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

2021/07/23

Zapraszamy do udziału w spotkaniu biznesowym online nt. możliwości współpracy na rynku indyjskim

Wydarzenie realizowane będzie we współpracy z Federation of Indian Chambers of Commerce and Industry, Indo – Polish Chamber of Commerce and Industry oraz przy wsparciu Ambasady RP w New Delhi. Spotkanie będzie miało charakter informacyjno – networkingowy, z krótkimi prezentacjami i dyskusją. Do udziału zapraszamy wybranych partnerów GT ze strony indyjskiej.

2021/07/21

Serdecznie zapraszamy na wystawę fotografii Tomasza Pruchnickiego „Karaiby”

Serdecznie zapraszamy na wystawę fotografii Tomasza Pruchnickiego „Karaiby” w Ośrodku wystawienniczym Kasztel w Szymbarku koło Gorlic. Wystawę można będzie oglądać od 22 lipca do 18 sierpnia bieżącego roku. Pasjonat fotografii i podróżnik udokumentował swoją fascynującą podróż do świata kultury majów i pragnie podzielić się pięknem Karaibów z miejscową społecznością.

2021/07/21

Otwarcie biura EDF w Warszawie i powołanie Thierry’ego Deschaux na stanowisko dyrektora zarządzającego

12 lipca 2021 r. podczas spotkania zorganizowanego w Rezydencji Ambasadora Francji z przedstawicielami polskiej prasy, Thierry Deschaux ogłosił otwarcie biura spółki EDF w Warszawie, na którego czele stanął jako Dyrektor Zarządzający.

2021/07/21

Wystąpienie Chargé d'affaires Izraela w Senacie RP

​Tekst wystąpienia chargé d'affaires Izraela w Polsce Tal Ben-Ari Yaalon podczas wysłuchania publicznego przed Komisją Ustawodawczą oraz Komisą Praw Człowieka, Praworządności i Petycji Senatu RP w ramach prac nad ustawą o zmianie ustawy – Kodeks postępowania administracyjnego (Kpa)​.

2021/07/21

Firma del Convenio de Cooperación entre la Cámara de Comercio de Lima y la Cámara de Comercio de Polonia

Con el objeto de promover el comercio, la cooperación técnica y las relaciones en el ámbito económico entre el Perú y Polonia, la Cámara de Comercio de Lima (CCL) y la Cámara Nacional de Comercio de Polonia (KIG) firmaron el 15 de Junio de 2021 el Memorando de Entendimiento (MdE) relativo a la cooperación bilateral.

2021/07/21

Specjalna wysłannik U.S. Department of State ds. Holokaustu kończy wizytę w Polsce.

Cherrie Daniels spotkała się ze strażnikami pamięci z muzeów, instytucji kultury i pomników historii. W Kielcach i Jedwabnem oddała hołd ofiarom tragedii, które komunistyczne władze chciały wymazać́ z kart historii. W Warszawie odwiedziła miejsce pamięci o jednym z najtragiczniejszych wydarzeń́ II WŚ i bohaterstwie Polaków walczących o wyzwolenie spod okupacji - Muzeum Powstania Warszawskiego, w Auschwitz - wstrząsające pozostałości po fabryce zagłady, która wyrosła na fundamentach pogardy dla drugiego człowieka.

2021/07/21

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  

2021/07/21

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

2021/07/20