Circle of latitude - wikipedia Circle of latitude This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. ( April 2012 ) Map of Earth Longitude ( λ ) Lines of longitude appear vertical with varying curvature in this projection, but are actually halves of great ellipses, with identical radii at a given latitude. Latitude ( φ ) Lines of latitude appear horizontal with varying curvature in this projection ; but are actually circular with different radii. All locations with a given latitude are collectively referred to as a circle of latitude. The equator divides the planet into a Northern Hemisphere and a Southern Hemisphere, and has a latitude of 0 °. Geodesy Fundamentals Geodesy Geodynamics Geomatics Cartography History Concepts Geographical distance Geoid Figure of the Earth Geodetic datum Geodesic Geographic coordinate system Horizontal position representation Latitude / Longitude Map projection Reference ellipsoid Satellite geodesy Spatial reference system Technologies Global Navigation Satellite System ( GNSS ) Global Positioning System ( GPS ) GLONASS ( Russian ) BeiDou ( BDS ) ( Chinese ) Galileo ( European ) Indian Regional Navigation Satellite System ( IRNSS ) ( India ) Quasi-Zenith Satellite System ( QZSS ) ( Japan ) Legenda ( satellite system ) Standards ( History ) NGVD 29 Sea Level Datum 1929 OSGB36 Ordnance Survey Great Britain 1936 SK - 42 Systema Koordinat 1942 goda ED50 European Datum 1950 SAD69 South American Datum 1969 GRS 80 Geodetic Reference System 1980 NAD 83 North American Datum 1983 WGS 84 World Geodetic System 1984 NAVD 88 N. American Vertical Datum 1988 ETRS89 European Terrestrial Reference System 1989 GCJ - 02 Chinese encrypted datum 2002 International Terrestrial Reference System Spatial Reference System Identifier ( SRID ) Universal Transverse Mercator ( UTM ) Mercator projection world map, true angles but untrue regarding areas, especially at high latitudes. Also note increasing distances between the latitudes towards the poles and the parallel longitude lines. The only true world maps are globes. The Mercator projection comes from a globe inside a cylinder. Picture shows projection and use of a worldwide Mercator projection map. The Mercator projection first came in use by the Dutch in the 16th century A circle of latitude on the Earth is an abstract east -- west circle connecting all locations around the Earth ( ignoring elevation ) at a given latitude. Circles of latitude are often called parallels because they are parallel to each other -- that is, any two circles are always the same distance apart. A location 's position along a circle of latitude is given by its longitude. Circles of latitude are unlike circles of longitude, which all are great circles with the centre of Earth in the middle, as the circles of latitude get smaller as the distance from the Equator increases. Their length can be calculated by a common sine or cosine function. The 60th circle of latitude is half as long as the equator ( disregarding Earth 's minor flattening by 0.3 % ). A circle of latitude is perpendicular to all meridians. The latitude of the circle is approximately the angle between the equator and the circle, with the angle 's vertex at Earth 's centre. The equator is at 0 °, and the North and South poles are at 90 ° north and 90 ° south respectively. The Equator is the longest circle of latitude and is the only circle of latitude which also is a great circle. There are 89 integral ( whole degree ) circles of latitude between the equator and the Poles in each hemisphere, but these can be divided into more precise measurements of latitude, and are often represented as a decimal degree ( e.g. 34.637 ° N ) or with minutes and seconds ( e.g. 22 ° 14'26 `` S ). There is no limit to how precisely latitude can be measured, and so there are an infinite number of circles of latitude on Earth. On a map, the circles of latitude may or may not be parallel, and their spacing may vary, depending on which projection is used to map the surface of the Earth onto a plane. On an equirectangular projection, centered on the equator, the circles of latitude are horizontal, parallel, and equally spaced. On other cylindrical and pseudocylindrical projections, the circles of latitude are horizontal and parallel, but may be spaced unevenly to give the map useful characteristics. For instance, on a Mercator projection the circles of latitude are more widely spaced near the poles to preserve local scales and shapes, while on a Gall -- Peters projection the circles of latitude are spaced more closely near the poles so that comparisons of area will be accurate. On most non-cylindrical and non-pseudocylindrical projections, the circles of latitude are neither straight nor parallel. Arcs of circles of latitude are sometimes used as boundaries between countries or regions where distinctive natural borders are lacking ( such as in deserts ), or when an artificial border is drawn as a `` line on a map '', which was made in massive scale during the 1884 Berlin Conference, regarding huge parts of the African continent. North American nations and states have also mostly been created by straight lines, which are often parts of circles of latitudes. For instance, the northern border of Colorado is at 41 ° N while the southern border is at 37 ° N. Roughly half the length of border between the United States and Canada follows 49 ° N. Contents 1 Major circles of latitude 1.1 Equator 1.2 Polar Circles 1.3 Tropical Circles 1.4 Movement of the Tropical and Polar circles 2 Other notable parallels 3 Altitude 4 See also 5 References 6 External links Major circles of latitude Diagram showing the locations of the five major circles of latitude on an equirectangular projection of the Earth. Relationship between Earth 's axial tilt ( ε ) to the tropical and polar circles There are five major circles of latitude, listed below from north to south. The position of the Equator is fixed ( 90 degrees from Earth 's axis of rotation ) but the latitudes of the other circles depend on the tilt of this axis relative to the plane of Earth 's orbit, and so are not perfectly fixed. The values below are for 17 December 2017 : Arctic Circle ( 66 ° 33 ′ 47.0 '' N ) Tropic of Cancer ( 23 ° 26 ′ 13.0 '' N ) Equator ( 0 ° latitude ) Tropic of Capricorn ( 23 ° 26 ′ 13.0 '' S ) Antarctic Circle ( 66 ° 33 ′ 47.0 '' S ) These circles of latitude, excluding the Equator, mark the divisions between the five principal geographical zones. Equator The equator is the circle that is equidistant from the North Pole and South Pole. It divides the Earth into the Northern Hemisphere and the Southern Hemisphere. Of the parallels or circles of latitude, it is the longest, and the only ' great circle ' ( a circle on the surface of the Earth, centered on Earth 's center ). All the other parallels are smaller and centered only on Earth 's axis. Equator Polar circles The Arctic Circle is the southernmost latitude in the Northern Hemisphere at which the sun can remain continuously above or below the horizon for 24 hours ( at the June and December solstices respectively ). Similarly, the Antarctic Circle marks the northernmost latitude in the Southern Hemisphere at which the sun can remain continuously above or below the horizon for 24 hours ( at the December and June Solstices respectively ). Arctic Circle Antarctic Circle Tropical circles The Tropic of Cancer and Tropic of Capricorn mark the northernmost and southernmost latitudes at which the sun may be seen directly overhead ( at the June solstice and December solstice respectively ). The latitude of the tropical circles is equal to the Earth 's axial tilt, about 23 °. Tropic of Cancer Tropic of Capricorn Movement of the Tropical and Polar circles See also : Axial tilt By definition, the positions of the Tropic of Cancer, Tropic of Capricorn, Arctic Circle and Antarctic Circle all depend on the tilt of the Earth 's axis relative to the plane of its orbit around the sun ( the `` obliquity of the ecliptic '' ). If the Earth were `` upright '' ( its axis at right angles to the orbital plane ) there would be no Arctic, Antarctic, or Tropical circles : at the poles the sun would always circle along the horizon, and at the equator the sun would always rise due east, pass directly overhead, and set due west. The positions of the Tropical and Polar circles are not fixed because the axial tilt changes slowly -- a complex motion determined by the superimposition of many different cycles ( some of which are described below ) with short to very long periods. In 2000 the mean value of the tilt was about 23 ° 26 ′ 21 ''. The main long - term cycle causes the axial tilt to fluctuate between about 22.1 ° and 24.5 ° with a period of 41,000 years. Currently, the average value of the tilt is decreasing by about 0.47 '' per year. As a result, ( approximately, and on average ) the Tropical Circles are drifting towards the equator ( and the Polar Circles towards the poles ) by 15 metres per year, and the area of the Tropics is decreasing by 1,100 square kilometres ( 420 sq mi ) per year. The Earth 's axial tilt has additional shorter - term variations due to nutation, of which the main term, with a period of 18.6 years, has an amplitude of 9.2 '' ( corresponding to almost 300 metres north and south ). There are many smaller terms, resulting in varying daily shifts of some metres in any direction. Finally, the Earth 's rotational axis is not exactly fixed in the Earth, but undergoes small fluctuations ( on the order of 15 meters ) called polar motion, which have a small effect on the Tropics and Polar circles and also on the Equator. Short - term fluctuations over a matter of days do not directly affect the location of the extreme latitudes at which the sun may appear directly overhead, or at which 24 - hour day or night is possible, except when they actually occur at the time of the solstices. Rather, they cause a theoretical shifting of the parallels, that would occur if the given axis tilt were maintained throughout the year. Other notable parallels See also : Baseline ( surveying ) A number of sub-national and international borders were intended to be defined by, or are approximated by, parallels. Parallels make convenient borders in the northern hemisphere because astronomic latitude can be roughly measured ( to within a few tens of meters ) by sighting the North Star. Parallel Description 70 ° N On Victoria Island, Canada, two sections of the border between Northwest Territories and Nunavut. 60 ° N In Canada, the southern border of Yukon with the northern border of British Columbia ; the southern border of Northwest Territories with the northern borders of British Columbia, Alberta and Saskatchewan ; and the southern border of mainland Nunavut with the northern border of Manitoba, leading to the expression `` north of sixty '' for the territories. 54 ° 40'N The border between 19th century Russian territories to the north and conflicting American and British land claims in western North America. The conflicting claims led to the Oregon boundary dispute between Britain and the United States, giving rise to the slogan `` Fifty - four forty or fight. '' 52 ° N In Canada, part of the border between Newfoundland and Labrador and Quebec. 51 ° N The southern limit of Russian America from 1799 to 1821. 49 ° N Much of the border between Canada and the United States, from British Columbia to Manitoba ; `` 49th parallel '' is a common expression for the border, though the majority of Canada 's population actually lives south of the parallel. 48 ° N In Canada, part of the border between Quebec and New Brunswick. 46 ° N In the United States, part of the border between Washington and Oregon. 45 ° N Part of the border between Canada ( Quebec ) and the USA ( New York and Vermont ) is approximated by the parallel. Also, in the USA, it approximates most of the border between Montana and Wyoming. 43 ° 30'N In the USA, the border between Minnesota and Iowa. 43 ° N In the USA, much of the border between South Dakota and Nebraska. 42 ° 30'N In the USA, the border between Wisconsin and Illinois. 42 ° N Originally the northward limit of New Spain. In the USA, the southern borders of Oregon and Idaho where they meet the northern borders of California, Nevada and Utah. The parallel also defines much of the border between Pennsylvania and New York. 41 ° N In the USA, part of the border between Wyoming and Utah, the border between Wyoming and Colorado, and part of the border between Nebraska and Colorado. 40 ° N In the USA, the border between Nebraska and Kansas. The parallel was originally chosen for the Mason -- Dixon line, but the line was moved several miles south to avoid bisecting the city of Philadelphia. 38 ° N The boundary between the Soviet and American occupation zones in Korea, and later between North Korea and South Korea, from 1945 until the Korean War ( 1950 -- 1953 ). 37 ° N In the USA, the southern border of Utah with the northern border of Arizona. The southern border of Colorado with the northern borders of New Mexico and Oklahoma. The southern border of Kansas with the northern border of Oklahoma. 36 ° 30'N The historic Missouri Compromise line. In the USA, defines part of the border between Oklahoma and Texas, most of the border between Missouri and Arkansas. Geographically it is a Westward extension of the border between Virginia and North Carolina and part of the border between Kentucky and Tennessee. 36 ° N In the USA, a short section of the border between the Missouri Bootheel and Arkansas. 35 ° N In the USA, the southern border of Tennessee, which meets Mississippi, Alabama and Georgia. Also, part of the border between North Carolina and Georgia. 33 ° N In the USA, the southern border of Arkansas, which meets the northern border of Louisiana, is approximated by the parallel. Historically, it defined the southern border of the Louisiana Territory. 32 ° N In the USA, part of the border between New Mexico and Texas. 31 ° 20'N Part of the border between the USA and Mexico ( Sonora and Chihuahua ) ; the southern border of Arizona and the New Mexico Bootheel. 31 ° N Part of the border between Iran and Iraq. In the USA, part of the border between Mississippi and Louisiana, and part of the border between Alabama and Florida. 28 ° N In Mexico, the border between Baja California and Baja California Sur. 26 ° N Part of the border between Western Sahara ( claimed by Morocco ) and Mauritania. 25 ° N Part of the border between Mauritania and Mali. 22 ° N Much of the border between Egypt and Sudan, partly disputed ( see also Hala'ib Triangle ). 20 ° N A short section of the border between Libya and Sudan, and within Sudan, the northern border of the Darfur region. 17 ° N The division between Republic of Vietnam ( South Vietnam ) and Democratic Republic of Vietnam ( North Vietnam ) during the Vietnam War. 15 ° N de facto maritime border between Honduras and Nicaragua. 13 ° 05'N Part of the border between Chad and Cameroon, over a stretch of 41.6 km, partly in Lake Chad 10 ° N Part of the border between Guinea and Sierra Leone. 8 ° N Part of the border between Somalia and Ethiopia. 1 ° N Part of the border between Equatorial Guinea and Gabon. 1 ° S Most of the border between Uganda and Tanzania, and a very short section of the border between Kenya and Tanzania in Lake Victoria. 7 ° S A short section of the border between Democratic Republic of the Congo and Angola. 8 ° S Two short sections of the border between Democratic Republic of the Congo and Angola. 10 ° S A short section of the border between Brazil and Peru. 13 ° S Part of the border between Angola and Zambia. 16 ° S Part of the border between Mozambique and Zimbabwe. 22 ° S A short section of the border between Namibia and Botswana, and parts of the border between Bolivia and Argentina. 26 ° S In Australia, the border between South Australia and the Northern Territory, and part of the border between South Australia and Queensland. 28 ° S In Argentina, the border between Chaco Province and Santa Fe Province. 29 ° S In Australia, much of the border between Queensland and New South Wales. 35 ° S In Argentina, part of the border between Córdoba Province and La Pampa Province. 36 ° S In Argentina, part of the border between Mendoza Province and La Pampa Province, and part of the border between San Luis Province and La Pampa Province. 42 ° S In Argentina, the border between Río Negro Province and Chubut Province. 46 ° S In Argentina, the border between Chubut Province and Santa Cruz Province. 52 ° S Part of the border between Argentina and Chile. 60 ° S The northern boundary of Antarctica for the purposes of the Antarctic Treaty System ( see map ). The northern boundary of the Southern Ocean. Altitude Note that the features of the spheroid cross-section ( orange ) in this image are exaggerated with respect to the Earth. Altitude has an effect on a location 's position relative to the plane formed by a circle of latitude. Since altitude is determined by the normal to the Earth 's surface, locations sharing the same latitude -- but having different elevations ( e.g., lying along this normal ) -- no longer lie within this plane. Rather, all points sharing the same latitude and of varying elevation occupy a cone formed by the rotation of this normal around the Earth 's axis. See also List of circles of latitude References Jump up ^ `` ' ' Trópico en movimiento ' ' ( in Spanish ) ''. Groups.google.com. Retrieved 2014 - 05 - 13. Jump up ^ `` Basics of Space Flight, Chapter 2 ''. Jet Propulsion Laboratory. Jet Propulsion Laboratory / NASA. 2013 - 10 - 29. Retrieved 2015 - 03 - 26. Jump up ^ `` Maritime Delimitation between Nicaragua and Honduras in the Caribbean Sea ( Nicaragua v. Honduras ) '' ( PDF ). Retrieved 2014 - 05 - 13. External links Wikimedia Commons has media related to Latitudes. U.S. Naval Observatory - mean obliquity of the ecliptic 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 Ancient Greek astronomy Astronomers Aglaonice Agrippa Anaximander Andronicus Apollonius Aratus Aristarchus Aristyllus Attalus Autolycus Bion Callippus Cleomedes Cleostratus Conon Eratosthenes Euctemon Eudoxus Geminus Heraclides Hicetas Hipparchus Hippocrates of Chios Hypsicles Menelaus Meton Oenopides Philip of Opus Philolaus Posidonius Ptolemy Pytheas Seleucus Sosigenes of Alexandria Sosigenes the Peripatetic Strabo Thales Theodosius Theon of Alexandria Theon of Smyrna Timocharis Works Almagest ( Ptolemy ) On Sizes and Distances ( Hipparchus ) On the Sizes and Distances ( Aristarchus ) On the Heavens ( Aristotle ) Instruments Antikythera mechanism Armillary sphere Astrolabe Dioptra Equatorial ring Gnomon Mural instrument Triquetrum Concepts Callippic cycle Celestial spheres Circle of latitude Counter-Earth Deferent and epicycle Equant Geocentrism Heliocentrism Hipparchic cycle Metonic cycle Octaeteris Solstice Spherical Earth Sublunary sphere Zodiac Influences Babylonian astronomy Egyptian astronomy Influenced Medieval European science Indian astronomy Medieval Islamic astronomy Retrieved from `` https://en.wikipedia.org/w/index.php?title=Circle_of_latitude&oldid=815887154 '' Categories : Lines of latitude Hidden categories : Articles needing additional references from April 2012 All articles needing additional references Talk Contents About Wikipedia Asturianu Azərbaycanca Башҡортса Беларуская Беларуская ( тарашкевіца ) ‎ Български Català Čeština Dansk Deutsch Dolnoserbski Eesti Ελληνικά Español Euskara فارسی Français Frysk Galego 한국어 Հայերեն Hornjoserbsce Hrvatski Ilokano Italiano ქართული Кыргызча Latina Latviešu Lëtzebuergesch Lumbaart Magyar Македонски मराठी Bahasa Melayu Nederlands 日本 語 Occitan Polski Português Русский Scots Simple English Slovenčina Slovenščina Српски / srpski Srpskohrvatski / српскохрватски Suomi ไทย Українська Tiếng Việt Winaray 中文 Edit links This page was last edited on 17 December 2017, at 21 : 12. 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Question: what are the 5 major circles of latitude
Answer: Arctic Circle