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In geography, a pole of inaccessibility is the farthest (or most difficult to reach) location in a given landmass, sea, or other topographical feature, starting from a given boundary, relative to a given criterion. A geographical criterion of inaccessibility marks a location that is the most challenging to reach according to that criterion. Often it refers to the most distant point from the coastline, implying the farthest point into a landmass from the shore, or the farthest point into a body of water from the shore. In these cases, a pole of inaccessibility is the center of a maximally large circle that can be drawn within an area of interest only touching but not crossing a coastline. Where a coast is imprecisely defined, the pole will be similarly imprecise.
Northern pole of inaccessibilityEdit
The northern pole of inaccessibility, sometimes known as the Arctic pole, is located on the Arctic Ocean pack ice at a distance farthest from any landmass. The original position was wrongly believed to lie at 84°3′N 174°51′W. It is not clear who first defined this point, but it may have been Sir Hubert Wilkins, who wished to traverse the Arctic Ocean by aircraft in 1927. He was finally successful in 1928. In 1968 Sir Wally Herbert came very close to reaching what was then considered to be the position by dogsled, but by his own account, Across the Top of the World, did not make it due to the flow of sea ice.<ref>Template:Cite book</ref> In 1986, an expedition of Soviet polar scientists led by Dmitry Shparo claimed to reach the original position by foot during a polar night.Template:Citation needed
In 2005, explorer Jim McNeill asked scientists from The National Snow and Ice Data Center and Scott Polar Research Institute to re-establish the position using modern GPS and satellite technology. This was published as a paper in the Polar Record, Cambridge University Press in 2013.<ref name="Rees2014" /> McNeill launched his own, unsuccessful attempt to reach the new position in 2006, while measuring the depth of sea-ice for NASA.<ref>Template:Cite news</ref> In 2010 he and his Ice Warrior team were thwarted again by the poor condition of the sea ice.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The new position lies at Template:Coord, Template:Convert from the three closest landmasses: Henrietta Island in the De Long Islands, at Arctic Cape on Severnaya Zemlya, and on Ellesmere Island. It is over Template:Convert from the originally accepted position.<ref>Template:Cite journal</ref> Due to constant motion of the pack ice, no permanent structure can exist at this pole. On 12 September 2024, the French icebreaking cruise ship Le Commandant Charcot became the first ship to reach the Northern Pole of Inaccessibility.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Southern pole of inaccessibilityEdit
The southern pole of inaccessibility is the point on the Antarctic continent most distant from the Southern Ocean. A variety of coordinate locations have been given for this pole. The discrepancies are due to the question of whether the "coast" is measured to the grounding line or the edges of ice shelves, the difficulty of determining the location of the "solid" coastline, the movement of ice sheets and improvements in the accuracy of survey data over the years, as well as possible topographical errors.
The point commonly referred to as the pole of inaccessibility is the site of the Soviet Union research station mentioned below, which was constructed at Template:Coord<ref name = meteorological>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> (though some sources give Template:Coord<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>). This lies Template:Convert from the South Pole, at an elevation of Template:Convert. Using different criteria, the Scott Polar Research Institute locates this pole at Template:Coord.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Using recent datasets and cross-confirmation between the adaptive gridding and B9-Hillclimbing<ref name="Barnes2019"/> methods discussed below, Rees et al. (2021)<ref name="Rees2021"/> identify two poles of inaccessibility for Antarctica: an "outer" pole defined by the edge of Antarctica's floating ice shelves and an "inner" pole defined by the grounding lines of these sheets. They find the Outer pole to be at Template:Coord, Template:Convert from the ocean, and the Inner pole to be at Template:Coord, Template:Convert from the grounding lines.
The southern pole of inaccessibility is far more remote and difficult to reach than the geographic South Pole. On 14 December 1958, the 3rd Soviet Antarctic Expedition for International Geophysical Year research work, led by Yevgeny Tolstikov, established the temporary Pole of Inaccessibility Station (Template:Langx, Template:Transliteration) at Template:Coord. A second Russian team returned there in 1967. Today, a building still remains at this location, marked by a bust of Vladimir Lenin that faces towards Moscow, and protected as a historical site.
On 11 December 2005, at 7:57 UTC, Ramón Hernando de Larramendi, Juan Manuel Viu, and Ignacio Oficialdegui, members of the Spanish Transantarctic Expedition, reached for the first time in history the southern pole of inaccessibility at Template:Coord, updated that year by the British Antarctic Survey. The team continued their journey towards the second southern pole of inaccessibility, the one that accounts for the ice shelves as well as the continental land, and they were the first expedition to reach it, on 14 December 2005, at Template:Coord. Both achievements took place within an ambitious pioneer crossing of the eastern Antarctic Plateau that started at Novolazarevskaya Station and ended at Progress Base after more than Template:Convert. This was the fastest polar journey ever achieved without mechanical aid, with an average rate of around Template:Convert per day and a maximum of Template:Convert per day, using kites as their power source.<ref name="thepoles.com">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
On 4 December 2006, Team N2i, consisting of Henry Cookson, Rupert Longsdon, Rory Sweet and Paul Landry, embarked on an expedition to be the first to reach the historic pole of inaccessibility location without direct mechanical assistance, using a combination of traditional man hauling and kite skiing. The team reached the old abandoned station on 19 January 2007, rediscovering the forgotten statue of Lenin left there by the Soviets some 48 years previously.<ref name="teamn2i">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The team found that only the bust on top of the building remained visible; the rest was buried under the snow.<ref name="BBC" /> The explorers were picked up from the spot by a plane from Vostok base, flown to Progress Base and taken back to Cape Town on the Akademik Fyodorov, a Russian polar research vessel.<ref name="BBC">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
On 27 December 2011, Sebastian Copeland and partner Eric McNair-Laundry also reached the Template:Coord southern pole of inaccessibility. They were the first to do so without resupply or mechanical support, departing from Novolazarevskaya Station on their way to the South Pole to complete the first East/West crossing of Antarctica through both poles, over Template:Cvt.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
As mentioned above, due to improvements in technology and the position of the continental edge of Antarctica being debated, the exact position of the best estimate of the pole of inaccessibility may vary. However, for the convenience of sport expeditions, a fixed point is preferred, and the Soviet station has been used for this role. This has been recognized by Guinness World Records for Team N2i's expedition in 2006–2007.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>Template:Better source needed
Oceanic pole of inaccessibilityEdit
The oceanic pole of inaccessibility, also known as Point Nemo, is located at roughly Template:Coord<ref name="Where is Point Nemo">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> and is the place in the ocean that is farthest from land. It represents the solution to the "longest swim" problem.<ref name="Point Nemo, revisited">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The problem entails finding such a place in the world ocean where, if a person fell overboard while on a ship at sea, they would be as far away from any land in any direction as possible. It lies in the South Pacific Ocean, and is equally distant from the three closest land vertices which are each roughly Template:Convert away. Those vertices are Pandora Islet of the Ducie Island atoll (an island of the Pitcairn Islands) to the north; Motu Nui (adjacent to Easter Island) to the northeast; and Maher Island (near the larger Siple Island, off the coast of Marie Byrd Land, Antarctica) to the south.<ref name="Where is Point Nemo"/> The exact coordinates of Point Nemo depend on what the exact coordinates of these three islands are, since the nature of the "longest swim" problem means that the ocean point is equally far from each.<ref name="Point Nemo, revisited"/>
The three nearest land points are Template:Convert away from Point Nemo, but on a map, the three islands nearest will be listed at slightly different distances, because maps list the distance to the center of each respective island instead of each of the exact coastal points on the islands used to calculate Point Nemo.
The area is so remote that, since no regular marine or air traffic routes are within Template:Convert, sometimes the closest human beings are astronauts aboard the International Space Station when it passes overhead.<ref name="pointnemo"/><ref name=Plastic>Template:Cite news</ref>
The antipode of Point Nemo – the point on the surface of the Earth that is diametrically opposite of it – is located at roughly Template:Coord, in the Aktobe region of western Kazakhstan, roughly 50 km (30 miles) SSE of the town of Shubarkuduk.
Point Nemo is relatively lifeless; its location within the South Pacific Gyre blocks nutrients from reaching the area, and being so far from land it gets little nutrient run-off from coastal waters.<ref name="pointnemo">Template:Cite news</ref>
To the west the region of the South Pacific Ocean is also the site of the geographic center of the water hemisphere, at Template:Coord near New Zealand's Bounty Islands. The geographic center of the Pacific Ocean lies further north-west where the Line Islands begin, west from Starbuck Island at Template:Coord.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
HistoryEdit
Point Nemo was first identified by Croatian survey engineer Template:Ill in 1992.<ref name=Plastic/> In 2022, Lukatela recalculated the coordinates of Point Nemo using OpenStreetMap data and Google Maps data in order to compare those results with the coordinates he first calculated using Digital Chart of the World data.<ref name="Point Nemo, revisited"/>
The point and the areas around it have attracted literary and cultural attention, and the point has become known as Point Nemo, which is Latin for "nobody" and a reference to Jules Verne's Captain Nemo from the 1870 novel Twenty Thousand Leagues Under the Seas.<ref name="pointnemo" /><ref name="Where is Point Nemo"/> The novel was a childhood favorite of Lukatela's, and such, he named the point after Captain Nemo.<ref name="Where is Point Nemo"/><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The general area plays a major role in the 1928 short story "The Call of Cthulhu" by H. P. Lovecraft, as holding the location of the fictional city of R'lyeh, although this story was written 66 years before the identification of Point Nemo.<ref name="pointnemo" />
The wider area is also known as a "spacecraft cemetery", because hundreds of decommissioned satellites, space stations, and other spacecraft have been made to fall there upon re-entering the atmosphere, to lessen the risk of hitting inhabited locations<ref>Template:Cite magazine</ref> or maritime traffic. The International Space Station (ISS) is planned to crash into Point Nemo in 2031.<ref>Template:Cite news</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Continental poles of inaccessibilityEdit
EurasiaEdit
Template:Multiple image The Eurasian pole of inaccessibility (EPIA) is located in northwestern China, near the Kazakhstan border. It is also the furthest possible point on land from the ocean anywhere on Earth.
However, Eurasia (or even Asia alone) being the largest continent does not necessarily mean that its pole of inaccessibility is the furthest from the ocean anywhere.
Earlier calculations suggested that it is Template:Convert from the nearest coastline, located at Template:Coord, approximately Template:Convert north of the city of Ürümqi, in the Xinjiang Autonomous Region of China, in the Gurbantünggüt Desert. The nearest settlements to this location are Hoxtolgay Town at Template:Coord, about Template:Convert to the northwest, Xazgat Township (Template:Lang-zh) at Template:Coord, about Template:Convert to the west, and Suluk at Template:Coord, about Template:Convert to the east.Template:Citation needed
However, the previous pole location disregards the Gulf of Ob as part of the oceans, and a 2007 study<ref name="Garcia2007"/> proposes two other locations as the ones farther from any ocean (within the uncertainty of coastline definition): EPIA1 Template:Coord and EPIA2 Template:Coord, located respectively at 2,510±10 km (1,560±6 mi) and 2,514±7 km (1,562±4 mi) from the oceans.<ref name="Garcia2007" /> These points lie in a close triangle about the Dzungarian Gate, a significant historical gateway to migration between the East and West. EPIA2 is located near a settlement called K̂as K̂îr Su in a region named K̂îzîlk̂um (قىزىلقۇم) in the Template:Ill, Burultokay County.
Elsewhere in Xinjiang, the location Template:Coord in the southwestern suburbs of Ürümqi (Ürümqi County) was designated by local geography experts as the "center point of Asia" in 1992, and a monument to this effect was erected there in the 1990s. The site is a local tourist attraction.<ref name="confluence">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Coincidentally, the continental and oceanic poles of inaccessibility have a similar radius; the Eurasian poles EPIA1 and EPIA2 are about Template:Convert closer to the ocean than the oceanic pole is to land.
AfricaEdit
In Africa, the pole of inaccessibility is at Template:Coord, Template:Convert from the coast,<ref name="Garcia2007" /> near the town of Obo in the Central African Republic and close to the country's tripoint with South Sudan and the Democratic Republic of the Congo.
North AmericaEdit
In North America, the continental pole of inaccessibility is on the Pine Ridge Reservation in southwest South Dakota about Template:Convert north of the town of Allen, Template:Convert from the nearest coastline at Template:Coord.<ref name="Garcia2007" /> The first documented visit was in 2014 by two travelers and a local resident.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The pole was marked in 2021 with a marker that represents the 7 Lakota Values and the four colors of the Lakota Medicine Wheel.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
South AmericaEdit
In South America, the continental pole of inaccessibility is in Brazil at Template:Coord, near Arenápolis, Mato Grosso,<ref name="Garcia2007" /> Template:Convert from the nearest coastline. In 2017, the Turner Twins went from coastal Chile to the South American Pole of Inaccessibility, becoming the first adventurers to go from the nearest coastline to the pole by foot.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> In 2019, it was discovered that there is a second South American pole of inaccessibility to the north, its position varying greatly between the two coastline datasets used.<ref name="Barnes2019"/>
AustraliaEdit
In Australia, the continental pole of inaccessibility is located at Template:Coord<ref name="Garcia2007" /> Template:Convert from the nearest coastline, approximately 161 km (100 miles) west-northwest of Alice Springs. The nearest town is Papunya, Northern Territory, about Template:Convert west-southwest of the pole.
Methods of calculationEdit
As detailed below, several factors determine how a pole is calculated using computer modeling.
Poles are calculated with respect to a particular coastline dataset. Currently used datasets are the GSHHG (Global Self-consistent, Hierarchical, High-resolution Geography Database)<ref name="GSHHG"/> as well as OpenStreetMap (OSM) planet dumps. The GSHHG claims 500-meter precision for 90% of identifiable coastal features, while the volunteer-build OSM give no such guarantee but nevertheless "have characteristics suggesting accuracy".<ref name="Barnes2019"/>
Next, a distance function must be determined for calculating distances between coastlines and potential Poles. Some works tended to project data onto planes or perform spherical calculations; more recently, other works have used different algorithms and high-performance computing with ellipsoidal calculations.<ref name="Barnes2019"/>
Finally, an optimization algorithm must be developed. Several works<ref name="Garcia2007"/><ref name="Rees2014"/> use the 2007 adaptive grid method of Garcia-Castellanos and Lombardo. In this method, a rectangular grid of, e.g., 21×21 points is created. Each point's distance from the coastline is determined and the point farthest from the coast identified. The grid is then recentered on this point and shrunk by some factor. This process iterates until the grid becomes very small (e.g. at 100-meter precision).<ref name="Rees2014"/> Some authors claim this method could sink into a local minimum.<ref name="Rees2021"/> A more recent method from 2019, B9-Hillclimbing by Barnes, uses a polyhedron in 3D space to find initial points evenly spaced by 100 kilometers. These points are then grouped; the more "unique" points are subject to numerical optimization (hill climbing, simulated annealing) for the farthest distance, accelerated by a 3D Cartesian point cloud.<ref name="Barnes2019"/> Rees (2021) shows that the two methods agree with each other to meter level.<ref name="Rees2021"/>
To date there has been no meta-study of the various works, and the algorithms and datasets they use. However, successive works have compared themselves with previous calculations and claimed improvement. For example, the GC & L article from 2007 was able to find hundred-kilometer errors in the "traditional" Eurasian PIA in Crane & Crane, 1987.<ref name="Garcia2007"/> Rees using the same method updated the arctic PIA by over 200 kilometers.<ref name="Rees2014"/> Barnes, which improved upon the method and the dataset used, was able to improve the GC & L South American PIA by 50 kilometers, showing that bad coastline data caused an error of 57 kilometers in their reported PIA-to-coast distance.<ref name="Barnes2019"/>
List of poles of inaccessibilityEdit
Poles of Inaccessibility, as determined by some authors, are listed in the table below. This list is incomplete and may not capture all works done to date.
| Pole | Location | Distance from coast (km) |
Dataset | Projection | Method | Reference | |
|---|---|---|---|---|---|---|---|
| Africa | Template:Coord | 1,814 | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| Africa | Template:Coord | 1,814.5158 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Africa | Template:Coord | 1,815.4150 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Antarctica | Template:Coord | 1,301 | ? Traditional | ? | ? | Soviet site (1958)<ref name="meteorological" /> | |
| Antarctica | Template:Coord | 1,136.2129 | GSHHG v2.3.6 (L1+L6). Erroneous. | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Antarctica | Template:Coord | 1,273.2928 | GSHHG v2.3.6 (L1+L5). Erroneous. | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Antarctica | Template:Coord | 1,590.36 | ADDv7.2 "Outer" | WGS84 | B9-Hillclimbing | Rees (2021)<ref name="Rees2021"/> | |
| Antarctica | Template:Coord | 1,179.40 | ADDv7.2 "Inner" | WGS84 | B9-Hillclimbing | Rees (2021)<ref name="Rees2021"/> | |
| Arctic Pole | Template:Coord | 1,008 | GSHHG 2014 | WGS84 | Adaptive Grid | Rees (2014)<ref name="Rees2014" /> | |
| Arctic Pole | Template:Coord | 1,008.9112 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Arctic Pole | Template:Coord | 1,007.6777 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Atlantic Ocean | Template:Coord | 2,033.8849 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Atlantic Ocean | Template:Coord | 2,033.5187 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Australia | Template:Coord | 928Template:NoteTag | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| Australia | Template:Coord | not claimed | SF53-13 | ? | Planar map | citation | CitationClass=web
}}</ref> |
| Australia | Template:Coord | 925.4459 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Australia | Template:Coord | 921.9290 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Eurasia 1 | Template:Coord | 2,514 | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| Eurasia 1 | Template:Coord | 2,513.9415 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Eurasia 1 | Template:Coord | 2,509.9536 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Eurasia 2 | Template:Coord | 2,510 | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| Eurasia 2 | Template:Coord | 2,509.9685 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Eurasia 2 | Template:Coord | 2,505.2134 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Great Britain | Template:Coord | 108 | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| Great Britain | Template:Coord | 114.4462 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Great Britain | Template:Coord | 108.0925 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Greenland | Template:Coord | 469 | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| Greenland | Template:Coord | 471.9905 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Greenland | Template:Coord | 474.2257 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Indian Ocean | Template:Coord | 1,940.8913 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Indian Ocean | Template:Coord | 1,943.3848 | GSHHG L1 | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Madagascar | Template:Coord | 260 | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| Madagascar | Template:Coord | 259.5957 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Madagascar | Template:Coord | 264.0657 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| North America | Template:Coord | 1,639Template:NoteTag | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| North America | Template:Coord | 1,639.6549 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| North America | Template:Coord | 1,643.7562 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Pacific Ocean (Point Nemo) | Template:Coord | 2,690 | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| Pacific Ocean (Point Nemo) | Template:Coord | 2,701.1721 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| Pacific Ocean (Point Nemo) | Template:Coord | 2,704.7991 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| South America | Template:Coord | 1,517Template:NoteTag | GSHHS 1996 | Sphere | Adaptive Grid | Garcia-Castellanos (2007)<ref name="Garcia2007"/> | |
| South America 1 | Template:Coord | 1,490.5321 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| South America 1 | Template:Coord | 1,511.6636 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| South America 2 | Template:Coord | 1,467.2206 | OpenStreetMap | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> | |
| South America 2 | Template:Coord | 1,476.4901 | GSHHG v2.3.6 (L1) | WGS84 | B9-Hillclimbing | Barnes (2019)<ref name="Barnes2019"/> |
ArcGIS personnel wrote a 2015 page with their calculations based on a flat Earth. The results are too inaccurate to be included here.<ref name="Barnes2019"/>
See alsoEdit
- Antipodes
- Extremes on Earth
- Geographical pole
- Geographical centre
- Land and water hemispheres
- List of mainland settlements that are inaccessible by road
- Pole of Inaccessibility research station