Antarctica

**Antarctica**, the world’s southernmost and fifth largest continent. Its landmass is almost wholly covered by a vast ice sheet. Often described as a continent of superlatives, Antarctica is not only the world’s southernmost continent. It is also the world’s highest, driest, windiest, coldest, and iciest continent. Antarctica is about 5.5 million square miles (14.2 million square km) in size, and thick ice covers about 98 percent of the land. The continent is divided into East Antarctica (which is largely composed of a high ice-covered plateau) and West Antarctica (which is largely an ice sheet covering an archipelago of mountainous islands). Lying almost concentrically around the South Pole, Antarctica’s name means “opposite to the Arctic.” It would be essentially circular except for the outflaring Antarctic Peninsula, which reaches toward the southern tip of South America (some 600 miles [970 km] away), and for two principal embayments, the Ross Sea and the Weddell Sea. These deep embayments of the Southern Ocean make the continent somewhat pear-shaped, dividing it into two unequal-sized parts. East Antarctica lies mostly in the east longitudes and is larger than West Antarctica, which lies wholly in the west longitudes. East and West Antarctica are separated by the approximately 2,100-mile- (about 3,400-km-) long Transantarctic Mountains. The continental ice sheet contains approximately 7 million cubic miles (about 29 million cubic km) of ice, representing about 90 percent of the world’s ice and 80 percent of its fresh water. Its average thickness is about 5,900 feet (1,800 metres). Ice shelves, or ice sheets floating on the sea, cover many parts of the Ross and Weddell seas. These shelves—the Ross Ice Shelf and the Filchner-Ronne Ice Shelf—together with other shelves around the continental margins, fringe about 45 percent of Antarctica. Around the Antarctic coast, shelves, glaciers, and ice sheets continually “calve,” or discharge, icebergs into the seas. The continent is a cold dry desert where access to water determines the abundance of life. While the terrestrial ecosystem contains more than a thousand known species of organisms, most of these are microorganisms. Maritime Antarctica—the islands and coasts—supports more life than inland Antarctica, and the surrounding ocean is as rich in life as the land is barren. From the late 18th to the mid-20th century, whalers and sealers plied the rich seas that surround the continent. Science then replaced whaling and sealing as the primary year-round human activity in Antarctica. In addition, krill harvesting and other types of commercial fishing in the Southern Ocean expanded from the 1960s onwards. The new millennium saw tourism and (to a lesser extent) biological prospecting (the search for useful chemical compounds and genes in local species) become established sectors of the Antarctic economic landscape.

Governments mandated many early expeditions—whether ostensibly economic, scientific, or exploratory in character—to make territorial claims. With the International Geophysical Year (IGY) in 1957–58, the present scale of scientific investigation of Antarctica began, and on December 1, 1959, the twelve countries that were active in Antarctica during the IGY signed the Antarctic Treaty. This treaty, which was an unprecedented landmark in diplomacy, preserves the continent for nonmilitary scientific pursuits and placed Antarctica under an international regime that, for the treaty’s duration, holds all territorial claims in place. The treaty bound its members indefinitely, with a review of its provisions possible after 30 years. A subsequent treaty, called the Madrid Protocol (adopted in 1991), prohibited mining, required environmental impact assessments for new activities, and designated the continent as a natural reserve.

Knowledge about Antarctica has increased greatly since the IGY. Geologists, geophysicists, glaciologists, biologists, and other scientists have mapped and visited all of the continent’s mountain regions. Until the 1970s, scientists relied on ground-based geophysical techniques such as seismic surveys of the Antarctic ice sheets to reveal hidden mountain ranges and peaks. Advances in radar technology since then have resulted in airborne radio-echo sounding systems that can measure ice-thickness, which has enabled scientific teams to make systematic remote surveys of ice-buried terrains. Satellites and other remote-sensing technologies have become key tools in providing mapping data.