Geography of Antarctica
| |
Continent | Antarctica |
---|---|
Coordinates | 80°S 90°E / 80°S 90°E |
Area | Ranked 2nd (unofficially) |
• Total | 14,000,000 km2 (5,400,000 sq mi) |
• Land | 98% |
• Water | 2% |
Coastline | 17,968 km (11,165 mi) |
Borders | No land boundaries |
Highest point | Vinson Massif, 4,897 m (16,066 ft) |
Lowest point | Bentley Subglacial Trench, −2,555 m (−8,382.5 ft) |
Longest river | Onyx River, 25 km |
Largest lake | Lake Vostok, 26,000 sq m (est.) |
Climate | subantarctic to antarctic |
Terrain | ice and barren rock |
Natural Resources | krill, fin fish, crab |
Natural Hazards | high winds, blizzards, cyclonic storms, volcanism |
Environmental Issues | depleting ozone layer, rising sea level |
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 million km².
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 1.6 km thick, the ice is so massive that it has depressed the continental bedrock in some areas more than 2.5 km 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]
Regions
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
There are four volcanoes on the mainland of Antarctica that are considered to be active on the basis of observed fumarolic activity or "recent" tephra deposits: Mount Melbourne (2,730 m) (74°21'S., 164°42'E.), a stratovolcano; Mount Berlin (3,500 m) (76°03'S., 135°52'W.), a stratovolcano; Mount Kauffman (2,365 m) (75°37'S., 132°25'W.), a stratovolcano; and Mount Hampton (3,325 m) (76°29'S., 125°48'W.), a volcanic caldera.
Several volcanoes on offshore islands have records of historic activity. Mount Erebus (3,795 m), a stratovolcano on Ross Island with 10 known eruptions and 1 suspected eruption. On the opposite side of the continent, Deception Island (62°57'S., 60°38'W.), a volcanic caldera with 10 known and 4 suspected eruptions, have been the most active. Buckle Island in the Balleny Islands (66°50'S., 163°12'E.), Penguin Island (62°06'S., 57°54'W.), Paulet Island (63°35'S., 55°47'W.), and Lindenberg Island (64°55'S., 59°40'W.) are also considered to be active. In 2017, the researchers of Edinburgh University discovered 91 underwater volcanoes under West Antarctica.[2][3]
West Antarctica
West Antarctica is the smaller part of the continent, divided into:
Areas
Seas
Ice shelves
Larger ice shelves are:
- Filchner-Ronne Ice Shelf
- Larsen Ice Shelf
- Abbot Ice Shelf
- Getz Ice Shelf
- Sulzberger Ice Shelf
- Ross Ice Shelf
For all ice shelves see List of Antarctic ice shelves.
Islands
For a list of all Antarctic islands see List of Antarctic and sub-Antarctic islands.
East Antarctica
East Antarctica is the larger part of the continent, both the South Magnetic Pole and geographic South Pole are situated here. Divided into:
Areas
Seas
Ice shelves
Larger ice shelves are:
- Riiser-Larsen Ice Shelf
- Ekstrom Ice Shelf
- Amery Ice Shelf
- West Ice Shelf
- Shackleton Ice Shelf
- Voyeykov Ice Shelf
For all ice shelves see List of Antarctic ice shelves.
Islands
For a list of all Antarctic islands see List of Antarctic and sub-Antarctic islands.
Research stations
Territorial landclaims
Seven nations have made official Territorial claims in Antarctica.
Dependences and territories
See also
References
- ↑ Stirone, Shannon (7 September 2018). "New Antarctica Map Is Like 'Putting on Glasses for the First Time and Seeing 20/20' – A high resolution terrain map of Earth's frozen continent will help researchers better track changes on the ice as the planet warms". The New York Times. Retrieved 9 September 2018.
- ↑ McKie, Robin (2017-08-12). "Scientists discover 91 volcanoes below Antarctic ice sheet". The Guardian. ISSN 0261-3077. Retrieved 2017-08-16.
- ↑ "Student's idea leads to Antarctic volcano discovery". The University of Edinburgh. Retrieved 2017-08-16.
Sources
- Ivanov, L. General Geography and History of Livingston Island. In: Bulgarian Antarctic Research: A Synthesis. Eds. C. Pimpirev and N. Chipev. Sofia: St. Kliment Ohridski University Press, 2015. pp. 17–28. ISBN 978-954-07-3939-7
External links
- High resolution map (2018) – Reference Elevation Model of Antarctica (REMA)
- Political Claims Map
- USGS TerraWeb: Satellite Image Map of Antarctica
- United States Antarctic Resource Center (USARC)
- BEDMAP
- Antarctic Digital Database (Topographic data for Antarctica, including web map browser)
- Landsat Image Mosaic of Antarctica (LIMA; USGS web pages)
- Landsat Image Mosaic of Antarctica (LIMA; NASA web pages)
- Geography of the land under the ice of Antarctica:
- http://www.cbc.ca/news/technology/nasa-map-shows-what-antarctica-would-look-like-without-ice-1.1304997
- https://www.bas.ac.uk/project/bedmap-2/
- https://www.bas.ac.uk/data/our-data/maps/thematic-maps/bedmap2/
- https://www.the-cryosphere.net/7/375/2013/tc-7-375-2013.pdf article in The Cryosphere, 7, 375–393, 2013
- https://www.google.com/search?q=bedmap2&ie=utf-8&oe=utf-8&client=firefox-b Google search