Welcome to Panama | Places to Visit & Things to Do

Start planning your Panama vacation and discover rainforests, national parks, pristine beaches, and expansive city views.

2025/11/05

Constitution Day of the Kingdom of Tonga

Tonga, officially Kingdom of Tonga, Tongan Fakatuʿi ʿo Tonga, also called Friendly Islands, country in the southwestern Pacific Ocean. It consists of some 170 islands divided into three main island groups: Tongatapu in the south, Haʿapai in the centre, and Vavaʿu in the north. Isolated islands include Niuafoʿou, Niuatoputapu, and Tafahi (together known as the Niuatoputapu, or Niuas, island group) in the far north and ʿAta in the far south. Tonga’s total land area is dispersed between latitudes 15° and 23° S and longitudes 173° and 177° W. The capital, Nukuʿalofa, is on the island of Tongatapu. Tonga is a member of the Commonwealth and of the United Nations. Land - Relief The summit of volcanic undersea mountains forms the two roughly parallel chains of the Tongan islands. Most of the islands of the western chain are classified as high islands, because they have been raised well above sea level by repeated volcanic activity. Four of them are still active volcanoes. Some of the islands composed of lava formed by shield volcanoes, such as Late and Kao, have a hard cone-shaped surface that is not easily eroded. Others, such as Fonuafoʿou (Falcon Island), were formed by more explosive volcanoes, and their surfaces, composed of ash and pumice, erode readily. Fonuafoʿou has arisen and disappeared repeatedly, owing to its cycles of eruption and erosion. The low islands of the eastern chain have been capped by coral polyps and foraminifera (marine organisms that have calcareous shells), which build coral rock and limestone reefs. The continuing growth of coral counteracts the sea’s erosion of the reefs and the islands enclosed by them. A protective reef surrounds Tongatapu Island; many islands in the Vavaʿu Group lack such protection and are shrinking. Tongatapu Island, a raised atoll in the Tongatapu Group, with an area of 100.6 square miles (260.5 square km), is the largest and most densely populated island in Tonga. The highest point in Tonga, 3,389 feet (1,033 metres), is on Kao Island in the Haʿapai Group. ʿEua Island (Tongatapu Group) has an old volcanic ridge rising to 1,078 feet (329 metres) above sea level. The Vavaʿu Group has hills ranging from 500 to 1,000 feet (150 to 300 metres), and Late Island, in its western volcanic chain, rises to 1,700 feet (518 metres). Vavaʿu Island has a fine, large landlocked harbour. The effects of natural erosion are particularly vivid in Vavaʿu. Rainwater reacting with the carbon dioxide in vegetation acquires acidic properties and dissolves coral and limestone rock, thereby forming caves. The constant action of the waves has created the sheer cliffs and sandspits of Vavaʿu and Nukuʿalofa. There are no rivers in Tonga, although ʿEua and Niuatoputapu have creeks. Climate Tonga has a semitropical climate except in the northernmost islands, where truly tropical conditions prevail. Temperatures range between 60 and 70 °F (16 and 21 °C) in June and July and reach 80 °F (27 °C) in December and January. The mean annual humidity is 77 percent. The mean annual precipitation varies from 64 inches (1,620 mm) in the Haʿapai Group to 97 inches (2,450 mm) on Niuafoʿou. Humidity increases as the distance from the Equator lessens. The northern islands, which are closest to the Equator, are particularly vulnerable to typhoons, which generally occur between December and April. Plant and animal life The well-drained, fertile soils of ʿEua, Kao, Tofua, and Late islands and the slopes and hilltops of Vavaʿu support original forests. ʿEua has the greatest number and variety of trees, and the ridge on the eastern side is a forest reserve. The fast-growing toi and the tavahi constitute a majority of the tree cover on ʿEua. The sandy, rocky, dry soils of the coasts and the direct exposure there to strong winds and salty spray create unfavourable conditions for coastal vegetation. To conserve moisture, plants near the shore have small waxy or hairy leaves. Tidal sand and mudflats have swampy areas that support mangroves. Behind the mudflats, trees with buttress roots, such as the lekileki, sometimes grow. Tonga’s land birds include doves, rails, starlings, kingfishers, and many others. The red-breasted musk parrot and the blue-crowned lory, considered by some to be the most beautiful birds in the Pacific, inhabit ʿEua. Island cliffs serve as homes for red-tailed and white-tailed tropic birds. Among the native birds of Niuafoʿou Island is the incubator bird. The common reef heron is a native shorebird. Transient species include golden plovers, wandering tattlers, long-billed curlews, and bar-tailed godwits. Tongan waters attract several varieties of seabirds such as noddies, terns, frigate birds, and mutton birds. The village of Kolovai on Tongatapu Island is home to a colony of flying foxes (Pteropus tonganus, a type of Old World fruit bat). The bats cling to large trees by day and fly at night to forage for food. People Nearly the entire population is of Polynesian ancestry. Tongans are closely related to Samoans and other Polynesians in culture and language as well as in genetic heritage. There is also a small amount of Melanesian influence through contact with Fiji. Intermarriage with Europeans has become more common, especially as a result of the increasing out-migration of Tongans since the 1970s. Religion is an important aspect of Tongan society, and most Tongan families are members of a Christian church. About one-third of Tongans belong to the Free Wesleyan (Methodist) Church; nearly one-fifth are Mormons; and there are smaller but significant proportions of Roman Catholics and members of the Free Church of Tonga. The remainder belong to smaller, mostly Protestant, denominations. The Tongan language is taught in primary schools and is the official language, in addition to English, which is studied as a second language. Most of the Tongan population lives in the three major island groups, and nearly three-fourths live on Tongatapu Island. The urban population has been steadily growing and now accounts for about one-third of the total population. Many Tongans migrate overseas, in particular to the United States and New Zealand. The majority of the population lives in villages. Traditional structures are called fale; they are rectangular in shape and have thatched or corrugated tin roofs and sides made of woven coconut leaves, reeds, or timber. Some Tongans reside in South Seas colonial-style wooden homes with gingerbread trim and exterior walls in pastel shades. Nukuʿalofa has all the amenities of a capital city. It is also a major port of entry and has several wharves and piers. Much of Nukuʿalofa’s economic activity revolves around coconuts and coconut products. Other ports and commercial centres are Neiafu in the Vavaʿu Group and Pangai in the Haʿapai Group. More … Score: https://www.britannica.com/place/Tonga

2025/11/04

Tonga - From Above - DJI Phantom 4

Tonga from a drone perspective.

2025/11/03

Independence Day Federated States of Micronesia

Micronesia, country in the western Pacific Ocean. It is composed of more than 600 islands and islets in the Caroline Islands archipelago and is divided roughly along cultural and linguistic lines into the states of—from west to east—Yap, Chuuk, Pohnpei, and Kosrae. The capital is Palikir, on the island of Pohnpei. To the west of the Federated States of Micronesia lies the Republic of Palau, also in the Caroline archipelago, and to the east is the Republic of the Marshall Islands. Those two countries, together with the Commonwealth of the Northern Mariana Islands and the Federated States of Micronesia, were administered by the United States as the Trust Territory of the Pacific Islands from 1947 to 1986. Land The islands are of two general types: high volcanic islands that support a large variety of plant forms and low-lying coral atolls with poorer soil. Yap Island is distinctive in that it was formed by folds in the Earth’s crust and is continental in geologic composition. Each of the four states has as its population centre an elevated landmass of fairly large extent—ranging from Pohnpei Island, with an area of 129 square miles (334.1 square km), to Yap Island (38.7 square miles [100.2 square km]). The volcanic islands of Chuuk are an anomaly in the Pacific because they are encircled by a reef but have not yet subsided beneath sea level to become a classic atoll. Yap Island and six islands in the Chuuk group rise to more than 500 feet (150 metres), and Kosrae and Pohnpei islands have peaks of 2,064 feet (629 metres) and 2,595 feet (791 metres), respectively. The coral atolls consist of groups of small islands, formed atop a coral reef enclosing a lagoon. The climate is tropical, with high humidity and a mean annual temperature in the low 80s F (about 27 °C). There is little seasonal variation in temperature. Rainfall averages about 120 inches (3,000 mm) per year throughout the area, although Pohnpei receives more than 200 inches (5,000 mm) yearly. There are distinct rainy and dry seasons, the latter occurring during the height of the northeasterly trade-wind season between December and April. Yap, which alone is situated in the monsoon area, has westerly winds for part of the year. Numerous typhoons (tropical cyclones) originate in the east each year, usually spinning off to the northwest toward Yap and the Mariana Islands and seldom striking any of the other islands. On the high islands, mangrove swamps grow along the shore, and grassland or scrub ascends to tropical rainforests in the interior mountain areas. Settlements are almost without exception located near the coast. Volcanic islands, with their richer soil, support many different species of plant life. On coral atolls the predominant forms of vegetation are the coconut palm along with pandanus and breadfruit trees. Atoll dwellers typically locate their houses on the lagoon side of the island. People The people of the Federated States, while generally classified as Micronesian, are very diverse culturally and linguistically. The people of Yap Island speak Yapese, a language only distantly related to the other languages of the area (which are known as Nuclear Micronesian languages). Inhabitants of the coral atolls in Yap state are similar in language and culture to the people of Chuuk, although the Chuukese and Yapese languages are not mutually intelligible. Both Chuuk and Pohnpei contain several dialects, and the inhabitants of Kapingamarangi and Nukuoro, two atolls in the southwestern portion of Pohnpei state, are Polynesians and speak languages unrelated to Pohnpeian. Only Kosrae has complete ethnic and linguistic unity. Altogether, eight local languages are recognized as distinct, and dialectal differences in the outlying atolls add further variety. About half the total population lives in Chuuk state. Pohnpei has about one-third of the population, and Yap and Kosrae have about one-tenth each. In the late 20th century there began a trend toward migration to the towns for employment and education; more than one-fifth of the population was considered urban by the 2010s. The population growth rate is one of the highest in the region. Nearly three-fifths of the population is under the age of 30. Almost the entire population is Christian; more than half the people are Roman Catholic, and another two-fifths are Protestant. The country has no official language, but English is spoken widely in government and commerce. Economy Subsistence farming and fishing are the principal economic activities. The main staples are breadfruit, taros, coconuts, and bananas, but yams, cassava, and sweet potatoes also are grown on some of the high islands. Poultry, pigs, and dogs are sometimes also raised for food. The main source of revenue is U.S. government grant aid, which continues under the Compact of Free Association signed in 1982. External grants account for almost two-thirds of revenue. The terms of the original compact, which expired in 2001, were renewed with slight amendment in 2003. Because of the nature of the aid arrangement, servicing the debt consumed only a small portion of government outlays in the late 1990s. The major source of income is the service sector, including government employment. The government also derives income from the sale of fishing rights. Tourism is slowly expanding; as with the economy in general, the growth of tourism is restrained by the islands’ remote location and an underdeveloped infrastructure. Local commercial fishing is developed only on a small scale, and large-scale agriculture has repeatedly proved a failure. The only mineral resources to speak of are unexploited offshore deposits of high-grade phosphate. Much of the Federated States’ food, including rice, fruits, vegetables, meat, and fish, and almost all manufactured goods and fuel oil must be imported. Indeed, over the course of the late 20th century, the islanders’ traditional diet was largely displaced by imported processed foods. Imports, whose sources include the United States, Guam, Singapore, Taiwan, and Thailand, also include machinery and transport equipment. Marine products are the primary export; other significant exports are garments, betel nuts, and copra. The major export destinations are Thailand, Taiwan, and Guam. Interisland and international transportation are by air or ocean freighter. The major commercial ports are at Dekehtik (Takatik Island), near Pohnpei; Kosrae; Colonia on Yap; and Weno (Moen). International airports are located on the main islands of each state, and there are airstrips on several outlying islands in Chuuk. Small ships operated by the government service the outlying atolls in each state. Some of the atolls are also linked by weekly flights on smaller airplanes. All villages on the major islands are connected by a road system, and the primary roads in the commercial centres are paved. Government and society Under the 1979 constitution, the government of the Federated States of Micronesia consists of executive, legislative, and judicial branches. The president and vice president are elected by the legislature, the unicameral National Congress. The legislature comprises one at-large senator from each state, who serves four-year terms, and a variable number of single-district senators (determined on the basis of population), who serve two-year terms. Most major governmental functions other than those relating to defense and foreign affairs are carried out at the state rather than the national level. Each of the four state governments has a popularly elected governor and a unicameral legislature. There are no political parties. The judicial system consists of the Supreme Court of the Federated States of Micronesia, state courts in each of the four states, and municipal courts in each political subdivision of each state. Recognized customary law is in force wherever it does not conflict with constitutional law. Under the Compact of Free Association, the United States provides for the defense of the islands; under other terms of the agreement, Micronesian citizens are free to live, work, or study in the United States without restriction. There are elementary schools on every island, and each state has at least one public high school. Primary education is compulsory between ages 6 and 14. The College of Micronesia-FSM was founded in 1963 for teacher training and later became a community college offering a range of coursework and vocational training. It has a national campus on Pohnpei and branch campuses in each of the other states and is the only institution for higher education in the Federated States of Micronesia. Several universities in the United States and the Pacific region offer extension programs for training in various disciplines. Widespread vaccination has helped to reduce the impact of many infectious diseases. Tuberculosis and leprosy occur at moderate rates in the islands, and outbreaks of cholera periodically sweep through the population centres, but in the late 20th century obesity and chronic noncommunicable diseases such as diabetes, hypertension, and heart disease emerged as the major health concerns for adults. While a hospital is maintained in each of the state capitals and dispensaries have been built on all major islands, the overall state of health care is relatively poor. Local healers continue to practice massage and other traditional medical skills. More … Score: https://www.britannica.com/place/Micronesia-republic-Pacific-Ocean  

2025/11/03

Independence Day of the Community of Dominica

Dominica, island country of the Lesser Antilles in the eastern Caribbean Sea. It lies between the French islands of Guadeloupe and Marie-Galante to the north and Martinique to the south. The country has been a member of the Commonwealth since independence in 1978. The island is 29 miles (47 km) long and has a maximum breadth of 16 miles (26 km). The capital and chief port is Roseau. Dominica’s great natural beauty, especially its spectacular mountainous topography, has impressed generations of nature lovers. Land - Relief, drainage, and soils The island is of volcanic formation. Dominica has a number of active volcanoes, although eruptions are rare. Other signs of geothermal activity include fumaroles (volcanic vents) and hot springs. In the south, Boiling Lake lies 2,300 feet (700 metres) above sea level; its waters are often forced 3 feet (1 metre) above normal by the pressure of escaping gases. The island has rich alluvial and volcanic soils. There are numerous rivers, all of them unnavigable. A range of high forest-clad mountains runs north to south, broken in the centre by a plain drained by the Layou River, which flows to the west; the highest points are Mount Diablotins (4,747 feet [1,447 metres]) and Mount Trois Pitons (4,670 feet [1,424 metres]). Climate Dominica has a pleasant climate, particularly during the cooler months from December to March. Summer temperatures reach an average high of 90 °F (32 °C). Winter temperatures are not much lower, the average high being anywhere from 84 to 86 °F (29 to 30 °C). The dry season is from February to May, and the rainy season is from June to October, the most likely period for hurricanes (tropical cyclones). Rainfall varies, being especially heavy in the mountainous interior. Average annual coastal rainfall varies from about 60 inches (1,500 mm) to 145 inches (3,700 mm), but in the mountains average rainfall can reach 250 inches (6,350 mm). Plant and animal life Dominica is the most heavily forested island of the Lesser Antilles. The forest is the habitat of a considerable variety of birds and animals. Two parrots—the imperial parrot, or sisserou (Amazona imperialis), and the smaller red-necked parrot (Amazona arausiaca)—are found only in Dominica. There are many hummingbirds, of which the blue-headed (Cyanophaia bicolor) is native only to Dominica and the neighbouring island of Martinique. The large frog known as crapaud or mountain chicken (Leptodactylus fallax), one of four amphibian species on the island, was long an emblematic part of Dominica’s fauna (and a national dish), but it has become highly endangered because of a fungal disease. People The population is mainly of African descent, with some Europeans, people from the Indian subcontinent, and Caribs. Dominica is the only island with a relatively large and distinctive group of Carib Indians, descendants of the people who inhabited the island before European colonization. Most of the remaining Caribs, a small number of whom are solely of Carib descent, live in the approximately 3,700-acre (1,500-hectare) Carib Territory in the east of the island and are among Dominica’s poorest residents. English is the official language, but a French patois is commonly spoken, and the original Carib language is evidenced in a number of place-names. The majority of the population is Roman Catholic, but there are also Methodists, Pentecostals, and Seventh-day Adventists. Dominica experienced out-migration throughout the 1970s, a trend that culminated with a massive exodus after Hurricane David in 1979. This wave continued in the 1980s but moderated in the 1990s. In 1992 the government initiated a controversial scheme to offer “economic citizenship” to investors from other countries. Economy Dominica is one of the poorest of the Caribbean countries. Its economy is dependent upon agriculture, which is intermittently destroyed by hurricanes. Attempts to diversify have had some success, with a growing tourism industry and a small offshore financial sector. Agriculture, forestry, and fishing Agriculture remains the most important sector of the economy, in terms of both employment and contribution to the gross national product. The main crops are bananas, citrus fruits, and coconuts. Bananas accounted for nearly half of Dominica’s export earnings in the 1980s, but in the late 20th and early 21st centuries the banana crops were devastated repeatedly by hurricanes. Production also fell in the 1990s in part as a result of a World Trade Organization ruling that the European Union had breached free-trade rules by offering Dominica and other former European colonies—notably, other eastern Caribbean banana-producing islands—preferential access to the European market. Cocoa, coffee, and vegetables are also produced. Dominica is self-sufficient in fruit and vegetables and exports foodstuffs to Guadeloupe. The forests have potential for marketable timber. The fishing industry was devastated by Hurricane David in 1979, when nearly all of the island’s fishing boats were destroyed, but, beginning in the 1990s, a new fishing port and market were built at Roseau (and subsequently repaired and renovated) with Japanese financial support. Resources Pumice, a volcanic rock used chiefly for building purposes, is the most important commercial mineral. There are also deposits of clay and limestone. Extensive copper deposits in the northeast have been investigated for possible exploitation. Manufacturing, trade, and services Most of the main products and exports are derived from the agricultural sector; they include copra, coconut oil, soap, bay oil, and fruit juices. Soap, derived from coconut oil, is an important export. There is a small garment-assembly sector. Wood products, including furniture, are produced from local timber. Portsmouth is the main boatbuilding centre. Imports include food, mineral fuels, and manufactured goods. Tourism developed dramatically in the late 20th century despite the island’s poor transportation infrastructure and the relative lack of hotel facilities and good beaches. Approximately 80,000 “stay-over” tourists visit the island each year, while the ports of Prince Rupert Bay and Roseau serve more than 300,000 cruise-ship passengers on day visits annually. The island has sought to develop reserves of its unique flora and fauna to attract tourists and markets itself as the “nature island” of the Caribbean. High rainfall and rugged terrain have impeded road building in Dominica. The first road across the island was not completed until 1956, and it was not until 1984 that a major road-rehabilitation project was launched to greatly improve accessibility. The main airport is Melville Hall, located at Marigot, on the northeast coast. A second airport is at Canefield, near Roseau. Larger vessels use the deepwater port at Woodbridge Bay near Roseau, but Portsmouth remains the major banana-shipping port. Government and society Constitutional framework The constitution adopted at independence provides for a president as head of state and a prime minister as head of government. The legislative branch of government, called Parliament, consists of the president (ex officio) and a single-chamber House of Assembly. Of the 32 total house members, 21 are elected from constituent districts; 9, called senators, are presidential appointees; and 1, the speaker, is elected either from among members who do not belong to the cabinet or from outside the House of Assembly. The attorney general is also considered a member of the house. The president is elected by the legislature, and the prime minister is appointed by the president from among the elected members of the House of Assembly. The prime minister heads a cabinet chosen by the president from among members of the house, although no more than three cabinet members may be senators. Terms of office are for five years, and there is universal adult suffrage. Dominica is a member of the Commonwealth, the United Nations, the Organization of American States, the Caribbean Community, and the Organisation of Eastern Caribbean States (OECS). Dominica uses the Eastern Caribbean dollar (EC$), the common currency of the OECS. Health and welfare There are several major hospitals. Local medical needs are handled by health centres throughout the island. Intestinal diseases, diabetes, anemia, tuberculosis, and sexually transmitted diseases constitute the major health problems of Dominica. Education Primary education is compulsory and free in government-run schools. There are many secondary schools, a teacher-training college, a medical school, a nursing school, and a branch of the University of the West Indies. Literacy is estimated at nearly 90 percent. More … Score: https://www.britannica.com/place/Dominica

2025/11/03

Visit Antigua & Barbuda – The beach is just the beginning

Antigua and Barbuda Tourism Authority (ABTA), the Official source for destination information for a perfect travel experience! Official hashtag ..

2025/11/03

Independence Day of the Republic of Panama

Panama, country of Central America located on the Isthmus of Panama, the narrow bridge of land that connects North and South America. Embracing the isthmus and more than 1,600 islands off its Atlantic and Pacific coasts, the tropical nation is renowned as the site of the Panama Canal, which cuts through its midsection. It is equally well known for its natural beauty, for its diverse plant and animal life, including hundreds of bird and tree species, and for its vibrant music and culture. The home of several Native American peoples, such as the Guaymí, Kuna, and Chocó, Panama became the first Spanish colony on the Pacific. Celebrated as “the door to the seas and key to the universe,” it served in the 1530s as the staging point for the Spanish conquest of the Inca empire, and until the 19th century it was a transshipment point for gold and silver destined for Spain. With the independence of Colombia, which once controlled Panama, from Spain, Panama came to serve as another staging point, this time for oceangoing migrants to the gold fields of California. Since 1914 the 51-mile- (82-km-) long Panama Canal, which connects the Atlantic and Pacific Oceans, has afforded a long-sought shortcut for shipping and assures the country’s standing as one of the most strategic transportation hubs of the world. The canal also secures Panama’s ongoing role in international affairs and world commerce. The United States relinquished jurisdiction of the Panama Canal on December 31, 1999, marking an unprecedented shift in Panamanian society. For the first time in nearly a century as an independent nation, Panama controlled the entirety of its national territory. Panama enjoys a lively mix of cultural influences, expressed in the country’s cuisine, artwork, music, and literature. Its capital, Panama City, is located on the Pacific coast just east of the canal. A cosmopolitan city where skyscrapers tower above whitewashed bungalows, it enjoys a handsome setting and a growing importance as a commercial and financial services centre for the region. However, its economic progress has been hampered periodically by environmental problems and political turmoil. Land - Relief Panama is bounded to the north by the Caribbean Sea (an extension of the Atlantic Ocean) and to the south by the Pacific Ocean. It has an elongated S shape, with its Caribbean coastline stretching some 800 miles (1,290 km) and the Pacific coast some 1,060 miles (1,700 km); however, a line drawn from the Costa Rican frontier in the west to the Colombian border in the east would extend only 480 miles (770 km). The shortest distance across the isthmus is about 30 miles (50 km), from the mouth of the Nergalá (Necategua) River, which flows into the Gulf of San Blas on the Caribbean shore, to the mouth of the Chepo River on the Pacific coast. Nearly as narrow is the portion of the isthmus traversed by the Panama Canal. A central spine of mountain ranges extends almost the entire length of Panama, dividing the country into Atlantic- and Pacific-facing slopes. The two principal ranges, the Tabasará Mountains (Cordillera Central) in the west and the Cordillera de San Blas in the east, are separated near the centre of the country by a saddle of lower land. This depression (the Panama Canal site) divides the country again—roughly into western and eastern halves. Of the four quadrants thus formed, the southwestern has the largest number of settlements; however, the environs of the canal account for most of Panama’s population and commerce. The country’s highest peak is an inactive volcano, Barú (Chiriquí), which reaches an elevation of 11,401 feet (3,475 metres). Paralleling the principal mountain chains, a lower mountain arc extends along Panama’s southern coast. It appears only in well-separated segments—for example, on Azuero Peninsula as the Canajagua Massif and in eastern Panama as the Sierra de Jungurudó, Sapo Mountains, and the Majé Mountains. The highlands and mountains are made up primarily of igneous (volcanic) rocks. The lowlands include the plains of Panamá and Chiriquí provinces, the plains and hills of Colón province, the Chepo and Chucunaque river basins in the east, and the narrow northeastern plains of the Caribbean region. Sedimentary rocks such as slates and shales underlie most of the lowland zones. The Pacific coastline is extended by the Azuero Peninsula and the Gulf of Panama and by numerous headlands and bays, whereas the largest embayment on the Caribbean side is Chiriquí Lagoon. The Pacific coastline is more indented and irregular, and its continental shelf is much wider than that on the Atlantic side. In addition, most of the republic’s more than 1,600 islands lie off its Pacific coast; they include the Perlas Archipelago (Pearl Islands) and the islands of Taboga, Cébaco, Parida, Jicarón, and Coiba, the largest. The principal archipelagoes off the Caribbean coast are those of Bocas del Toro and San Blas. Drainage and soils Of Panama’s many short rivers, those that flow to the Caribbean include the Sixaola, Changuinola, Indio, Cricamola, La Miel, and Chagres. Rivers flowing to the Pacific include the Chiriquí Viejo, Santa María, Chepo, Chucunaque, and Tuira. During the rainy season the Tuira is navigable for some 40 miles (60 km) and the Chepo for 20 miles (30 km). Water in the Panama Canal does not flow from coast to coast; rather, it is released from the rain-fed Gatún and Alajuela (Madden) lakes in the central highlands. In effect, the water flows to both coasts simultaneously via the canal’s system of locks and dams. For details on the engineering and operation of the waterway, see Panama Canal. Soils are commonly reddish to brown and rich in clay. They vary in fertility, and in many areas crops can be grown continuously only if fertilizers are applied. On poorer soils, a shifting subsistence agriculture is practiced. Under this system small plots are cleared, cropped for a few years, then abandoned until their natural fertility is restored—a practice called roza in Panama. Areas of alluvial soils (which develop from clay, silt, sand, and gravel deposited by streams) are especially fertile but are limited to the lower parts of river valleys. The commercial banana plantations around Puerto Armuelles and in western Bocas del Toro province are mainly on alluvial soils. Some of the soils along the inland edges of coastal mangrove swamps have also proved productive. In some areas, exceptionally fertile soils have developed from volcanic ash. Climate of Panama Climatic conditions are markedly different on the Atlantic and Pacific sides of western Panama, especially in the amount and seasonal distribution of rainfall. On the Caribbean slopes of the Tabasará Mountains, which face the rain-bearing trade winds, average rainfall is approximately twice as heavy as on the leeward Pacific slopes. The Caribbean coast receives 60–140 inches (1,500–3,550 mm) per year, while the more populated Pacific region receives 45–90 inches (1,140–2,290 mm). Furthermore, on the Caribbean side rain falls almost throughout the year, while on the Pacific side there is more seasonal variation—in Chiriquí province, for example, there is a pronounced dry season lasting from January to April, and March is usually the driest month. In accordance with this rainfall pattern, tropical rainforests are typical on Caribbean slopes, whereas savannas (tropical grasslands) are more common southward in the seasonally dry areas between the Tabasará Mountains and the Pacific shoreline. Toward the Colombian border both sides of the isthmus have year-round rainfall. Because of Panama’s tropical location, the mean temperature of the coldest month seldom drops below 78 °F (26 °C) on either coast. The Panamanian mountain slopes create three climatic zones: a low, hot zone, lying at elevations below 2,300 feet (700 metres), which makes up nearly nine-tenths of the country’s territory; a temperate zone, at elevations ranging from 2,300 to 4,900 feet (700 to 1,500 metres), which accounts for most of the rest of the land; and a tiny cold zone, lying above 4,900 feet. Each zone has its characteristic plant growth and crops; cacao and bananas are produced mainly in the hot lowlands, whereas coffee is grown in the temperate zone. More … Score: https://www.britannica.com/place/Panama  

2025/11/03

Web portal for Algerian exports promotion

ALGIERS- A virtual gallery destined for the promotion of Algerian exports abroad will be shortly launched by the National Agency for Foreign ...

2025/11/03

We Are Micronesia

A slide show of some beautiful images of the Federated States of Micronesia in the Pacific.

2025/11/02