Saturday, May 21, 2011

USA - Minnesota - State Bird


Common Loon (Gavia immer, sitting on its nest. The Common Loon is the Minnesota State Bird.

Sent by Ruth, a WiP partner from Minnesota, USA.

This is from Wikipedia : The loons (North America) or divers (UK/Ireland) are a group of aquatic birds found in many parts of North America and northern Eurasia (Europe, Asia and debatably Africa). All living species of loons are members of the genus (Gavia), family (Gaviidae) and order (Gaviiformes).

The loon, the size of a large duck or small goose, resembles these birds in shape when swimming. Like ducks and geese but unlike coots (which are Rallidae) and grebes (Podicipedidae), the loon's toes are connected by webbing. The bird may be confused with cormorants (Phalacrocoracidae), not too distant relatives of divers and like them are heavy set birds whose bellies – unlike those of ducks and geese – are submerged when swimming. Flying loons resemble a plump goose with a seagull's wings, relatively small in proportion to the bulky body. The bird holds its head pointing slightly upwards during swimming, but less so than cormorants do. In flight the head droops more than in similar aquatic birds.

Male and female loons have identical plumage. Plumage is largely patterned black-and-white in summer, with grey on the head and neck in some species. All have a white belly. This resembles many sea-ducks (Merginae) – notably the smaller goldeneyes (Bucephala) – but is distinct from most cormorants which rarely have white feathers, and if so usually as large rounded patches rather than delicate patterns. All species of divers have a spear-shaped bill.

Males are larger on average, but relative size is only apparent when the male and female are together.

In winter plumage is dark gray above, with some indistinct lighter mottling on the wings, and a white chin, throat and underside. The species can then be distinguished by certain features, such as size and colour of head, neck, back and bill, but often reliable identification of wintering divers is difficult even for experts – particularly as the smaller immature birds look similar to winter-plumage adults, making size an unreliable means of identification.

Gaviiformes are among the few groups of birds in which the young moult into a second coat of down feathers after shedding the first one, rather than growing juvenile feathers with downy tips that wear off as is typical in many birds. This trait is also found in tubenoses (Procellariiformes) and penguins (Sphenisciformes), both relatives of the loons.

USA - Delaware - Kalmar Nyckel


Launched in Sptember of 1997, the Kalmar Nyckel is a a 97 foot, 317-ton replica of the tall ship that brought the first Swedish settlers to the Delaware River Valley in 1638. The ship can be toured in its working shipyard, and it ocassionally leaves its port in Wilmington to sail to nearby Lewes.

Sent by Rose, a WiP partner from USA.

This is from Wikipedia : The Kalmar Nyckel (Key of Kalmar) was a Dutch-built armed merchant ship famed for carrying Finnish and Swedish settlers to North America in 1638 to establish the colony of New Sweden. A replica of the ship was launched at Wilmington, Delaware, in 1997.

The Kalmar Nyckel was constructed in about 1625 and was of a design called a pinnace. The ship was named after the city of Kalmar, which purchased the ship in 1628 as its contribution to the Royal Swedish Navy. When Sweden decided to establish a trading colony in the New World under the direction of Peter Minuit, the Kalmar Nyckel was chosen for the voyage. A smaller vessel, the Fogel Grip (Griffin Bird), accompanied her.

The ships sailed from Gothenburg in December 1637, commanded by Jan Hindriksen van der Water, but encountered a severe storm in the North Sea and had to divert to the Netherlands for repairs. They departed on New Year's Day 1638, arriving in North America in March 1638.

A second voyage, which departed on February 7, 1640, and arrived at Fort Christina on April 17, brought additional settlers for New Sweden. One of them was Reorus Torkillus, the first Lutheran clergyman in New Sweden. The Kalmar Nyckel made four successive round trips from Sweden, a record unchallenged by any other colonial vessel. She later served the Royal Swedish Navy in the Swedish-Danish War, then was used as a merchant ship. She was lost at sea in the late 17th century. There are conflicting reports on where she was lost. One says she sank off the coast of the city of Kalmar, while another says she was lost in the North Sea off the coast of England.

In 1986, a group of citizens of Wilmington, Delaware, established the Kalmar Nyckel Foundation, whose primary source of funding is from the taxpayers of the State of Delaware, plus donations from corporations and individuals. The foundation designed, built, and launched a replica of the Kalmar Nyckel. The modern ship, designed by naval architects Thomas C. Gillmer, Melbourne Smith, Joel Webster, and Ken Court, was built at a shipyard in Wilmington on the Christina River near the original 1638 Swedish settlers' landing site at Fort Christina. She was launched on September 28, 1997, and commissioned on May 9, 1998. The re-creation measures 94 feet (29 m) on deck and 131 feet (40 m) overall, with a 25-foot (7.6 m) beam, a 12-foot (3.7 m) draft, and a displacement of 300 tons.

The ship is operated and maintained by a volunteer staff, under the leadership of a paid captain, boatswain, and a chief mate. In November 2006, the captain of the Kalmar Nyckel, David W. Hiott, who had commanded her for nine seasons, died from the effects of recurring melanoma. Captain Lauren Morgens took over on April 1, 2007, with Sharon Litcofsky as Chief Mate and Relief Captain. Volunteers maintain the ship, run the education program, and sail her from port to port.

Portugal - Algarve


Algarve : Ruin of an ancient monastery.

Sent by Carlos, a postcrosser from Faro, Portugal.

Indonesia - Sangiran Early Man Site


Sent by Shinta from Semarang, Indonesia.

Sangiran is one of the key sites for the understanding of human evolution. It illustrates the development of Homo sapiens sapiens from the Lower Pleistocene to the present through the outstanding fossil and artefactual material that it has produced.

The archaeological site of Sangiran is situated 15 km east of Solo. The geological stratigraphy of the Sangiran area covers 2 million years, from the late Pliocene to the recent periods. The Lower and Middle Pleistocene Ievels have produced considerable fossil and artefactual material. Fifty early human fossils (Pithecanthropus erectus/Homo erectus ) have been found, representing 50% of all the known hominid fossils in the world, together with numerous animal and floral fossils such as rhinoceros, elephant ivory, buffalo horn, deer horn and many others.

Palaeolithic stone tools (Sangiran flakes) found at Ngebung include flakes, choppers and cleavers in chalcedony and jasper and, more recently, bone tools. The site has also produced Neolithic axes. This evidence indicates that hominids have inhabited the area for at Ieast 1.5 million years. The Palaeolithic tools can be dated to around 800,000 BP, and the sequence of cultural material from this period through to the Neolithic illustrates continuous evolution of man in relation to the ecosystem over a long period.

The geology of the Sangiran Early Man Site is sedimentary in origin, beginning with the late Pliocene. It was deformed into a domed anticline by diaper intrusion. The summit was subsequently eroded by river action, turning it into a recessed, reversed dome. Early hominid fossils occur in successive formations, starting with the Pucangang (0.5-1.5 million years BP), but more particularly in the Kabuh (0.25-0.5 million years BP) and Notopuro (11,000-250,000 years BP). Nowadays, it is an unfertile hill and the region is now entirely devoted to peasant agriculture.

Ever since von Koenigswald found flake tools in the Ngebung village in 1934, the site has made an immense contribution to the study of evolution over the past million years by illustrating the evolution of Homo erectus . Homo erectus is important to the study of the early history of mankind before the emergence of the modern Homo sapiens . Fossils of Homo erectus have been found from time to time in a site covering 8 km by 7 km since 1936 to the present day.

Not only has the Sangiran site contributed to the understanding of the family tree of mankind, it has also thrown much light the evolution of culture, of animals, and of the ancient environment. Large quantities of human and animal fossils, along with Palaeolithic tools, have been found on the Sangiran site in a geological-stratigraphical series that has been laid down continuously for more than 2 million years. (Source)


Indonesia - Prambanan Temple Compounds (2)


Prambanan Hindu Temple in Yogyakarta.

Sent by Shinta from Semarang, Indonesia.


Wednesday, May 18, 2011

Poland - Fontanna Neptuna


Fontanna Neptuna or Neptune's Fountain in Gdańsk.

Sent by Magdalena, a postcrosser from Gdańsk in Poland.

"Neptune's Fountain, in the center of Dlugi Targ (the Long Market) has grown to be one of Gdansk's most recognizable symbols. The bronze statue of the Roman god of the sea was first erected in 1549, before being aptly made into a fountain in 1633. Like the city he represents, Neptune has had a storied history, himself - dismantled and hidden during World War II, old Neptune didn't come out of hiding until 1954 when he was restored to his rightful place in the heart of the city, reminding us of Gdansk's relationship to the sea. Chances are you've already had your photo taken with this mighty trident-wielding behemoth, or will soon. The colourful buildings of Dlugi Targ make a great backdrop for any photo-op, so flash those gums and say 'cheese!"(Source)

Martta Wendelin (12)


Martta Wendelin.

Sent by Mecu, a postcrosser from Hämeenlinna, Finland.

Tuesday, May 17, 2011

Slovakia - Mapcard (2)


SLOVAKIA
Despite its rather small size, Slovakia offers great diversity of landscapes, untouched nature, numerous magic castles and charming historic towns.

Sent by Zuzana from Bratislava, Slovakia.

USA - Connecticut - Connecticut River


The Connecticut River is the largest river in New England, flowing south from the Connecticut Lakes in northern New Hampshire, along the border between New Hampshire and Vermont, through Western Massachusetts and central Connecticut into Long Island Sound at Old Saybrook, Connecticut.

Sent by Ezza, a postcrosser from USA.

This is from Wikipedia : The Connecticut River is the largest river in New England, flowing south from the Connecticut Lakes in northern New Hampshire, along the border between New Hampshire and Vermont, through western Massachusetts and central Connecticut discharging into Long Island Sound at Old Saybrook and Old Lyme, Connecticut. It has a total length of 407 miles (655 km), and a drainage basin extending over 11,250 square miles (29,100 km2). The mean freshwater discharge into Long Island Sound is 19,600 cubic feet (560 m3) per second. The largest city on the river is Springfield, Massachusetts. Hartford, the capital of Connecticut, is also on the river, 24 miles (39 km) miles south of Springfield.

The Connecticut River is tidal up to Windsor Locks, Connecticut, approximately 60 miles (97 km) from the mouth. The source of the river is the Fourth Connecticut Lake in New Hampshire. Some tributaries include the Ashuelot, West, Miller's, Deerfield, White, and Chicopee rivers. The Swift River, a tributary of the Chicopee, has been dammed and largely replaced by the Quabbin Reservoir which provides water to Boston.

The river carries a heavy amount of silt, especially during the spring snow melt, from as far north as Quebec. The heavy silt concentration of the river forms a large sandbar near its mouth on Long Island Sound and has historically provided a formidable obstacle to navigation. The difficulty of navigation on the river is the primary reason that it is one of the few large rivers in the region without a major city near its mouth. The Connecticut River estuary and tidal wetlands complex is listed as one of the 1,759 wetlands of international importance under the Ramsar Convention on Wetlands.

Australia - Blue-winged Kookaburra


Blue-winged Kookaburra (Dacelo leachii).

Sent by Haining, a postcrosser from Australia.

This is from Wikipedia : The Blue-winged Kookaburra, Dacelo leachii, is a large species of kingfisher native to northern Australia and southern New Guinea.

Measuring around 40 cm (16 in), it is slightly smaller than the more familiar Laughing Kookaburra. It has cream-coloured upper- and underparts barred with brownish markings. It has blue wings and brown shoulders and blue rump. It is sexually dimorphic, with a blue tail in the male, and a rufous tail with blackish bars in the female.

The adult Blue-winged Kookaburra measures around 38 to 42 cm (15-17 in) in length and weighs 260 to 330 g. Compared to the related Laughing Kookaburra, it is smaller, lacks a dark mask, has more blue in the wing, and striking white eye. It has a heavier bill than its larger relative. The head and underparts are cream-coloured with brownish streaks. It is sexually dimorphic, with a blue tail in the male, and a rufous tail with blackish bars in the female. Immature birds have more prominent brown bars and marks in their plumage, giving a 'dirty' appearance, and their eyes are predominantly brown for the first two years of life.

The call has been described as a maniacal cackling or barking.

Canada - Kluane / Wrangell-St. Elias / Glacier Bay / Tatshenshini-Alsek


SPECTACLES OF NATURE
Within the borders of one of Canada's newest National Parks, Kluane, lie many of nature's more awesome spectacles. Here, like a giant white highway from the stars. Kaskawulsh Glacier creeps slowly down through the mountain range. In the background is Mt. Logan, at 19,850 ft. Canada's highest.

Sent by Renee, a postcrosser from USA.

A unique area with high mountain peaks, foothills, glacial systems, lakes, streams, valleys and coastal landscapes. The Wrangell-St Elias region represents the most extensive array of glaciers and ice fields outside the polar region. These features and the high mountains of the Wrangell-St Elias, Chugach and Kluane ranges have resulted in the region becoming known as the 'Mountain Kingdom' of North America. Geologically the mountains are included in the Pacific mountain system and include the 130 km long Bagley ice field, the second-highest peak in the USA (Mount St Elias) and the largest piedmont glacier on the North American continent (Malaspina Glacier). Extensive lowlands are found only in the centre and along north-western fringes of the region. Elsewhere lowlands are sandwiched between mountains and sea or occur as narrow valleys and plateaux grading into upland and serrated peaks. Principal drainages include the Copper, Chitina, White, Alsek and Donjek rivers and tributaries. The Malaspina foreland coastal area comprises mainly long, straight piedmont glacial beaches cut through by numerous often sizeable glacial-melt drainage-ways.

The wide ranges of climatic zones and elevations in the region have resulted in a great variety of ecosystems representing three major biomes or broad vegetational subdivisions: the coastal coniferous biome; the northern coniferous biome; and the alpine tundra biome. The coastal coniferous biome includes coastal spruce-hemlock forests, tall shrub thickets and bogs and marshes.
The northern coniferous biome includes closed tall spruce and deciduous forests, open, low mixed evergreen and deciduous forests, tall shrub thickets and low shrub thickets.
The alpine tundra biome includes moist sedge and grass alpine tundra and dry alpine tundra: moist sedge and grass alpine tundra at 900-1,500 m on gradual slopes, meadow-like tundra composed of sedges and grasses interspersed with low shrubs such as blueberry and Labrador tea; and dry alpine tundra, on steeper mountain slopes and exposed ridges from 900 m to the elevation of perpetual ice and snow comprising low, matted alpine plants dominated by mountain avens.
There is a great variety of fauna reflecting the habitat diversity. Carnivores include coyote, grey wolf, red fox, short-tailed weasel, mink, wolverine, river otter, lynx and the more easily visible brown bear and black bear. A rare bluish colour phase of the black bear, known locally as the glacier bear, is centred in the vicinity of Yakutat. Other mammals include pica and snowshoe hare, arctic ground squirrel, beaver Castor, muskrat and porcupine. Rodents include the hoary marmot. Moose and caribou range in lower elevations and mountain goat and Dally sheep occupy high mountainous areas. Bison were introduced in 1950 and again in 1962. Black-tailed deer may occur along coastal fringes.
The avifauna includes spruce grouse, ruffed grouse, willow ptarmigan, rock ptarmigan, white-tailed ptarmigan, trumpeter swan and many song birds.
All five species of Alaskan Pacific salmon including red salmon, chum, silver salmon, pink salmon and king salmon spawn in park or preserve waters. Freshwater fish species include Dolly Virden, lake trout, steelhead, cutthroat trout, arctic grayling, turbot, round whitefish and humpback whitefish. (Source)


Canada - British Columbia - Marble Canyon Kootenay National Park


CANADA
Marble Canyon Kootenay National Park

Sent by Gail, a postcrosser from Canada.

This is from Wikipedia : Marble Canyon is a small canyon in the south-central Interior of British Columbia, Canada a few kilometres east of the Fraser River and the community of Pavilion, British Columbia, approximately midway between the towns of Lillooet and Cache Creek. A collapsed karst formation, the canyon's name comes from the brilliant limestone of its walls. Despite the name, however, the bedrock is microcrystalline limestone (sedimentary rock) rather than marble (metamorphic rock). The north wall is over 965m (3150') high above Pavilion Lake and is the southernmost extent of the Marble Range; the south wall is c. 515m (1500') and is the northern extremity of the Clear Range. Higher peaks lie in behind the walls, increasing the depth if measured from their summits.

Australia - Sydney's Centrepoint Tower


New South Wales/Sydney's Centrepoint Tower.

Sent by Sara, a postcrosser from Australia.

This is from Wikipedia : Sydney Tower (also known as the AMP Tower, AMP Centrepoint Tower, Centrepoint Tower or just Centrepoint) is Sydney's tallest free-standing structure, and the second tallest in Australia (with the Q1 building on the Gold Coast being the tallest). It is also the second tallest observation tower in the Southern Hemisphere (after Auckland's Sky Tower, though Sydney Tower's main observation deck is almost 50 m (164 ft) higher than that of Auckland's Sky Tower). The Sydney Tower is a member of the World Federation of Great Towers.

The tower stands 309 m (1,014 ft) above the Sydney CBD, being located at 100 Market Street, between Pitt and Castlereagh Streets. It is accessible from the Pitt Street Mall, and sits upon Centrepoint (to which the tower is often referred), an office and shopping centre development. The tower is open to the public, and is one of the most prominent tourist attractions in the city, being visible from a number of vantage points throughout town and from adjoining suburbs.

While AMP managed the Centrepoint shopping centre, the tower was officially referred to as "AMP Tower". After the Westfield Group took over ownership of Centrepoint in December 2001, the name was changed to Sydney Tower. Locals almost always refer to it as Centrepoint Tower.

Whilst the Shopping centre at the base of the Tower is run by the Westfield Group the tower itself is part of the Village Roadshow Theme Parks Group. Visitors can buy a pass from Village or at the gate that allows them a visit all of the Sydney attractions under the Village Roadshow Banner (Sydney Tower, Wildlife World and The Sydney Aquarium).

Czech Republic - Mapcard


A mapcard of Czech Republic.

Sent by Julic, a postcrosser from Czech Republic.

Monday, May 16, 2011

USA - Virginia - State Flower


VIRGINIA
Dogwood - State Flower

The American dogwood is well distributed throughout the Commonwealth, and its beauty is symbolic of the many attractive features of Virginia, thus it was chosen as the official state flower. The dogwood blooms in early spring and its blossom is a tiny cluster of flowers surrounded by four white leaves that look like petals. No tree says "Southern" better than the flowering dogwood.

Sent by Mads, a postcrosser from Washinton D.C., USA.

This is from Wikipedia : Cornus florida (Flowering Dogwood, syn. Benthamidia florida (L.) Spach) is a species of dogwood native to eastern North America, from southern Maine west to southern Ontario and eastern Kansas, and south to northern Florida and eastern Texas and also in Illinois, with a disjunct population in eastern Mexico in Nuevo León and Veracruz.

Flowering dogwood is a small deciduous tree growing to 10 m (33 ft) high, often wider than it is tall when mature, with a trunk diameter of up to 30 cm (1 ft). A 10-year-old tree will stand about 5 m (16 ft) tall. The leaves are opposite, simple, ovate, 6–13 cm long and 4–6 cm broad, with an apparently entire margin (actually very finely toothed, under a lens); they turn a rich red-brown in fall.

The flowers are individually small and inconspicuous, with four greenish-yellow petals 4 mm long. Around 20 flowers are produced in a dense, rounded, umbel-shaped inflorescence, or flower-head, 1–2 cm in diameter. The flower-head is surrounded by four conspicuous large white, pink or red "petals" (actually bracts), each bract 3 cm long and 2.5 cm broad, rounded, and often with a distinct notch at the apex. The flowers are bisexual.

While most of the wild trees have white bracts, some selected cultivars of this tree also have pink bracts, some even almost a true red. They typically flower in early April in the southern part of their range, to late April or early May in northern and high altitude areas. The similar Kousa Dogwood (Cornus kousa), native to Asia, flowers about a month later.

The fruit is a cluster of two to ten drupes, each 10–15 mm long and about 8 mm wide, which ripen in the late summer and the early fall to a bright red, or occasionally yellow with a rosy blush. They are an important food source for dozens of species of birds, which then distribute the seeds.

Austria - Hallstatt-Dachstein/Salzkammergut Cultural Landscape (1)


Hallstatt-Dachstein/Salzkammergut Cultural Landscape, a UNESCO World Heritage Site.

Sent by Julia, a postcrosser from Austria.

This is from UNESCO : The Hallstatt-Dachstein/Salzkammergut Alpine region is an outstanding example of a natural landscape of great beauty. It also has great scientific interest because it contains evidence of a fundamental human economic activity, the production of salt.

Human activity in the magnificent natural landscape of the Salzkammergut began in prehistoric times, with the salt deposits being exploited as early as the 2nd millennium BC. The name of the medieval town, derived from the West German hal (salt) and the Old High German stat (settlement), first recorded in a deed of 1305, testifies to its primary function. This resource formed the basis of the area's prosperity until the mid-20th century, a prosperity that is reflected in the fine architecture of the town of Hallstatt.

The town grew up along the narrow strip between the steep mountainside of the Salzberg and the lake, and on the Mühlbach, an artificial promontory out into the lake resulting from the dumping of mining debris over the centuries. Here in the inner market town the houses, largely late Gothic, are ranged round a triangular market square. The typical Hallstatt house is tall and narrow, making maximum use of the restricted space and the steep topography. The lower storeys are constructed in stone with barrel vaulting supporting timber-framed upper storeys, as is customary in the Alpine region. Only a few preserve the original flat saddleback roofs covered with wooden planks or shingles. The southern part of the town, known as In der Lahn, located at the mouth of the Echterntal, is largely of 18th-century date, much of it built after the 1750 fire.

Among the more notable buildings are the St Mary's Roman Catholic Parish Church built in the late 15th century to replace an earlier Romanesque structure, parts of which survive. Having suffered only slight damage during the 1750 fire its only Baroque features are the roof and the multi-tiered spire. It contains a number of outstanding works of art, including a late Gothic altarpiece from the Astl workshop.

The small St Michael Chapel and Charnel House is a Gothic structure in the tiny graveyard immediately north of the parish church. Its basement, viewable at ground level, contains a neatly arranged assemblage of human skulls and long bones, the skulIs being marked with names and other details of the deceased.

The property also includes the Dachstein Mountains, rising to some 3,000 m, which form the highest of the karst massifs in the northern limestone Alps. They are notable for the large number of caves they contain, the longest being the Hillatzhöhle (81 km). Each cave is speleologically different, but the fact that they enjoy single management allows a range of information and experience to be made available in a coherent programme of conservation, accessibility and interpretation. The Dachstein-Rieseneishöhle is the most impressive ice cave in Austria. Some parts of the mine are now accessible to visitors, including areas made safe for displays arising from the continuing programme of archaeological investigation.

The Dachstein massif is exceptional among Alpine karstic areas for retaining its glaciation. Its landscape takes eight distinct forms: each of these zones has its own distinct climate and hence a characteristic flora and fauna.

Sunday, May 15, 2011

USA - Florida - Everglades National Park


Everglades National Park.

Sent by Ariel, a postcrosser from Miami, USA.

This is from UNESCO : Everglades National Park is situated on the southern tip of the Florida Peninsula. The park is bounded by the Gulf of Mexico to the west, the Tamiami Trail and mostly state lands to the north and the Florida Keys to the south and south-east. It includes most of Florida Bay. The biosphere reserve includes Dry Tortugas National Park, a group of seven coral reefs and surrounding shoals, coral reefs and waters.

Everglades National Park is a shallow basin tilted to the south-west and underlain by extensive Pleistocene limestone with oolitic and bryozoan facies. The park serves as a vital recharge area for the Biscayne Aquifer, a major source of freshwater for Miami and south-east Florida. It lies at the interface between temperate and subtropical America and between fresh and brackish water, shallow bays and deeper coastal waters, thus creating a complex of habitats supporting a high diversity of flora and fauna. The area of transition from freshwater (glades) to saltwater (mangrove) is a highly productive zone that incubates great numbers of economically valuable crustacea. The vegetation and flora of south Florida have fascinated scientists and naturalists since their discovery and were a primary reason for the establishment of the park. One cause of this fascination is the presence of a high percentage of West Indian species. A noteworthy feature is the rather high degree of local endemism. Hammocks or tree islands are dominated by hardwood species of both tropical and temperate affinities. The most important trees are mangroves, taxa, slash pine and cypress. Prairies can be dominated by sawgrass, muhley grass, or cordgrass in coastal areas.

The Everglades protect 800 species of land and water vertebrates, including over 14 threatened species, and 25 mammals, over 400 bird species, 60 known species of reptile, amphibian and insect, including two threatened swallowtail butterfly species. Over 20 species of snake have been recorded, including the threatened indigo snake. More than 275 species of fish are known from the Everglades, most inhabiting the marine and estuarine waters. Several species are important game species that attract thousands of anglers to the park. During autumn a continuous procession of songbirds and other migrants fly over or rest on these islands.

The park is rich in both prehistoric and historic heritage: it contains 200 known archaeological sites. A Native American group, the Miccosukee tribe of Florida, has a special use permit area inside the park. Fort Jefferson, in Dry Tortugas National Park, is the largest brick masonry fort in America. It was large enough to garrison 1,500 men, but was never involved in battle, although it did secure a post for Union forces during the Civil War and afterwards served as a prison. The park's northern boundary is retained by the Miccosukee Indians under a special use permit for community development.

China - Imperial Palaces of the Ming and Qing Dynasties in Beijing and Shenyang


Interior of Imperial Palace.

Sent by Sun, a postcrosser from Beijing, China.

The Imperial Palaces bear exceptional testimony to Chinese civilization, being true reserves of landscapes, architecture, furnishings and objects of art, as well as containing exceptional evidence to the living traditions and the customs of shamanism practised by the Manchu people for centuries. They illustrate the grandeur of the imperial institution from the Qing dynasty to the earlier Ming and Yuan dynasties, as well as Manchu traditions, and present evidence on the evolution of this architecture in the 17th and 18th centuries.

Lying at the centre of Beijing to the north of Tiananmen Square, the Forbidden City was the Imperial Palace during the Ming and Qing dynasties. Now known as the Palace Museum, it is rectangular in shape and is the world's largest palace complex, covering 74 ha. The curtain wall has a gate on each side and there are towers at each of the four corners, affording views over both the palace and the city outside.
The Forbidden City is an extremely formal place: it is almost symmetrical and hierarchically arranged so that all the important buildings run down the centre, north-south. The Hall of Supreme Harmony, the Hall of Central Harmony and the Hall of Preserving Harmony, which comprise the outer palace where the Emperor exercised his supreme power over the nation, and the Hall of Heavenly Purity, the Hall of Union and the Hall of Earthly Tranquillity, comprising the inner palace where the imperial family lived, stand in a line from south to north on the central axis. In keeping with geomancy, the main gate is in the south and the northern side is 'protected' by the artificial Coal Hill. The buildings of the Forbidden City fully embody the artistic features and style of ancient Chinese palace architecture, and can be called a masterpiece in Chinese, even world, architectural history.
In 1406 the Ming dynasty Emperor Zhu Di ordered the construction of an imperial palace: its construction began in 1407 and was completed in 1420. The stone needed was quarried from Fangshan, a suburb of Beijing: for 20,000 peasants to be able to move an enormous stone cylinder in winter, engineers created a huge ice path by pouring liquid water on the frozen soil, and thousands of horses pulled the stone across the ice to the centre of Beijing. Wood was even more difficult to move. Giant trees in Sichuan province were felled for the main halls, but it was found that they were too large to move. Workers had to wait until torrential rains washed the logs into rivers, where boatmen steered them into the Grand Canal, from where they were floated north to Beijing and towed into the palace grounds.
The Imperial Palace of the Qing dynasty in Shenyang consists of 114 buildings; it contains an important library and testifies to the foundation of the last dynasty that ruled China, before it expanded its power to the centre of the country and moved the capital to Beijing. This palace then became auxiliary to the Imperial Palace in Beijing. This remarkable architectural edifice offers important historical testimony to the history of the Qing dynasty and to the cultural traditions of the Manchu and other tribes in the north of China.
Work began on building the palace in 1625 and it was completed in 1636. Although considered to be a miniature of the Forbidden City in Beijing, the Shenyang Palace by comparison is smaller in scale. The Manchurian influence behind its construction also shows a departure in style from its predecessor. The main architecture on the central axis is the Chong Zheng Dian, where the Emperoro attended to his political affairs (this is where Juchen was renamed Manchu). Behind are Feng Huang Lou (Phoenix Tower) and Qing Ning Gong (Palace of Celestial Peace) in which he and his concubines lived. Da Zheng Dian (Hall of Great Affairs) is the main building on the east axis. In front of the hall there are eight pavilions where the Manchurian tribal lords gathered to discuss state affairs and for other important ceremonies. (Source)


Saturday, May 14, 2011

Canada - Alberta - Edmonton


Edmonton has a northern continental climate with extreme seasonal temperatures. It has mild summers and chilly winters, withe the average daily temperatures ranging from -11.7°C (10.9°F) in January to 17.5°C (63.5°F) in July. Annually, temperatures exceed 30°C (86°F) on an average of three days and fall below -20°C (-4°F) on an average of twenty-eight days.

Sent by Cassandra, a postcrosser from Canada.

This is from Wikipedia : Edmonton ( /ˈɛdməntən/) is the capital of the Canadian province of Alberta and is the province's second-largest city. Edmonton is located on the North Saskatchewan River and is the centre of the Edmonton Capital Region, which is surrounded by the central region of the province.

The city and its census metropolitan area had populations of 730,372 and 1,034,945 as of the 2006 Census respectively, making it the northernmost North American city with a metropolitan population over one million. The city's 2009 civic census showed a population of 782,439, while Statistics Canada estimated its metropolitan population at 1,155,383 in 2009, making it the sixth-largest metropolitan area in the nation. A resident of Edmonton is known as an Edmontonian.

The majority of Edmonton's metropolitan population lives within the City of Edmonton rather than in the surrounding suburban municipalities. Historically Edmonton was surrounded by few other urban municipalities and many of the nearby settlements that did exist were absorbed through amalgamation or annexation. Edmonton annexed a significant amount of land up until the early 1980s, and as such it has sustained much of the region's suburban growth within the city.

Edmonton serves as the northern anchor of the Calgary–Edmonton Corridor and is a staging point for large-scale oil sands projects occurring in northern Alberta and large-scale diamond mining operations in the Northwest Territories.

Edmonton is a cultural, governmental and educational centre. It plays host to a year-round slate of world-class festivals, earning it the title of "The Festival City." It is home to North America's largest mall, West Edmonton Mall (the world's largest mall from 1981 until 2004), and Fort Edmonton Park, Canada's largest living history museum. In 2004, Edmonton celebrated the centennial of its incorporation as a city.

France - Breton's Costume


Boy wearing the Breton costume.

Sent by Stef, a postcrosser from France.

Wednesday, May 11, 2011

United Arab Emirates - Burj Khalifa


Burj Khalifa or Khalifa Tower.

Sent by Salah from United Arab Emirates.

This is from Wikipedia : Burj Khalifa (Arabic: برج خليفة‎ "Khalifa Tower"),[8] known as Burj Dubai prior to its inauguration, is a skyscraper in Dubai, United Arab Emirates, and is currently the tallest man-made structure ever built, at 828 m (2,717 ft). Construction began on 21 September 2004, with the exterior of the structure completed on 1 October 2009. The building officially opened on 4 January 2010, and is part of the new 2 km2 (490-acre) flagship development called Downtown Dubai at the 'First Interchange' along Sheikh Zayed Road, near Dubai's main business district.

The tower's architecture and engineering were performed by Skidmore, Owings and Merrill of Chicago, with Adrian Smith as chief architect, and Bill Baker as chief structural engineer. The primary contractor was Samsung C&T of South Korea.

The total cost for the project was about US $1.5 billion; and for the entire "Downtown Dubai" development, US $20 billion. In March 2009, Mohamed Ali Alabbar, chairman of the project's developer, Emaar Properties, said office space pricing at Burj Khalifa reached US $4,000 per sq ft (over US $43,000 per m²) and the Armani Residences, also in Burj Khalifa, sold for US $3,500 per sq ft (over US $37,500 per m²).

The project's completion coincided with the global financial crisis of 2007–2010, and with vast overbuilding in the country, led to high vacancies and foreclosures. With Dubai mired in debt from its huge ambitions, the government was forced to seek multibillion dollar bailouts from its oil rich neighbor Abu Dhabi. Subsequently, in a surprise move at its opening ceremony, the tower was renamed Burj Khalifa, said to honour the UAE President Khalifa bin Zayed Al Nahyan for his crucial support.

Due to the slumping demand in Dubai's property market, the rents in the Burj Khalifa plummeted 40% some ten months after its opening. Out of 900 apartments in the tower around 825 were still empty at that time.

USA - North Dakota - State Bird


The Western Meadow Lark was adopted as the official bird of the State of North Dakota on March 10, 1947.

Sent by Hazel from North Dakota, USA.

This is from Wikipedia : The Western Meadowlark (Sturnella neglecta) is a medium-sized icterid bird, about 8.5 in (21.6 cm) long. It nests on the ground in open country in western and central North America. It feeds mostly on insects, but also seeds and berries. It has distinctive calls described as watery or flute-like, which distinguish it from the closely related Eastern Meadowlark.

Adults have yellow underparts, with a black "V" on the breast, and white flanks which are streaked with black. Their upper parts are mostly brown, but also have black streaks. These birds have long pointed bills and their heads are striped with light brown and black.

Their breeding habitats are grasslands, prairies, pastures, and abandoned fields, all of which may be found from across western and central North America to northern Mexico. Where their range overlaps with the eastern species, these birds prefer thinner, drier vegetation; the two types of birds generally do not interbreed but do defend territory against one another. Their nests are situated on the ground, and are covered with a roof woven from grass. There may be more than one nesting female in a male's territory. Their nests are sometimes destroyed by mowing operations with eggs and young in them.

Western Meadowlarks will interbreed with Eastern Meadowlarks where their ranges overlap; however, resulting young appear to have low fertility.

Western Meadowlarks are permanent residents throughout much of their range. Northern birds may migrate to the southern parts of their range; some birds also move east in the southern United States.

These birds forage on the ground or in low to semi-low vegetation. They sometimes search for food by probing with their bills. They mainly eat insects, although they will devour seeds and berries. In winter, these birds often feed in flocks.

These birds have a flute-like warbled song. These calls contrast with the simple, whistled call of the Eastern Meadowlark.

These two species were considered to be the same species for some time; the western species, having been overlooked for some time, was given the species name neglecta.

This is the state bird of Kansas, Montana, Nebraska, North Dakota, Oregon and Wyoming. Only the Northern Cardinal is the state bird of more states.

USA - Minnesota - State Flower & State Bird


MINNESOTA
State Bird : Common Loon
State Flowers : Showy Lady's Slipper

Sent by Nadezhda, a postcrosser from Belarus.

Canada - Alberta


Home in the foothills. Alberta, Canada.

Sent by Garnet, a postcrosser from Canada.

Alberta /ælˈbɜrtə/ is a province of Canada. It had a population of 3,645,257 in 2011, making it the most populous of Canada's three prairie provinces. Alberta and its neighbour, Saskatchewan, were established as provinces on September 1, 1905.
Alberta is located in western Canada, bounded by the provinces of British Columbia to the west and Saskatchewan to the east, the Northwest Territories to the north, and the U.S. state of Montana to the south. Alberta is one of three Canadian provinces and territories to border only a single U.S. state and is also one of only two provinces that are landlocked.
Edmonton, the capital city of Alberta, is located near the geographic centre of the province and is the primary supply and service hub for Canada's oil sands and other northern resource industries. Approximately 290 km (180 mi) south of the capital is Calgary, Alberta's largest city and a major distribution and transportation hub. Calgary and Edmonton centre Alberta's two census metropolitan areas, both of which have populations exceeding 1 million, while the province has 16 census agglomerations. Notable tourist destinations in the province include BanffCanmoreDrumhellerJasper and Sylvan Lake.
The current Premier of the province is Alison Redford. (Source)

Monday, May 9, 2011

Malaysia - Johor - Masjid Jamek Muar


Masid Jamek Muar; 2004; Acrylic; 105cm x 90cm; Artist - Muhammad Alif @ Hud Hassan.

Sent by Aameea from Johor Bahru, Johor.

OFFICIAL WEBSITE OF MASJID JAMEK MUAR (IN BAHASA MELAYU)