Antarctica

Antarctica is Earth's southernmost continent. It contains the geographic South Pole and is situated in the Antarctic region of the Southern Hemisphere, almost entirely south of the Antarctic Circle, and is surrounded by the Southern Ocean. At 14,200,000 square kilometres (5,500,000 square miles), it is the fifth-largest continent and nearly twice the size of Australia.
 At 0.00008 people per square kilometre, it is by far the least densely
populated continent. About 98% of Antarctica is covered by ice that averages 1.9 km (1.2 mi; 6,200 ft) in thickness, which extends to all but the northernmost reaches of the Antarctic Peninsula.
Antarctica, on average, is the coldest, driest, and windiest continent, and has the highest average elevation of all the continents. Most of Antarctica is a polar desert, with annual precipitation of 20 cm (7.9 in) along the coast and far less inland. The temperature in Antarctica has reached −89.2 °C (−128.6 °F)
 (or even −94.7 °C (−135.8 °F) as measured from space ), though the
average for the third quarter (the coldest part of the year) is −63 °C
(−81 °F). Anywhere from 1,000 to 5,000 people reside throughout the year
 at research stations scattered across the continent. Organisms native to Antarctica include many types of algae, bacteria, fungi, plants, protista, and certain animals, such as mites, nematodes, penguins, seals and tardigrades. Vegetation, where it occurs, is tundra.
Antarctica is noted as the last region on Earth in recorded history to be discovered, unseen until 1820 when the Russian expedition of Fabian Gottlieb von Bellingshausen and Mikhail Lazarev on Vostok and Mirny sighted the Fimbul ice shelf.
 The continent, however, remained largely neglected for the rest of the
19th century because of its hostile environment, lack of easily
accessible resources, and isolation. In 1895, the first confirmed
landing was conducted by a team of Norwegians.

The name Antarctica is the romanised version of the Greek compound word ἀνταρκτική (antarktiké), feminine of ἀνταρκτικός (antarktikós), meaning "opposite to the Arctic", "opposite to the north".
Aristotle wrote in his book Meteorology about an Antarctic region in c. 350 BC. Marinus of Tyre reportedly used the name in his unpreserved world map from the 2nd century CE. The Roman authors Hyginus and Apuleius (1–2 centuries CE) used for the South Pole the romanised Greek name polus antarcticus, from which derived the Old French pole antartike (modern pôle antarctique) attested in 1270, and from there the Middle English pol antartik in a 1391 technical treatise by Geoffrey Chaucer (modern Antarctic Pole).
Before
 acquiring its present geographical connotations, the term was used for
other locations that could be defined as "opposite to the north". For
example, the short-lived French colony established in Brazil in the 16th century was called "France Antarctique".
The first formal use of the name "Antarctica" as a continental name in the 1890s is attributed to the Scottish cartographer John George Bartholomew.

The long-imagined (but undiscovered) south polar continent was originally called Terra Australis,
 sometimes shortened to 'Australia' as seen in a woodcut illustration
titled Sphere of the winds, contained in an astrological textbook
published in Frankfurt in 1545. Although the longer Latin phrase was
better known, the shortened name Australia was used in Europe's
scholarly circles.
Then in the nineteenth century, the colonial authorities in Sydney removed the Dutch name from New Holland.
 Instead of inventing a new name to replace it, they took the name
Australia from the south polar continent, leaving it nameless for some
eighty years. During that period, geographers had to make do with clumsy
 phrases such as "the Antarctic Continent". They searched for a more
poetic replacement, suggesting various names such as Ultima and
Antipodea. Eventually Antarctica was adopted in the 1890s.

Antarctica has no indigenous population, and there is no evidence that
it was seen by humans until the 19th century. However, in February 1775,
 during his second voyage, Captain Cook
 called the existence of such a polar continent "probable" and in
another copy of his journal he wrote: "[I] firmly believe it and it's
more than probable that we have seen a part of it".
However, belief in the existence of a Terra Australis—a vast continent in the far south of the globe to "balance" the northern lands of Europe, Asia and North Africa—had prevailed since the times of Ptolemy
 in the 1st century AD. Even in the late 17th century, after explorers
had found that South America and Australia were not part of the fabled
"Antarctica", geographers believed that the continent was much larger
than its actual size. Integral to the story of the origin of
Antarctica's name is that it was not named Terra Australis—this name was
 given to Australia instead, because of the misconception that no significant landmass could exist further south. Explorer Matthew Flinders,
 in particular, has been credited with popularising the transfer of the
name Terra Australis to Australia. He justified the titling of his book A Voyage to Terra Australis (1814) by writing in the introduction:
There
 is no probability, that any other detached body of land, of nearly
equal extent, will ever be found in a more southern latitude; the name
Terra Australis will, therefore, remain descriptive of the geographical
importance of this country and of its situation on the globe: it has
antiquity to recommend it; and, having no reference to either of the two
 claiming nations, appears to be less objectionable than any other which
 could have been selected.
European maps continued to show this hypothesised land until Captain James Cook's ships, HMS Resolution and Adventure, crossed the Antarctic Circle on 17 January 1773, in December 1773 and again…

Positioned asymmetrically around the South Pole and largely south of the Antarctic Circle, Antarctica is the southernmost continent and is surrounded by the Southern Ocean; alternatively, it may be considered to be surrounded by the southern Pacific, Atlantic, and Indian Oceans, or by the southern waters of the World Ocean. There are a number of rivers and lakes in Antarctica, the longest river being the Onyx. The largest lake, Vostok,
 is one of the largest sub-glacial lakes in the world. Antarctica covers
 more than 14 million km (5,400,000 sq mi), making it the
fifth-largest continent, about 1.3 times as large as Europe. The
coastline measures 17,968 km (11,165 mi) and is mostly characterised by
 ice formations, as the following table shows:
Antarctica is divided in two by the Transantarctic Mountains close to the neck between the Ross Sea and the Weddell Sea.
 The portion west of the Weddell Sea and east of the Ross Sea is called
West Antarctica and the remainder East Antarctica, because they roughly
correspond to the Western and Eastern Hemispheres relative to the Greenwich meridian.
About 98% of Antarctica is covered by the Antarctic ice sheet, a sheet of ice averaging at least 1.6 km (1.0 mi) thick. The continent has about 90% of the world's ice (and thereby about 70% of the world's fresh water). If all of this ice were melted, sea levels would rise about 60 m (200 ft). In most of the interior of the continent, precipitation is very low, down to 20 mm (0.8 in) per year; in a few "blue ice" areas precipitation is lower than mass loss by sublimation, and so the local mass balance is negative. In the dry valleys, the same effect occurs over a rock base, leading to a desiccated landscape.
West Antarctica is covered by the West Antarctic Ice Sheet. The sheet has been of recent concern because of the small possibility of its collapse. If the sheet were to break down, ocean levelswould rise …

Geological history and palaeontology
More than 170 million years ago, Antarctica was part of the supercontinent Gondwana.
 Over time, Gondwana gradually broke apart, and Antarctica as we know it
 today was formed around 25 million years ago. Antarctica was not always
 cold, dry, and covered in ice sheets. At a number of points in its long
 history, it was farther north, experienced a tropical or temperate
climate, was covered in forests, and inhabited by various ancient life
forms.
Palaeozoic era (540–250 Ma)
During the Cambrian period, Gondwana had a mild climate. West Antarctica was partially in the Northern Hemisphere, and during this period large amounts of sandstones, limestones and shales were deposited. East Antarctica was at the equator, where sea floor invertebrates and trilobites flourished in the tropical seas. By the start of the Devonian period (416 Ma), Gondwana was in more southern latitudes and the climate was cooler, though fossils of land plants are known from this time. Sand and silts were laid down in what is now the Ellsworth, Horlick and Pensacola Mountains. Glaciation began at the end of the Devonian period (360 Ma), as Gondwana became centred on the South Pole and the climate cooled, though flora remained. During the Permian period, the land became dominated by seed plants such as Glossopteris, a pteridosperm which grew in swamps. Over time these swamps became deposits of coal in the Transantarctic Mountains. Towards the end of the Permian period, continued warming led to a dry, hot climate over much of Gondwana.
Mesozoic era (250–66 Ma)
As a result of continued warming, the polar ice caps melted and much of Gondwana became a desert.

Antarctica is the coldest of Earth's
 continents. It used to be ice-free until about 34 million years ago,
when it became covered with ice. The coldest natural air temperature
ever recorded on Earth was −89.2 °C (−128.6 °F) at the Russian Vostok Station in Antarctica on 21 July 1983. For comparison, this is 10.7 °C (20 °F) colder than subliming dry ice
 at one atmosphere of partial pressure, but since CO2 only makes up
0.039% of air, temperatures of less than −140 °C (−220 °F) would be
needed to produce dry ice snow in Antarctica. A lower air temperature of
 −94.7 °C (−138.5 °F) was recorded in 2010 by satellite—however, it may
be influenced by ground temperatures and was not recorded at a height of
 7 feet (2 m) above the surface as required for the official air
temperature records. Antarctica is a frozen desert with little
precipitation; the South Pole receives less than 10 cm (4 in) per year,
on average. Temperatures reach a minimum of between −80 °C (−112 °F) and
 −89.2 °C (−128.6 °F) in the interior in winter and reach a maximum of
between 5 °C (41 °F) and 15 °C (59 °F) near the coast in summer. Sunburn
 is often a health issue as the snow surface reflects almost all of the
ultraviolet light falling on it. Given the latitude, long periods of
constant darkness or constant sunlight create climates unfamiliar to
human beings in much of the rest of the world.
East Antarctica is colder than its western counterpart because of its higher elevation. Weather fronts
 rarely penetrate far into the continent, leaving the centre cold and
dry. Despite the lack of precipitation over the central portion of the
continent, ice there lasts for extended periods. Heavy snowfalls are
common on the coastal portion of the continent, where snowfalls of up to
 1.22 metres (48 in) in 48 hours have been recorded.
At the edge of the continent, strong katabatic winds off the polar plateau often blow at storm force.

Several governments maintain permanent manned research stations
 on the continent. The number of people conducting and supporting
scientific research and other work on the continent and its nearby
islands varies from about 1,000 in winter to about 5,000 in the summer,
giving it a population density
 between 70 and 350 inhabitants per million square kilometres (180 and
900 per million square miles) at these times. Many of the stations are
staffed year-round, the winter-over personnel typically arriving from
their home countries for a one-year assignment. An Orthodox church—Trinity Church, opened in 2004 at the Russian Bellingshausen Station—is manned year-round by one or two priests, who are similarly rotated every year.
The first semi-permanent inhabitants of regions near Antarctica (areas situated south of the Antarctic Convergence) were British and American sealers who used to spend a year or more on South Georgia, from 1786 onward. During the whaling
 era, which lasted until 1966, the population of that island varied from
 over 1,000 in the summer (over 2,000 in some years) to some 200 in the
winter. Most of the whalers were Norwegian, with an increasing
proportion of Britons. The settlements included Grytviken, Leith Harbour, King Edward Point, Stromness, Husvik, Prince Olav Harbour, Ocean Harbour and Godthul.
 Managers and other senior officers of the whaling stations often lived
together with their families. Among them was the founder of Grytviken,
Captain Carl Anton Larsen, a prominent Norwegian whaler and explorer who, along with his family, adopted British citizenship in 1910.
The first child born in the southern polar region was Norwegian girl Solveig Gunbjørg Jacobsen, born in Grytviken on 8 October 1913, and her birth was registered by the resident British Magistrate of South Georgia. She was a daughter of Fridthjof Jacobsen, the assistant manager of the whaling station, and …