Landlocked country

Landlocked country is a country entirely enclosed by land, or whose only coastlines lie on closed seas. There are 47 landlocked countries in the world, including partially recognized states. Of the major landmasses, only North America, Australia, and inhospitable Antarctica do not have a landlocked country inside their respective continents.

History and significance

Bolivia's loss of its coast in the War of the Pacific (1879-1884) remains a major political issue. In the mural is written: "What once was ours, will be ours once again", and "Hold fast, rotos (Chileans), for here come the Colorados (Reds) of Bolivia".

Historically, being landlocked was regarded as a disadvantageous position. It cuts the country off from sea resources such as fishing, but more importantly cuts off access to seaborne trade which, even today, makes up a large percentage of international trade. Coastal regions tended to be wealthier and more heavily populated than inland ones. Paul Collier in his book The Bottom Billion argues that being landlocked in a poor geographic neighborhood is one of four major development "traps" by which a country can be held back. In general, he found that when a neighboring country experiences better growth, it tends to spill over into favorable development for the country itself. For landlocked countries, the effect is particularly strong, as they are limited from their trading activity with the rest of the world. "If you are coastal, you serve the world; if you are landlocked, you serve your neighbors. Others have argued that being landlocked may actually be a blessing as it creates a 'natural tariff barrier' which protects the country from cheap imports. In some instances this has led to more robust local food systems. 

Landlocked developing countries have significantly higher costs of international cargo transportation compared to coastal developing countries (in Asia the ratio is 3:1).

Countries thus have made particular efforts to avoid being landlocked:

The International Congo Society, which owned the modern-day Democratic Republic of the Congo, was given a thin piece of land cutting through Angola to connect it to the sea by the Conference of Berlin in 1885.

The Republic of Ragusa once gifted the town of Neum to the Ottoman Empire because it did not want to have a land border with Venice; this small municipality was inherited by Bosnia and Herzegovina and now provides limited sea access, splitting the Croatian part of the Adriatic coast in two.

After World War I, in the Treaty of Versailles, a part of Germany, designated "the Polish corridor", was given to the new Second Polish Republic, for access to the Baltic Sea. This was also the pretext for making Danzig (now Gdańsk) with its harbour the Free City of Danzig. This gave Poland a slight coastline, which was soon enlarged as the small fishing harbor of Gdynia grew into a large one.

The Treaty of Versailles also enforced that Germany needs to offer Czechoslovakia a lease for 99 years for a part of the ports in Hamburg and Stettin, allowing Czechoslovakia sea trade over the Elbe and Oder rivers. While the former Stettin is now part of Poland after World War II, Hamburg still continued the contract so that the part of the port (now called Moldauhafen) may still be used for sea trade by the successor of Czechoslovakia, the Czech Republic.

The Danube is an international waterway so that landlocked Austria, Hungary, Serbia, and Slovakia (plus the southern parts of Germany, itself not landlocked) could have secure access to the Black Sea.

Losing access to the sea is generally a great blow to a nation, politically, militarily, and particularly with respect to international trade and therefore economic security:

The independence of Eritrea and Montenegro, brought about by successful separatist movements, have caused Ethiopia and Serbia respectively to become landlocked.

Bolivia lost its coastline to Chile in the War of the Pacific. The Bolivian Navy still trains in Lake Titicaca for an eventual recovery, and the Bolivian people annually celebrate a patriotic "Dia del Mar" (Day of the Sea) to remember its territorial loss, which included both the coastal city of Antofagasta and what has proven to be one of the most significant and lucrative copper deposits in the world. In the 21st century, the selection of the route of gas pipes from Bolivia to the sea fueled popular uprisings.

Austria and Hungary also lost their access to the sea as a consequence of the Treaty of Saint-Germain-en-Laye (1919) and the Treaty of Trianon (1920) respectively. Before, although Croatia had a constitutional autonomy within Hungary, the City of Fiume/Rijeka on the Croatian coast was governed directly from Budapest by an appointed governor as a corpus separatum, to provide Hungary with its only international port in the periods 1779–1813, 1822–1848 and 1868–1918.

When the Entente Powers divided the former Ottoman Empire under the Treaty of Sèvres at the close of World War I, Armenia was promised part of the Trebizond vilayet (roughly corresponding to the modern Trabzon and Rize provinces in Turkey). This would have granted Armenia access to the Black Sea. However, the Sèvres treaty collapsed with the Turkish War of Independence and was superseded by the Treaty of Lausanne which firmly established Turkish rule over the area.

The United Nations Convention on the Law of the Sea now gives a landlocked country a right of access to and from the sea without taxation of traffic through transit states. The United Nations has a programme of action to assist landlocked developing countries, and the current responsible Undersecretary-General is Anwarul Karim Chowdhury.

List of landlocked countries

Afghanistan 647,500 29,117,000

Andorra 468 84,082

Armenia 29,743 3,254,300

Austria 83,871 8,396,760

Azerbaijan  86,600 8,997,400

Belarus 207,600 9,484,300

Bhutan 38,394 691,141

Bolivia 1,098,581 10,907,778

Botswana 582,000 1,990,876

Burkina Faso 274,222 15,746,232

Burundi 27,834 8,988,091

Central African Republic 622,984 4,422,000

Chad 1,284,000 10,329,208

Czech Republic 78,867 10 674 947

Ethiopia 1,104,300 85,237,338

Hungary 93,028 10,005,000

Kazakhstan 2,724,900 16,372,000

Kosovo 10,908 1,804,838

Kyrgyzstan 199,951 5,482,000

Laos 236,800 6,320,000

Lesotho 30,355 2,067,000

Liechtenstein 160 35,789

Luxembourg 2,586 502,202

Republic of Macedonia 25,713 2,114,550

Malawi 118,484 15,028,757

Mali 1,240,192 14,517,176

Moldova 33,846 3,567,500

Mongolia 1,564,100 2,736,800

Nagorno-Karabakh 11,458 138,000

Nepal 147,181 29,331,000

Niger 1,267,000 15,306,252

Paraguay 406,752 6,349,000

Rwanda 26,338 10,746,311

San Marino 61 31,716

Serbia 88,361 7,306,677

Slovakia 49,035 5,429,763

South Ossetia 3,900 72,000

South Sudan 619,745 8,260,490

Swaziland 17,364 1,185,000

Switzerland 41,284 7,785,600

Tajikistan 143,100 7,349,145

Transnistria 4,163 537,000

Turkmenistan 488,100 5,110,000

Uganda 241,038 32,369,558

Uzbekistan 447,400 27,606,007

Vatican City 0.44 826

Zambia 752,612 12,935,000

Zimbabwe 390,757 12,521,000

Total 16,963,624 470,639,181

Percentage of World 11.4% 6.9%

a Has a coast on the saltwater Caspian Sea

b Has a coast on the saltwater Aral Sea

c Disputed region with limited international recognition

d Completely landlocked by exactly one country

They can be grouped in contiguous groups as follows:

Central Asian cluster (6): Afghanistan, Kazakhstan, Kyrgyzstan, Tajikistan, Turkmenistan, Uzbekistan

European cluster (9): Austria, Czech Republic, Hungary, Kosovo (partially recognized), Liechtenstein, Macedonia, Serbia, Slovakia and Switzerland

Central and East African cluster (10): Burkina Faso, Burundi, Central African Republic, Chad, Mali, Niger, Rwanda, Uganda, Ethiopia, South Sudan

South African cluster (4): Botswana, Malawi, Zambia, Zimbabwe

Caucasian cluster (3): Armenia, Azerbaijan, Nagorno-Karabakh (unrecognized)

South American cluster (2): Bolivia, Paraguay

If it were not for the 40 km of coastline at Muanda, DR Congo would join the two African clusters into one, making them the biggest contiguous group in the world.

There are the following 'single' landlocked countries (each of them borders no other landlocked country):

Africa (2): Lesotho, Swaziland

Asia (4): Bhutan, Laos, Mongolia, Nepal

Europe (6): Andorra, Belarus, Luxembourg, Moldova, San Marino, and the State of the Vatican City

Caucasus (1): South Ossetia (partially recognized)

If Transnistria is included then Moldova and Transnistria form their own cluster.

If the Caucasian countries are counted as part of Europe, then Europe has the most landlocked countries, at 19. Kazakhstan is also sometimes regarded as a transcontinental country, so if that is included, the count for Europe goes up to 20. If these countries are included in Asia, then Africa has the most, at 16. Depending on the status of the three transcontinental countries, Asia has between 9 and 14, while South America has only 2. North America and Oceania are the only continents with no landlocked countries.

Doubly landlocked country

A landlocked country surrounded only by other landlocked countries may be called a "doubly landlocked" country. A person in such a country has to cross at least two borders to reach a coastline.

There are currently two such countries in the world:

Liechtenstein in Central Europe surrounded by Switzerland and Austria.

Uzbekistan in Central Asia surrounded by Afghanistan, Kazakhstan, Kyrgyzstan, Tajikistan, and Turkmenistan.

Uzbekistan has borders with Turkmenistan and Kazakhstan that border the landlocked but saltwater Caspian Sea, from which ships can reach the Sea of Azov by using the man-made Volga-Don Canal, and thence the Black Sea, the Mediterranean Sea, and the oceans.

There were no doubly landlocked countries in the world from the Unification of Germany in 1871 until the end of World War I. This is because Uzbekistan was part of the Russian Empire, and thus part of a country that was not landlocked; while Liechtenstein bordered Austria-Hungary, a country which had an Adriatic coast until it was dissolved in 1918. Upon the dissolution of Austria-Hungary Liechtenstein became a doubly landlocked country. There were again no doubly landlocked countries from 1938 until the end of World War II, as Nazi Germany had incorporated Austria, which meant that Liechtenstein bordered a country with a coast. After World War II Austria regained its independence and Liechtenstein became doubly landlocked once more. Upon the dissolution of the Soviet Union, Uzbekistan became the second doubly landlocked country.

Great Salt Lake

Great Salt Lake, located in the northern part of the U.S. state of Utah, is the largest salt water lake in the western hemisphere, the fourth-largest terminal lake in the world, and the 37th-largest lake on Earth. In an average year the lake covers an area of around 1,700 square miles (4,400 km2), but the lake's size fluctuates substantially due to its shallowness. For instance, in 1963 it reached its lowest recorded level at 950 square miles (2,460 km²), but in 1987 the surface area was at the historic high of 3,300 square miles (8,500 km2).

The lake is the largest remnant of Lake Bonneville, a pluvial lake which covered much of western Utah in prehistoric times. The Great Salt Lake is endorheic (has no outlet besides evaporation) and has very high salinity, far saltier than sea water. The Jordan, Weber, and Bear rivers (the three major tributaries) deposit around 1.1 million tons of minerals in the lake each year, and since water (but not the minerals) is constantly being evaporated, the concentration of minerals increases further. Because of its unusually high salt concentration, most people can easily float in the lake as a result of the higher density of the water, particularly in the saltier north arm of the lake, Gunnison Bay. The lake's shallow, warm waters cause frequent, sometimes heavy lake-effect snows during late fall, early winter, and spring.

Although it has been called "America's Dead Sea", the lake provides habitat for millions of native birds, brine shrimp, shorebirds, and waterfowl, including the largest staging population of Wilson's Phalarope in the world.

Island

Categorically stating the number of islands is difficult, as the method used to determine what is an island is not necessarily the same in each source. Since the water level of the lake can vary greatly between years, what may be considered an island in a high water year may be considered a peninsula in another, or an island in a low water year may be covered during another year. According to the US Dept of the Interior/US Geological Survey, "there are eight named islands in the lake that have never been totally submerged during historic time. All have been connected to the mainland by exposed shoals during periods of low water." In addition to these eight islands, the lake also contains a number of small islands, rocks, or shoals which become fully or partially submerged at high water levels.

The Utah Geological Survey, on the other hand, states "the lake contains 11 recognized islands, although this number varies depending on the level of the lake. Seven islands are in the southern portion of the lake and four in the northwestern portion."

The size and whether they are counted as islands during any particular year depends mostly on the level of the lake. From largest to smallest, they are Antelope, Stansbury, Fremont, Carrington, Dolphin, Cub, Badger, Strongs Knob, Gunnison, Goose, Browns, Hat (Bird), Egg Island, Black Rock and White Rock. Dolphin, Gunnison, Cub, and Strongs Knob are in the northwest arm. The rest are in the southern portion. There are also a number of small, unnamed islands.

Commerce

With its sudden storms and expansive spread, the lake is a great test of sailing skills. Single mast, simple sloops are the most popular boats. Sudden storms and lack of experience on the part of boatmen are the two most dangerous elements in boating and sailing on the Great Salt Lake.

The lake's north arm contains deposits of oil, but it is of poor quality and it is not economically feasible to extract and purify it. As of 1993, around 3,000 barrels (480 m3) of crude oil had been produced from shallow wells along the shore.

Solar evaporation ponds at the edges of the lake produce salts and brine (water with high salt quantity). Minerals extracted from the lake include: sodium chloride (common salt), used in water softeners, salt lick blocks for livestock, and to melt ice on local roadways; potassium sulfate (potash), used as a commercial fertilizer; and magnesium-chloride brine, used in the production of magnesium metal, chlorine gas, and as a dust suppressant. Food-grade salt is not produced from the lake, as it would require further costly processing to ensure its purity. Mineral-extraction companies operating on the lake pay royalties on their products to the State of Utah, which owns the lake.

The harvest of brine shrimp cysts during fall and early winter has developed into a significant local industry, with cysts selling for as high as $35 a pound. Brine shrimp were first harvested during the 1950s and sold as commercial fish food. In the 1970s the focus changed to their eggs, known as cysts, which were sold primarily outside of the United States to be used as food for shrimp, prawns, and some fish. Today, these are mostly sold in the Orient and South America. The amount of cysts and the quality are affected by several factors, but salinity is most important. The cysts will hatch at 2 to 3% salinity, but the greatest productivity is at salinities above about 10%. If the salinity drops near 5 to 6%, the cysts will lose buoyancy and sink, making them more difficult to harvest.

A large resort called Saltair has been operated on the southern shore of the lake off and on for many years. Rising and lowering water levels have affected Saltair, and it has burned down twice. Currently it serves as a concert venue. The new resort, built in 1981 after large fires completely destroyed the second and largest in the 1960s, is only a shadow of the resort's former grandeur.

Dramatically fluctuating lake levels have inhibited the creation and success of tourist-related developments. There is a problem with pollution of the lake by industrial and urban effluent. Also, especially when the waters are low, decay of insects and other wildlife give the shore of the lake a distinctive odor which may keep some tourists from coming near the lake. Despite these issues, the lake remains one of Utah's largest tourist attractions. Antelope Island State Park is a popular tourist destination that offers panoramic views of the lake, hiking and biking trails, wildlife viewing and access to beaches.

Miscellaneous

The Great Salt Lake as seen looking north towards Antelope Island from Sunset Beach

Spiral Jetty

The northwest arm of the lake, near Rozel Point, is the location for Robert Smithson's work of land art, Spiral Jetty (1970), which is only visible when the level of Great Salt Lake drops below 4,197.8 feet (1,280.2 m) above sea level.

Oolitic sand

The lake and its shores contain oolitic sand, which are small, rounded, or spherical grains of sand made up of a nucleus (generally a small mineral grain) and concentric layers of calcium carbonate (lime) and look similar to very small pearls.

Lake monster

In mid-1877, J.H. McNeil was with many other Barnes and Co. Salt Works employees on the lake’s north shore in the evening. They claimed to have seen a large monster with a body like a crocodile and a horse’s head in the lake. They claimed this monster attacked the men, who quickly ran away and hid until morning. This creature is regarded by some to have simply been a buffalo in the lake. Thirty years prior, "Brother Bainbridge" claimed to have sighted a creature that looked like a dolphin in the lake near Antelope Island. This monster is called by some the North Shore Monster.

History

While the lake was well known by local Native Americans, it entered the annals of written history through the records of Silvestre Vélez de Escalante, who learned of its existence from the Timpanogos Utes in 1776. No name was given to it at the time, and it was not shown on the map by Bernardo Miera y Pacheco, the cartographer for the expedition. It was first seen by Europeans in 1824, apparently independently, by Jim Bridger and Etienne Provost. Shortly thereafter other trappers saw it and walked around it.

Most of the trappers, however, were illiterate and did not record their discoveries. As oral reports of their findings made their way to those who did make records, some errors were made. Escalante had been on the shores of Utah Lake, which he named Laguna Timpanogos. It was the larger of the two lakes that appeared on Miera's map. Other cartographers followed his lead and charted Lake Timpanogos as the largest (or larger) lake in the region. As people came to know of Great Salt Lake, they interpreted the maps to think that "Timpanogos" referred to Great Salt Lake. On some maps the two names were used synonymously. In time "Timpanogos" was dropped from the maps and its original association with Utah Lake was forgotten.