Visit Iran | Official Travel Guide of Iran

Iran owns an enormous wealth of traditional masterpieces remained from old, middle, and modern arenas. The geographical location of Iran, bridging west to ...

2026/02/13

Victory Day of the Iranian Revolution of the Islamic Republic of Iran

Iran, a mountainous, arid, and ethnically diverse country of southwestern Asia. Much of Iran consists of a central desert plateau, which is ringed on all sides by lofty mountain ranges that afford access to the interior through high passes. Most of the population lives on the edges of this forbidding, waterless waste. The capital is Tehrān, a sprawling, jumbled metropolis at the southern foot of the Elburz Mountains. Famed for its handsome architecture and verdant gardens, the city fell somewhat into disrepair in the decades following the Iranian Revolution of 1978–79, though efforts were later mounted to preserve historic buildings and expand the city’s network of parks. As with Tehrān, cities such as Eṣfahān and Shīrāz combine modern buildings with important landmarks from the past and serve as major centres of education, culture, and commerce. The heart of the storied Persian empire of antiquity, Iran has long played an important role in the region as an imperial power and later—because of its strategic position and abundant natural resources, especially petroleum—as a factor in colonial and superpower rivalries. The country’s roots as a distinctive culture and society date to the Achaemenian period, which began in 550 bce. From that time the region that is now Iran—traditionally known as Persia—has been influenced by waves of indigenous and foreign conquerors and immigrants, including the Hellenistic Seleucids and native Parthians and Sasanids. Persia’s conquest by the Muslim Arabs in the 7th century ce was to leave the most lasting influence, however, as Iranian culture was all but completely subsumed under that of its conquerors. An Iranian cultural renaissance in the late 8th century led to a reawakening of Persian literary culture, though the Persian language was now highly Arabized and in Arabic script, and native Persian Islamic dynasties began to appear with the rise of the Ṭāhirids in the early 9th century. The region fell under the sway of successive waves of Persian, Turkish, and Mongol conquerors until the rise of the Safavids, who introduced Twelver Shiʿism as the official creed, in the early 16th century. Over the following centuries, with the state-fostered rise of a Persian-based Shiʿi clergy, a synthesis was formed between Persian culture and Shiʿi Islam that marked each indelibly with the tincture of the other. With the fall of the Safavids in 1736, rule passed into the hands of several short-lived dynasties leading to the rise of the Qājār line in 1796. Qājār rule was marked by the growing influence of the European powers in Iran’s internal affairs, with its attendant economic and political difficulties, and by the growing power of the Shiʿi clergy in social and political issues. The country’s difficulties led to the ascent in 1925 of the Pahlavi line, whose ill-planned efforts to modernize Iran led to widespread dissatisfaction and the dynasty’s subsequent overthrow in the revolution of 1979. This revolution brought a regime to power that uniquely combined elements of a parliamentary democracy with an Islamic theocracy run by the country’s clergy. The world’s sole Shiʿi state, Iran found itself almost immediately embroiled in a long-term war with neighbouring Iraq that left it economically and socially drained, and the Islamic republic’s alleged support for international terrorism left the country ostracized from the global community. Reformist elements rose within the government during the last decade of the 20th century, opposed both to the ongoing rule of the clergy and to Iran’s continued political and economic isolation from the international community. Land Iran is bounded to the north by Azerbaijan, Armenia, Turkmenistan, and the Caspian Sea, to the east by Pakistan and Afghanistan, to the south by the Persian Gulf and the Gulf of Oman, and to the west by Turkey and Iraq. Iran also controls about a dozen islands in the Persian Gulf. About one-third of its 4,770-mile (7,680-km) boundary is seacoast. Relief of Iran A series of massive, heavily eroded mountain ranges surrounds Iran’s high interior basin. Most of the country is above 1,500 feet (460 metres), with one-sixth of it over 6,500 feet (1,980 metres). In sharp contrast are the coastal regions outside the mountain ring. In the north a strip 400 miles (650 km) long bordering the Caspian Sea and never more than 70 miles (115 km) wide (and frequently narrower) falls sharply from 10,000-foot (3,000-metre) summits to the marshy lake’s edge, some 90 feet (30 metres) below sea level. Along the southern coast the land drops away from a 2,000-foot (600-metre) plateau, backed by a rugged escarpment three times as high, to meet the Persian Gulf and the Gulf of Oman. The Zagros (Zāgros) Mountains stretch in a northwest-southeast direction, from Iran’s borders with Turkey and Iraq in the northwest to the Strait of Hormuz in the southeast. Farther to the south the range broadens into a band of parallel ridges 125 miles (200 km) wide that lies between the plains of Mesopotamia and the great central plateau of Iran. The range is drained on the west by streams that cut deep narrow gorges and water fertile valleys. The land is extremely rugged and difficult to access and is populated largely by pastoral nomads. The Elburz (Alborz) Mountains run along the south shore of the Caspian Sea to meet the border ranges of the Khorāsān region to the east. The tallest peak in the chain is the snow-clad Mount Damāvand (Demavend), which is also Iran’s highest point. Many parts of Iran are isolated and poorly surveyed, and the elevation of many of its peaks are still in dispute; the height of Mount Damāvand is generally given as 18,605 feet (5,671 metres). Volcanic and tectonic activity Mount Taftān, a massive cone reaching 13,261 feet (4,042 metres) in southeastern Iran, emits gas and mud at sporadic intervals. In the north, however, Mount Damāvand has been inactive in historical times, as have Mount Sabalān (15,787 feet [4,812 metres]) and Mount Sahand (12,172 feet [3,710 metres]) in the northwest. The Sahand-Bazman Belt, formed by Eocene volcanism, extends some 1,200 miles (1,900 km) from the border with Azerbaijan in the northwest to Baluchistan in the southeast and includes volcanic peaks such as Mount Sahand, Mount Karkas in Eṣfahān province, Mount Lalahezar in Kermān province, and Bazman in Sīstān va Balūchestān province. In addition, in the northwestern section of the country, lava and ashes cover a 200-mile (320-km) stretch of land from Jolfā on the border with Azerbaijan eastward to the Caspian Sea. A third volcanic region, which is 250 miles (400 km) long and 40 miles (65 km) wide, runs between Lake Urmia (Orūmiyyeh) and the city of Qazvīn. Earthquake activity is frequent and violent throughout the country. During the 20th century—when reliable records were available—there were fully a dozen earthquakes of 7.0 or higher on the Richter scale that took large numbers of lives. In 1990 as many as 50,000 people were killed by a powerful tremor in the Qazvīn-Zanjān area. In 2003 a relatively weak quake struck the ancient town of Bam in eastern Kermān province, leveling the town and destroying a historic fortress. More than 25,000 people perished. The interior plateau The arid interior plateau, which extends into Central Asia, is bounded on the west by the Zagros Mountains, on the north by the Elburz Mountains and the Kopet-Dag (Koppeh Dāgh) Range, and on the south by the Bashagard Range, which extends east from the Strait of Hormuz into the Baluchistan region of Iran. The plateau is cut by several smaller mountain ranges. In the flatlands lie the plateau’s most-remarkable features, the Kavīr and Lūt deserts, also called the Dasht-e Kavīr and Kavīr-e Lūt. At the lowest elevations, series of basins in the poorly drained soil remain dry for months at a time; the evaporation of any accumulated water produces the salt wastes known as kavīrs. As elevation rises, surfaces of sand and gravelly soil gradually merge into fertile soil on the hillsides and mountain slopes. More … Source: https://www.britannica.com/place/Iran

2026/02/11

Iran Travel Video——Colorful Persian

Iran is the favorite country I have been to. She is warm, friendly and safe, and has too many colorful scenes. Please don't misunderstand her. She is also an ancient civilization with a history of 5,000 years. You are here, you will fall in love with it. I am grateful to those who have helped me during my trip to Iran, and to all the Iranian friends who have appeared in the picture.

2026/02/10

Pure Grenada: The Official Website of the Grenada Tourism ...

Welcome to Pure Grenada, a hidden gem with unspoiled beauty offering a lifestyle so pure and authentic that you will feel instantly renewed.

2026/02/09

Welcome to New Zealand | Official site for Tourism New Zealand

Welcome to New Zealand. Get official travel information, maps, itineraries, best time to travel & things to do to help you plan your next holiday to New ..

2026/02/08

Granada's Independence Day

Grenada, byname Isle of Spice, island country of the West Indies. It is the southernmost island of the north-south arc of the Lesser Antilles, lying in the eastern Caribbean Sea about 100 miles (160 km) north of the coast of Venezuela. Oval in shape, the island is approximately 21 miles (34 km) long and 12 miles (19 km) wide. The southern Grenadines—the largest of which is Carriacou, about 20 miles (32 km) north-northeast, with an area of 13 square miles (34 square km)—are a dependency. The capital, St. George’s, on the southwest coast, is also the main port, having a fine natural harbour, and its picturesque pastel-coloured houses rise up the hillsides from the waterfront. The waterfront itself is known as the Carenage because island schooners were once careened (beached for cleaning or repair) there. St. George’s is the yachting and charter-boat centre of the eastern Caribbean. Land - Relief Grenada is volcanic in origin, with a ridge of mountains running north and south—the steeper slopes to the west and a more gradual incline to the east and southeast. The highest point is Mount St. Catherine (2,757 feet [840 metres]) in the northern part of the interior. The landscape is scenic, with fairly deep steep-sided valleys and about 10,000 acres (4,000 hectares) of forest. Drainage and soils Several short, swiftly flowing streams supply all towns and most villages with piped clean water. A further source of water is Grand Etang, a lake covering 36 acres in the crater of an extinct volcano at an elevation of 1,740 feet (530 metres). The fertile soils are chiefly volcanic, with some limestone in the north. Climate The island has equable temperatures, varying with altitude and averaging 82 °F (28 °C). Rainfall is adequate, except in the Point Salines area in the southwest; it varies from an average of 60 inches (1,500 mm) in coastal districts to more than 150 inches (3810 mm) in the mountainous regions. The rainy season lasts from June to December. November is the wettest month, but showers occur frequently during the other months. Grenada lies south of the usual track of hurricanes, but when they do occur, as in 1955, 1979, and 1980, they often cause extensive damage. Plant and animal life The island is verdant, with a year-round growing season and a wide variety of tropical fruits, flowering shrubs, and ferns. There are also forests of teak, mahogany, saman (known as the rain tree), and blue mahoe (a strong-fibred tree) in the interior. The animal life is varied and includes such wild animals as the mona monkey (a small, long-tailed, West African species that was introduced by slaves), the manicou (a species of opossum), the agouti (a rabbit-sized rodent, which is brown or grizzled in colour), the iguana, the mongoose, and a variety of turtles and land crabs. People Most of the population is black, having descended from African slaves, and there is a large minority of mulattoes and other mixtures. There are also small minorities of East Indians, descendants of indentured labourers brought to replace the freed slaves; descendants of the old French and British settlers; and more-recent immigrants from North America and Europe. Although English is the accepted language, a form of patois is still spoken by older people in the villages. Nearly one-half of the population is Protestant. More than one-third is Roman Catholic, and small but significant portions of the population adhere to the Rastafarian and Jehovah’s Witnesses’ faiths. Although Grenada is densely populated, its population grew slowly during the 20th century. Economy Agriculture and tourism are the most important sectors of the economy, although fishing and agriculturally based industries are becoming more significant. Grenada relies on financial support from the United Kingdom and other sources to bolster the economy. Agriculture, forestry, and fisheries To a greater extent than in most West Indian islands, Grenada’s arable land is divided into small holdings on which peasant proprietors cultivate diversified crops. Because of these small holdings and the generally hilly terrain, mechanical tilling is rare. The major agricultural export crops—cocoa, bananas, nutmeg, and mace—in the past were controlled by cooperative associations, but these associations have begun to come under greater government control. Banana exports depend upon preferential terms given by the United Kingdom and are affected by the policies of the European Union. Exports of mace and lime juice provide substantial earnings. Copra and, increasingly, other products processed from the coconut are also exported, and a wide variety of tropical fruits—mangoes, passion fruit, guavas, tamarind, and citrus fruits—are grown. The government has encouraged increased production of staple vegetables, such as peas, tomatoes, sweet potatoes, pumpkins, and corn (maize). The island’s forests yield mostly teak and mahogany, and the government has worked to upgrade fishing. Manufacturing, services, and trade Tourism, a major factor in the island’s economy, has been encouraged by the government. Air transport facilities have been improved, and the harbour is visited by numerous cruise ships. Other sources of employment are such secondary industries as clothing manufacture, sugar milling, brewing, rum distilling (a strong white rum being made for local consumption), food canning, copra processing, cigarette manufacturing, and soapmaking. There is a cotton ginnery on Carriacou. Grenada’s principal trading partner is the United States. Exports go largely to the United States, Germany, Malaysia, the Netherlands, and Egypt and to other Caribbean countries. Most imports come from the United States, China, the United Kingdom, Malaysia, and Barbados. Transportation of Grenada Bus service is available between the larger towns and villages. An international airport at Point Salines was inaugurated in 1984. Pearls Airport—providing service to nearby islands with connecting flights to Venezuela—is located on the northeastern coast. An airport on Carriacou also provides flights to nearby islands. The harbour at St. George’s has berths for oceangoing vessels, as well as a yacht basin and service facilities. Several shipping lines maintain regular passenger and cargo services to North America, the United Kingdom, Europe, and neighbouring West Indian islands. Government and society - Constitutional framework Grenada is governed as a constitutional monarchy, with the British monarch represented by a governor-general as the nominal head of state. Executive authority is vested in a prime minister, who is the head of the majority party in the elected House of Representatives, the lower house of the two-chamber legislature. The Senate is appointed by the governor-general on the advice of the prime minister and the opposition leader. Health and welfare Grenada has several main health centres, as well as district medical stations. Medical and dental treatment in government hospitals and clinics is free. The government has launched a program to eradicate malaria and mongoose-spread rabies. Education School attendance is not compulsory, although primary and secondary education is free. Grenada has vocational and technical schools as well as the St. George’s University School of Medicine and a branch of the University of the West Indies. Cultural life The Grenada National Museum in St. George’s is dedicated to archaeology and history and houses the Grenada Historical Society. Two Grenadian artists, Elinus Cato and Canute Caliste, have achieved international recognition for their primitive-style paintings. Several weekly newspapers are published, and islandwide radio and television broadcasting is available. History Grenada was sighted by Christopher Columbus on August 15, 1498, when he sailed past the island without landing and gave it the name Concepción. The origin of the name Grenada remains obscure. After Europeans first encountered it, Grenada was dominated for 150 years by the warlike Carib people, who had earlier killed off the more peaceful Arawak. In 1609 British merchants attempted to form a settlement, but the Caribs forced them to leave. More … Source: https://www.britannica.com/place/Grenada

2026/02/07

Grenada - the spice island (Travel Video)

We travelled through Grenada and Carriacou for two and a half weeks mainly by bus. We stayed at a couple of great places and really enjoyed our stay on Carriacou. Luckily the tropical storm Bret lost power and only a bit of rain reached us.

2026/02/06

Waitangi Day New Zealand

New Zealand, Māori Aotearoa, island country in the South Pacific Ocean, the southwesternmost part of Polynesia. New Zealand is a remote land—one of the last sizable territories suitable for habitation to be populated and settled—and lies more than 1,000 miles (1,600 km) southeast of Australia, its nearest neighbour. The country comprises two main islands—the North and the South Island—and a number of small islands, some of them hundreds of miles from the main group. The capital city is Wellington and the largest urban area Auckland; both are located on the North Island. New Zealand administers the South Pacific island group of Tokelau and claims a section of the Antarctic continent. Niue and the Cook Islands are self-governing states in free association with New Zealand. New Zealand is a land of great contrasts and diversity. Active volcanoes, spectacular caves, deep glacier lakes, verdant valleys, dazzling fjords, long sandy beaches, and the spectacular snowcapped peaks of the Southern Alps/Kā Tiritiri o te Moana on the South Island—all contribute to New Zealand’s scenic beauty. New Zealand also has a unique array of vegetation and animal life, much of which developed during the country’s prolonged isolation. It is the sole home, for example, of the long-beaked, flightless kiwi, the ubiquitous nickname for New Zealanders. New Zealand was the largest country in Polynesia when it was annexed by Great Britain in 1840. Thereafter it was successively a crown colony, a self-governing colony (1856), and a dominion (1907). By the 1920s it controlled almost all of its internal and external policies, although it did not become fully independent until 1947, when it adopted the Statute of Westminster. It is a member of the Commonwealth. The ascent of Mount Everest by New Zealander Sir Edmund Hillary with Sherpa Tenzing Norgay in 1953 was one of the defining moments of the 20th century. “In some ways,” Hillary suggested, “I believe I epitomise the average New Zealander: I have modest abilities, I combine these with a good deal of determination, and I rather like to succeed.” Despite New Zealand’s isolation, the country has been fully engaged in international affairs since the early 20th century, being an active member of a number of intergovernmental institutions, including the United Nations. It has also participated in several wars, including World Wars I and II. Economically the country was dependent on the export of agricultural products, especially to Great Britain. The entry of Britain into the European Community in the early 1970s, however, forced New Zealand to expand its trade relations with other countries. It also began to develop a much more extensive and varied industrial sector. Tourism has played an increasingly important role in the economy, though this sector has been vulnerable to global financial instability. The social and cultural gap between New Zealand’s two main groups—the indigenous Māori of Polynesian heritage and the colonizers and later immigrants from the British Isles and their descendants—has decreased since the 1970s, though educational and economic differences between the two groups remain. Immigration from other areas—Asia, Africa, and eastern Europe—has also made a mark, and New Zealand culture today reflects these many influences. Minority rights and race-related issues continue to play an important role in New Zealand politics. Land New Zealand is about 1,000 miles (1,600 km) long (north-south) and about 280 miles (450 km) across at its widest point. The country has slightly less surface area than the U.S. state of Colorado and a little more than the United Kingdom. About two-thirds of the land is economically useful, the remainder being mountainous. Because of its numerous harbours and fjords, the country has an extremely long coastline relative to its area. Relief of New Zealand Although New Zealand is small, its geologic history is complex. Land has existed in the vicinity of New Zealand for most of the past 500 million years. The earliest known rocks originated as sedimentary deposits some 545 million to 540 million years ago, at the close of Precambrian time (4.6 billion to 541 million years ago) and the beginning of the Cambrian Period (541 million to 485 million years ago); their source area was probably the continental forelands of Australia and Antarctica, then part of a nearby single supercontinent. Continental drift (the movement of large plates of Earth’s crust) created a distinct island arc and oceanic trench structure by the Carboniferous Period (about 359 to 299 million years ago), when deposition began in the downwarps (trenches) of the sedimentary rocks that today make up some three-fourths of New Zealand. This environment lasted about 250 million years and is typified by both downwarped oceanic sedimentary rocks and terrestrial volcanic rocks. This period was terminated in the west at the beginning of the Cretaceous Period (about 145 million years ago) by the Rangitata Orogeny (mountain-building episode), although downwarp deposition continued in the east. These mountains were slowly worn down by erosion, and the sea transgressed, eventually covering almost all of the land. At the end of the Oligocene Epoch (about 23 million years ago), the Kaikōura Orogeny began, raising land above the sea again, including the Southern Alps/Kā Tiritiri o te Moana of the South Island. Many of the great earth movements associated with this final orogeny took place (and take place today) along faults, which divide the landscape into great blocks, chief of which is the Alpine Fault of the South Island. The erosion and continued movement of these faulted blocks, together with the continuing volcanism of the North Island, define to a large extent the landscape of the country. New Zealand is part of the Ring of Fire—the circum-Pacific seismic belt marked by frequent earthquakes and considerable volcanic activity. The North Island and the western part of the South Island are on the Indian-Australian Plate, and the remainder of the South Island is on the Pacific Plate. Their collision creates violent seismic activity in subduction zones and along faults. Numerous earthquakes occur annually, including hundreds that can be felt by New Zealanders. A number of these temblors have been disastrous, such as one that devastated the towns of Napier and Hastings in 1931 and a series of quakes that did likewise in Christchurch in 2010–11. Both the North and the South islands are roughly bisected by mountains. Swift snow-fed rivers drain from the hills, although only in the east of the South Island have extensive alluvial plains been built up. The alluvial Canterbury Plains contrast sharply with the precipitous slopes and narrow coastal strip of the Westland region on the west coast of the South Island. The Southern Alps/Kā Tiritiri o te Moana are a 300-mile- (480-km-) long chain of fold mountains containing New Zealand’s highest mountain—Aoraki/Mount Cook at 12,316 feet (3,754 metres)—and some 20 other peaks that rise above 10,000 feet (3,000 metres), as well as an extensive glacier system with associated lakes. There are more than 360 glaciers in the Southern Alps/Kā Tiritiri o te Moana. The Tasman Glacier, the largest in New Zealand, with a length of 18 miles (29 km) and a width of more than 0.5 mile (0.8 km), flows down the eastern slopes of Aoraki/Mount Cook. Other important glaciers on the eastern slopes of the Southern Alps/Kā Tiritiri o te Moana are the Murchison, Mueller, and Godley; the Fox and Franz Josef are the largest on the western slopes. The North Island has seven small glaciers on the slopes of Mount Ruapehu. In the north of the South Island, the Alps break up into steep upswelling ridges. On their western face there are mineral deposits, and to the east they continue into two parallel ranges, terminating in a series of sounds. To the south the Alps break up into rugged, dissected country of difficult access and magnificent scenery, particularly toward the western tip of the island (called Fiordland). On its eastern boundary this wilderness borders a high central plateau called Central Otago, which has an almost continental climate. The terrain of the North Island is much less precipitous than that of the South and has a more benign climate and greater economic potential. In the centre of the island, the Volcanic Plateau rises abruptly from the southern shores of Lake Taupō, New Zealand’s largest natural lake, itself an ancient volcanic crater. To the east, ranges form a backdrop to rolling country in which pockets of highly fertile land are associated with the river systems. To the south, more ranges run to the sea. On the western and eastern slopes of these ranges, the land is generally poor, although the western downland region is fertile until it fades into a coastal plain dominated by sand dunes. To the west of the Volcanic Plateau, fairly mountainous country merges into the undulating farmlands of the Taranaki region, where the mild climate favours dairy farming even on the slopes of Mount Taranaki (Mount Egmont), a volcano that has been dormant since the 17th century. North of Mount Taranaki are the spectacular Waitomo caves, where stalactites and stalagmites are illuminated by thousands of glowworms. The northern shores of Lake Taupō bound a large area of high economic activity, including forestry. Even farther north there are river terraces sufficiently fertile for widespread dairy and mixed farming. The hub of this area is Auckland, which is situated astride an isthmus with a deep harbour on the east and a shallow harbour on the west. The peninsular region north of Auckland, called Northland, becomes gradually subtropical in character, marked generally by numerous deep-encroaching inlets of the sea bordered by mangrove swamps. More … Source: https://www.britannica.com/place/New-Zealand

2026/02/06

New Zealand Promotion

For more canoe, kayak and paddle sport news visit http://www.sportscene.tv

2026/02/05