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What's important: you can compare and book not only Sylt hotels and resorts, but also villas and holiday cottages, inns and B&Bs (bed and breakfast), condo hotels and apartments, timeshare properties, guest houses and pensions, campsites (campgrounds), motels and hostels on Sylt. If you're going to Sylt save your money and time, don't pay for the services of the greedy travel agencies. Instead, book the best hotel on Sylt online, buy the cheapest airline tickets to Sylt, and rent a car on Sylt right now, paying the lowest price! Besides, here you can buy the Sylt related books, guidebooks, souvenirs and other goods.
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How to Book a Hotel on Sylt
In order to book an accommodation on Sylt enter the proper dates and do the hotel search. If needed, sort the found Sylt hotels by price, star rating, property type, guest rating, hotel features, hotel theme or hotel chain. Then take a look at the found hotels on Sylt map to estimate the distance from the main Sylt attractions and sights. You can also read the guest reviews of Sylt hotels and see their ratings.
When a hotel search on Sylt is done, please select the room type, the included meals and the suitable booking conditions (for example, "Deluxe double room, Breakfast included, Non-Refundable"). Press the "View Deal" ("Book Now") button. Make your booking on a hotel booking website and get the hotel reservation voucher by email. That's it, a perfect hotel on Sylt is waiting for you!
Hotels of Sylt
A hotel on Sylt is an establishment that provides lodging paid on a short-term basis. Facilities provided may range from a basic bed and storage for clothing, to luxury features like en-suite bathrooms. Larger on Sylt hotels may provide additional guest facilities such as a swimming pool, business centre, childcare, conference facilities and social function services. Hotel rooms on Sylt are usually numbered (or named in some smaller hotels and B&Bs) to allow guests to identify their room. Some Sylt hotels offer meals as part of a room and board arrangement. Hotel operations vary in size, function, and cost. Most Sylt hotels and major hospitality companies that operate hotels on Sylt have set widely accepted industry standards to classify hotel types. General categories include the following:
Upscale luxury hotels on Sylt
An upscale full service hotel facility on Sylt that offers luxury amenities, full service accommodations, on-site full service restaurant(s), and the highest level of personalized and professional service. Luxury Sylt hotels are normally classified with at least a Four Diamond or Five Diamond status or a Four or Five Star rating depending on classification standards.
Full service hotels on Sylt
Full service Sylt hotels often contain upscale full-service facilities with a large volume of full service accommodations, on-site full service restaurant(s), and a variety of on-site amenities such as swimming pools, a health club, children's activities, ballrooms, on-site conference facilities, etc.
Historic inns and boutique hotels on Sylt
Boutique hotels of Sylt are smaller independent non-branded hotels that often contain upscale facilities of varying size in unique or intimate settings with full service accommodations. Sylt boutique hotels are generally 100 rooms or less. Some historic inns and boutique hotels on Sylt may be classified as luxury hotels.
Focused or select service hotels on Sylt
Small to medium-sized hotel establishments that offer a limited amount of on-site amenities that only cater and market to a specific demographic of Sylt travelers, such as the single business traveler. Most Sylt focused or select service hotels may still offer full service accommodations but may lack leisure amenities such as an on-site restaurant or a swimming pool.
Economy and limited service hotels on Sylt
Small to medium-sized Sylt hotel establishments that offer a very limited amount of on-site amenities and often only offer basic accommodations with little to no services, these facilities normally only cater and market to a specific demographic of travelers, such as the budget-minded Sylt traveler seeking a "no frills" accommodation. Limited service Sylt hotels often lack an on-site restaurant but in return may offer a limited complimentary food and beverage amenity such as on-site continental breakfast service.
Guest houses and B&Bs on Sylt
A bed and breakfast on Sylt is a small lodging establishment that offers overnight accommodation and inclusive breakfast. Usually, Sylt bed and breakfasts are private homes or family homes offering accommodations. The typical Sylt B&B has between 4 and 11 rooms, with 6 being the average. Generally, guests are accommodated in private bedrooms with private bathrooms, or in a suite of rooms including an en suite bathroom. Some homes have private bedrooms with a bathroom which is shared with other guests. Breakfast is served in the bedroom, a dining room, or the host's kitchen. Often the owners of guest house themselves prepare the breakfast and clean the rooms.
Hostels on Sylt
Sylt hostels provide budget-oriented, sociable accommodation where guests can rent a bed, usually a bunk bed, in a dormitory and share a bathroom, lounge, and sometimes a kitchen. Rooms can be mixed or single-sex, although private rooms may also be available. Hostels are often cheaper for both the operator and occupants; many Sylt hostels have long-term residents whom they employ as desk agents or housekeeping staff in exchange for experience or discounted accommodation.
Apartment hotels, extended stay hotels on Sylt
Extended stay hotels are small to medium-sized Sylt hotels that offer longer term full service accommodations compared to a traditional hotel. Extended stay hotels may offer non-traditional pricing methods such as a weekly rate that cater towards travelers in need of short-term accommodations for an extended period of time. Similar to limited and select service hotels, on-site amenities are normally limited and most extended stay hotels on Sylt lack an on-site restaurant.
Timeshare and destination clubs on Sylt
Sylt timeshare and destination clubs are a form of property ownership also referred to as a vacation ownership involving the purchase and ownership of an individual unit of accommodation for seasonal usage during a specified period of time. Timeshare resorts on Sylt often offer amenities similar that of a Full service hotel with on-site restaurant(s), swimming pools, recreation grounds, and other leisure-oriented amenities. Destination clubs of Sylt on the other hand may offer more exclusive private accommodations such as private houses in a neighborhood-style setting.
Motels on Sylt
A Sylt motel is a small-sized low-rise lodging establishment similar to that of a limited service hotel, but with direct access to individual rooms from the car park. Common during the 1950s and 1960s, motels were often located adjacent to a major road, where they were built on inexpensive land at the edge of towns or along stretches of highways. They are still useful in less populated areas of Sylt for driving travelers, but the more populated an area becomes the more hotels fill the need. Many of Sylt motels which remain in operation have joined national franchise chains, rebranding themselves as hotels, inns or lodges.
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Sylt (German pronunciation:[ˈzʏlt]; Danish: Sild; Söl'ring North Frisian: Söl) is an island in northern Germany, part of Nordfriesland district, Schleswig-Holstein, and well known for the distinctive shape of its shoreline. It belongs to the North Frisian Islands and is the largest island in North Frisia. The northernmost island of Germany, it is known for its tourist resorts, notably Westerland, Kampen and Wenningstedt-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 the North Sea and its ongoing loss of land during storm tides. Since 1927, Sylt has been connected to the mainland by the Hindenburgdamm causeway. In latter years, it has been a resort for the German jet set and tourists in search of occasional celebrity sighting.
satellite image of Sylt
Map of Sylt (North Frisian, German and Danish place names)
With 99.14 square kilometres (38.28 square miles), Sylt is the fourth-largest German island and the largest German island in the North Sea. Sylt is located from 9 to 16 kilometres (6–10 miles) off the mainland, to which it is connected by the Hindenburgdamm. Southeast of Sylt are the islands of Föhr and Amrum, to the north lies the Danish island of Rømø. The island of Sylt extends for 38 kilometres (24 miles) in a north-south direction. At its northern point at Königshafen, it is only 320 metres (1,050 feet) wide. Its greatest width, from the town of Westerland in the west to the eastern Nössespitze near Morsum, 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 the Wadden Sea, which belongs to the Schleswig-Holstein Wadden Sea National Park and mostly falls dry during low tide.
The island's shape has constantly shifted over time, a process which is still ongoing today. The northern and southern spits of Sylt are exclusively made up of infertile sand deposits, while the central part with the municipalities of Westerland, Wenningstedt-Braderup and Sylt-Ost consists of a geestland core, which becomes apparent in the form of the Red Cliff of Wenningstedt. The geestland facing the Wadden Sea gradually turns into fertile marshland around Sylt-Ost. Today sources show that Sylt has only been an island since the Grote Mandrenke flood of 1362. The so-called Uwe-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 mainland geestland, it was formed of moraines from the older ice ages, thus being made up of a till core, which is now apparent in the island's west and centre by the cliff, dunes and beach. This sandy core began to erode 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 the Grote Mandrenke flood it belonged to a landscape cut by tidal creeks and, at least during low tide, it could be reached on foot. It is only since this flood that the creation of a spit 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 the Königshafen (King's Harbour) began to silt up as the "elbow" spit began to form.
In addition to the constant loss of land, the inhabitants during the Little 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 of marram 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 annual land 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.
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 500m wide is especially threatened.
An armoured concrete groyne at Westerland
Concrete tetrapods in Westerland
Geotextile 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).
Measures of protection against the continuous erosion date back to the early 19th century when groynes 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 installing tetrapods 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.
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. 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 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. In the 1995 study Klimafolgen 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).
The enforcement of a natural reef off Sylt is being discussed as an alternative solution. A first experiment was conducted from 1996 to 2003. A sand drainage as being successfully used on Danish islands is not likely to work on Sylt owing to the underwater slope here.
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 continuous global 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. The dunes of the island constitute nature 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.
The Wadden Sea on the east side between Sylt and the mainland has been a nature reserve and bird 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 for land 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.
Sylt: Flora and fauna
Rosa rugosa, known as "Sylt rose" on the island
The flora of Sylt is shaped by the island's original sparseness. Until the mid 19th century Sylt was an island almost completely devoid of trees, only artificial plantations created small areas of forest and bush. Still today one can recognize the man-made structure of the Friedrichshain and Südwäldchen forests in Westerland, the trees mostly standing in rank and file. Also the now widespread rose Rosa rugosa, known as the "Sylt rose" on the island was only imported to Sylt. It originates from the Kamchatka peninsula in Siberia. 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.
The ample heaths 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 the IUCN Red List. Especially notable are the 600 species of butterflies that live in the heaths, small tortoiseshell, brimstone, painted lady and peacock butterfly among them.
With several thousand individuals in the dune belt of Sylt, the natterjack 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. The main threat for this species on Sylt is road traffic.
The many water birds and other coastal avians, that have their hatching grounds on Sylt or use the island for resting on their migrations constitute an ornithological feature. There are two notable hatching areas on Sylt, the Königshafen bay with the small island Uthörn in the north and the Rantum basin in the southeast. Birds that hatch on Sylt include black-headed gull, Arctic tern, pied avocet, common redshank, common gull, oystercatcher, northern lapwing, common shelduck and tufted duck. During the migration, Sylt is a resting spot for thousands of brent geese and shelducks, Eurasian wigeons and common eiders, as well as bar-tailed godwits, red knots, dunlins and Eurasian golden plovers. Ringed plover, common snipe, ruff and other species are less common visitors to the island.
Regarding land mammals, there is no significant difference from the neighbouring areas of mainland Nordfriesland. Primarily European hare, rabbit and roe deer can be found and are also hunted as game on the island. When the island was connected to the mainland by the causeway fox and badger also became common.
West of Sylt a breeding area of harbour porpoises is located. In addition, great numbers of harbour seals and grey 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 their branches on Sylt. Among them are the Alfred-Wegener-Institute for Polar and Marine Research, Verein Jordsand and Wadden Sea Conservation Station. Also the Federal Office for the Environment operates a research station in the dunes at Westerland.
On Sylt, a marine climate influenced by the Gulf stream is predominant. With an average of 2 °C, winter months are slightly milder than on the mainland, summer months though, with a median of 17 °C, 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. Clouds cannot accumulate as quickly and are generally scattered by the constant westerly or northwesterly winds.
The annual mean temperature is 8.5 °C. The annually averaged wind speed measures 6.7 m/s, predominantly from western directions. The annual rainfall amounts to about 650 millimetres. Since 1937 weather data are collected at Deutscher Wetterdienst's northernmost station on a dune near List, which has meanwhile become automated. A number of commercial meteorological services like Meteomedia AG operate stations in List too.
Sylt features an oceanic climate that is influenced by the Gulf Stream. On average, the winter season is slightly warmer than in mainland Nordfriesland. The summer season, however, is cooler despite of 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.
Climate data for List (1961–1990 averages)
Daily mean °C (°F)
Average precipitation mm (inches)
Mean monthly sunshine hours
Source: German Meteorological Service
Climate data for List, (1990–2014 averages)
Daily mean °C (°F)
Average precipitation mm (inches)
Mean monthly sunshine hours
view from a hotel room in Westerland
A beach in Kampen (Sylt)
Sylt is divided into two administrative bodies: the Amt Landschaft Sylt with its seat in Keitum administrates all municipalities on the island, save for the independent town of Westerland. As of December 2007, Sylt had 21,190 inhabitants, 9,072 of whom living in Westerland. These numbers do not include owners of summer residences.
A referendum held in May 2008 resulted in a merger of the Sylt-Ost municipality with the town of Westerland due 1 January 2009. Various interest groups hope to merge every island municipality into one governing body.
Sylt: Settlements along the west coast
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 of Denmark. On its eastern shore, a harbour is located where, in addition to tourist ships, the "Sylt-Express" ferry-boat sails to Havneby on the Danish island Rømø. Wenningstedt together with Braderup and Kampen used to form the Norddörfer (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 white Kampen lighthouse is located between Kampen and Wenningstedt, it is the oldest one on the island. East of there, the Braderuper 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, 50 years later Westerland was granted town privileges. In 1949 it was officially recognised as a health resort. In 2007, the town counted 9,072 citizens.
South of Westerland, the island extends for about 15 km in the form of a spit, until it is cut by the Hörnumtief tidal creek, that runs through the Wadden Sea mudflats east of Sylt. Here is the location of Rantum. 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 of marram grass stopped the dunes and put an end to this threat. To the east there are a few scattered spots of marshland, while the area is mostly dominated by dunes.
Hörnum on the island's southern headland is the youngest village, having been founded shortly after 1900. But already in former times the uninhabited southern tip of Sylt was said to serve as refuge for pirates and fishermen. The name Budersand in the area emanates from that custom, marking a great dune where booths (German: Buden) stood in former times to serve as shelters. This southern headland, called Odde, 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.
Main article: Sylt-Ost
Sylt-Ost (East Sylt) is a former municipality which was formed in 1970 out of several small villages on the Nössehalbinsel of Sylt. The population (as of 2000) was 5,500. The villages included Tinnum, Munkmarsch, Archsum, Morsum and Keitum. In 2009, Sylt-Ost merged with Westerland and Rantum to form Gemeinde Sylt.
Geographically, Sylt was originally part of Jutland (today Schleswig-Holstein and mainland Denmark), with evidence of human habitation going back to 3000 BC at Denghoog. 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 and oyster 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. During World War I, Sylt became a military outpost. On 25 March 1916 British seaplanes bombed the German airship sheds on Sylt. The main connection for tourists was boats from Højer. Since Højer was ceded to Denmark in 1920, a rail causeway to the mainland was built in 1927, the Hindenburgdamm, named after Paul von Hindenburg. During World War II, Sylt became a fortress, with concrete bunkers built below the dunes at the shore, some of which are still visible today. Lager Sylt, the concentration camp on Alderney was named after the island. Rudolf Höss hid on the island after Nazi Germany's defeat, but he was later captured and brought to trial in Poland.
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. The Windsurf World Cup Sylt, established in 1984, is annually held at Westerland's beach front. Sylt is also popular for second home owners, and many German celebrities who own vacation homes on "the island".
Sylt is a part of the Frisian Islands. It has its own local dialect, Söl'ring, which is the indigenous speech of Sylt. Söl'ring is a dialect of insular North Frisian, with elements of Danish, Dutch and English. 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 in Schleswig-Holstein on New 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 and/or money.
Sylt also features many Frisian-style houses with thatched roofs.
The vowel sound in the name of the island is represented in standard written German as "y" for unknown reasons, whereas the expected spelling of the name would be "Sült".
Sylt is connected to the German mainland by the Hindenburgdamm, a causeway with a railway line on top. The passenger trains connect Westerland (Sylt) to Niebüll or Klanxbüll, and the Deutsche Bahn's "Syltshuttle" allows the transfer of cars and trucks between Westerland and Niebüll. There are also ferry services to the nearby Danish island of Rømø. Sylt Airport at Westerland serves the region.
Sylt: In other media
The island was used during the filming of The Ghost Writer, as an alternate location for Martha'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.
Sylt: See also
Üüs Söl’ring Lön’, insular anthem
Heinz Reinefarth a Nazi-German military officer The butcher of Warsaw became mayor of Sylt after World War II.
Kehl, H. "Entstehung der Insel Sylt im Laufe von 700 Jahren" (in German). Institute of Ecology, Technical University Berlin.
Thiede, J; K. Ahrendt (2000). "Klimaänderung und Küste – Fallstudie Sylt" (PDF) (in German). GEOMAR, University of Kiel.
Landesamt für den Nationalpark Schleswig-Holsteinisches Wattenmeer, Umweltbundesamt, ed. (1998). Umweltatlas Wattenmeer (Wadden Sea environmental Atlas) (in German). I – Nordfriesisches und Dithmarscher Wattenmeer. Stuttgart. p. 38.
Müller, W. W.; Saathoff, F. (2015). "Geosynthetics in geoenvironmental engineering". Science and Technology of Advanced Materials. 16 (3): 034605. doi:10.1088/1468-6996/16/3/034605.
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.CS1 maint: Multiple names: authors list (link) CS1 maint: Unfit url (link)
Von Liebermann, Nicole. "Küstenschutz: Bisherige und zukünftige Maßnahmen" (PDF) (in German). Technical University of Harburg. Archived from the original on 11 June 2007.CS1 maint: Unfit url (link)
Daschkeit, Achim; Horst Sterr. "Küste, Ökologie und Mensch, Integriertes Küstenmanagement als Instrument nachhaltiger Entwicklung". In Bernhard Glaeser. Edition Humanökologie (PDF). 2. Deutsche Gesellschaft für Humanökologie.
Daschkeit, Achim; Peter Schottes (2002). Klimafolgen für Mensch und Küste am Beispiel der Nordseeinsel Sylt (in German). ISBN 978-3-540-42569-4.
Bleck, Matthias. "Funktionale Bemessung künstlicher Riffe für aktiven und sanften Küstenschutz" (PDF). Stiftung deutscher Küstenschutz.
Newig, J. "Sand auf Sylt" (PDF). University of Kiel.
"Interessantes über die Braderuper Heide" (in German). Naturschutzgemeinschaft Sylt. Archived from the original on 17 February 2012.CS1 maint: Unfit url (link)
"Morsum-Kliff" (in German). Naturschutzgemeinschaft Sylt. Archived from the original on 17 February 2012.CS1 maint: Unfit url (link)
Klinge, Andreas (2003). "Die Amphibien und Reptilien Schleswig-Holsteins, Rote Liste" (PDF). 3rd version (in German). Schleswig-Holstein State Office for Nature and Environment.
Lohmann, M.; K. Haarmann. Vogelparadiese (in German). 1 – Norddeutschland. Paul Parey. ISBN 3-490-16418-0.
"Tourimusstatistik 2005" (PDF) (in German). Town of Westerland.
"List auf Sylt (climate chart)". Bernhard Mühr. 1 June 2007.
"Das Wetter auf Sylt: viel Sonne und eine frische Brise" [The Weather on Sylt: A lot of Sunshine and a fresh Breeze]. Zeit Reisen (in German). Retrieved 23 October 2012.
"Frei zugängliche Klimadaten" (in German). German Meteorological Service.
"CLimate Robot List/Sylt". WeatherOnline.co.uk.
"Orte, Städte, Gemeinden im Landkreis Nordfriesland" (in German). Deutschland auf einen Blick.
"Westerland und Sylt-Ost fusionieren". Sylter Rundschau (in German). Schleswig-Holsteinischer Zeitungsverlag. 26 May 2008. Archived from the original on 16 February 2012.CS1 maint: Unfit url (link)
"Der Fahrplan zur Teilfusion: So geht es jetzt weiter". Sylter Rundschau (in German). Schleswig-Holsteinischer Zeitungsverlag. 27 May 2008. Archived from the original on 16 February 2012.CS1 maint: Unfit url (link)
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.
"First World War.com Day by day". First World War.com. Retrieved 27 March 2016.
"Auschwitz: Inside the Nazi State. Auschwitz 1940–1945. Liberation & Revenge". PBS.
Sylt: External links
Wikimedia Commons has media related to Sylt.
Sylt travel guide from Wikivoyage
West Frisian Islands
East Frisian Islands
Langlütjen I & II
North Frisian Islands
Danish Wadden Sea Islands
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