Odkryj Polskę / Explore Poland

Najpiękniejszy film o Polsce 2018. Niezwykła, zachwycająca, wyjątkowa i niepowtarzalna - POLSKA!

2025/11/10

Welcome to Angola

2025/11/10

Independence day of the Kingdom of Cambodia

Cambodia, country on the Indochinese mainland of Southeast Asia. Cambodia is largely a land of plains and great rivers and lies amid important overland and river trade routes linking China to India and Southeast Asia. The influences of many Asian cultures, alongside those of France and the United States, can be seen in the capital, Phnom Penh, one of a handful of urban centres in the largely rural country. For 2,000 years Cambodia’s civilization absorbed influences from India and China and, in turn, transferred them to other Southeast Asian civilizations. From the Hindu-Buddhist kingdoms of Funan and Chenla (1st–8th century) through the classical age of the Angkor period (9th–15th century), it held sway over territories that are now part of Thailand, Vietnam, and Laos. The Khmer (Cambodian) empire reached its apex in the 12th century, a time marked by the construction of the massive temple complexes known as Angkor Wat and Bayon and the imperial capital of Angkor Thom. Following 400 years of decline, Cambodia became a French colony and during the 20th century experienced the turmoil of war, occupation by the Japanese, postwar independence, and political instability. Between 1975 and 1979 the country was devastated by the reign of the Khmer Rouge, a rural communist guerrilla movement. During the Khmer Rouge’s period of power, at least 1.5 million Cambodians were killed or died, a monumental tragedy from which the country still suffers. Cambodia began the process of recovery under the Vietnam-backed regime of the People’s Republic of Kampuchea (1979–89), and in the 1990s it regained political autonomy, reestablished a constitutional government, and subsequently instituted free elections. The Cambodian economy has steadily improved, and the country seems to be living by the words of the Cambodian proverb, "Fear not the future, weep not for the past." Land Cambodia, about one-third the size of France and somewhat larger than the U.S. state of Missouri, is bordered to the west and northwest by Thailand, to the northeast by Laos, to the east and southeast by Vietnam, and to the southwest by the Gulf of Thailand. The country’s maximum extent is about 280 miles (450 km) from north to south and 360 miles (580 km) from east to west. Get a Britannica Premium subscription and gain access to exclusive content. Relief Cambodia’s landscape is characterized by a low-lying central alluvial plain that is surrounded by uplands and low mountains and includes the Tonle Sap (Great Lake) and the upper reaches of the Mekong River delta. Extending outward from this central region are transitional plains, thinly forested and rising to elevations of about 650 feet (200 metres) above sea level. To the north the Cambodian plain abuts a sandstone escarpment, which forms a southward-facing cliff stretching more than 200 miles (320 km) from west to east and rising abruptly above the plain to heights of 600 to 1,800 feet (180 to 550 metres). This escarpment marks the southern limit of the Dangrek (Khmer: Dângrêk) Mountains. Flowing south through the country’s eastern regions is the Mekong River. East of the Mekong the transitional plains gradually merge with the eastern highlands, a region of forested mountains and high plateaus that extend into Laos and Vietnam. In southwestern Cambodia two distinct upland blocks, the Krâvanh (Cardamom) Mountains and the Dâmrei (Elephant) Mountains, form another highland region that covers much of the land area between the Tonle Sap and the Gulf of Thailand. In this remote and largely uninhabited area, Mount Aôral, Cambodia’s highest peak, rises to an elevation of 5,949 feet (1,813 metres). The southern coastal region adjoining the Gulf of Thailand is a narrow lowland strip, heavily wooded and sparsely populated, which is isolated from the central plain by the southwestern highlands. Drainage The two dominant hydrological features of Cambodia are the Mekong River and the Tonle Sap. Rising in the Plateau of Tibet and emptying into the South China Sea, the Mekong enters Cambodia from Laos at the Khone Falls and flows generally southward to the border with Vietnam, a distance within Cambodia of approximately 315 miles (510 km). The Mekong is connected to the Tonle Sap by the Sab River. During the rainy season (mid-May to early October), the Mekong’s enormous volume of water backs up into the Sab and flows up into the Tonle Sap 65 miles (105 km) to the northwest, expanding the lake’s surface area from a dry-season minimum of 1,200 square miles (3,100 square km) to a rainy-season maximum of more than 3,000 square miles (7,800 square km). As the water level of the Mekong falls during the dry season, the process is reversed: water drains from the Tonle Sap back down into the Mekong, switching the direction of its flow. As a result of this annual phenomenon, the Tonle Sap is one of the world’s richest sources of freshwater fish. Soils Most of Cambodia’s soils are sandy and poor in nutrients. The so-called red-soil areas in the eastern part of the country, however, are suitable for commercial crops such as rubber and cotton. The annual flooding of the Mekong during the rainy season deposits a rich alluvial sediment that accounts for the fertility of the central plain and provides natural irrigation for rice cultivation. Climate of Cambodia Cambodia’s climate is governed by the monsoon winds, which define two major seasons. From mid-May to early October, the strong prevailing winds of the southwest monsoon bring heavy rains and high humidity. From early November to mid-March, the lighter and drier winds of the northeast monsoon bring variable cloudiness, infrequent precipitation, and lower humidity. The weather between these seasons is transitional. Maximum temperatures are high throughout the year, ranging from about 82 to 83 °F (28 °C) in January, the coolest month, to about 95 °F (35 °C) in April. Annual precipitation varies considerably throughout the country, from more than 200 inches (5,000 mm) on the seaward slopes of the southwestern highlands to about 50–55 inches (1,270–1,400 mm) in the central lowland region. Three-fourths of the annual rainfall occurs during the months of the southwest monsoon. Plant and animal life Although much of Cambodia is heavily forested, the central lowland region is covered with rice paddies, fields of dry crops such as corn (maize) and tobacco, tracts of tall grass and reeds, and thinly wooded areas. Savanna grassland predominates in the transitional plains, with the grasses reaching a height of 5 feet (1.5 metres). In the eastern highlands the high plateaus are covered with grasses and deciduous forests. Broad-leaved evergreen forests grow in the mountainous areas to the north, with trees 100 feet (30 metres) high emerging from thick undergrowths of vines, rattans, palms, bamboos, and assorted woody and herbaceous ground plants. In the southwestern highlands, open forests of pines are found at the higher elevations, while the rain-drenched seaward slopes are blanketed with virgin rainforests growing to heights of 150 feet (45 metres) or more. Vegetation along the coastal strip ranges from evergreen forests to nearly impenetrable mangroves. The northeastern forests of Cambodia—like the neighbouring areas of Laos and Vietnam—once sheltered large populations of wild animals such as elephants, wild oxen, rhinoceroses, and several species of deer, but the loss of forest cover, combined with warfare and unregulated hunting in the region, sharply reduced those numbers. Small populations of most of these species may still be found, along with some tigers, leopards, bears, and many small mammals. Among the more common birds are herons, cranes, grouse, pheasant, peafowl, pelicans, cormorants, egrets, and wild ducks. Four varieties of snakes are especially dangerous: the Indian cobra, the king cobra, the banded krait, and Russell’s viper. More … Score: https://www.britannica.com/place/Cambodia

2025/11/09

קמבודיה ומקדשי אנקור וואט

סרט הסבר על המקדשים המדהימים בקמבודיה אנגקור וואט כמה טיפים ממני ומידע על המקום המדהים הזה!!

2025/11/08

The Kingdom Of Tonga

With over 170 islands full of wonder and un-spoilt beauty, there are plenty of unforgettable adventures on offer for any traveller in the Kingdom of Tonga

2025/11/06

Micronesia's Official Travel and Tour ...

This is Micronesia's Official Travel Destination Website, for Guam, Northern Mariana Islands (CNMI), Palau, Federates States of Micronesia (FSM),

2025/11/05

Community Tourism Project

The official website of the Ministry of Tourism, International Transport and Maritime Initiatives.

2025/11/05

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