E-ambasada

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. Easily accessible mountain passes (now superseded by tunnels) through Slovenia’s present-day territory have long served as routes for those crossing the Mediterranean and transalpine regions of Europe. The Slovenes are a South Slavic people with a unique language. For most of its history, Slovenia was largely controlled by the Habsburgs of Austria, who ruled the Holy Roman Empire and its successor states, the Austrian Empire and Austria-Hungary; in addition, coastal portions were held for a time by Venice. As part of Yugoslavia, Slovenia came under communist rule for the bulk of the post-World War II period. With the dissolution of the Yugoslav federation in 1991, a multiparty democratic political system emerged. Slovenia’s economic prosperity in the late 20th century attracted hundreds of thousands of migrants from elsewhere in the Balkans. In the early 21st century, Slovenia integrated economically and politically with western Europe, joining the North Atlantic Treaty Organization as well as the European Union in 2004. Slovenia’s capital and most important city is Ljubljana. Land Slovenia is bordered by Austria to the north and Hungary to the far northeast. To the east, southeast, and south, Slovenia shares a 416-mile- (670-km-) long border with Croatia. To the southwest Slovenia is adjacent to the Italian port city of Trieste and occupies a portion of the Istrian Peninsula, where it has an important coastline along the Gulf of Venice. Italy’s Friuli-Venezia Giulia region is situated to the west. Slovenia is mostly elevated. Outside the coastal area, its terrain consists largely of karstic plateaus and ridges, magnificently precipitous Alpine peaks, and (between the elevated areas) valleys, basins, and arable or pastorally useful karstic poljes. The only major flat area is in the northeast. Tectonic fault lines cross the country, and Ljubljana suffered a devastating earthquake in 1895. Relief In Slovenia four main physiographic regions can be distinguished. The first is the Alpine region, which takes up about two-fifths of Slovenia’s surface area. In the north and northwest, along the borders with Italy and Austria, are the High Alps, comprising the Kamnik and Savinja, the Karavanke (Karawanken), and the Julian Alps; the latter includes Slovenia’s highest peak, Mount Triglav, at 9,396 feet (2,864 metres). In a vale beneath Triglav lie idyllic Lake Bohinj and Lake Bled. Slightly lower than the High Alps is the subalpine “ridge-and-valley” terrain. The main subalpine range is the Pohorje, located south of the Drava River. The historical name for the central Alpine lands is Gorenjska (Upper Carniola), a name that Slovenes still use. Slovenes refer to the Mea and Mislinja river valleys as Koro&scaron;ka (Carinthia). On Gorenjska’s southern edge is the spacious Ljubljana basin, which contains the capital as well as the industrial city of Kranj. Slovenia’s second major physiographic region, the Kras (Karst), a spur of the lengthy Dinaric Alps in the southwestern part of the country, is dotted with caves and underground rivers, the characteristic features of karst topography (whose term is derived from the name of the region). Although it constitutes one-fourth of Slovenia’s area, the Kras region has only a fraction of the country’s population, which is concentrated between the wooded limestone ridges in dry and blind valleys, hollows, and poljes. Water is scarce in this region. The Suha Krajina is a karstified plateau; the Bela Krajina is a transitional belt that contains plains and points toward the Subpannonia (Pannonian Plain). Most of the region is known to Slovenes by its historical names: Dolenjska (Lower Carniola) and Notranjska (Inner Carniola). Scientific study of karst terrain is a Slovene specialty, research having begun during the 18th century in Habsburg Carniola. The next largest physiographic region (occupying one-fifth of the country) is the fertile Subpannonia; it is located in eastern and northeastern Slovenia and includes the valleys of the Sava, Drava, and Mura rivers. Its basins contain the cities of Maribor (on the Drava) and Celje (on the Savinja River, a tributary of the Sava). Subpannonia corresponds in part to the lower part of the old Austrian duchy of Styria; Slovenes call their portion &Scaron;tajerska and share some traits with their Austrian neighbours. Beyond a saddle of hills known as the Slovenske Gorice is Prekmurje, a wheat-growing region drained by the Mura River in the extreme northeast of the country. It was ruled by Hungary until 1918; its main town is Murska Sobota. The fourth principal region (occupying barely one-twelfth of Slovenia’s surface) is Primorska, or the Slovene Littoral. It overlaps what were the Habsburg regions of Trieste and Gorizia and is made up of Slovenia’s portion of the Istrian Peninsula, the Adriatic hinterland, and the Soča and Vipava river valleys. The 29-mile (47-km) strip of coast makes up Slovenia’s riviera. The city of Koper (just south of Trieste) is Slovenia’s major port. Drainage Most of Slovenia’s intricate fluvial network is directed toward the Danube River. The Sava originates in the Julian Alps and flows past Ljubljana toward Croatia; its narrow valley serves as a rail conduit to Zagreb, Croatia’s capital, and farther to Belgrade, Serbia’s capital. The Drava enters Slovenia from the Austrian state of Kärnten, and the Mura emerges from the Austrian state of Steiermark; they meet in Croatia and, like the Sava, ultimately reach the Danube. In the west the Soča originates beneath Mount Triglav and, after a precipitous course, reaches the Gulf of Venice in Italian territory. The relatively steep gradients of Slovenia’s topography create fast runoff, which in turn ensures most of Slovenia copious water and hydroelectric resources. On the other hand, it also washes away valuable soil nutrients. Pollution of the rivers remains a problem. Soils Slovenia’s complex geology has created a pedological mosaic. The small, thick Pleistocene cover is acidic and viscid. Permeable thin brown podzols—cambisols and fluvisols—are productive if fertilized, but they cover only about one-tenth of its surface, chiefly to the northeast. The carbonate bedrock underlying much of the country produces thin lithosols suited to forest growth. There are many good alluvial soils (particularly in Subpannonia) as well as bog varieties. Karstic sinkholes and poljes are famous for having terra rossa, a red soil produced by the degradation of the underlying limestone. More … Score: https://www.britannica.com/place/Slovenia    

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2022/06/25

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

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2022/06/25

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

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2022/06/25

Newsletter January-June 2022 / Newsletter Styczeń-Czerwiec 2022

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2022/06/24

Cérémonie de remise du label LabelFrancEducation au lycée n°11 de Lodz

L’Attachée de coopération éducative, Fabienne Ricordel, a remis le label LabelFrancEducation au Lycée n°11 de Lodz lors d’une cérémonie organisée le 2 juin 2022 dans l’établissement. Les représentants des autorités éducatives locales et les acteurs francophones de la région étaient au rendez-vous et ont pu apprécier la présentation historique de l’établissement réalisée en français par les élèves et le spectacle de chansons francophones.

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2022/06/24

第21届“汉语桥”世界大学生中文比赛波兰赛区比赛举行

5月26日，第21届“汉语桥”世界大学生中文比赛波兰赛区决赛在波兰南部城市奥波莱落幕，来自波兹南密兹凯维奇大学的刘艾琳（Aleksandra Łukasiewicz）夺得冠军，她将代表波兰赛区参加下一阶段的全球决赛。本次比赛由中国驻波兰大使馆主办，奥波莱孔子学院承办，有来自弗罗茨瓦夫、波兹南、克拉科夫等地的14名选手参赛，比赛分为主题演讲、知识问答、才艺展示三个环节。比赛中，选手们分享了自己学习中文的故事，阐述了对“天下一家”和人类命运共同体理念的认知和理解，展示了有关中国国情、文化知识等方面的知识储备。在“才艺展示”环节，选手们各显神通，展示了中国舞、中文歌、脱口秀、乐器演奏以及剪纸和中国书法等。

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2022/06/24

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