Independence day of Republic of Djibouti

Djibouti, small strategically located country on the northeast coast of the Horn of Africa. It is situated on the Bab el Mandeb Strait, which lies to the east and separates the Red Sea from the Gulf of Aden. Formerly known as French Somaliland (1896–1967) and the French Territory of the Afars and Issas (1967–77), the country took Djibouti as its name when it gained independence from France on June 27, 1977. Djibouti’s capital, Djibouti city, is built on coral reefs that jut into the southern entrance of the gulf; other major towns are Obock, Tadjoura, Ali Sabieh, Arta, and Dikhil. The country’s Lilliputian aspect belies its regional and geopolitical importance. The capital is the site of a modern deepwater port that serves Indian Ocean and Red Sea traffic and hosts a French naval base. Djibouti city is also the railhead for the only line serving Addis Ababa, the capital of neighbouring Ethiopia. Land - Relief Djibouti is bounded by Eritrea to the north, Ethiopia to the west and southwest, and Somalia to the south. The Gulf of Tadjoura, which opens into the Gulf of Aden, bifurcates the eastern half of the country and supplies much of its 230 miles (370 km) of coastline. The landscape of Djibouti is varied and extreme, ranging from rugged mountains in the north to a series of low desert plains separated by parallel plateaus in the west and south. Its highest peak is Mount Moussa at 6,654 feet (2,028 metres). The lowest point, which is also the lowest in Africa, is the saline Lake Assal, 509 feet (155 metres) below sea level. The country is internationally renowned as a geologic treasure trove. Located at a triple juncture of the Red Sea, Gulf of Aden, and East African rift systems, the country hosts significant seismic and geothermal activity. Slight tremors are frequent, and much of the terrain is littered with basalt from past volcanic activity. In November 1978 the eruption of the Ardoukoba volcano, complete with spectacular lava flows, attracted the attention of volcanologists worldwide. Of particular interest was the tremendous seismic activity that accompanied the eruption and led to the widening by more than a metre of the plates between Africa and the Arabian Peninsula. Drainage Besides Lake Assal, the other major inland body of water is Lake Abbe, located on Djibouti’s southwestern border with Ethiopia. The country is completely devoid of any permanent above-ground rivers, although some subterranean rivers exist. Climate The often torrid climate varies between two major seasons. The cool season lasts from October to April and typifies a Mediterranean-style climate in which temperatures range from the low 70s to the mid-80s F (low 20s to low 30s C) with low humidity. The hot season lasts from May to September. Temperatures increase as the hot khamsin wind blows off the inland desert, and they range from an average low in the mid-80s F (low 30s C) to a stifling high in the low 110s F (mid-40s C). This time of year is also noted for days in which humidity is at its highest. Among the coolest areas in the country is the Day Forest, which is located at a high elevation; temperatures in the low to mid-50s F (low to mid-10s C) have been recorded. The average annual precipitation is limited and is usually spread over 26 days. Different regions of the country receive varying amounts of precipitation: the coastal regions receive 5 inches (130 mm) of rainfall per annum, while the northern and mountainous portions of the country receive about 15 inches (380 mm). The rainy season lasts between January and March, with the majority of precipitation falling in quick, short bursts. One outcome of this erratic rainfall pattern is periodic flash floods that devastate those areas located at sea level. Plant and animal life Despite Djibouti’s relatively harsh landscape, abundances of flora and fauna abound. In the northern portion of the country, one finds the ancient Day Forest National Park and a variety of tree species, such as jujube, fig, olive, juniper, and momosa. To the south and southwest of the Gulf of Tadjoura, the vegetation is similar to that found in other arid regions of Africa, inclusive of acacia and doum palm trees. Among the types of fauna are a wide variety of bird species, numerous types of antelopes and gazelles, and more limited numbers of carnivores (such as cheetahs) and scavengers (such as hyenas), as well as monkeys, squirrels, and warthogs. Perhaps most spectacular is the extremely rich diversity of marine life found along Djibouti’s coastline and coral reefs, a factor that has made the country a special point of interest for international scuba-diving associations. People - Ethnic groups On the basis of linguistic criteria, the two largest ethnic groups are the Somali and the Afar. Both groups speak related, but not mutually intelligible, eastern Cushitic languages. The Afar (Denakil, or Danakil) speak a language that forms a dialect continuum with Saho. Saho-Afar is usually classified as an Eastern Cushitic language of the Afro-Asiatic language phylum. The Afar live in the sparsely populated areas to the west and north of the Gulf of Tadjoura. This region includes parts of several former as well as extant Afar sultanates. The sultans’ roles are now largely ceremonial, and the social divisions within the traditional Afar hierarchy are of diminished importance. The Afar are also found across the border in neighbouring Ethiopia. Their population distribution in the two countries forms a pattern that is somewhat elongated and triangular in shape and is often referred to as the “Afar triangle.” The Somali, who also speak an Eastern Cushitic language, are concentrated in the capital and the southeastern quarter of the country. Their social identity is determined by clan-family membership. More than half the Somali belong to the Issa, whose numbers exceed those of the Afar; the remaining Somali are predominately members of the Gadaboursi and Isaaq clans that migrated from northern Somalia during the 20th century to work on the construction of the Djibouti–Addis Ababa railway and Djibouti city’s port expansion. Djibouti city is home to a long-established community of Yemeni Arabs and houses a sizable contingent of French technical advisers and military personnel. In recent decades these groups have been joined by small but significant numbers of ethnic Ethiopians as well as Greek and Italian expatriates. Language of Djibouti The republic recognizes two official languages: French and Arabic. However, Somali is the most widely spoken language, although it is rarely written and is not taught in the schools. The use of Afar is mostly restricted to Afar areas. Many Djiboutians are multilingual. Fluency in French is particularly important for those with political aspirations. French is the means of instruction in primary and secondary schools, although Arabic is also taught as the first language at both these levels. Religion More than nine-tenths of the population is Muslim; nearly all adhere to the Sunni branch of Islam. Some Christian religions are represented in Djibouti, including Eastern Orthodoxy and Roman Catholicism. More: Score: https://www.britannica.com/place/Djibouti

2021/06/27

Independence Day of Republic of Madagascar

Madagascar, island country lying off the southeastern coast of Africa. Madagascar is the fourth largest island in the world, after Greenland, New Guinea, and Borneo. Although located some 250 miles (400 km) from the African continent, Madagascar’s population is primarily related not to African peoples but rather to those of Indonesia, more than 3,000 miles (4,800 km) to the east. The Malagasy peoples, moreover, do not consider themselves to be Africans, but, because of the continuing bond with France that resulted from former colonial rule, the island developed political, economic, and cultural links with the French-speaking countries of western Africa. The animal life and vegetation of the island are equally anomalous, differing greatly from that of nearby Africa and being in many respects unique. Although the coastlands have been known to Europeans for more than 400 years and to Arabs for much longer, recent historical development has been more intense and concentrated in the central plateau, which contains the capital city of Antananarivo (formerly Tananarive). Land Madagascar is located in the southwestern Indian Ocean and is separated from the African coast by the 250-mile- (400-km-) wide Mozambique Channel. Relief Madagascar consists of three parallel longitudinal zones—the central plateau, the coastal strip in the east, and the zone of low plateaus and plains in the west. Situated between 2,500 and 4,500 feet (800 and 1,400 metres) above sea level, the plateau has been uplifted and worn down several times and is tilted to the west. Three massifs are more than 8,500 feet (2,600 metres) high. The Tsaratanana region in the north is separated from the rest of the plateau by the Tsaratanana Massif, whose summit, Maromokotro, reaches 9,436 feet (2,876 metres) and is the highest point on the island. Ankaratra Massif in the centre is an enormous volcanic mass whose summit, Tsiafajavona, is 8,671 feet (2,643 metres) high. Ankaratra is a major watershed divide separating three main river basins. Farther south, Andringitra is a vast granite massif north of Tôlan̈aro (Faradofay); it rises to 8,720 feet (2,658 metres) at Boby Peak. The plateau slopes with some regularity toward the extreme southern plain, but its boundaries to the east and west are more abrupt. To the east it descends in a sharp fault, by vertical steps of 1,000 to 2,000 feet (300 to 600 metres). This cliff, which is called the Great Cliff or the Cliff of Angavo, is often impassable and is itself bordered by the Betsimisaraka Escarpment, a second and lower cliff to the east, which overhangs the coastal plain. Behind the scarp face are the remains of ancient lakes, including one called Alaotra. To the south the two steep gradients meet and form the Mahafaly and the Androy plateaus, which overhang the sea in precipitous cliffs. Toward the west the descent is made in a series of steps. However, in places the central plateau is bordered by an impassable escarpment, such as the Cliff of Bongolava in the west-central part of the island. To the extreme north the plateau is bordered by the low belt of the Ambohitra Mountains, which include a series of volcanic craters. The coastal strip has an average width of about 30 miles (50 km). It is a narrow alluvial plain that terminates in a low coastline bordered with lagoons linked together by the Pangalanes (Ampangalana) Canal, which is more than 370 miles (600 km) long. To the south of Farafangana the coast becomes rocky, and in the southeast there occur many little bays. To the northeast is the deep Bay of Antongil (Antongila). The western zone is between 60 and 125 miles (100 and 200 km) wide. Its sedimentary layers slope toward the Mozambique Channel and produce a succession of hills. The inland (eastern) side of these steep hills dominates the hollows formed in the soft sediments of the interior, while the other side descends to the sea in rocky slopes. The coastline is straight, bordered by small dunes and fringed with mangroves. The currents in the Mozambique Channel have favoured the offshore deposit of alluvium and the growth of river deltas. On the northwestern coast there are a number of estuaries and bays. This coast is bordered by coral reefs and volcanic islands, such as Nosy Be (Nossi-Bé), which protects Ampasindava Bay. Drainage The steep eastern face of the plateau is drained by numerous short, torrential rivers, such as the Mandrare, the Mananara, the Faraony, the Ivondro, and the Maningory, which discharge either into the coastal lagoons or directly into the sea over waterfalls and rapids. The more gently sloping western side of the plateau is crossed by longer and larger rivers, including the Onilahy, the Mangoky, the Tsiribihina, and the Betsiboka, which bring huge deposits of fertile alluvium down into the vast plains and many-channeled estuaries; the river mouths, while not completely blocked by this sediment, are studded with numerous sandbanks. There are many lakes of volcanic origin on the island, such as Lake Itasy. Alaotra is the last surviving lake of the eastern slope. Lake Tsimanampetsotsa, near the coast south of Toliara (formerly Tuléar), is a large body of saline water that has no outlet. Soils The central plateau and the eastern coast are mainly composed of gneiss, granite, quartz, and other crystalline rock formations. The gneiss decomposes into red murrum, laterite, and deeper and more fertile red earths, giving Madagascar its colloquial name the Great Red Island. Fertile alluvial soils in the valleys support intensive cultivation. There also are scattered volcanic intrusions that produce fertile but easily erodible soils. Lake Alaotra is a large sedimentary pocket in the central plateau containing some of the island’s most productive farmland. The western third of the island consists entirely of deposits of sedimentary rock, giving rise to soils of medium to low fertility. Climate of Madagascar The hot, wet season extends from November to April and the cooler, drier season from May to October. The climate is governed by the combined effects of the moisture-bearing southeast trade and northwest monsoon winds as they blow across the central plateau. The trade winds, which blow throughout the year, are strongest from May to October. The east coast is to the windward and has a high annual rate of precipitation, reaching nearly 150 inches (3,800 mm) at Maroantsetra on the Bay of Antongil. As the winds cross the plateau, they lose much of their humidity, causing only drizzle and mists on the plateau itself and leaving the west in a dry rain shadow. The southwest in particular is almost desert, with the dryness aggravated by a cold offshore current. The monsoon, bringing rain to the northwest coast of Madagascar and the plateau, is most noticeable during the hot, humid season. The wind blows obliquely onto the west coast, which receives a moderate amount of precipitation annually; the southwest, which is protected, remains arid. Annual precipitation drops from about 80 inches (about 2,000 mm) on the northwestern island of Nosy Be to about 40 inches (1,000 mm) at Maintirano on the west coast to about 14 inches (360 mm) at Toliara in the southwest. The plateau receives moderate levels of precipitation, with about 50 inches (1,200 mm) falling annually at both Antananarivo and Fianarantsoa, which lies about 200 miles (320 km) farther south. July is the coolest month, with mean monthly temperatures around the island ranging from the low 50s F (low 10s C) to the high 70s F (mid-20s C), and December is the hottest month, with temperatures between the low 60s and mid-80s F (mid 10s and high 20s C). Temperatures generally decrease with elevation, being highest on the northwest coast and lowest on the plateau. Tropical cyclones are an important climatic feature. They form far out over the Indian Ocean, especially from December to March, and approach the eastern coast, bringing torrential rains and destructive floods. Plant and animal life Much of the island was once covered with evergreen and deciduous forest, but little now remains except on the eastern escarpment and in scattered pockets in the west. The plateau is particularly denuded and suffers seriously from erosion. The forest has been cut in order to clear rice fields, to obtain fuel and building materials, and to export valuable timber such as ebony, rosewood, and sandalwood. About seven-eighths of the island is covered with prairie grasses and bamboo or small thin trees. There also are screw pines, palms, and reeds on the coasts. In the arid south of the island grow thorn trees, giant cacti, dwarf baobab trees, pachypodium succulents, and other xerophytes (drought-resistant plants) that are peculiar to the island. Because of the island’s isolation, many zoologically primitive primates have survived and evolved into unique forms. About 40 species of lemurs are indigenous to Madagascar. Several unique hedgehoglike insectivores, such as the tenrec, have evolved there, and there are also many kinds of chameleons of varying size. Birds are numerous and include guinea fowl, partridges, pigeons, herons, ibis, flamingos, egrets, cuckoos, Asian robins, and several kinds of birds of prey. There are about 800 species of butterflies, many moths, and a variety of spiders. The only large or dangerous animals are the crocodiles, which occupy the rivers. The snakes, including the do, which is 10 to 13 feet (3 to 4 metres) in length, are harmless. Inland waters contain tilapia (an edible perchlike fish), rainbow trout, and black bass. Marine fish and crustaceans abound on the coasts and in the lagoons, estuaries, and even in some upland streams. They include groupers, giltheads, tuna, sharks, sardines, whitings, crayfish, crabs, shrimps, mussels, and oysters. The coelacanth, referred to as a living fossil and once thought extinct for millions of years, inhabits offshore waters. More … Score: https://www.britannica.com/place/Madagascar

2021/06/26

Republic of Mozambique Independence Day

Mozambique, a scenic country in southeastern Africa. Mozambique is rich in natural resources, is biologically and culturally diverse, and has a tropical climate. Its extensive coastline, fronting the Mozambique Channel, which separates mainland Africa from the island of Madagascar, offers some of Africa’s best natural harbours. These have allowed Mozambique an important role in the maritime economy of the Indian Ocean, while the country’s white sand beaches are an important attraction for the growing tourism industry. Fertile soils in the northern and central areas of Mozambique have yielded a varied and abundant agriculture, and the great Zambezi River has provided ample water for irrigation and the basis for a regionally important hydroelectric power industry. Yet Mozambique’s turbulent recent history has kept its people from fully enjoying these natural advantages and from developing a stable, diversified economy. A former colony of Portugal, Mozambique provided mineral and agricultural products to its distant ruler while receiving few services in return. Following independence in 1975, Mozambique was torn by internal conflict as the Marxist government, supported in part by the Soviet Union and Cuba, battled anticommunist forces funded by South Africa and the former Rhodesia (now Zimbabwe) for control of the country. Marked by countless acts of terror, the ensuing warfare displaced at least four million people and resulted in the death of perhaps a million more as a result of the violence, famine, and disease it engendered. Violence and disunity hindered economic development, especially the broadening of tourism, and discouraged foreign investment. The conflict formally ended in 1992, but its lingering effects are many: in the early 21st century, as many as one million unexploded land mines still remained along the country’s trails and roads, and much political strife continued between the major opposition forces and the central government. In 2005, as part of a torch relay program to mark 30 years of independence, President Armando Guebuza noted that the torch’s flame was a symbol of Mozambique’s history and would light the people’s path “to the consolidation of independence and construction of their well-being.” As the torch was passed to a Mozambican born in the year that the country gained its independence, Guebuza remarked Handing this torch over to a youth symbolizes our certainty that the combat we wage against poverty will be continued by our young people, guardians of our glorious political, historical and cultural heritage. The capital is Maputo. Known until independence as Lourenço Marques, the city boasts fine colonial-era architecture and an attractive natural setting alongside the deepwater harbour of Maputo Bay. Maputo is the commercial and cultural centre of the country, and its sidewalk cafés, bars, and discotheques offer some of the liveliest nightlife in southern Africa. Other major cities and towns, most of which lie on or near the Indian Ocean coast, include Beira, Quelimane, Chimoio, Tete, Nampula, and Nacala. Land Mozambique is about the size of the combined areas of the U.S. states of Colorado, New Mexico, and Utah; most of its territory stretches along the Indian Ocean coast from Cape (Cabo) Delgado in the north past the capital city of Maputo in the south. It is bordered to the north by Tanzania, to the east by the Mozambique Channel, which separates it from the island of Madagascar, to the south and southwest by South Africa and Swaziland, to the west by Zimbabwe, and to the northwest by Zambia, Malawi, and Lake Nyasa. Relief Lowlands dominate the southern provinces, narrowing to a mere coastal plain north of the cleft where the Zambezi River cuts through the country’s midsection. The Zambezi valley, the lower section of which is a part of the Eastern (Great) Rift Valley, is Mozambique’s most dramatic geographic feature. Throughout the country the land rises gently from east to west. In the centre and north it slopes steadily into the high plains and ultimately to the mountainous regions on the northwest border with Malawi and Zambia. Four of Mozambique’s five highland regions straddle the west and northwest border areas: the Chimoio Plateau on the border with Zimbabwe, the Marávia highlands bordering Zambia, and the Angónia highlands and Lichinga Plateau, which lie, respectively, west and east of Malawi’s protrusion into Mozambique. Mount Binga, the country’s highest elevation at 7,992 feet (2,436 metres), is part of the Chimoio highlands. The 7,936-foot (2,419-metre) peak at Mount Namúli dominates the Mozambican highland, which constitutes much of the northern interior. Drainage of Mozambique Mozambique’s ample water resources have the potential to compensate for the mixed quality of its soils. Major river systems provide alluvial deposits and offer both hydroelectric and irrigation potential. The Rovuma (Ruvuma) River defines most of Mozambique’s northern border with Tanzania. The Zambezi River and its tributaries dominate the central region, and the Maputo River forms part of the southernmost boundary with Swaziland and South Africa. Rivers—including the Lúrio, Ligonha, Save (Sabi), Changane, and Incomáti (Komati)—also define many of the country’s local political boundaries. Other important drainage systems include the Messalo River in the north, the Púngoè (Púnguè), Revuè, and Búzi rivers, which enter the Mozambique Channel together just south of the port of Beira, and the Limpopo River in the south. The massive Zambezi flows 509 miles (819 km) through the country and drains more than 87,000 square miles (225,000 square km) of the central region. The Rovuma, Lúrio, Save, and Messalo systems follow in size, respectively. Mozambique shares the borders of Lakes Nyasa, Chiuta, and Chilwa with Malawi, but aside from these and the lakes created by the country’s hydroelectric dam network—particularly the extensive system created by the Cahora Bassa Dam at Songo on the Zambezi—the country has no important lakes. Soils Africa’s ancient basement complex of granite rock underlies most of northern and west-central Mozambique, whereas the soils of the southern and east-central regions are sedimentary. Mozambique’s soils are diverse in quality and type, but the northern and central provinces have generally more fertile, water-retentive soils than does the south, where sandy, infertile soils prevail. The northern soils, whose qualities allow agricultural potential to extend beyond the river valleys, have a higher content of red clay, with a varying range of fertility. In contrast, the central region has a broad expanse of rich alluvial soils along the Zambezi delta. South of Beira, fertility is largely limited to alluvial soils in the valleys of the Save, Limpopo, Incomáti, Umbelúzi, and Maputo rivers, although several pockets of fertile but heavy soil occur southwest of Inhambane. Mozambique lies largely within the tropics, and much of the coastline is subject to the regular seasonal influence of the Indian Ocean monsoon rains. The monsoon influence is strongest in the northeast but is modified somewhat in the south by the island barriers of Madagascar, the Comoros, and the Seychelles. With the exception of highland areas on the northern and western borders and around Gurue (east of the Malawi protrusion into Mozambique), where elevation modifies both temperature and humidity, the climate is seasonal and tropical. Daily temperatures throughout the country average in the mid- to upper 70s °F (lower to mid-20s °C), with the highest temperatures occurring between October and February and the lowest in June and July. Uncomfortably warm average daily temperatures in the upper 80s °F (low 30s °C) are normal only in the upper Zambezi valley and along the northeastern coast, while cool temperatures in the 60s °F (10s °C) occur year-round only in the mountainous areas on the western borders. Humidity and precipitation vary widely throughout the country. Again, the sharpest contrast is between north and south. The entire region north of the Zambezi and east of the Shire River valley is humid and warm, as is the coastal plain in the south, while the southern interior and most of the Zambezi valley west of the Shire are quite dry; the south-central area is even considered semiarid. Precipitation is greatest throughout the north and in the central region east of the Shire River, where it ranges between 40 and 70 inches (1,010 and 1,780 mm); the highest precipitation, averaging more than 70 inches, is in the highlands and in coastal pockets around Beira and Quelimane. In the Zambezi valley west of the Shire, however, average precipitation declines to between 24 and 32 inches (610 and 810 mm), whereas in the south, to the west of the coastal plain, average annual precipitation is only about 24 inches. The semiarid southern regions receive only about 3 inches (75 mm) of precipitation per month in the wet season from November to February and almost none in the dry season between April and October. As the annual precipitation figures suggest, west-central and southern Mozambique are subject to periodic drought. more … https://www.britannica.com/place/Mozambique

2021/06/26

Spotkanie wiceszefów dyplomacji Polski i Tadżykistanu

Tadżykistan pozostaje partnerem Polski w Azji Centralnej, zarówno w sferze polityki międzynarodowej, jak i w ujęciu regionalnym – ocenił wiceminister Marcin Przydacz po rozmowach z wiceszefem dyplomacji Tadżykistanu, Muzaffarem Huseinzodą. Sąsiedztwo Tadżykistanu z Afganistanem, w którego stabilizację Polska angażuje się od wielu lat, sprawia, że problematyka bezpieczeństwa jest jedną z najważniejszych kwestii będących przedmiotem zainteresowania Polski i Tadżykistanu.

2021/06/25

Ambasador Niemiec Arndt Freytag von Loringhoven z wizytą w Gdańsku

Nie była to w ogóle pierwsza wizyta nowego ambasadora Niemiec w Gdańsku, ale pierwsza oficjalna. Wcześniej Arndt Freytag von Loringhoven był już w naszym mieście, prywatnie i na krótko z powodu obostrzeń przeciwepidemicznych. Druga wizyta pozwoliła m.in. na spotkanie z prezydent Aleksandrą Dulkiewicz i omówienie relacji polsko-niemieckich w kontekście gdańskim.

2021/06/25

Bienal del Cusco - Convocatoria Internacional

La Embajada del Perú en Polonia tiene el agrado de informar que el Patronato Cultural del Cusco, con el valioso apoyo del Ministerio de Relaciones Exteriores del Perú, ha lanzado el evento "Independencia: Bienal de Arte de Cusco", en una edición especial por el Bicentenario de la Independencia del Perú.

2021/06/25

Statehood Day of Republic of Slovenia

Slovenia, country in central Europe that was part of Yugoslavia for most of the 20th century. Slovenia is a small but topographically diverse country made up of portions of four major European geographic landscapes—the European Alps, the karstic Dinaric Alps, the Pannonian and Danubian lowlands and hills, and the Mediterranean coast.

2021/06/25

Statehood Day of Republic of Croatia

Croatia, country located in the northwestern part of the Balkan Peninsula. It is a small yet highly geographically diverse crescent-shaped country. Its capital is Zagreb, located in the north. The present-day republic is composed of the historically Croatian regions of Croatia-Slavonia (located in the upper arm of the country), Istria (centred on the Istrian Peninsula on the northern Adriatic coast), and Dalmatia (corresponding to the coastal strip). Although these regions were ruled for centuries by various foreign powers, they remained firmly Western-oriented in culture, acquiring a legacy of Roman law, the Latin alphabet, and western European political and economic traditions and institutions. A part of Yugoslavia for much of the 20th century, Croatia suffered considerably from the disintegration of that federation in the early 1990s. The European trajectory of Croatia was finally realized in 2013 when it joined the European Union. As the Croatian Canadian scholar Tony Fabijančić writes, Croatia’s tumultuous first years as an independent country also have obscured its centuries-long history: Croatia (Hrvatska) is an ancient nation, yet a very young nation state. Once a formidable kingdom under Tomislav in the tenth century, a naval power in the sixteenth and seventeenth, and an awakening national entity in the nineteenth, it had to endure a thousand years of foreign meddling, subjugation, incursions, and outright wars before being recognized in 1992 as a distinct entity. Land The upper arm of the Croatian crescent is bordered on the east by the Vojvodina region of Serbia and on the north by Hungary and Slovenia. The body of the crescent forms a long coastal strip along the Adriatic Sea, and the southern tip touches on Montenegro. Within the hollow of the crescent, Croatia shares a long border with Bosnia and Herzegovina, which actually severs a part of southern Croatia from the rest of the country by penetrating to the Adriatic in a narrow corridor. Relief Croatia is composed of three major geographic regions. In the north and northeast, running the full length of the upper arm of the Croatian crescent, are the Pannonian and para-Pannonian plains. To the north of Zagreb, the Zagorje Hills, fragments of the Julian Alps now covered with vines and orchards, separate the Sava and Drava river valleys. To the west and south of the Pannonian region, linking it with the Adriatic coast, is the central mountain belt, itself part of the Dinaric Alps. The karst plateaus of this region, consisting mostly of limestone, are barren at the highest elevations; lower down, they are heavily forested. The highest mountain in Croatia, Dinara (6,007 feet [1,831 metres]), is located in the central mountain belt. The third geographic region, the Croatian littoral, is composed of the Istrian Peninsula in the north and the Dalmatian coast extending south to the Gulf of Kotor. Wedged between the Dinaric Alps to the east and the Adriatic Sea to the west, its 1,100 miles (1,800 km) of coastline are fringed by more than 1,100 islands and islets. Drainage Of the 26 rivers that flow for more than 30 miles (50 km) in Croatia, the Sava and the Drava, coursing through the Pannonian and para-Pannonian plains, are of particular importance—both because of their length and because, along with the Kupa River, they are in large part navigable. The Sava originates in Slovenia, passes Croatia’s capital city of Zagreb, and then forms most of the border between Croatia and Bosnia and Herzegovina along the inside of the Croatian crescent. The Drava enters Croatia from Slovenia and forms all but a small section of the border with Hungary before joining the Danube, which in turn forms most of the border between Croatia and the Vojvodina province of Serbia. The Kupa, which forms part of the frontier between Slovenia and Croatia, and the Una River, which meanders along part of the border between Croatia and Bosnia and Herzegovina, both flow into the Sava. In Dalmatia the Krka and Cetina rivers are of particular importance because of their hydroelectric potential and because they flow into the Adriatic Sea. In addition, a great deal of water circulates in underground rivers and pools in the karstic regions of the central mountain belt and the littoral. These waters account for many of the unique geologic formations and the picturesque landscape of central and western Croatia. Soils The Pannonian and para-Pannonian plains are enriched with alluvial soil deposited by the Sava and Drava rivers. These plains are the most fertile agricultural regions of Croatia and form the country’s breadbasket. The soil of the central mountainous belt is rather poor but offers some cultivable land in the fields and meadows and some grazing land in the plateaus. The Croatian littoral is mostly mountainous and barren, with rocky soil and poor agricultural land. Climate Two main climatic zones dominate Croatia. The Pannonian and para-Pannonian plains and the mountain regions are characterized by a continental climate of warm summers and cold winters. In the plains, temperatures average in the low 70s F (low 20s C) in June and in the low 30s F (around 0 °C) in January—although they can range from a low of −5 °F (−20 °C) in the winter to a high of 105 °F (40 °C) in the summer. The central mountain regions of Lika and Krbava have slightly cooler summers and cold winters, with a milder climate in the valleys. The average temperature range is between about 65 °F (about 18 °C) in June and the upper 20s F (about −2 °C) in January. Considerable rainfall, turning to snow in winter, is characteristic of the region. The Dalmatian coast, Istria, and the islands have a mild Mediterranean climate. In southern Dalmatia, where the sirocco winds (known there as the jugo) bring a moderating influence from Africa, summers are sunny, warm, and dry, and winters are rainy. In the north the winters are drier and colder as a result of the cold northeast wind known as the bora (bura). In the summer the mistral wind has a cooling effect on the coast and the islands. The average temperature ranges from the low 40s F (about 5 °C) in January to the low 70s F (low 20s C) in June. Rainfall is moderate and occurs mainly in the winter. Reflecting the country’s diverse geography, the flora and fauna of Croatia are highly varied. On the Dalmatian coast, grapes and olives are grown to produce wine and oil, while Istria is dominated by firs, and Slavonia has many oak forests. In terms of animal life, lizards are found on the coast, while wolves and even bears can be found in the inland forests. Hares, foxes, boars, wildcats, and mouflons (wild sheep) also inhabit Croatia. Sea life in the Adriatic is rich as well, with many coral reefs and underwater caves serving as habitats. People of Croatia - Ethnic groups and religions A variety of ethnic groups coexist within the republic. Croats constitute about nine-tenths of the population. Serbs make up the largest minority group; however, their proportion fell dramatically as a result of the 1990s war of independence—from more than one-tenth of the population before the war to less than half that figure in 2001. In addition to the Croats and the Serbs, there are small groups of Bosnian Muslims (Bosniaks), Hungarians, Italians, and Slovenes as well as a few thousand Albanians, Austrians, Bulgarians, Czechs, Germans, and other nationalities. It has been estimated that the number of Croats living outside the borders of Croatia is comparable to the number living inside the country. Many ethnic Croats reside in Bosnia and Herzegovina, where Croats have lived since the Slavs first migrated to the western Balkan Peninsula in the 6th and 7th centuries ce. Although there has traditionally been a yearning for unification with Croatia among the Croats of Herzegovina (a region contiguous to Dalmatia), this sentiment has not generally been shared by Croats within Croatia or even by Croats in Bosnia. Many of the Serbs in Croatia are descendants of people who migrated to the border areas of the Holy Roman Empire between the 16th and 18th centuries, following the Ottoman conquest of Serbia and Bosnia. There is traditionally a close correlation between ethnic identity and religious affiliation. The Croats are overwhelmingly Roman Catholic and more Western-influenced than the Serbs, who are overwhelmingly Eastern Orthodox. A small minority of people are nonreligious or atheist. Bosniaks constitute most of the Muslim population. Languages Croats speak Croatian, a South Slavic language of the Indo-European family. Croatian is quite similar to Serbian and Bosnian, but political developments since the collapse of Yugoslavia have encouraged the three ethnic groups to emphasize the differences between their languages. The clearest distinction between the Croatian and Serbian variants of what was previously called the Serbo-Croatian language is the script, with Croatian written in the Latin alphabet and Serbian in the Cyrillic. Distinctions of grammar and pronunciation also occur, as do more striking differences in vocabulary, which result partly from differential historical patterns of foreign domination. For Croats, this has resulted in a sprinkling of German, Hungarian, and (in Dalmatia and Istria) Italian vocabulary, while the Serbs’ speech shows Turkish and Russian influences. In addition, there have been various movements to “purify” the Croatian language, which have led to further differences. Another linguistic distinction, reflecting the legacies of history as well as the effects of geography, can be heard in the colourful medley of regional dialects and subdialects that survive to this day. The standard Croatian literary language, based on the Shtokavian dialect, emerged in the second half of the 19th century as a result of an effort to unite all South Slavs. Although all three major branches of Serbo-Croatian (Shtokavian, Chakavian, and Kajkavian) were spoken by Croats (as they still are today), the Shtokavian dialect was the most widely heard in Croatian regions of eastern Slavonia, the Adriatic littoral from Makarska to Dubrovnik, and Herzegovina, as well as Montenegro and Serbia. It was therefore adopted by leading Croatian national intellectuals of the 19th century. More … https://www.britannica.com/place/Croatia

2021/06/25

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