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 Easily accessible mountain passes (now superseded by tunnels) through Slovenia’s present-day territory have long served as routes for those crossing the Mediterranean and transalpine regions of Europe.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 Koroška (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 Štajerska 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    

2024/06/25

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

2024/06/25

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

2024/06/25

Luxembourg let’s make it happen

Welcome to the official portal of the Grand Duchy of Luxembourg. Discover a multicultural and multilingual country located right at the heart of Europe.

2024/06/25

This is Slovenia - 2020

Beautiful Slovenian landscape footage made during COVID-19 lockdown. I am so glad I am stuck in my home country.

2024/06/24

Visit Mozambique WEB.mov

2024/06/24

Croatia Full Of Life - new promotional

Take a Tour of Champions in the Tiny Country Which Dared to Dream: http://bit.ly/2nSwsqv Visit the city where Marin Čilić found his love! Visit and discover Mario Mandžukić’s Slavonia and its tremendous food and wine Visit the National Parks approved by Ivan Rakitic

2024/06/24

Saint John the Baptist Day

Hospitallers, also spelled Hospitalers, also called Order of Malta or Knights of Malta, formally (since 1961) Sovereign Military and Hospitaller Order of St. John of Jerusalem, of Rhodes, and of Malta, previously (1113–1309) Hospitallers of St. John of Jerusalem, (1309–1522) Order of the Knights of Rhodes, (1530–1798) Sovereign and Military Order of the Knights of Malta, or (1834–1961) Knights Hospitaller of St. John of Jerusalem, a religious military order that was founded at Jerusalem in the 11th century and that, headquartered in Rome, continues its humanitarian tasks in most parts of the modern world under several slightly different names and jurisdictions. Heraldic flagsBanner: The blazon of the shield is applied to the whole surface of a square or a vertically or horizontally oriented rectangular flag. This is the Royal Banner of Scotland, which follows the blazon of the second quarter of the Royal Arms of the United Kingdom. Although it is the banner of the sovereign, it is widely but incorrectly used today as the national symbol.Fork-tailed pennon: Shown here is that of the Sovereign and Military Order of the Knights of Malta, in heraldic terms gules a cross argent.Standard: The Cross of St. George at the hoist identifies this as English. The profusion of badges, the diagonally placed motto, and the border of alternating tinctures are typical. This is the standard of Sir Henry Stafford, c. 1475. Drawing by Wm. A. Norman, Encyclopædia Britannica, Inc. The origin of the Hospitallers was an 11th-century hospital founded in Jerusalem by Italian merchants from Amalfi to care for sick and poor pilgrims. After the Christian conquest of Jerusalem in 1099 during the First Crusade, the hospital’s superior, a monk named Gerard, intensified his work in Jerusalem and founded hostels in Provençal and Italian cities on the route to the Holy Land. The order was formally named and recognized on February 15, 1113, in a papal bull issued by Pope Paschal II. Raymond de Puy, who succeeded Gerard in 1120, substituted the Augustinian rule for the Benedictine and began building the power of the organization. It acquired wealth and lands and combined the task of tending the sick with defending the Crusader kingdom. Along with the Templars, the Hospitallers became the most formidable military order in the Holy Land. When the Muslims recaptured Jerusalem in 1187, the Hospitallers removed their headquarters first to Margat and then, in 1197, to Acre. When the Crusader principalities came to an end after the fall of Acre in 1291, the Hospitallers moved to Limassol in Cyprus. In 1309 they acquired Rhodes, which they came to rule as an independent state, with right of coinage and other attributes of sovereignty. Under the order’s rule, the master (grand master from c. 1430) was elected for life (subject to papal confirmation) and ruled a celibate brotherhood of knights, chaplains, and serving brothers. For more than two centuries these Knights of Rhodes were the scourge of Muslim shipping on the eastern Mediterranean. They constituted the last Christian outpost in the East. By the 15th century the Turks had succeeded the Arabs as the protagonists of militant Islam, and in 1522 Süleyman the Magnificent laid final siege to Rhodes. After six months the Knights capitulated and on January 1, 1523, sailed away with as many of the citizens as chose to follow them. For seven years the wandering Knights were without a base, but in 1530 the Holy Roman emperor Charles V gave them the Maltese archipelago in return, among other things, for the annual presentation of a falcon to his viceroy of Sicily. The superb leadership of the grand master Jean Parisot de la Valette prevented Süleyman the Magnificent from dislodging the Knights from Malta in 1565 in one of the most famous sieges in history, which ended in a Turkish disaster. What was left of the Turkish navy was permanently crippled in 1571 at the Battle of Lepanto by the combined fleets of several European powers that included the Knights of Malta. The Knights then proceeded to build a new Maltese capital, Valletta, named after la Valette. In it they built great defense works and a hospital of grand dimensions that attracted many physically and mentally ill patients from outside Malta. Thereafter the Knights continued as a territorial sovereign state in Malta but gradually gave up warfare and turned wholly to territorial administration and to medical care. In 1798, however, their reign in Malta came to an end, when Napoleon, on his way to Egypt, occupied the island. The order’s return to Malta was provided for in the Treaty of Amiens (1802) but eliminated by the Treaty of Paris (1814), which assigned Malta to Great Britain. In 1834 the Knights of Malta became permanently established in Rome. From 1805 they were ruled by lieutenants until Pope Leo XIII revived the office of grand master in 1879. A new constitution containing a more precise definition of both the religious and the sovereign status of the order was adopted in 1961, and a code was issued in 1966. Although the order no longer exercises territorial rule, it issues passports, and its sovereign status is recognized by the Holy See and some other Roman Catholic states. Membership is confined to Roman Catholics, and the central organization is essentially aristocratic, being ruled chiefly by a primary class of “professed” knights of justice and chaplains who can prove the nobility of their four grandparents for two centuries. More …. Score: https://www.britannica.com/event/Siege-of-Rhodes

2024/06/24

National Day. Birthday of the Grand Duchess of Luxembourg Charlotte von Nassau-Weilburg

Luxembourg, country in northwestern Europe. One of the world’s smallest countries, it is bordered by Belgium on the west and north, France on the south, and Germany on the northeast and east. Luxembourg has come under the control of many states and ruling houses in its long history, but it has been a separate, if not always autonomous, political unit since the 10th century. The ancient Saxon name of its capital city, Lucilinburhuc (“Little Fortress”), symbolized its strategic position as “the Gibraltar of the north,” astride a major military route linking Germanic and Frankish territories. Luxembourg is a point of contact between the Germanic- and Romance-language communities of Europe, and three languages are regularly employed in the grand duchy itself: Luxembourgish, German, and French. The peoples of Luxembourg and their languages reflect the grand duchy’s common interests and close historical relations with its neighbours. In the 20th century Luxembourg became a founding member of several international economic organizations. Perhaps most importantly, the grand duchy was an original member of the Benelux Economic Union (1944), which linked its economic life with that of the Netherlands and of Belgium and would subsequently form the core of the European Economic Community (EEC; ultimately succeeded by the European Union). Land - Relief and soils The northern third of Luxembourg, known as the Oesling (Ösling), comprises a corner of the Ardennes Mountains, which lie mainly in southern Belgium. It is a plateau that averages 1,500 feet (450 metres) in elevation and is composed of schists and sandstones. This forested highland region is incised by the deep valleys of a river network organized around the Sûre (or Sauer) River, which runs eastward through north-central Luxembourg before joining the Moselle (or Mosel) River on the border with Germany. The Oesling’s forested hills and valleys support the ruins of numerous castles, which are a major attraction for the region’s many tourists. The fertility of the relatively thin mountain soils of the region was greatly improved with the introduction in the 1890s of a basic-slag fertilizer, which is obtained as a by-product of the grand duchy’s steel industry. The southern two-thirds of Luxembourg is known as the Bon Pays, or Gutland (French and German: “Good Land”). This region has a more-varied topography and an average elevation of 800 feet (about 245 metres). The Bon Pays is much more densely populated than the Oesling and contains the capital city, Luxembourg, as well as smaller industrial cities such as Esch-sur-Alzette. In the centre of the Bon Pays, the valley of the northward-flowing Alzette River forms an axis around which the country’s economic life is organized. Luxembourg city lies along the Alzette, which joins the Sûre farther north. In the east-central part of the Bon Pays lies a great beech forest, the Müllerthal, as well as a sandstone area featuring an attractive ruiniform topography. The country’s eastern border with Germany is formed (successively from north to south) by the Our, Sûre, and Moselle rivers. The slopes of the Moselle River valley, carved in chalk and calcareous clay, are covered with vineyards and receive a substantial amount of sunshine, which has earned the area the name “Little Riviera.” Besides vineyards, the fertile soils of the Moselle and lower Sûre valleys also support rich pasturelands. Luxembourg’s former iron mines are located in the extreme southwest, along the duchy’s border with France. Climate Luxembourg has a mild climate with considerable precipitation. The north is slightly colder and more humid than the south. The mean temperatures in Luxembourg city range from the mid-30s F (about 0.7 °C) in January to the low 60s F (about 17 °C) in July, but in the Oesling both extremes are slightly lower. The Oesling receives more precipitation than the Bon Pays, but the greatest amount, about 40 inches (1,000 mm), and the least, about 27 inches (about 685 mm), fall in the southwest and southeast, respectively. The sheltered valley of the Moselle River benefits from a gentler and sunnier climate than does the rest of the duchy. People - Ethnic groups, languages, and religion Luxembourg has been one of the historic crossroads of Europe, and myriad peoples have left their bloodlines as well as their cultural imprints on the grand duchy. The Celts, the Belgic peoples known as the Treveri, the Ligurians and Romans from Italy, and especially the Franks were most influential. The language spoken by Luxembourg’s native inhabitants is Luxembourgish, or Lëtzebuergesch, a Moselle-Franconian dialect of German that has been enriched by many French words and phrases. Luxembourgish is the national language; German and French are both languages of administration. There is a strong sense of national identity among Luxembourgers despite the prevalence of foreign influences. The great majority of Luxembourg’s native citizens are Roman Catholic, with a small number of Protestants (mainly Lutherans), Jews, and Muslims. Lxembourg has a high proportion of foreigners living within its borders. This is chiefly the result of an extremely low birth rate among native Luxembourgers, which has led to a chronic labour shortage. Nearly half of the total population is of foreign birth and consists mainly of Portuguese, French, Italians, Belgians, and Germans. Among the foreign workers are many in the iron and steel industry, and numerous others work in foreign firms and international organizations located in the capital. Settlement patterns Northern Luxembourg is sparsely populated compared with the heavily urbanized and industrialized south. The north’s rural population is clustered in villages of thick-set stone houses with slate roofs. The urban network in the south is dominated by the capital city, Luxembourg, which rises in tiers, with the upper (and older) section of the city separated from the lower-lying suburbs by the gorges of the Alzette and Petrusse rivers. A newer quarter housing many European organizations nestles in a picturesque site carved into the river valley’s sandstone cliffs. The second largest city in Luxembourg, Esch-sur-Alzette, lies in the extreme southwest and is a traditional iron- and steel-making centre. Its growth, like that of the neighbouring iron and steel centres of Pétange, Differdange, and Dudelange, has slowed since the shrinkage of those industries in western Europe in the late 20th century. The remainder of the country’s population lives in towns and villages of relatively small size. Many of Luxembourg’s villages date from ancient Celtic and Roman times or originated in Germanic and Frankish villages after about 400 ce. In addition, many medieval castle villages continue to thrive, centuries after the castles themselves fell into ruin. More : Score: https://www.britannica.com/place/Luxembourg

2024/06/23