Everglades National Park

Everglades National Park

Everglades National Park is a U.S. National Park in Florida that protects the southern 20 percent of the original Everglades. In the United States, it is the largest tropical wilderness, the largest wilderness of any kind east of the Mississippi River, and is visited on average by one million people each year. It is the third-largest national park in the lower 48 states after Death Valley and Yellowstone. It has been declared an International Biosphere Reserve, a World Heritage Site, and a Wetland of International Importance, one of only three locations in the world to appear on all three lists.

Everglades National Park

Although most U.S. national parks preserve unique geographic features, Everglades National Park was the first created to protect a fragile ecosystem. The Everglades are a network of wetlands and forests fed by a river flowing .25 miles (0.40 km) per day out of Lake Okeechobee, southwest into Florida Bay. The Park is the most significant breeding ground for tropical wading birds in North America, contains the largest mangrove ecosystem in the western hemisphere, is home to 36 threatened or protected species including the Florida panther, the American crocodile, and the West Indian manatee, and supports 350 species of birds, 300 species of fresh and saltwater fish, 40 species of mammals, and 50 species of reptiles. The majority of South Florida's fresh water, which is stored in the Biscayne Aquifer, is recharged in the park.

Humans have lived for thousands of years in or around the Everglades, until plans arose in 1882 to drain the wetlands and develop the recovered land for agricultural and residential use. As the 20th century progressed, water flow from Lake Okeechobee was increasingly controlled and diverted to enable explosive growth of the South Florida metropolitan area. The park was established in 1934 to protect the quickly vanishing Everglades, and dedicated in 1947 as massive canal building projects were initiated across South Florida. The ecosystems in Everglades National Park have suffered significantly from human activity, and restoration of the Everglades is a politically charged issue in South Florida.

Climate

Everglades National Park has a tropical savanna climate and tropical monsoon climate, depending on location. Most of the central region has a savanna climate while regions closer to shore, especially the eastern quarter of the park has a monsoonal climate. Both climates are characterized by two seasons: wet and dry. The park's dry season lasts from December to April, when temperatures vary from 53 °F (12 °C) to 77 °F (25 °C) and humidity is low. Since water levels are low at that time, animals congregate at central water locations, providing popular opportunities for viewing the wildlife. During the wet season, from May to November, temperatures are consistently above 90 °F (33 °C) and humidity over 90 percent. Storms can drop 10 to 300 mm of rain at a time, providing half the year's average of 60 inches of rainfall in just two months.

Ecosystems

At the turn of the 20th century common concepts of what should be protected in national parks invariably included formidable geologic features like mountains, geysers, or canyons. As Florida's population began to grow significantly and urban areas near the Everglades were developed, proponents of the park's establishment faced difficulty in persuading the federal government and the people of Florida that the subtle and constantly shifting ecosystems in the Everglades were just as worthy of protection. When the park was established in 1947, it became the first area within the U.S. to protect flora and fauna native to a region as opposed to geologic scenery. The National Park Service recognizes nine distinct interdependent ecosystems within the park that constantly shift in size owing to the amount of water present and other environmental factors.

Freshwater sloughs and marl prairies

Freshwater marl prairies are similar to sloughs, but lack the slow movement of surface water; instead, water seeps through a calcitic mud called marl. Algae and other microscopic organisms form periphyton, which attaches to limestone. When it dries it turns into a gray mud. Sawgrass and other water plants grow shorter in freshwater marl than they do in peat, the other type of soil in the Everglades which is found where water remains present longer throughout the year. Marl prairies are usually under water from three to seven months of the year, whereas sloughs may remain submerged for longer than nine months and sometimes remain under water from one year to the next. Sawgrass may dominate sloughs, creating a monoculture. Other grasses, such as muhly grass (Muhlenbergia filipes) and broad-leafed water plants can be found in marl prairies. Animals living in the freshwater sloughs also inhabit in marl prairies. Marl prairies may go dry in some parts of the year; alligators play a vital role in maintaining life in remote parts of the Everglades by burrowing in the mud during the dry season, creating pools of water where fish and amphibians survive from one year to the next. Alligator holes also attract other animals who congregate to feed on smaller prey. When the region floods again during the wet season, the fish and amphibians who were sustained in the alligator holes then repopulate freshwater marl prairies.

Endangered and threatened animals

The American crocodile has notable differences from the alligator. Habitat destruction and vehicle collisions are some of the largest threats it experiences.

Thirty-six federally protected animals live in the park, some of which face grave threats to their survival.

In the United States, the American crocodile's only habitat is within South Florida. They were once overhunted for their hides. They are protected today from hunting, but are still threatened due to habitat destruction and injury from vehicle collisions when crossing roads to reach waterways. About 1,000 crocodiles live in Florida and there are roughly 50 nests in the Everglades and Biscayne National Parks. Crocodiles populations in South Florida have increased as has the number of alligators. Crocodiles were reclassified from "endangered" to "threatened" in the United States in 2007. The Florida panther is one of the most endangered mammals on earth. About 50 live in the wild, primarily in the Everglades and the Big Cypress Swamp. The biggest threats to the panther include habitat destruction from human development, vehicle collisions, inbreeding due to their limited gene pool, parasites, diseases, and mercury poisoning.

Four Everglade species of sea turtle including the Atlantic green sea turtle, the Atlantic hawksbill, the Atlantic loggerhead (Caretta caretta), and the Atlantic ridley (Lepidochelys kempii) are endangered. Also, the leatherback sea turtle (Dermochelys coriacea) is threatened. Numbers are difficult to determine, since males and juveniles do not return to their birthplace, although females lay eggs in the same location every year. Habitat loss and illegal poaching and destructive fishing practices are the biggest threats to these animals.

Two species of birds in the park are in danger of disappearing. The range of the Cape Sable seaside sparrow is restricted to Everglades National Park and the Big Cypress Swamp. In 1981 6,656 Cape Sable seaside sparrows were reported in park boundaries, but surveys over 10 years documented a decline to an estimated 2,624 birds by 2002. Attempts to return natural levels of water to the park have been controversial; Cape Sable seaside sparrows nest about a foot off the ground, and rising water levels may harm future populations, as well as threaten the endangered snail kite. The Everglades snail kite eats apple snails almost exclusively, and the Everglades is the only location in the United States where this bird of prey exists. There is some evidence that the population may be increasing, but loss of habitat and food sources keep the estimated number of these birds at several hundred.

Read More

Chaco Culture National Historical Park

Chaco Culture National Historical Park

Chaco Culture National Historical Park

Chaco Culture National Historical Park is a United States National Historical Park hosting the densest and most exceptional concentration of pueblos in the American Southwest. The park is located in northwestern New Mexico, between Albuquerque and Farmington, in a remote canyon cut by the Chaco Wash. Containing the most sweeping collection of ancient ruins north of Mexico, the park preserves one of the United States' most important pre-Columbian cultural and historical areas.

Between AD 900 and 1150, Chaco Canyon was a major center of culture for the Ancient Pueblo Peoples. Chacoans quarried sandstone blocks and hauled timber from great distances, assembling fifteen major complexes that remained the largest buildings in North America until the 19th century. Evidence of archaeoastronomy at Chaco has been proposed, with the "Sun Dagger" petroglyph at Fajada Butte a popular example. Many Chacoan buildings may have been aligned to capture the solar and lunar cycles, requiring generations of astronomical observations and centuries of skillfully coordinated construction. 

Geology

After the Pangaean supercontinent sundered during the Cretaceous period, the region became part of a shifting transition zone between a shallow inland sea—the Western Interior Seaway—and a band of plains and low hills to the west. A sandy and swampy coastline oscillated east and west, alternately submerging and uncovering the area atop the present Colorado Plateau that Chaco Canyon now occupies. The Chaco Wash flowed across the upper strata of what is now the 400-foot (120 m) Chacra Mesa, cutting into it and gouging out a broad canyon over the course of millions of years. The mesa comprises sandstone and shale formations dating from the Late Cretaceous, which are of the Mesa Verde formation. The canyon bottomlands were further eroded, exposing Menefee Shale bedrock; this was subsequently buried under roughly 125 feet (38 m) of sediment. The canyon and mesa lie within the "Chaco Core"—which is distinct from the wider Chaco Plateau, a flat region of grassland with infrequent stands of timber. As the Continental Divide is only 15.5 miles (25 km) east of the canyon, geological characteristics and different patterns of drainage differentiate these two regions both from each other and from the nearby Chaco Slope, the Gobernador Slope, and the Chuska Valley.

Climate

An arid region of high xeric scrubland and desert steppe, the canyon and wider basin average 8 inches of rainfall annually; the park averages 9.1 inches. Chaco Canyon lies on the leeward side of extensive mountain ranges to the south and west, resulting in a rainshadow effect that fosters the prevailing lack of moisture in the region. The region sees four distinct seasons. Rainfall is most likely between July and September, while May and June are the driest months. Orographic precipitation, which results from moisture wrung out of storm systems ascending the mountain ranges around Chaco Canyon, is responsible for most of the summer and winter precipitation, and rainfall increases with higher elevation. Occasional aberrant northward excursions of the intertropical convergence zone may boost precipitation in some years.

Chaco endures remarkable climatic extremes: temperatures range between -38 to 102 °F (-39 to 39 °C), and may swing 60 °F (33 °C) in a single day. The region averages fewer than 150 frost-free days per year, and the local climate swings wildly from years of plentiful rainfall to prolonged drought. The heavy influence of the El Niño-Southern Oscillation contributes to the canyon's fickle climate.

Flora and fauna

Chacoan flora typifies that of North American high deserts: sagebrush and several species of cactus are interspersed with dry scrub forests of piñon and juniper, the latter primarily on the mesa tops. The canyon is far drier than other parts of New Mexico located at similar latitudes and elevations, and it lacks the temperate coniferous forests plentiful to the east. The prevailing sparseness of plants and wildlife was echoed in ancient times, when overpopulation, expanding cultivation, overhunting, habitat destruction, and drought may have led the Chacoans to strip the canyon of wild plants and game. It has been suggested that even during wet periods the canyon was able to sustain only 2,000 people.

Among Chacoan mammals are the plentiful coyote (Canis latrans); mule deer, elk, and pronghorn also live within the canyon, though they are rarely encountered by visitors. Important smaller carnivores include bobcats, badgers, foxes, and two species of skunk. The park hosts abundant populations of rodents, including several prairie dog towns. Small colonies of bats, are present during the summer. The local shortage of water means that relatively few bird species are present; these include roadrunners, large hawks (such as Cooper's hawks and American kestrels), owls, vultures, and ravens, though they are less abundant in the canyon than in the wetter mountain ranges to the east. Sizeable populations of smaller birds, including warblers, sparrows, and house finches, are also common. Three species of hummingbirds are present: one is the tiny but highly pugnacious rufous hummingbird, which compete intensely with the more mild-tempered black-chinned hummingbirds for breeding habitat in shrubs or trees located near water. Western rattlesnakes are occasionally seen in the backcountry, though various lizards and skinks are far more abundant.

Read More

Biscayne National Park

Biscayne National Park

Biscayne National Park is a U.S. National Park located in southern Florida, south of Miami. The park preserves Biscayne Bay and its offshore barrier reefs. Ninety-five percent of the park is water, and the shore of the bay is the location of an extensive mangrove forest. The park covers 172,971 acres (69,999 ha) and includes Elliott Key, the park's largest island and first of the true Florida Keys, formed from fossilized coral reef. The islands farther north in the park are transitional islands of coral and sand. The offshore portion of the park includes the northernmost region of the Florida Reef, one of the largest coral reefs in the world. Biscayne National Park protects four distinct ecosystems: the shoreline mangrove swamp, the shallow waters of Biscayne Bay, the coral limestone keys and the offshore Florida Reef. The shoreline swamps of the mainland and island margins provide a nursery for larval and juvenile fish, molluscs and crustaceans. The bay waters harbor immature and adult fish, seagrass beds, sponges, soft corals, and manatees. The keys are covered with tropical vegetation including endangered cacti and palms, and their beaches provide nesting grounds for endangered sea turtles. Offshore reefs and waters harbor more than 200 species of fish, pelagic birds, whales and hard corals. Sixteen endangered species including Schaus' swallowtail butterflies, smalltooth sawfish, manatees, and green and hawksbill sea turtles may be observed in the park. Biscayne also has a small population of threatened American crocodiles and a few American alligators.

The people of the Glades culture inhabited the Biscayne Bay region as early as 10,000 years ago before rising sea levels filled the bay. The Tequesta people occupied the islands and shoreline from about 4,000 years before the present to the 16th century, when the Spanish took possession of Florida. Reefs claimed ships from Spanish times through the 20th century, with more than 40 documented wrecks within the park's boundaries. While the park's islands were farmed during the 19th and early 20th centuries, their rocky soil and periodic hurricanes made agriculture difficult to sustain. In the early 20th century the islands became secluded destinations for wealthy Miamians who built getaway homes and social clubs. Mark C. Honeywell's guesthouse on Boca Chita Key was the area's most elaborate private retreat, featuring a mock lighthouse. The Cocolobo Cay Club was at various times owned by Miami developer Carl G. Fisher, yachtsman Garfield Wood, and President Richard Nixon's friend Bebe Rebozo, and was visited by four United States presidents. The amphibious community of Stiltsville was established in the 1930s in the shoals of northern Biscayne Bay, taking advantage of its remoteness from land to offer offshore gambling and alcohol during Prohibition. Following the Cuban Revolution of 1959, Elliott Key was used as a training ground for infiltrators into Fidel Castro's Cuba by the Central Intelligence Agency and by Cuban exile groups.

Originally proposed for inclusion in Everglades National Park, Biscayne Bay was cut from the proposed park to ensure Everglades' establishment. It remained undeveloped until the 1960s, when a series of proposals were made to develop the keys in the manner of Miami Beach, and to construct a deepwater seaport for bulk cargo, along with refinery and petrochemical facilities on the mainland shore of Biscayne Bay. Through the 1960s and 1970s, two fossil-fueled power plants and two nuclear power plants were built on the bay shores. A backlash against development led to the 1968 designation of Biscayne National Monument. The preserved area was expanded by its 1980 re-designation as Biscayne National Park. The park is heavily used by boaters, and apart from the park's visitor center on the mainland, its land and sea areas are accessible only by boat.

Climate

Biscayne's tropical climate reflects its location in extreme South Florida. Southern Miami-Dade County is classified as tropical savanna in the Köppen-Geiger system. Seasons may be divided into the November–April dry season and the May–October wet season. Dry season temperatures average between 66 and 76 °F (19 and 24 °C) with an average monthly rainfall of 2.1 inches (53 mm). Wet season temperatures average between 76 and 85 °F (24 and 29 °C) with an average monthly rainfall of 5.39 inches (137 mm). The wet season roughly coincides with hurricane season, with frequent thunderstorms. 

Like many locations in southern Florida, Biscayne National Park is affected by hurricanes every few years. Most storms require temporary closings and occasional repairs to park facilities. A direct hit by a powerful hurricane can produce severe consequences, primarily by its impact on human interventions in the environment rather than on the natural environment of the park, which is well-adapted to these events.  Significant hurricanes to strike Biscayne include storms in 1835 and 1904, the 1906 Florida Keys hurricane, the 1926 Miami hurricane, the 1929 Bahamas hurricane, the 1935 Labor Day hurricane, the 1935 Yankee hurricane, the 1941 Florida hurricane, the 1945 Southeast Florida hurricane, the 1948 Miami hurricane, Hurricane King in 1950, Hurricane Donna in 1960. Hurricane Cleo in 1964, and Hurricane Andrew in 1992. The park can be affected by wave action from more distant tropical storms such as 2012's Hurricane Sandy, which damaged facilities on Elliott Key.

Exploration

Juan Ponce de León explored the area in 1513, discovering the Florida Keys and encountering the Tequesta on the mainland. Other Spanish explorers arrived later in the 16th century and Florida came under Spanish rule. The Tequesta were resettled by the then-Spanish government in the Florida Keys, and the South Florida mainland was depopulated. Ponce de León referred to the bay as "Chequescha" after its inhabitants, becoming "Tequesta" by the time of Spanish governor Pedro Menéndez de Avilés later in the century. The present name has been attributed to a shipwrecked Basque sailor known as the "Biscaino" or "Viscayno" who lived in the area for a time, or to a more general allusion to the Bay of Biscay. Spanish treasure fleets regularly sailed past the Florida Keys and were often caught in hurricanes. There are 44 documented shipwrecks in the park from the 16th through the 20th centuries. At least two 18th-century Spanish ships were wrecked in the park area. The Spanish galleon Nuestra Senora del Popolo is believed to have been wrecked in park waters in 1733, though the site has not been found. HMS Fowey was wrecked in 1748 in what is now Legare Anchorage, at some distance from the Fowey Rocks. The discovery of the ship in 1975 resulted in a landmark court case that established the wreck as an archaeological site rather than a salvage site. 43 wrecks are included on the National Register of Historic Places in the Offshore Reefs Archeological District, which extends for 30 mi (48 km) along the seaward side of the Biscayne National Park keys. During the 18th century, Elliott Key was the reputed base of two different pirates, both of whom were called Black Caesar, commemorated by Caesar's Creek between Elliott and Old Rhodes Key.

Ecology

South Florida is a transitional zone between the Nearctic and Neotropical ecozones, resulting in a wide variety of plant and animal life. The intersection of ecozones brings opportunities for visitors to see species, particularly birds, that are not seen elsewhere in North America. The park includes four distinct ecosystems, each supporting its own flora and fauna. Mangrove swamp, lagoon, island key and offshore reef habitats provide diversity for many species. In this semi-tropical environment, the seasons are differentiated mainly by rainfall. Warm to hot and wet summers bring occasional tropical storms. Though only marginally cooler, the winters tend to be relatively drier. Bay salinity varies accordingly, with lower salinity levels in the wet summer, trending to more fresh water on the west side where new fresh water flows in.

Hundreds of species of fish are present in park waters, including more than fifty crustacean species ranging from isopods to giant blue land crabs, about two hundred species of birds and about 27 mammal species, both terrestrial and marine. Molluscs include a variety of bivalves, terrestrial and marine snails, sea hares, sea slugs and two cephalopods, the Caribbean reef octopus and the Caribbean reef squid.way between North American, the Caribbean islands, and South America. Many southbound land birds stop in the fall at Bill Baggs Cape Florida State Park, just north of the park on Key Biscayne, before venturing across the open waters of Biscayne Bay. Northbound spring migrants do likewise on Elliott Key. Most of the small passerine migrants are warblers, with ovenbirds, palm warblers, American redstarts, common yellowthroats, prairie warblers, worm-eating warblers and black-throated blue warblers accounting for the majority. Migrant raptors include short-tailed hawks, sharp-shinned hawks, merlins, peregrine falcons and swallow-tailed kites, while bald eagles and ospreys nest in the park. Both white-tailed and red-tailed tropicbirds are seen in the park, as are American flamingos, with some of the latter probably escaped captive birds.

Read More

Banff National Park

Banff National Park

Banff National Park is Canada's oldest national park, established in 1885 in the Rocky Mountains. The park, located 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, encompasses 6,641 square kilometres (2,564 sq mi)of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.

Banff National Park

The Canadian Pacific Railway was instrumental in Banff's early years, building the Banff Springs Hotel and Chateau Lake Louise, and attracting tourists through extensive advertising. In the early 20th century, roads were built in Banff, at times by war internees from World War I, and through Great Depression-era public works projects. Since the 1960s, park accommodations have been open all year, with annual tourism visits to Banff increasing to over 5 million in the 1990s. Millions more pass through the park on the Trans-Canada Highway. As Banff is one of the world's most visited national parks, the health of its ecosystem has been threatened. In the mid-1990s, Parks Canada responded by initiating a two-year study, which resulted in management recommendations, and new policies that aim to preserve ecological integrity.

History

Throughout its history, Banff National Park has been shaped by tension between conservation and development interests. The park was established on 25 November 1885 as Banff Hot Springs Reserve, in response to conflicting claims over who discovered hot springs there, and who had the right to develop the hot springs for commercial interests. Instead, Prime Minister John A. Macdonald set aside the hot springs as a small, protected reserve, which was later expanded to include Lake Louise and other areas extending north to the Columbia Icefield.

Archaeological evidence found at Vermilion Lakes radiocarbon dates the first human activity in Banff to 10,300 B.P. Prior to European contact, aboriginals, including the Stoneys, Kootenay, Tsuu T'ina, Kainai, Peigans, and Siksika, were common in the region where they hunted bison and other game.

With the admission of British Columbia to Canada on 20 July 1871, Canada agreed to build a transcontinental railroad. Construction of the railroad began in 1875, with Kicking Horse Pass chosen, over the more northerly Yellowhead Pass, as the route through the Canadian Rockies.Ten years later, on 7 November 1885, the last spike was driven in Craigellachie, British Columbia.

Wildlife

The park has 56 mammal species that have been recorded. Grizzly and black bears inhabit the forested regions. Cougar, lynx, wolverine, weasels, northern river otter and wolves are the primary predatory mammals. Elk, mule deer, and white-tailed deer are common in the valleys of the park, including around (and sometimes in) the Banff townsite, while moose tend to be more elusive, sticking primarily to wetland areas and near streams. In the alpine regions, mountain goats, bighorn sheep, marmots and pika are widespread. Other mammals such as beavers, porcupines, squirrels, chipmunks, and Columbian ground squirrels are the more commonly observed smaller mammals. In 2005, a total of five caribou were counted, making this species one of the rarest mammals found in the park.

Due to the harsh winters, the park has few reptiles and amphibians with only one species of toad, three species of frog, one salamander species and two species of snakes that have been identified.At least 280 species of birds can be found in Banff including bald and golden eagles, red-tailed hawk, osprey, and merlin, all of which are predatory species. Additionally, commonly seen species such as the gray jay, American three-toed woodpecker, mountain bluebird, Clark's nutcracker, mountain chickadee and pipit are frequently found in the lower elevations. The white-tailed ptarmigan is a ground bird that is often seen in the alpine zones. Rivers and lakes are frequented by over a hundred different species including loons, herons and mallards who spend their summers in the park.

Endangered species in Banff include the Banff Springs snail (Physella johnsoni) which is found in the hot springs of Banff. Woodland caribou, found in Banff, are listed as a threatened species.

Tourism

Banff National Park is the most visited Alberta tourist destination and one of the most visited national parks in North America, with 3,927,557 visitors in 2004/2005.During summer, 51 percent of park visitors are from Canada (30 percent from Alberta), while 31 percent are from the United States and 14 percent from Europe. Tourism in Banff contributes an estimated C$6 billion annually to the economy. A park pass is required for stopping in the park and permit checks are common during the summer months, especially at Lake Louise and the start of the Icefields Parkway. A permit is not required if travelling straight through the park without stopping. Approximately 5 million people pass through Banff annually on the Trans-Canada Highway without stopping.Attractions in Banff include Upper Hot Springs, and a 27-hole golf course at Fairmont Banff Springs Hotel, and three ski resorts including Sunshine Village, Lake Louise Mountain Resort, and Mount Norquay ski resort. The Banff Lodging Co is a hospitality company in the park. Day hikes, such as the Cory Pass Loop, are popular with visitors. Other activities include alpine and Nordic skiing, and horseback riding.

Backcountry activities in Banff include hiking, camping, climbing, and skiing. Parks Canada requires those using backcountry campgrounds, Alpine Club of Canada huts, or other backcountry facilities to purchase a wilderness pass. Reservations for using the campgrounds are also required.

In 2009, the Banff Lake Louise Tourism hoped the appearance of the "Crasher Squirrel" internet meme would stimulate interest in the park. The meme is based a photograph of a Minnesotan couple visiting the park on the shore of Lake Minnewanka that was "crashed" by a Columbian ground squirrel; the photograph was published in major news sources around the world and the image of the squirrel was digitally manipulated into humorous photos.

Transportation

Banff National Park is bisected by two highways that cross the Alberta/British Columbia border while another provides a third access within Alberta. The Trans-Canada Highway (Highway 1) bisects the park in an east-west direction, connecting it to Vancouver to the west and Calgary to the east. Highway 93 bisects the park in a north-south direction, connecting it to Cranbrook to the south and Jasper to the north. The portion of Highway 93 north of Lake Louise is known as the Icefields Parkway whereas the portion southwest of Castle Junction is known as the Banff-Windermere Parkway. Highway 11 (the David Thompson Highway) connects the Icefields Parkway at Saskatchewan River Crossing to Rocky Mountain House to the northeast. Within the park, Highway 1A, also known as the Bow Valley Parkway, loosely parallels Highway 1 between Banff and Lake Louise. Other transportation facilities within Banff National Park include a Canadian Pacific rail line that generally parallels Highway 1 and an airport known as the Banff Park Compound Heliport.

Read More

Bicauri National Park

Bicauri National Park

Bicauri National Park

Bicauri National Park (Portuguese: Parque Nacional do Bicuar; also called Bicuar National Park or Bikuar/Huila National Park) is a national park in Angola. It is located in the south-west region of the country on the Huila Plateau, about 120 km SE of Lubango. The park is an area of sandy hills and shrub thicket character. The climate is tropical semi-arid. Bicuar was established as a hunting reserve in 1938, and reformed as a national park in 1964. Historically known for its large mammals, such as the Black Buffalo, the park suffered heavily in the Angolan Civil War (1975-2002). During this time the animals were mostly or entirely exterminated, but the Angolan Government is now undertaking efforts to rebuild the infrastructure and resettle the animals.

Natural features

The park is bordered on the East by the Cunene River, one of the few perennial rivers in the region. The dominant vegetation is described as Angolan Miombo Woodlands and Angolan Mopane Woodlands, an area of savanna and woodlands on the plateau East of the coastal hills. Portions of the park are seasonally wet or wetland swamps and dambo grasslands.

The Bicuar stands at the northern end of a distinct ecoregion known as the Angolan Mopane Woodland. The area is known for high species richness, variable rainfall, and the importance of mopane trees to the animals and people of the region. The climate of Bicuari is described under the Köppen climate classification system as Temperate highland tropical climate with dry winters, and the warmest months temperatures averaging below 22 degC. Average rainfall is 600-800mm/year.

Animal life

The area has historically been known for large herds of common antelopes, elephants, and other large mammals. All species populations are believed to have be severely reduced the war (the park was reportedly used as a practice artillery range), poaching, and human encroachment. Since cessation of hostilities, work has begun by the Huila provincial government to rebuild the infrastructure of the park to attract and protect animals. As of 2013, it has been reported that some of the large mammals are returning to Bicuar. 

Read More

Dukhan City

Read More

Hohensalzburg Castle in Salzburg, Austria

Hohensalzburg Castle in Salzburg, Austria

Hohensalzburg Castle in Salzburg, Austria

Hohensalzburg Castle (German: Festung Hohensalzburg, literally "High Salzburg Fortress") sits atop the Festungsberg, a small hill in the Austrian city of Salzburg. Erected at the behest of the Prince-Archbishops of Salzburg with a length of 250 m (820 ft) and a width of 150 m (490 ft), it is one of the largest medieval castles in Europe. Hohensalzburg Castle is situated at an altitude of 506 m. One of the earliest depictions of the castle in the 1460s, from the Schedel'sche Weltchronik. Construction of the fortress began in 1077 under Archbishop Gebhard von Helfenstein.[2] This original design was just a basic bailey with a wooden wall. In the Holy Roman Empire, the archbishops of Salzburg were already powerful political figures and they expanded the castle to protect their interests. Gebhard's conflict with Emperor Henry IV during the Investiture Controversy influenced the expansion of the castle, with the Archbishop taking the side of Pope Gregory VII and the German anti-king Rudolf of Rheinfelden. The castle was gradually expanded during the following centuries. The ring walls and towers were built in 1462 under Prince-Archbishop Burkhard II von Weißpriach.

Prince-Archbishop Leonhard von Keutschach during his term from 1495 until 1519 further expanded the castle. His coadjutor Matthäus Lang von Wellenburg, who was later to succeed Leonhard, in 1515 wrote a description of the Reisszug, a very early and primitive funicular railway that provided freight access to the upper courtyard of the castle. The line still exists, albeit in updated form, and is probably the oldest operational railway in the world. The current external bastions, begun in the 16th century and completed in the 17th, were added as a precaution because of fears of Turkish Invasion.

The only time that the fortress actually came under siege was during the German Peasants' War in 1525, when a group of miners, farmers and townspeople tried to oust Prince-Archbishop Matthäus Lang, but failed to take the castle. In 1612 the deposed Archbishop Wolf Dietrich von Raitenau died here in prison. During the Thirty Years' War, Archbishop Count Paris of Lodron strengthened the town's defenses, including Hohensalzburg. He added various parts to the fortress, such as the gunpowder stores and additional gatehouses. The fort was surrendered without a fight to French troops under General Jean Victor Marie Moreau during the Napoleonic War of the Second Coalition in 1800 and the last Prince-Archbishop Count Hieronymus von Colloredo fled to Vienna. In the 19th century, it was used as barracks, storage depot and dungeon before being abandoned as a military outpost in 1861.

Recent history:

Hohensalzburg castle was refurbished from the late 19th century onwards and became a major tourist attraction with the Festungsbahn cable car, opened in 1892, leading up from the town to the Hasengrabenbastei. It stands today as one of the best preserved castles in Europe. During the early 20th century it was used as a prison, holding Italian prisoners of war during World War I and Nazi activists (before the Anschluss with Germany) in the 1930s. Hohensalzburg castle was recently selected as main motif for the Austrian Nonnberg Abbey commemorative coin minted on April 5, 2006. This was the first coin of the series "Great Abbeys of Austria". It shows the Benedictine convent of Nonnberg Abbey. In the hilltop on the background, the castle and the Kajetaner church can be seen. Also in 1977 the Austrian Mint issued a coin for the 900th anniversary of Hohensalzburg castle.

Salzburg Bull:

The Krautturm (powder tower) houses a large aerophon of more than 200 pipes which is called the "Salzburg Bull" (Salzburger Stier). This huge mechanical organ was built in 1502 by Archbishop Leonhard von Keutschach. It was renewed by Rochus Egedacher in 1735. From Palm Sunday to 31 October the "Salzburg Bull" is played daily at 7, 11 and 18 o'clock. The aerophone thus initiated the playing of the carillon at the Residenzplatz and ended it again. One of Austria's most famous cabaret groups is named after it.

Golden Hall:

Starting in 1498, Archbishop Leonhard von Keutschach had the magnificent state apartments installed on the third floor. The rooms in which the archbishops would normally have lived were one floor below. The state apartments were primarily used for representative purposes and for festivities. The Golden Hall was richly decorated and indicates that the fortress served the archbishops not only as a refuge in times of crisis, but frequently also as a residence up to the 16th century. In order to gain more space, Archbishop Leonhard von Keutschach had four massive marble pillars constructed on the right-hand outer wall and had a loggia added on. As in the other rooms the ceiling is coffered, each coffer being adorned with gold buttons symbolising the stars in the sky. The 17 metre long beam, supporting the ceiling, is particularly worth mentioning. The coat of arms of Leonhard von Keutschach together with those of the Holy Roman Empire, the most powerful German towns and the bishoprics that were connected to Salzburg, are painted on it.

Chapel of Archbishop Leonhard von Keutschach:

Archbishop Leonhard von Keutschach (1495-1519) had the chapel built at a later time. One of the figure consoles in the beam ceiling had to be removed to make room for it. A richly ornamented star vault decorates the ceiling of the chapel. The inner part of the door at the entrance is covered with stucco. The painted frame shows red columns on a high plinth with grey capitals. The coat of arms of Salzburg and of Leonhard von Keutschach is reproduced in the tympanum beneath the mitre, legate cross and sword. A special feature of the coat of arms is the turnip and in many places in the fortress this can be found as an indication of prince-archbishop Keutschach's building activity. In the north wall of the chapel there are two openings which made it possible to attend the church service from the side room.

Golden Chamber:

The Golden Chamber is the most magnificently furnished room of the princely chambers. The two long walls are taken up by benches that are richly decorated with vines, grapes, foliage and animals. These benches used to be covered with cloth or leather, but the upholstery has not survived into the modern age. The walls also used to be covered in gold-embossed leather tapestry which adorned the lower part of the wall.

Bedchamber:

The bedchamber is the most intimate room of the princely chambers. The original furniture and precious textiles, such as tapestry, were in the course of time replaced by more "modern" ones. The elaborate wainscoting to keep out the cold still bears witness to the splendour of the past. The upper part of the panels is decorated with gilded buttons and rosettes, whereas the lower part, which is bare today, was probably covered with leather or velvet tapestry. The door conceals a toilet, which is basically a hole in the floor with a wooden frame. Back in the past this was a highly modern sanitary facility and was accessible from each floor.

Read More

Great Wall of China

Great Wall of China

Great Wall of China

The Great Wall of China is a series of fortifications made of stone, brick, tamped earth, wood, and other materials, generally built along an east-to-west line across the historical northern borders of China to protect the Chinese states and empires against the raids and invasions of the various nomadic groups of the Eurasian Steppe. Several walls were being built as early as the 7th century BCE; these, later joined together and made bigger and stronger, are now collectively referred to as the Great Wall.Especially famous is the wall built 220–206 BCE by Qin Shi Huang, the first Emperor of China. Little of that wall remains. Since then, the Great Wall has on and off been rebuilt, maintained, and enhanced; the majority of the existing wall is from the Ming Dynasty. Other purposes of the Great Wall have included border controls, allowing the imposition of duties on goods transported along the Silk Road, regulation or encouragement of trade and the control of immigration and emigration. Furthermore, the defensive characteristics of the Great Wall were enhanced by the construction of watch towers, troop barracks, garrison stations, signaling capabilities through the means of smoke or fire, and the fact that the path of the Great Wall also served as a transportation corridor.

The Great Wall stretches from Dandong in the east, to Lop Lake in the west, along an arc that roughly delineates the southern edge of Inner Mongolia. A comprehensive archaeological survey, using advanced technologies, has concluded that the Ming walls measure 8,850 km (5,500 mi). This is made up of 6,259 km (3,889 mi) sections of actual wall, 359 km (223 mi) of trenches and 2,232 km (1,387 mi) of natural defensive barriers such as hills and rivers. Another archaeological survey found that the entire wall with all of its branches measure out to be 21,196 km (13,171 mi).

Contents

History

The Chinese were already familiar with the techniques of wall-building by the time of the Spring and Autumn period between the 8th and 5th centuries BCE. During this time and the subsequent Warring States period, the states of Qin, Wei, Zhao, Qi, Yan, and Zhongshan[20][21] all constructed extensive fortifications to defend their own borders. Built to withstand the attack of small arms such as swords and spears, these walls were made mostly by stamping earth and gravel between board frames.

King Zheng of Qin conquered the last of his opponents and unified China as the First Emperor of the Qin dynasty ("Qin Shi Huang") in 221 BCE. Intending to impose centralized rule and prevent the resurgence of feudal lords, he ordered the destruction of the sections of the walls that divided his empire among the former states. To position the empire against the Xiongnu people from the north, however, he ordered the building of new walls to connect the remaining fortifications along the empire's northern frontier. Transporting the large quantity of materials required for construction was difficult, so builders always tried to use local resources. Stones from the mountains were used over mountain ranges, while rammed earth was used for construction in the plains. There are no surviving historical records indicating the exact length and course of the Qin walls. Most of the ancient walls have eroded away over the centuries, and very few sections remain today. The human cost of the construction is unknown, but it has been estimated by some authors that hundreds of thousands, if not up to a million, workers died building the Qin wall. Later, the Han, the Sui, and the Northern dynasties all repaired, rebuilt, or expanded sections of the Great Wall at great cost to defend themselves against northern invaders. The Tang and Song dynasties did not undertake any significant effort in the region. The Liao, Jin, and Yuan dynasties, who ruled Northern China throughout most of the 10th–13th centuries, constructed defensive walls in the 12th century but those were located much to the north of the Great Wall as we know it, within China's province of Inner Mongolia and in Mongolia itself.

The Great Wall concept was revived again under the Ming in the 14th century, and following the Ming army's defeat by the Oirats in the Battle of Tumu. The Ming had failed to gain a clear upper hand over the Mongolian tribes after successive battles, and the long-drawn conflict was taking a toll on the empire. The Ming adopted a new strategy to keep the nomadic tribes out by constructing walls along the northern border of China. Acknowledging the Mongol control established in the Ordos Desert, the wall followed the desert's southern edge instead of incorporating the bend of the Yellow River. Unlike the earlier fortifications, the Ming construction was stronger and more elaborate due to the use of bricks and stone instead of rammed earth. Up to 25,000 watchtowers are estimated to have been constructed on the wall. As Mongol raids continued periodically over the years, the Ming devoted considerable resources to repair and reinforce the walls. Sections near the Ming capital of Beijing were especially strong. Qi Jiguang between 1567 and 1570 also repaired and reinforced the wall, faced sections of the ram-earth wall with bricks and constructed 1,200 watchtowers from Shanhaiguan Pass to Changping to warn of approaching Mongol raiders. During the 1440s–1460s, the Ming also built a so-called "Liaodong Wall". Similar in function to the Great Wall (whose extension, in a sense, it was), but more basic in construction, the Liaodong Wall enclosed the agricultural heartland of the Liaodong province, protecting it against potential incursions by Jurched-Mongol Oriyanghan from the northwest and the Jianzhou Jurchens from the north. While stones and tiles were used in some parts of the Liaodong Wall, most of it was in fact simply an earth dike with moats on both sides.

Towards the end of the Ming, the Great Wall helped defend the empire against the Manchu invasions that began around 1600. Even after the loss of all of Liaodong, the Ming army held the heavily fortified Shanhai Pass, preventing the Manchus from conquering the Chinese heartland. The Manchus were finally able to cross the Great Wall in 1644, after Beijing had already fallen to Li Zicheng's rebels. Before this time, the Manchus had crossed the Great Wall multiple times to raid, but this time it was for conquest. The gates at Shanhai Pass were opened on May 25 by the commanding Ming general, Wu Sangui, who formed an alliance with the Manchus, hoping to use the Manchus to expel the rebels from Beijing. The Manchus quickly seized Beijing, and eventually defeated both the rebel-founded Shun dynasty and the remaining Ming resistance, establishing the Qing dynasty rule over all of China. Under Qing rule, China's borders extended beyond the walls and Mongolia was annexed into the empire, so constructions on the Great Wall were discontinued. On the other hand, the so-called Willow Palisade, following a line similar to that of the Ming Liaodong Wall, was constructed by the Qing rulers in Manchuria. Its purpose, however, was not defense but rather migration control.

Characteristics:

Before the use of bricks, the Great Wall was mainly built from rammed earth, stones, and wood. During the Ming, however, bricks were heavily used in many areas of the wall, as were materials such as tiles, lime, and stone. The size and weight of the bricks made them easier to work with than earth and stone, so construction quickened. Additionally, bricks could bear more weight and endure better than rammed earth. Stone can hold under its own weight better than brick, but is more difficult to use. Consequently, stones cut in rectangular shapes were used for the foundation, inner and outer brims, and gateways of the wall. Battlements line the uppermost portion of the vast majority of the wall, with defensive gaps a little over 30 cm (12 in) tall, and about 23 cm (9.1 in) wide. From the parapets, guards could survey the surrounding land. Communication between the army units along the length of the Great Wall, including the ability to call reinforcements and warn garrisons of enemy movements, was of high importance. Signal towers were built upon hill tops or other high points along the wall for their visibility. Wooden gates could be used as a trap against those going through. Barracks, stables, and armories were built near the wall's inner surface.

Condition:

While some portions north of Beijing and near tourist centers have been preserved and even extensively renovated, in many locations the Wall is in disrepair. Those parts might serve as a village playground or a source of stones to rebuild houses and roads. Sections of the Wall are also prone to graffiti and vandalism, while inscribed bricks were pilfered and sold on the market for up to 50 renminbi. Parts have been destroyed because the Wall is in the way of construction. A 2012 report by the State Administration of Cultural Heritage states that 22% of the Ming Great Wall has disappeared, while 1,961 kilometres (1,219 mi) of wall have vanished. More than 60 km (37 mi) of the wall in Gansu province may disappear in the next 20 years, due to erosion from sandstorms. In places, the height of the wall has been reduced from more than 5 metres (16 feet) to less than 2 metres (6.6 ft). Various square lookout towers that characterize the most famous images of the wall have disappeared. Many western sections of the wall are constructed from mud, rather than brick and stone, and thus are more susceptible to erosion.

Visibility from space (From the Moon)

One of the earliest known references to this myth appears in a letter written in 1754 by the English antiquary William Stukeley. Stukeley wrote that, "This mighty wall of four score miles in length (Hadrian's Wall) is only exceeded by the Chinese Wall, which makes a considerable figure upon the terrestrial globe, and may be discerned at the Moon." The claim was also mentioned by Henry Norman in 1895 where he states "besides its age it enjoys the reputation of being the only work of human hands on the globe visible from the Moon." The issue of "canals" on Mars was prominent in the late 19th century and may have led to the belief that long, thin objects were visible from space. The claim that the Great Wall is visible also appears in 1932's Ripley's Believe It or Not! strip and in Richard Halliburton's 1938 book Second Book of Marvels.

The claim the Great Wall is visible from space has been debunked many times, but is still ingrained in popular culture. The wall is a maximum 9.1 m (30 ft) wide, and is about the same color as the soil surrounding it. Based on the optics of resolving power (distance versus the width of the iris: a few millimeters for the human eye, meters for large telescopes) only an object of reasonable contrast to its surroundings which is 70 mi (110 km) or more in diameter (1 arc-minute) would be visible to the unaided eye from the Moon, whose average distance from Earth is 384,393 km (238,851 mi). The apparent width of the Great Wall from the Moon is the same as that of a human hair viewed from 3.2 kilometers (2 mi) away. To see the wall from the Moon would require spatial resolution 17,000 times better than normal (20/20) vision. Unsurprisingly, no lunar astronaut has ever claimed to have seen the Great Wall from the Moon.

Read More

Lumbini

Lumbini

Lumbini, Birth Place of  Gautama Buddha

Lumbini is a Buddhist pilgrimage site in the Rupandehi District of Nepal. It is the place where, according to Buddhist tradition, Queen Mayadevi gave birth to Siddhartha Gautama in 563 BCE. Gautama, who achieved Enlightenment some time around 528 BCE, became the Gautama Buddha and founded Buddhism.Lumbini is one of many magnets for pilgrimage that sprang up in places pivotal to the life of Gautama Buddha; other notable pilgrimage sites include Kushinagar, Bodh Gaya and Sarnath. Lumbini has a number of temples, including the Mayadevi Temple and several others which are still under construction. Many monuments, monasteries and a museum — the Lumbini International Research Institute — are also located within the holy site. Also located there is the Puskarini or Holy Pond where the Buddha's mother took the ritual dip prior to his birth and where he, too, had his first bath. At other sites near Lumbini, earlier Buddhas were, according to tradition, born, achieved ultimate Enlightenment and finally relinquished their earthly forms. Lumbini was granted World Heritage status by UNESCO in 1997.

In the Buddha's time, Lumbini was situated between Kapilavastu and Devadaha (both in Nepal). It was there, that the Buddha was born. A pillar now marks the spot of Ashoka's visit to Lumbiní. According to an inscription on the pillar, it was placed there by the people then in charge of the park to commemorate Ashoka's visit and gifts. The park was previously known as Rummindei, two miles (3.2 km) north of Bhagavanpura. In the Sutta Nipáta (vs. 683) it is stated that the Buddha was born in a village of the Sákyans in the Lumbineyya Janapada. The Buddha stayed in Lumbinívana during his visit to Devadaha and there preached the Devadaha Sutta.

Eternal Peace Flame

In 1896, Nepalese archaeologists (led by Khadga Samsher Rana and assisted by Alois Anton Führer) discovered a great stone pillar at Lumbini. Führer postulated that the pillar was placed at the site by Ashoka (emperor of the Maurya Empire) circa 245 BCE. Records made by the Chinese pilgrim Faxian in the early fifth century CE were also used in the process of identifying this religiously acclaimed site.

Eternal Peace Flame

Recent excavations beneath existing brick structures at the Mayadevi Temple at Lumbini have uncovered evidence for an older timber structure beneath the walls of the newer brick Buddhist shrine, which was constructed during the Ashokan era. The layout of the Ashokan shrine closely follows that of the earlier timber structure, which suggests a continuity of worship at the site. The pre-Mauryan timber structure appears to be an ancient bodhigara (tree shrine), consisting of postholes and a wooden railing surrounding a clay floor containing mineralized tree roots that appears to have been worn smooth by visitors. Radiocarbon dating of charcoal from the wooden postholes and optically stimulated luminescence dating of elements in the soil suggests human activity (possibly pre-Buddhist tree worship) began at the site around 1000 BCE, followed by the development of a Buddhist monastery-like community by approximately 550 BCE.

The present-day Lumbini historic site is 4.8 km (3 mi) in length and 1.6 km (1.0 mi) in width. The holy site of Lumbini is bordered by a large monastic zone in which only monasteries can be built, no shops, hotels or restaurants. It is separated into an eastern and western monastic zone, the eastern having the Theravadin monasteries, the western having Mahayana and Vajrayana monasteries. The holy site of Lumbini has ruins of ancient monasteries, a sacred Bodhi tree, an ancient bathing pond, the Ashokan pillar and the Mayadevi Temple, where the supposed place of birth of Buddha is located. From early morning to early evening, pilgrims from various countries perform chanting and meditation at the site.

A non-governmental organization named Samriddhi Foundation started in 2013 working extensively in the field of education and health specially in government schools of the area where underprivileged children study. A non-governmental organisation called "Asia Pacific Exchange and Cooperation Foundation" (APECF) backed by chairman of the Unified Communist Party of Nepal (Maoist) and then Prime Minister Prachanda, the Chinese government and a UN group called "United Nations Industrial Development Organization" (UNIDO) signed a deal to develop Lumbini into a "special development zone" with funds worth $3 billion. The venture was a China-UN joint project. A broader 'Lumbini Development National Director Committee' under the leadership of Pushpa Kamal Dahal was formed on 17 October 2011.The six-member committee included Communist Party of Nepal (Unified Marxist-Leninist) leader Mangal Siddhi Manandhar, Nepali Congress leader Minendra Rijal, Forest Minister Mohammad Wakil Musalman, among other leaders. The committee was given the authority to "draft a master plan to develop Lumbini as a peaceful and tourism area and table the proposal" and the responsibility to gather international support for the same. Nipponzan Myohoji decided to build a Peace Pagoda in the park in 2001, which is visited by many different cultures and religions every day.

Hindus regard the Buddha as an incarnation of Vishnu and thousands of Hindu pilgrims go there on the full moon of the Nepali month of Baisakh (April–May) to worship Queen Mayadevi as Rupa Devi, the mother goddess of Lumbini.

Read More

Zubarah

Zubarah

Zubarah, Qatar

The name 'Zubarah' is derived from the Arabic word for sand mounds. It was presumably given this name due its abundance of sand and stony hillocks. During the early Islamic period, trade and commerce boomed in northern Qatar. Settlements began to appear on the coast, primarily between the towns of Zubarah and Umm al-Ma'a. A village dating back to the Islamic period was discovered near the town.Zubarah is a district located on the north western coast of the Qatar peninsula in the Madinat ash Shamal municipality, about 105 km from the Qatari capital of Doha. It was founded by merchants from Kuwait in the mid 18th century. It was designated a UNESCO World Heritage Site in 2013. It was once a successful center of global trade and pearl fishing positioned midway between the Strait of Hormuz and the west arm of the Persian Gulf. It is one of the most extensive and best preserved examples of an 18th–19th century settlement in the region. The layout and urban fabric of the settlement has been preserved in a manner unlike any other settlements in the Persian Gulf, providing an insight into the urban life, spatial organization, and the social and economic history of the Gulf before the discovery of oil and gas in the 20th century. Covering an area of circa 400 hectares (60 hectares inside the outer town wall), Zubarah is Qatar’s most substantial archaeological site. The site comprises the fortified town with a later inner and an earlier outer wall, a harbour, a sea canal, two screening walls, Qal'at Murair (Murair fort), and the more recent Zubarah Fort.

Between September 1627 and April 1628, a Portuguese naval squadron led by D. Goncalo da Silveira set a number of neighboring coastal villages ablaze. Zubarah's settlement and growth during this period is attributed to the dislodging of people from these adjacent settlements. The main settlers of the town were from the Al Musallam tribe, who derive from the Bani Khalid of Arabia. The Al Musallam were influential in Qatar and had even ruled the country as early as 1555 according to Ottoman records. They eventually became tributary to the other branches of Bani Khalid as the latter expanded their domain eastwards in the first half of the eighteenth century. There remains some uncertainty over the earliest mention of Zubarah in written documents. Qatar's Memorial, a 1986 Arabic history book, alleges that a functional self-governing town existed before the arrival of the Utub. It supported this claim by invoking two purported historical documents, but they were later discovered to be forgeries produced by Qatar in an attempt to gain leverage over Bahrain in their long-standing dispute over the sovereignty of the town.

Most sources assert that Zubarah rose to prominence only after people of the Utub tribe from Kuwait settled at Zubarah in the second half of the eighteenth century, possibly in 1762 or 1766, helping to build a large town characterized by a safe harbour. It soon emerged as one of the principal emporiums and pearl trading centres of the Persian Gulf.

Relations between the Al Khalifa branch of the Utub and the dominant and ruling tribe of Al Musallam gradually declined. This culminated in the former's refusal to pay taxes. They also expanded their settlements, and constructed walls and a fort called Qal'at Murair (Murair Castle), which was completed by 1768. In addition to Qal'at Murair, there existed other forts and towers in the town which were built by previous settlers.

The town was eventually monopolized by the Al Khalifa after they had effectually driven out the Al Musallam. Under their jurisdiction, the town developed trade links with India, Oman, Iraq and Kuwait. Many goods were transported through its ports, including dates, spices and metals. The town soon became a favorite transit point for traders after the Al Khalifa abolished trade taxes. The town's prosperity further increased after the 1775–76 Persian occupation of Basra when merchants and other refugees fleeing from Basra settled in Zubarah. Merchants from nearby settlements migrated to Zubarah en masse during the 1770s due to the prevalence of attacks and the plague in the Persian Gulf region.

Communal life

Zubarah was at that time a well-organised town, with many of the streets running at right angles to one another and some neighbourhoods built according to a strict grid pattern. This layout suggests that the town was laid out and built as part of a major event, although seemingly constructed in closely dated stages. An estimate of the population at the height of the town has been calculated to a maximum number of between 6,000 and 9,000 people.

Most of the settler's dietary requirements were fulfilled from the consumption of livestock animals. Remnants of sheep, goat, birds, fish and gazelle were among the waste collected from the palatial compounds. The wealthiest members of the community consumed mainly livestock, whereas the poorer residents relied on fish as their primary source of protein. Social, economic and political activity was most likely centered in the souq. The discovery of numerous ceramic tobacco pipe bowls indicate a reluctant acceptance and growing social addiction to smoking tobacco. Coffee pots, mainly of Chinese origin, were used by Zubarah's inhabitants to drink Arabic coffee.

Economic history

Zubarah was primarily an emporium and pearling settlement that capitalized on its proximity to pearl beds, possession of a large harbour and its central position on the Gulf routes. Its economy depended on the pearl diving season, which took place during the long summer months. Pearling would draw Bedouin from the interior of Qatar as well as the people from all over the Persian Gulf to dive, trade and safeguard the town from attack while the town’s men were at sea. Boats from Zubarah would sail out to the pearl beds found all along the southern shore of the Persian Gulf, from Bahrain to the United Arab Emirates. The trips lasted several weeks at a time. Men would work in pairs to harvest mollusks potentially hiding pearls inside them. A man would dive for about a minute and the other remained on the ship to pull the diver back to safety with his harvest. The archaeological evidence for pearling on site comes primarily from the tools used by the divers such, as pearl boxes, diving weights, and small measuring weights used during trading.

Global trade

Zubarah was the focal point of an extensive regional trade network during its peak in the late eighteenth century. Until the introduction of the cultured pearl in the early 1900s, the trade in pearls constituted the Persian Gulf’s most important industry, employing up to a third of the male population in the region. Zubarah, being one of the focal pearling and trading towns, contributed to the geopolitical, social, and cultural trajectories of Gulf history which shape the region today. Ceramics, coins, and the remains of foodstuffs from the excavations attest to Zubarah’s far reaching trade and economic links in the late 18th century, with material deriving from eastern Asia, Persia, the Ottoman Empire, Africa, Europe, and the Persian Gulf. Diving weights and other material culture show how closely the connection between the daily life in the town and the pearl fishing and trading were. The discovery of coffee cups and tobacco pipes in the excavations reveal the growing importance of these commodities all over the Persian Gulf during the eighteenth and nineteenth centuries. The etching of a merchant’s dhow, the traditional wooden boat of Arabia, found incised into the plaster in a room of a courtyard building, details how intimately the town's inhabitants associated their daily lives with long-distance maritime trade and commerce. Date trade also had an important role in the local economy.

Marketplace

A complex array of small storage rooms have been identified as part of the souq (market) of Zubarah. The wide variety of trade objects that have been found in the rooms points towards the area's classification as a place of trade. The souq would have been the centre of the town and of its economy. Various commodities, including ironsmithing, were sold at this souq.

Historical architecture

The architecture consisted mainly of courtyard houses, a traditional form of Arabic architecture which can be found throughout the Middle East. A series of small rooms were organized around a large central courtyard, where the majority of daily activity took place. Typically, a portico opened out onto the courtyard on the south side, which offered shelter from the sun. The houses of Zubarah were constructed from soft local stone, or from limestone quarried from the northern settlement of Freiha. The stone was then protected by a thick gypsum plaster coating. Features such as doorways and niches were decorated with geometric stucco designs. Housing units were accessible by a doorway and a bent corridor, in order to avert unauthorized viewing into the household, and to prevent sand from blowing into the house. Traces of what seems to be tent placements and/or palm-leaf and palm-matt huts found near the beach may be associated with transient members of the Zubaran society. It is likely that these interim dwellings housed the people who were the primary producers of Zubarah’s wealth: the pearl fishers and mariners who harvested the pearl banks each season.

The most impressive and colossal of the building complexes measures 110 m by 100 m in size and is commonly referred to as 'the palace'. This structure follows the same form as the domestic architecture seen elsewhere in Zubarah, but on a much larger scale. Nine interconnected compounds, each comprising a courtyard surrounded by a range of rooms, made up the interior of this structure. Plaster stucco decoration was used to embellish internal entrances and rooms. The discovery of internal staircases indicates that the compounds were multi-storeyed. The nine compounds of the complex were enclosed by a high circuit wall with circular towers at the four corners, each of which were capable of supporting a small cannon. The size and visual dominance of the palatial compound suggests that it was occupied by a family of wealthy and powerful sheikhs who were community leaders in the social and economic life of the town.

Fortifications

Protection of the town and its peoples' wealth was a clear priority. A large wall was built in the late-18th-century town and its bay in a 2.5 km arc from shore to shore. The wall was defended by 22 semi-circular towers placed at regular intervals. It was faced by parapet with a walkway, most likely to provide leverage for gunners. Access to the town was limited to a few defended gateways from the landside, or via its harbour. There was no sea wall, but a stout fort defended the main landing area on the sandy beach. In spite of its defensive fortifications, Zubarah was attacked on several occasions. In addition to two major attacks carried out at the behest of Nasr Al-Madhkur in 1778, and 1782, the residents of the town were engaged in a war with the Banu Kaab of Khuzestan during the late eighteenth century.

Read More

Iona National Park

Iona National Park

Iona National Park

Iona National Park is the largest national park in Angola. It is situated in the Southwestern-most part of the country, in Namibe Province. It is roughly bounded by the Atlantic Ocean to the West, an escarpment to the East that marks the beginning of the interior plateau, the Curoca River to the North, and the Cunene River to the South. It is about 200 kilometres  south of the city of Namibe and covers 5,850 square miles (15,200 km2) sq. miles. The topography of Iona is characterised by wild dunes, vast plains, and rough mountains and cliffs. Annual average precipitation is approximately 18mmm. The Curoca River is intermittent but has lagoons, while the Cunene is permanent and has marshy areas at its mouth. Iona had been proclaimed as a reserve in 1937 and upgraded to a national park in 1964. However, as is true for most Angolan national parks, the Angolan Civil War greatly disrupted the area. Illegal poaching and the destruction of infrastructure have caused considerable damage to the once rich park. In recent years, a number of government and international projects have begun rebuilding the infrastructure of the park.

Iona is part of the northern Namib Desert, the only true desert in Southern Africa. The area, also known as the Kaokoveld Desert, has been arid for 55-80 million years may be the oldest desert in the world. It faces the Atlantic Ocean for 180 kilometres (110 mi) on the edge of the Benguela Current, a cold up-welling from the depths of the Atlantic that creates a rich ecosystem off-shore. To the east, Iona rises to the base of the Great Escarpment at the Tchamaline and Cafema mountains. Iona is ounded on the north and south by the Cunene and Curoca Rivers, respectively. The climate is noteworthy for the heavy fogs created as the cold, wet air of the Benguela up-welling meets the hot, dry air of the desert. The strong fogs and currents have led to numerous shipwrecks through history. The coast is sometimes called Skeleton Coast after the bones of whales and seals that were seen on the beaches by sailors. The area is classified as a Hot Desert Climate, KWh in the Köppen climate classification. The park is contiguous with the Skeleton Coast Park in Namibia, which is itself contiguous with the Namib-Naukluft National Park so that all three protected areas form a continuous block covering some 1,200 km of Namib Desert coastline and adjacent dunes.

Vegetation

According to the Angola Ministry of the Environment, there are three types of vegetation at Iona National Park: · Sub-coastal steppes with woody and herbaceous components (Barbosa’s Type 27). This type of vegetation is a sub-coastal African steppe-like formation dominated by Acacia, Commiphora, Colophosphormum, Aristida, Schmidita, and Staria species. · Discontinued coastal steppes (Barbosa’s Type 28), which corresponds to sub-desert-like vegetation. This type of vegetation is dominated by Aristida, Cissus, Salvadora, and Welwitschia species. Desert with moving dunes (Barbosa’s type 29). This type of vegetation is dominated by Odyssea and Sporobulus species.The park is the main habitat of Welwitchia Mirabilis, a plant sometimes referred to as a "living fossil". The plant derives its moisture from sea-fog dew which rolls in from the Atlantic. The dew is absorbed through the leaves rather than through roots alone.

Animals

Because of its distinctive habitat and climate, Iona and the Kaokoveld Desert have a number of endemic animals, particularly reptiles. 63 species have been recorded in the ecoregion, eight are strictly endemic. The endemics include two lizards, three geckos, and three skinks. The mouth of the Cunene River to the south supports a small wetland area that is important to migrating birds. South African cheetah have been sighted in the park for the first time in 2010.

Read More

Zion National Park

Zion National Park

Zion National Park, US

Zion National Park is located in the Southwestern United States, near Springdale, Utah. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to half a mile (800 m) deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft (1,117 m) at Coalpits Wash and the highest elevation is 8,726 ft (2,660 m) at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches.

Human habitation of the area started about 8,000 years ago with small family groups of Native Americans; the semi-nomadic Basketmaker Anasazi (300 CE) stem from one of these groups. In turn, the Virgin Anasazi culture (500 CE) developed as the Basketmakers settled in permanent communities. A different group, the Parowan Fremont, lived in the area as well. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s. In 1909 the President of the United States, William Howard Taft, named the area a National Monument to protect the canyon, under the name of Mukuntuweap National Monument. In 1918, however, the acting director of the newly created National Park Service changed the park's name to Zion, the name used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." The United States Congress established the monument as a National Park on November 19, 1919. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the park in 1956.

The geology of the Zion and Kolob canyons area includes 9 formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet (3,000 m) starting 13 million years ago.

Settlements had expanded 30 miles (48 km) south to the lower Virgin River by 1858. That year, a Southern Paiute guide led young Mormon missionary and interpreter Nephi Johnson into the upper Virgin River area and Zion Canyon. Johnson wrote a favorable report about the agricultural potential of the upper Virgin River basin, and returned later that year to found the town of Virgin. In 1861 or 1862, Joseph Black made the arduous journey to Zion Canyon and was very impressed by its beauty. The floor of Zion Canyon was settled in 1863 by Isaac Behunin, who farmed corn, tobacco, and fruit trees. The Behunin family lived in Zion Canyon near the site of today's Zion Lodge during the summer, and wintered in Springdale. Behunin is credited with naming Zion, a reference to a place of peace mentioned in the Bible. Two more families settled Zion Canyon in the next couple of years, bringing with them cattle and other domesticated animals. The canyon floor was farmed until Zion became a Monument in 1909.

The Powell Geographic Expedition entered the area in 1869 after their first trip through the Grand Canyon. John Wesley Powell visited Zion Canyon in 1872 and named it Mukuntuweap, under the impression that that was the Paiute name. Powell Survey photographers John K. Hillers and James Fennemore first visited the Zion Canyon and Kolob Plateau region in the spring of 1872. Hillers returned in April 1873 to add more photographs to the "Virgin River Series" of photographs and stereographs. Hillers described wading the canyon for four days and nearly freezing to death to take his photographs. Touring cars could reach Zion Canyon by the summer of 1917. The first visitor lodging in Zion Canyon, called Wylie Camp, was established that same year as a tent camp. The Utah Parks Company, a subsidiary of the Union Pacific Railroad, acquired Wylie Camp in 1923, and offered ten-day rail/bus tours to Zion, nearby Bryce Canyon, Kaibab, and the North Rim of the Grand Canyon. The Zion Lodge complex was built in 1925 at the site of the Wylie tent camp. Architect Gilbert Stanley Underwood designed the Zion Lodge (photo) in the "Rustic Style" and the Utah Parks Company funded the construction.

Work on the Zion – Mount Carmel Highway started in 1927 to enable reliable access between Springdale and the east side of the park. The road opened in 1930 and park visit and travel in the area greatly increased. The most famous feature of the Zion - Mount Carmel Highway is the 1.1-mile (1.8 km) Zion - Mt. Carmel Tunnel, which has six large windows cut through the massive sandstone cliff. In 1896, local rancher John Winder improved the Native American footpath up Echo Canyon, which later became the East Rim Trail. Entrepreneur David Flanigan used this trail in 1900 to build cableworks that lowered lumber into Zion Canyon from Cable Mountain. More than 200,000 board feet (470 m3) of lumber were lowered by 1906. The auto road was extended to the Temple of Sinawava, and a trail built from there 1 mile (1.6 km) to the start of the Narrows. Angel's Landing Trail was constructed in 1926 and two suspension bridges were built over the Virgin River. Other trails were constructed by the Civilian Conservation Corps during the 1930s. Zion Canyon Scenic Drive provides access to Zion Canyon. Traffic congestion in the narrow canyon was recognized as a major problem in the 1990s and a public transportation system using propane-powered shuttle buses was instituted in the year 2000. As part of its shuttle fleet, Zion has two electric trams each holding up to 36 passengers. Usually from early April through late October, the scenic drive in Zion Canyon is closed to private vehicles and visitors ride the shuttle buses.

On April 12, 1995, heavy rains triggered a landslide that blocked the Virgin River in Zion Canyon. Over a period of two hours, the river carved away part of the only exit road from the canyon, trapping 450 guests and employees at the Zion Lodge. A one-lane, temporary road was constructed within 24 hours to allow evacuation of the Lodge. A more stable — albeit temporary — road was completed on May 25, 1995 to allow summer visitors to access the canyon. This road was replaced with a permanent road during the first half of 1996. 

Read More