Independence Day of the Dominican Republic

Dominican Republic, country of the West Indies that occupies the eastern two-thirds of Hispaniola, the second largest island of the Greater Antilles chain in the Caribbean Sea. Haiti, also an independent republic, occupies the western third of the island. The Dominican Republic’s shores are washed by the Caribbean to the south and the Atlantic Ocean to the north. Between the eastern tip of the island and Puerto Rico flows the Mona Passage, a channel about 80 miles (130 km) wide. The Turks and Caicos Islands are located some 90 miles (145 km) to the north, and Colombia lies about 300 miles (500 km) to the south. The republic’s area, which includes such adjacent islands as Saona, Beata, and Catalina, is about half the size of Portugal. The national capital is Santo Domingo, on the southern coast. The Dominican Republic has much in common with the countries of Latin America (with which it is often grouped), and some writers have referred to the country as a microcosm of that region. Dominicans have experienced political and civil disorder, ethnic tensions, export-oriented booms and busts, and long periods of military rule, including a Haitian occupation (1822–44), the oppressive dictatorship of Rafael Trujillo (1930–61), and military interventions by the United States (1916–24 and 1965–66). However, the nation’s troubles have paled in comparison with those of neighbouring Haiti. The two countries have long been strategic because of their proximity to the United States and their positions on major sea routes leading to the Caribbean and the Panama Canal. The land Relief, drainage, and soils The Dominican Republic includes the highest and lowest elevations in the West Indies. Its major mountain ranges and elongated, fertile valleys mainly extend from northwest to southeast. The Cordillera Septentrional, the northernmost range, looms above a narrow coastal plain drained by such short rivers as the Balabonico and the Yasica. The southern slopes of the mountains give way to the extensive Cibao Valley, which stretches from Manzanillo Bay in the northwest to the Samaná Peninsula and the Bay of Samaná in the east. The valley’s fertile soils are fed by two of the nation’s main river systems: the Yaque del Norte, which flows generally northwestward, and the Camu-Yuna system, which flows eastward. The Cordillera Central, the island’s most rugged and imposing feature, is known in Haiti as the Massif du Nord (“Northern Massif”). In Dominican territory its crest line averages some 6,000 feet (1,800 metres) in elevation and rises to 10,417 feet (3,175 metres) at Duarte Peak, the highest mountain in the Caribbean. Other prominent peaks are Yaque, La Rucilla, Bandera, and Mijo. Tributaries of the Yaque del Norte drain most of the range’s northern flanks, whereas its southern flanks are drained by the Yaque del Sur system and the Ocoa, Nizao, and other smaller rivers. The San Juan River, one of the Yaque del Sur’s main tributaries, is the centrepiece of the fertile San Juan Valley, which connects with Haiti’s Central Plateau via the upper Artibonite River valley. Bounding the San Juan Valley to the south is the Sierra de Neiba, which corresponds to the Matheux and Trou d’Eau mountains of Haiti; its high peaks reach approximately 7,200 feet (2,200 metres). Water flowing off the Neiba range drains partly to the Caribbean, via the Yaque del Sur system, and partly inland, to saline Lake Enriquillo. Enriquillo is the country’s largest natural lake, about 23 miles (37 km) long and up to 11 miles (18 km) wide; the lake’s surface is also the lowest point in the West Indies, at 144 feet (44 metres) below sea level. The Dominican Republic’s southernmost range, the Sierra de Baoruco (Bahoruco), is called the Massif de la Selle in Haiti; it overlooks Cape Beata and the arid southwestern plain, including the largely infertile Pedernales region. The Cordillera Oriental forms the country’s less-rugged eastern spine, separating a narrow coastal plain to the north from a wider belt of rolling lowlands to the south, where most of the country’s sugarcane is grown. The region’s main rivers all flow to the Caribbean, including the Ozama, which reaches the coast at Santo Domingo, and the Macorís, Soco, Chavón, and Yuma. The country’s most fertile alluvial soils are located in the valleys of the Yaque del Norte, Yuna, San Juan, and Yaque del Sur rivers, as well as the Ozama and various smaller rivers in the southeast. The mountain slopes have lower-quality soils and are generally covered in forests and grasslands. Salt deposited around Lake Enriquillo creates some of the nation’s only unproductive soils. Climate The Dominican Republic has a moderate, relatively mild tropical climate, although it lies well within the tropical zone. Conditions are ameliorated in many areas by elevation and by the northeast trade winds, which blow steadily from the Atlantic all year long. The annual mean temperature is 77 °F (25 °C); regional mean temperatures range from 69 °F (21 °C) in the heart of the Cordillera Central to as high as 82 °F (28 °C) on the coastal plains. Temperatures rarely rise above 90 °F (32 °C), and freezing temperatures are unknown. The heaviest precipitation is in the mountainous northeast (the windward side of the island), where the average annual rainfall is more than 100 inches (2,540 mm). As the trade winds pass over the country, they lose their moisture on various mountain slopes, so that the far western and southwestern valleys, along the Haitian border, remain relatively dry, with less than 30 inches (760 mm) of annual precipitation. The northwestern and southeastern extremes of the country are also arid. The Dominican Republic is occasionally damaged by tropical storms and hurricanes, which originate in the mid-Atlantic and southeastern Caribbean from August until October each year; hurricanes in 1930, 1954, 1979, and 1998 were particularly devastating. Plant and animal life Vegetation varies considerably, but there is generally more ground cover in the Dominican Republic than in neighbouring Haiti. The mountains are still largely forested with pines and tropical hardwoods, although the trees on the lower and more accessible slopes have been severely cut for use as charcoal and commercial lumber. In the drier regions low shrubs and scrub predominate, but grasslands and dense rainforests occur where there is heavier precipitation. Royal palms grow throughout much of the country. Cultivated crops have largely replaced the natural vegetation in many areas, particularly in the more fertile upland valleys and on the lower mountain slopes. Mangrove swamps line some coastal areas, whereas extensive sandy beaches are found elsewhere, notably along the northern shore. Wild animals are not abundant; for several centuries cattle and goats, introduced by the early Spanish colonists, ran wild on the grasslands and in the desert areas. Alligators are found near the mouths of the Yaque rivers and in the waters of Lake Enriquillo. A great variety of birds, including ducks, are hunted. Fish and shellfish inhabit the surrounding waters, particularly within the coral reefs. Settlement patterns The nation’s coasts and interior plains have been inhabited since Arawak Indians maintained villages there in pre-Columbian times. Settlement from the late 15th century was closely tied to sugarcane plantations and export-oriented commerce. Throughout the colonial period the population of European colonists and African slaves grew slowly, and their mulatto (mixed African and European) descendents now predominate in most regions of the country. People of mainly European descent inhabit the southeastern savannas, which include large sugar plantations, cattle ranches, and small and medium-size farms. However, the southeastern coastline itself is increasingly inhabited by Blacks from Haiti and other West Indian nations who have gone there to work on the plantations, in the mills, or on the docks; most are temporary or seasonal workers. Many of the inhabitants of the town of Azua and its environs are the descendants of immigrants from the Canary Islands.Santo Domingo, the nation’s largest city, is central to one of the nation’s most densely populated regions; founded by the Spanish in 1496, it was the first permanent town established by Europeans in the Americas. The Cibao Valley is also densely settled, particularly in its central and eastern sections at Santiago, San Francisco de Macorís, and La Vega. Santiago, the nation’s second largest city, vies with Santo Domingo in political, cultural, and economic matters. Secondary coastal centres include La Romana and San Pedro de Macorís in the southeast, Barahona in the southwest, and Puerto Plata in the north. South of the Cordillera Central lies an alluvial plain where rice is grown; its population is centred on San Juan de la Maguana. Traditionally, the Dominican Republic had a large rural population, but growing numbers have moved to cities and towns since the mid-20th century, and today about fourth-fifths of the population is urban In rural areas some settlements exist as well-defined villages, but most take the form of scattered neighbourhoods, typically clustered around a small store or church or stretched along a roadside, with cultivated patches behind the houses. In addition, there are still many households so isolated from roadways that they can be reached only on foot or horseback. The people - Ethnicity The population of the Dominican Republic is predominantly of mixed African and European ethnicity, and there are small Black and white minorities. It has long been believed that few people are descended, even indirectly, from the indigenous Taino peoples, who were largely decimated by disease, warfare, and the effects of forced labour shortly after their first contact with Europeans. Some scholars, however, have argued that Taino legacy is more pronounced than this, both genetically in the current population and in terms of survival elements in Dominican language and material culture. The colonizing whites, mostly Spaniards, were joined in the 19th and 20th centuries by immigrants from East Asia and from such European countries as France, Italy, England, and Germany, as well as by small numbers of Sephardic Jews and Arabs from North Africa and the Middle East. This last group of immigrants at first competed with Chinese peddlers and shopkeepers in the rural areas, but most later moved to the cities, where they now occupy positions in commerce and industry. The Chinese particularly established themselves in the hotel and restaurant business. A small group of Japanese developed truck farming in the Constanza River valley before World War II, and their descendants are now found throughout the republic. Intermarriage among all these groups has blurred, but not erased, their ethnic origins. The exact African heritage of the large Black population is unknown, although many of their ancestors arrived as slaves from West Africa. Some were brought in within the first two decades of the Spanish conquest to work in mines and early sugar plantations. Others came indirectly, via the French colony of Saint-Domingue (later independent Haiti), particularly during the early 19th century when Haitian troops occupied the Dominican Republic. Haitian workers without immigration papers have long crossed over the mountainous frontier between the two countries; other Haitians have worked legally in the south as itinerant cane cutters, and some have found ways to remain after their contracts expired. Language and religion The Spanish language has always been predominant, although English is becoming more common because of continued emigration to the United States—which has been accompanied by continual visiting back and forth—plus some repatriation. A French Creole is spoken among Haitian immigrants. More than four-fifths of the people are adherents to the Roman Catholic church, which exerts a marked influence on all levels of cultural, political, and economic life. Many of the religious beliefs and practices of the rural populace are syncretic, rooted in the cultures of both the early Spanish and African communities. Evangelical groups account for a small but growing segment of the population. There are a few adherents of Judaism and other religions. Demographic trends The rate of population increase in the Dominican Republic is greater than in most other West Indian nations, and about three-tenths of the population is less than 15 years of age. Both birth and death rates in the republic have long been higher than the regional average, although they have been lower than in Haiti (see Health and welfare). The country experienced one of the world’s highest urbanization rates in the late 20th century: in 1950 roughly one-fourth of Dominicans lived in cities, but by the late 1990s nearly two-thirds of the population was urban. Santo Domingo expanded into formerly rural zones as it became more crowded, and its urban slums grew as well. Santiago, La Romana, and other cities also grew considerably. The Dominican Republic’s high rate of emigration has been primarily directed to New York City and other cities in the United States. Since the mid-1960s more than one-tenth of the total population has emigrated, principally to improve their economic situation; many have been illegal immigrants. The outward flow of people alleviated the strain on local resources (notably housing, water supplies, and food production) while boosting many families’ incomes with remittances of cash and consumer goods. More … Source: https://www.britannica.com/place/Dominican-Republic

2026/02/27

e-Estonia - We have built a digital society & we can show you ...

Experience Estonian digitalisation, gain insights on how to build a digital society & meet Estonian companies behind our e-solutions.

2026/02/26

Me Gusta República Dominicana | Ministerio de Turismo

Me Gusta República Dominicana | Ministerio de Turismo

2026/02/26

National Day of Kuwejt

Kuwait, country of the Arabian Peninsula located in the northwestern corner of the Persian Gulf. A small emirate nestled between Iraq and Saudi Arabia, Kuwait is situated in a section of one of the driest, least-hospitable deserts on Earth. Its shore, however, includes Kuwait Bay, a deep harbour on the Persian Gulf. There, in the 18th century, Bedouin from the interior founded a trading post. The name Kuwait is derived from the Arabic diminutive of the Hindustani kūt (“fort”). Since the emirate’s ruling family, the Āl Ṣabāḥ, formally established a sheikhdom in 1756, the country’s fortunes have been linked to foreign commerce. In time and with accumulated wealth, the small fort grew to become Kuwait city, a modern metropolis mingling skyscrapers, apartment buildings, and mosques. Kuwait city has most of the country’s population, which makes Kuwait one of the world’s most-urbanized countries. The tiny country, which was a British protectorate from 1899 until 1961, drew world attention in 1990 when Iraqi forces invaded and attempted to annex it. A United Nations coalition led by the United States drove Iraq’s army out of Kuwait within days of launching an offensive in February 1991, but the retreating invaders looted the country and set fire to most of its oil wells (see Persian Gulf War). Kuwait has largely recovered from the effects of the war and again has one of the highest per capita incomes in the world. Its generally conservative government continues to provide generous material benefits for Kuwaiti citizens, and, though conservative elements in its society resisted such reforms as women’s suffrage (women were not enfranchised until 2005), it has remained relatively stable. It has been called an “oasis” of peace and safety amid an otherwise turbulent region. Land Slightly larger in area than the U.S. state of Hawaii, Kuwait is bounded to the west and north by Iraq, to the east by the Persian Gulf, and to the south by Saudi Arabia. Kuwait Towers The Kuwait Towers, containing two water reservoirs and restaurants, in Kuwait city, Kuwait. Kuwait is largely a desert, except for Al-Jahrāʾ oasis, at the western end of Kuwait Bay, and a few fertile patches in the southeastern and coastal areas. Kuwaiti territory includes nine offshore islands, the largest of which are the uninhabited Būbiyān and Al-Warbah. The island of Faylakah, which is located near the entrance of Kuwait Bay, has been populated since prehistoric times. A territory of 2,200 square miles (5,700 square km) along the gulf was shared by Kuwait and Saudi Arabia as a neutral zone until a political boundary was agreed on in 1969. Each of the two countries now administers half of the territory (called the Neutral, or Partitioned, Zone), but they continue to share equally the revenues from oil production in the entire area. Although the boundary with Saudi Arabia is defined, the border with Iraq remains in dispute. Relief The relief of Kuwait is generally flat or gently undulating, broken only by occasional low hills and shallow depressions. The elevations range from sea level in the east to 951 feet (290 metres) above sea level at Al-Shiqāyā peak, in the western corner of the country. The Al-Zawr Escarpment, one of the main topographic features, borders the northwestern shore of Kuwait Bay and rises to a maximum elevation of 475 feet (145 metres). Elsewhere in coastal areas, large patches of salty marshland have developed. Throughout the northern, western, and central sections of Kuwait, there are desert basins, which fill with water after winter rains; historically these basins formed important watering places, refuges for the camel herds of the Bedouin. Drainage Kuwait has no permanent surface water, either in the form of standing bodies such as lakes or in the form of flows such as perennial rivers. Intermittent water courses (wadis) are localized and generally terminate in interior desert basins. Little precipitation is absorbed beyond the surface level, with most being lost to evaporation. Soils True soils scarcely exist naturally in Kuwait. Those that exist are of little agricultural productivity and are marked by an extremely low amount of organic matter. Eolian soils and other sedimentary deposits are common, and a high degree of salinity is found, particularly in basins and other locations where residual water pools. One of the environmental consequences of the Persian Gulf War was the widespread destruction of the desert’s rigid surface layer, which held underlying sand deposits in place; this has led to an increase in wind-borne sand and the creation of larger and more numerous sand dunes in the country. Climate The climate is desert, tempered somewhat in the coastal regions by the warm waters of the gulf. If there is enough rainfall, the desert turns green from mid-March to the end of April. But during the dry season, between April and September, the heat is severe—daytime temperatures ordinarily reach 111 °F (44 °C) and on occasion approach 130 °F (54 °C). The winter is more agreeable (frost can even occasionally occur in the interior, though never on the seacoast). Annual rainfall averages only from 1 to 7 inches (25 to 180 mm), chiefly between October and April, though cloudbursts can bring more than 2 inches (50 mm) of rain in a single day. The frequent winds from the northwest are cool in winter and spring and hot in summer. Southeasterly winds, usually hot and damp, spring up between July and October; hot and dry south winds prevail in spring and early summer. The shamāl, a northwesterly wind common during June and July, causes dramatic sandstorms. Plant and animal life Except in the new green belt of Kuwait city and in a few desert oases such as Al-Jahrāʾ, where cultivation and irrigation are carried out, the vegetation consists of scrub and low bushes (and ephemeral grass in the spring). Halophytes (salt-loving plants) grow on the marshy stretches along the coast. The harsh climate limits mammals to the occasional gazelle, fox, or civet. Among lizards are the rare and venomous sand viper (Cerastes vipera) and the monitor and vegetarian dab lizards (Uromastix spinipes). People Historically, there were several important class divisions in Kuwait. These divisions emerged during the period when the country was a trade entrepôt and were largely economic; thus, as the state became Kuwait’s primary employer after oil was discovered in the 1930s and these reserves were commercially developed in subsequent decades, this class structure became less pronounced. The one historically important class that remains politically important is the old merchant oligarchy, the Banū (Banī) ʿUtūb—of which the ruling family is a member. Ethnic groups Despite a government policy to reduce the number of foreign workers following the Iraqi invasion in 1990, Kuwaitis remain a minority in their own country. About two-thirds of the population are expatriate workers, formerly from other Arab states but now largely from South and Southeast Asia. These nonnationals do not enjoy citizenship rights, economic or political, which are reserved for Kuwaiti citizens—defined as those able to prove Kuwaiti ancestry prior to 1920. Naturalization is strictly limited. Arabs—either Bedouin, sedentary, or descendants of immigrants from elsewhere in the region—constitute the largest ethnic group, and a small number of ethnic Persians have resided in the country for centuries. Languages The native and official language is Arabic, fluency in which is a requirement for naturalization. Kuwaitis speak a dialect of Gulf Arabic, and Modern Standard Arabic is taught in schools. English is the second language taught in public schools. Hindi, Urdu, Persian (Farsi), and other languages also are widely spoken among the foreign population. Religion Kuwaiti citizens are almost entirely Muslim, and a law passed in 1981 limits citizenship to Muslims. The majority are Sunni, but about one-third are Shiʿi. Both the Iranian revolution of 1979 and the Kuwaiti government’s subsequent discrimination against the Shiʿah fostered a heightened sense of community among the country’s Shiʿi population in the 1980s and ’90s, and this led to political tension between the two groups. Settlement patterns The old town of Kuwait, although located in a harsh desert climate, opened onto an excellent sheltered harbour. Kuwait developed in the 18th and 19th centuries as a trading city, relying on the pearl banks of the gulf as well as on long-distance sea and caravan traffic. The old city—facing the sea and bounded landward from 1918 to 1954 by a mud wall, the gates of which led out into the desert—was compact, only 5 square miles (13 square km) in area; its typical dwelling was a courtyard house. After the discovery of oil in the 1930s and the petroleum industry’s rapid expansion after World War II, Kuwait city underwent a transformation. The ensuing urban explosion led to the destruction of the semicircular city wall (its gates were preserved as a reminder of the early years), and city planners formally laid out new suburbs. The government invested large portions of oil revenues in infrastructure and urban development, creating in the process a modern metropolis. Kuwaitis are now scattered at a relatively low density throughout the urban area and surrounding suburbs. Non-Kuwaitis, largely excluded from the restricted suburbs, live at higher densities in the old city and in the suburbs of Ḥawallī and Al-Sālimiyyah, mostly in apartments. Demographic trends Until the Iraqi invasion, Palestinians, some of them third-generation residents of Kuwait, were the largest single expatriate group, numbering perhaps 400,000. Popular Palestinian support for Iraq during the war and persistent Palestinian demands for political inclusion led the Kuwaiti government to deport most of them following the restoration of authority, and by early 1992 their number had fallen to 50,000. They have been largely replaced by Egyptians, Syrians, Iranians, and South Asians. Life expectancy in Kuwait is high, with males living to about 77 years and females to 79. Although Kuwait’s birth rate is roughly equal to the world average, its low death rate has led to a high rate of natural increase. The leading cause of death is circulatory disease. The country is young, with roughly one-fourth of the population under the age of 15. Economy Virtually all of Kuwait’s wealth is derived directly or indirectly, by way of overseas investments, from petroleum extraction and processing. The most dramatic element of Kuwait’s economic development has been the steady and rapid expansion of its oil industry since the 1970s. By the mid-1980s Kuwait was refining four-fifths of its oil domestically and marketing some 250,000 barrels a day in its own European retail outlets under the name “Q8.” This oil income and the investment income it generated—the latter surpassed direct sales of oil revenues by the 1980s—gave Kuwait one of the highest per capita incomes in the world. However, both the Iraqi invasion (which nearly exhausted Kuwait’s overseas investment revenues) and the increasing volatility of the global oil market in the 1980s reduced this income substantially, but income levels rebounded when oil prices rose dramatically in the early 21st century. Other sectors of Kuwait’s economy are weak by comparison; agriculture, manufacturing, and trade each constitute only a small proportion of gross domestic product (GDP). Agriculture and fishing The possibilities of agricultural development are severely limited. Only a small amount of the land is arable, and, because of scarcity of water, soil deficiencies, and lack of workers trained in agricultural skills, only a portion of that land area is under actual cultivation. Agriculture’s contribution, therefore, is insignificant to the output of the economy. Fish are plentiful in the Persian Gulf, and fishing in Kuwait was a leading industry before the discovery of oil. The United Fisheries of Kuwait continues the tradition today. Shrimp was one of the few commodities besides oil that Kuwait continued to export after World War II. Shrimp production, devastated by the environmental havoc wreaked in the gulf by the Persian Gulf War, had recovered by the mid-1990s. Resources and power Kuwait has nearly one-tenth of the world’s proven oil reserves. Kuwait’s proven recoverable reserves are thought to be enough to sustain current production levels for some 150 years, and, though the oil industry sustained severe damage during the Iraqi invasion, most of that was repaired by the mid-1990s. Kuwait also has considerable natural gas reserves, almost all in the form of associated gas—i.e., gas that is produced together with crude oil. There are no other important minerals. Naturally occurring fresh water is scarce; until desalination plants were built after World War II, water had to be imported. The generation of electricity also has increased significantly as population and industry have grown. Production is concentrated in several large natural-gas–fired power stations, including one at Al-Shuwaykh and another at Al-Shuʿaybah. Oil In 1934 the Kuwait Oil Company (KOC), the ownership of which was divided equally between what were then the British Petroleum Company and the Gulf Oil Corporation (of the United States), obtained a concession covering the whole territory except the Neutral Zone. Oil was struck in 1938, but World War II deferred development until 1946. Thereafter, progress was spectacular. In 1953 the American Independent Oil Company and the Getty Oil Company, which jointly held concessions for the Neutral Zone, struck oil in commercial quantities, and in 1955 oil was discovered in northern Kuwait. By 1976 Kuwait had achieved complete control of the KOC, with the former owners retaining the right to purchase at a discount. The government also achieved full ownership of the Kuwait National Petroleum Company (KNPC), which it had formed in 1960 with private Kuwaiti investors. The KNPC, designed to serve as an integrated oil company, controlled the supply and distribution of petroleum products within the country and began marketing operations abroad. In 1980 the government founded the Kuwait Petroleum Corporation as an umbrella organization overseeing the KOC and the KNPC as well as the Kuwait Oil Tanker Company, the Petrochemicals Industries Company, and the Kuwait Foreign Petroleum Exploration Company. The relatively low cost of oil production in Kuwait stems from certain unique advantages. Most important, there are a number of highly productive wells, the output of which can be varied at short notice, which thus eliminates the need for large numbers of storage tanks. Most of the storage tanks themselves are placed on a ridge set back a few miles from the seacoast at a height of some 300 feet (90 metres); this enables loading operations to be carried out by gravity rather than by pumps. There are also extensive refineries and bunkers for tankers. While retreating from Kuwait at the end of the Persian Gulf War, Iraqi forces set fire to more than 700 of the country’s 950 wells. By the fall of 1991, the fires, which had consumed about six million barrels of oil per day, had been extinguished, and production soon returned to preinvasion levels. More …. Source: https://www.britannica.com/place/Kuwait  

2026/02/25

Brunei Tourism – Abode of Peace

Browse through our website, find your next travel inspiration with us and start planning for your dream vacation in the Abode of Peace. Brunei Tourism.

2026/02/25

Destination Guyana

Explore the cities and towns of Guyana, which make for exciting gateways into the rainforest and savannahs within the hinterland of the country. Start with

2026/02/25

Saint Lucia Caribbean Island | Official Tourism Website | Let ..

Equal parts beauty and mystique, Saint Lucia captivates anyone who sets foot on her coastline. Always evocative, she welcomes visitors with her soothing waves, ...

2026/02/24

KUWAIT - Small Country, Big Heart / الكويت بلد صغير بقلب كبير | QCPTV.com

A tourism based video taking a look at one of the smallest yet most welcoming and friendly countries in the world. As Ban Ki Moon said on the 9th of September 2014 "Kuwait may be small in size, but she has a big and compassionate heart"

2026/02/24

Independence Day of Estonia

The Estonians are first mentioned by the Roman historian Tacitus (1st century ad) in Germania. Their political system was patriarchal, based on clans headed by elders. The first invaders of the country were Vikings, who from the mid-9th century passed through Estonia and Latvia on their way to the Slavonic hinterland. In the 11th and 12th centuries, the Danes and the Swedes tried to Christianize the Estonians, without success. Between 1030 and 1192, the Russians made 13 incursions into Estonia but failed to establish supremacy. German conquest Meinhard, a monk from Holstein, landed in 1180 on what is now the Latvian coast and for 16 years preached Christianity to the Livs, a Finno-Ugric tribe. His successor, Berthold of Hanover, appointed bishop of Livonia, decided that the sword had to be used against the recalcitrant pagans. He was killed in 1198 in battle. Albert of Buxhoevden, who succeeded him as bishop, proved himself a shrewd colonizer, pacifying the “treacherous Livs” and forcing them to build the fortress of Riga. To popularize recruitment for his army, Albert dedicated Livonia to the Virgin Mary. In 1202 he established the Order of the Brothers of the Sword. By 1208 the knights were firmly established on both banks of the Western Dvina (Daugava) River, and Albert felt strong enough to proceed northward to the conquest of Estonia. In the following years, the Estonians decreased steadily in manpower, while the knights replenished theirs with new Crusaders from Germany. The Russian princes of Novgorod and Pskov also raided Estonia on many occasions, penetrating especially deep in 1212 and 1216. Finally, in a major battle in 1217, the knights defeated the Estonians and killed their commander, Lembitu. Northern Estonia and the islands, however, remained free for another 10 years. To complete the conquest, Albert concluded an alliance with King Valdemar II of Denmark, who in 1219 landed with a strong army on the northern coast, on the site of Tallinn. In 1237 the Order of the Brothers of the Sword suffered a crushing defeat and was absorbed by the Teutonic Order, which assumed control of Livonia. Northern Estonia and the islands were under Danish rule; Livonia (i.e., southern Estonia and Latvia) was shared between the Teutonic Order and the bishops. The terms under which the Estonian localities submitted were not severe, but the conquerors violated them as their position became stronger, provoking a series of revolts. After major risings in 1343–45, the Danish crown sold its sovereignty over northern Estonia to the Livonian branch of the Teutonic Order in 1346. The Germans became the masters in the “Land of the Virgin” and, with minor exceptions, dominated its government, its commerce, and the church for the next five centuries. The Estonians, the Latvians, and the Livs became the serfs of their conquerors, with little to sustain national feeling save their folklore and traditional crafts. Swedish period By the end of the 15th century, two major powers were emerging around Livonia: Poland-Lithuania, already united in the south, and Muscovy, which had conquered Novgorod, in the east. More by diplomacy than by victory in battle, Lithuania gained Livonia on the dissolution of the Teutonic Order in 1561. Three years before, northern Estonia had capitulated to the king of Sweden. The Muscovite tsar Ivan IV (the Terrible) had captured Narva in 1558 and penetrated deep into Estonia, bringing devastation with him, and it was not until 1581 that the Russians were expelled by the Swedes. In 1559 the bishop of Saaremaa had sold the Estonian islands to Denmark, but in 1645 they became part of the Swedish province. By the Truce of Altmark (1629), which ended the first Polish-Swedish war, the Polish-Lithuanian Commonwealth surrendered to Sweden the major part of Livonia, so that all Estonian lands then came under Swedish rule. Prolonged wars left the country devastated, and many farms were unoccupied. The vacancies were partly filled by foreign settlers who were soon assimilated. This also gave the German nobility the opportunity to enlarge its estates, increase taxes, and exact more unpaid labour. The Swedish kings attempted to curb the power of the nobility and improve the lot of the peasants. Soon after Charles XI of Sweden came of age (1672), the nobles of Livonia were forced to show their title deeds, and those who failed to do so became tenants of the crown. Russian conquest The “good old Swedish days” for Estonia were more a legend than reality, and they ended with the Second Northern War (Great Northern War). The Russian tsar, Peter I (the Great), was finally able to achieve the dream of his predecessors and conquer the Baltic provinces. After the defeat of Charles XII of Sweden at the Battle of Poltava (1709), Russian armies seized Livonia. The barons did not resist, angered as they were at the Swedish crown for its policy of reversion of estates. By the Peace of Nystad in 1721, Sweden ceded to Russia all its Baltic provinces. The peasants’ lot became the worst ever. In 1804, however, under Tsar Alexander I, the peasants of Livonia were given the right of private property and inheritance; a bill abolishing serfdom was passed in Estonia in 1816 and in 1819. Other agrarian laws followed—in particular that of 1863 establishing the peasants’ right of free movement, that of 1866 abolishing the landowners’ right of jurisdiction on their estates, including the right to flog, and that of 1868 abolishing the corvée. Estonian national awakening The Estonian peasants benefited from these reforms, and, at the end of the 19th century, they possessed two-fifths of the privately owned land of the country. With the growth of urban prosperity as a result of industrialization, the population increased. Improvement in education was such that by 1886 only about 2 percent of the Estonian army recruits were unable to read. National consciousness also increased. The accession of Alexander III marked the beginning of a period of more rigid Russification. The Russian municipal constitution was introduced in 1882. Russian criminal and civil codes replaced the old Baltic ones. In 1887 Russian was made the language of instruction, instead of German and Estonian. In 1893 the University of Dorpat (now Tartu), which was then an important centre of German learning, was Russified. The first reaction of the Estonians was that poetic justice was being administered to their age-old oppressors, but they also feared reactionary Pan-Slavism. In 1901 in Tallinn (Revel), Konstantin Päts founded the moderately radical newspaper Teataja. In 1904, thanks to Päts, the Estonians won a clear victory on the Tallinn town council. In January 1905 the revolution that started in Russia spread immediately to Estonia. Jaan Tönisson founded a National Liberal Party and organized its first congress in Tallinn on November 27. The 800 delegates soon split into a Liberal and a Radical wing, but both voted for resolutions demanding political autonomy for Estonia. In December Päts summoned a peasant congress in Tallinn. The Russian government responded by declaring martial law; this prompted parties of workers to scatter into the countryside, where they looted and burned manor houses. In the repression that followed, 328 Estonians were shot or hanged, and Päts and the Radical leader Jaan Teemant fled abroad, both having been sentenced—in contumacy—to death. (Päts returned in 1910.) At the elections to the first and the second Russian Duma, Estonian voters returned five deputies to the council. Independence The Russian Revolution of 1917 during World War I brought autonomy to Estonia. An Estonian National Council, which came to be known as the Maapäev, met on July 14 and on October 12 appointed a provisional government with Päts as premier. The November coup d’état that brought the Bolsheviks into power in Petrograd (St. Petersburg) made itself felt in Estonia. On Nov. 28, 1917, the Estonian Diet decided to break away from the Russian state, but on December 8 the Russian Council of People’s Commissars appointed a puppet communist government headed by Jaan Anvelt, who seized power in Tallinn but never obtained control of the whole country. In February 1918, German forces entered Estonia. The communists fled, and on February 24 the Maapäev declared Estonia independent. The following day German troops entered Tallinn. Päts was briefly arrested, and other Estonian leaders went abroad or underground. On March 3 the Treaty of Brest-Litovsk was signed; sovereignty over the Baltic countries was transferred from Russia to Germany. German rule lasted until Germany’s capitulation to the Allies on Nov. 11, 1918. The Estonian provisional government, again headed by Päts, immediately proclaimed independence, but the Soviet government declared the Treaty of Brest-Litovsk null and void, and on November 28 the Red Army took Narva and entered Estonia. Col. (later Gen.) Johan Laidoner opened a counteroffensive in January 1919, supported by weapons and war matériel from the Allies, a British naval squadron, and a Finnish voluntary force of 2,700 men. By the end of February, all Estonian territory had been freed, and the Estonian army penetrated into Soviet and Latvian territory. On June 15, 1920, the constituent assembly (elected in April 1919), with August Rei as president, adopted a new constitution providing for a single-chamber Parliament (Riigikogu) of 100 members elected for three years, a system of proportional representation, and a chief of state (riigivanem), who was also the premier. Because no party had an absolute majority, government by coalition became the rule, and, from May 1919, when the first constitutional cabinet was formed, to May 1933, Estonia had 20 coalitions headed by 10 statesmen. On Dec. 1, 1924, 300 conspirators, mostly Russians working on the transit base at Tallinn or smuggled in, tried to seize communications and call in Soviet troops but failed ignominiously. The Communist Party was outlawed, and the movement became virtually extinct. The Great Depression of the early 1930s resulted in unemployment and falling agricultural prices. The strong government action necessary to cope with the situation was precluded under the 1920 constitution. A new constitution in 1933 gave sweeping powers to the president. Päts became acting president and was expected to prepare the ground for the first presidential election. Instead, he proclaimed a state of emergency on March 12, 1934. Opposition leaders were arrested; the political activities of all parties were forbidden; and Päts assumed dictatorial powers. In December 1936, a new constituent assembly was elected. It prepared a third constitution calling for the creation of a chamber of 80 deputies elected by the majority system and a national council of 40 members. A legislative election was held in February 1938. In April Päts was elected president for a term of six years. Independence lost The fate of Estonia was decided by the German-Soviet Nonaggression Pact of August 1939 between Nazi Germany and the U.S.S.R. On September 28 the Soviet government imposed on Estonia a treaty of mutual assistance that conceded to the Soviet Union several Estonian military bases, which were occupied forthwith. A broadly based nonpolitical government under Juri Uluots was appointed, but on June 16, 1940, a Soviet ultimatum demanded a new Estonian government, “able and willing to secure the honest application of the Soviet-Estonia mutual assistance treaty.” The following day, Soviet forces occupied the whole country. On July 21 the Chamber of Deputies was presented with a resolution to join the U.S.S.R.; it was unanimously adopted the next day in spite of being contrary to constitutional procedure. On August 6 the Moscow Supreme Soviet incorporated Estonia into the U.S.S.R. as one of its constituent republics. Meanwhile, Päts, Laidoner, and many other political leaders were arrested and deported to the U.S.S.R. In the first 12 months of Soviet occupation, more than 60,000 persons were killed or deported; more than 10,000 were removed in a mass deportation during the night of June 13–14, 1941. Score: https://www.britannica.com/place/Estonia/History

2026/02/24