who refuse to make sales. A compromise is reached the next day on the amount of the taxes. * January 17 – King Louis XIV of France reports the success of the Edict of Fontainebleau, issued on October 22 against the Protestant Huguenots, and reports that after less than three months, the vast majority of the Huguenot population had left the country. * January 29 – In Guatemala, Spanish Army Captain Melchor Rodríguez Mazariegos leads a campaign to conquer the indigenous Maya people in the rain forests of Lacandona, departing fr ...
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Netherlands
) , anthem = ( en, "William of Nassau") , image_map = , map_caption = , subdivision_type = Sovereign state , subdivision_name = Kingdom of the Netherlands , established_title = Before independence , established_date = Spanish Netherlands , established_title2 = Act of Abjuration , established_date2 = 26 July 1581 , established_title3 = Peace of Münster , established_date3 = 30 January 1648 , established_title4 = Kingdom established , established_date4 = 16 March 1815 , established_title5 = Liberation Day (Netherlands), Liberation Day , established_date5 = 5 May 1945 , established_title6 = Charter for the Kingdom of the Netherlands, Kingdom Charter , established_date6 = 15 December 1954 , established_title7 = Dissolution of the Netherlands Antilles, Caribbean reorganisation , established_date7 = 10 October 2010 , official_languages = Dutch language, Dutch , languages_type = Regional languages , languages_sub = yes , languages = , languages2_type = Reco ...
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Christopher Packe (physician And Cartographer)
Christopher Packe (1686–1749) was an English physician and geologist. His 1743 work ''A New Philosophico-chorographical Chart of East Kent'' was the first geological map of Southern England. Life Packe was born at St. Albans, Hertfordshire, on 6 March 1686. He was probably the son of Christopher Packe the chemist. Packe was admitted to Merchant Taylors' School on 11 September 1695. He was created M.D. at Cambridge in 1717, and was admitted a candidate of the College of Physicians on 25 June 1723. At the request of Robert Romney, the then vicar, he gave an organ to the Church of St Peter, St. Albans, the organ being inaugurated on 16 January 1726. About 1726 Packe settled at Canterbury. He practiced as a physician, with a good reputation, for nearly a quarter of a century. He died on 15 November 1749, and was buried in St. Mary Magdalene, Canterbury. Bibliography Packe had a heated controversy with Dr. John Gray of Canterbury respecting the treatment of Robert Worger of Hinxhi ...
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Robert Plot
Robert Plot (13 December 1640 – 30 April 1696) was an English naturalist, first Professor of Chemistry at the University of Oxford, and the first keeper of the Ashmolean Museum. Early life and education Born in Borden, Kent to parents Robert Plot and Elisabeth Patenden, and baptised on 13 December 1640, Plot was educated at the Wye Free School in Kent. He entered Magdalen Hall, Oxford in 1658 where he graduated with a BA in 1661 and an MA in 1664. Plot subsequently taught and served as dean and vice principal at Magdalen Hall while preparing for his BCL and DCL, which he received in 1671 before moving to University College in 1676.A. J. Turner, 'Plot, Robert (bap. 1640, d. 1696)', Oxford Dictionary of National Biography, Oxford University Press, 200accessed 4 June 2013/ref>Plot, Robert." Complete Dictionary of Scientific Biography. Vol. 11. Detroit: Charles Scribner's Sons, 2008. 40–41. Gale Virtual Reference Library. Web. 4 June 2013. Natural history and chemistry By ...
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Thomas Wharton, 1st Marquess Of Wharton
Thomas Wharton, 1st Marquess of Wharton PC (August 1648 – 12 April 1715) was an English nobleman and politician. A man of great charm and political ability, he was also notorious for his debauched lifestyle. Background He was the son of Philip Wharton, 4th Baron Wharton, and his second wife, Jane Goodwin, only daughter of Colonel Arthur Goodwin of Upper Winchendon, Buckinghamshire, and heiress to the extensive Goodwin estates in Buckinghamshire, including Winchendon, Wooburn, Waddeston, Weston, and other properties. Career In his long political career, he was a Member of Parliament for seventeen years and spearheaded the Whig opposition to King James II's government, which later developed the two-party political system under Queen Anne. Before the Glorious Revolution he was in close contact with a group of army officers conspiring against King James, including his brother Captain Henry Wharton. In 1689 he was sworn of the Privy Council and made Comptroller of the Ho ...
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Lillibullero
"Lillibullero" (also spelled Lillibulero, Lilliburlero, or Lilli Burlero) is a march attributed to Henry Purcell that became popular in England at the time of the Glorious Revolution of 1688. Background Henry Purcell is alleged to have composed the melody of "Lillibulero" for a march in 1686, but this is still disputed: LILLBURLERO. A 17th-century party tune ... It has been attributed to Henry Purcell, but whether Purcell composed the melody or only fitted the bass is a question not finally settled. The melody is found in the second half of Purcell's piece, the quickstep. There is no extant manuscript of this 1686 march. It was first published that year in ''The Delightful Companion'', John Playford's method book for recorder. Writing over 200 years later, William Chappell surmised that Purcell's tune deserves nine-tenths of the credit for the popularity of the song.Chappell, William.Purcell, Grove's Dictionary of Music and Musicians, Volume 2. 1900. Also in 1686 ...
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Henry Purcell
Henry Purcell (, rare: September 1659 – 21 November 1695) was an English composer. Purcell's style of Baroque music was uniquely English, although it incorporated Italian and French elements. Generally considered among the greatest English opera composers, Purcell is often linked with John Dunstaple and William Byrd as England's most important early music composers. No later native-born English composer approached his fame until Edward Elgar, Ralph Vaughan Williams, Gustav Holst, William Walton and Benjamin Britten in the 20th century. Life and work Early life Purcell was born in St Ann's Lane, Old Pye Street, Westminster – the area of London later known as Devil's Acre, a notorious slum – in 1659. Henry Purcell Senior, whose older brother Thomas Purcell was a musician, was a gentleman of the Chapel Royal and sang at the coronation of King Charles II of England. Henry the elder had three sons: Edward, Henry and Daniel. Daniel Purcell, the youngest of the b ...
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John Playford
John Playford (1623–1686/7) was a London bookseller, publisher, minor composer, and member of the Stationers' Company, who published books on music theory, instruction books for several instruments, and psalters with tunes for singing in churches. He is perhaps best known today for his publication of ''The English Dancing Master'' in 1651. Biography Playford was born in Norwich, the younger son of John Playford. He served an apprenticeship in London with publisher John Benson from 1639/40 to 1647, after which he remained in the capital, opening a shop in the porch of Temple Church. Playford was clerk to the church, and probably resided with his wife Hannah over the shop until 1659. He was, it appears (from the title-pages of his publications) temporarily in partnership with John Benson in 1652, and with Zachariah Watkins in 1664 and 1665. Under the Commonwealth (1649–60), and for some years of Charles II's reign, Playford almost monopolised the business of music pu ...
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Philosophical Transactions Of The Royal Society
''Philosophical Transactions of the Royal Society'' is a scientific journal published by the Royal Society. In its earliest days, it was a private venture of the Royal Society's secretary. It was established in 1665, making it the first journal in the world exclusively devoted to science, and therefore also the world's longest-running scientific journal. It became an official society publication in 1752. The use of the word ''philosophical'' in the title refers to natural philosophy, which was the equivalent of what would now be generally called ''science''. Current publication In 1887 the journal expanded and divided into two separate publications, one serving the physical sciences ('' Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences'') and the other focusing on the life sciences ('' Philosophical Transactions of the Royal Society B: Biological Sciences''). Both journals now publish themed issues and issues resulting from pap ...
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Earth's Atmosphere
The atmosphere of Earth is the layer of gases, known collectively as air, retained by Earth's gravity that surrounds the planet and forms its planetary atmosphere. The atmosphere of Earth protects life on Earth by creating pressure allowing for liquid water to exist on the Earth's surface, absorbing ultraviolet solar radiation, warming the surface through heat retention (greenhouse effect), and reducing temperature extremes between day and night (the diurnal temperature variation). By mole fraction (i.e., by number of molecules), dry air contains 78.08% nitrogen, 20.95% oxygen, 0.93% argon, 0.04% carbon dioxide, and small amounts of other gases. Air also contains a variable amount of water vapor, on average around 1% at sea level, and 0.4% over the entire atmosphere. Air composition, temperature, and atmospheric pressure vary with altitude. Within the atmosphere, air suitable for use in photosynthesis by terrestrial plants and breathing of terrestrial animals is found only in ...
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Monsoon
A monsoon () is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator. Usually, the term monsoon is used to refer to the rainy phase of a seasonally changing pattern, although technically there is also a dry phase. The term is also sometimes used to describe locally heavy but short-term rains. The major monsoon systems of the world consist of the West African, Asia–Australian, the North American, and South American monsoons. The term was first used in English in British India and neighboring countries to refer to the big seasonal winds blowing from the Bay of Bengal and Arabian Sea in the southwest bringing heavy rainfall to the area. Etymology The etymology of the word monsoon is not wholl ...
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Trade Wind
The trade winds or easterlies are the permanent east-to-west prevailing winds that flow in the Earth's equatorial region. The trade winds blow mainly from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemisphere, strengthening during the winter and when the Arctic oscillation is in its warm phase. Trade winds have been used by captains of sailing ships to cross the world's oceans for centuries. They enabled colonial expansion into the Americas, and trade routes to become established across the Atlantic Ocean and the Pacific Ocean. In meteorology, they act as the steering flow for tropical storms that form over the Atlantic, Pacific, and southern Indian oceans and make landfall in North America, Southeast Asia, and Madagascar and East Africa. Shallow cumulus clouds are seen within trade wind regimes and are capped from becoming taller by a trade wind inversion, which is caused by descending air aloft from within the subtropical ridge. The weak ...
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