Wyoming - jeden z najbarwniejszych stanów USA

To na jego terenie znajduje się największa część Parku Narodowego Yellowstone, znanego za sprawą kolorowych, gorących źródeł i zachwycających gejzerów. ?? Najsłynniejszy z nich to Old Faithful, którego wysokie erupcje są bardzo regularne, bo mają miejsce mniej więcej co 90 minut. Wyoming to też górzysty park Grand Teton z charakterystyczną, zabytkową wioską mormońską tuż obok. W stanie można znaleźć wiele typowo westernowych miasteczek (na przykład skansen w Cody lub tętniące życiem Jackson i Pinedale), a nawet słynne areny rodeo!

2022/07/26

Predstavljanje prioriteta predsjedanja Češke Republike Vijećem EU

Veleposlanik Republike Češke u Poljskoj Jakub Dürr je u Veleposlanstvu Republike Češke u Varšavi u petak 1. srpnja predstavio prioritete predsjedanja Češke Republike Vijećem EU za narednih 6 mjeseci, u drugoj polovini ove godine. Na predstavljanju je sudjelovalo niz dužnosnika ministarstva vanjskih poslova Republike Poljske na čelu sa ministrom za Europsku uniju Konradom Szymańskim, te predstavnici diplomatsko-konzularnog zbora među kojima i veleposlanik Tomislav Vidošević.

2022/07/26

Independence day of the Republic of Liberia

Liberia, country along the coast of western Africa. Liberia’s terrain ranges from the low and sandy coastal plains to rolling hills and dissected plateau further inland. The country is home to a lush rainforest containing a rich diversity of flora and fauna. Liberia is the only Black state in Africa never subjected to colonial rule and is Africa’s oldest republic. It was established on land acquired for freed U.S. slaves by the American Colonization Society, which founded a colony at Cape Mesurado in 1821. In 1824 the territory was named Liberia, and its main settlement was named Monrovia, which is the present-day capital. Liberian independence was proclaimed in 1847, and its boundaries were expanded. The country enjoyed relative stability until a rebellion in 1989 escalated into a destructive civil war in the 1990s that did not fully cease until 2003. The country’s first post-conflict elections, held in 2005, were noteworthy for the election of Ellen Johnson Sirleaf to the presidency, as she was the first woman to be elected head of state in Africa. Land Liberia is bounded by Sierra Leone to the northwest, Guinea to the north, Côte d’Ivoire to the east, and the Atlantic Ocean to the south and west. Relief The four physiographic regions of Liberia parallel the coast. The coastal plains are about 350 miles (560 km) long and extend up to 25 miles (40 km) inland. They are low and sandy, with miles of beaches interspersed with bar-enclosed lagoons, mangrove swamps, and a few rocky promontories—the highest being Cape Mount (about 1,000 feet [305 metres] in elevation) in the northwest, Cape Mesurado in Monrovia, and Cape Palmas in the southeast. Parallel to the coastal plains is a region of rolling hills some 20 miles (32 km) wide with an average maximum elevation of about 300 feet (90 metres); a few hills rise as high as 500 feet (150 metres). It is a region suitable for agriculture and forestry. Behind the rolling hills, most of the country’s interior is a dissected plateau with scattered low mountains ranging from 600 to 1,000 feet (180 to 305 metres) in elevation; some mountains rise to 2,000 feet (600 metres). A striking feature of the mountainous northern highlands along the Guinea frontier is Mount Nimba. Drainage The Mano and Morro rivers in the northwest and the Cavalla in the east and southeast are major rivers and form sections of Liberia’s boundaries. Other major rivers are the Lofa in the north and, moving southward, the St. Paul, St. John, and Cestos, all of which parallel each other and flow perpendicular to the coast. The Farmington River is a source of hydroelectric power. Waterfalls, rapids, rocks, and sandbanks occur frequently in upstream sections of most rivers, inhibiting river traffic, and limiting navigation inland to short distances. During the rainy season there is often severe flooding in the coastal plains. Liberia forms part of the West African Shield, a rock formation 2.7 to 3.4 billion years old, composed of granite, schist, and gneiss. In Liberia the shield has been intensely folded and faulted and is interspersed with iron-bearing formations known as itabirites. Along the coast lie beds of sandstone, with occasional crystalline-rock outcrops. Monrovia stands on such an outcropping, a ridge of diabase (a dark-coloured, fine-grained rock). Soils Four types of soil are found in Liberia. Latosols of low to medium fertility occur in rolling hill country and cover about three-fourths of the total land surface. Shallow, coarse lithosols, in the hilly and rugged terrain, cover about one-eighth of the land. Infertile regosols, or sandy soils, are found along the coastal plains. Highly fertile alluvial soils represent a small percentage of the land area and are utilized largely for agriculture. Climate The climate, especially on the coast, is warm and humid year-round, dominated by a dry season from November to April and by a rainy season from May to October. The dusty and dry harmattan (desert winds) blow from the Sahara to the coast in December, bringing relief from the high relative humidity. Deforestation and drought in the Sahel have affected the climate, lengthening the dry season by almost a month in some areas. Mean annual temperatures range between 65° F (18° C) in the northern highlands to 80° F (27° C) along the coast. Rainfall is irregular, and the rainy season varies in intensity and begins earlier at the coast than in the interior. The greatest amount of rainfall, 205 inches (5,200 mm), occurs at Cape Mount and diminishes inland to about 70 inches (1,800 mm) on the central plateau. The interior has hot but pleasant days and cool nights during the dry season. Plant and animal life Liberia has year-round evergreen vegetation. Many trees—such as red ironwood, camwood, whismore, teak, and mahogany—are valuable, but occur with other species, preventing easy harvest. Other trees of value are rubber, cacao, coffee, and the raffia palm. Liberia’s rainforest used to abound with animals such as monkeys, chimpanzees, small antelopes, pygmy hippopotamuses, and anteaters. However, these animals, along with the already threatened elephants, bush cows (short-horned buffalo), and leopards, were hunted for food during the civil war; their populations are recovering. There are many reptiles, including three types of crocodiles and at least eight poisonous snakes. There are several unique species of bats and birds, and scorpions, lizards, and fish are numerous. Sapo National Park, established in 1983 in the country’s southeast, was expanded in 2003 to encompass an area of some 700 square miles (1,800 square km). The 2000s saw an expansion of protected regions in Liberia, with new and enlarged wildlife reserves at Gola National Forest, the Wonegizi National Forest Reserve, and Lake Piso, and ecotourism was seen as a potential growth industry for the country. People of Liberia - Ethnic groups and languages The people of Liberia are classified into three major groups: the indigenous people, who are in the majority and who migrated from the western Sudan in the late Middle Ages; Black immigrants from the United States (known historically as Americo-Liberians) and the West Indies; and other Black immigrants from neighbouring western African states who came during the anti-slave-trade campaign and European colonial rule. The Americo-Liberians are most closely associated with founding Liberia. Most of them migrated to Liberia between 1820 and 1865; continued migration has been intermittent. Americo-Liberians controlled the government until a military coup in 1980. Liberia’s indigenous ethnic groups may be classified into three linguistic groups, all belonging to the Niger-Congo language family: the Mande, Kwa, and Mel (southern Atlantic). The Mande are located in the northwest and central regions of Liberia and also in Senegal, Mali, Guinea, and Sierra Leone. Prominent among them are the Vai, who invented their own alphabet and who, in addition, use Arabic and English; the Kpelle, the largest Mande group, who are also found in Guinea; Loma (also found in Guinea); Ngbandi; Dan (Gio); Mano; Mende; and Malinke. Kwa-speaking peoples include the Bassa, the largest group in this category and the largest ethnic group in Monrovia; the Kru and Grebo, who were among the earliest converts to Christianity; the De; Belleh (Belle); and Krahn. The Kwa-speaking group occupies the southern half of the country. The Mel group includes the Gola and Kisi, who are also found in Sierra Leone and are known to be the oldest inhabitants of Liberia. These people live in the north and in the coastal region of the northwest. More than two dozen languages are spoken in Liberia. English is the official language. Predominant languages include Kpelle, Bassa, Grebo, Dan, Kru, Mano, Loma, and Mandingo (spoken by the Malinke). Religion About four-fifths of Liberians are Christian, about one-tenth are Muslim, and a small number profess other religions—primarily traditional beliefs—or are nonreligious. The largest number of Christians are Kpelle, followed by the Bassa. Some Liberians who identify themselves primarily as Christian incorporate traditional beliefs into their personal theologies. The Muslims are found predominantly among the Mande peoples in the northwest region of the country. Settlement patterns The present pattern of population distribution in Liberia is both a reflection of its migration history and a response to such social, economic, and cultural factors as war, employment, and superstition. Migrants from north-central Africa, who began to arrive in the 13th century, originally settled in the hinterlands but were driven by overcrowding to the coast. Immigrants from the United States and the West Indies, and from neighbouring African countries, also settled on the coast. The former migrated mostly to selected areas such as Monrovia (the oldest immigrant settlement), Buchanan, Edina, Greenville, Harper, Robertsport, and Marshall. Scattered settlements were created along newly constructed or improved roads, while plantation and mining activities encouraged larger settlements in a few interior and coastal areas. There are more than 2,000 villages, the majority of which are concentrated in central Liberia, in the northwest, and in the coastal region near Monrovia. The predominantly forested regions of south-central and northern Liberia have remained sparsely populated. There is a strong rural-to-urban movement, especially to Monrovia. Other destinations include enclaves around rubber plantations and mines. The trend toward urbanization has had little impact on the villages. The result has been the segmentation of Liberian society into two coexisting subsystems—traditional-rural and modern-urban. Monrovia, founded in 1822, is the focal point of political, economic, and cultural activities. Situated on the left bank of the St. Paul River on the ridge formed by Cape Mesurado, it commands an imposing view of the Atlantic Ocean and the coastal plains. The city and its outlying districts and suburbs occupy five square miles. The old style of architecture that once characterized it, reminiscent of that of the southern United States before 1860, is giving way to contemporary styles. All of the ethnic groups of Liberia are represented in its population, as are refugees, African nationals from other countries, and Europeans. Demographic trends More than two-fifths of the population of Liberia is under age 15; only about 5 percent is older than 60. The country’s birth and death rates are similar to or greater than those of other sub-Saharan African countries and are among the highest in the world. Life expectancy, about 57 years for males and 60 years for females, is similar to that of neighbouring countries and is among the lowest in the world. It fell as a result of the civil war and strife that began in the late 1980s and continued until 2003. Economy of Liberia The Liberian economy is predominantly agrarian, and raw materials, equipment, and consumer goods are imported. Production for export is carried out on a large scale through foreign investment in rubber, forestry, and mining. Foreign ships registering under a Liberian “flag of convenience” have made Liberia one of the world’s foremost countries in registered shipping tonnage. Liberia nevertheless remains primarily agricultural. The distribution of wealth is uneven, the coastal districts receiving a greater share of economic benefits than the hinterland, after which the administrative centres are the next beneficiaries. After the mid-1970s the once-vibrant economy took a sharp downturn. Between 1976 and 1980 sluggish demand and low prices stagnated the economy and the annual growth rate plunged. But gradual signs of recovery appeared, especially in agriculture and forestry. In the early 1990s, however, civil war disrupted Liberia’s economy. Since the end of the conflict in 2003, and particularly after a democratically elected government was inaugurated in early 2006, efforts to rebuild the country’s economic infrastructure have been under way. More … Source: https://www.britannica.com/place/Liberia

2022/07/26

Independence day of the Republic of Maldives

Maldives, in full Republic of Maldives, also called Maldive Islands, independent island country in the north-central Indian Ocean. It consists of a chain of about 1,200 small coral islands and sandbanks (some 200 of which are inhabited), grouped in clusters, or atolls. The islands extend more than 510 miles (820 km) from north to south and 80 miles (130 km) from east to west. The northernmost atoll is about 370 miles (600 km) south-southwest of the Indian mainland, and the central area, including the capital island of Male (Male’), is about 400 miles (645 km) southwest of Sri Lanka. Land The Maldive Islands are a series of coral atolls built up from the crowns of a submerged ancient volcanic mountain range. All the islands are low-lying, none rising to more than 6 feet (1.8 metres) above sea level. Barrier reefs protect the islands from the destructive effects of monsoons. The rainy season, from May to August, is brought by the southwest monsoon; from December to March the northeast monsoon brings dry and mild winds. The average annual temperature varies from 76 to 86 °F (24 to 30 °C). Rainfall averages about 84 inches (2,130 mm) per year. The atolls have sandy beaches, lagoons, and a luxuriant growth of coconut palms, together with breadfruit trees and tropical bushes. Fish abound in the reefs, lagoons, and seas adjoining the islands; sea turtles are caught for food and for their oil, a traditional medicine. People The population of Maldives belongs almost entirely to the Maldivian ethnic group, which is the result of various peoples settling in the islands successively through the country’s history. The first settlers, it is generally believed, were Tamil and Sinhalese peoples from southern India and Sri Lanka. Traders from Arab countries, Malaya, Madagascar, Indonesia, and China visited the islands through the centuries. The official language is an Indo-European language called Dhivehi (or Maldivian); Arabic, Hindi, and English are also spoken. Islam is the state religion. More than half of the population is considered rural. With the exception of those living in Male, the only relatively large settlement in the country, the inhabitants of the Maldives live in villages on small islands in scattered atolls. Only about 20 of the islands have more than 1,000 inhabitants, and the southern islands are more densely populated than the northern ones. The birth rate for the Maldives is somewhat higher than the world average, but the death rate is lower. More than one-fifth of the total population is under 15 years of age. Life expectancy is about 74 years for men and 79 for women. Economy Since the 1970s the economy of the Maldives has developed rapidly. Annual growth of gross domestic product (GDP) has been high, averaging about 6 percent in the 2010s, and the gross national income (GNI) per capita—among the lowest in the world in the 1970s—reached the level of upper middle-income countries by the late 2010s. The economy is based on tourism, fishing, boatbuilding, and boat repairing, with the tourism sector driving the rapid growth. Agriculture, forestry, and fishing Fishing, long the traditional base of the economy, has been far surpassed by tourism as the main source of gross domestic product (GDP). While the sector still produces the bulk of the country’s exports and continues to grow (albeit at a slower pace than the tourism industry), it employs less than one-fifth of the labour force and contributes less than one-tenth of the GDP. Tuna is the predominant fish caught, traditionally by the pole-and-line method, although a good deal of the fishing fleet has been mechanized. Most of the fish catch is sold to foreign companies for processing and export. Although formal businesses have seen rapid growth in the country, especially on the main islands, much of the population subsists outside the money economy on fishing, coconut collecting, and the growing of vegetables and melons, roots and tubers (cassava, sweet potatoes, and yams), and tropical fruits. Cropland, scattered over many small islands, is minimal, and nearly all the staple foods must be imported. Manufacturing Industries are largely of the handicraft or cottage type, including the making of coir (coconut-husk fibre) and coir products, fish canning, and boatbuilding. Textile and garment manufacturing was among the more lucrative industries from the mid-1990s until the 2005 expiry of an import quota regime in international textile trade left factories in the Maldives unable to compete. Construction makes up the bulk of the industrial sector. Trade Maldives entered the South Asian Free Trade Area (SAFTA) in 2006 and signed a free trade agreement with China in 2017. Imports include consumer goods such as food (principally rice), textiles, medicines, and petroleum products. Fish—mostly dried, frozen, or canned skipjack tuna—accounts for the bulk of exports. China, India, the United Arab Emirates, Thailand, Sri Lanka, and Singapore are among the main trading partners. Services The tourism industry, although nonexistent before 1972, underpins the services sector. Annually, more than 1.5 million tourists visit the Maldives. Its more than 130 resort islands include high-end hotel brands, and its marine geography offers unique diving and water sports opportunities as well as undersea accommodations, restaurants, and spas. By the mid-2010s the service sector accounted for four-fifths of the country’s GDP. Labour and taxation The rapid growth of the tourism industry left its mark on the labour market, which saw a dramatic shift away from agriculture and toward services. In part because of lack of training among the general population, a number of foreign workers from South Asia provide skills needed to help develop businesses. As businesses on resort islands away from the general populace demanded an increasing share of the total labour force, the participation rate of women, who are discouraged by the culture from living away from their families, fell substantially. About three-fifths of women participated in the labour force in the 1970s, but the rate dipped as low as one-fifth of women in the mid-1990s. By the 2010s, however, the participation rate had recovered to about half of women. Beginning in 2011, the Maldives collected taxes primarily on the profits of businesses and financial institutions and on goods and services within the tourism sector. An income tax was implemented in 2020. Transportation Transportation between islands and atolls is vital for the country. China and India, competing for influence over the strategically located Maldive Islands, have provided significant foreign direct investment to develop infrastructure that would further connect the islands. Boats provide the principal means of transport between the atolls, and scheduled shipping services link the country with Sri Lanka, Singapore, and India. The national airline carries passengers between several airports in the country as well as internationally. The airport at Male handles most international traffic, although there are other airports that serve limited international travel. More … Score: https://www.britannica.com/place/Maldives    

2022/07/26

Anniversary of the Revolution Arab Republic of Egypt

Egypt, country located in the northeastern corner of Africa. Egypt’s heartland, the Nile River valley and delta, was the home of one of the principal civilizations of the ancient Middle East and, like Mesopotamia farther east, was the site of one of the world’s earliest urban and literate societies. Pharaonic Egypt thrived for some 3,000 years through a series of native dynasties that were interspersed with brief periods of foreign rule. After Alexander the Great conquered the region in 323 bce, urban Egypt became an integral part of the Hellenistic world. Under the Greek Ptolemaic dynasty, an advanced literate society thrived in the city of Alexandria, but what is now Egypt was conquered by the Romans in 30 bce. It remained part of the Roman Republic and Empire and then part of Rome’s successor state, the Byzantine Empire, until its conquest by Arab Muslim armies in 639–642 ce. Until the Muslim conquest, great continuity had typified Egyptian rural life. Despite the incongruent ethnicity of successive ruling groups and the cosmopolitan nature of Egypt’s larger urban centres, the language and culture of the rural, agrarian masses—whose lives were largely measured by the annual rise and fall of the Nile River, with its annual inundation—had changed only marginally throughout the centuries. Following the conquests, both urban and rural culture began to adopt elements of Arab culture, and an Arabic vernacular eventually replaced the Egyptian language as the common means of spoken discourse. Moreover, since that time, Egypt’s history has been part of the broader Islamic world, and though Egyptians continued to be ruled by foreign elite—whether Arab, Kurdish, Circassian, or Turkish—the country’s cultural milieu remained predominantly Arab. Egypt eventually became one of the intellectual and cultural centres of the Arab and Islamic world, a status that was fortified in the mid-13th century when Mongol armies sacked Baghdad and ended the Abbasid caliphate. The Mamluk sultans of Egypt, under whom the country thrived for several centuries, established a pseudo-caliphate of dubious legitimacy. But in 1517 the Ottoman Empire defeated the Mamluks and established control over Egypt that lasted until 1798, when Napoleon I led a French army in a short occupation of the country. The French occupation, which ended in 1801, marked the first time a European power had conquered and occupied Egypt, and it set the stage for further European involvement. Egypt’s strategic location has always made it a hub for trade routes between Africa, Europe, and Asia, but this natural advantage was enhanced in 1869 by the opening of the Suez Canal, connecting the Mediterranean Sea to the Red Sea. The concern of the European powers (namely France and the United Kingdom, which were major shareholders in the canal) to safeguard the canal for strategic and commercial reasons became one of the most important factors influencing the subsequent history of Egypt. The United Kingdom occupied Egypt in 1882 and continued to exert a strong influence on the country until after World War II (1939–45). In 1952 a military coup installed a revolutionary regime that promoted a combination of socialism and Pan-Arab nationalism. The new regime’s extreme political rhetoric and its nationalization of the Suez Canal Company prompted the Suez Crisis of 1956, which was only resolved by the intervention of the United States and the Soviet Union, whose presence in the Mediterranean region thereafter kept Egypt in the international spotlight. During the Cold War, Egypt’s central role in the Arabic-speaking world increased its geopolitical importance as Arab nationalism and inter-Arab relations became powerful and emotional political forces in the Middle East and North Africa. Egypt led the Arab states in a series of wars against Israel but was the first of those states to make peace with the Jewish state, which it did in 1979. Egypt’s authoritarian political system was long dominated by the president, the ruling party, and the security services. With opposition political activity tightly restricted, decades of popular frustration erupted into mass demonstrations in 2011. The uprising forced Pres. Hosni Mubarak to step down, leaving a council of military officers in control of the country. Power was transferred to an elected government in 2012, and a new constitution was adopted at the end of the year. This elected government, however, was toppled a year later when the military intervened to remove the newly elected president, Mohamed Morsi, a member of the Islamist Muslim Brotherhood, following a series of massive public demonstrations against his administration. (For a discussion of unrest and political change in Egypt in 2011, see Egypt Uprising of 2011.) The ancient Greek historian Herodotus called Egypt the “gift of the Nile.” Indeed, the country’s rich agricultural productivity—it is one of the region’s major food producers—has long supported a large rural population devoted to working the land. Present-day Egypt, however, is largely urban. The capital city, Cairo, is one of the world’s largest urban agglomerations, and manufacturing and trade have increasingly outstripped agriculture as the largest sectors of the national economy. Tourism has traditionally provided an enormous portion of foreign exchange, but that industry has been subject to fluctuations during times of political and civil unrest in the region. Land of Egypt Egypt’s land frontiers border Libya to the west, Sudan to the south, and Israel to the northeast. Egypt’s border with Sudan is notable for two areas, the Ḥalāʾib Triangle along the Red Sea and Biʾr Ṭawīl further inland, that are subject to differing claims by the two countries (see Researcher’s Note). In the north its Mediterranean coastline is about 620 miles (1,000 km), and in the east its coastline on the Red Sea and the Gulf of Aqaba is about 1,200 miles (1,900 km). Relief The topography of Egypt is dominated by the Nile. For about 750 miles (1,200 km) of its northward course through the country, the river cuts its way through bare desert, its narrow valley a sharply delineated strip of green, abundantly fecund in contrast to the desolation that surrounds it. From Lake Nasser, the river’s entrance into southern Egypt, to Cairo in the north, the Nile is hemmed into its trenchlike valley by bordering cliffs, but at Cairo these disappear, and the river begins to fan out into its delta. The Nile and the delta form the first of four physiographic regions, the others being the Western Desert (Arabic Al-Ṣaḥrāʾ al-Gharbiyyah), the Eastern Desert (Al-Ṣaḥrāʾ al-Sharqiyyah), and the Sinai Peninsula. The Nile divides the desert plateau through which it flows into two unequal sections—the Western Desert, between the river and the Libyan frontier, and the Eastern Desert, extending to the Suez Canal, the Gulf of Suez, and the Red Sea. Each of the two has a distinctive character, as does the third and smallest of the Egyptian deserts, the Sinai. The Western Desert (a branch of the Libyan Desert) is arid and without wadis (dry beds of seasonal rivers), while the Eastern Desert is extensively dissected by wadis and fringed by rugged mountains in the east. The desert of central Sinai is open country, broken by isolated hills and scored by wadis. Egypt is not, as is often believed, an entirely flat country. In addition to the mountains along the Red Sea, mountainous areas occur in the extreme southwest of the Western Desert and in the southern Sinai Peninsula. The high ground in the southwest is associated with the ʿUwaynāt mountain mass, which lies just outside Egyptian territory. The coastal regions of Egypt, with the exception of the delta, are everywhere hemmed in either by desert or by mountain; they are arid or of very limited fertility. The coastal plain in both the north and east tends to be narrow; it seldom exceeds a width of 30 miles (48 km). With the exception of the cities of Alexandria, Port Said, and Suez and a few small ports and resorts such as Marsā Maṭrūh and Al-ʿAlamayn (El-Alamein), the coastal regions are sparsely populated and underdeveloped. More … Score: https://www.britannica.com/place/Egypt

2022/07/23

National holiday of the Kingdom of Belgium

Belgium, country of northwestern Europe. It is one of the smallest and most densely populated European countries, and it has been, since its independence in 1830, a representative democracy headed by a hereditary constitutional monarch. Initially, Belgium had a unitary form of government. In the 1980s and ’90s, however, steps were taken to turn Belgium into a federal state with powers shared among the regions of Flanders, Wallonia, and the Brussels-Capital Region. Culturally, Belgium is a heterogeneous country straddling the border between the Romance and Germanic language families of western Europe. With the exception of a small German-speaking population in the eastern part of the country, Belgium is divided between a French-speaking people, collectively called Walloons (approximately one-third of the total population), who are concentrated in the five southern provinces (Hainaut, Namur, Liège, Walloon Brabant, and Luxembourg), and Flemings, a Flemish- (Dutch-) speaking people (more than one-half of the total population), who are concentrated in the five northern and northeastern provinces (West Flanders, East Flanders [West-Vlaanderen, Oost-Vlaanderen], Flemish Brabant, Antwerp, and Limburg). Just north of the boundary between Walloon Brabant (Brabant Walloon) and Flemish (Vlaams) Brabant lies the officially bilingual but majority French-speaking Brussels-Capital Region, with approximately one-tenth of the total population. (See also Fleming and Walloon.)Belgium and the political entities that preceded it have been rich with historical and cultural associations, from the Gothic grandeur of its medieval university and commercial cities and its small, castle-dominated towns on steep-bluffed winding rivers, through its broad traditions in painting and music that marked one of the high points of the northern Renaissance in the 16th century, to its contributions to the arts of the 20th century and its maintenance of the folk cultures of past eras. The Belgian landscape has been a major European battleground for centuries, notably in modern times during the Battle of Waterloo (1815) and the 20th century’s two world wars. Given its area and population, Belgium today is one of the most heavily industrialized and urbanized countries in Europe. It is a member of the Benelux Economic Union (with the Netherlands and Luxembourg), the European Union (EU), and the North Atlantic Treaty Organization (NATO)—organizations that all have headquarters in or near the capital city of Brussels. Land The country has a total of 860 miles (1,385 km) of land boundaries with neighbours; it is bounded by the Netherlands to the north, Germany to the east, Luxembourg to the southeast, and France to the south. Belgium also has some 40 miles (60 km) of shoreline on the North Sea. Relief, drainage, and soils Belgium generally is a low-lying country, with a broad coastal plain extending in a southeasterly direction from the North Sea and the Netherlands and rising gradually into the Ardennes hills and forests of the southeast, where a maximum elevation of 2,277 feet (694 metres) is reached at Botrange. The main physical regions are the Ardennes and the Ardennes foothills; Côtes Lorraines (Belgian Lorraine), the intrusion of the Paris Basin in the south; and the Anglo-Belgian Basin in the north, comprising the Central Plateaus, the plain of Flanders, and the Kempenland (French: Campine). The Ardennes region is part of the Hercynian orogenic belt of mountain ranges, which reaches from western Ireland into Germany and was formed roughly 300 to 400 million years ago, during the Paleozoic Era. The Ardennes is a plateau cut deeply by the Meuse River and its tributaries. Its higher points contain peat bogs and have poor drainage; these uplands are unsuitable as cropland. A large depression, known east of the Meuse River as the Famenne and west of it as the Fagne, separates the Ardennes from the geologically and topographically complex foothills to the north. The principal feature of the area is the Condroz, a plateau more than 1,100 feet (335 metres) in elevation comprising a succession of valleys hollowed out of the limestone between sandstone crests. Its northern boundary is the Sambre-Meuse valley, which traverses Belgium from south-southwest to northeast. Situated south of the Ardennes and cut off from the rest of the country, Côtes Lorraines is a series of hills with north-facing scarps. About half of it remains wooded; in the south lies a small region of iron ore deposits. A region of sand and clay soils lying between 150 and 650 feet (45 and 200 metres) in elevation, the Central Plateaus cover northern Hainaut, Walloon Brabant, southern Flemish Brabant, and the Hesbaye plateau region of Liège. The area is dissected by the Dender, Senne, Dijle, and other rivers that enter the Schelde (Escaut) River; it is bounded to the east by the Herve Plateau. The Brussels region lies within the Central Plateaus. Bordering the North Sea from France to the Schelde is the low-lying plain of Flanders, which has two main sections. Maritime Flanders, extending inland for about 5 to 10 miles (8 to 16 km), is a region of newly formed and reclaimed land (polders) protected by a line of dunes and dikes and having largely clay soils. Interior Flanders comprises most of East and West Flanders and has sand-silt or sand soils. At an elevation of about 80 to 300 feet (25 to 90 metres), it is drained by the Leie, Schelde, and Dender rivers flowing northeastward to the Schelde estuary. Several shipping canals interlace the landscape and connect the river systems. Lying between about 160 and 330 feet (50 and 100 metres) in elevation, the Kempenland contains pastureland and is the site of a number of industrial enterprises; it forms an irregular watershed of plateau and plain between the extensive Schelde and Meuse drainage systems. Climate of Belgium Belgium has a temperate, maritime climate predominantly influenced by air masses from the Atlantic. Rapid and frequent alternation of different air masses separated by fronts gives Belgium considerable variability in weather. Frontal conditions moving from the west produce heavy and frequent rainfall, averaging 30 to 40 inches (750 to 1,000 mm) a year. Winters are damp and cool with frequent fogs; summers are rather mild. The annual mean temperature is around 50 °F (10 °C). Brussels, which is roughly in the middle of the country, has a mean minimum temperature of just below 32 °F (0 °C) in January and a mean maximum of about 71 °F (22 °C) in July. Regional climatic differences are determined by elevation and distance inland. Farther inland, maritime influences become weaker, and the climate becomes more continental, characterized by greater seasonal extremes of temperature. The Ardennes region, the highest and farthest inland, is the coldest. In winter, frost occurs on about 120 days, snow falls on 30 to 35 days, and January mean minimum temperatures are lower than elsewhere. In summer, the elevation counteracts the effect of distance inland, and July mean maximum temperatures are the lowest in the country. Because of the topography, the region has the highest rainfall in Belgium. In contrast, the Flanders region enjoys generally higher temperatures throughout the year. There are fewer than 60 days of frost and fewer than 15 of snow. On the seacoast these figures are reduced to below 50 and 10, respectively. There are a few hot days, especially on the coast, where the annual rainfall is the lowest in the country. More … Score: https://www.britannica.com/place/Belgium  

2022/07/21

Independence day of the Republic of Colombia

Colombia, officially Republic of Colombia, Spanish República de Colombia, country of northwestern South America. Its 1,000 miles (1,600 km) of coast to the north are bathed by the waters of the Caribbean Sea, and its 800 miles (1,300 km) of coast to the west are washed by the Pacific Ocean. The country is bordered by Panama, which divides the two bodies of water, on the northwest, Venezuela and Brazil on the east, and Peru and Ecuador on the south. It is more than twice the size of France and includes the San Andrés y Providencia archipelago, located off the Nicaraguan coast in the Caribbean, some 400 miles (650 km) northwest of the Colombian mainland. The population is largely concentrated in the mountainous interior, where Bogotá, the national capital, is situated on a high plateau in the northern Andes Mountains. The only American nation that is named for Christopher Columbus, the “discoverer” of the New World, Colombia presents a remarkable study in contrasts, in both its geography and its society. The lofty snow-tipped peaks of the country’s interior cordilleras tower high above equatorial forests and savannas where surviving Indian groups still follow the lifeways and traditions of their ancestors. In the cooler mountains, at intermediate elevations, modern cities are juxtaposed with traditional rural landscapes where mestizo farmers cultivate their small plots of coffee, corn (maize), and other crops. The more accessible Atlantic lowlands, dominated by large livestock haciendas and a tri-ethnic population, have a distinctively different character.Colombia strongly reflects its history as a colony of Spain. It is often referred to as the most Roman Catholic of the South American countries, and most of its people are proud of the relative purity of their Spanish language. Its population is heavily mestizo (of mixed European and Indian descent) with substantial minorities of European and African ancestry. The economy is traditionally based on agriculture, particularly coffee and fruit production, but industries and services are increasing in importance. Colombia is the most populous nation of Spanish-speaking South America. More than one-third of its inhabitants live in the six largest metropolitan areas, of which Bogotá is the largest. The nation’s political instability has been historically tied to the unequal distribution of wealth, and the illicit trade in drugs (mainly cocaine) remains a major disruptive factor in Colombian life. Land - Relief Few countries boast such striking physical variety as does Colombia. Its broken, rugged topography, together with its location near the Equator, creates an extraordinary diversity of climates, vegetation, soils, and crops. The Andean cordillera, one of the world’s great mountain ranges, dominates the landscape of the western part of the country, where most of the people live. North of the border with Ecuador the cordillera flares out into three distinct parallel ranges. Two great river valleys, those of the Magdalena and the Cauca, separate them and provide avenues of penetration from the Atlantic coastal lowlands into the heart of the country. Volcanic activity in the geologic past blocked the middle course of the Cauca River to form a great lake that once filled the western inter-Andean trough for some 120 miles (190 km) south of Cartago. The river eventually broke through the dam to leave the level floor of the Cauca valley at some 3,000 feet (900 metres) above sea level; today it is one of the nation’s most productive agricultural areas. The Colombian cordilleras belong to the northern portion of the great Andean mountain system, which extends along the Pacific coast of South America. The Andes are among the world’s most youthful mountain ranges and among the highest. The geologic history of this northern sector is less well understood than that of the central and southern parts. It is clear, however, that the entire cordillera has been thrust up through the subduction of the crumpled eastern margin of the Nazca Plate and, to the north, the Caribbean Plate under the more rigid but lighter South American Plate, which has been forced westward by the spreading Atlantic seafloor. These tectonic forces, similar to those found elsewhere around the Pacific Rim, continue to operate, as is evidenced by the high frequency of often destructive earthquakes. At the Pasto Massif, near the Ecuadoran border, the mountains divide into the Cordillera Occidental (“Western Range”), which runs parallel to the Pacific coast, and the Cordillera Central (“Central Range”), which, with its numerous volcanoes, forms the backbone of the system in Colombia and runs generally southwest to northeast. At the Great Colombian Massif of the Cordillera Central, near the San Agustín Archeological Park, the Cordillera Oriental (“Eastern Range”) branches off in a more decidedly northeasterly direction.Of the three ranges, the nonvolcanic Cordillera Occidental, which forms the barrier between the Cauca valley and the rain-drenched Pacific coast, is the lowest and least populated. Two passes at elevations less than 5,000 feet (1,500 metres) between Cali and Buenaventura on the Pacific coast mark the lowest depressions in the range. Elsewhere the crest is much higher, reaching 12,992 feet (3,960 metres) at Mount Paramillo in the department of Antioquia. From there the Cordillera Occidental fingers north into the three distinct serranías of Abibe, San Jerónimo, and Ayapel, forested ranges that drop gradually toward the piedmont plains of the Caribbean littoral. A lesser topographic feature on the Pacific coast is the Baudó Mountains, separated from the Cordillera Occidental by the valley of the Atrato River, which empties into the Caribbean Gulf of Urabá; the Baudó Mountains represent a southward extension of the Isthmus of Panama. The Cordillera Central is the highest of the Andean ranges of Colombia, rising to an average height of 10,000 feet (3,000 metres). It is a continuation of the Ecuadoran volcanic structure. Crystalline rocks are exposed at several places on its flanks and are the foci of localized gold and silver deposits. Sandstones and shales of the Paleogene and Neogene periods (about 65 to 2.6 million years ago) are also a part of the older basement that has been capped by ash and lava derived from some 20 volcanoes of the Quaternary Period (the past 2.6 million years). Several of the latter reach well into the zone of permanent snow, above 15,000 feet (4,600 metres). The highest are Mount Huila (18,865 feet [5,750 metres]), southeast of Cali, and the Ruiz-Tolima complex (some 17,700 feet [5,400 metres]) between Manizales and Ibagué. The fertile ash from their eruptions has produced the high, cool plateaus of Nariño department and the often steep slopes to the north that support much of Colombia’s coffee production. In November 1985 Mount Ruíz erupted, melting the snow and ice that covered it and sending great mudflows downslope, destroying the city of Armero and killing more than 25,000 in one of the country’s greatest catastrophes. North of Mount Ruíz, near Sonsón in the department of Antioquia, the volcanic Cordillera Central gives way to the deeply weathered, granitic Antioquia batholith (an exposed granitic intrusion), a tableland averaging some 8,000 feet (2,500 metres) above sea level. It is divided into two parts by the deep transverse cleft of the Porce River, which occupies the U-shaped valley in which is situated the expanding metropolis of Medellín, Colombia’s second city. The batholith contains gold-bearing quartz veins, which were the source of the placer gravels that gave rise to an active colonial mining economy. Beyond Antioquia the lower, remote San Lucas Mountains extend northward toward the confluence of the Magdalena and Cauca rivers. More … Score: https://www.britannica.com/place/Colombia

2022/07/20

DPIIT-CII delegation meeting with Ministry of Economic Development of Poland and Polish Agency for Investment and Trade

Useful discussions on deepening India-Poland economic ties , esp promoting investment and manufacturing in India, were held between officials of the Ministry of Economic Development of Poland and Polish Agency for Investment and Trade and the DPIIT-CII delegation, 24 June, 2022

2022/07/15

Polsko-rumuńskie konsultacje z udziałem wiceministrów Grzegorza Piechowiaka i Luciana-loan Rusa

Rozwój współpracy handlowej i inwestycyjnej między Polską a Rumunią, promocja eksportu, współpraca w ramach Inicjatywy Trójmorza, wsparcie Ukrainy i wpływ wojny na gospodarki – to główne tematy spotkania sekretarzy stanu odpowiedzialnych za handel międzynarodowy Luciana-loan Rusa wiceministra przedsiębiorczości i turystyki Rumunii oraz Grzegorza Piechowiaka, pełnomocnika rządu ds. inwestycji zagranicznych.

2022/07/15