Ecuador Travel Information - Ecuador Ministry of Tourism

Welcome to Ecuador´s official site. You will find here all the INFORMATION about the country and its favorite tourist DESTINATIONS. You will also find USEFUL INFORMATION for your comfort and security if you´re PLANNING A TRIP to Ecuador.

2026/08/12

Independence Day of the Republic of Chad

Chad, landlocked state in north-central Africa. The country’s terrain is that of a shallow basin that rises gradually from the Lake Chad area in the west and is rimmed by mountains to the north, east, and south. Natural irrigation is limited to the Chari and Logone rivers and their tributaries, which flow from the southeast into Lake Chad. The capital, N’Djamena (formerly Fort-Lamy), is almost 1,000 miles (1,600 km) by road from the western African coastal ports. Although it is the fifth largest country on the continent, Chad—much of the northern part of which lies in the Sahara—has a population density of only about 20 persons per square mile (8 persons per square km). Most of the population lives by agriculture; cotton is grown in the south, and cattle are raised in the central region. Chad joined the ranks of oil-producing countries in 2003, raising hopes that the revenues generated would improve the country’s economic situation. Land Chad is bounded on the north by Libya, on the east by Sudan, on the south by the Central African Republic, and on the west by Cameroon, Nigeria, and Niger. The frontiers of Chad, which constitute a heritage from the colonial era, do not coincide with either natural or ethnic boundaries. Relief and drainage In its physical structure Chad consists of a large basin bounded on the north, east, and south by mountains. Lake Chad, which represents all that remains of a much larger lake that covered much of the region in earlier geologic periods, is situated in the centre of the western frontier; it is 922 feet (281 metres) above sea level. The lowest altitude of the basin is the Djourab Depression, which is 573 feet (175 metres) above sea level. In the early Holocene Epoch, possibly until as recently as 7,000 years ago, the lake stood at a level of about 1,100 feet (335 metres) above sea level, or some 180 feet (55 metres) higher than today, and was as much as 550 feet (170 metres) deep. At that stage Mega-Chad, as it has been called, occupied an area of some 130,000 square miles (336,700 square km) and overflowed southward via the present-day Kébi River and then over the Gauthiot Falls westward to the Benue River and the Atlantic Ocean. Older dune systems, flooded by Mega-Chad, form linear islands in the present lake and extend hundreds of miles to the east, the interdunal hollows being occupied by diatomites and other lake sediments. The mountains that rim the basin include the volcanic Tibesti Massif to the north (of which the highest point is Mount Koussi, with an elevation of 11,204 feet [3,415 metres]), the sandstone peaks of the Ennedi Plateau to the northeast, the crystalline rock mountains of the Ouaddaï (Wadai) region to the east, and the Oubangui Plateau to the south. The semicircle is completed to the southwest by the mountains of Adamawa and Mandara, which lie mostly beyond the frontier in Cameroon and Nigeria. Chad’s river network is virtually limited to the Chari and Logone rivers and their tributaries, which flow from the southeast to feed Lake Chad. The remaining Chad waterways are either seasonal or are of insignificant size. The Chari, which arises from headstreams in the Central African Republic to the south, is later joined from the east by the Salamat Wadi and from the west by the Ouham River, its largest tributary. After entering an ill-defined area of swampland between Niellim and Dourbali, it flows through a large delta into Lake Chad. The Chari is about 750 miles (1,200 km) in length and has a flow that normally varies between 600 and 12,000 cubic feet (17,000 to 340,000 litres) per second, according to the season. The Logone, which for some of its course runs along the Cameroon frontier, is formed by the junction of the Pendé and Mbéré rivers; its flow varies between 170 and 3,000 cubic feet (4,800 and 85,000 litres) per second, and its course is more than 600 miles (965 km) long before it joins the Chari at N’Djamena. The level of Lake Chad fluctuates according to the flow of these rivers, as well as according to the degree of precipitation, evaporation, and seepage. The droughts of the 1970s and early ’80s in the Sahel region of western Africa reduced the lake to record low levels. By 1985 it had been reduced to a pool, immediately to the north of the Chari–Logone mouth, occupying about 1,000 square miles (2,600 square km). The size of the lake continued to decline, and in the early 21st century, the area was typically about 580 square miles (1,500 square km). Soils Several types of soil formation occur in Chad, apart from the sand of the desert zone and the sheer rock of the mountainous areas. On the south side of Lake Chad the soils are derived from clayey deposits that accumulated on the floor of Mega-Chad. Along the seasonally flooded banks of the Chari and Logone rivers and the Salamat Wadi, hydromorphic (waterlogged) soils occur. Tropical iron-bearing soils, red in colour, are found on the exposed folds and mounds of the Ouaddaï region’s upland slopes. In the area north of Lake Chad, subarid soils are characteristic, except in the depressions that occur between the dunes on the shores of Lake Chad, where hydromorphic soils liable to salinization are found. Climate of Chad Chad’s wide range in latitudes (that extend southward from the Tropic of Cancer for more than 15°) is matched by a climatic range that varies from wet and dry tropical to hot arid. At the towns of Moundou and Sarh, in the wet and dry tropical zone, between 32 and 48 inches (800 and 1,200 mm) of rain falls annually between May and October. In the central semiarid tropical (Sahel) zone, where N’Djamena is situated, between 12 and 32 inches (300 and 800 mm) of rain falls between June and September. In the north rains are infrequent, with an annual average of less than one inch being recorded at Largeau. Chad thus has one relatively short rainy season. The dry season, which lasts from December to February everywhere in the country, is relatively cool, with daytime temperatures in the mid-80s to mid-90s F (upper 20s to mid-30s C) and nighttime temperatures that drop to the mid-50s F (low to mid-10s C). From March onward it becomes very hot until the first heavy rains fall. At N’Djamena, for example, daytime temperatures average more than 100° F (38° C) between March and June. Heavy rains begin at N’Djamena in July, and average daytime temperatures drop to the low 90s F (mid-30s C), but nighttime temperatures remain in the 70s F (20s C) until the onset of N’Djamena’s dry, cool season in November. Plant and animal life Three vegetation zones, correlated with the rainfall, may be distinguished. These are a wet and dry tropical zone in the south, characterized by shrubs, tall grasses, and scattered broad-leaved deciduous trees; a semiarid tropical (Sahel) zone, in which savanna vegetation gradually merges into a region of thorn bushes and open steppe country; and a hot arid zone, composed of dunes and plateaus in which vegetation is scarce and occasional palm oases are to be found. The tall grasses and the extensive marshes of the savanna zone have an abundant wildlife. There large mammals—such as elephants, hippopotamuses, rhinoceroses, warthogs, giraffes, antelopes, lions, leopards, and cheetahs—coexist with a wide assortment of birds and reptiles. The rivers and the lake are among the richest in fish of all African waters. The humid regions also contain swarms of insects, some of which are dangerous. More … Score: https://www.britannica.com/place/Chad  

2026/08/11

Passion Made Possible - Visit Singapore Official Site

Get inspired by the official destination website on what to see and do in Singapore. Find local guides, traveller essentials and discover new possibilities.

2026/08/11

Discover N'Djamena The Capital City of Chad November 2020 (Central Africa)

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2026/08/10

Independence day of the Republic of Ecuador

Ecuador, country of northwestern South America. Ecuador is one of the most environmentally diverse countries in the world, and it has contributed notably to the environmental sciences. The first scientific expedition to measure the circumference of Earth, led by Charles-Marie de La Condamine of France, was based in Ecuador. Moreover, research in Ecuador by the renowned naturalists Alexander von Humboldt of Prussia and Charles Darwin of England helped establish basic theories of modern geography, ecology, and evolutionary biology. Ecuador has a rich cultural heritage. Much of what is now Ecuador came to be included in the Inca empire, the largest political unit of pre-Columbian America. Economically, Ecuador became known for exporting Panama hats (straw hats so named because they were shipped to Panama in the mid-18th century and bought by traveling gold seekers and because they were worn by Panama Canal work crews in the early 19th century) and agricultural products, notably cacao (the source of cocoa beans), bananas, and flowers. It is a major exporter of petroleum and an increasingly important tourist destination. Its history has been marked by political and economic challenges, including long periods of military rule, boom-and-bust economic cycles, and inequitable distributions of wealth. Ecuador is unusual among Latin American countries in having two major centres of population and commerce, the vibrant port city of Guayaquil acting as a counterbalance to the capital, Quito, located in the Andean highlands in the north-central part of the country. Land – Relief Ecuador straddles part of the Andes Mountains and occupies part of the Amazon basin. Situated on the Equator, from which its name derives, it borders Colombia to the north, Peru to the east and the south, and the Pacific Ocean to the west. It includes the Pacific archipelago of the Galapagos Islands (Archipiélago de Colón). The Costa is composed of lowlands that extend eastward from the Pacific Ocean to the western edge of the Andes and rise from sea level to an elevation of 1,650 feet (500 metres). Running north-south, small coastal mountain ranges—the Colonche, Chindul, and Mache mountains—rise to 2,600 feet (800 metres). Between these coastal ranges and the Andes, interior valleys are mantled with silt deposits left by rivers that largely drain into the Gulf of Guayaquil. Puná, in the gulf, is the major island. The Sierra includes two high mountain chains and their western and eastern foothills. The western and central ranges of the Andes bordering the Sierra constitute the country’s highest and most continuous mountain chains. Many peaks are volcanic or snow-covered; these include Cayambe (18,996 feet [5,790 metres]), Antisana (18,714 feet [5,704 metres]), Cotopaxi, which is one of the world’s highest active volcanoes (19,347 feet [5,897 metres]), Chimborazo (20,702 feet [6,310 metres]), Altar (17,451 feet [5,319 metres]), and Sangay (17,158 feet [5,230 metres]). These are included in two ranges connected at intervals by transversal mountain chains, between which are large isolated valleys or basins, called hoyas. To the east of the main ranges are peaks Reventador (11,434 feet [3,485 metres]) and Sumaco (12,759 feet [3,889 metres]); the Cordillera de Cutucú, which borders the Upano valley and includes the central peaks; and the Cordillera del Cóndor to the south, which borders the Zamora valley. Beyond this eastern cordillera, to the east, is the Amazon basin, extending below 900 feet (300 metres). The volcanic Galapagos Islands consist of 19 rugged islands and scores of islets and rocks situated about 600 miles (900 km) west of the mainland. The largest island, Isabela (Albemarle), rises to 5,541 feet (1,689 metres) at Mount Azul, the archipelago’s highest point. The second largest island is Santa Cruz. Because Ecuador is situated on the Ring of Fire—the long horseshoe-shaped seismically active belt of earthquake epicentres, volcanoes, and tectonic plate boundaries that fringes the Pacific basin—it has experienced several significant and deadly earthquakes. Drainage Numerous rivers originate in the mountains, pass through the hoyas of the Sierra, and flow either west to the Pacific coast or east to the Amazon River. In the Sierra the rivers are torrential in their upper courses and become calmer in the plains areas but nonetheless remain unnavigable. The main watercourse of the Costa is the Guayas River. Formed by the juncture of the Daule and Babahoyo rivers and their affluents, the Guayas River is navigable for the greater part of its course. Other rivers that flow to the ocean include the Cayapas, the Esmeraldas, the Naranjal, the Jubones, and the Santa Rosa. The rivers of the Oriente carry the greatest volume of water. The most important is the Napo River, which receives the Coca and Aguarico rivers as well as other large tributaries as it takes its course toward Peru, where it joins the Amazon River. Other large rivers include the Pastaza, Morona, and Santiago, all of which drain into the Marañón River in Peru. Soils Ecuador’s soils are among the most varied on Earth. Volcanic activity at higher elevations in the Andes has resulted in the formation of fertile volcanic and prairie soils, called andosols and mollisols, with dark surface layers rich in organic matter. However, the soils are typically underlain by a yellow hardpan, locally called cangahua, which is often exposed on eroded steeper slopes. The eroded topsoil accumulates on lower slopes and especially on flats, which form the most desirable locations for agriculture. Indigenous people, over thousands of years, developed effective methods for the fertilization of these soils, including the use of manure, the mounding of fertilizing muck from drainage ditches, the creation of raised fields, and the use of irrigation canals. In the Costa the floodplains of the Guayas and other rivers have accumulated fertile silts from the highlands. These coastal soils are of great fertility but often consist of clays that are subject to shrinking and swelling and thus present problems for construction. The effectiveness of traditional methods of managing these soils has come to be more widely recognized, and such prehistoric techniques as embanked fields for runoff management (albarradas) and raised fields (artificially constructed earthen platforms built on shallow lakes or marshy areas) have been studied by development experts. In the Amazon basin, soils have not been fully studied and mapped; nevertheless, it appears that soils there are quite diverse, including areas of fertile alluvial soil, organic soils called histosols, and more-weathered tropical soils called oxisols. The latter may be used for crops with appropriate technology, such as shifting cultivation or agroforestry (crops and useful trees managed together), but some agronomists suggest that they are better utilized for timber and other renewable tropical forest products. More … Score: https://www.britannica.com/place/Ecuador

2026/08/10

National Day of The Republic of Singapore

Singapore, city-state located at the southern tip of the Malay Peninsula, about 85 miles (137 kilometres) north of the Equator. It consists of the diamond-shaped Singapore Island and some 60 small islets; the main island occupies all but about 18 square miles of this combined area. The main island is separated from Peninsular Malaysia to the north by Johor Strait, a narrow channel crossed by a road and rail causeway that is more than half a mile long. The southern limits of the state run through Singapore Strait, where outliers of the Riau-Lingga Archipelago—which forms a part of Indonesia—extend to within 10 miles of the main island. Singapore is the largest port in Southeast Asia and one of the busiest in the world. It owes its growth and prosperity to its focal position at the southern extremity of the Malay Peninsula, where it dominates the Strait of Malacca, which connects the Indian Ocean to the South China Sea. Once a British colony and now a member of the Commonwealth, Singapore first joined the Federation of Malaysia on its formation in 1963 but seceded to become an independent state on August 9, 1965. The land - Relief Nearly two-thirds of the main island is less than 50 feet (15 metres) above sea level. Timah Hill, the highest summit, has an elevation of only 531 feet (162 metres); with other peaks, such as Panjang and Mandai hills, it forms a block of rugged terrain in the centre of the island. To the west and south are lower scarps with marked northwest-southeast trends, such as Mount Faber. The eastern part of the island is a low plateau cut by erosion into an intricate pattern of hills and valleys. These physical units reflect their geologic foundations: the central hills are formed from granite rocks, the scarp lands from highly folded and faulted sedimentary rocks, and the eastern plateau from uncompacted sands and gravels. Drainage and soils A dense network of short streams drains the island, but floods are locally severe because the streams have low gradients and because of excessive water runoff from cleared land. Many streams, especially those draining northward, have broad mangrove-fringed estuaries that extend far inland. None of the soils is even reasonably fertile, but those derived from the granites tend to be better than most. Soils developed from the sedimentary rocks are variable, but many contain hardpans (compacted layers) that restrict plant roots and impede soil drainage. The soils of eastern Singapore are extremely infertile. All have suffered extensive degradation through erosion as a result of generations of careless human exploitation. Climate Singapore is in the equatorial monsoon region of Southeast Asia, and its climate is characterized by uniformly high temperatures and nearly constant precipitation throughout the year. The average monthly temperature varies from about 81° F (27° C) in June to 77° F (25° C) in January. The daily range is somewhat greater, averaging about 13° F (7° C). Singapore’s maritime location and constant humidity, however, keep maximum temperatures relatively moderate: the highest temperature ever recorded was only 97° F (36° C). The seasons are defined by the relative incidence of rainfall, which, in turn, is determined by the movements of the monsoon air masses. The wettest and windiest period is during the northeast monsoon (November–March), with rainfall reaching an average monthly high of more than 10 inches (250 millimetres) in December. Conversely, the period of the least amount of rainfall and the lightest winds is during the southwest monsoon (May–September), with rainfall dropping to a monthly low of less than 7 inches in July. April and October are intermonsoonal periods characterized by sluggish air movements and intense afternoon showers and thunderstorms. Altogether, Singapore’s precipitation averages about 95 inches annually, and rain falls somewhere on the island every day of the year. Plant and animal life Little remains of the original vegetation or animal life, except for a few thousand acres of evergreen rain forest preserved around catchment areas. Some mangrove vegetation survives in the Kranji area on the northwest side of the island, but elsewhere tracts of scrub or cogon grass (called lalang locally) are common. Many exotic plants have been introduced for ornamental use. The largest native animals are the long-tailed macaque (an Asian species of monkey), the slow loris (a large-eyed tailless nocturnal lemur), and the scaly anteater. Birds are numerous, especially those like the Indian mynah bird, the brahminy kite (a kite with reddish brown plumage and a white head and breast), and the house swallow that have adapted to a symbiotic relationship with humans. Reptiles, such as cobras and lizards, also are common. Fringing coral reefs with their associated fish and wildlife occur around many parts of the coast. Settlement patterns The city of Singapore is situated in the southern portion of the main island. Over time, urbanization has blurred the differences between city and country. Built-up areas now cover a large part of the city-state. The older parts of the city have been substantially refurbished, especially along the Singapore River but elsewhere as well. The once-common Chinese shop-house, consisting of living quarters above a commercial establishment, gradually has been disappearing from the city. Instead, the government’s Housing and Development Board (HDB) has relocated commerce into separate districts and has created integrated residential communities inhabited by people with a mixture of incomes. About four-fifths of Singapore’s population now resides in high-rise HDB flats located in housing estates and new towns. The new towns—such as Woodlands, Tampines, and Yishun—are scattered across the island and are characterized by easy access to places of employment and shopping districts. The traditional Malay kampong settlements—consisting of stilt houses built along the shoreline—are declining in number and are now found only in select rural areas. More … Score: https://www.britannica.com/place/Singapore  

2026/08/09

Discover the must-see attractions of Ivory Coast

Tourism in Ivory Coast, must-see attractions, ecotourism, historical tourism, seaside, cultural, Safari, sports tourism, sustainable tourism.

2026/08/09

Ecuador ?? sights from the Coast to the Amazon

Ecuador highlights to help you make the most of your time in Ecuador. Learn more about the highlights of Ecuador in this travel video.

2026/08/09

Welcome To Singapore

Welcome to Singapore.. A city state which unifies the frantic life of a Megapolis with the calm and modern. It's a home for businessmen as well as for people being part of the lower class. Enjoy our perception!

2026/08/08