Friday, June 5, 2009

Kakadu National Park



Kakadu National Park is in the Northern Territory of Australia, 171 km southeast of Darwin.

Kakadu National Park is located within the Alligator Rivers Region of the Northern Territory of Australia. It covers an area of 1,980,400 ha (4,894,000 acres),[1] extending nearly 200 kilometres from north to south and over 100 kilometres from east to west. It is the size of Israel, about one-third the size of Tasmania, or nearly half the size of Switzerland. The Ranger Uranium Mine, one of the most productive Uranium mines in the world, is contained within the park.

The name Kakadu comes from the mispronunciation of ‘Gagudju’ which is the name of an Aboriginal language spoken in the northern part of the Park. Kakadu is ecologically and biologically diverse.

Aboriginal people have occupied the Kakadu area continuously for at least 40 000 years. Kakadu National Park is renowned for the richness of its Aboriginal cultural sites. There are more than 5000 recorded art sites illustrating Aboriginal culture over thousands of years. The archaeological sites demonstrate Aboriginal occupation for at least 20 000 and possibly up to 40 000 years.


The cultural and natural values of Kakadu National Park were recognised internationally when the Park was placed on the UNESCO World Heritage List. This is an international register of properties that are recognised as having outstanding cultural or natural values of international significance. Kakadu was listed in three stages: Stage 1 in 1981, Stage 2 in 1987, and the entire Park in 1992.


Approximately half of the land in Kakadu is Aboriginal land under the Aboriginal Land Rights (Northern Territory) Act 1976 and most of the remaining land is currently under claim by Aboriginal people. The areas of the Park that are owned by Aboriginal people are leased by the traditional owners to the Director of National Parks to be managed as a national park. The remaining area is Commonwealth land vested under the Director of National Parks. All of Kakadu is declared a national park under the Environment Protection and Biodiversity Conservation Act 1999.


The Aboriginal traditional owners of the Park are descendants of various clan groups from the Kakadu area and have longstanding affiliations with this country. Their lifestyle has changed in recent years, but their traditional customs and beliefs remain very important. About 500 Aboriginal people live in the Park; many of them are traditional owners. All of Kakadu is jointly managed by Aboriginal traditional owners and the Australian Government’s Department of the Environment and Water Resources through a division known as Parks Australia. Park Management is directed by the Kakadu Board of Management.


Kakadu is located in the tropics, between 12° and 14° south of the Equator. The climate is monsoonal, characterised by two main seasons: the dry season and the rain season. The ‘build up’ describes the transition between the dry and the rain.During the dry season (from April/May to September), dry southerly and easterly trade winds predominate. Humidity is relatively low and rain is unusual. At Jabiru, the average maximum temperature for June-July is 32 °C.During the 'build up' (October to December) conditions can be extremely uncomfortable with high temperatures and high humidity. However 'build up' storms are impressive and lightning strikes are frequent. In fact the Top End of Australia records more lightning strikes per year than any other place on earth. At Jabiru the average maximum temperature for October is 37.5 °C.

The rain season (January to March/April) is characterised by warm temperatures and, as one would expect, rain. Most of the rain is associated with monsoonal troughs formed over Southeast Asia, although occasionally tropical cyclones produce intense heavy rain over localised areas. At Jabiru the average maximum temperature for January is 33 °C.Annual rainfall in Kakadu National Park ranges from 1,565 mm in Jabiru to 1,300 mm in the Mary River region.


Most non Aboriginal people really only refer to the rain and dry seasons, but Aboriginal people Bininj/Mungguy identify as many as six seasons in the Kakadu region:
* Gunumeleng - mid-October to late December, pre-monsoon storm season with hot weather and building thunderstorms in the afternoons
* Gudjewg - from January to March, monsoon season with thunderstorms, heavy rain, and flooding; the heat and humidity generate an explosion of plant and animal life
* Banggerreng - April, the "knock 'em down storm" season where floodwater recedes but violent, windy storms knock down grasses
* Yegge - from May to mid-June, relatively cool with low humidity, the Aboriginal people historically started burning the woodlands in patches to 'clean the country' and encourage new growth for grazing animals
* Wurrgeng - from mid-June to mid-August, the cold weather season with low humidity; most creeks stop flowing and the floodplains quickly dry out
* Gurrung - from mid-August to mid-October, hot dry weather with ever shrinking billabongs.

Periods of torrential rain and long dry spells mean that Kakadu can change its appearance according to the season, so is a place deserving of more than one visit.

Kakadu's flora is among the richest in northern Australia with more than 1700 plant species recorded which is a result of the Park's geological, landform and habitat diversity. Kakadu is also considered to be one of the most weed free national parks in the world.


The distinctly different geographical areas of Kakadu have their own specialised flora. The environment referred to as ‘the Stone Country’ features ‘resurrection grasses’ that are able to cope with extreme heat and long dry spells followed by periods of torrential rain. Monsoon forests often develop in the cool moist gorges dissecting the stone country. The southern hills and basins support several endemic plants that are only found in Kakadu such as Eucalyptus koolpinensis near Jarrangbarnmi (Koolpin Gorge). Lowland areas form a large proportion of Kakadu National Park and are mainly covered in eucalypt-dominated open woodland with the ground layer consisting of a large range of grasses including spear grass, sedges and wildflowers.

The floodplains, which are inundated for several months each, year feature sedges such as spike rush as well patches of freshwater mangroves (itchy tree), pandanus and paper bark trees (Melaleuca). Varieties of water lilies, such as the blue, yellow and white snowflake, are commonly found in these areas. Estuaries and tidal flats are populated with varieties of mangroves (39 of the 47 Northern Territory species of mangrove occur in Kakadu) that are important for stabilising the coastline. Mangroves serve as feeding and breeding grounds for many fish species including the barramundi.


On the tidal flats behind the mangroves, hardy succulents (samphire), grasses and sedges grow. Isolated pockets of monsoon forest grow along the coast and river banks. These forests contain several impressive trees, among them the banyan fig, which can be recognised by its large, spreading aerial roots, and the kapok tree, which has a spiny trunk, large, waxy red flowers and pods full of cotton-like material.

The diverse environments of Kakadu National Park support an astonishing array of animals, a number of which have adapted to particular habitats. Some animals in the Park are rare, endangered, vulnerable or endemic. Responding to the extreme weather conditions experienced in the Park, many animals are active only at particular times of the day or night or at particular times of the year.

About 60 mammal species—marsupials and placental mammals—have been recorded in the Park. Most of them inhabit the open forest and woodlands and are nocturnal, making it difficult to see them. Others, such as wallabies and kangaroos (macropods), are active in the cooler parts of the day and are easier to see. However, recent surveys have revealed a disturbing decline of nearly all mammal species throughout Kakadu, including once common and widespread species such as northern quolls. Kakadu’s many habitats support more than 280 species of birds, or about one-third of Australia’s bird species. Some birds range over a number of habitats, but many are found in only one environment.

To date, 117 species of reptiles have been recorded in Kakadu. Being cold blooded, these animals rely on heat from an external source such as the sun to regulate their body temperature. This is not to say that reptiles are active only during the day; in fact, few snakes can withstand Kakadu’s midday heat and most are active at night.


There are six main landforms in Kakadu National Park: the Arnhem Land plateau and escarpment complex, known as the stone country; the outliers; the lowlands; the southern hills and basins; the floodplains; and the tidal flats. Each landform has its own range of habitats. Kakadu’s varied landscapes and the habitats they contain are features that contributed to its listing as a World Heritage Area.

Most of Kakadu was under a shallow sea approximately 140 million years ago, with the escarpment wall formed from sea cliffs and Arnhem Land from a flat plateau above the sea. Currently the escarpment rises 330 metres above the plateau and extends approximately 500 kilometres along the East edge of the park and on into Arnhem Land. The escarpment varies from near vertical cliffs in the Jim Jim Falls area to isolated outliers and stepped cliffs in the North.

Kakadu National Park is a major tourist attraction in Australia’s north. Visitation in 2005 was 202,000. Kakadu’s dramatic landscape, Aboriginal cultural significance and diverse and abundant wildlife are what visitors are drawn to. There are many beautiful waterfalls and gorges within the Park that are popular with visitors such as Maguk, Gunlom, Twin Falls and Jim Jim Falls.

Kakadu National Park has some of the best examples of Aboriginal rock art in Australia. The sites of Nourlangie and Ubirr are among the most visited locations in the Park. It is possible to view some of Kakadu’s diverse wildlife at places like Yellow Water Billabong, Cooinda on board a wildlife cruise or at Mamukala Wetlands or Anbangbang Billabong. The Kakadu region is one of the world’s best for bird watching as approximately 30 percent of Australia’s bird species can be seen here.
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Thursday, June 4, 2009

Hongkong



Hong Kong officially the Hong Kong Special Administrative Region, is a largely self-governing territory of the People's Republic of China (PRC), located south of Guangdong province and facing the South China Sea to the east, west and south. A British dependent territory until 1997, Hong Kong has a highly developed capitalist economy and enjoys a high degree of autonomy from the PRC under the "one country, two systems" policy.

Beginning as a trading port, Hong Kong became a crown colony (later British overseas territories) of the United Kingdom in 1842, and remained so until its transfer of sovereignty to the People's Republic of China in 1997.


Along with Macau, Hong Kong is one of the two special administrative regions under the "one country, two systems" policy. As a result, Hong Kong is largely self-governing, has a high degree of autonomy in all areas except foreign affairs and defence, which are the responsibility of Government of the PRC. As part of this arrangement, Hong Kong maintains its own currency, separate legal and political systems, and is generally not considered part of mainland China.


Renowned for its expansive skyline and natural setting, its identity as a cosmopolitan centre where east meets west is reflected in its cuisine, cinema, music and traditions, Although the population is predominantly Chinese, residents and expatriates of other ethnicities form a small but significant segment of society. With a population of 7 million people, but only 1,108 km2 (428 sq mi) of land, Hong Kong is one of the most densely populated areas in the world.

The name "Hong Kong" in the English language is an approximate phonetic rendering of the Cantonese or Hakka pronunciation of the Chinese name "香港", meaning "fragrant harbour".

Before 1842, the name Hong Kong originally referred colloquially to a small inlet (now Aberdeen Harbour/Little Hong Kong) between the island of Ap Lei Chau and the south side of the island which later became known as Hong Kong. The inlet was one of the first points of contact between British sailors and local fishermen.The reference to fragrance may refer to the harbour waters sweetened by the fresh water esturine influx of the Pearl River, or to the incense factories lining the coast to the north of Kowloon which was stored around Aberdeen Harbour for export, before the development of Victoria Harbour.


In 1842, the Treaty of Nanking was signed, and the name Hong Kong was first recorded on official documents to encompass the entirety of the Island. The Convention of Peking (1860) and Convention for the Extension of Hong Kong Territory (1898) added the Kowloon peninsula and New Territories into Hong Kong's territory, which has remained unchanged until the present.
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Wednesday, June 3, 2009

Istanbul



Istanbul is the largest city in Turkey, largest city proper and second largest metropolitan area in Europe, and fourth largest city proper in the world with a population of 12.6 million. Istanbul is also a megacity. Istanbul is the cultural and financial center of Turkey. The city covers 27 districts of the Istanbul province. It is located on the Bosphorus Strait and encompasses the natural harbor known as the Golden Horn, in the northwest of the country. It extends both on the Europe (Thrace) and on the Asia (Anatolia) side of the Bosphorus, and is thereby the only metropolis in the world that is situated on two continents. In its long history, İstanbul served as the capital city of the Roman Empire (330–395), the East Roman (Byzantine) Empire (395–1204 and 1261–1453), the Latin Empire (1204–1261), and the Ottoman Empire (1453–1922). The city was chosen as joint European Capital of Culture for 2010. The historic areas of Istanbul were added to the UNESCO World Heritage List in 1985.


In 2008, during the construction works of the Yenikapı subway station and the Marmaray tunnel at the historic peninsula on the European side, a previously unknown Neolithic settlement dating from circa 6500 BC has been discovered. The first human settlement on the Anatolian side, the Fikirtepe mound, is from the Copper Age period, with artifacts dating from 5500–3500 BC. In nearby Kadıköy (Chalcedon) a port settlement dating back to the Phoenicians has been discovered. Cape Moda in Chalcedon was the first location which the Greek settlers from Megara chose to colonize in 685 BC, prior to colonizing Byzantion on the European side of the Bosphorus under the command of King Byzas in 667 BC. Byzantion was established on the site of an ancient port settlement named Lygos, founded by Thracian tribes between the 13th and 11th centuries BC, along with the neighbouring Semistra, of which Plinius had mentioned in his historical accounts. Only a few walls and substructures belonging to Lygos have survived to date, near the Seraglio Point (Turkish: Sarayburnu), where the famous Topkapı Palace now stands. During the period of Byzantion, the Acropolis used to stand where the Topkapı Palace stands today.


Istanbul is located in the north-west Marmara Region of Turkey. It encloses the southern Bosphorus which places the city on two continents—the western portion of Istanbul is in Europe, while the eastern portion is in Asia. The city boundaries cover a surface area of 1,830.92 square kilometres (707 sq mi), while the metropolitan region, or the Province of Istanbul, covers 6,220 square kilometres (2,402 sq mi).


Istanbul is situated near the North Anatolian fault line, which runs from northern Anatolia to the Marmara Sea. Two tectonic plates, the African and the Eurasian, push against each other here. This fault line has been responsible for several deadly earthquakes in the region throughout history. In 1509 a catastrophic earthquake caused a tsunami which broke over the sea-walls of the city, destroying over 100 mosques and killing 10,000 people. In 1766 the Eyüp Sultan Mosque was largely destroyed. The 1894 earthquake caused the collapse of many parts of the Grand Bazaar. A devastating earthquake on August 17, 1999, with its epicenter in nearby İzmit, left 18,000 dead and many more homeless. In all of these earthquakes, the devastating effects are a result of the building density and poor construction of buildings. Seismologists predict another earthquake, possibly measuring magnitude 7.0, occurring before 2025.


Istanbul like the Marmara region it is situated in is characterized by a temperate climate as well as a "transitional climate", midway between that of the oceanic climate of the Black Sea, the humid continental climate of the Balkan peninsula and the mediterranean climate of the southwest. This is also reflected in its plant geography since flora of these three regions flourish here. Istanbul is one of the provinces that best illustrates this aspect of the Marmara region. Thanks to the constantly very humid climate of Istanbul, plants of the Europe-Siberia region are concentrated here, especially in the northern areas near the Black Sea coast. An increase in mediterranean flora is observed in the warmer areas to the south of the city especially on the Princes' Islands, the only place in Istanbul with a mediterranean vegetation. With around 2500 different natural plant species, Istanbul alone puts European countries such as the whole of the United Kingdom in the shade in this respect. Even more importantly, this means that in Istanbul approximately one-fourth of the more than ten thousand documented plants that grow naturally in Turkey; some of these plants are endemic, in other words, they live only in Istanbul and nowhere else in the whole world.

Istanbul is becoming increasingly colorful in terms of its rich social, cultural, and commercial activities. While world famous pop stars fill stadiums, activities like opera, ballet and theater continue throughout the year. During seasonal festivals, world famous orchestras, chorale ensembles, concerts and jazz legends can be found often playing to a full house. The Istanbul International Film Festival is one of the most important film festivals in Europe, while the Istanbul Biennial is another major event of fine arts.

Istanbul has numerous historic shopping centers, such as the Grand Bazaar (1461), Mahmutpaşa Bazaar (1462) and the Egyptian Bazaar (1660). The first modern shopping mall was Galleria Ataköy (1987), which was followed by dozens of others in the later decades, such as Akmerkez (1993) which is the only mall to win both "Europe's Best" and "World's Best" awards by the ICSC; Metrocity (2003); Cevahir Mall (2005) which is the largest mall in Europe; and Kanyon Mall (2006) which won the 2006 Cityscape Architectural Review Award for its interesting design. İstinye Park (2007) and City's Nişantaşı (2008) are two new malls which target high-end consumers and are almost exclusively dedicated to world-famous fashion brands.

Along with the traditional Turkish restaurants, many European and Far Eastern restaurants and numerous other cuisines are also thriving in the city.

There are many night clubs, pubs, restaurants and taverns with live music in the city. The night clubs, restaurants and bars increase in number and move to open air spaces in the summer. The areas around Istiklal Avenue and Nişantaşı offer all sorts of cafés, restaurants, pubs and clubs as well as art galleries, theaters and cinemas.

The most popular open air summer time seaside night clubs are found on the Bosphorus, such as Reina, Sortie and Anjelique in the Ortaköy district. Babylon and Nu Pera in Beyoğlu are popular night clubs both in the summer and in the winter, while Istanbul Arena in Maslak frequently hosts the live concerts of famous singers and bands from all corners of the world. Parkorman in Maslak hosted the Isle of MTV Party in 2002 and is a popular venue for live concerts and rave parties in the summer. Q Jazz Bar in Ortaköy offers live jazz music in a stylish environment.
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Tuesday, June 2, 2009

Havana


Havana officially Ciudad de La Habana, is the capital city, major port, and leading commercial centre of Cuba. The city is one of the 14 Cuban provinces. The city/province has 2.4 million inhabitants, and the urban area over 3.7 million, making Havana the largest city in both Cuba and the Caribbean region. The city extends mostly westward and southward from the bay, which is entered through a narrow inlet and which divides into three main harbours: Marimelena, Guanabacoa, and Atarés. The sluggish Almendares River traverses the city from south to north, entering the Straits of Florida a few miles west of the bay.


King Philip II of Spain granted Havana the title of City in 1592 and a royal decree in 1634 recognized its importance by officially designated as the "Key to the New World and Rampart of the West Indies". Havana's coat of arms carries this inscription. The Spaniards began building fortifications, and in 1553 they transferred the governor's residence to Havana from Santiago de Cuba on the eastern end of the island, thus making Havana the de facto capital. The importance of harbour fortifications was early recognized as English, French, and Dutch sea marauders attacked the city in the 16th century. The sinking of the U.S. battleship Maine in Havana's harbor in 1898 was the immediate cause of the Spanish-American War.


The current Havana area and its natural bay were first visited by Europeans during Sebastián de Ocampo's circumnavigation of the island in 1509. Shortly thereafter, in 1510, the first Spanish colonists arrived from Hispaniola and began the conquest of Cuba.


Conquistador Diego Velázquez de Cuéllar founded Havana on August 25, 1515 on the southern coast of the island, near the present town of Surgidero de Batabanó. Between 1514 and 1519, the city had at least two different establishments. All attempts to found a city on Cuba's south coast failed. The city's location was adjacent to a superb harbor at the entrance to the Gulf of Mexico, and with easy access to the Gulf Stream, the main ocean current that navigators followed when traveling from the Americas to Europe. This location led to Havana’s early development as the principal port of Spain's New World colonies. An early map of Cuba drawn in 1514 places the town at the mouth of the river Onicaxinal, also on the south coast of Cuba. Another establishment was La Chorrera, today in the neighbourhood of Puentes Grandes, next to the Almendares River.
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Monday, June 1, 2009

The Grand Canyon


The Grand Canyon is a steep-sided gorge carved by the Colorado River in the United States in the state of Arizona. It is largely contained within the Grand Canyon National Park — one of the first national parks in the United States. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.


Longstanding scientific consensus has been that the canyon was created by the Colorado River over a six million year period. The canyon is 277 miles (446 km) long, ranges in width from 4 to 18 miles (6.4 to 29 km) and attains a depth of over a mile (1.83 km) (6000 feet). Nearly two billion years of the Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. The "canyon began in the west, followed by another that formed in the east. Eventually, the two broke through and met as a single majestic rent in the earth some six million years ago. The merger apparently occurred where the river today bends to the west, in the area known as the Kaibab Arch."


The Grand Canyon is a massive rift in the Colorado Plateau that exposes uplifted Proterozoic and Paleozoic strata, and is also one of the six distinct physiographic sections of the Colorado Plateau province. The Grand Canyon is unmatched throughout the world for the vistas it offers to visitors on the rim. It is not the deepest canyon in the world — Cotahuasi Canyon (11598 feet or 3535 m) and Colca Canyon (10499 feet or 3200 m), both in Arequipa, Peru, and Hells Canyon (7,993 feet or 2436 m) on the Oregon-Idaho border, are all deeper — but Grand Canyon is known for its overwhelming size and its intricate and colorful landscape. Geologically it is significant because of the thick sequence of ancient rocks that are beautifully preserved and exposed in the walls of the canyon. These rock layers record much of the early geologic history of the North American continent.


The principal consensus among geologists is that the Colorado River basin (of which the Grand Canyon is a part) has developed in the past 40 million years. A recent study places the origins of the canyon beginning some 17 million years ago. Previous estimates had placed the age of the canyon at 5 to 6 million years. The study, which was published in 2008 in the journal Science utilized uranium-lead dating to analyze calcite deposits found on the walls of nine caves throughout the canyon. There is a substantial amount of controversy because this research suggests such a substantial departure from prior widely supported scientific consensus.


Weather in the Grand Canyon varies according to elevation.
The forested rims are high enough to receive winter snowfall, but along the Colorado River in the Inner Gorge, temperatures are similar to those found in Tucson and other low elevation desert locations in Arizona. Conditions in the Grand Canyon region are generally dry, but substantial precipitation occurs twice annually, during seasonal pattern shifts in winter (when Pacific storms usually deliver widespread, moderate rain and high-elevation snow to the region from the west) and in late summer (a phenomenon known as the monsoon, which delivers waves of moisture from the southeast, causing dramatic, localized thunderstorms fueled by the heat of the day). Average annual precipitation on the South Rim is less than 16 inches (35 cm), with 60 inches (132 cm) of snow, the higher North Rim usually receives 27 inches (59 cm) of moisture, with a typical snowfall of 144 inches (317 cm), and Phantom Ranch, far below the Canyon's rims along the Colorado River at 2,500 feet (762 m) gets just 8 inches (17.6 cm) of rain, and snow is a rarity. The weather is different on the north rim and south rim.

The Grand Canyon has suffered some problems with air pollution, attributed to the nearby Navajo Generating Station, a coal-burning power plant. In 1991 an agreement was reached with the Navajo Generating Station in Page, Arizona, to add air pollution control devices to their smokestacks.

Grand Canyon National Park is one of the world’s premier natural attractions, attracting about five million visitors per year. Overall, 83% were from the United States: California (12.2%), Arizona (8.9%), Texas (4.8%), Florida (3.4%) and New York (3.2%) represented the top domestic visitors. Seventeen percent of visitors were from outside the United States; the most prominently represented nations were the United Kingdom (3.8%), Canada (3.5%), Japan (2.1%), Germany (1.9%) and The Netherlands (1.2%).

Aside from casual sightseeing from the South Rim (averaging 7000 feet (2100 m) above sea level), whitewater rafting, hiking and running are especially popular. The floor of the valley is accessible by foot, muleback, or by boat or raft from upriver. Hiking down to the river and back up to the rim in one day is discouraged by park officials because of the distance, steep and rocky trails, change in elevation, and danger of heat exhaustion from the much higher temperatures at the bottom. Rescues are required annually of unsuccessful rim-to-river-to-rim travelers. Nevertheless, hundreds of fit and experienced hikers complete the trip every year.

Lipan Point is a promontory located on the South Rim. This point is located to the east of the Grand Canyon Village along the Desert View Drive. There is a parking lot for visitors who care to drive along with the Canyon's bus service that routinely stops at the point. The trailhead to the Tanner Trail is located just before the parking lot. The view from Lipan Point shows a wide array of rock strata and the Unkar Creek area in the inner canyon.
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