Prime meridian - wikipedia Prime meridian A line of longitude, at which longitude is defined to be 0 ° `` Prime Meridian '' redirects here. For the meridian often called the Prime Meridian, see Prime meridian ( Greenwich ). 0 ° Prime Meridian A prime meridian is a meridian ( a line of longitude ) in a geographic coordinate system at which longitude is defined to be 0 °. Together, a prime meridian and its antimeridian ( the 180th meridian in a 360 ° - system ) form a great circle. This great circle divides the sphere, e.g., Earth, into two hemispheres. If one uses directions of East and West from a defined prime meridian, then they can be called the Eastern Hemisphere and the Western Hemisphere. Gerardus Mercator in his Atlas Cosmographicae ( 1595 ) uses a prime meridian somewhere close to 25 ° W, passing just to the west of Santa Maria Island in the Atlantic. His 180th meridian runs along the Strait of Anián ( Bering Strait ) A prime meridian is ultimately arbitrary, unlike an equator, which is determined by the axis of rotation -- and various conventions have been used or advocated in different regions and throughout history. The most widely used modern meridian is the IERS Reference Meridian. It is derived but deviates slightly from the Greenwich Meridian, which was selected as an international standard in 1884. Contents 1 History 2 List of prime meridians on Earth 3 International prime meridian 3.1 Prime meridian at Greenwich 3.2 IERS Reference Meridian 3.2. 1 List of places 4 Prime meridian on other planetary bodies 5 See also 6 Notes 7 Citations 8 Works cited 9 External links History See also : History of longitude Ptolemy 's 1st projection, redrawn under Maximus Planudes around 1300, using a prime meridian east of Africa The notion of longitude was developed by the Greek Eratosthenes ( c. 276 BC -- c. 195 BC ) in Alexandria, and Hipparchus ( c. 190 BC -- c. 120 BC ) in Rhodes, and applied to a large number of cities by the geographer Strabo ( 64 / 63 BC -- c. 24 AD ). But it was Ptolemy ( c. AD 90 -- c. AD 168 ) who first used a consistent meridian for a world map in his Geographia. Ptolemy used as his basis the `` Fortunate Isles '', a group of islands in the Atlantic which are usually associated with the Canary Islands ( 13 ° to 18 ° W ), although his maps correspond more closely to the Cape Verde islands ( 22 ° to 25 ° W ). The main point is to be comfortably west of the western tip of Africa ( 17.5 ° W ) as negative numbers were not yet in use. His prime meridian corresponds to 18 ° 40 ' west of Winchester ( about 20 ° W ) today. At that time the chief method of determining longitude was by using the reported times of lunar eclipses in different countries. Diogo Ribeiro 's map of 1529, now in the Vatican library Ptolemy 's Geographia was first printed with maps at Bologna in 1477, and many early globes in the 16th century followed his lead. But there was still a hope that a `` natural '' basis for a prime meridian existed. Christopher Columbus reported ( 1493 ) that the compass pointed due north somewhere in mid-Atlantic, and this fact was used in the important Treaty of Tordesillas of 1494 which settled the territorial dispute between Spain and Portugal over newly discovered lands. The Tordesillas line was eventually settled at 370 leagues west of Cape Verde. This is shown in Diogo Ribeiro 's 1529 map. São Miguel Island ( 25.5 ° W ) in the Azores was still used for the same reason as late as 1594 by Christopher Saxton, although by then it had been shown that the zero magnetic deviation line did not follow a line of longitude. 1571 Africa map by Abraham Ortelius, with Cabo Verde prime meridian In 1541, Mercator produced his famous 41 cm terrestrial globe and drew his prime meridian precisely through Fuerteventura ( 14 ° 1'W ) in the Canaries. His later maps used the Azores, following the magnetic hypothesis. But by the time that Ortelius produced the first modern atlas in 1570, other islands such as Cape Verde were coming into use. In his atlas longitudes were counted from 0 ° to 360 °, not 180 ° W to 180 ° E as is usual today. This practice was followed by navigators well into the 18th century. In 1634, Cardinal Richelieu used the westernmost island of the Canaries, Ferro, 19 ° 55 ' west of Paris, as the choice of meridian. The geographer Delisle decided to round this off to 20 °, so that it simply became the meridian of Paris disguised. In the early 18th century the battle was on to improve the determination of longitude at sea, leading to the development of the marine chronometer by John Harrison. But it was the development of accurate star charts, principally by the first British Astronomer Royal, John Flamsteed between 1680 and 1719 and disseminated by his successor Edmund Halley, that enabled navigators to use the lunar method of determining longitude more accurately using the octant developed by Thomas Godfrey and John Hadley. Between 1765 and 1811, Nevil Maskelyne published 49 issues of the Nautical Almanac based on the meridian of the Royal Observatory, Greenwich. `` Maskelyne 's tables not only made the lunar method practicable, they also made the Greenwich meridian the universal reference point. Even the French translations of the Nautical Almanac retained Maskelyne 's calculations from Greenwich -- in spite of the fact that every other table in the Connaissance des Temps considered the Paris meridian as the prime. '' In 1884, at the International Meridian Conference in Washington, D.C., 22 countries voted to adopt the Greenwich meridian as the prime meridian of the world. The French argued for a neutral line, mentioning the Azores and the Bering Strait, but eventually abstained and continued to use the Paris meridian until 1911. List of prime meridians on Earth Locality Modern longitude Meridian name Bering Strait 168 ° 30 ′ W Offered in 1884 as possibility for a `` neutral prime meridian '' by Pierre Janssen at the International Meridian Conference Washington, D.C. 77 ° 03 ′ 56.07 '' W ( 1897 ) or 77 ° 04 ′ 02.24 '' W ( NAD 27 ) or 77 ° 04 ′ 01.16 '' W ( NAD 83 ) New Naval Observatory meridian Washington, D.C. 77 ° 02 ′ 48.0 '' W, 77 ° 03 ′ 02.3 '', 77 ° 03 ′ 06.119 '' W or 77 ° 03 ′ 06.276 '' W ( both presumably NAD 27 ). If NAD27, the latter would be 77 ° 03 ′ 05.194 '' W ( NAD 83 ) Old Naval Observatory meridian Washington, D.C. 77 ° 02 ′ 11.56299 '' W ( NAD 83 ), 77 ° 02 ′ 11.55811 '' W ( NAD 83 ), 77 ° 02 ′ 11.58325 '' W ( NAD 83 ) ( three different monuments originally intended to be on the White House meridian ) White House meridian Washington, D.C. 77 ° 00 ′ 32.6 '' W ( NAD 83 ) Capitol meridian Philadelphia 75 ° 10 ′ 12 '' W Rio de Janeiro 43 ° 10 ′ 19 '' W Fortunate Isles / Azores 25 ° 40 ′ 32 '' W Used until the Middle Ages, proposed as one possible neutral meridian by Pierre Janssen at the International Meridian Conference El Hierro ( Ferro ), Canary Islands 18 ° 03 ′ W, later redefined as 17 ° 39 ′ 46 '' W Ferro meridian Tenerife 16 ° 38 ' 22 '' W Tenerife meridian Rose to prominence with Dutch cartographers and navigators after they abandoned the idea of a magnetic meridian Cadiz 6 ° 17 ' 15 '' W San Fernando meridian Lisbon 9 ° 07 ′ 54.862 '' W Madrid 3 ° 41 ′ 16.58 '' W Greenwich 0 ° 00 ′ 05.3101 '' W Greenwich meridian Airy Meridian Greenwich 0 ° 00 ′ 05.33 '' W United Kingdom Ordnance Survey Zero Meridian Bradley Meridian Greenwich 0 ° 00 ′ 00.00 '' IERS Reference Meridian Paris 2 ° 20 ′ 14.025 '' E Paris meridian Brussels 4 ° 22 ′ 4.71 '' E Antwerp 4 ° 24 ′ E Antwerp meridian Amsterdam 4 ° 53 ′ E through the Westerkerk in Amsterdam ; used to define the legal time in the Netherlands from 1909 to 1937 Bern 7 ° 26 ′ 22.5 '' E Pisa 10 ° 24 ′ E Oslo ( Kristiania ) 10 ° 43 ′ 22.5 '' E Florence 11 ° 15 ′ E Florence meridian used in the Peters projection, 180 ° from a meridian running through the Bering Strait Rome 12 ° 27 ′ 08.4 '' E meridian of Monte Mario Used in Roma 40 Datum Copenhagen 12 ° 34 ′ 32.25 '' E Rundetårn Naples 14 ° 15 ′ E Bratislava 17 ° 06 ′ 03 '' E Meridianus Posoniensis Used by Sámuel Mikoviny Stockholm 18 ° 03 ′ 29.8 '' E at the Stockholm Observatory Kraków 19 ° 57 ′ 21.43 '' E Kraków meridian at the Old Kraków Observatory at the Śniadecki ' College ; mentioned also in Nicolaus Copernicus 's work On the Revolutions of the Heavenly Spheres. Warsaw 21 ° 00 ′ 42 '' E Warsaw meridian Oradea 21 ° 55 ′ 16 '' E Between 1464 and 1667, a prime meridian was set in the Fortress of Oradea ( Varadinum at the time ) by Georg von Peuerbach. Alexandria 29 ° 53 ′ E Meridian of Alexandria The meridian of Ptolemy 's Almagest. Saint Petersburg 30 ° 19 ′ 42.09 '' E Pulkovo meridian Great Pyramid of Giza 31 ° 08 ′ 03.69 '' E 1884 Jerusalem 35 ° 13 ′ 47.1 '' E Mecca 39 ° 49 ′ 34 '' E see also Mecca Time Ujjain 75 ° 47 ′ E Used from 4th century CE Indian astronomy and calendars ( see also Time in India ). Kyoto 136 ° 14 ′ E Used in 18th and 19th ( officially 1779 -- 1871 ) century Japanese maps. Exact place unknown, but in `` Kairekisyo '' in Nishigekkoutyou - town in Kyoto, then the capital. ~ 180 Opposite of Greenwich, proposed 13 October 1884 on the International Meridian Conference by Sandford Fleming International prime meridian In October 1884 the Greenwich Meridian was selected by delegates ( forty - one delegates representing twenty - five nations ) to the International Meridian Conference held in Washington, D.C., United States to be the common zero of longitude and standard of time reckoning throughout the world. The modern prime meridian, the IERS Reference Meridian, is placed very near this meridian and is the prime meridian that currently has the widest use. Prime meridian at Greenwich Markings of the prime meridian at the Royal Observatory, Greenwich. Main article : Prime meridian ( Greenwich ) The modern prime meridian, based at the Royal Observatory, Greenwich, was established by Sir George Airy in 1851. The position of the Greenwich Meridian has been defined by the location of the Airy Transit Circle ever since the first observation was taken with it by Sir George Airy in 1851. Prior to that, it was defined by a succession of earlier transit instruments, the first of which was acquired by the second Astronomer Royal, Edmond Halley in 1721. It was set up in the extreme north - west corner of the Observatory between Flamsteed House and the Western Summer House. This spot, now subsumed into Flamsteed House, is roughly 43 metres to the west of the Airy Transit Circle, a distance equivalent to roughly 0.15 seconds of time. It was Airy 's transit circle that was adopted in principle ( with French delegates, who pressed for adoption of the Paris meridian abstaining ) as the Prime Meridian of the world at the 1884 International Meridian Conference. All of these Greenwich meridians were located via an astronomic observation from the surface of the Earth, oriented via a plumb line along the direction of gravity at the surface. This astronomic Greenwich meridian was disseminated around the world, first via the lunar distance method, then by chronometers carried on ships, then via telegraph lines carried by submarine communications cables, then via radio time signals. One remote longitude ultimately based on the Greenwich meridian using these methods was that of the North American Datum 1927 or NAD27, an ellipsoid whose surface best matches mean sea level under the United States. IERS Reference meridian Main article : IERS Reference Meridian Satellites changed the reference from the surface of the Earth to its centre of mass around which all satellites orbit regardless of surface irregularities. The requirement that satellite - based geodetic reference systems be centred on the centre of mass of the earth caused the modern prime meridian to be 5.3 '' east of the astronomic Greenwich prime meridian through the Airy Transit Circle. At the latitude of Greenwich, this amounts to 102 metres. This was officially accepted by the Bureau International de l'Heure ( BIH ) in 1984 via its BTS84 ( BIH Terrestrial System ) that later became WGS84 ( World Geodetic System 1984 ) and the various ITRFs ( International Terrestrial Reference Systems ). Due to the movement of Earth 's tectonic plates, the line of 0 ° longitude along the surface of the Earth has slowly moved toward the west from this shifted position by a few centimetres ; that is, towards the Airy Transit Circle ( or the Airy Transit Circle has moved toward the east, depending on your point of view ) since 1984 ( or the 1960s ). With the introduction of satellite technology, it became possible to create a more accurate and detailed global map. With these advances there also arose the necessity to define a reference meridian that, whilst being derived from the Airy Transit Circle, would also take into account the effects of plate movement and variations in the way that the Earth was spinning. As a result, the International Reference Meridian was established and is commonly used to denote Earth 's prime meridian ( 0 ° longitude ) by the International Earth Rotation and Reference Systems Service, which defines and maintains the link between longitude and time. Based on observations to satellites and celestial compact radio sources ( quasars ) from various coordinated stations around the globe, Airy 's transit circle drifts northeast about 2.5 centimetres per year relative to this Earth - centred 0 ° longitude. Circa 1999 the international reference meridian ( IRM ) passed 5.31 arcseconds east of Airy 's meridian or 102.5 metres ( 336.3 feet ) at the latitude of the Royal Observatory, Greenwich, London. It is also the reference meridian of the Global Positioning System operated by the United States Department of Defense, and of WGS84 and its two formal versions, the ideal International Terrestrial Reference System ( ITRS ) and its realization, the International Terrestrial Reference Frame ( ITRF ). A current convention on the Earth uses the opposite of the IRM as the basis for the International Date Line. List of places Map all coordinates using : OpenStreetMap Download coordinates as : KML GPX On Earth, starting at the North Pole and heading south to the South Pole, the IERS Reference Meridian ( as of 2016 ) passes through : Co-ordinates ( approximate ) Country, territory or sea Notes 90 ° 0 ′ N 0 ° 0 ′ E ﻿ / ﻿ 90.000 ° N 0.000 ° E ﻿ / 90.000 ; 0.000 ﻿ ( North Pole ) Arctic Ocean 81 ° 39 ′ N 0 ° 0 ′ E ﻿ / ﻿ 81.650 ° N 0.000 ° E ﻿ / 81.650 ; 0.000 ﻿ ( Greenland Sea ) Greenland Sea 72 ° 53 ′ N 0 ° 0 ′ E ﻿ / ﻿ 72.883 ° N 0.000 ° E ﻿ / 72.883 ; 0.000 ﻿ ( Norwegian Sea ) Norwegian Sea 61 ° 0 ′ N 0 ° 0 ′ E ﻿ / ﻿ 61.000 ° N 0.000 ° E ﻿ / 61.000 ; 0.000 ﻿ ( North Sea ) North Sea 53 ° 45 ′ N 0 ° 0 ′ E ﻿ / ﻿ 53.750 ° N 0.000 ° E ﻿ / 53.750 ; 0.000 ﻿ ( United Kingdom ) United Kingdom From Tunstall in East Riding to Peacehaven, passing through Greenwich 50 ° 47 ′ N 0 ° 0 ′ E ﻿ / ﻿ 50.783 ° N 0.000 ° E ﻿ / 50.783 ; 0.000 ﻿ ( English Channel ) English Channel 49 ° 19 ′ N 0 ° 0 ′ E ﻿ / ﻿ 49.317 ° N 0.000 ° E ﻿ / 49.317 ; 0.000 ﻿ ( France ) France From Villers - sur - Mer to Gavarnie 42 ° 41 ′ N 0 ° 0 ′ E ﻿ / ﻿ 42.683 ° N 0.000 ° E ﻿ / 42.683 ; 0.000 ﻿ ( Spain ) Spain From Cilindro de Marboré to Castellón de la Plana 39 ° 56 ′ N 0 ° 0 ′ E ﻿ / ﻿ 39.933 ° N 0.000 ° E ﻿ / 39.933 ; 0.000 ﻿ ( Mediterranean Sea ) Mediterranean Sea Gulf of Valencia 38 ° 52 ′ N 0 ° 0 ′ E ﻿ / ﻿ 38.867 ° N 0.000 ° E ﻿ / 38.867 ; 0.000 ﻿ ( Spain ) Spain From El Verger to Calpe 38 ° 38 ′ N 0 ° 0 ′ E ﻿ / ﻿ 38.633 ° N 0.000 ° E ﻿ / 38.633 ; 0.000 ﻿ ( Mediterranean Sea ) Mediterranean Sea 35 ° 50 ′ N 0 ° 0 ′ E ﻿ / ﻿ 35.833 ° N 0.000 ° E ﻿ / 35.833 ; 0.000 ﻿ ( Algeria ) Algeria From Stidia to Algeria - Mali border near Bordj Mokhtar 21 ° 50 ′ N 0 ° 0 ′ E ﻿ / ﻿ 21.833 ° N 0.000 ° E ﻿ / 21.833 ; 0.000 ﻿ ( Mali ) Mali 14 ° 59 ′ N 0 ° 0 ′ E ﻿ / ﻿ 14.983 ° N 0.000 ° E ﻿ / 14.983 ; 0.000 ﻿ ( Burkina Faso ) Burkina Faso 11 ° 6 ′ N 0 ° 0 ′ E ﻿ / ﻿ 11.100 ° N 0.000 ° E ﻿ / 11.100 ; 0.000 ﻿ ( Togo ) Togo For about 600 m 11 ° 6 ′ N 0 ° 0 ′ E ﻿ / ﻿ 11.100 ° N 0.000 ° E ﻿ / 11.100 ; 0.000 ﻿ ( Ghana ) Ghana For about 16 km 10 ° 57 ′ N 0 ° 0 ′ E ﻿ / ﻿ 10.950 ° N 0.000 ° E ﻿ / 10.950 ; 0.000 ﻿ ( Togo ) Togo For about 39 km 10 ° 36 ′ N 0 ° 0 ′ E ﻿ / ﻿ 10.600 ° N 0.000 ° E ﻿ / 10.600 ; 0.000 ﻿ ( Ghana ) Ghana From the Togo - Ghana border near Bunkpurugu to Tema Passing through Lake Volta at 7 ° 48 ′ N 0 ° 0 ′ E ﻿ / ﻿ 7.800 ° N 0.000 ° E ﻿ / 7.800 ; 0.000 ﻿ ( Lake Volta ) 5 ° 37 ′ N 0 ° 0 ′ E ﻿ / ﻿ 5.617 ° N 0.000 ° E ﻿ / 5.617 ; 0.000 ﻿ ( Atlantic Ocean ) Atlantic Ocean Passing through the Equator at 0 ° 0 ′ N 0 ° 0 ′ E ﻿ / ﻿ 0.000 ° N 0.000 ° E ﻿ / 0.000 ; 0.000 ﻿ ( Equator ) ( `` Null Island '' ) 60 ° 0 ′ S 0 ° 0 ′ E ﻿ / ﻿ 60.000 ° S 0.000 ° E ﻿ / - 60.000 ; 0.000 ﻿ ( Southern Ocean ) Southern Ocean 68 ° 54 ′ S 0 ° 0 ′ E ﻿ / ﻿ 68.900 ° S 0.000 ° E ﻿ / - 68.900 ; 0.000 ﻿ ( Antarctica ) Antarctica Queen Maud Land, claimed by Norway Prime meridian on other planetary bodies See also : Longitude ( planets ) `` Prime meridian ( planets ) '' redirects here. It is not to be confused with Central meridian ( planets ). As on the Earth, prime meridians must be arbitrarily defined. Often a landmark such as a crater is used ; other times a prime meridian is defined by reference to another celestial object, or by magnetic fields. The prime meridians of the following planetographic systems have been defined : Two different heliographic coordinate systems are used on the Sun. The first is the Carrington heliographic coordinate system. In this system, the prime meridian passes through the center of the solar disk as seen from the Earth on 9 November 1853, which is when Richard Christopher Carrington started his observations of sunspots. The second is the Stonyhurst heliographic coordinates system. In 1975 the prime meridian of Mercury was defined to be 20 ° east of the crater Hun Kal. Defined in 1992, the prime meridian of Venus passes through the central peak in the crater Ariadne. The prime meridian of the Moon lies directly in the middle of the face of the moon visible from Earth and passes near the crater Bruce. The prime meridian of Mars was established in 1971 and passes through the center of the crater Airy - 0, although it is fixed by the longitude of the Viking 1 lander, which is defined to be 47 °. 95137 west.. Jupiter has several coordinate systems because its cloud tops -- the only part of the planet visible from space -- rotate at different rates depending on latitude. It is unknown whether Jupiter has any internal solid surface that would enable a more Earth - like coordinate system. System I and System II coordinates are based on atmospheric rotation, and System III coordinates use Jupiter 's magnetic field. Titan, like the Earth 's moon, always has the same face towards Saturn, and so the middle of that face is 0 longitude. Pluto 's prime meridian is defined as the center of the face that is always pointed towards Charon, its largest moon, as the two are tidally locked towards each other. See also Geography portal 1st meridian east 1st meridian west 180th meridian Notes Jump up ^ Voting took place on 13 October and the resolutions were adopted on 22 October 1884. Citations Jump up ^ Prime Meridian, geog.port.ac.uk Jump up ^ Norgate & Norgate 2006 Jump up ^ Hooker 2006 Jump up ^ e.g. Jacob Roggeveen in 1722 reported the longitude of Easter Island as 268 ° 45 ' ( starting from Fuerteventura ) in the Extract from the Official log of Jacob Roggeveen reproduced in Bolton Glanville Corney, ed. ( 1908 ), The voyage of Don Felipe Gonzalez to Easter Island in 1770 - 1, Hakluyt Society, p. 3, retrieved 13 January 2013 Jump up ^ Speech by Pierre Janssen, director of the Paris observatory, at the first session of the Meridian Conference. Jump up ^ Sobel & Andrewes 1998, pp. 110 -- 115 Jump up ^ Sobel & Andrewes 1998, pp. 197 -- 199 Jump up ^ `` The Prime Meridian at Greenwich ''. Royal Museums Greenwich. n.d. Retrieved 28 March 2016. Jump up ^ International Conference Held at Washington for the Purpose of Fixing a Prime Meridian and a Universal Day. October, 1884. Project Gutenberg Jump up ^ NGS 2016, PID : HV1847. Jump up ^ NGS 2016, PID : HV1846. Jump up ^ NGS 2016, PID : AH7372. ^ Jump up to : Hooker ( 2006 ), introduction. ^ Jump up to : Oct. 13, 1884 : Greenwich Resolves Subprime Meridian Crisis, WIRED, 13 October 2010. Jump up ^ Atlas do Brazil, 1909, by Barão Homem de Mello e Francisco Homem de Mello, published in Rio de Janeiro by F. Briguiet & Cia. ^ Jump up to : `` The Project Gutenberg eBook of International Conference Held at Washington for the Purpose of Fixing a Prime Meridian and a Universal Day ''. Gutenberg.org. 12 February 2006. Retrieved 28 March 2016. Jump up ^ Ancient, used in Ptolemy 's Geographia. Later redefined 17 ° 39 ′ 46 '' W of Greenwich to be exactly 20 ° W of Paris. French `` submarin '' at Washington 1884. Jump up ^ A.R.T. Jonkers ; Parallel meridians : Diffusion and change in early modern oceanic reckoning, in Noord - Zuid in Oostindisch perspectief, The Hague, 2005, p. 7. Retrieved 2 February 2015. Jump up ^, ( 1 ), in El País, 2016, retrieved 23 December 2016. ^ Jump up to : Bartky, Ian R. ( 2007 ), One Time Fits All : The Campaigns for Global Uniformity, p. 98, retrieved through GoogleBooks, 6 May 2014. ^ Jump up to : Dolan 2013a. Jump up ^ ( in Dutch ) Eenheid van tijd in Nederland ( Unity of time in the Netherlands ), Utrecht University website, retrieved 28 August 2013. Jump up ^ Grids & Datums -- Italian Republic, asprs.org, Retrieved 10 December 2013. Jump up ^ meridian, article from Den Store Danske Encyklopædi Jump up ^ Oradea, Tourism office website, retrieved 3 February 2015. Jump up ^ `` Romanian astronaut makrsk 10th anniversary of Prime Meridian Astronomy Club ''. NineO'Clock.ro. 2015. Retrieved 26 June 2017. Jump up ^ Wilcomb E. Washburn, `` The Canary Islands and the Question of the Prime Meridian : The Search for Precision in the Measurement of the Earth Archived 29 May 2007 at the Wayback Machine. '' Jump up ^ Maimonides, Hilchot Kiddush Hachodesh 11 : 17, calls this point אמצע היישוב, `` the middle of the habitation '', i.e. the habitable hemisphere. Evidently this was a convention accepted by Arab geographers of his day. Jump up ^ Burgess 1860 Jump up ^ `` International Conference Held at Washington for the Purpose of Fixing a Prime Meridian and a Universal Day. October, 1884. Protocols of the proceedings ''. Project Gutenberg. 1884. Retrieved 30 November 2012. Jump up ^ Howse 1997, pp. 12, 137 ^ Jump up to : Greenwich Observatory... the story of Britain 's oldest scientific institution, the Royal Observatory at Greenwich and Herstmonceux, 1675 -- 1975 p. 10. Taylor & Francis, 1975 Jump up ^ McCarthy, Dennis ; Seidelmann, P. Kenneth ( 2009 ). TIME from Earth Rotation to Atomic Physics. Weinheim : Wiley - VCH. pp. 244 -- 5. Jump up ^ ROG Learning Team ( 23 August 2002 ). `` The Prime Meridian at Greenwich ''. Royal Museums Greenwich. Royal Museums Greenwich. Retrieved 14 June 2012. Jump up ^ Malys, Stephen ; Seago, John H. ; Palvis, Nikolaos K. ; Seidelmann, P. Kenneth ; Kaplan, George H. ( 1 August 2015 ). `` Why the Greenwich meridian moved ''. Journal of Geodesy. 89 ( 12 ) : 1263. Bibcode : 2015JGeod... 89.1263 M. doi : 10.1007 / s00190 - 015 - 0844 - y. Jump up ^ Dolan 2013b. ^ Jump up to : History of the Prime Meridian - Past and Present ^ Jump up to : IRM on grounds of Royal Observatory from Google Earth Accessed 30 March 2012 ^ Jump up to : The astronomic latitude of the Royal Observatory is 51 ° 28'38 `` N whereas its latitude on the European Terrestrial Reference Frame ( 1989 ) datum is 51 ° 28'40.1247 '' N. Jump up ^ Guinot, B., 2011. Solar time, legal time, time in use. Metrologica 48, S181 -- S185. Jump up ^ `` Carrington heliographic coordinates ''. Jump up ^ Davies, M.E., `` Surface Coordinates and Cartography of Mercury, '' Journal of Geophysical Research, Vol. 80, No. 17, June 10, 1975 Jump up ^ Davies, M.E., S.E. Dwornik, D.E. Gault, and R.G. Strom, NASA Atlas of Mercury, NASA Scientific and Technical Information Office, 1978. Jump up ^ Archinal, Brent A. ; A'Hearn, Michael F. ; Bowell, Edward G. ; Conrad, Albert R. ; Consolmagno, Guy J. ; et al. ( 2010 ). `` Report of the IAU Working Group on Cartographic Coordinates and Rotational Elements : 2009 '' ( PDF ). Celestial Mechanics and Dynamical Astronomy. 109 ( 2 ) : 101 -- 135. Bibcode : 2011CeMDA. 109... 101A. doi : 10.1007 / s10569 - 010 - 9320 - 4. Jump up ^ Davies, M.E. ; Colvin, T.R. ; Rogers, P.G. ; Chodas, P.G. ; Sjogren, W.L. ; Akim, W.L. ; Stepanyantz, E.L. ; Vlasova, Z.P. ; and Zakharov, A.I. ; `` The Rotation Period, Direction of the North Pole, and Geodetic Control Network of Venus '', Journal of Geophysical Research, vol. 97, no. 8, 1992, pp. 1 - 14, 151 Jump up ^ `` USGS Astrogeology : Rotation and pole position for the Sun and planets ( IAU WGCCRE ) ''. Retrieved 22 October 2009. Jump up ^ Davies, M.E., and Berg, R.A. ; `` Preliminary Control Net of Mars '', Journal of Geophysical Research, vol. 76, no. 2, January 10, 1971, pp. 373 - 393 Jump up ^ Archinal, Brent A. ; Acton, C.H. ; A'Hearn, Michael F. ; Conrad, Albert R. ; et al. ( 2018 ), `` Report of the IAU Working Group on Cartographic Coordinates and Rotational Elements : 2015 '', Celestial Mechanics and Dynamical Astronomy, 130 ( 22 ), doi : 10.1007 / s10569 - 017 - 9805 - 5 CS1 maint : Explicit use of et al. ( link ) Jump up ^ `` Planetographic Coordinates ''. Retrieved 24 May 2017. Works cited Burgess, Ebenezer ( 1860 ), `` Translation of the Surya - Siddhanta '', Journal of the American Oriental Society ( e book ), 6, Google ( published c. 2013 ), p. 185 Dolan, Graham ( 2013a ). `` The Greenwich Meridian before the Airy Transit Circle ''. The Greenwich Meridian. Dolan, Graham ( 2013b ). `` WGS84 and the Greenwich Meridian ''. The Greenwich Meridian. Hooker, Brian ( 2006 ), A multitude of prime meridians, retrieved 13 January 2013 Howse, Derek ( 1997 ), Greenwich Time and the Longitude, Phillip Wilson, ISBN 0 - 85667 - 468 - 0 Norgate, Jean ; Norgate, Martin ( 2006 ), Prime meridian, retrieved 13 January 2013 NGS datasheet station name form, National Geodetic Survey, 2016, retrieved 11 December 2016 Sobel, Dava ; Andrewes, William J.H. ( 1998 ), The Illustrated Longitude, Fourth Estate, London External links Wikimedia Commons has media related to Prime meridian. `` Where the Earth 's surface begins -- and ends '', Popular Mechanics, December 1930 scanned TIFFs of the conference proceedings Prime meridians in use in the 1880s, by country Time measurement and standards Chronometry Orders of magnitude Metrology International standards Coordinated Universal Time offset UT ΔT DUT1 International Earth Rotation and Reference Systems Service ISO 31 - 1 ISO 8601 International Atomic Time 6 - hour clock 12 - hour clock 24 - hour clock Barycentric Coordinate Time Barycentric Dynamical Time Civil time Daylight saving time Geocentric Coordinate Time International Date Line Leap second Solar time Terrestrial Time Time zone 180th meridian Obsolete standards Ephemeris time Greenwich Mean Time Prime meridian Time in physics Absolute space and time Spacetime Chronon Continuous signal Coordinate time Cosmological decade Discrete time and continuous time Planck time Proper time Theory of relativity Time dilation Gravitational time dilation Time domain Time translation symmetry T - symmetry Horology Clock Astrarium Atomic clock Complication History of timekeeping devices Hourglass Marine chronometer Marine sandglass Radio clock Watch stopwatch Water clock Sundial Dialing scales Equation of time History of sundials Sundial markup schema Calendar Astronomical Dominical letter Epact Equinox Gregorian Hebrew Hindu Intercalation Islamic Julian Leap year Lunar Lunisolar Solar Solstice Tropical year Weekday determination Weekday names Archaeology and geology Chronological dating Geologic time scale International Commission on Stratigraphy Astronomical chronology Galactic year Nuclear timescale Precession Sidereal time Other units of time Flick Shake Jiffy Second Minute Moment Hour Day Week Fortnight Month Year Olympiad Lustrum Decade Century Saeculum Millennium Related topics Chronology Duration music Mental chronometry Metric time System time Time value of money Timekeeper Circles of latitude / meridians Equator Tropic of Cancer Tropic of Capricorn Arctic Circle Antarctic Circle Equator Tropic of Cancer Tropic of Capricorn Arctic Circle Antarctic Circle Equator Tropic of Cancer Tropic of Capricorn Arctic Circle Antarctic Circle W 0 ° E 30 ° 60 ° 90 ° 120 ° 150 ° 180 ° 30 ° 60 ° 90 ° 120 ° 150 ° 180 ° 5 ° 15 ° 25 ° 35 ° 45 ° 55 ° 65 ° 75 ° 85 ° 95 ° 105 ° 115 ° 125 ° 135 ° 145 ° 155 ° 165 ° 175 ° 5 ° 15 ° 25 ° 35 ° 45 ° 55 ° 65 ° 75 ° 85 ° 95 ° 105 ° 115 ° 125 ° 135 ° 145 ° 155 ° 165 ° 175 ° 10 ° 20 ° 40 ° 50 ° 70 ° 80 ° 100 ° 110 ° 130 ° 140 ° 160 ° 170 ° 10 ° 20 ° 40 ° 50 ° 70 ° 80 ° 100 ° 110 ° 130 ° 140 ° 160 ° 170 ° 0 ° 10 ° 20 ° 30 ° 40 ° 50 ° 60 ° 70 ° 80 ° 90 ° 10 ° 20 ° 30 ° 40 ° 50 ° 60 ° 70 ° 80 ° 90 ° 5 ° N 15 ° 25 ° 35 ° 45 ° 55 ° 65 ° 75 ° 85 ° 5 ° S 15 ° 25 ° 35 ° 45 ° 55 ° 65 ° 75 ° 85 ° 45x90 45x90 45x90 45x90 Retrieved from `` https://en.wikipedia.org/w/index.php?title=Prime_meridian&oldid=863748079 '' Categories : Geodesy Lines of longitude Prime meridians Hidden categories : Articles with Dutch - language external links Webarchive template wayback links CS1 maint : Explicit use of et al. 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Question: what is the opposite of the prime meridian called
Answer: the 180th meridian