Liechtenstein

ONE OF WESTERN Europe’s five microstates, the story-book principality of Liechtenstein is in reality one of the few “absolutist” states in the world, thanks to a favorable referendum voting extensive powers to the ruling sovereign in March 2003. His Serene Highness, Prince Hans-Adam II von und zu Liechtenstein now has more political prerogatives than any other monarch in Europe.

Sandwiched between the Swiss cantons of St.Gallen to the west and Graubünden to the south and the Austrian province of Vorarlberg to the east, Liechtenstein’s history has naturally been closely linked to its larger neighbors. The family had served the Habsburgs in AUSTRIA for centuries, and in fact the family derives its name from its main castle just south of Vienna. Prince Johann Adam bought the county of Vaduz and the adjacent lordship of Schellenberg in 1699 and 1712, and the two territories were united as a fully independent member of the Holy Roman Empire in 1719. But the land itself was of secondary importance to the family: no sovereign prince of Liechtenstein even visited until the middle of the 19th century.

When the Holy Roman Empire fell apart thanks to Napoleon in 1806, Liechtenstein fell between the cracks and was not consolidated into one of the larger German states. Successive princes maintained their independence and forged a beneficial customs union with Austria in 1852. After the collapse of the Austro-Hungarian Empire, however, the princes turned west and formed a similar customs and monetary union with SWITZERLAND in 1923, which is still in effect today. The princely family still owns large estates in Austria and lays claim to numerous others in the CZECH REPUBLIC that were confiscated by the communists (equal to ten times the size of the principality itself). Still, the prince’s wealth is estimated at more than $2 billion.

The principality—15 mi (26 km) long, and an average of 4 mi (6 km) wide—lies on the eastern bank of the RHINE RIVER, between its emergence from the high Alpine valleys of Switzerland and Lake Constance to the north. Two canals running on either side of the river through this valley maintain its water levels to reduce risk of spring floods. The eastern third of Liechtenstein is divided from the rest by a range of mountains, forming the upper Samintal, or valley of the Samina River, which runs northward into the Ill in Austria, which in turn joins the RHINE just a few kilometers north of Liechtenstein. To the east and south of this valley rise the much greater Alpine heights dividing the country from Austria, including a number of peaks above 8,250 feet (2,500 m).

The main town, Vaduz, has a population of about 5,000. High above the town, the prince’s castle, dating from the 14th century, boasts one of the largest private art collections in the world and is a major tourist attraction. Much of this art collection has recently been transferred to Vienna’s newest major art gallery, the restored Liechtenstein Palace, opened to the public in March 2004. Liechtenstein itself has been transformed since World War II from a sleepy agricultural community to a modern industrialized society with one of the world’s highest standards of living. Revenue is generated locally through skiing and the sale of rare stamps, but it is the income from numerous so-called post-office-box companies, attracted by low business taxes, that has boosted the national economy (providing as much as 30 percent of state revenues). Concerns over tax evasion schemes and money laundering, however, have recently caused increased pressure from the EUROPEAN UNION and the principality’s authorities.

Libya

A RELATIVELY LARGE country, similar in size to the state of ALASKA, Libya largely consists of broad rolling deserts, barren rock inselbergs and immense dune fields or ERGS. It is a landscape of sandstorms; hot dusty wind, or ghibli; an expanding desert; and scarce water. More than 90 percent of the country is considered arid or semiarid. It primary cities are all located on the MEDITERRANEAN SEA coastline, which has facilitated its links across North Africa to Europe and western Asia.

Generally speaking, the Saharan plateau covers most of Libya. The exceptions are in the northwest corner in a region known as Tripolitania and in the northeast in Cyrenaica, Libya’s largest region. The Tripolitania region, which runs north to south, is a string of carefully cultivated coastal oases in addition to the triangular Al-Jifarah plain, and the Nafusah Plateau, 200 mi (320 km) of limestone between 2,000 and 3,000 ft (600 to 915 m) in elevation.

Libya has no perennial rivers, but there are extensive underground aquifers that support artesian wells and springs. Libya’s arid desert climate is moderated along the coast by the Mediterranean Sea. Precipitation ranges from 16 to 20 in (40 to 50 cm) in the northern hills to less than 5 in (12 cm) throughout most of the south, and to 1 in (2.5 cm) in the Libyan Desert.

Droughts are common, meaning natural vegetation is minimal. Libya’s principal mineral resource is its reserves of petroleum, Africa’s largest and among the world's largest. Since it earliest days as a major Phoenician and Roman territory on the North African coast of the Mediterranean Sea, Libya has been raided and colonized by Vandals, Arabs, Ottoman Turks, and Italians until its independence in 1951. Only a few years later, the country changed dramatically with the discovery of enormous oil reserves. In 1969, a 27-year-old Muammar Qaddafi led a successful coup to gain control of the nation. Qaddafi has been victorious in removing any imprints of previous cultures to create a landscape from his own vision. Based upon his Third International Theory, he created a political system combining Islam and socialism.

Using petroleum revenues in the 1970s and 1980s to promote political ideologies (including supporting terrorist activities) throughout the region, Libya prompted the United Nations (UN) to impose economic sanctions after the Lockerbie terrorist bombing was suspected to have had Libyan ties. The sanctions were then lifted in April 1999 when Qaddafi handed over Lockerbie bombing suspects.

Liberia

LIBERIA, “LAND OF THE FREE,” in western Africa, borders the north ATLANTIC OCEAN, between CÔTE D’IVOIRE and SIERRA LEONE. It has 10 to 50 mi (16 to 80 km) of flat coastal plain that contains creeks, mangrove swamps, and lagoons. Beyond that, forested hills, from 600 to 1,200 ft (180 to 370 m) high cover the rest of the country, excluding the mountains in the northern highlands. The maximum peak in the Nimba Mountains is 4,540 ft (1,383 m). Six principal rivers flow to the ATLANTIC OCEAN.

Vegetation is predominantly forest, and the tropical, humid climate sees rainfall averages of 183 in (465 cm) on the coast and 88 in (224 cm) in the southeast. The dry season (harmattan, December and January) splits two rainy seasons. Cities other than Monrovia are the ports of Harper and Buchanan. POPULATION GROUPS

There are 16 ethnicities in Liberia, including the Kpelle, Mano, Baso, Grebo, Kru, and Vaj. Seventy percent are native, traditional religion practitioners, while 20 percent are Muslim and 10 percent Christian. Although English is the official language, the native languages are used commonly. The Americo-Liberians, a minority residing in the cities, tend to be Protestants.

Other population groups include Lebanese merchants and European and American technicians. Liberia was founded in 1820 on the Grain Coast; it was the gift of the American Colonization Society, which received it from the Cape Mesurado chiefs. The founders fought bloody battles with the indigenous peoples. Eighty-six freed slaves from the United States established Christopolis, later Monrovia, in February 1820. Approximately 15,000 freed slaves emigrated from the United States until the American Civil War. In 1847, Liberia declared itself an independent republic.

Until 1980, the Americo-Liberian or True Whig Party (TWP) ruled Liberia. The first president was Joseph Jenkins Roberts, American-born. The government and constitution were modeled on that of the UNITED STATES. The republic traded with other parts of West Africa, but it modeled its style of living on those of the United States.

Modernization efforts led to a crisis of foreign debt in 1871. Conflicts with FRANCE and Britain led to losses of territory in 1885, 1892, and 1919. Liberia used the European rivalries and the support of the United States to remain independent. Still its exports declined and its debts rose, leading to foreign interference. Bankruptcy came in 1909. International loans saved Liberia. In 1926, Firestone, the American tire company, leased large rubber plantations. In 1930, the League of Nations investigated charges that Liberia was exporting labor, that is, engaging in the slave trade. The president resigned.

The new president, William Tubman, opened the country to international investment, allowed indigenes greater participation, and allowed the exploitation of iron and other minerals. Education, roads, infrastructures, and healthcare were improved. Tubman died in 1971. His vice president, W.R. Tolbert took over. A proposed increase in the price of rice in 1979 set off rioting. The TWP’s rule ended on April 12, 1980, when Master Sergeant Samuel K. Doe, a native Krahn, pulled off a successful coup. Doe’s forces executed Tolbert and several other Americo-Liberians. Doe’s People’s Redemption Council promised a return to civilian rule, then began repressing the opposition and abusing human rights. Doe instituted constitutional changes, survived numerous coups, and saw flight of thousands of refugees to the Côte d’Ivoire. The refugees returned in 1989, led by Charles Taylor. The war waxed and waned until finally in 2003 the Taylor regime ended, and the country and government struggled to maintain the uneasy truce.

Lesotho

LESOTHO IS LOCATED literally within SOUTH AFRICA: This small southern African country is landlocked and surrounded on all sides by the Republic of South Africa. Lesotho covers an area slightly smaller than MARYLAND. It is the only country in the world that lies entirely above 3,280 ft (1,000 m) and more than 80 percent of Lesotho is 5,905 ft (1,800 m) above sea level. Lesotho is mainly mountains, hills, and highlands with plateaus. It has a very temperate climate, with cool to cold dry winters and hot, wet summers.

Lesotho has four major mountain ranges within its borders. The DRAKENSBURG MOUNTAIN range, the Central range, and the Thoba Rutsoa range are all in the central and eastern parts of Lesotho and the Maloti range is in the western region. Thabana-Ntlenyana is the highest peak in all of southern Africa. It is also called “The Kingdom in the Sky,” “The Roof of Africa,” and “The Switzerland of Africa.” Deep river valleys and canyons cut these mountains; the water that flows through these canyons is the major water supply for all of southern Africa. Many of the rivers on the southern part of the African continent start in these hills, including the Orange River and its many tributaries.

This water is Lesotho’s main natural resource. Lesotho is exploiting its water through the Lesotho Highlands Water Project. This project is designed to capture, store, and transfer water from the Orange River system and send it to the Republic of South Africa. This project not only moves water but produces hydroelectricity as well. There are going to be approximately seven dams and two tunnels when the project is complete in 2020. With the first phase of the project already completed, Lesotho has become almost completely self-sufficient in the production of electricity. Already it has generated approximately $24 million annually through the sale of electricity and water to South Africa.

The kingdom of Lesotho is heavily populated especially in the western part of Lesotho where there is more arable land. There, the people raise crops of corn, sorghum, wheat, beans, peas, asparagus, tomatoes, and peaches. Most of the land is used for raising animals such as sheep, goats, cattle, pigs, chickens, and horses. These people, called the Basotho, are remnants of various ethnic groups made up mainly of various Bantu-speaking people and some of the original San or Bushmen who were Lesotho’s earliest inhabitants. The Basotho managed to fend off both the Zulus and the Boers in the 1800s.

On October 4, 1966, Lesotho gained independence. The Lesotho government is now a constitutional monarchy with a king as the head of state and a prime minister as the head of government. Currently, the king serves primarily as a ceremonial figure with no executive power. However, all land in Lesotho is held by the king and is allocated to the Basotho people through local chiefs. Foreigners in Lesotho are strictly forbidden from owning land. Lesotho has one of the highest literacy rates in Africa; official languages are English and Sesotho, a Bantu language.

Lena River

THE LENA RIVER is one of Russia’s great northern rivers, draining an area of 899,641 square mi (2,306,772 square km) and encompassing a region rich in wildlife and natural resources, including one of the world’s largest deposits of gold. This is also one of the most inhospitable regions on the planet, with extremes of temperature and vast stretches of northern forests (84 percent). Few people live in the region and there is only one city in the entire Lena basin, Yakutsk, the administrative seat of the former Yakut Autonomous Socialist Republic and now the capital of a semiindependent Yakutia, renamed the Republic of Sakha in 1991.

The river, 2,850 mi (4,597 km) long, flows mostly through Sakha, but its origins are in the Irkutsk District, immediately west of Lake BAIKAL. Its tributaries have their headwaters in the autonomous republic of Buryatiya and the districts of Chita, Amur, and Khabarovsk. The river starts in the Baikal range, only a short distance from the lake itself, though the lake’s waters flow into the Angara River and into the Yenisey, thousands of kilometers from the Lena. It then flows north and east to be joined by its first major tributaries, the Vitim and Olekma, whose headwaters originate in the Yablonov and other parallel mountain ranges east of Lake Baikal (which are also the source of the headwaters of the AMUR RIVER).

The river then turns again north in a large arc, following the contours of the Aldan Plateau to the south, from which emerges the Lena’s largest tributary, the Aldan, and the Verkhoyansk Range to the east. This range of mountains forms a steep escarpment for over 600 mi (1,000 km), stretching all the way to the Lena’s delta on the Laptev Sea, an arm of the ARCTIC OCEAN.

This semicircular area bounded by the Aldan and Verkhoyansk highlands forms a sort of climatic vortex, producing some of the coldest temperatures ever recorded on the planet: -88.9 F (-67 degrees C). To the west the terrain is much flatter, with larger tributary rivers, notably the Vilyui, which extends far into the Siberian Plateau. From the confluence of the Lena with the Aldan, 800 mi (1,300 km) from the sea, the river becomes very broad, sometimes reaching 5 mi (8 km) across. The delta, covering 12,352 square mi (31,672 square km), is the largest in RUSSIA and third largest in the world. It is formed of numerous islets, marshes and sandbars. The largest islands (hundreds of square kilometers) are covered with damp, mossy tundra and frozen lakes that do not permit the construction of roads, so travel between the eight permanent settlements continues mainly by dogsled.

The river is almost entirely navigable, with an abundance of fish, but is frozen eight months of the year. Ice has been measured at 53 in (136 cm) in the south, and up to 90 in (231 cm) at the delta. Because the Lena is almost entirely fed by mountain snows, spring thaws can bring disastrous floods, followed by equally breakups of river ice, sizable chunks of which can destroy entire sections of the riverbank and any settlements alongside it. The annual flow of the river is very irregular, with 90 to 95 percent of all of its discharge in spring and summer, when its volume increases by as much as 10 times that of the winter months. This irregular flow has limited the development of hydroelectric projects in the Lena basin, though there are two large dam-reservoir complexes on the Vilyuy. The Lena was used as a highway for trappers and traders in Russia’s expansion to the Pacific coast, with its main town of Yakutsk founded in 1632.

Russia’s relations with the indigenous Yakut and Evenki peoples were not always harmonious, and the region saw a good deal of oppression, lawlessness, and unbridled greed in the race for lucrative furs. Another boom period followed in the 19th century, with the discovery of gold in the Lena valley near the confluence with the Vitim River. Privatization since the 1990s has returned the region to its “Wild West” frontier days, ruled by hustlers, speculators and black marketers. The 1 million inhabitants who live in the Lena basin are looking to their mineral wealth, still undeveloped because of great distances, difficulties building roads and buildings on permafrost, and difficulty getting water half the year.

Leeward and Windward

THE TERMS leeward and windward are used in a number of ways to describe specific places, physical features, and climatic processes. In one sense, windward and leeward generally refer to the location of a place relative to the prevailing wind direction. A windward location is one that is exposed to the prevailing winds. Conversely, a leeward location is protected from the prevailing wind.

For example, Concepcion, CHILE, on the west side of the ANDES would be in a windward location relative to westerlies moving inland from the PACIFIC OCEAN simply because it is exposed to the approaching wind. However, the east side of the Andes would be a leeward location because of the protection afforded by the intervening mountains. The windward and leeward designations illustrated here are equally applicable to orographic lifting, the process involved when winds strike the front face of a mountain, are forced up the windward face of the mountain and then descend on the leeward side. If the winds are laden with moisture and the mountain is high enough, the moisture carried by the wind may condense and produce precipitation.

The resulting precipitation will in the highest volumes on the windward side of the mountain and the leeward side will invariably receive a lesser amount. There are a number of places in the world where this process is clearly evidenced. Among them are the moisture-laden westerlies reaching the Pacific coast of WASHINGTON, which are forced aloft by the Coastal Ranges. The windward side of this region receives an abundance of rainfall while the leeward side on the eastern slopes receives little or no rainfall. A classic example of orographic lifting is found in the HIMALAYAS when the summer monsoons bring warm, moist winds across the Indian subcontinent and are then forced aloft by the imposing Himalayan barrier. Areas on the windward side on the mountains may receive as much as 100 in (254 cm) of rainfall. However, because of the great heights of the Himalayas, little or no moisture reaches the leeward side. So within a relatively short distance the climatic results vary from near tropical conditions to the true deserts of Central Asia.

The terms are used in a more formal manner to name particular groups of islands. For example, the islands in the Lesser Antilles in the West Indies all lie in the pathway of the northeast trade winds. This wind belt moves from approximately 30 degrees north latitude toward the equator where it meets its counterpart from the Southern Hemisphere, the southeast trade winds. Historically, British sailing ships entered the region with the northeast trade winds at their backs. The first island encountered on these voyages was usually BARBADOS, the island farthest east and most to windward.

The Windward Islands, as they came to be called, include Barbados, the Caribees (a cluster of small islands), DOMINICA, MARTINIQUE, GRENADA, SAINT LUCIA, and SAINT VINCENT AND THE GRENADINES. The Windward Islands, a former British colony, are the southernmost islands in the Lesser Antilles and were once collectively named the Federal Colony of the Windward Islands and later the Territory of the Windward Islands. The northern continuation of the Lesser Antilles includes islands that are farther downwind from the Windward Islands. First discovered by Columbus in 1493, these are the Leeward Islands, which includes ANTIGUA AND BARBUDA, the British Virgin Islands, MONTSERRAT, SAINT KITTS AND NEVIS, and ANGUILLA. A string of leeward islands is also found northwest of the Hawaiian Islands, and this group has become a national bird sanctuary.

In addition, the Society Islands in French Polynesia, a region east of the COOK ISLANDS in the South Pacific, are identified as leeward islands. Reference may be made as well to another use of the word windward. The narrow sea-lane separating eastern CUBA and HAITI lies in the path of the northeast trade winds. As such, vessels traveling between the ATLANTIC OCEAN and the CARIBBEAN SEA are using the aptly named Windward Passage. Those traveling through the pass from northeast to southwest have the advantage of the northeast trade winds pushing them along.

Lebanon

LEBANON, ONE OF the world’s smallest countries, is on the eastern shore of the MEDITERRANEAN SEA. SYRIA is its neighbor to the north and east, and ISRAEL is located to the south. Although a small country, Lebanon has a wide range of geographical regions. All of the major cities are located on the coastal strip. The Mount Lebanon Range located inland, provides majestic peaks and ridges. The Bekaa Valley, located parallel to the coast, is home to a multitude of wine vineyards.

Thousands of years ago, the mountains of Lebanon were covered with great cedar forests. Only a few cedar forests remain, but Lebanon is still recognized as the most densely wooded country in the Middle East. Many pine trees cover the mountain land, and fruit trees are present all across the coastal plain. The mountains are home to many different birds, including eagles, red kites, Sardinian warblers, and Scop’s owls.

The climate in Lebanon is as diverse as the topography. Along the coast, hot conditions are prevalent during the summer, and cool, moist weather during the winter months. Snow and wind are common in the Bekaa Valley during the winter, and the mountains provide a typical alpine climate year-round.

The French created Lebanon in 1920. Originally, the Maronites, the largest religious community in the country, were placed in control of the government. However, to ensure the Maronites would remain loyal to the French, the French enlarged Lebanon to include mainly Muslim areas in the state. After this inclusion, only 30 percent of the population was Maronite. The tight grip of the French would last for decades, and the religious differences would last for the rest of the century.

In 1926, the constitution was passed; a single chamber of deputies was created that could elect a president. The president had limited authority to choose a prime minister and the cabinet. However, the French rule continued to control Lebanese foreign relations and the military. By 1936, French and Lebanese government officials signed a treaty that included a guarantee of fairness to all religious sects in the country. The Maronite Christian Emile Eddé was elected president and he chose a Muslim, Khayr al-Din al-Ahdab as the prime minister. This power sharing formula continued until the late 1980s.

The French left Lebanon after World War II, and for the next two decades, the Lebanese people tried to create a separate identity. In the early 1970s, many Palestinian Liberation Organization (PLO) fighters infiltrated the country. They conducted raids against the Israelis from southern Lebanon and urged many Palestinian refugees in Lebanon to fight for their cause. By April 1975, tensions reached new levels as civil war broke out in Lebanon. The conflict sided the Christian Maronites against the Muslim Lebanese National Movement (LNM). The Palestine Liberation Organization (PLO) soon joined the Muslim forces. One year later, the Syrian army intervened and, with Arab League support, worked out a cease-fire. By October 1976, an Arab Deterrent Force, mainly of 40,000 Syrian soldiers, occupied Lebanon. However, tensions were still high.

On June 6, 1982, after years of PLO attacks, Israel invaded Lebanon with the goal of eliminating the PLO and creating a 25-mile security zone in southern Lebanon. The Israelis bombarded Beirut, hoping the Christian militias would seize control of the government. By August 1982, the PLO evacuated Beirut and took refuge in eight different countries. The Christian Bashir Gemayel was elected Lebanese president but was assassinated a few weeks later. The Israelis immediately returned to Beirut. A multinational peace force returned to the country and Amin Gemayel became president. In June 1985, Israeli forces withdrew from Lebanon, but maintained a presence in the southern Lebanon security zone. The country remained divided for the next six years. On May 22, 1991, the Lebanese government signed a Treaty of Cooperation and Brotherhood. Syria was given control over Lebanon’s internal affairs and had around 16,000 troops stationed in the country. In 2005, under international pressure, Syria began to withdraw those troops.

Lebanon has attempted to pick up the pieces from the years of war. Muslims have been given a greater role in the government. Although the militant group, Hezballah still retains its weapons, most of the militias have been weakened or eliminated. The Lebanese armed forces have central government control over the majority of the country and Israel had withdrawn its forces from the southern security zone.