Jumat, 25 Mei 2012

10 WORLD MOST UNIQUE TOURIST ATTRACTION


10. THE CHOCOLATE HILLS, BOHOL PHILIPINES


Chocolate Hills
            The Chocolate Hills are probably Bohol's most famous tourist attraction. They look like giant mole hills, or as some say, women's breasts, and remind us of the hills in a small child's drawing. Most people who first see pictures of this landscape can hardly believe that these hills are not a man-made artifact. However, this idea is quickly abandoned, as the effort would surely surpass the construction of the pyramids in Egypt. The chocolate hills consist of are no less than 1268 hills (some claim this to be the exact number). They are very uniform in shape and mostly between 30 and 50 meters high. They are covered with grass, which, at the end of the dry season, turns chocolate brown. From this color, the hills derive their name. At other times, the hills are green, and the association may be a bit difficult to make.
            Legend has it that the hills came into existence when two giants threw stones and sand at each other in a fight that lasted for days. When they were finally exhausted, they made friends and left the island, but left behind the mess they made. For the more romantically inclined is the tale of Arogo, a young and very strong giant who fell in love with an ordinary mortal girl called Aloya. After she died, the giant Arogo cried bitterly. His tears then turned into hills, as a lasting proof of his grief.
            However, up to this day, even geologists have not reached consensus on how they where formed. The most commonly accept theory is that they are the weathered formations of a kind of marine limestone on top of a impermeable layer of clay. If you climb the 214 steps to the top of the observation hill near the complex, you can read this explanation on a bronze plaque.
Chocolate Hills

9. MARIANA TRENCH, PASIFIC OCEAN


            The Mariana Trench is located in the Pacific Ocean, just east of the 14 Mariana Islands (11"21' North latitude and 142" 12' East longitude ) near Japan.   As you probably already know, it is the deepest part of the earth's oceans, and the deepest location of the earth itself.  It was created by ocean-to-ocean subduction, a phenomena in which a plate topped by oceanic crust is subducted beneath another plate topped by oceanic crust. The deepest part of the Mariana Trench is the Challenger Deep, so named after the exploratory vessel HMS Challenger II; a fishing boat converted into a sea lab by  Swiss scientist Jacques Piccard. 
             On this site,  you will find information on the main characteristics of the Mariana Trench, its exploration, and its ecosystem. The Biology section of the site covers the fish and various (organisms and microorganisms) of the deep, what makes these creatures unique, and the fascinating ways in which they live and survive. The Oceanography section explores the data pertaining to the Mariana Trench and other deep sea formations.The Exploration section relates some of the events pertaining to the first survey of the MT, and the history of deep sea  exploration.
            We have also included a section on the Mariana Arc, from an article published by NOAA (National Oceanic and Atmospheric Administration) Magazine Online.  In addition to this, we also added a nautical measurement conversion table, so that you mayIn closing we have added two supplemental sections so that you may continue your research into the fascinating world of the deep.  Whether you are seeking answers to questions about the Mariana Trench, or are simply interested in Marine Biology, Oceanography, or related subjects, we hope our site will help you better understand the mysteries of the ocean floor.




8. PAMUKKALE SPRING, TURKEY


            The hot springs of Pamukkale can be found trickling down the white cliffs of Pamukkale in southern Turkey. The cliffs cascade downward in a widening series of steps from a plateau more than 100m (300ft) high on Cal Da?i mountain. Water constantly bubbles up from thermal springs under the plateau and emerges into the air at around 38°C (98.5°F). As it journeys underground to the surface, this warm water passes through beds of limestone, dissolving calcium carbonate from the rock.
         
   As the water flows over the edge of Pamukkale's escarpment, it cools and loses its ability to hold the mineral in solution. Consequently, the calcium carbonate, known in its solid form as travertine, gradually and continually precipitates out of solution as it descends the cliff face.The graded steps on the cliff face are formed by Pamukkale's many scallop-shaped, water-filled pools. Because the outer margins of a pool cool first, the travertine precipitates at a faster rate here than at the centre. As the pools continue to deposit travertine, they grow slowly upward, and after many years create a series of "columns".
            Water that steadily spills over a pool's raised edges trickles down the outside of the "column", depositing more travertine as a growing outer skin.By constantly adding fresh layers of travertine to the cliffs, the mineral-rich water prevents plants from gaining a foothold and the elements from weathering Pamukkale into a dull, shapeless mass.The name Pamukkale is Turkish for "cotton castle".




7. SALAR DE UYUNI, BOLIVIA


            World's largest salt lake known as Salar de Uyuni (Uyuni salt flat) is a visually captivating place, one of the most stunningly beautiful places you will ever come across in Bolivia and South America. A surreal vision in the Bolivian Altiplano created by amazing geological formations, geothermal springs and brine lakes.
            Covering an area of over 10,000 square km. in the departmentes of Oruro and Potosi (SW Bolivia), Salar de Uyuni is estimated to have a reserve of 10 billion tons of salt. Some 40,000 years ago the region was covered by the giant salt lake Minchin. At some point the lake dried, leaving behind two small lakes (Poopó and Uri Uri) plus two salt lakes: Coipasa and Uyuni.
            The vast expanse of salt in Salar de Uyuni will definitely leave you amazed by its beauty and its mere existence. Salt can be as thick as ten meters in the center and during wet seasons, the vast expanse will be covered with water.Most tours that include Salar de Uyuni will also offer you other various attractions that are also breathtaking. Another common attraction that you can also see when going on tour is Laguna Hedionda and Isla de Pescados which are both spectacular.



6. GUAIRA FALLS, BRAZIL-PARAGUAY BORDER

If you’ve ever seen Niagara Falls, you know the tremendous amount of water that tumbles over the edge of the falls each second. Could you believe there’s a waterfall with a flow more than twice as great as Niagara?
This waterfall, known as Guaira, is on the Parana River, on the border between Paraguay and Brazil. In Brazil, the waterfall is known as Sete Quedas. Guaira is just ,ver three miles wide, and only about 110 feet high. But Guaira has the largest .iverage flow of any single waterfall on earth.
On the average, about 212,000 cubic feet of water passes over Niagara Falls each second. The average flow of Guaira is 470,000 cubic feet per second. And during seasons when the Parana River is high, the flow over Guaira can reach 1.7 million cubic feet per second!









5. METEOR CRATER, USA


            The story of the Barringer Meteorite Crater is a story about the collisions and impacts that have shaped the Earth and other planets in our solar system. But it is also a story about how we know what we know about craters, meteorites, and the planet we live on.
            The crater is named for Daniel Moreau Barringer, a Philadelphia mining engineer. Barringer was one of the first people to claim that the crater was the result of an impact, contradicting the most eminent scientists of his time. Though he never found the fortune in meteoritic iron he was convinced lay beneath the floor of the crater, Barringer’s theory of the crater’s origin was eventually vindicated and accepted by the scientific community.
            The story of the crater is the story of scientific discovery, and of the heated debates and complex personal histories that make discovery possible. It is a story about how we have come to understand our world, and it begins 50,000 years ago, high above the Arizona desert.

4. SOCOTRA, REPUBLIK OF YAMEN


            The Socotra Archipelago is a part of the Republic of Yemen.  Located in the northwestern Indian Ocean, about 350 km south of the Arabian peninsula.  The archipelago consists of the main island of Socotra and three smaller islands:  Abd Al Kuri: 25x5 km, about 200 inhabitants, reachable in 10 hours by boat from Qalansiya Samha: 10x5 km, about 60 inhabitants, reachable in 4 hours by boat from Qalansiya Darsa: not inhabited
            The long geological isolation from Arabia and Africa has resulted in very high levels of endemism. 308 endemic plants (36 % of the total),  36 endemic vertebrates (reptiles, birds), more than  300 species of endemic invertebrates are found on the islands.  Rich marine diversity: to-date 33 genera of hermatic corals found; 3 possible endemic species including an ophichthis-like eel which may be new to science
            Socotra is the  9th of ten most important islands in the world, in terms of biodiversity conservation importance. (Millet et al. 1996, Royal Botanical Garden Edinburgh) One of the Globe 200 important eco regions (according to WWF). Socotra forms  one of the world’s 221 globally important Endemic Bird Areas (BirdLife International recognizes 22 Important Bird Areas on the islands) International Union for Conservation of Nature (IUCN) names 52 endemic Socotri plants in the  Red List of Threatened Species.

3. MOUNT RORAIMA, SOUTH AMERIKA

Mount Roraima (mountain, South America) giant flat-topped mountain, or mesa, in the Pakaraima Mountains of the Guiana Highlands , at the point where the boundaries of Brazil, Venezuela, and Guyana meet. About 9 miles (14 km) long and 9,094 feet (2,772 metres) high, it is the source of many rivers of Guyana, and of the Amazon and Orinoco. Mount Roraima is a pretty remarkable place. It is a tabletop mountain with sheer 400-metre high cliffs on all sides. There is only one ‘easy’ way up, on a natural staircase-like ramp on the Venezuelan side – to get up any other way takes and experienced rock climber. On the top of the mountain it rains almost every day, washing away most of the nutrients for plants to grow and creating a unique landscape on the bare sandstone surface
                This also creates some of the highest waterfalls in the world over the sides (Angel falls is located on a similar tabletop mountain some 130 miles away). Though there are only a few marshes on the mountain where vegetation can grow properly, these contain many species unique to the mountain, including a species of carnivorous pitcher plant. The mountain marks the border between Venezuela, Brazil and Guyana, although more than three quarters of the mountain is in Venezuelan territory. It is the highest mountain in Guyana, but Venezuela and Brazil have higher mountains. The triple border point on the summit is at 5°12'08N, 60°44'07W. Roraima lies on the Guiana Shield in the southeastern corner of Venezuela's 30,000 km² Canaima National Park, which is roughly located in the Gran Sabana region . The tabletop mountains of the park are considered some of the oldest geological formations on Earth, dating back to the Precambrian Era, some two billion years ago.The average height of the plateau is about 2,500 metres (8,200 feet), making it the highest point for distance of 549.44 kilometres (341.48 miles) in any direction. The nearest peak that is taller is Cerro Marahuaca, to the west-southwest. Despite the fact the steep sides of the plateau make it difficult to access, it was the first major tepui to be climbed: Sir Everard im Thurn walked up a forested ramp in December 1884 to scale the strangely wind-and-water sculpted plateau. This is the same route hikers take today. It is thought that the reports from early Victorian expeditions to the mountain inspired Sir Arthur Conan Doyle to write his classic adventure yarn, The Lost World, in 1912 - now made into countless films.
                Since long before the arrival of European explorers in Venezuela the mountain has held a special significance for the indigenous people of the region and it is central to many of their myths and legends. The Pemon Indians of the Gran Sabana see Roraima as the stump of a mighty tree that once held all the fruits and tuberous vegetables in the world. Felled by one of their ancestors, the tree crashed to the ground, unleashing a terrible flood. "Roroi" in the Pemon language means blue-green and "ma" means great. Mount Roraima has been climbed on a few occasions from the Guyana and Brazil sides, but as the mountain is entirely bordered on both these sides by enormous sheer cliffs that include high overhanging (negative-inclination) stretches, these are extremely difficult and technical rock climbing routes


2. THE GREAT DUNE OF PYLA, FRANCE
                Largest sand dune in Europe is the great dune of Pyla. Size of sand dune of Pyla is about 60,000,000 cubic meters, It measures 1,640 feet (500 m) wide and 1.86 miles (3 km long), with the height ranging from 328 to 383.8 feet (100 to 117 m) above sea level. The Dune of Pilat is also known as the Great Dune of Pyla It is located in the La Teste-de-Buch of the Arcachon Bay area at 60Km from Bordeaux, in the South of the Arcachon Bay, it is possible to visit the highest dune in Europe, the Great Dune of Pyla (or Pilat)
                This hight of dune of Pyla reaches upto a height of 107m. At this summit, the view is spectacular with the ocean coast, the inlet of the Bay, the large pine forest and, when the sky is very clear, the Pyrenees Range. This Great Dune is constituted of fine sand which the siliceous grains have about the same size. Since about ten years, this area is also became a point of start to the lover of delta planes. The Great Dune of Pyla is located on the “La Teste de Buch” district (Gironde) and it is a national listed landscape. Since Europe has no deserts, you’d think the title of “Europe’s largest sand dune” would go to something that wasn’t particularly impressive. But you’d be wrong. The Great Dune of Pyla is 3km long, 500m wide and 100m high, and for reasons I will probably never understand, it seems to have formed in a forest. The dune is very steep on the side facing the forest and is famous for being a paragliding site. At the top it also provides spectacular views out to sea and over the forest (since the dune is far higher than any of the trees surrounding it). This unique place is great traveling opportunity for those who would like to experience how it is like to be in desert and this little version of desert is less than a hour of ride away from Bordeaux. A number of such smaller sand dunes can be found at the soul of sandy moor of Gascony. This dune is huge enough to be visible from the space. From above, it looks like huge white rectangle


1.THE DOOR TO HELL, TURKMENISTAN

                1971. A group of Soviet Scientists were rooting around the small village of Dervaza. The village crucially lies in the Ahal Province of Turkmenistan, an area known for its abundance in one useful resource… Natural Gas. They found it. A site was identified next to the village and preparations were made for the drilling rig and camp to be set up on site, so as to facilitate the gathering of the sweet, sweet combustible resource. There was, of course, an incident.On an undisclosed date shortly after completion, the drilling rig was drilling. Surrounding it was a cornucopia of equipment dotted around the drilling camp. Gas was rapidly pouring in and being stored for transportation and the Soviet Scientists were reveling in their success.In an instant the ground beneath the camp cracked and tore open, revealing a new crater 100 metres across. The camp and rig plummeted downwards, swallowed by the depths of this new menacing construct. It was a disaster none of them saw coming, fortunately no lives were lost. Despite the lack of injuries or deaths the Scientists were faced with a substantial problem, besides the massive new crater of course. The problem was the gas, of which there was a great deal. The Soviet Scientists recognised the threat, if left to its own devices, the crater would continue to pour out natural gas into the local atmosphere and poisoning the air itself and killing hundreds of people in the vicinity. This was undesirable to say the least. A plan was conceived.
                Firstly they would leave the camp and drilling rig down there, as you can imagine volunteers to enter the crater filled with poisonous gas were thin on the ground. Instead they would set the gas alight. This would prevent the air being poisoned and after a few days the crater should burn off any excess gas seeping through before the fires too died out. Then they could return and see what was salvageable from the camp. The plan worked. The gas was burnt, preventing the poisoning, and the crater kept burning over the next few days. It has been 40 years, the crater still burns. It is known as the,’Door to Hell.‘The cursed craters effects are noticeable to this day and have not made it a nice thing to be around.From its burning mouth pours the stench of sulphur, fouling the local air and making anything with nasal cavities flee from the vicinity. Were the stench not untenable not enough, the roaring flames in the crater do their part also. In addition it glows day and night, the leaping flames nested are so ferocious that they produce a hazy glow which can be seen from several miles away.
                In April 2010 the president of Turkmenistan ordered the fire to be quelled and the hole to be sealed so as to stop it removing gas from nearby gas drilling sites. While it is an amazing site that many would like to keep around we cannot expect it to last forever, the gas being burnt is much worse than Carbon Dioxide in its contributions to global warming. While the planet should preserve its places of oddity we must respect the environment.To this very day no-one knows where all of the gas is coming from and we may never understand quite how the,’Gateway to Hell ,’ has kept burning for 40 years.



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