Statehood Day of Montenegro

Montenegro, country located in the west-central Balkans at the southern end of the Dinaric Alps. It is bounded by the Adriatic Sea and Croatia (southwest), Bosnia and Herzegovina (northwest), Serbia (northeast), Kosovo (east), and Albania (southeast). Montenegro’s administrative capital is Podgorica, though its cultural centre is the historical capital and older city of Cetinje. For much of the 20th century Montenegro was a part of Yugoslavia, and from 2003 to 2006 it was a component of the federated union of Serbia and Montenegro.The country’s names—both Montenegro (from Venetian Italian) and Crna Gora—denote “Black Mountain,” in reference to Mount Lovćen (5,738 feet [1,749 metres]), its historical centre near the Adriatic Sea and its stronghold in the centuries of struggle with the Turks. Alone among the Balkan states, Montenegro was never subjugated. The old heartland of Montenegro, in the southwest, is mainly a karstic region of arid hills, with some cultivable areas—e.g., around Cetinje and in the Zeta valley. The eastern districts, which include part of the Dinaric Alps (Mount Durmitor), are more fertile and have large forests and grassy uplands. The drainage system of Montenegro flows in two opposite directions. The Piva, Tara, and Lim rivers follow northerly courses, the Morača and Zeta rivers southerly ones.Relief The terrain of Montenegro ranges from high mountains along its borders with Kosovo and Albania, through a segment of the Karst region of the western Balkan Peninsula, to a narrow coastal plain that is only 1 to 4 miles (2 to 6 km) wide. The coastal plain disappears completely in the north, where Mount Lovćen and other peaks rise abruptly from the inlet of the Gulf of Kotor. The coastal region is noted for seismic activity. Montenegro’s section of the Karst lies generally at an elevation of 3,000 feet (900 metres) above sea level—although some areas rise to 6,000 feet (1,800 metres). The lowest segment is in the valley of the Zeta River, which is at about 1,500 feet (450 metres). The river occupies the centre of Nikšić Polje, a flat-floored, elongated depression typical of karstic regions, as is the predominantly limestone underlying rock, which dissolves to form sinkholes and underground caves.The high mountains of Montenegro include some of the most rugged terrain in Europe and average more than 7,000 feet (2,000 metres) in elevation. Notable is Bobotov Peak in the Durmitor Mountains, which reaches 8,274 feet (2,522 metres) and is the country’s highest point. The Montenegrin mountains were the most ice-eroded section of the Balkan Peninsula during the last glacial period.Drainage Montenegro’s surface runoff in the north is carried away by the Lim and Tara river systems, which enter the Danube via the Drina River, which forms the border between Bosnia and Herzegovina and Serbia. In southern Montenegro, streams flow toward the Adriatic. Much of the drainage of the karstic region is not on the surface but travels in underground channels. Lake Scutari (known in Montenegro as Skadarsko Jezero), the country’s largest lake, lies near the coast and extends across the international border into northern Albania. It is 25 miles (40 km) long and 10 miles (16 km) wide, with a total surface area of 140 square miles (360 square km), and some three-fifths of it lies within Montenegrin territory. The lake occupies a karstic polje depression, the floor of which lies below sea level. Montenegro’s mountainous regions are noted for their numerous smaller lakes. Soils A distinctive feature of Montenegro is the accumulations of terra rossa in its coastal area. This red soil, a product of the weathering of dolomite and limestone rocks, is also found in depressions in the Karst. Mountainous areas above the plateaus have typical gray-brown forest soils and podzols. Climate Montenegro’s lower areas have a Mediterranean climate, with dry summers and mild, rainy winters. Temperature varies greatly with elevation. Podgorica, lying near sea level, is noted for having the warmest July temperatures in the country, averaging 81 °F (27 °C). Cetinje, in the Karst region at an elevation of 2,200 feet (670 metres), has an average temperature that is 10 °F (5 °C) lower. Average January temperatures range from 46 °F (8 °C) at Bar on the southern coast to 27 °F (−3 °C) in the northern mountains. Montenegro’s mountainous regions receive some of the highest amounts of rainfall in Europe. Annual precipitation at Crkvice, in the Karst above the Gulf of Kotor, is nearly 200 inches (5,100 mm). Like most areas along the Mediterranean Sea, precipitation occurs principally during the cold part of the year, but in the higher mountains a secondary summer maximum is present. Snow cover is rare along the Montenegrin coast, averaging 10 days in karstic polje depressions and increasing to 120 days in the higher mountains. Plant and animal life One-third of Montenegro, principally in the high mountains, remains covered with broad-leaved forest. However, bare rock characterizes most of the southern Karst zone, where soils generally are absent. This area remained forested through Classical times, with oaks and cypresses predominating, but removal of forests for domestic fuel and construction led to widespread soil erosion and, ultimately, to replacement of the woodlands by the Mediterranean scrub assemblage known as maquis. Sparsely populated Montenegro is noted as a habitat for numerous mammals, including bears, deer, martens, and wild pigs (Sus scrofa). It has many predatory wild animals, including wolves, foxes, and wildcats. The country also has a rich variety of birds, reptiles, and fish. People of Montenegro - Ethnic groups Differences between Montenegrins and Serbs are a matter of continuing controversy. Although isolated from each other for centuries during the Ottoman period, when Albanian families came to dominate the intervening Kosovo region, both groups retained their Orthodox religious traditions and many other common cultural attributes—including the Cyrillic alphabet. Because of such obvious commonalities, most Serbs see Montenegrins as “Mountain Serbs,” and many—but certainly not all—Montenegrins see themselves as Serb in origin. Fluctuations between a Serb and a Montenegrin identity have been reflected in census figures. In 1981, for example, more than two-thirds of the residents of Montenegro identified themselves as Montenegrin, while only a tiny percentage reported themselves as Serb. By the early 1990s those proportions had changed to about three-fifths and one-tenth, respectively. In the early 21st century almost half of the population was identified as Montenegrin and about one-fourth as Serb. The largest non-Serb minorities are Bosniaks (Muslims) and Albanians, the former concentrated in the northern mountains and the latter along the Adriatic coast. Nearly three-fourths of the population of the coastal community of Ulcinj is Albanian.Languages and religion During the long period of separation from Serbia, Montenegrins developed characteristics and institutions of their own. For example, they did not adhere to the Serbian Orthodox Church but were led by their own metropolitan until the Montenegrin church was absorbed into the Serbian patriarchate in 1920. In addition, Montenegrin pronunciation is closer to Croatian than to Serbian. A strong nationalist movement grew alongside Montenegrin resentment of Serbian attempts to minimize their distinctiveness. Many (but by no means all) Montenegrins joined Bosnians, Croats, and Serbs in insisting that what is spoken in each of their respective countries is a language distinct from neighbouring languages, despite mutual intelligibility. Thus, they prefer that their language be called Montenegrin. Montenegrin, Serbian, Bosnian, Albanian, and Croatian are all recognized by the constitution as official languages. More … Score: https://www.britannica.com/place/Montenegro

2023/07/13

Invest in Mongolia

Mongolia gives investors preferential market access through 2 trade agreements to 8 countries with nearly 3 billion consumers

2023/07/13

Independence Day of the Democratic Republic of the St. Sao Tome and Principe

Sao Tome and Principe, island country of Central Africa, located on the Equator in the Gulf of Guinea. It consists of two main islands—São Tomé and Príncipe—and several rocky islets, including Rôlas, south of São Tomé island, and Caroço, Pedras, and Tinhosas, south of Príncipe. Land São Tomé, which is oval in shape, is larger than Príncipe, which lies about 90 miles (145 km) northeast of its sister island. The capital of the country, São Tomé city, is situated in the northeastern part of São Tomé island. The country’s closest neighbours are Gabon and Equatorial Guinea on the Atlantic coast of central Africa. Relief and drainage In the south and west of both islands, high volcanic mountains fall precipitously to the sea, although neither island has witnessed any volcanic activity in recent centuries. The mountains descend gradually to small plains in the northeast. São Tomé Peak, the highest point on the main island, rises to 6,640 feet (2,024 metres) above sea level, and Príncipe Peak on the smaller island reaches 3,110 feet (948 metres). These mountainous areas are deeply dissected by stream erosion, and spectacular isolated volcanic plugs stand out as landmarks. Swift and rocky streams rush down to the coast in every direction. Climate The climate is basically maritime and tropical, but, because of the rough topography, there is a wide range of microclimates. The prevailing moist southwesterly winds are intercepted by the mountains, so annual rainfall exceeds 275 inches (7,000 mm) in the southwestern part of São Tomé island, while the far northeast receives less than 30 inches (760 mm). The dry season, called gravana, lasts from June to September in the northeast but is scarcely discernible in the wetter regions. In the coastal areas the mean annual temperature is high, in the low 80s F (upper 20s C); the average relative humidity is also high, about 80 percent. Average temperatures decline sharply with elevation, and night temperatures fall below 50 °F (10 °C) at about 2,300 feet (700 metres). Above 3,300 feet (1,000 metres) fine misty rain falls almost continuously and the nights are cold, although frost and snow are unknown. Plant and animal life The original vegetation of the islands was luxuriant tropical rainforest, with a gradual transition from lowland forest to mist forest. Some of the islands’ area, mainly in the south and west, is still covered with rainforest. Much of this is secondary growth on abandoned plantation land. The flora and fauna include many rare and endemic species, reflecting the isolation and environmental diversity of the islands. Birds such as the ibis, shrike, and grosbeak can be found in Sao Tome and Principe. Many of the plants, birds, reptiles, and small mammals are threatened by pressure on the remaining rainforest. People - Ethnic groups The population consists mainly of Forros (from forro, Portuguese for “free man”), descendants of immigrant Europeans and enslaved Africans. Another group, the Angolares, descended from formerly enslaved Angolans who were shipwrecked on São Tomé about 1540. The Angolares remained apart in the isolated southern zone of São Tomé island until the late 19th century, but they later spread throughout the country and became largely assimilated. Cabo Verdeans form the largest group of resident foreigners; many have adopted Sao Tomean nationality. Angolans and Mozambicans make up most of the rest of the African immigrant community. Like the Cabo Verdeans, they are relatively well integrated with the other islanders, because of a shared Luso-African cultural background. There is a small European population—primarily Portuguese—in the country. Languages Standard Portuguese is the official language and is understood by virtually all islanders. In addition, three Portuguese-based creoles are spoken: Sãotomense, spoken by the Forros and having by far the largest number of speakers; Angolar, the language of the Angolares, spoken on the southern tip of São Tomé; and Principense, spoken by only a few hundred individuals on Príncipe. Religion More than half of the population belongs to the Roman Catholic Church. The remainder of those professing a religious affiliation is primarily Protestant. Traditional African religious practices and beliefs are widespread, even among adherents of other faiths. About one-fifth of the population identifies as nonreligious. Settlement patterns Almost three-fourths of the population resides in urban areas. The population is concentrated in the drier and flatter areas of both islands. Whereas a third of the inhabitants live in São Tomé city and its outskirts, only about 5 percent live on the island of Príncipe. Many people live in dispersed settlements known locally as lucháns. Houses made of wooden planks and raised above the ground are typical of the local building methods, although there are also many concrete structures in the Portuguese colonial style. Many people still live in barracklike accommodations on the plantations. Demographic trends Population growth is above the world average but below the average for sub-Saharan Africa. About two-fifths of the population is younger than 15 years of age, and another one-fourth is younger than 30, assuring continued rapid growth. Life expectancy in the early 21st century was more than 65 years of age, relatively high for an African country and close to the world average. Economy of Sao Tome and Principe Decades of colonial stagnation were followed by economic disruption after independence in 1975. Under the tutelage of the International Monetary Fund (IMF) and the World Bank since the mid-1980s, Sao Tome and Principe has tried to restore a functioning economy by devaluing its currency, reducing the budget deficit, privatizing formerly nationalized companies, attracting foreign investment, and removing price subsidies and controls. Despite all efforts and considerable inflows of foreign funds, however, the results of the imposed reforms did not match the original targets. During that time corruption became rampant, and mass poverty increased tremendously. In the late 1990s, IMF measures helped the country’s economy improve considerably, as did the advent of petroleum concessions sales, which continued into the 21st century. Sao Tome and Principe’s economy has historically been dependent on agriculture, and much of the total agricultural area of the two islands belongs to the state. Until 1993 this land was divided into 15 large plantation enterprises, but, by the end of the decade, most of the former plantations were dissolved and their land distributed to smallholders and medium-sized enterprises on a usufruct basis as part of attempted agricultural reform. High levels of unemployment coexist with a critical labour shortage on the former plantations, where wages and working conditions are poor. Agriculture, forestry, and fishing São Tomé is endowed with excellent conditions for tropical agriculture. The growing season is long, the volcanic soils are fertile, and there is no lack of water. Consequently, the economy remains dependent on plantation agriculture, especially cacao (grown for its seeds, cocoa beans). About two-fifths of the total land area is under cultivation, with cacao trees covering a little less than two-thirds of the cultivated land; coconut palms cover most of the remainder. Large areas of plantation land have been poorly maintained since independence; they are harvested from time to time but not otherwise tended. The country has never been self-sufficient in staple foodstuffs, and a combination of local eating habits, the legacy of the plantation economy, and foreign food aid has undermined the production of food crops for the local market. Fine stands of timber remain in the mountains, but the difficulty of removing logs from the steep terrain and the pressing need for effective conservation limit long-term prospects. The country’s small size prevents farmers from keeping large herds of livestock, but conditions for poultry raising are quite favourable. Fishing resources are limited by the narrow continental shelf. The domestic demand for fish exceeds supply by the local artisan fishermen, and trawlers from European Union countries pay small license fees for the right to fish in the country’s national waters. The deep-sea tuna resources of the Gulf of Guinea and shellfish in coastal waters represent the best hopes for fishery exports. Resources and power There are numerous sites for small hydroelectric schemes but no large rivers for major installations. The islands have no known mineral resources, but the country claims an area of the Gulf of Guinea that may have considerable deepwater hydrocarbon reserves; in the late 1990s and early 2000s this potential attracted foreign investors who purchased exploration concessions. In 2001 Sao Tome and Principe and Nigeria reached an agreement to oversee the exploration and development of potential oil fields in the Joint Development Zone (JDZ), an area of overlapping maritime boundaries about 125 miles (200 km) from the Nigerian coast. The agreement was renegotiated in 2003, after which oil companies began bidding for the right to develop sections within the JDZ. The first exploratory drilling in the JDZ began in 2006. Manufacturing Manufacturing, which accounts for a tiny fraction of the gross domestic product, is hampered by the small size of the domestic market, limited energy resources, and the lack of skilled labour. It consists mainly of small processing factories producing foodstuffs, beverages, soap products, bricks, and sawn wood for the domestic market. Finance and trade Sao Tome and Principe is reputed to be the recipient of one of the highest amounts of foreign aid per capita in the world, but this has not prevented large budgetary and balance-of-payment deficits. There are several commercial banks active in the country, and the Central Bank of Sao Tome and Principe controls foreign exchange dealings and issues the country’s currency, the dobra. Cocoa, despite decreasing production, still accounts for almost all foreign exchange earnings from merchandise exports. Belgium, the Netherlands, and France are the country’s most significant export destinations. Portugal is the main source of imports. Source: https://www.britannica.com/place/Sao-Tome-and-Principe  

2023/07/12

All the beauties of Montenegro

2023/07/12

Island Vacations - The Official Website of The Bahamas

Experience unmatched island vacations across 100000 square miles of the world's clearest water. The Islands of The Bahamas.

2023/07/12

Naadam National Day of Mongolia

Mongolia, historically Outer Mongolia, country located in north-central Asia. It is roughly oval in shape, measuring 1,486 miles (2,392 km) from west to east and, at its maximum, 782 miles (1,259 km) from north to south. Mongolia’s land area is roughly equivalent to that of the countries of western and central Europe, and it lies in a similar latitude range. The national capital, Ulaanbaatar (Mongolian: Ulan Bator) is in the north-central part of the country. Landlocked Mongolia is located between Russia to the north and China to the south, deep within the interior of eastern Asia far from any ocean. The country has a marked continental climate, with long cold winters and short cool-to-hot summers. Its remarkable variety of scenery consists largely of upland steppes, semideserts, and deserts, although in the west and north forested high mountain ranges alternate with lake-dotted basins. Mongolia is largely a plateau, with an average elevation of about 5,180 feet (1,580 metres) above sea level. The highest peaks are in the Mongolian Altai Mountains (Mongol Altain Nuruu) in the southwest, a branch of the Altai Mountains system.Some three-fourths of Mongolia’s area consists of pasturelands, which support the immense herds of grazing livestock for which the country is known. The remaining area is about equally divided between forests and barren deserts, with only a tiny fraction of the land under crops. With a total population of fewer than three million, Mongolia has one of the lowest average population densities of any country in the world.The Mongols have a long prehistory and a most remarkable history. The Huns, a people who lived in Central Asia from the 3rd to the 1st century bce, may have been their ancestors. A united Mongolian state of nomadic tribes was formed in the early 13th century ce by Genghis Khan, and his successors controlled a vast empire that included much of China, Russia, Central Asia, and the Middle East. The Mongol empire eventually collapsed and split up, and from 1691 northern Mongolia was colonized by Qing (Manchu) China. With the collapse of Qing rule in Mongolia in 1911/12, the Bogd Gegeen (or Javzandamba), Mongolia’s religious leader, was proclaimed Bogd Khan, or head of state. He declared Mongolia’s independence, but only autonomy under China’s suzerainty was achieved. From 1919, nationalist revolutionaries, with Soviet assistance, drove out Chinese troops attempting to reoccupy Mongolia, and in 1921 they expelled the invading White Russian cavalry. July 11, 1921, then became celebrated as the anniversary of the revolution. The Mongolian People’s Republic was proclaimed in November 1924, and the Mongolian capital, centred on the main monastery of the Bogd Gegeen, was renamed Ulaanbaatar (“Red Hero”). From 1921 until the end of the 1980s, Mongolia was a one-party state closely tied to the Soviet Union. It received technical, economic, and military assistance from the Soviet Union and generally followed Soviet guidance in political and economic matters and in the building of a socialist society. However, beginning in 1990, forces for change in Mongolia ended the monopoly of political power by the communists in favour of free multiparty elections, coalition government, a new constitution, greater cultural and religious freedom with more emphasis on Mongol national traditions, a neutral position in international relations, and a transition to a market economy. Land - Relief Mongolia can be divided into three major topographic zones: the mountain chains that dominate the northern and western areas, the basin areas situated between and around them, and the enormous upland plateau belt that lies across the southern and eastern sectors. The entire country is prone to seismic movements, and some earthquakes are extremely severe. Their effects, however, are limited by the low population density. The mountains There are three major mountain chains in Mongolia: the Mongolian Altai Mountains, the Khangai Mountains (Khangain [or Hangayn] Nuruu), and the Khentii Mountains (Khentiin [or Hentiyn] Nuruu). The Mongolian Altai in the west and southwest constitute the highest and the longest of these chains. Branching southeastward from the main Altai range at the northwestern border with Russia, the Mongolian Altai stretch southeastward for some 250 miles (400 km) along the Chinese border before turning slightly more eastward for another 450 miles (725 km) in southwestern Mongolia. The range—the only one in the country where contemporary glaciation has developed—reaches an elevation of 14,350 feet (4,374 metres) at Khüiten Peak (Nayramadlyn Orgil) at the western tip of the country, Mongolia’s highest point. Extending eastward from the Mongolian Altai are the Gobi Altai Mountains (Govi Altain Nuruu), a lesser range of denuded hills that lose themselves in the expanses of the Gobi. The Khangai Mountains, also lying from northwest to southeast, form a solid mountain mass near the centre of the country. The range’s peaks reach some 12,000 feet (3,700 metres), with Otgontenger, the highest, rising to some 13,200 feet (4,025 metres) in the northwest. Characteristic of the Khangai are gentle slopes covered with fine pastureland. To the north the Eastern Sayan Mountains of Siberia lie along the border with Russia. The alignment of the third mountain chain, the Khentii range of northeastern Mongolia, is southwest to northeast, extending into Siberia. The highest peak is Asraltkhairkhan, which reaches about 9,200 feet (2,800 metres), but, in general, maximum elevations are about 7,000 feet (2,130 metres). Ulaanbaatar lies at the southwestern edge of the range. The Da Hinggan (Greater Khingan) Range rises along and beyond the eastern frontier with China. The northern intermontane basins Around and between the main ranges lie an important series of basins. The Great Lakes region, with more than 300 lakes, is tucked between the Mongolian Altai, the Khangai, and the mountains along the border with Siberia. Another basin lies between the eastern slopes of the Khangai Mountains and the western foothills of the Khentii range. The southern part of it—the basins of the Tuul and Orkhon (Orhon) rivers—is a fertile region important in Mongolian history as the cradle of settled ways of life. The remarkable Khorgo region, on the northern flanks of the Khangai Mountains, has a dozen extinct volcanoes and numerous volcanic lakes. Swift and turbulent rivers have cut jagged gorges. The source stream of the Orkhon River is in another volcanic region, with deep volcanic vents and hot springs. Near the northern border, Lake Khövsgöl (Hövsgöl) is the focus of another rugged region that is noted for its marshlands.More … Score: https://www.britannica.com/place/Mongolia

2023/07/11

Mongolia tourism promotional video

This promotional video about Tourism in Mongolia will give you a brief idea about tourism in Mongolia. You can visit /www.mongoliatrip.com/ to choose a tour of your interest.

2023/07/10

Independence Day of the Commonwealth of the Bahamas

The Bahamas, archipelago and country on the northwestern edge of the West Indies. Formerly a British colony, The Bahamas became an independent country within the Commonwealth in 1973. The name Bahamas is of Lucayan Taino (Arawakan) derivation, although some historians believe it is from the Spanish bajamar, meaning “shallow water.” The islands occupy a position commanding the gateway to the Gulf of Mexico, the Caribbean Sea, and the entire Central American region. Their strategic location has given the history of The Bahamas a unique and often striking character. It was there that Christopher Columbus made his original landfall in the Americas. The subsequent fate of the peaceful original inhabitants remains one of the more tragic episodes in the development of the entire region, while the early attempts at European-dominated settlement were marked by intense national rivalries, interspersed with long periods of lawlessness and piracy. As a result, the society and culture that has evolved in The Bahamas is a distinctive blend of European and African heritages, the latter a legacy of the slave trade and the introduction of the plantation system using African slaves. The islands, lacking natural resources other than their agreeable climate and picturesque beaches, have become heavily dependent on the income generated by the extensive tourist facilities and the financial sector that have been developed, often as a result of the injection of foreign capital. The continued popularity of the islands with tourists, largely from North America, has helped to maintain a relatively high standard of living among the population, most of whom are of African descent. The capital, Nassau, is located on small but important New Providence Island. Land Lying to the north of Cuba and Hispaniola, the archipelago comprises nearly 700 islands and cays, only about 30 of which are inhabited, and more than 2,000 low, barren rock formations. It stretches more than 500 miles (800 km) southeast-northwest between Grand Bahama Island, which has an area of 530 square miles (1,373 square km) and lies about 60 miles (100 km) off the southeastern coast of the U.S. state of Florida, and Great Inagua Island, some 50 miles (80 km) from the eastern tip of Cuba. The islands other than New Providence are known collectively as the Out (Family) Islands. They include Grand Bahama, which contains the major settlements of Freeport and West End; Andros (2,300 square miles [6,000 square km]), the largest island of The Bahamas; Abaco, or Great Abaco, (372 square miles [963 square km]); and Eleuthera (187 square miles [484 square km]), the site of one of the early attempts at colonization. Relief and soils The Bahamas occupies an irregular submarine tableland that rises out of the depths of the Atlantic Ocean and is separated from nearby lands to the south and west by deepwater channels. Extensive areas of flatland, generally a few feet in elevation, are the dominant topographic features of the major islands; the Bimini group (9 square miles [23 square km]), for example, has a maximum elevation of only 20 feet (6 metres). A number of islands fronting the Atlantic have a range or series of ranges of hills on the northeastern side that parallel the longer axes of the islands. These ranges are formed of sand washed ashore and blown inland by the trade winds. The newer hills adjacent to the seashore are normally sand dunes. Solidity increases toward the interior, where the particles become cemented to form Bahama limestone. Eleuthera and Long Island (230 square miles [596 square km]) have the greatest number of hills exceeding 100 feet (30 metres). The highest point in The Bahamas, Mount Alvernia, at 206 feet (63 metres), is on Cat Island (150 square miles [388 square km]). Beneath the soil, the islands are composed of limestone rock and skeletal remains of coral fossils and other marine organisms. There are no rivers, but several islands—particularly New Providence, San Salvador (63 square miles [163 square km]), and Great Inagua—have large lakes. There is abundant fresh water on Andros Island. Climate of the The Bahamas The Bahamian climate, mild throughout the year, is one of the great attractions of the area. The average temperature varies from the low 70s F (about 21 °C) during the winter to the low 80s F (about 27 °C) during the summer, and extremes seldom fall below the low 60s F (about 16 °C) or rise above the low 90s F (about 32 °C). The average annual rainfall is about 44 inches (1,120 mm), occurring mostly during the summer months. Prevailing winds, coming from the northeast in winter and from the southeast in summer, lend a cooling influence to a generally humid atmosphere. Tropical cyclones (hurricanes) pose a threat during the period from June to November and have occasionally caused great destruction. Plant and animal life Extensive and beautiful forests of Caribbean pine are found on Grand Bahama, Abaco, Andros, and New Providence islands. Hardwood forests also occur on some of the islands. Elsewhere the woody vegetation consists mostly of shrubs and low trees. Animal life is dominated by frogs, lizards, and snakes, all of them nonpoisonous, and several species of bats are found in caves along the more rocky coasts. Larger animals include the agouti, a rodent; the raccoon; the iguana; and the elegant flamingo, the national bird. All of these have been much reduced in numbers and in distribution. In addition, several animals—notably sheep, horses, and other livestock—have been introduced from Europe. The surrounding waters abound with fish and other edible marine animals, such as conch and spiny lobster (crayfish). More … Score: https://www.britannica.com/place/The-Bahamas  

2023/07/10

4K AERIAL FILM OF NASSAU, BAHAMAS

4K aerial film and cinematic visual journey of the beautiful Nassau, Bahamas. White sand beaches, blue gatorade colored water, watersports, luxury, the Bahamas have it all- making it the ultimate destination.

2023/07/09