Koncert humanitarny zespołu „Lado” w Krakowie i Katowicach

Narodowy Chorwacki Zespół Pieśni i Tańca „Lado” wystąpił na dwóch koncertach humanitarnych w Polsce. Pierwszy koncert odbył się we wtorek 29 czerwca w Krakowie w Centrum Kongresowym ICE, drugi w środę 30 czerwca w Katowicach w Sali koncertowej „Miasto Ogrodów” we współpracy z Zespołem Pieśni i Tańca „Śląsk“. Zebrane środki przeznaczone są na odbudowę chorwackich terenów dotkniętych trzęsieniem ziemi.

2021/07/07

La Embajada de Colombia en Polonia presentó de manera presencial las películas “Mamá” y “Jericó, el infinito vuelo de los días” en el Festival de Cultura de Viajes ŚwiatoPogląd de Torun

Como parte del Plan de Promoción de Colombia en el Exterior, la Embajada de Colombia en Polonia participó con la proyección de las películas “Mamá” y “Jericó, el infinito vuelo de los días” en el Festival de Cultura de Viajes ŚwiatoPogląd de la ciudad de Torun, cuya tercera edición se realizó del 18 al 20 de junio de 2021.

2021/07/07

Среща на Посланик Маргарита Ганева с г-н Анджей Гут-Мостови държавен секретар и пълномощник на министър-председателя за сектор туризъм и популяризирането на полската марка

На 24 юни 2021 г. в Министерство на развитието, труда и технологиите във Варшава се проведе среща на извънредния и пълномощен посланик на Република България в Република Полша, г-жа Маргарита Ганева с държавния секретар и пълномощник на министър-председателя за сектор туризъм и популяризирането на полската марка, Министерство на развитието, труда и технологиите на Република Полша, г-н Анджей Гут-Мостови, която се състоя по инициатива на българската страна.

2021/07/06

Muzeum Fałszerstw w Wiedniu

Jaka jest różnica między oryginałem, kopią a falsyfikatem? Jak fałszerze mogli rozpowszechniać swoje dzieła? Czy kopie i falsyfikaty są cenne same w sobie? Odpowiedź na te pytania można znaleźć w Muzeum Fałszerstw w Wiedniu, gdzie opowiadane są również ciekawe historie o fałszywych dziełach.

2021/07/06

Republic of Malawi Day

Malawi, landlocked country in southeastern Africa. Endowed with spectacular highlands and extensive lakes, it occupies a narrow, curving strip of land along the East African Rift Valley. Lake Nyasa, known in Malawi as Lake Malawi, accounts for more than one-fifth of the country’s total area. Most of Malawi’s population engages in cash-crop and subsistence agriculture. The country’s exports consist of the produce of both small landholdings and large tea and tobacco estates. Malawi has received a significant amount of foreign capital in the form of development aid, which has contributed greatly toward the exploitation of its natural resources and has allowed Malawi to at times produce a food surplus. Nevertheless, its population has suffered from chronic malnutrition, high rates of infant mortality, and grinding poverty—a paradox often attributed to an agricultural system that has favoured large estate owners. Most Malawians reside in rural locations. The country’s few large urban centres include Lilongwe, the capital, and Blantyre, the seat of the country’s judiciary. Land Malawi stretches about 520 miles (840 km) from north to south and varies in width from 5 to 100 miles (10 to 160 km). It is bordered by Tanzania to the north, Lake Malawi to the east, Mozambique to the east and south, and Zambia to the west. Relief While Malawi’s landscape is highly varied, four basic regions can be identified: the East African (or Great) Rift Valley, the central plateaus, the highlands, and the isolated mountains. The East African Rift Valley—by far the dominant feature of the country—is a massive troughlike depression running through the country from north to south and containing Lake Malawi (north and central) and the Shire River valley (south). The lake’s littoral, situated along the western and southern shores and ranging from 5 to 15 miles (8 to 24 km) in width, covers almost one-tenth of the total land area and is dotted with swamps and lagoons. The Shire valley stretches some 250 miles (400 km) from the southern end of Lake Malawi at Mangochi to Nsanje at the Mozambique border and contains Lake Malombe at its northern end. The plateaus of central Malawi rise to elevations of 2,500 to 4,500 feet (760 to 1,370 metres) and lie just west of the Lake Malawi littoral; the plateaus cover about three-fourths of the total land area. The highland areas are mainly isolated tracts that rise as much as 8,000 feet (2,400 metres) above sea level. They comprise the Nyika, Viphya, and Dowa highlands and Dedza-Kirk mountain range in the north and west and the Shire Highlands in the south. The isolated massifs of Mulanje (which reach 9,849 feet [3,002 metres], the highest point in the country) and Zomba (which reach 6,846 feet [2,087 metres]) represent the fourth physical region. Surmounting the Shire Highlands, they descend rapidly in the east to the Lake Chilwa–Phalombe plain. Drainage and soils The major drainage system is that of Lake Malawi, which covers some 11,430 square miles (29,600 square km) and extends beyond the Malawi border. It is fed by the North and South Rukuru, Dwangwa, Lilongwe, and Bua rivers. The Shire River, the lake’s only outlet, flows through adjacent Lake Malombe and receives several tributaries before joining the Zambezi River in Mozambique. A second drainage system is that of Lake Chilwa, the rivers of which flow from the Lake Chilwa–Phalombe plain and the adjacent highlands. Soils, distributed in a complex pattern, are composed primarily of red earths, with brown soils and yellow gritty clays on the plateaus. Alluvial soils occur on the lakeshores and in the Shire valley, while other soil types include hydromorphic (excessively moist) soils, black clays, and sandy dunes on the lakeshore. Climate There are two main seasons—the dry season, which lasts from May to October, and the wet season, which lasts from November to April. Temperatures vary seasonally, and they tend to decrease on average with increasing elevation. Nsanje, in the Shire River valley, has a mean July temperature in the high 60s F (low 20s C) and an October mean in the mid-80s F (high 20s C), while Dedza, which lies at an elevation of more than 5,000 feet (1,500 metres), has a July mean in the high 50s F (mid-10s C) and an October mean in the high 60s F (low 20s C). On the Nyika Plateau and on the upper levels of the Mulanje massif, frosts are not uncommon in July. Annual precipitation levels are highest over parts of the northern highlands and on the Sapitwa peak of the Mulanje massif, where they are about 90 inches (2,300 mm); they are lowest in the lower Shire valley, where they range from 25 to 35 inches (650 to 900 mm). Plant and animal life The natural vegetation pattern reflects the country’s diversity in relief, soils, and climate. Savanna (grassy parkland) occurs in the dry lowland areas. Miombo woodlands—sparse, open deciduous woodland characteristic of dry parts of eastern Africa—are an important habitat, particularly for the country’s large mammal populations. Woodlands with species of acacia trees cover isolated, more fertile plateau sites and river margins. Grass-covered broad depressions, called madambo (singular: dambo), dot the plateaus. Grasslands and evergreen forests are found in conjunction on the highlands and on the Mulanje and Zomba massifs. However, Malawi’s natural vegetation has been altered significantly by human activities. Swamp vegetation has given way to agricultural species as swamps have been drained and cultivated. Much of the original woodland has been cleared, and, at the same time, forests of softwoods have been planted in the highland areas. High population density and intensive cultivation of the Shire Highlands have also hindered natural succession there, while wells have been sunk and rivers dammed to irrigate the dry grasslands for agriculture. Game animals abound only in the game reserves, where antelope, buffalo, elephants, leopards, lions, rhinoceroses, and zebras occur; hippopotamuses live in Lake Malawi. The lakes and rivers of Malawi contain hundreds of species and numerous families of fish. Lake Malawi is particularly renowned for its remarkable biodiversity—an enormous range of fish species inhabit the lake, most of them endemic—and its southern region, as part of Lake Malawi National Park, was designated a UNESCO World Heritage site in 1984. The most common and commercially significant fish found in Malawi include the endemic tilapia, or chambo (nest-building freshwater fish); catfish, or mlamba; and minnows, or matemba. The Ministry of Mines, Natural Resources, and Environmental Affairs is charged with the responsibility of ensuring the protection of Malawi’s environment, mainly through the implementation of the Environmental Management Act of 1996. Among the major concerns are efficient resource utilization, land degradation, deforestation, conservation of marine life, biodiversity, climate change, ozone layer protection, sewage, the pollution of water from agriculture runoff such as fertilizers, endangered species, and industrial pollution. The majority of pollution comes from greenhouse gas emissions, mostly from the usage of coal and charcoal, natural gas, and petroleum. People of Malawi - Ethnic groups and languages Ten major ethnic groups are historically associated with modern Malawi—the Chewa, Nyanja, Lomwe, Yao, Tumbuka, Sena, Tonga, Ngoni, Ngonde, and the Lambya/Nyiha. All the African languages spoken are Bantu languages. From 1968 to 1994, Chewa was the only national language; it is now one of the numerous languages used in print and broadcast media and is spoken by a majority of the population. In 1996 government policy indicated that education in grades 1–4 would be provided in the students’ mother tongue or vernacular language; from grade 5, the medium of instruction would be English, which, though understood by less than one-fifth of the population at independence in 1964, continues to be used widely in business, administrative and judicial matters, higher education, and elsewhere. Other major languages include Lomwe, Yao, and Tumbuka. More … Score: https://www.britannica.com/place/Malawi

2021/07/06

Ambasador Tajlandii na Mistrzostwach Polski Muaythai IFMA w Krakowie

Chettaphan Meksamphan, Ambasador Tajlandii w Warszawie, przyjechał do Krakowa, by wziąć udział w rozgrywanych u nas Mistrzostwach Polski Muaythai IFMA dla dzieci, kadetów, juniorów i seniorów oraz Mistrzostwach Polski Wai Khru i Kick Pads dla dzieci 6-11 lat. Uroczystość otwarcia mistrzostw, w której uczestniczył zarówno Prezydent Miasta Krakowa Jacek Majchrowski, jak i Ambasador Chettaphan Meksamphan odbyła się w hali sportowej III Liceum Ogólnokształcącego na os. Wysokim w Krakowie.

2021/07/05

La Embajada de Colombia en Polonia realizará la proyección de UNIBIRDS

Como parte del Plan de Promoción de Colombia en el Exterior, la Embajada de Colombia en Polonia realizará una proyección de UNIBIRDS, obra de los artistas colombianos Sergio Mantilla y Miguel Chaparro, en el metro de Varsovia y en el Rondo Romana Dmowskiego, durante los días viernes 25 y sábado 26 de junio de 2021 respectivamente.

2021/07/05

Independence Day of Cape Verde

Cabo Verde, also called Cape Verde, country comprising a group of islands that lie 385 es (620 km) off the west coast of Africa. Praia, on Santiago, is the capital. Cabo Verde is named for the westernmost cape of Africa, Cape Verde (French: Cap Vert), which is located in nearby Senegal and is the nearest point on the continent. The largest port in the islands is located at Mindelo, on São Vicente. Its deepwater harbour accommodates sizable vessels and has been used as a fueling station since the 19th century. Land Cabo Verde consists of nine inhabited islands, one uninhabited island, and various islets, located between 14°30′ and 17°30′ N and between 22°30′ and 25°30′ W. The archipelago is divided into the Barlavento (Windward) group to the north and the Sotavento (Leeward) group to the south. The Barlavento Islands include Santo Antão, São Vicente, Santa Luzia (which is uninhabited), São Nicolau, Sal, and Boa Vista, together with the islets of Raso and Branco. The Sotavento Islands include Maio, Santiago, Fogo, and Brava and the three islets called the Rombos—Grande, Luís Carneiro, and Cima. Relief, drainage, and soils The terrain of the Cabo Verde islands varies from the geologically older, flatter islands in the east and the newer, more mountainous islands in the west. The eastern islands of Boa Vista, Maio, and Sal, for example, have been heavily eroded by the wind over time and are very sandy and flat. The others are very rocky, jagged, and mountainous. Fogo (“Fire”) Island’s active volcano, Pico, rises 9,281 feet (2,829 metres) and is the highest point of the archipelago. On the northern island of Santo Antão, Tope de Coroa reaches 6,493 feet (1,979 meters). There are few permanent watercourses in the islands, which generally suffer from seasonal rains, cyclical drought, and chronic water shortages. When precipitation does occur, it is often in the form of torrential downpours that cause significant damage through water erosion, flooding, and the destruction of containment dams. Cabo Verde’s soils, primarily volcanic or igneous in origin, are generally shallow, coarse, and rocky. Almost a quarter of the land area is rock of volcanic origin; basalt is a common type. More than three-fifths of the land is arid and lacking in humus and thus is suitable only for rough grazing; sand and limestone outcrops are common in these areas. Only a fraction of the total area has proper humus and sufficient water supplies for significant irrigation agriculture. Soil loss through wind and water erosion is a serious challenge. Since independence a nationwide campaign to prevent erosion—e.g., by promoting reforestation—has been under way. Climate Generally moderate, the climate is characterized by stable temperatures with extreme aridity. February is the coolest month, with temperatures in the low 70s F (low 20s C). August and September are the hottest and wettest months, with temperatures in the low 80s F (high 20s C). The islands are profoundly affected by the two-season nature of the intertropical convergence zone (ITCZ), a belt of converging trade winds and rising air that encircles Earth near the Equator. Winter winds from Europe are cool and dry, but in the summer months the ITCZ front moves to the north and the Guinea Current brings more heat and moisture, which can result in increased precipitation, especially in the higher elevations of the more mountainous islands. Precipitation levels are a function of how far north the ITCZ progresses and how much tropical moisture it carries and are, as a result, unpredictable: years may go by with little or no precipitation. The clashing fronts near Cabo Verde generate hurricanes that travel westward across the Atlantic Ocean to the Caribbean and the eastern coast of the United States. Plant and animal life On most of the larger islands, elevations are great enough to generate precipitation on the windward slopes; grasses and some pine plantations are found in these relatively moist locations. The leeward slopes, however, exhibit a characteristic rain-shadow effect that produces desert conditions, and the sparse shrub cover almost disappears. The shrubs remaining in these areas are mostly thorny or bitter; some are toxic. Agriculture is practiced either in a limited way at high elevations or by intense terracing of the sharp-cut valleys. Some xerophilous (desert-type) plants are found rooted in the brackish subsoil of Maio, Sal, and Boa Vista. The scarcity of water limits the number of land turtles in the archipelago, but two species of sea turtles lay their eggs on the sandy shores of the uninhabited islets. There are many geckos and lizards and several species of skinks, including a rare and endangered giant skink. There are a number of species of butterflies, but none is endemic, and all the species are of African origin. There are more than 100 known species of birds, of which only a portion, including four species of petrels and two of shearwaters, breed regularly. Other bird species include the greater flamingo, the frigate bird and the buzzard (both nearly extinct), the Egyptian vulture, the Cape Verde Islands kite, and the red-billed tropic bird. Several other birds are represented by local species, of which the kingfisher is among the most conspicuous. The only truly endemic species, however, are the cane warbler and the Raso lark, which is restricted to Raso, one of the smallest uninhabited islets. The rest of the birds are overseas migrants. Remarkably, gulls and terns do not breed on the islands. Mammals of Cabo Verde include the feral goats found on Fogo, the descendants of domestic goats that were taken to the islands. The islands’ rodent population probably originated with rodents carried on early ships. Monkeys, introduced from the African continent, are also present on the islands. The long-eared bat is the only indigenous mammal. People - Ethnic groups The overwhelming majority of the population of Cabo Verde is of mixed European and African descent and is often referred to as mestiço or Crioulo. There is also an African minority, which includes the Fulani (Fulbe), the Balante, and the Mandyako peoples. A small population of European origin includes those of Portuguese descent (especially from the Algarve, a historical province, and the Azores islands), as well as those of Italian, French, and English descent. There is also a substantial number that traces its roots to Sephardic Jews who were expelled from the Iberian Peninsula in the 15th and 16th centuries during the Inquisition and were among the islands’ early settlers, or to other groups of Jews—mainly tradesmen—who arrived in the 19th century from Morocco. Languages Although Portuguese is the official language and is used in formal situations, Crioulo, one of the oldest of the Portuguese creole languages, is by far the most widely spoken. The different dialects of Crioulo that exist on the islands may be broadly divided into Sotavento and Barlavento groups. There has been a struggle to legitimate and regularize Crioulo orthography in a dictionary and in schools. Religion of Cabo Verde The majority of the population is Roman Catholic, but a flourishing Protestant mission is based in Praia with a publishing venture in Fogo. In practice, Catholicism is often enriched with African elements. The celebration of saints’ days, for example, may be accompanied by drumming, processionals, masks, and dancing in African styles, particularly on Santiago. Although many Cabo Verdeans can trace Jewish ancestry, virtually none are practicing. More … Score: https://www.britannica.com/place/Cabo-Verde

2021/07/05

Independence Day of the Bolivarian Republic of Venezuela

Venezuela, country located at the northern end of South America. It occupies a roughly triangular area that is larger than the combined areas of France and Germany. Venezuela is bounded by the Caribbean Sea and the Atlantic Ocean to the north, Guyana to the east, Brazil to the south, and Colombia to the southwest and west. The national capital, Caracas, is Venezuela’s primary centre of industry, commerce, education, and tourism. Venezuela administers a number of Caribbean islands and archipelagos, among which are Margarita Island, La Blanquilla, La Tortuga, Los Roques, and Los Monjes. Since the early 19th century Venezuela has claimed jurisdiction over Guyanese territory west of the Essequibo River totaling some 53,000 square miles (137,000 square km)—nearly two-thirds of the land area of Guyana. Venezuela also has had a long dispute with Colombia over the delimitation of maritime boundaries in the Gulf of Venezuela and around the archipelago of Los Monjes. A physiographically diverse country, Venezuela incorporates the northern Andean mountain chains and interior highlands, the main portions of the Orinoco River basin with its expansive Llanos (plains), Lake Maracaibo, which is the largest lake in South America, and the spectacular Angel Falls, the world’s highest waterfall. The republic’s development pattern has been unique among Latin American countries in terms of the speed, sequence, and timing of economic and demographic growth. In the 20th century Venezuela was transformed from a relatively poor agrarian society to a rapidly urbanizing one, a condition made possible by exploiting huge petroleum reserves. These changes, however, have been accompanied by imbalances among the country’s regions and socioeconomic groups, and Venezuela’s cities have swelled because of a massive and largely uncontrolled migration from rural areas, as well as mass immigration, much of it illegal, from Colombia and other neighbours. Venezuela, like many Latin American countries, has a high percentage of urban poverty, a massive foreign debt, and widespread governmental patronage and corruption. Venezuela’s social and political ills have been compounded by natural disasters such as the floods that devastated sections of Caracas, La Guaira, and other coastal areas in late 1999. On the other hand, the republic since 1958 has been more democratic and politically stable than most other Latin American nations, and its economic prospects remain strong, particularly in regard to the petroleum industry. The land The Venezuelan landscape includes towering mountains, tropical jungles, broad river plains, and arid coastal plains, all of which provide a diversity of natural habitats and a range of challenges to social integration and economic development. More … Score: https://www.britannica.com/place/Venezuela  

2021/07/05