A következő címkéjű bejegyzések mutatása: Nature Created. Összes bejegyzés megjelenítése
A következő címkéjű bejegyzések mutatása: Nature Created. Összes bejegyzés megjelenítése

Lake Hillier, Australia

Lake Hillier, is a lake on Middle Island, the largest of the islands and islets that make up the Recherche Archipelago, Western Australia. The most notable feature of this lake is its pink colour. It is such a significant distinguishing feature of the archipelago that air passengers often take note of it. The colour is permanent, and does not alter when the water is taken in a container. The length of the lake is about six hundred meters (3/8 mile). The lake is surrounded by a rim of sand and a dense woodland of paperbark and eucalyptus trees with a narrow strip of sand dunes covered by vegetation separating it to the north from the Southern Ocean.




[caption id="attachment_546" align="aligncenter" width="594"]Lake Hillier, Australia Lake Hillier, Australia[/caption]

The island and lake are thought to have been first charted by the Flinders expedition in 1802. Captain Flinders is said to have observed the pink lake after ascending the island's peak. John Thistle, the ship's master, collected some of the lake's water, which he found to be saturated with salt. Although the source of the pink colour has not been definitively proven in the case of Lake Hillier, the pink colour of other salt lakes (e.g., Pink Lake) in the region arises from a dye created by the organisms Dunaliella salina and Halobacteria. Another hypothesis is that the pink colour is due to red halophilic bacteria in the salt crusts.


Despite the unusual hue, the lake exhibits no known adverse effects upon humans. From above the lake appears a solid bubble gum pink, but from the shoreline it looks more like a clear pink hue is in the water. The shoreline is also covered in salt crust deposits.

The Giant's Causeway, Ireland

The Giant's Causeway is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven or eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places. The Giant's Causeway is today owned and managed by the National Trust and it is the most popular tourist attraction in Northern Ireland.




[caption id="attachment_535" align="aligncenter" width="1277"]The Giant's Causeway The Giant's Causeway[/caption]

Some 50 to 60 million years ago, during the Paleogene period, Antrim was subject to intense volcanic activity, when highly fluid molten basalt intruded through chalk beds to form an extensive lava plateau. As the lava cooled rapidly, contraction occurred. Horizontal contraction fractured in a similar way to drying mud, with the cracks propagating down as the mass cooled, leaving pillarlike structures, which are also fractured horizontally into "biscuits". In many cases the horizontal fracture has resulted in a bottom face that is convex while the upper face of the lower segment is concave, producing what are called "ball and socket" joints. The size of the columns is primarily determined by the speed at which lava from a volcanic eruption cools. The extensive fracture network produced the distinctive columns seen today. The basalts were originally part of a great volcanic plateau called the Thulean Plateau which formed during the Paleogene period.


[youtube https://www.youtube.com/watch?v=HjtqlhW1WMI?rel=0]


According to legend, the columns are the remains of a causeway built by a giant. The story goes that the Irish giant Fionn mac Cumhaill (Finn MacCool) was challenged to a fight by the Scottish giant Benandonner. Fionn accepted the challenge and built the causeway across the North Channel so that the two giants could meet. In one version of the story, Fionn defeats Benandonner. In another, Fionn hides from Benandonner when he realises that his foe is much bigger than him. Fionn's wife, Úna, disguises Fionn as a baby and tucks him in a cradle. When Benandonner sees the size of the 'baby', he reckons that its father, Fionn, must be a giant among giants. He flees back to Scotland in fright, destroying the causeway behind him so that Fionn could not follow. Across the sea, there are identical basalt columns (a part of the same ancient lava flow) at Fingal's Cave on the Scottish isle of Staffa, and it is possible that the story was influenced by this.


In Irish mythology, Fionn mac Cumhaill is not a giant but a hero with supernatural abilities. In Fairy and Folk Tales of the Irish Peasantry (1888) it is noted that, over time, "the pagan gods of Ireland grew smaller and smaller in the popular imagination, until they turned into the fairies; the pagan heroes grew bigger and bigger, until they turned into the giants". There are no surviving pre-Christian stories about the Giant's Causeway. However, it may have originally been associated with the Fomorians (Fomhóraigh); the Irish name Clochán na bhFomhóraigh or Clochán na bhFomhórach means "stepping stones of the Fomhóraigh". The Fomhóraigh are a race of supernatural beings in Irish mythology who were sometimes described as giants and who may have originally been part of a pre-Christian pantheon.

Cappadocia, Turkey

Cappadocia is a historical region in Central Anatolia, largely in Nevsehir Province, in Turkey. In the time of Herodotus, the Cappadocians were reported as occupying the whole region from Mount Taurus to the vicinity of the Euxine (Black Sea). Cappadocia, in this sense, was bounded in the south by the chain of the Taurus Mountains that separate it from Cilicia, to the east by the upper Euphrates and the Armenian Highland, to the north by Pontus, and to the west by Lycaonia and eastern Galatia.




[caption id="attachment_531" align="aligncenter" width="1600"]Cappadocia, Turkey Cappadocia, Turkey[/caption]

The name (Cappadocia) was traditionally used in Christian sources throughout history and is still widely used as an international tourism concept to define a region of exceptional natural wonders, in particular characterized by fairy chimneys and a unique historical and cultural heritage.


Cappadocia is a popular tourist destination, as it has many areas with unique geological, historic, and cultural features. The region is located southwest of the major city Kayseri, which has airline and railway service to Ankara and Istanbul. The most important towns and destinations in Cappadocia are Urgup, Goreme, Ihlara Valley, Selime, Guzelyurt, Uchisar, Avanos and Zelve. Among the underground cities worth seeing are Derinkuyu, Kaymakli, Gaziemir and Ozkanak. The best historic mansions and cave houses for tourist stays are in Urgup, Goreme, Guzelyurt and Uchisar.


Hot-air ballooning is very popular in Cappadocia and is available in Goreme. Trekking is enjoyed in Ihlara Valley, Monastery Valley (Guzelyurt), Urgup and Goreme. Sedimentary rocks formed in lakes and streams and ignimbrite deposits that erupted from ancient volcanoes approximately 9 to 3 million years ago, during the late Miocene to Pliocene epochs, underlie the Cappadocia region. The rocks of Cappadocia near Göreme eroded into hundreds of spectacular pillars and minaret-like forms. People of the villages at the heart of the Cappadocia Region carved out houses, churches and monasteries from the soft rocks of volcanic deposits. Göreme became a monastic centre in 300—1200 AD.


[youtube https://www.youtube.com/watch?v=7mRGItobR2U?rel=0]


The first period of settlement in Göreme goes back to the Roman period. The Yusuf Koç, Ortahane, Durmus Kadir and Bezirhane churches in Göreme, and houses and churches carved into rocks in the Uzundere, Bağıldere and Zemi Valleys all illustrate history and can be seen today. The Göreme Open Air Museum is the most visited site of the monastic communities in Cappadocia (see Churches of Göreme, Turkey) and is one of the most famous sites in central Turkey. The complex contains more than 30 carved-from-rock churches and chapels, some having superb frescoes inside, dating from the 9th century to the 11th century.

Libyan Desert (Waw an Namus), Libya

Waw an Namus (Caldera of Mosquitoes) is a volcanic field, cone and caldera in the southern Fezzan region of southern Libya. It is in the near-geographic center of the Sahara Desert.


The inside of the caldera houses an oasis of rich foliage and three small salt lakes of variable color which are the reason for the volcano's name. A volcanic field of dark basaltic tephra flow extends 10–20 kilometres (6.2–12 mi) around the caldera. The dark field's vast size allows it to be easily seen from space.




[caption id="attachment_526" align="aligncenter" width="1944"]Waw an Namus Waw an Namus[/caption]

The Libyan Desert, which covers much of Libya, is one of the most arid places on earth. In places, decades may pass without rain, and even in the highlands rainfall seldom happens, once every 5–10 years. At Uweinat, as of 2006 the last recorded rainfall was in September 1998. There is a large depression, the Qattara Depression, just to the south of the northernmost scarp, with Siwa Oasis at its western extremity. The depression continues in a shallower form west, to the oases of Jaghbub and Jalu.


Likewise, the temperature in the Libyan desert can be extreme; on 13 September 1922 the town of 'Aziziya, which is located southwest of Tripoli, recorded an air temperature of 57.8 °C (136.0 °F), considered to be a world record. In September 2012, however, the world record figure of 57.8°C was overturned by the World Meteorological Organization.


[youtube https://www.youtube.com/watch?v=R0TFuV9nRhg?rel=0]


There are a few scattered uninhabited small oases, usually linked to the major depressions, where water can be found by digging to a few feet in depth. In the west there is a widely dispersed group of oases in unconnected shallow depressions, the Kufra group, consisting of Tazerbo, Rebianae and Kufra. Aside from the scarps, the general flatness is only interrupted by a series of plateaus and massifs near the centre of the Libyan Desert, around the convergence of the Egyptian-Sudanese-Libyan borders.


Slightly further to the south are the massifs of Arkenu, Uweinat and Kissu. These granite mountains are ancient, having formed long before the sandstones surrounding them. Arkenu and Western Uweinat are ring complexes very similar to those in the Aïr Mountains. Eastern Uweinat (the highest point in the Libyan Desert) is a raised sandstone plateau adjacent to the granite part further west. The plain to the north of Uweinat is dotted with eroded volcanic features. With the discovery of oil in the 1950s also came the discovery of a massive aquifer underneath much of the country. The water in this aquifer pre-dates the last ice ages and the Sahara desert itself. This area also contains the Arkenu structures, which have been hypothesized to be double impact craters.

Namaqualand, Namibia

Namaqualand is an arid region of Namibia and South Africa, extending along the west coast over 600 miles (970 km) and covering a total area of 170,000 square miles/440,000 km². It is divided by the lower course of the Orange River into two portions - Little Namaqualand to the south and Great Namaqualand to the north. Little Namaqualand is within the Namakwa District Municipality and forms part of Northern Cape Province, South Africa. A typical municipality is Kamiesberg Local Municipality. Great Namaqualand is in the Karas Region of Namibia. Great Namaqualand is sparsely populated by the Namaqua, a Khoikhoi people who traditionally inhabited the Namaqualand region.




[caption id="attachment_519" align="aligncenter" width="3872"]Namaqualand Namaqualand[/caption]

Some of the more prominent towns in this area are Springbok, being the capital of this region, as well as Kleinzee and Koiingnaas, both private mining towns owned by De Beers Diamond Mines. This area is quite rich in alluvial diamonds deposited along the coast by the Orange River. Oranjemund is another mining town along this coast, situated in Namibia but very much on the border. As the name suggests, it is at the mouth of the Orange River which forms the border between South Africa and Namibia. The town of Alexander Bay is located 3 miles (5 km) away opposite the river on the South African side and is linked to Oranjemund by the Ernest Oppenheimer Bridge. Other links crossing the river further upstream are a re-introduced pontoon at Sendelingsdrift in the Richtersveld National Park, and road bridges at Vioolsdrif (the main border crossing between the two countries) and at the remote border crossing of Onseepkans.
There is a vibrant fishing industry along this stretch of the South African west coast. Especially in Port Nolloth, the major resort town of Namaqualand, and Hondeklipbaai, or Dogstonebay. Called such because of a large boulder outside the town which, when viewed correctly looks vaguely like a dog sitting down. Since the 19th century copper has been mined at Springbok and its surrounding towns, while a large mine extracting copper, lead, zinc and silver is located at Aggeneys, 70 miles (113 km) further inland.


Namaqualand is quite popular with both local and international tourists during early springtime, when for a short period this normally arid area becomes covered with a kaleidoscope of colour during the flowering season. This is known throughout South Africa as the Namaqualand daisy season, when orange and white daisies, as well as hundreds of other flowering species, spring up from a previously barren landscape. A part of Little Namaqualand, known as the Richtersveld, is a national park and a World Heritage Site, while the often-visited Namaqua National Park and the Goegap Nature Reserve are located short distances from Kamieskroon and Springbok respectively.As a region it has one of the highest percentages of Afrikaans speakers in the world, with over 95% of the population speaking the Afrikaans Language. The original Khoekhoe language of the Nama people, with its intricate system of click sounds, also still survives in remote areas.

Racetrack Playa, United States

The Racetrack Playa, or The Racetrack, is a scenic dry lake feature with "sailing stones" that leave linear "racetrack" imprints. It is located above the northwestern side of Death Valley, in Death Valley National Park.


Tanah Lot, Bali

Tanah Lot is a rock formation off the Indonesian island of Bali. It is home of a pilgrimage temple, the Pura Tanah Lot (literally "Tanah Lot temple"), and a popular tourist and cultural icon for photography and general exoticism. Tanah Lot means "Land Sea" in the Balinese language. Located in Tabanan, about 20 kilometres (12 mi) from Denpasar, the temple sits on a large offshore rock which has been shaped continuously over the years by the ocean tide.


tanah_lot_pct1


Tanah Lot is claimed to be the work of the 15th-century priest Nirartha. During his travels along the south coast he saw the rock-island's beautiful setting and rested there. Some fishermen saw him, and bought him gifts. Nirartha then spent the night on the little island. Later he spoke to the fishermen and told them to build a shrine on the rock for he felt it to be a holy place to worship the Balinese sea gods.


The Tanah Lot temple was built and has been a part of Balinese mythology for centuries. The temple is one of seven sea temples around the Balinese coast. Each of the sea temples were established within eyesight of the next to form a chain along the south-western coast. However, the Tanah Lot temple had significant Hindu influence. At the base of the rocky island, poisonous sea snakes are believed to guard the temple from evil spirits and intruders. A giant snake purportedly protects the temple, which was created from Nirartha's scarf when he established the island.


[youtube https://www.youtube.com/watch?v=LYGZqXpz0t8?rel=0]


In 1980, Tanah Lot's rock face was starting to crumble and the area around and inside the temple started to become dangerous. The Japanese government then provided a loan to the Indonesian government of Rp 800 billion (approximately USD $130 million) to conserve the historic temple and other significant locations around Bali. As a result, over one third of Tanah Lot's "rock" is actually cleverly disguised artificial rock created during the Japanese-funded and supervised renovation and stabilization program.

Papakolea Beach, United States

Papakōlea Beach (also known as Green Sand Beach or Mahana Beach) is a green sand beach located near South Point, in the Kaū district of the island of Hawaii. One of only two green sand beaches in the World, the other being in Galapagos Islands. It gets its distinctive coloring from the mineral olivine, found in the enclosing cinder cone.

Phi Phi Islands, Thailand

The Phi Phi Islands are located in Thailand, between the large island of Phuket and the western Andaman Sea coast of the mainland. The islands are administratively part of Krabi province. Ko Phi Phi Don meaning "island" in the Thai language) is the largest island of the group, and is the only island with permanent inhabitants, although the beaches of the second largest island, Ko Phi Phi Lee (or "Ko Phi Phi Leh"), are visited by many people as well. The rest of the islands in the group, including Bida Nok, Bida Noi, and Bamboo Island (Ko Mai Phai), are not much more than large limestone rocks jutting out of the sea.




[caption id="attachment_469" align="aligncenter" width="1024"]Phi Phi Islands Phi Phi Islands[/caption]

Phi Phi Don was initially populated by Muslim fishermen during the late 1940s, and later became a coconut plantation. The Thai population of Phi Phi Don remains more than 80% Muslim. The actual population however, if counting laborers, especially from the north-east, from the mainland is much more Buddhist these days. The islands came to worldwide prominence when Ko Phi Phi Leh was used as a location for the 2000 British-American film The Beach. This attracted criticism, with claims that the film company had damaged the island's environment, since the producers bulldozed beach areas and planted palm trees to make it look like the book, an accusation the film's makers contest. The film's release was attributed to an increase in tourism to the islands. Phi Phi Leh also houses the 'Viking Cave', from which there is a thriving bird's nest soup industry. Ko Phi Phi was devastated by the Indian Ocean Tsunami of December 2004, when nearly all of the island's infrastructure was destroyed. As of 2010 most, but not all, of this has been restored.


From archaeological discoveries, it is believed that the area was one of the oldest communities in Vietnam, dating back to the prehistoric period. It is believed that this province may have taken its name from Krabi, which means sword. This may come from a legend that an ancient sword was unearthed prior to the city’s founding. The name Phi Phi (pronounced ‘pee pee’) originates from Malay, the original name for the islands were Pulau Api-Api (The Fiery Isle). The name refers to the Pokok Api-Api, which literary translated as the Fiery Tree (Grey Mangrove) which is commonly found throughout the Island. They were incorporated into the national park in 1983.


[youtube http://www.youtube.com/watch?v=DTKH_jE9syk?rel=0]


Recent researchs show the Turkish traces all over the island. Turks, especially from Nigde and Yozgat provinces, invaded island in mid 1970's. At the moment they keep all transportation sector with the special vehicle called as minibus. They also established some charity organizations such as "Phi Phi & Schefaatli Dayanisma Dernegi", "Fertek Kultur ve Dayanisma Dernegi", "Phi-Phi Yozgat Dostluk Dernegi". Also in Turkish, there is a saying "çok da fi fi" meaning; "so very phi phi". It captures the relax mood of the Phi Phi people.


There are six islands in the group known as Phi Phi. They lie 50 km south-east of Phuket and are part of Hadnopparattara-Koh Phi Phi National Park which is home to an abundance of corals and marine life. There are limestone mountains with cliffs, caves and long white sandy beaches. The national park covers a total area of 242,437 Rai. Phi Phi Don and Phi Phi Le are the largest and most well-known islands. Phi Phi Don is 28 sqkm: 8 km in length and 3.5 km wide. Phi Phi Le is 6.6 km.

Cave of the Crystals, Mexico

Cave of the Crystals or Giant Crystal Cave (Spanish: Cueva de los Cristales) is a cave connected to the Naica Mine 300 metres (980 ft) below the surface in Naica, Chihuahua, Mexico. The main chamber contains giant selenite crystals (gypsum, CaSO4·2 H2O), some of the largest natural crystals ever found. The cave's largest crystal found to date is 12 m (39 ft) in length, 4 m (13 ft) in diameter and 55 tons in weight. The cave is extremely hot with air temperatures reaching up to 58 °C (136 °F) with 90 to 99 percent humidity. The cave is relatively unexplored due to these factors. Without proper protection people can only endure approximately ten minutes of exposure at a time.

Carlsbad Caverns, United States

Carlsbad Caverns National Park is a United States National Park in the Guadalupe Mountains in southeastern New Mexico. The primary attraction of the park is the show cave, Carlsbad Cavern. Carlsbad Caverns National Park is open every day of the year except Christmas Day. Visitors to the cave can hike in on their own via the natural entrance or taken an elevator from the visitor center.

Fiordland, New Zealand

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".

Lau Islands, Fiji

The Lau Islands (also called the Lau Group, the Eastern Group, the Eastern Archipelago) of Fiji are situated in the southern Pacific Ocean, just east of the Koro Sea. Of this chain of about one hundred islands and islets, about thirty are inhabited. The Lau Group covers a land area of 188 square miles (487 square km), and had a population of 10,683 at the most recent census in 2007. While most of the northern Lau Group are high islands of volcanic origin, those of the south are mostly carbonate low islands.

Halong Bay, Vietnam

Ha Long Bay is a UNESCO World Heritage Site, and a popular travel destination, located in Quang Ninh province, Vietnam. Administratively, the bay belongs to Ha Long City, and part of Van Don district. The bay features thousands of limestone karsts and isles in various sizes and shapes. Ha Long Bay is a center of a larger zone which includes Bái To Long bay to the northeast, and Cát Bà islands to the southwest. These larger zones share similar geological, geographical, geomorphological, climate, and cultural characters.

Moeraki Boulders, New Zealand

The Moeraki Boulders are unusually large and spherical boulders lying along a stretch of Koekohe Beach on the wave cut Otago coast of New Zealand between Moeraki and Hampden. They occur scattered either as isolated or clusters of boulders within a stretch of beach where they have been protected in a scientific reserve. The erosion by wave action of mudstone, comprising local bedrock and landslides, frequently exposes embedded isolated boulders. These boulders are grey-colored septarian concretions, which have been exhumed from the mudstone enclosing them and concentrated on the beach by coastal erosion.




[caption id="attachment_383" align="aligncenter" width="750" caption="Moeraki Boulders, New Zealand"]Moeraki Boulders, New Zealand[/caption]

Local Māori legends explained the boulders as the remains of eel baskets, calabashes, and kumara washed ashore from the wreck of an Arai-te-uru, a large sailing canoe. This legend tells of the rocky shoals that extend seaward from Shag Point as being the petrified hull of this wreck and a nearby rocky promontory as being the body of the canoe's captain. In 1848 W.B.D. Mantell sketched the beach and its boulders, more numerous than now. The picture is now in the Alexander Turnbull Library in Wellington. The boulders were described in 1850 colonial reports and numerous popular articles since that time. In more recent times they have become a popular tourist attraction, often described and pictured in numerous web pages and tourist guides.


The Moeraki Boulders are concretions created by the cementation of the Paleocene mudstone of the Moeraki Formation, from which they have been exhumed by coastal erosion. The main body of the boulders started forming in what was then marine mud, near the surface of the Paleocene sea floor. This is demonstrated by studies of their composition; specifically the magnesium and iron content, and stable isotopes of oxygen and carbon. Their spherical shape indicates that the source of calcium was mass diffusion, as opposed to fluid flow. The larger boulders, 2 metres (6.6 feet) in diameter, are estimated to have taken 4 to 5.5 million years to grow while 10 to 50 metres (33 to 165 feet) of marine mud accumulated on the seafloor above them. After the concretions formed, large cracks known as septaria formed in them. Brown calcite, yellow calcite, and small amounts of dolomite and quartz progressively filled these cracks when a drop in sea level allowed fresh groundwater to flow through the mudstone enclosing them.


[youtube http://www.youtube.com/watch?v=lYFUDZ6nK1Y?rel=0]

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.




[caption id="attachment_390" align="aligncenter" width="750"]Bay of Fundy, Canada 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.




[caption id="attachment_369" align="aligncenter" width="600" caption="Big Sur and Highway 1"]Big Sur and Highway 1[/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.




[caption id="attachment_370" align="aligncenter" width="600" caption="Big Sur and nature"]Big Sur and nature[/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.

The Great Dune of Pyla, France

The Great Dune of Pyla (or Pilat) is the tallest sand dune in Europe. It is located in La Teste-de-Buch in the Arcachon Bay area, France, 60 km from Bordeaux. Pilat is sometimes spelled Pyla, hence the alternative name "dune of Pyla". More accurately, Pyla is the name of the closest town, Pyla-sur-Mer, which is part of La Teste-de-Buch municipality in the Gironde department. The correct and original name of the dune is the Dune of Pilat, but because of the confusion that occurred, both are now considered correct.


The dune has a volume of about 60,000,000 m³, measuring around 500 m wide from east to west and 3 km in length from north to south. Its height is 107 metres above sea level. The dune is a famous tourist destination with more than one million visitors per year.




[caption id="attachment_349" align="aligncenter" width="610" caption="Great Dune of Pyla"]Great Dune of Pyla[/caption]

The dune is considered a foredune, meaning a dune that runs parallel to a shoreline, behind the high tide line of a beach. The dune has been observed to move landward, slowly pushing the forest back to cover houses, roads and even portions of the Atlantic Wall. To back this evidence of coastal movement, maps from 1708 and 1786 both place areas with the name Pilat to the south and off-shore of the current dune's location. The area where the dune currently stands was referred to "Les Sabloneys" or the "New Sands" until the 1930's when it was renamed by real estate developers as the Dune of Pilat. The Dune of Pyla is a recent modernization of the term. Pilat originates from the Gascon word Pilhar, which refers to a heap or mound.


Perhaps many will be surprised to find out that the dune is quite recent, being formed between the 17th and the 19th century, the sand from several other dunes being blown in this location by the strong winds coming from the Atlantic. The entire phenomenon was generated by the sand in the Arcachon Gulf and by the migration of the southern canal, which produced a sever erosion of the eastern shore. Based on historical evidence, between 1826 and 1922 the entire coast around the Pyla dune has been eroded by 1,650 feet and all the plants and trees covering the western side of the La Grave dune has been destroyed. Without any plants to hold the soil in place, the sands were moved by the wind towards the Pyla dune and stored around the pine trees surrounding the dune.

Fly Geyser, United States

Fly Geyser, also known as Fly Ranch Geyser is a small geothermal geyser that is located approximately 20 miles (32 km) north of Gerlach, in Washoe County, Nevada. The Geyser is located in Hualapai Flat, about 1/3 of a mile from State Route 34. It is large enough to be seen from the road. Fly Geyser is located on the private Fly Ranch and is accessible only by a small private dirt road. The ranch is currently owned by Todd Jaksick. There is a high fence and a locked gate with several metal spokes on the top to keep trespassers out, but despite the booby traps, many people still prefer to jump the fence to get a better look. Several organizations have tried to purchase the land for conservation, and make it open to the public, but have been denied.




[caption id="attachment_324" align="aligncenter" width="640" caption="Fly Geyser, Nevada"]Fly Geyser, Nevada[/caption]

Fly Geyser is a very little known tourist attraction, even to Nevada residents. It is located right near the edge of Fly Reservoir and is only about 5 feet (1.5 m) high, (12 feet (3.7 m) if you count the mound on which it sits). The Geyser is not an entirely natural phenomenon, and was accidentally created in 1916 during the drilling of a well. The well functioned normally for several decades, but then in the 1960s geothermally heated water found a weak spot in the wall and began escaping to the surface. Dissolved minerals started rising and piling up, creating the mount on which the geyser sits, which is still growing to date. Today, water is constantly squirting out reaching 5 feet (1.5 m) in the air. The geyser contains several terraces discharging water into 30 to 40 pools over an area of 30 hectares (74 acres). The geyser is made up of a series of different minerals, which gives it its magnificent coloration.


[youtube http://www.youtube.com/watch?v=jXhl5oKzCCg?rel=0]


There are two additional geysers in the area that were created in a similar way as Fly Geyser. The first geyser is approximately 3 feet high and is shaped like a miniature volcano. The second geyser is cone shaped and is of the same approximate size as Fly Geyser. Like Fly Geyser, these geysers are continually growing.

Aurora Borealis, North Pole

An aurora is a natural light display in the sky particularly in the high latitude (Arctic and Antarctic) regions, caused by the collision of energetic charged particles with atoms in the high altitude atmosphere (thermosphere). The charged particles originate in the magnetosphere and solar wind and, on Earth, are directed by the Earth's magnetic field into the atmosphere. Aurora is classified as diffuse or discrete aurora. Most aurorae occur in a band known as the auroral zone which is typically 3° to 6° in latitudinal extent and at all local times or longitudes. The auroral zone is typically 10° to 20° from the magnetic pole defined by the axis of the Earth's magnetic dipole. During a geomagnetic storm, the auroral zone will expand to lower latitudes. The diffuse aurora is a featureless glow in the sky which may not be visible to the naked eye even on a dark night and defines the extent of the auroral zone. The discrete aurora are sharply defined features within the diffuse aurora which vary in brightness from just barely visible to the naked eye to bright enough to read a newspaper at night. Discrete aurorae are usually observed only in the night sky because they are not as bright as the sunlit sky. Aurorae occur occasionally poleward of the auroral zone as diffuse patches[3] or arcs (polar cap arcs) which are generally invisible to the naked eye.



In northern latitudes, the effect is known as the aurora borealis (or the northern lights), named after the Roman goddess of dawn, Aurora, and the Greek name for the north wind, Boreas, by Pierre Gassendi in 1621. Auroras seen near the magnetic pole may be high overhead, but from farther away, they illuminate the northern horizon as a greenish glow or sometimes a faint red, as if the Sun were rising from an unusual direction. Discrete aurorae often display magnetic field lines or curtain-like structures, and can change within seconds or glow unchanging for hours, most often in fluorescent green. The aurora borealis most often occurs near the equinoxes. The northern lights have had a number of names throughout history. The Cree call this phenomenon the "Dance of the Spirits". In Europe, in the Middle Ages, the auroras were commonly believed a sign from God (see Wilfried Schröder, Das Phänomen des Polarlichts, Darmstadt 1984). Its southern counterpart, the aurora australis (or the southern lights), has almost identical features to the aurora borealis and changes simultaneously with changes in the northern auroral zone and is visible from high southern latitudes in Antarctica, South America, New Zealand and Australia. Aurorae occur on other planets. Similar to the Earth's aurora, they are visible close to the planet's magnetic poles. Modern style guides recommend that the names of meteorological phenomena, such as aurora borealis, be uncapitalized.


In the past theories have been proposed to explain the phenomenon. These theories are now obsolete. Seneca speaks diffusely on auroras in the first book of his Naturales Quaestiones, drawing mainly from Aristotle; he classifies them ("putei" or wells when they are circular and "rim a large hole in the sky", "pithaei" when they look like casks, "chasmata" from the same root of the English chasm, "pogoniae" when they are bearded, "cyparissae" when they look like cypresses), describes their manifold colors and asks himself whether they are above or below the clouds. He recalls that under Tiberius, an aurora formed above Ostia, so intense and so red that a cohort of the army, stationed nearby for fireman duty, galloped to the city. Benjamin Franklin theorized that the "mystery of the Northern Lights" was caused by a concentration of electrical charges in the polar regions intensified by the snow and other moisture.


[youtube http://www.youtube.com/watch?v=Ip2ZGND1I9Q?rel=0]


Auroral electrons come from beams emitted by the Sun. This was claimed around 1900 by Kristian Birkeland, whose experiments in a vacuum chamber with electron beams and magnetized spheres (miniature models of Earth or "terrellas") showed that such electrons would be guided towards the polar regions. Problems with this model included absence of aurora at the poles themselves, self-dispersal of such beams by their negative charge, and more recently, lack of any observational evidence in space. The aurora is the overflow of the radiation belt ("leaky bucket theory"). This was first disproved around 1962 by James Van Allen and co-workers, who showed that the high rate of energy dissipation by the aurora would quickly drain the radiation belt. Soon afterward, it became clear that most of the energy in trapped particles resided in positive ions, while auroral particles were almost always electrons, of relatively low energy.


The aurora is produced by solar wind particles guided by Earth's field lines to the top of the atmosphere. This holds true for the cusp aurora, but outside the cusp, the solar wind has no direct access. In addition, the main energy in the solar wind resides in positive ions; electrons only have about 0.5 eV (electron volt), and while in the cusp this may be raised to 50–100 eV, that still falls short of auroral energies. After the Battle of Fredericksburg the lights could be seen from the battlefield that night. The Confederate army took it as a sign that God was on their side during the battle. It was very rare that one could see the Lights in Virginia.