Geography of Antarctica – Wikipedia

Geographic features of Antarctica

The geography of Antarctica is dominated by its south polar location and, thus, by ice. The Antarctic continent, located in the Earth's southern hemisphere, is centered asymmetrically around the South Pole and largely south of the Antarctic Circle. It is washed by the Southern (or Antarctic) Ocean or, depending on definition, the southern Pacific, Atlantic, and Indian Oceans. It has an area of more than 14 millionkm2.

Some 98% of Antarctica is covered by the Antarctic ice sheet, the world's largest ice sheet and also its largest reservoir of fresh water. Averaging at least 1.6km thick, the ice is so massive that it has depressed the continental bedrock in some areas more than 2.5km below sea level; subglacial lakes of liquid water also occur (e.g., Lake Vostok). Ice shelves and rises populate the ice sheet on the periphery.

In September 2018, researchers at the National Geospatial-Intelligence Agency released a high resolution terrain map (detail down to the size of a car, and less in some areas) of Antarctica, named the "Reference Elevation Model of Antarctica" (REMA).[1]

Physically, Antarctica is divided in two by Transantarctic Mountains close to the neck between the Ross Sea and the Weddell Sea. Western Antarctica and Eastern Antarctica correspond roughly to the eastern and western hemispheres relative to the Greenwich meridian. This usage has been regarded as Eurocentric by some, and the alternative terms Lesser Antarctica and Greater Antarctica (respectively) are sometimes preferred.

Lesser Antarctica is covered by the West Antarctic Ice Sheet. There has been some concern about this ice sheet, because there is a small chance that it will collapse. If it does, ocean levels would rise by a few metres in a very short period of time.

Volcanoes that occur underneath glacial ice sheets are known by the term "Glaciovolcanism", or subglacial volcanoes. An article published in 2017 claims that researchers from Edinburgh University recently discovered 91 new volcanoes below the Antarctic ice sheet, adding to the 47 volcanoes that were already known.[2] As of today, there have been 138 possible volcanoes identified in West Antarctica.[3] There is limited knowledge about West Antarctic Volcanoes due to the presence of the West Antarctic Ice Sheet, which heavily covers the West Antarctic Rift System -- a likely hub for volcanic activity.[4] Researchers find it difficult to properly identify volcanic activity due to the comprehensive ice covering.

East Antarctica is significantly larger than West Antarctica, and similarly remains widely unexplored in terms of its volcanic potential. While there are some indications that there is volcanic activity under the East Antarctic Ice Sheet, there is not a significant amount of present information on the subject.

Mount Erebus is one of the most notable sites in the study of Antarctic Volcanism, in that it is the southernmost historically active volcanic site on the planet.[5]

Deception Island is another active Antarctic volcano. It is one of the most protected areas in the Antarctic, given its situation between the South Shetland Islands and the Antarctic Peninsula. As the most active volcano in the Antarctic peninsula, it has been studied closely since its initial discovery in 1820.

There are four volcanoes on the mainland of Antarctica that areconsidered to be active on the basis of observed fumarolic activity or "recent" tephra deposits: Mount Melbourne (2,730 m) (7421'S., 16442'E.), a stratovolcano; Mount Berlin (3,500 m) (7603'S., 13552'W.), a stratovolcano; Mount Kauffman (2,365 m) (7537'S., 13225'W.), a stratovolcano; and Mount Hampton (3,325 m) (7629'S., 12548'W.), a volcanic caldera.Mount Rittmann (2,600 m) (73.45S 165.5 E), a volcanic caldera.

Several volcanoes on offshore islands have records of historic activity.Mount Erebus (3,795 m), a stratovolcano onRoss Island with 10 known eruptions and 1 suspected eruption.On the opposite side of the continent, Deception Island(6257'S., 6038'W.), a volcanic caldera with 10 knownand 4 suspected eruptions, have been the most active.Buckle Island in the Balleny Islands (6650'S., 16312'E.), Penguin Island (6206'S., 5754'W.), Paulet Island (6335'S., 5547'W.), and Lindenberg Island (6455'S., 5940'W.) are also considered to be active. In 2017, the researchers of Edinburgh University discovered 91 underwater volcanoes under West Antarctica.[6][7]

The definition of Glaciovolcanism is the interactions of magma with ice in all its forms, including snow, firn and any meltwater.[8] It defines a special field of volcanic that is specifically centered around ice and ice melt. This field of science is less than 100 years old, and thus continuously makes new discoveries. Glaciovolcanism is characterized by three kinds of eruptions: sub-glacial eruptions, supraglacial volcanism, and ice-marginal volcanism.[9]

The study of glaciovolcanism is vital to the understanding of ice sheet formation. It is also a valuable tool to predict volcanic hazards, such as the ash hazard following the Eyjafjallajkull eruption in Iceland.

The Marie Byrd Land is an incredibly large portion of West Antarctica, consisting of the Area below the Antarctic Peninsula. The Marie Byrd land is a large formation of volcanic rock, characterized by 18 exposed and subglacial volcanoes. 16 of the 18 volcanoes are entirely covered by the antarctic ice sheet.[10] There have been no eruptions recorded from any of the volcanoes in this area, however scientists believe that some of the volcanoes may be potentially active.

Scientists and researchers debate whether or not the 138 identified possible volcanoes are active or dormant. It is very hard to definitively say, given that many of these volcanic structures are buried underneath several kilometers of ice.[11] However, ash layers within the West Antarctic Ice Sheet,[12] as well as deformations in the ice surface[13] indicate that the West Antarctic Rift System could be active and contain erupting volcanoes. Additionally, seismic activity in the region hints at magma movement beneath the crust, a sign of volcanic activity.[14] Despite this, however, there is not yet definitive evidence of presently active volcanoes.

Subglacial volcanism is often characterized by ice melt and subglacial water.[15] Though there are other sources of subglacial water, such as geothermal heat, it almost always is a condition of volcanism. Scientists remain uncertain about the presence of water underneath the West Antarctic Ice Sheet, with some claiming to have found evidence indicating the existence.

In West Antarctica's Marie Byrd Land, volcanoes are typically composed of alkaline and basaltic lava. Sometimes, the volcanoes are entirely basaltic in composition. Due to the geographic similarity of the Marie Byrd Land, it is believed that the volcanoes in the West African Rift System are also composed of basalt.[16]

Above-ice basaltic volcanoes, also known as subaerial basaltic volcanoes, generally form in tall, broad cone shapes.[17] Since they are formed from repeated piling of liquid magma sourced from the center, they spread widely and grow upwards relatively slowly.[18] However, West Antarctic Volcanoes form underneath ice sheets, and are thus categorized as subglacial volcanoes. Subglacial volcanoes that are monogenetic are far more narrow, steeper, flat topped structures. Polygenetic subglacial volcanoes have a wider variety of shapes and sizes due to being made up of many different eruptions. Often, they look more cone shaped, like stratovolcanoes.

Little has been studied about the implications of volcanic ash from eruptions within the Antarctic Circle. It is likely that an eruption at lower latitudes would cause global health and aviation hazards due to ash disbursement. The clockwise air circulation around the low pressure system at the South Pole forces air upwards, hypothetically sending ash upwards towards the Stratospheric jet streams, and thus quickly dispersing it throughout the globe.[19]

Recently, in 2017, a study found evidence of subglacial volcanic activity within the West Antarctic Ice Sheet. This activity poses a threat to the stability of the Ice Sheet, as volcanic activity leads to increased melting.[20] This could possibly plunge the West Antarctic Ice Sheet into a positive feedback loop of rising temperatures and increased melting.

There are three vast canyons that run for hundreds of kilometers, cutting through tall mountains. None of the canyons are visible at the snow-covered surface of the continent since they are buried under hundreds of meters of ice. The largest of the canyons is called Foundation Trough and is over 350km long and 35km wide. The Patuxent Trough is more than 300km long and over 15km wide, while the Offset Rift Basin is 150km long and 30km wide. These three troughs all lie under and cross the so-called "ice divide" - the high ice ridge that runs all the way from the South Pole out towards the coast of West Antarctica.[21]

West Antarctica is the smaller part of the continent, (50 180W), divided into:

Larger ice shelves are:

For all ice shelves see List of Antarctic ice shelves.

For a list of all Antarctic islands see List of Antarctic and sub-Antarctic islands.

East Antarctica is the larger part of the continent, (50W 180E), both the South Magnetic Pole and geographic South Pole are situated here. Divided into:

Larger ice shelves are:

For all ice shelves see List of Antarctic ice shelves.

For a list of all Antarctic islands see List of Antarctic and sub-Antarctic islands.

Seven nations have made official Territorial claims in Antarctica.

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Geography of Antarctica - Wikipedia