Interesting Causeways in the World

A causeway is a road or railway route across a broad body of water or wetland raised up on an embankment. Some causeways may only be usable at low tide and the distinction between causeways and viaducts can become blurred when flood-relief culverts are incorporated in the structure; a causeway is however primarily supported on earth or stone, whereas a bridge or viaduct is mainly supported by free-standing columns or arches.



1. Great Salt Lake Causeway, USA


The causeway running across the Great Salt Lake, Utah, was built in the 1950s by the Morrison-Knudsen construction company for the Southern Pacific Railroad as a replacement to a previously built wooden trestle, and is now owned and operated by Union Pacific.



About 15 trains cross the 20-mile (32km) causeway each day. Because water flow is so constrained by the causeway, it has a significant impact on various industries. The salt discrepancy is visible to anyone who flies over the causeway. The water on the north side usually has a distinct reddish tint, while on the south side it's greenish-blue. The colors are attributed to different species of algae that thrive in different concentrations of salt.



The unusual color scheme is a direct result of the causeway. The original trestle allowed water to flow freely under the railroad tracks, but the causeway that replaced it essentially acts as a 20-mile (32km) dam. The salt imbalance developed over many years because the south arm of the lake gets nearly all the freshwater.



There are no significant creeks or rivers flowing into the north arm, while the south arm gets flushed continually by waters of the Jordan, Weber and Bear Rivers.



2. Hindenburg Dam, Germany


Hindenburg Dam is an 11 km-long (7mi) causeway joining the North Frisian island of Sylt to mainland Schleswig-Holstein. It was opened on 1 June 1927 and is exclusively a railway corridor. A train trip along the causeway takes about 10 minutes, and the time between the auto terminals at Niebüll on the mainland and Westerland on Sylt is about 30 minutes.



The Hindenburg Dam is part of the railway line known as the Marschbahn ("Marsh Railway"), which is double-tracked along much of the route, although there as yet exists a single-tracked stretch. On the causeway is a signal box. Every day, more than 100 trains pass over the causeway, 50 of those ferrying cars (there is no road link to Sylt).



Each year, the railway ferries more than 450,000 vehicles over the causeway. The causeway, which bears the Weimar Republic Reichspräsident Paul von Hindenburg's name, has interrupted the tidal flow, which until the causeway's appearance had flowed freely between Sylt and the mainland.



This change in tides, it is believed, is part of what has led to the loss of a certain amount of land at Sylt's southern end. The causeway lies in the specially protected Zone I of the Schleswig-Holsteinisches Wattenmeer National Park. Walks on the tidal flats are not allowed here, although they are quite popular elsewhere.



3. Passage du Gois, France


Le Passage de Gois ou Gôa is a natural, periodically flooded causeway leading to the island of Noirmoutier in France. It is located between Île de Noirmoutier and Beauvoir-sur-Mer, in the department of Vendée. Causeway is flooded twice a day by the high tide. Every year, a foot race – the Foulées du Gois– is held across it, starting at the onset of the high tide.



In 1999 Passage du Gois was used by Tour de France bicycle race during Stage 2. It proved to be decisive for the race after a fall took place because of its slippery surface.


Tour de France

The crash created a six minute split in the peloton which ended the hopes of many favourites to win the race, like Alex Zülle, who would eventually finish second overall, seven minutes after Lance Armstrong. Passage du Gois was used again in 2011 as the starting point of the first stage.



4. Funafuti Causeway, Tuvalu


Made up of four coral islands and five atolls off the coast of Australia, Tuvalu has a maximum height of only 4.5 meters (15 feet) above sea level. There's a section on island of Funafuti where the island was too narrow for a road, so they built this concrete section that they refer to as "the causeway".



This causeway is quite important for local traffic, because it connects the northern and southern part of the island. As you can see in the picture above, waves often wash over this causeway.



5. Causeway Between Jindo and Modo Islands, South Korea


The tide-related sea level variations result in a local phenomenon (a "Moses Miracle") when a land pass 2.9 km (1.8 mi) long and 10–40 meters (11-33 yds) wide opens for an hour between Modo and Jindo islands (Jindo County, South Jeolla province).



The event occurs approximately twice a year, around April-June. It had long been celebrated in a local festival called "Jindo's Sea Way", but was largely unknown to the world until 1975, when the French ambassador Pierre Randi described the phenomenon in a French newspaper. Nowadays, nearly half a million foreign and local tourists attend the event annually.



6. Rough Island Causeway, UK


Rough Island is accessible across the causeway from Kippford when the tides allow or across the mudflats from Rockcliffe, the isle of Rough can be walked to from the Scottish mainland.



As the island is a bird sanctuary visitors should avoid travelling to the island during the months of May and June to avoid disturbing the nesting oystercatchers and ringed plovers. The islands' causeway is flooded and underwater for 5 (five) hours during high tide and visitors to the island need to take this into account when travelling there.



7. Låningsvejen, Denmark


Mandø is one of the Danish Wadden Sea islands off the southwest coast of Jutland, Denmark in the Wadden Sea, part of the North Sea.



Island is barely accessible at high tide over an unpaved surface level causeway of about four kilometers (2.5 mi) in length that connects the island to the mainland.


Mandøbussen link

Låningsvejen is the name of this causeway which connects Mandø to the mainland in Jutland. It is a public road which you can use if you know the tides and when it is low tide. Only the two tractor busses “Mandø Traktorbus” and “Mandøbussen” are allowed to use “Ebbevejen”. They carry the post, school children and tourist to and from the island.



8. Colchester Causeway, USA


Along the edges of Lake Champlain (Vermont) is a scenic 12-mile (19,3km) trail that extends from downtown Burlington north through Colchester onto the Causeway. It's a multi-use trail so you will see walkers, runners, inline skaters and bikers.



It's wide enough and relatively flat so jogging strollers or burlees are do-able for the little ones. It is paved with the exception of 5 miles (8km) in Colchester.



The causeway connects the 7.5 mile (12km) bike path and intersects with Colchester Airport Park and unites with the Island Line in South Hero. This is a wonderful 14 mile (22,5km) trail that travels along Lake Champlain. The trail is unpaved and lined with large boulders on each side. The view from the causeway is unbelievable.



9. Julia Tuttle Causeway, USA


The Julia Tuttle Causeway carries Interstate 195 across Biscayne Bay. Interstate 195 (I-195) is a 4.424-mile-long (7.120 km) spur freeway connecting I-95 (its parent route) in the west with Miami Beach in the east.



Causeway is named after Miami founder Julia Tuttle. Construction of Interstate 195 (Florida) began in 1959, culminating with an opening on December 23, 1961. The Julia Tuttle Causeway was widened from 1988-1990 to improve the shoulders.



The Julia Tuttle Causeway is 4 kilometers (2.5mi) long and has a 6 lane of I-195. Traffic lanes are in the middle of the causeway, and between them and the water stretching lines of trees.



10. Gated Causeway, USA


A gated causeway (Caritas Island, Connecticut) leads to a four-acre island compound with a restored 14,000-square-foot (1.300 sqm) english manor, dock, lap pool, beach, koi pond, three-bedroom guest cottage and carriage house. Caritas Island is currently on the market for $12.8 million.



11. The Amador Causeway, Panama


The Amador Causeway Panama is a six kilometer (3.7mi) long causeway which is a must see for any visitor to Panama City. Any given day of the week the Amador Causeway is bustling with tourists taking in the spectacular views of Panama City. There are people watching as ships enter the passage to the Panama Canal, locals going to dinner, families taking a stroll along the sidewalk, athletes exercising, sailors coming in off the ships, travelers heading to the local islands off the coast and people taking advantage of the Duty Free store on the Flamenco Island.



The Amador Causeway is made up of four islands. The islands are Naos Island, Culebra Island, Perico Island and Flamenco Island at the end of the chain of islands. The causeway was originally constructed as a breakwater for the Panama Canal entrance. Over the last century the islands have transformed. During World War II the islands were utilized by the US military as a post to protect against an attack on the Panama Canal. Today we have a bustling tourist destination. The Amador Causeway was constructed using rocks excavated from Culebra Cut and Gaillard Cut during the excavation of the Panama Canal. Originally the breakwater only reached Naos Island. The fill used for the causeway was brought in by an ingenious rail system from the canal excavation sites.



12. Causeway Kunoy, Faroe Islands


The causeway between Borðoy island (right) and Kunoy island (left), Faroe Islands. On Kunoy the village of Haraldssund can be seen.



The reason for the unusual form of the causeway is unknown to us. In Haraldssund, the entrance to the 3km (1.9mi) one-lane tunnel to the 'bygd' of Kunoy is visible, as well as a quarry on Borðoy, and some aquaculture rings in the water.





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Wolfe Creek Crater in Australia

Wolfe Creek Crater is a well-preserved meteorite impact crater located in the flat plains of the northeastern edge of the Great Sandy Desert in Western Australia, some 150 km south of the town of Halls Creek. The crater is considered the second largest in the world from which meteorite fragments have been collected, after the famous Barringer Crater in Arizona. Because of its excellent preservation, the crater clearly shows the classic features that result from a large meteorite striking the Earth.

Wolfe Creek Crater measures roughly 880 meters in diameter, and the mostly flat crater floor sits some 55 meters below the crater rim and some 25 meters below the sand plain outside of the crater. At the crater’s center, the ground rises slightly. Here grows some surprisingly large trees that draw moisture from the crater’s water reserves that remain after summer rains.



The crater was formed 300,000 years ago when a meteorite weighing more than 50,000 metric tons struck the Earth at an estimated 15 kilometers per second. The impact punctured a hole on the surface and shattered rocks well below the ground surface, and the intense heat of the impact liquefied both the meteorite and the nearby terrestrial rocks. These rocks now take the form of rusted balls of iron-shale that occur in the vicinity. These balls can weigh as much as 250 kilograms apiece.

The Wolfe Creek Crater had been known for long by Australia’s Aboriginal people before it was identified by aerial survey in 1947. The locals refer to the crater as “Gandimalal” and it is prominent in art from the region. The European name for the crater comes from a nearby creek, which was in turn named after Robert Wolfe, a prospector and storekeeper during the gold rush that established the town of Halls Creek.





























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Pingualuit Impact Crater, Canada

In the far north of Quebec, a province in Canada, lies an exceptional natural wonder – a circular lake of blue waters confined within the walls of an ancient but well-preserved meteorite crater. Largely unknown to the outside world, the lake-filled crater had long been known to local Inuit who knew it as the "Crystal Eye of Nunavik" for its clear water. The lake was first observed by the crew of a United States Army Air Force plane in June 1943, who used the lake’s unusual shape and color for navigation, but pictures of it weren’t made public until 1950.

When Ontario diamond prospector Frederick W. Chubb saw the photographs, he became interested in it. He hoped that this might be an extinct volcano and there was a possibility to find diamonds nearby. Chubb sought the opinion of geologist V. Ben Meen of the Royal Ontario Museum, who immediately saw the possibility of an impact crater. Meen organized an expedition to this remote area together with Chubb. It was on this trip that Meen proposed the name "Chubb Crater". Meen organized two more expeditions to the crater, and from the data collected from the site, concluded that the structure was a meteorite crater produced from an impact roughly 1.4 million years ago.



The name of the lake was later changed to "New Quebec Crater" at the request of the Quebec Geographic Board. In 1999, the name was again changed, to "Pingualuit". The crater and the surrounding area are now part of Pingualuit National Park.

Pingualuit crater is 3.44 km in diameter. The crater rises 160 meters above the surrounding tundra and is 400 meters deep. A 267 meters deep body of water fills the depression, forming one of the deepest lakes in North America. The lake also holds some of the purest fresh water in the world, with a salinity level of less than 3 ppm. The lake has no inlets or apparent outlets, so the water accumulates solely from rain and snow and is only lost through evaporation. It is also one of most transparent lakes in the world with visibilities up to 35 meters.













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Kalavantin Durg (Prabalgad Fort), India

Prabalgad Fort, also known as Kalavantin Durg (Kalavantin’s Fort), is located between Matheran and Panvel in the Indian state of Maharashtra, at an elevation of 2,300 feet in the Western Ghats. It was built at the pinnacle of a rocky plateau very close to Matheran. Previously, the fort was known as Muranjan until it was taken over and renamed by the Maratha forces under Shivaji's rule.

The fort can be approached via a chillingly steep climb. The steps leading up to the fort were cut into the rock of the hill. There are no safety rails on the edge and no ropes on the wall to grab on to. The hardest part is the descent, especially if you have vertigo.



According to legend the fort was built for a queen named Kalavantin but that really seems to be all that anybody knows. Around 1458 Malik Ahmad, the prime minister of the kingdom of Ahmednagar, took over the fort during his conquest of Konkan. The Mughals took control of Prabalgad along with Kalyan, Mahuli, Karnala and a number of other forts after Sambhaji's death.

The fort was conquered by Shivaji from the Mughals in 1657, after he establishing himself in the Kalyan-Bhivandi area. At the time of the attack the fort was governed by Kesar Singh, a Mughal sardar, and was the only fort to put up a strong resistance. On seeing the signs of defeat the women in the fort performed Jauhar, a tradition of self immolation to ensure an honorable and respectful death. Singh died during the battle in October 1657, Shivaji in an act of kindness allowed Singh's mother and her grandchild a safe passage out.



















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