Sylt (German pronunciation:[ˈzʏlt]ⓘ;Danish:Sild;Söl'ring North Frisian:Söl) is an island in northernGermany, part ofNordfriesland district,Schleswig-Holstein, with a distinctively shaped shoreline. It belongs to theNorth Frisian Islands and is the largest island inNorth Frisia.The northernmost island of Germany, it is known for its tourist resorts, notablyWesterland,Kampen andWenningstedt-Braderup, as well as for its 40-kilometre-long (25-mile) sandy beach. It is frequently covered by the media in connection with its exposed situation in theNorth Sea and its ongoing loss of land duringstorm tides. Since 1927, Sylt has been connected to the mainland by theHindenburgdamm causeway. In later years, it has been a resort for the German jet set and tourists in search of occasional celebrity sightings.[citation needed]
Satellite image of SyltMap of Sylt (North Frisian, German and Danish place names)
With 99.14 square kilometres (38.28 square miles), Sylt is the fourth-largestGerman island and the largest German island in theNorth Sea. Sylt is located from 9 to 16 kilometres (6–10 miles) off the mainland, to which it is connected by theHindenburgdamm. Southeast of Sylt are the islands ofFöhr andAmrum, to the north lies theDanish island ofRømø. The island of Sylt extends for 38 kilometres (24 miles) in a north-south direction. At its northern point atKönigshafen, it is only 320 metres (1,050 feet) wide. Its greatest width, from the town of Westerland in the west to the easternNössespitze nearMorsum, measures 12.6 kilometres (7.8 miles). On the western and northwestern shore, there is a 40-kilometre-long (25-mile) sandy beach. To the east of Sylt, is theWadden Sea, which belongs to theSchleswig-Holstein Wadden Sea National Park and mostly falls dry during lowtide.
The island's shape has constantly shifted over time, a process which is still ongoing today. The northern and southernspits of Sylt are exclusively made up of infertile sand deposits, while the central part with the municipalities ofWesterland,Wenningstedt-Braderup andSylt-Ost consists of ageestland core, which becomes apparent in the form of the Red Cliff of Wenningstedt. The geestland facing the Wadden Sea gradually turns into fertilemarshland around Sylt-Ost. Sylt has only been an island since theGrote Mandrenke flood of 1362.[1] The so-calledUwe-Düne (Uwe Dune) is the island's highest elevation with 52.5 metres (172.2 feet)above sea level.
The island in its current form has only existed for about 400 years. Like the mainlandgeestland, it was formed ofmoraines from the olderice ages, thus being made up of atill core, which is now apparent in the island's west and centre by the cliff, dunes and beach. This sandy core began toerode as it was exposed to a strong current along the island's steep basement when the sea level rose 8000 years ago. During the process,sediments were accumulated north and south of the island. The west coast, which was originally situated 10 kilometres (6 miles) off today's shore, was thus gradually moved eastward, while at the same time the island began to extend to the north and south. After the ice ages, marshland began to form around this geestland core.
In 1141, Sylt is recorded as an island, yet before theGrote Mandrenke flood it belonged to a landscape cut bytidal creeks and, at least during low tide, it could be reached on foot.[1] It is only since this flood that the creation of aspit from sediments began to form the current characteristic shape of Sylt. It is the northern and southern edges of Sylt which were, and still are, the subject of greatest change. For example, Listland was separated from the rest of the island in the 14th century and from the later 17th century onwards theKönigshafen (King's Harbour) began to silt up as the "elbow" spit began to form.[2]
In addition to the constant loss of land, the inhabitants during theLittle Ice Age were constrained by sand drift. Dunes shifting to the east threatened settlements and arable land and had to be stopped by the planting ofmarram grass in the 18th century. Consequently, though, material breaking off the island was increasingly washed away and the island's extent continued to decrease.
Records of the annualland loss exist since 1870. According to them, Sylt lost an annual 0.4 metres (16 inches) of land in the north and 0.7 metres (28 inches) in the south from 1870 to 1951. From 1951 to 1984, the rate increased to 0.9 metres (35 inches) and 1.4 metres (55 inches) respectively, while shorelines at the island's very edges at Hörnum and List are even more affected.[3]
Severe storm surges of the last decades have repeatedly endangered Sylt to the point of breaking in two, e.g. Hörnum was temporarily cut off from the island in 1962. Part of the island near Rantum which is only 500 metres (yards) wide is especially threatened.
An armoured concrete groyne at WesterlandConcrete tetrapods in WesterlandGeotextile sand cushions successfully protected the historic house Kliffende on Sylt against storms, which strongly eroded the cliffs on the north and south sides of the sand cushion barrier (1999).[4]
Measures of protection against the continuous erosion date back to the early 19th century whengroynes of wooden poles were constructed. Those were built at right angles into the sea from the coast line. Later they were replaced by metal and eventually by armoured concrete groynes. The constructions did not have the desired effect of stopping the erosion caused by crossways currents. "Leeward erosion", i.e. erosion on the downwind side of the groynes prevented sustainable accumulation of sand.
In the 1960s, breaking the power of the sea was attempted by installingtetrapods along the groyne bases or by putting them into the sea like groynes. The four-armed structures, built in France and many tons in weight, were too heavy for Sylt's beaches and were equally unable to prevent erosion. Therefore, they were removed from the Hörnum west beach in 2005.[5]
Since the early 1970s, the only effective means so far has been flushing sand onto the shore.Dredging vessels are used to pump a mixture of sand and water to a beach where it is spread by bulldozers. Thus storm floods would only erase the artificial accumulation of sand, while the shoreline proper remains intact and erosion is slowed down.[6] This procedure incurs considerable costs. The required budget of an annual€10 million is currently provided by federal German, Schleswig-Holstein state and EU funds. Since 1972, an estimated 35.5 million cubic metres (46.4 million cu. yd.) of sand have been flushed ashore and dumped on Sylt. The measures have so far cost more than €134 million in total, but according to scientific calculations they are sufficient to prevent further loss of land for at least three decades, so the benefits for the island's economic power and for the economically underdeveloped region in general would outweigh the costs.[7] In the 1995 studyKlimafolgen für Mensch und Küste am Beispiel der Nordseeinsel Sylt (Climate impact for Man and Shores as seen on the North Sea island Sylt), it reads:"Hätte Sylt nicht das Image einer attraktiven Ferieninsel, gäbe es den Küstenschutz in der bestehenden Form gewiss nicht" (If Sylt did not have the image of an attractive holiday island, coastal management in its current form would certainly not exist).[8]
The enforcement of a naturalreef off Sylt is being discussed as an alternative solution. A first experiment was conducted from 1996 to 2003.[9] A sand drainage as being successfully used on Danish islands is not likely to work on Sylt owing to the underwater slope here.[10]
In parallel to the ongoing sand flushing, the deliberate demolition of groynes has begun amid great effort at certain beach sections where they were proven largely ineffective. This measure also terminated the presumably most famous groyne of Sylt,Buhne 16 – the namesake of the local naturist beach.
A number of experts, however, fears that Sylt will still have to face considerable losses of land until the mid 21st century. The continuousglobal warming is thought to result in increasing storm activity, which would result in increased land loss and, as a first impact, might mean the end of property insurance. Measurements showed that, unlike in former times, the wave energy of the sea is no longer lost offshore, today it carries its destructive effects on to the beaches proper. This will result in an annual loss of sand of 1.1 million m³ (1.4 million cu. yd.).[2]The dunes of the island constitutenature reserves and may only be traversed on marked tracks. So called "wild paths" promote erosion and are not to be followed. Where vegetation is tread upon, no roots are left to hold the sand and it will be removed by wind and water.
TheWadden Sea on the east side between Sylt and the mainland has been a nature reserve andbird sanctuary since 1935 and is part of the Schleswig-Holstein Wadden Sea National Park. The construction of breakwaters in this area will abate sedimentation and is used forland reclamation.
Also the grazing of sheep on the sea dikes and heaths of Sylt eventually serves coastal management, since the animals keep the vegetation short and compress the soil with their hooves. Thus they help create a denser dike surface, which in case of storm surges provides less area for the waves to impact.
Theflora of Sylt is shaped by the island's original sparseness. Until the mid 19th century, Sylt was an island almost completely devoid of trees except for small areas of forest and bush created by plantations. Today, one can still recognize the man-made origin of theFriedrichshain andSüdwäldchen forests in Westerland where many of the trees stand in rank and file. Also, the now widespread roseRosa rugosa, known as the "Sylt rose" on the island was imported to Sylt. It originates from theKamchatka peninsula inSiberia. The undemanding rose met ideal conditions on Sylt and spread so quickly that it is now a common sight on the island. Its proliferation is viewed critically from a biological point of view, since it threatens to displace endangered local species, especially on the heaths.[11]
The ampleheaths on the eastern side of the island provide habitats for many rare species of plants and animals which are adapted to the extreme conditions such as drought, warmth, wind. About 2,500 animal species and 150 species of plants have so far been recorded. 45% of those plants are on theIUCN Red List.[11] Especially notable are the 600 species ofbutterflies that live in the heaths,small tortoiseshell,brimstone,painted lady andpeacock butterfly among them.[12]
With several thousand individuals in the dune belt of Sylt, thenatterjack toad, endangered in Germany, has one of Germany's largest populations here. Their spawning places are wet dune slacks and shallow, short-lived pools. For a habitat they prefer sandy areas with vegetation, but the species has also been observed on the top of the Uwe Dune. The main threat for this species on Sylt is road traffic.[13]
Regarding landmammals, there is no significant difference from the neighbouring areas of mainland Nordfriesland. PrimarilyEuropean hare,rabbit androe deer can be found and are also hunted as game on the island. When the island was connected to the mainland by the causeway,red fox andEuropean badger also became common.
West of Sylt a breeding area ofharbour porpoises is located. In addition, great numbers ofharbour seals andgrey seals, the latter being rather uncommon in German seas, can be found on sand banks off Sylt.
Numerous associations and societies that care for the exploration and the protection of endangered animals and plants have branches on Sylt. Among them are theAlfred-Wegener-Institute for Polar and Marine Research, Verein Jordsand andWadden Sea Conservation Station. Also the Federal Office for the Environment operates a research station in the dunes at Westerland.
On Sylt, amarine climate influenced by theGulf Stream is predominant. With an average of 2 °C (36°F), winter months are slightly milder than on the mainland, summer months though, with a median of 17 °C (62°F), are somewhat cooler, despite a longer sunshine period. The annual average sunshine period on Sylt is 4.4 hours per day. It is due to the low relief of the shoreline that Sylt had a total of 1,899 hours of sunshine in 2005, 180 hours above the German average.[15] Clouds cannot accumulate as quickly and are generally scattered by the constant westerly or northwesterly winds.
The annual mean temperature is 8.5 °C (47°F). The annually averaged wind speed measures 6.7 m/s (15 mph), predominantly from western directions. The annual rainfall amounts to about 650 millimetres (25½").[16] Since 1937 weather data are collected atDeutscher Wetterdienst's northernmost station on a dune nearList, which has meanwhile become automated. A number of commercial meteorological services likeMeteomedia AG operate stations in List too.
Sylt features anoceanic climate that is influenced by theGulf Stream. On average, the winter season is slightly warmer than in mainland Nordfriesland. The summer season, however, is cooler despite longer sunshine periods. The yearly average sunshine period is greater than 4.4 hours per day with some years exceeding the average sunshine for all of Germany. Also precipitation is lower than on the mainland. This is due to the low relief of Sylt's shoreline where clouds are not able to accumulate and rain off.[17]
view from a hotel room inWesterlandThe red cliff next toKampen, Sylt
Sylt is divided into two administrative bodies: theAmtLandschaft Sylt administers all municipalities on the island, save for theGemeinde Sylt, which was established in 2009 from the formerly independent municipalities ofWesterland,Rantum andSylt-Ost. As of December 2007, Sylt had 21,190 inhabitants, 9,072 of whom living in Westerland.[22] These numbers do not include owners of summer residences.
A referendum held in May 2008 resulted in a merger of theSylt-Ost municipality with the town of Westerland on 1 January 2009.[23] Various interest groups hope to merge every island municipality into one governing body.[24]
Six municipalities are situated along the west coast of Sylt.List in the very north of the island constitutes Germany's northernmost municipality; it retained a certain independence due to its remote location and its long-time adherence to the kingdom ofDenmark. On its eastern shore, a harbour is located where, in addition to tourist ships, the "Sylt-Express" ferry-boat sails toHavneby on the Danish island ofRømø.Wenningstedt together withBraderup andKampen used to form theNorddörfer (Northern Villages) municipality, an early intercommunal association, which partly remains today in form of a school union. While Kampen, mainly in the 1950s and 1960s, was famous in Germany for attracting celebrities, Wenningstedt has been known as a "family resort" for more than 100 years. Since 1855, the prominent black and whiteKampen Lighthouse has been located between Kampen and Wenningstedt; it is the oldest one on the island. East of there, theBraderuper Heide nature reserve is situated. Right south of Wenningstedt are the town limits of the island's largest town, Westerland.
After the complete destruction of the village Eidum by a storm surge on 1 November 1436, the survivors founded a new village northeast of their old home: Westerland. The name was first recorded in 1462. In 1865, a seaside spa was founded and, 50 years later, Westerland was grantedtown privileges. In 1949, it was officially recognised as a health resort. In 2007, the town numbered 9,072 citizens.
South of Westerland, the island extends for about 15 km (10 miles) in the form of a spit, until it is cut by theHörnumtief tidal creek that runs through the Wadden Sea mudflats east of Sylt. Here is the location ofRantum. This village, like no other on Sylt, had to fight sand drift during the past centuries. Many farmsteads and a church had to be abandoned because of shifting dunes moving eastward. Only the planting ofmarram grass stopped the dunes and put an end to this threat. To the east, there are a few scattered spots of marshland, but the area is mostly dominated by dunes.
Hörnum on the island's southern headland is the youngest village. It was founded shortly after 1900, although the uninhabited southern tip of Sylt was said to serve as refuge for pirates and fishermen. The nameBudersand in the area emanates from that custom, marking a great dune where booths (German:Buden) stood in former times to serve as shelters.[25] This southern headland, calledOdde, is marked by continuous loss of land. Each year great amounts of sand are washed away by storm floods and coastal management has not yet seen sustainable effects in the area, so that further losses have to be expected.
Sylt-Ost (East Sylt) is a former municipality which was formed in 1970 out of several small villages on theNössehalbinsel of Sylt. The population (as of 2000) was 5,500. The villages includedTinnum,Munkmarsch,Archsum,Morsum andKeitum. In 2009, Sylt-Ost merged with Westerland and Rantum to formGemeinde Sylt.
Geographically, Sylt was originally part ofJutland (today Schleswig-Holstein and mainlandDenmark), with evidence of human habitation going back to 3000 BC atDenghoog. The first settlements of Frisians appeared during the 8th century and 9th century. In 1386, Sylt was divided between the Duke of Schleswig and the King of Denmark; except for the village of List, Sylt became part of the Duchy of Schleswig in 1435.
During the 17th and 18th century,whaling, fishing andoyster breeding increased the wealth of the population. At this time, Keitum became the capital of the island, and a place for rich captains to settle down. In the 19th century, tourism began. Westerland replaced Keitum as the capital. DuringWorld War I, Sylt became a military outpost. On 25 March 1916, British seaplanes bombed the German[26][better source needed] airship sheds on Sylt. The main connection for tourists was boats fromHøjer. Since Højer was ceded to Denmark in 1920, a rail causeway to the mainland was built in 1927, theHindenburgdamm, named afterPaul von Hindenburg. DuringWorld War II, Sylt became a fortress, with concrete bunkers built below thedunes at the shore, some of which are still visible today.Lager Sylt, theconcentration camp onAlderney was named after the island.Rudolf Höss hid on the island afterNazi Germany's defeat, but he was later captured and brought to trial in Poland.[27]
Windsurf World Cup Sylt in 2006
Today, Sylt is mainly a tourist destination, famous for its sandy beaches and healthy climate. The 40 km-long (25 mi) west beach has a number of surf schools and also a nude section. ThePWA World Tour Windsurf World Cup Sylt, established in 1984, is annually held at Westerland's beach front.[28] Sylt is also popular for second home owners, and many German celebrities who ownvacation homes on "the island".
At the beginning of the 20th century, the bathing beaches on Sylt weresegregated by sex into "ladies' bath" (Damenbad) and "men's bath" (Herrenbad); one bathed in long bathing dresses of that time period. From the beginning of the 20th century - starting from the Free German Youth camp Klappholttal and the intellectuals and artists in the village ofKampen - a social movement developed that lived a beach life without clothing (part of the GermanFreikörperkultur - FKK andLebensreform movement). The first official nude bathing beach in Germany was opened on Sylt in 1920.[29] Nude bathing and sunbathing (also erroneously referred to as "nudist" or "nudism") spread over the entire island. "Sylt" was associated with nude bathing and the ideal environment for supporters of theFreikörperkultur (FKK). Since the 1960s, there have been designatednudist beaches (markedFKK-Strand) with names such as "Abyssinia", "Samoa" or "Zanzibar" on the entire west beach. The most famous nudist beach on Sylt became the "Groyne 16" (Buhne 16) in Kampen through regular reports in the tabloid media. Today the boundaries between nude and textile beaches are becoming more and more blurred. While nude beaches have lost some of their popularity, it is no longer unusual or sensational to bathe or sunbathe on "normal" beaches with no clothes on.
Sylt is a part of theFrisian Islands. It has its own local dialect,Söl'ring, which is the indigenous speech of Sylt. Söl'ring is a dialect of insularNorth Frisian, with elements ofDanish,Dutch andEnglish. The island has a museum calledAltfriesisches Haus (Sölring Museen, Altfriesisches Haus in Keitum).
Today, only a small fraction of the population still speak Söl'ring. A law to promote the language (Friesisch-Gesetz) was passed in 2004. The northernmost part of the island,Listland, was traditionally Danish-speaking.
As in many areas inSchleswig-Holstein onNew Year's Eve, groups of children go masked from house to house, reciting poems. This is known as "Rummelpottlaufen", and as a reward, children receive sweets or money.
Sylt also features many Frisian-style houses withthatched roofs.
Since the mid-18th century, the vowel in the name of the island has been represented as "y" for unknown reasons, while older spellings areSildt andSilt, allegedly derived from Danishsild "herring",[30] or maybe related to Englishsilt.
Sylt is mentioned in apangram, a sentence that uses every letter in the German alphabet, including every umlaut (ä, ö, ü) plus the ß:Victor jagt zwölf Boxkämpfer quer über den großen Sylter Deich ("Victor chases twelve boxers across the Great Levee of Sylt").
Among the first painters who discovered Sylt as atheme wereEugen Dücker andEugen Bracht.Franz Korwan followed them.The painter Andreas Dirks was born inTinnum on Sylt in 1865. He studied at the Düsseldorf Art Academy and in Weimar, lived in Düsseldorf since 1895, accepted a professorship there in 1916 and at the same time maintained a studio in Westerland.Ulrich Schulte-Wülwer described him as "... the strongest artistic talent that the island has produced".Carl Arp came to Sylt in 1903.Painters likeEmil Nolde,Erich Heckel,Anita Rée andAlbert Aereboe moved to Sylt. Contemporary artists include the painters and sculptorsRainer Fetting andIngo Kühl, who live in Berlin and on Sylt.
Dirk Meinerts Hahn (born 1804 in Westerland, Sylt – 1860) best known as the captain of the shipZebra that he captained to South Australia
Cornelius Jensen (1814 in Sylt – 1886) a Danish sea captain for 20 years; arriving in San Francisco in 1848, he became a rancher, a vintner and served as a California politician.
Sylt is connected to the German mainland by theHindenburgdamm, acauseway with a railway line on top. The passenger trains connectWesterland (Sylt) toNiebüll orKlanxbüll, and the Deutsche Bahn's "Syltshuttle" as well as RDC's "Autozug Sylt", allow the transfer of cars and trucks between Westerland and Niebüll. There are alsocar ferry services to the nearbyDanish island ofRømø, which offers a road connection to the mainland.Sylt Airport at Westerland serves the region.
The island was used during the filming ofThe Ghost Writer, as an alternate location forMartha's Vineyard, due to the film's director,Roman Polanski being unable to travel to the United States, due to an outstanding arrest warrant for rape. The ferry between the islands of Sylt and Rømø features prominently in the film.
^Witte, J.-O.; Kohlhase, Sören, J. Radomski, P. Fröhle."Fallstudie Sylt"(PDF) (in German).University of Rostock. Archived from the original on 10 August 2007.{{cite web}}: CS1 maint: multiple names: authors list (link)
^Daschkeit, Achim; Horst Sterr. "Küste, Ökologie und Mensch, Integriertes Küstenmanagement als Instrument nachhaltiger Entwicklung". In Bernhard Glaeser (ed.).Edition Humanökologie(PDF). Vol. 2. Deutsche Gesellschaft für Humanökologie. Archived fromthe original(PDF) on 27 November 2009. Retrieved28 September 2008.
^Daschkeit, Achim; Peter Schottes (2002).Klimafolgen für Mensch und Küste am Beispiel der Nordseeinsel Sylt (in German).Springer.ISBN978-3-540-42569-4.
^Pahl, Max (1983).Hörnum. Heimat am Horn – Querschnitt und Streifzüge durch Geschichte, Leben und Landschaft des Nordseebades Hörnum auf Sylt (in German). Lunden: Verlagsdruckerei Schallhorn.
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