盆地英文

1、准噶尔盆地（汉语拼音：zhǔn gá ěr pén dì，英文Junggar Basin），应该读作zhǔn gá ěr pén dì，很多人误认为应该念gě 其实是错误的。位于中国新疆的北部，是中国第二大的内陆盆地。 2、准噶尔盆地位于阿尔泰山与天山之间，西侧为准噶尔西部山地，东至北塔山麓。盆地呈不规则三角形，地势向西倾斜，北部略高于南部，北部的乌伦古湖（布伦托海）湖面高程479.1米，中部的玛纳斯湖湖面270米，西南部的艾比湖湖面189米，是盆地最低点。盆地西侧有几处缺口，如额尔齐斯河谷、额敏河谷及阿拉山口。西风气流由缺口进入，为盆地及周围山地带来降水。

basin 盆地关于死海关于格陵兰岛

basin 例如 柴达木盆地 the Qaidam Basin

basin 盆地 关于死海 关于格陵兰岛 Dead Sea, salt lake in southwestern Asia. Bounded on the west by Israel and the West Bank and on the east by Jordan, the Dead Sea forms part of the Israeli-Jordanian border. The surface of the Dead Sea, 408 m (1,340 ft) below sea level as of 1996, is the lowest water surface on earth. The lake is 80 km (50 mi) long and has a maximum width of 18 km (11 mi); its area is 1,020 sq km (394 sq mi). The Dead Sea occupies a north portion of the Great Rift Valley. On the east the high plateau of Moab rises about 1,340 m (about 4,400 ft) above the sea; on the west the plateau of Judea rises to half that height. From the eastern shore a peninsula juts out into the lake. To the south of this peninsula the lake is shallow, less than 6 m (less than 20 ft) deep; in the north it reaches its greatest depth of 399 m (about 1,309 ft) below surface level, and 799 m (about 2,621 ft) below sea level. The Dead Sea is fed mainly by the Jordan River, which enters the lake from the north. Several smaller streams also enter the sea, chiefly from the east. The lake has no outlet, and the heavy inflow of fresh water is carried off solely by evaporation, which is rapid in the hot desert climate. Due to large-scale projects by Israel and Jordan to divert water from the Jordan River for irrigation and other water needs, the surface of the Dead Sea has been dropping for at least the past 50 years. Nearly seven times as salty as the ocean, the Dead Sea contains at a depth of 305 m (1,000 ft) some 27 percent solid substances: sodium chloride (common salt), magnesium chloride, calcium chloride, potassium chloride, magnesium bromide, and many other substances. Because of the density of solids in the water, the human body easily floats on the surface. The lake contains no life of any sort except for a few kinds of microbes; sea fish put into its waters soon die. The Dead Sea is economically important as a source of potash, bromine, gypsum, salt, and other chemical products, which are extracted inexpensively. The shores of the Dead Sea are of growing importance as a winter health resort. The lake is closely associated with biblical history; the sites of the cities of Sodom and Gomorrah are believed to lie beneath the lake. 格陵兰岛 Greenland I INTRODUCTION Greenland (Greenlandic Kalaallit Nunaat; Danish Grønland), island which is an internally self-governing part of Denmark, situated between the North Atlantic and Arctic oceans. Greenland lies mostly north of the Arctic Circle and is separated from the Canadian Arctic Archipelago, on the west, primarily by Davis Strait and Baffin Bay, and from Iceland, on the east, by the Denmark Strait. The largest island in the world, Greenland has a maximum extent, from its northernmost point on Cape Morris Jesup to Cape Farewell in the extreme south, of 2,660 km (1,650 mi). The maximum distance from east to west is 1,300 km (800 mi). The entire coast, which is deeply indented with fjords, is roughly estimated at 44,000 km (27,000 mi). The total area of Greenland is 2,180,000 sq km (840,000 sq mi), of which 1,834,000 sq km (708,000 sq mi) is ice cap. The capital and largest city is Nuuk. II LAND AND RESOURCES Greenland consists of an interior ice-covered plateau surrounded by a mountainous, generally ice-free, rim. The interior ice cap varies in thickness, measuring 3,000 m (9,800 ft) in the center of the island. Underneath the ice cover are the ancient rocks of the Greenland Shield, which is geologically related to the Canadian Shield. The greatest heights of land are along the eastern coast, where the extreme elevation is Gunnbjørn Fjeld (about 3,700 m/ 12,000 ft). Drainage is afforded mainly by the so-called ice fjords, in which glaciers from the ice caps pass through valleys to the sea, where they form thousands of icebergs each year. The climate is extremely cold, but during the short summer in the south the mean temperature is 9° C (48° F). The mammals of Greenland are more American than European, and include the musk-ox, wolf, lemming, and reindeer. The varieties of seal and whale, and most of the species of fish and seabirds, are also American rather than European. Circumpolar animals, such as the polar bear, arctic fox, polar hare, and stoat, are also found. III POPULATION Greenlanders are a people of mixed ancestry, primarily Inuit and European, especially Danish-Norwegian. The total population of Greenland (2002 estimate) is 56,376. Nearly all the population is located on the narrow southwestern coastal fringe. The capital, Nuuk, formerly known as Godthåb (1994 population, 12,483), is located on the southwestern coast. Nuuk is the largest and oldest Danish settlement on the island, having been founded in 1721. Holsteinsborg (also called Sisimiut; 1994 population, 4,839), on the western coast just north of the Arctic Circle, is the second largest town. Other settlements include Julianehåb (Qaqortoq), Frederikshåb (Paamiut), and Narsaq (Narssaq), on the southern coast; Thule (Qaanaaq), on the northwestern coast; and Ammassalik (Angmagssalik), on the eastern coast. Education is free and compulsory for all children between the ages of 7 and 14. About 85 school centers were in operation in 1992, instructing primarily in Greenlandic (an Inuit language with some Danish words). Danish, the other official language of Greenland, is also used in the schools. A university is located at Nuuk. IV ECONOMY Fishing, sealing, and fur trapping are the principal economic activities in Greenland, which must rely on large amounts of financial support from Denmark. The fish catch is primarily cod, shrimp, and salmon; fish processing is the major manufacturing industry. Agriculture is only possible on one percent of Greenland's total area. Cattle, sheep, and goats are raised in small numbers in some portions of the southwestern coast, and hardy vegetables are grown. Greenland was formerly the world's main source of natural cryolite, a mineral used in the manufacture of aluminum, but by the late 1980s, reserves were exhausted. Lead and zinc were also produced until the mines were exhausted in 1990, and deposits of coal and uranium are known to exist. Denmark is Greenland's largest trading partner, and its main exports are fish, hides and skins, and fish oil. Thule Air Base (formerly Dundas) in the north supports a community of American and Danish civilian and military personnel. V GOVERNMENT In a referendum in 1979, Greenland voted for home rule. Denmark continues to administer external affairs. Executive power is held by a seven-member body, the Landsstyre, headed by a premier. Legislative power is vested in a 31-member parliament, the Landsting. Greenlanders elect two representatives to the Danish parliament. VI HISTORY Greenland was first explored by Eric the Red, a Norwegian settler in Iceland and father of Leif Eriksson, toward the end of the 10th century, and Icelandic settlements were subsequently established there under his leadership. By the early 15th century, however, these settlements had vanished, and all contact with Greenland was lost. In the course of the search for the Northwest Passage, Greenland was sighted again. The English navigator John Davis visited the island in 1585, and his explorative work, together with that of the English explorers Henry Hudson and William Baffin, afforded knowledge of the west coast of Greenland. A Danish Authority Established The foundation of Danish rule was laid by a mission at Godthåb (now Nuuk) in 1721 by a Norwegian missionary, Hans Egede. In the 19th century Greenland was explored and mapped by numerous explorers and navigators. From 1930 to 1931, British and German expeditions made weather observations on the inland ice north of the Arctic Circle. In 1933 an American expedition sponsored by the University of Michigan and Pan-American Airways engaged in meteorological research more than 545 km (more than 340 mi) north of the Arctic Circle. The United States relinquished its claim to land in northern Greenland, based on the explorations of the American explorer Robert Edwin Peary, when it purchased the Virgin Islands from Denmark in 1917. In May 1921, Denmark declared the entire island of Greenland to be Danish territory, causing a dispute with Norway over hunting and fishing rights. In 1931 a strip of land on the east coast was claimed by some Norwegian hunters, whose action was later recognized by the Norwegian government. The occupation was invalidated by the Permanent Court of International Justice at The Hague in 1933. B U.S. Protection Germany's occupation of Denmark in 1940, during World War II, brought the status of Greenland again into question. Negotiations between the U.S. government and the Danish minister to Washington resulted in an agreement on April 9, 1941, granting the United States the right “to construct, maintain and operate such landing fields, seaplane facilities and radio and meteorological installations as may be necessary” to protect the status quo in the western hemisphere; the United States also assumed protective custody over Greenland for the duration of World War II, although recognizing Danish sovereignty. Greenland is the source of many of the weather changes in the northern hemisphere, and knowledge of Greenland weather is of prime importance for the prediction of conditions in the North Atlantic Ocean and in western Europe. Weather and radio stations are of inestimable value for Atlantic air traffic. In 1944, during World War II, a German radio-weather station on the northeast coast was destroyed by the U.S. Coast Guard, and various German attempts to establish weather bases on Greenland were thwarted by Coast Guard vessels. In May 1947, Denmark requested that the United States end the 1941 agreement. Protracted negotiations culminated during April 1951, in a 20-year pact providing for Danish control of the chief U.S. naval station in Greenland and for the establishment of jointly operated defense areas. By the terms of other provisions, the armed forces of the members of the North Atlantic Treaty Organization were authorized to use all naval, air, and military bases on the island. In the early 1950s the United States expanded its military operations in Greenland, constructing a vast strategic air base at Thule, about 1,500 km (about 930 mi) from the North Pole. In June 1952, the Danish government and private Danish, Swedish, and Canadian interests formed a company to exploit deposits of zinc, lead, tungsten, and cryolite in eastern Greenland. C New Political Status Under the new Danish constitution of May 1953, the country became an integral part of the Danish monarchy and obtained representation in the national parliament. Greenland and Denmark both joined the European Community in 1972. Following a popular referendum in January 1979, Greenland attained home rule. Elections in April of that year for a new parliament were won by the left-wing Siumut Party. In a referendum held in February 1982, the Greenlanders voted by a narrow margin to withdraw from the European Community (now called the European Union); the withdrawal was completed by early 1985. In the June 1984 elections, the Siumut (Forward) Party and a moderate opposition group, the Atassut (Community) Party, each won 11 seats in parliament; the Inuit Ataqatigiit (IA), or Inuit Brotherhood, won 3 seats. Results of the May 1987 elections were similarly divided. In March 1991 the balance shifted as Atassut lost three seats and the IA gained two. In elections held in March 1995 Siumut won 12 seats and formed a coalition government with Atassut, which won 10 seats; the IA secured 6 seats.

死海Dead Sea, salt lake in southwestern Asia. Bounded on the west by Israel and the West Bank and on the east by Jordan, the Dead Sea forms part of the Israeli-Jordanian border. The surface of the Dead Sea, 408 m (1,340 ft) below sea level as of 1996, is the lowest water surface on earth. The lake is 80 km (50 mi) long and has a maximum width of 18 km (11 mi); its area is 1,020 sq km (394 sq mi). The Dead Sea occupies a north portion of the Great Rift Valley. On the east the high plateau of Moab rises about 1,340 m (about 4,400 ft) above the sea; on the west the plateau of Judea rises to half that height. From the eastern shore a peninsula juts out into the lake. To the south of this peninsula the lake is shallow, less than 6 m (less than 20 ft) deep; in the north it reaches its greatest depth of 399 m (about 1,309 ft) below surface level, and 799 m (about 2,621 ft) below sea level.The Dead Sea is fed mainly by the Jordan River, which enters the lake from the north. Several smaller streams also enter the sea, chiefly from the east. The lake has no outlet, and the heavy inflow of fresh water is carried off solely by evaporation, which is rapid in the hot desert climate. Due to large-scale projects by Israel and Jordan to divert water from the Jordan River for irrigation and other water needs, the surface of the Dead Sea has been dropping for at least the past 50 years.Nearly seven times as salty as the ocean, the Dead Sea contains at a depth of 305 m (1,000 ft) some 27 percent solid substances: sodium chloride (common salt), magnesium chloride, calcium chloride, potassium chloride, magnesium bromide, and many other substances. Because of the density of solids in the water, the human body easily floats on the surface. The lake contains no life of any sort except for a few kinds of microbes; sea fish put into its waters soon die.The Dead Sea is economically important as a source of potash, bromine, gypsum, salt, and other chemical products, which are extracted inexpensively. The shores of the Dead Sea are of growing importance as a winter health resort. The lake is closely associated with biblical history; the sites of the cities of Sodom and Gomorrah are believed to lie beneath the lake.格陵兰岛GreenlandI INTRODUCTION Greenland (Greenlandic Kalaallit Nunaat; Danish Grønland), island which is an internally self-governing part of Denmark, situated between the North Atlantic and Arctic oceans. Greenland lies mostly north of the Arctic Circle and is separated from the Canadian Arctic Archipelago, on the west, primarily by Davis Strait and Baffin Bay, and from Iceland, on the east, by the Denmark Strait. The largest island in the world, Greenland has a maximum extent, from its northernmost point on Cape Morris Jesup to Cape Farewell in the extreme south, of 2,660 km (1,650 mi). The maximum distance from east to west is 1,300 km (800 mi). The entire coast, which is deeply indented with fjords, is roughly estimated at 44,000 km (27,000 mi). The total area of Greenland is 2,180,000 sq km (840,000 sq mi), of which 1,834,000 sq km (708,000 sq mi) is ice cap. The capital and largest city is Nuuk.II LAND AND RESOURCES Greenland consists of an interior ice-covered plateau surrounded by a mountainous, generally ice-free, rim. The interior ice cap varies in thickness, measuring 3,000 m (9,800 ft) in the center of the island. Underneath the ice cover are the ancient rocks of the Greenland Shield, which is geologically related to the Canadian Shield. The greatest heights of land are along the eastern coast, where the extreme elevation is Gunnbjørn Fjeld (about 3,700 m/ 12,000 ft). Drainage is afforded mainly by the so-called ice fjords, in which glaciers from the ice caps pass through valleys to the sea, where they form thousands of icebergs each year. The climate is extremely cold, but during the short summer in the south the mean temperature is 9° C (48° F). The mammals of Greenland are more American than European, and include the musk-ox, wolf, lemming, and reindeer. The varieties of seal and whale, and most of the species of fish and seabirds, are also American rather than European. Circumpolar animals, such as the polar bear, arctic fox, polar hare, and stoat, are also found.III POPULATION Greenlanders are a people of mixed ancestry, primarily Inuit and European, especially Danish-Norwegian. The total population of Greenland (2002 estimate) is 56,376. Nearly all the population is located on the narrow southwestern coastal fringe.The capital, Nuuk, formerly known as Godthåb (1994 population, 12,483), is located on the southwestern coast. Nuuk is the largest and oldest Danish settlement on the island, having been founded in 1721. Holsteinsborg (also called Sisimiut; 1994 population, 4,839), on the western coast just north of the Arctic Circle, is the second largest town. Other settlements include Julianehåb (Qaqortoq), Frederikshåb (Paamiut), and Narsaq (Narssaq), on the southern coast; Thule (Qaanaaq), on the northwestern coast; and Ammassalik (Angmagssalik), on the eastern coast.Education is free and compulsory for all children between the ages of 7 and 14. About 85 school centers were in operation in 1992, instructing primarily in Greenlandic (an Inuit language with some Danish words). Danish, the other official language of Greenland, is also used in the schools. A university is located at Nuuk.IV ECONOMY Fishing, sealing, and fur trapping are the principal economic activities in Greenland, which must rely on large amounts of financial support from Denmark. The fish catch is primarily cod, shrimp, and salmon; fish processing is the major manufacturing industry. Agriculture is only possible on one percent of Greenland's total area. Cattle, sheep, and goats are raised in small numbers in some portions of the southwestern coast, and hardy vegetables are grown. Greenland was formerly the world's main source of natural cryolite, a mineral used in the manufacture of aluminum, but by the late 1980s, reserves were exhausted. Lead and zinc were also produced until the mines were exhausted in 1990, and deposits of coal and uranium are known to exist. Denmark is Greenland's largest trading partner, and its main exports are fish, hides and skins, and fish oil. Thule Air Base (formerly Dundas) in the north supports a community of American and Danish civilian and military personnel.V GOVERNMENT In a referendum in 1979, Greenland voted for home rule. Denmark continues to administer external affairs. Executive power is held by a seven-member body, the Landsstyre, headed by a premier. Legislative power is vested in a 31-member parliament, the Landsting. Greenlanders elect two representatives to the Danish parliament.VI HISTORY Greenland was first explored by Eric the Red, a Norwegian settler in Iceland and father of Leif Eriksson, toward the end of the 10th century, and Icelandic settlements were subsequently established there under his leadership. By the early 15th century, however, these settlements had vanished, and all contact with Greenland was lost. In the course of the search for the Northwest Passage, Greenland was sighted again. The English navigator John Davis visited the island in 1585, and his explorative work, together with that of the English explorers Henry Hudson and William Baffin, afforded knowledge of the west coast of Greenland.A Danish Authority Established The foundation of Danish rule was laid by a mission at Godthåb (now Nuuk) in 1721 by a Norwegian missionary, Hans Egede. In the 19th century Greenland was explored and mapped by numerous explorers and navigators. From 1930 to 1931, British and German expeditions made weather observations on the inland ice north of the Arctic Circle. In 1933 an American expedition sponsored by the University of Michigan and Pan-American Airways engaged in meteorological research more than 545 km (more than 340 mi) north of the Arctic Circle.The United States relinquished its claim to land in northern Greenland, based on the explorations of the American explorer Robert Edwin Peary, when it purchased the Virgin Islands from Denmark in 1917. In May 1921, Denmark declared the entire island of Greenland to be Danish territory, causing a dispute with Norway over hunting and fishing rights. In 1931 a strip of land on the east coast was claimed by some Norwegian hunters, whose action was later recognized by the Norwegian government. The occupation was invalidated by the Permanent Court of International Justice at The Hague in 1933.B U.S. Protection Germany's occupation of Denmark in 1940, during World War II, brought the status of Greenland again into question. Negotiations between the U.S. government and the Danish minister to Washington resulted in an agreement on April 9, 1941, granting the United States the right “to construct, maintain and operate such landing fields, seaplane facilities and radio and meteorological installations as may be necessary” to protect the status quo in the western hemisphere; the United States also assumed protective custody over Greenland for the duration of World War II, although recognizing Danish sovereignty.Greenland is the source of many of the weather changes in the northern hemisphere, and knowledge of Greenland weather is of prime importance for the prediction of conditions in the North Atlantic Ocean and in western Europe. Weather and radio stations are of inestimable value for Atlantic air traffic. In 1944, during World War II, a German radio-weather station on the northeast coast was destroyed by the U.S. Coast Guard, and various German attempts to establish weather bases on Greenland were thwarted by Coast Guard vessels. In May 1947, Denmark requested that the United States end the 1941 agreement. Protracted negotiations culminated during April 1951, in a 20-year pact providing for Danish control of the chief U.S. naval station in Greenland and for the establishment of jointly operated defense areas. By the terms of other provisions, the armed forces of the members of the North Atlantic Treaty Organization were authorized to use all naval, air, and military bases on the island. In the early 1950s the United States expanded its military operations in Greenland, constructing a vast strategic air base at Thule, about 1,500 km (about 930 mi) from the North Pole.In June 1952, the Danish government and private Danish, Swedish, and Canadian interests formed a company to exploit deposits of zinc, lead, tungsten, and cryolite in eastern Greenland.C New Political Status Under the new Danish constitution of May 1953, the country became an integral part of the Danish monarchy and obtained representation in the national parliament. Greenland and Denmark both joined the European Community in 1972.Following a popular referendum in January 1979, Greenland attained home rule. Elections in April of that year for a new parliament were won by the left-wing Siumut Party. In a referendum held in February 1982, the Greenlanders voted by a narrow margin to withdraw from the European Community (now called the European Union); the withdrawal was completed by early 1985. In the June 1984 elections, the Siumut (Forward) Party and a moderate opposition group, the Atassut (Community) Party, each won 11 seats in parliament; the Inuit Ataqatigiit (IA), or Inuit Brotherhood, won 3 seats. Results of the May 1987 elections were similarly divided. In March 1991 the balance shifted as Atassut lost three seats and the IA gained two. In elections held in March 1995 Siumut won 12 seats and formed a coalition government with Atassut, which won 10 seats; the IA secured 6 seats.