Fiordland is a geographic region of New Zealand that is situated on the south-western corner of the South Island, comprising the western-most third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lakes and its ocean-flooded, steep western valleys. Indeed, the name "Fiordland" comes from a variant spelling of the Scandinavian word for this type of steep valley, "fjord".
A következő címkéjű bejegyzések mutatása: nature. Összes bejegyzés megjelenítése
A következő címkéjű bejegyzések mutatása: nature. Összes bejegyzés megjelenítése
Bay of Fundy, Canada
The Bay of Fundy (French: Baie de Fundy) is a bay on the Atlantic coast of North America, on the northeast end of the Gulf of Maine between the Canadian provinces of New Brunswick and Nova Scotia, with a small portion touching the U.S. state of Maine. Some sources believe the name "Fundy" is a corruption of the French word "Fendu", meaning "split", while others believe it comes from the Portuguese fondo, meaning "funnel". The bay was also named Baie Française (French Bay) by explorer/cartographer Samuel de Champlain during a 1604 expedition led by Pierre Dugua, Sieur de Monts which resulted in a failed settlement attempt on St. Croix Island.
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Bay of Fundy, Canada[/caption]The Bay of Fundy is known for having the highest tidal range in the world. Rivaled by Ungava Bay in northern Quebec, King Sound in Western Australia, Gulf of Khambhat in India, and the Severn Estuary in the UK, it has one of the highest vertical tidal ranges in the world. The Guinness Book of World Records (1975) declared that Burntcoat Head, Nova Scotia has the highest tides in the world: “The Natural World, Greatest Tides: The greatest tides in the world occur in the Bay of Fundy.... Burntcoat Head in the Minas Basin, Nova Scotia, has the greatest mean spring range with 14.5 metres (47.5 feet) and an extreme range of 16.3 metres (53.5 feet).”
Portions of the Bay of Fundy, Shepody Bay and Minas Basin, form one of six Canadian sites in the Western Hemisphere Shorebird Reserve Network, and is classified as a Hemispheric site. It is administered by the provinces of New Brunswick and Nova Scotia, and the Canadian Wildlife Service, and is managed in conjunction with Ducks Unlimited Canada and the Nature Conservancy of Canada. In July 2009, the Bay of Fundy was named as a finalist for the New 7 Wonders of Nature contest that ended in November 2011. It was not chosen as a wonder.
The Bay of Fundy is known for its high tidal range. The quest for world tidal dominance has led to a rivalry between the Minas Basin in the Bay of Fundy and the Leaf Basin in Ungava Bay, over which body of water lays claim to the highest tides in the world, with supporters in each region claiming the record. The Canadian Hydrographic Service finally declared it a statistical tie, with measurements of a 16.8 metre (55.1 feet) tidal range in Leaf Basin for Ungava Bay and 17 meters (55.8 feet) at Burntcoat Head for the Bay of Fundy. The highest water level ever recorded in the Bay of Fundy system occurred at the head of the Minas Basin on the night of October 4–5, 1869 during a tropical cyclone named the “Saxby Gale”. The water level of 21.6 meters (70.9 feet) resulted from the combination of high winds, abnormally low atmospheric pressure, and a spring tide.
[youtube http://www.youtube.com/watch?v=qfhNjpu_IU4?rel=0]
Leaf Basin has only been measured in recent years, whereas the Fundy system has been measured for many decades. The tide at Leaf Basin is higher on average than tides at Minas Basin; however, the highest recorded tidal ranges ever measured are at Burntcoat Head and result from spring tides measured at the peak of the tidal cycle every 18 years. Folklore in the Mi'kmaq First Nation claims that the tides in the Bay of Fundy are caused by a giant whale splashing in the water. Oceanographers attribute it to tidal resonance resulting from a coincidence of timing: the time it takes a large wave to go from the mouth of the bay to the inner shore and back is practically the same as the time from one high tide to the next. During the 12.4 hour tidal period, 115 billion tonnes of water flow in and out of the bay. The tides in the Bay of Fundy are semidiurnal. Semidiurnal tides are tides that have two highs and two lows each day. The height that the water rises and falls to each day during these tides are approximately equal. There are approximately six hours and thirteen minutes between each high and low tide.
Big Sur, United States
Big Sur is a sparsely populated region of the Central Coast of California where the Santa Lucia Mountains rise abruptly from the Pacific Ocean. The name "Big Sur" is derived from the original Spanish-language "el sur grande", meaning "the big south", or from "el país grande del sur", "the big country of the south". The terrain offers stunning views, making Big Sur a popular tourist destination. Big Sur's Cone Peak is the highest coastal mountain in the contiguous 48 states, ascending nearly a mile (5,155 feet/1571 m) above sea level, only three miles (4.8 km) from the ocean.
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[/caption]Although Big Sur has no specific boundaries, many definitions of the area include the 90 miles (140 km) of coastline from the Carmel River south to the San Carpoforo Creek, and extend about 20 miles (32 km) inland to the eastern foothills of the Santa Lucias. Other sources limit the eastern border to the coastal flanks of these mountains, only three to 12 miles (19 km) inland. Another practical definition of the region is the segment of California State Route 1 between San Simeon and Carmel. The northern end of Big Sur is about 120 miles (190 km) south of San Francisco, and the southern end is approximately 245 miles (394 km) northwest of Los Angeles.
Although some Big Sur residents catered to adventurous travelers in the early twentieth century,[39] the modern tourist economy began when Highway 1 opened the region to automobiles, and only took off after World War II-era gasoline rationing ended in the mid-1940s. Most of the 3 million tourists who visit Big Sur each year never leave Highway 1, because the adjacent Santa Lucia mountain range is one of the largest roadless areas near a coast in the contiguous United States. The highway winds along the western flank of the mountains mostly within sight of the Pacific Ocean, varying from near sea level up to a thousand-foot sheer drop to the water. Because gazing at the views while driving is inadvisable, the highway features many strategically placed vista points allowing motorists to stop and admire the landscape. The section of Highway 1 running through Big Sur is widely considered as one of the most scenic driving routes in the United States, if not the world. These breathtaking views were one reason that Big Sur ranked second among all United States destinations in TripAdvisor's 2008 Travelers' Choice Destination Awards.
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[/caption]The land use restrictions that preserve Big Sur's natural beauty also mean that tourist accommodations are limited, often expensive, and fill up quickly during the busy summer season. There are fewer than 300 hotel rooms on the entire 90 mile (140 km) stretch of Highway 1 between San Simeon and Carmel, only three gas stations, and no chain hotels, supermarkets, or fast-food outlets. The lodging options are rustic cabins, motels, and campgrounds, or costly, exclusive five-star resorts, with little in between. Most lodging and restaurants are clustered in the Big Sur River valley, where Highway 1 leaves the coast for a few miles and winds into a redwood forest, protected from the chill ocean breezes and summer fog.
Besides sightseeing from the highway, Big Sur offers hiking, mountain climbing, and other outdoor activities. There are a few small, scenic beaches that are popular for walking, but usually unsuitable for swimming because of unpredictable currents and frigid temperatures. Big Sur's nine state parks have many points of interest, including one of the few waterfalls on the Pacific Coast that plunges directly into the ocean, located at Julia Pfeiffer Burns State Park, although visitors are not allowed on the beach itself to preserve the natural habitat. The waterfall is located near the ruins of a grand stone cliffside house that was the region's first electrified dwelling. Another notable landmark is the only complete nineteenth century lighthouse complex open to the public in California, set on a lonely, windswept hill that looks like an island in the fog.
Blood Pond Hot Spring, Japan
A hot spring is a spring that is produced by the emergence of geothermally heated groundwater from the Earth's crust. There are geothermal hot springs in many locations all over the crust of the earth.The water issuing from a hot spring is heated by geothermal heat, i.e., heat from the Earth's mantle. In general, the temperature of rocks within the earth increases with depth. The rate of temperature increase with depth is known as the geothermal gradient. If water percolates deeply enough into the crust, it will be heated as it comes into contact with hot rocks. The water from hot springs in non-volcanic areas is heated in this manner.
Blood Pond Hot Spring is one of the “hells” (jigoku) of Beppu, Japan — nine spectacular natural hot springs that are more for viewing rather than bathing. The “blood pond hell” features a pond of hot, red water, colored as such by iron in the waters. It’s allegedly the most photogenic of the nine hells.
Hotels in the jungle, Bali
Bali : Island of the Gods, The Morning of the World, a mystical place that evokes different visions for all that have experienced it, and for those that have only heard the name. An island that encompasses many diverse regions and styles – regions of untouched beauty, traditional villages, heaving and raucous budget-traveler districts, resort areas, playgrounds for the rich and famous, and many little hideaways all combined to form the identity that is Bali. Though not untouched by the impact of being a popular tourist destination, Bali has successfully managed to accommodate its many foreign visitors while maintaining its own rich culture.
Historically, Bali was a collection of independent kingdoms, before being brought under Dutch colonial control in the 19th century and incorporated into what was then the Dutch East Indies . In 1948, shortly after WWII, Bali, along with the rest of the country, achieved independence from Holland and become a part of Indonesia .
Having been a tourist destination since the early 1900's, Bali is accustomed to playing host to visitors from all over the world. This is expressed in the numerous facilities and activities for tourists on the island, along with the famed Balinese smile accompanying their friendly, relaxed, and personable demeanor.
The Stone Forrest, China
The Stone Forest or Shilin (Chinese: Shílín) is a notable set of karst formations located in Shilin Yi Autonomous County, Yunnan Province, People's Republic of China, approximately 120 kilometres (75 mi) from the provincial capital Kunming. The tall rocks seem to emanate from the ground in the manner of stalagmites, with many looking like petrified trees thereby creating the illusion of a forest made of stone. Since 2007, two parts of the site, the Naigu Stone Forest and Suogeyi Village, have been UNESCO World Heritage Sites as part of the South China Karst.
According to legend, the forest is the birthplace of Ashima, a beautiful girl of the Yi people. After falling in love she was forbidden to marry her chosen suitor and instead turned into a stone in the forest that still bears her name. Each year on the 24th day of the sixth lunar month, many Yi people celebrate the Torch Festival, which features folk dances and wrestling competitions.
[youtube http://www.youtube.com/watch?v=Ln5K3_8Cxrc?rel=0]
Son Doong Cave, Vietnam
Son Doong cave (meaning Mountain River Cave) is a cave in Phong Nha-Ke Bang National Park, Bo Trach District, Quang Binh Province, Vietnam. The cave is located near the Laos-Vietnam border. It has a large fast-flowing underground river inside.
The cave was found by a local man named Ho-Khanh in 1991. The local jungle men were afraid of the cave for the whistling sound it makes from the underground river. However, not until 2009 was it made known to the public when a group of British scientists from the British Cave Research Association, led by Howard and Deb Limbert, conducted a survey in Phong Nha-Ke Bang from April 10-14, 2009. Their progress was stopped by a large calcite wall. According to Limbert, this cave is five times larger than the Phong Nha cave, previously considered the biggest cave in Vietnam. The biggest chamber of Son Doong is over five kilometers in length, 200 meters high and 150 meters wide. With these dimensions, Son Doong overtakes Deer Cave in Malaysia to take the title of the world's largest cave.
[youtube http://www.youtube.com/watch?v=VFWhqJeThfc?rel=0]