冬季南岸三日游｜杰古沙龙冰河湖＋蓝冰洞＋北极光＋冰川徒步＋黄金圈＋维克

• 运营日期 11月. - 3月.
• 长度 3 天
• 项目 冰川徒步, 观光, 寻猎极光, 冰洞探险
• 难度 容易
• 最低年龄 8 岁
• 解说语言 English
• 亮点

  The Golden Circle is a 300 km route to the 3 most popular natural attractions in Iceland. The Golden Circle consists of Geysir, Gullfoss and Thingvellir.

  See this for Golden circle tours.

  Geysir area

  Geysir is a geyser that gives its name to hot springs all over the world. But although Geysir itself is not active anymore the area features spectacular hot springs such as the powerful Strokkur (spouting a vast amount of water every 10 minutes, regularly about 15-20 meters into the air), Smidur and Litli-Strokkur. 

  Gullfoss waterfall

  The 'Golden Waterfall', is the second part of the Golden Circle, and one of the most beautiful and powerful waterfalls in Iceland, plummeting 32 meters into the river gorge of the popular rafting river Hvita. It is Iocated about 10 km from Geysir. 

  Thingvellir national park

  The largest attraction of the Golden Circle is Thingvellir National Park. The Icelandic parliament was founded there in 930 and remained until the year 1798.

  Today it is a UNESCO World Heritage Site and one of the most important places to visit in Iceland, not just for its historical and cultural values, but for also its magnificent landscape.

  Thingvellir is surrounded by a beautiful mountain and volcano range and is the site of a rift valley, where the tectonic plates meet, marking the crest of the Mid-Atlantic ridge. 

  Of particular note at Thingvellir are the magnificent Almannagja gorge, and the beautiful lake Thingvallavatn, the largest lake in Iceland. The popular Gjabakkahellir lava cave is also in the area.

  The fissure Silfra is located by Thingvallavatn, Iceland's largest lake, and is famous for its clear waters and popular for diving and snorkeling, as you can literally swim between continents.

  黄金圈,

  Stretching from the wide Eastfjords mountain range, set with many small fjords, through the fertile Fljotsdalsherad district and towards the highlands, East Iceland is a vast area of incredible nature, striking contrasts and fascinating history and culture.

  East Iceland is characterised by a large number of fjords, surrounded by high villages. Fishing villages can be found by most of them.

  From Seydisfjordur a ferryboat goes to Scandinavia, and the town also hosts the popular annual festival LungA. Neskaupsstadur features two highly popular annual festivals, Neistaflug and Eistnaflug, as well as being the home to a highly interesting museum and close to fascinating nature.

  The main airport of East Iceland is in Egilsstadir, the largest town of the East and its main center for service, transport and administration.

  Further inland is the fertile agricultural district Fljotsdalsherad (see the link above). Natural birchwoods are in the area, the most famous being Hallormsstadaskogur, the largest forrest in Iceland. Big rivers run through the district and by their estuaries many seals may be found.

  Up in the mountains is also the Karahnjukar Hydroelectric Power Station, the construction of which led to hot debates and continues to do so. The station serves the alumnium smelter by Reydarfjordur.

  The impressive mountain Snaefell is close by, Iceland's highest freestanding mountain. East of Snaefell is the highland oasis Eyjabakkar, one of the largest nesting place for the pink footed goose in the world.  

  Of particular cultural note in Fljotsdalsherad is the cultural and history center Skriduklaustur. In the middle ages a monastery stood there, and in the 20th century, Icelandic author Gunnar Gunnarsson lived there. Gunnar wrote such masterworks as Adventa (e. The Good Shepherd), Svartfugl (The Black Cliffs), Saga Borgaraettarinnar (Guest the One-Eyed, made into the Danish film Borgslægtens history in 1919) and the autobiographical novel cycle Fjallkirkjan ('The Church on the Mountain' published in English as Ships in the Sky and The Night and the Dream).

  Other notable attractions of the beautiful Fljotadalsherad district, of which there are many, are listed under the Egilsstadir section.

  Reindeers roam the mountains of East Iceland and a large number of migratory birds land near Hofn in  Hornafjordur, in the Southeast, on their way from Skotland, returning back to Scotland in late summer.

  Vatnajokull, Europe's largest glacier stretches to the boarders of East Iceland.

  东部冰岛,

  Reykjavik is the capital of Iceland and the northernmost capital of a sovereign state in the world.

  Despite a small population (120.000 and more than 200.000 in the Greater Reykjavik area), it is a vibrant city that draws an ever increasing number of visitors. It is the financial, cultural and governmental center of Iceland. It also has a reputation of being one of the cleanest and safest cities in the world.

  Geography

  The city of Reykjavik is located in southwest Iceland by the creek of the same name. Throughout the ages, the landscape has been shaped by glaciers, earthquakes and volcanic eruptions and the area is geothermal.  Much of the current city area area was subglacial during the Ice Age, with the glacier reaching as far as the Alftanes peninsula, while other areas lay under the sea.  After the end of the ice age the land rose as the glaciers drifted away, and it began to take on its present form.

  The coastline of Reykjavik is set with peninsulas, coves, straights and islands, most notably the island of Videy, and seabirds and whales frequent the shores. The mountain ring as seen from the shore is particularly beautiful. Mount Esja is the highest mountain in the vicinity of Reykjavik and lends its distinct feature to the whole area. This majestic mountain is also highly popular for climbing. Other notable mountains that can be seen from the seaside are Akrafjall and Skardsheidi and on clear days one may even see as far to the legendary Snaefellsjokull glacier, at the end of the Snafellsnes peninsula.

  The largest river to run through the city is Ellidaa in Ellidaardalur valley, which is also one of Iceland‘s best rivers for salmon fishing.

  Transportion

  There are no trains or trams in Iceland, but most people travel by car. The city also operates a bus system. There are two major harbours in town, the old harbour in the center and Sundahofn in the east. The domestic Reykjavik Airport is located at Vatnsmyrin, not far from the city center and close to Oskjuhlid and Perlan. The international  Keflavik Airport at Midnesheidi heath then lies around 50 km from the city. Cars, jeeps and bicycles can be readily rented in the city and many organized tours are also being offered.

  What to See & Do in Reykjavik

  The local arts scene is strong in Iceland, with both annual events and single ones, many of whom have hit the international stage. For the annual ones please check our articles Best Annual Events in Iceland and the Top Ten Festivals in Iceland. Major events taking place in Reykjavik include the Iceland Airwaves, Gay Pride, RIFF (The Reykjavik International Film Festival), The Reykjavik Literature Festival, Cultural Night, the Reykjavik Arts Festival, Food & Fun, the Reykjavik Fashion Festival and the Sónar music festival.

  Among famous people from Reykjavik are artists Bjork Gudmundsdottir, Sigur Ros, writers Halldor Laxness (born in Laugarvegur) and Arnaldur Indridason and mayor Jon Gnarr. For more well-known and fairly-well known Icelanders, check our article on the subject.

  You might also want to check our article on some of the many things to see and do in Reykjavik, such as visiting the city‘s many museums, exhibitions and galleries, checking out live music, visiting the Harpa music hall or the theaters, visiting the lighthouse at Grotta, the main shopping street of Laugavegur, visiting the old harbour and the flea market, going on a bird- and whalewatching tour or visiting Videy island. We also have a top ten list of things to do.

  Make sure to visit the publis square of Austurvollur, one of the city‘s most popular gathering places, where you‘ll also find the national parliament, Althingi, the state church a statue of independence hero Jon Sigurdson, as well as cafés, bars and restaurants. Austurvollur was central in the 2008 protests, along with Laekjargata, home to the House of Government. You are also not likely to miss the great church of Hallgrimskirkja that towers over the city from the hill of Skolavorduholt, wherefrom you‘ll get a great view of the city.

   Try a walk by the city pond, greet the many birds that frequent the area and visit the city hall, stationed by its banks. The Hljomaskalagardur is a beautiful park that lies by the pond, it ideal for a nice walk and sometimes concerts get held there. Further off is the campus of the university of Iceland, the Nordic house and the Vatnsmyri wetland, a particularly pleasant place, but be mindful of not disturbing the wildlife there and keep to the pathways.

   For a nice swim on a warm day, we particularly recommend Nautholsvik beach.

  Visit the Laugardalur valley, home to one of the city‘s best swimming pools, as well as the Asmundarsafn gallery, a beautiful botanical garden and a domestic zoo. A walk by the Aegissida beach, with it‘s old fishing sheds, in the west part of Reykjavik also holds a particular charm. The aforementioned Elllidaardalur valley is also a popular resort.  

  Another place that offers one of the city‘s best (and free) views is Perlan, up in Oskjuhlid hill. The hill itself is a popular resort, with over 176.000 trees and great opportunities for walking and cycling.

  Travel to Alftanes to see the president‘s house at Bessastadir, which is also a historical site in it‘s own right, having been the educational center of Iceland for centuries. Nearby is a beautiful lava field, Galgahraun, well worth a visit, though there is currently an environmental struggle going on as to it‘s future state.

  The city is furthermore a short drive from many of Iceland‘s major attractions, most famously the Golden Circle and the Blue Lagoon. In close vicinity you‘ll also find the Heidmork preservation area, a favorite passtime resort of the people of Reykjavik, as well as the Blue Mountains, one of Iceland‘s most beloved skiing venues.

  Check our Best of Reykjavik guide further for tips on the best cheap things to do in Reykjavik, some of the best restaurants in the city, happy hours, the top ten value places to eat and our two articles on the famous Reykjavik nightlife; Nightlife in Reykjavik and Nightlife and mating.

  Finally, we‘d like to stress that these are only some suggestions of the many things you might check out in Reykjavik. Whatever you choose to do, we hope you‘ll be able to make the most of your visit and we wish you a pleasant stay in our capital.

  雷克雅未克,

  

  Jökulsárlón is Iceland’s most famous glacier lagoon. Conveniently located in the southeast by Route 1, about halfway between the Skaftafell Nature Reserve and Höfn, it is a popular stop for those travelling along the South Coast or around the circular ring road of the country.

  Geography

  As a glacier lagoon, Jökulsárlón is a lake that is filled with the meltwater from an outlet glacier. In this case, it is Breiðamerkurjökull, a tongue of Europe’s largest ice cap, Vatnajökull.

  It stands out, however, due to the fact that it also fills with icebergs breaking from the glacier, some of which tower several stories high.

  These icebergs, other than their scale, are notable for their colouration. Although they are, as expected, largely white, most are also dyed electric blue in part, with black streaks of ash from eruptions centuries past.

  When the icebergs finally make it across the lagoon, they either drift out to sea or wash up on the nearby shore. Because of the way they glisten against the black sands of Breiðamerkursandur, this area has been nicknamed ‘the Diamond Beach’.

  In spite of being a rather recent formation, Jökulsárlón is the deepest lake in the country, with depths reaching 248 metres. With a surface area of 18 square kilometres, it is also growing to be one of the largest.

  History

  Jökulsárlón has not been around since Iceland’s settlement; it only formed around 1935. This was due to rapidly rising temperatures in the country from the turn of the twentieth century; since 1920, Breiðamerkurjökull has been shrinking at a dramatic rate, and the lagoon has begun to fill its space.

  Today, the expansion of Jökulsárlón is accelerating. As recently as 1975, it was just 8 square kilometres, and now that size has more than doubled.

  In the relatively near future, it is expected that the lagoon will continue to grow until it becomes a large, deep fjord.

  Though a dark omen for Iceland’s glaciers and ice caps in general, the retreat of Breiðamerkurjökull has resulted in an incredibly beautiful, if temporary, site. This has not been overlooked by Hollywood.

  Jökulsárlón has been featured in the James Bond films A View to Kill in 1985 and Die Another Day in 2002, 2001’s Lara Croft: Tomb Raider, and 2005’s Batman Begins.

  In 2017, Jökulsárlón was enveloped into the Vatnajökull National Park, thus it is now fully protected by Icelandic law.

  Wildlife

  Because of the wealth of herring and capelin that the tides bring into the lagoon, Jökulsárlón is somewhat of a hot-spot for Iceland’s wildlife.

  In summer, it is a nesting site for Arctic Terns; stay well away from this area, as these birds are notorious for the fierceness with which they protect their eggs, dive-bombing the heads of any they see as a threat. Skuas also nest on the lake’s shores in this season.

  Seals can be reliably spotted here throughout the year, swimming amongst or else hauling out on the icebergs. Jökulsárlón provides them with a safe haven to rest and socialise, especially considering the waters of southeast Iceland are renowned for their population of orcas.

  杰古沙龙冰河湖,

  

  Vatnajökull is the largest ice cap in Iceland and the third largest glacier in Europe, covering 8% of the island's landmass. 

  Facts about Vatnajökull 

  • Surface: 8,100 km2 
  • Average thickness: 400 - 600 m
  • Maximum thickness: 1,000 m
  • Height: 1,400 - 1,800 m
  • Highest peak: 2,200 m (Hvannadalshnjúkur)

  Information about Vatnajökull 

  Vatnajökull Glacier belongs to the greater Vatnajökull National Park, which encompasses the former national parks Skaftafell in the southwest and Jökulsárgljúfur in the north. Vatnajökull's highest summit is Hvannadalshnjúkur, which rests on top of the stratovolcano known as Öræfajökull. 

  Underneath the glacier rest some of the most active volcanoes in the country, the most notable being Grímsvötn, Öræfajökull and Bárðabunga. The volcanic activity of the glacial area occurs at intervals throughout the ages, and many geologists believe such a period is scheduled to happen in the immediate future. If their calculations are correct, it would mean a significant volcanic activity for Vatnajökull over the scope of the next half century. 

  The glacier boasts of over 30 outlet glaciers, which are channels of ice that flow out of ice caps but remain constrained on the sides to valleys. The major outlet glaciers of Vatnajökull include Dyngjujökull in the north, Breiðamerkurjökull and Skeiðarárjökull to the south; and Síðujökull, Skaftárjökull and Tungnaárjökull to the west. 

  Glaciers are in constant motion underneath their weight, as they form over centuries when the accession of snow exceeds its melting. Each year, due to the melting ice water, new ice caves form that disappear come spring. 

  • Click here for a selection of Ice Cave tours 

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  Numerous rivers run out of Vatnajökull, making up some of the greatest glacial rivers in Iceland:

  • Tungnaá (west)
  • Köldukvísl (west)
  • Þjórsá (west)
  • Jökulsá á Fjöllum (north)
  • Skjálfandafljót (north)
  • Jökulsá á Brú (north east) 
  • Jökulsá í Fljótsdal (north east)
  • Jökulsá í Lóni (south)
  • Hornafjarðarfljót (south)
  • Jökulsá á Breiðamerkursandi (south)
  • Skeiðará (south)
  • Núpsvötn (south)
  • Hverfisfljót (south)
  • Skaftá (south) 

  Vatnajökull National Park 

  The Vatnajökull National Park in its current state was established in June 2008. The park now covers an area of 14.141 km2, making it the second largest national park in Europe with a 14% coverage of the island of Iceland.

  The combined forces of volcanic and geothermal activity, glacial rivers and ice make up the different features of incredible landscapes that together give Vantajökull National Park its unique qualities. 

  Rivers divide the highland plateau to the north of the park; an area that sees massive glacial flows in the summertime. The volcanic table mountain Herðubreið towers over this particular region, along with volcanoes Askja, Snæfell and Kverkfjöll. 

  The canyon Jökulsárgljúfur was carved out by glacial floods centuries ago. At the upper end of the canyon, you'll find Dettifoss, the most powerful waterfall in Europe. Further north, the horseshoe-shaped canyon Ásbyrgi is believed to have formed when Óðinn's horse Sleipnir stepped his foot down from the heavens. 

  East around Snæfell, wetlands and ranges are home to roaming herds of wild reindeer and abundant birdlife. Steep mountain ridges make up the south side of Vatnajökull, where outlet glaciers crawl in between the ridges onto the lowlands. The sandy plains of Skeiðarársandur also lie to the south as they reach out to sea. The glacial river Skeiðará runs through this vast desert. 

  One of Iceland's most visited landmarks is the Jökulsárlón glacier lagoon, which sits at the head of outlet glacier Breiðamerkurjökull. There, large icebergs that have broken off the glacier gather to float in the lake before ending up in the Atlantic Ocean, or on the nearby Diamond Beach. 

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  • Click here for a selection of Jökulsárlón tours

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  The Future of Vatnajökull 

  The volume of Vatnajökull reached its peak around 1930 but has since been in a steady process of decline. Because of rising levels of global temperature, approximately over the last 15 years, Vatnajökull has on average lost about a metre of its thickness annually. 

  If temperature levels continue to rise, the glacier could be all but gone nearing the end of the next century, leaving only small ice caps on top of the highest mountain summits.  

  Vatnajökull and Jökulsárlón in Popular Culture

  • HBO's Game of Thrones (season 2, 2012)
  • Batman Begins (2005)
  • James Bond: Die Another Day (2002)
  • James Bond: A View to a Kill (1985) 
  瓦特那冰川,

  

  Skógafoss is one of the country’s biggest and most beautiful waterfalls with an astounding width of 25 meters (82 ft) and a drop of 60 meters (197 ft). Due to the amount of spray the cascade produces, a rainbow is present any time the sun emerges from behind the clouds.

  Located on the Skógá river, this mighty cascade is clearly visible from Route 1 and is an excellent place to stop and stretch the legs while travelling Iceland’s South Coast. The river below Skógafoss holds a large char and salmon population and is thus a favourite spot for fishermen in the summer.

  The land underneath the waterfall is very flat, allowing visitors to walk right up to the wall of water. Keep in mind, however, that this will get you drenched. Skógafoss can also be viewed from the top as a steep staircase leads to an observational platform above the cascade.

  Geography

  Skógafoss is located near the small village of Skógar, south of the Eyjafjallajökull glacier volcano. There you’ll find the Skógasafn folk museum, an open-air museum with both old wooden houses and turf houses, as well as a regional museum with various artefacts from this area.

  A part of the Skógasafn Regional Museum is the Museum of Transportation, which showcases the history and evolution of transportation, communication and technologies in Iceland. There, you can see how this nation evolved from the age of the working horse to the digital communications of the 21st century.

  The Skógasafn museum also includes a café and a museum shop, and in the village of Skógar, you will find both a hotel and a restaurant.

  At the eastern side of Skógafoss, you will find one of Iceland’s most famed hiking routes; the Fimmvörðuháls pass. The 22 km (14 mi) trail takes you along Skógá river, between two glaciers, Mýrdalsjökull and Eyjafjallajökull, before ending in the beautiful Þórsmörk valley.

  Folklore

  A gold ring is on display at the Skógasafn museum. According to legend, the ring is from a chest that was owned by Þrasi Þórólfsson, one of the first Viking settlers in the area. Folklore states that before his death in 900 AD, Þrasi buried a chest filled with gold in a cave behind Skógafoss waterfall.

  Many attempts were made to retrieve the chest after Þrasi’s death, and years later, locals managed to grasp a ring on the side of the chest. As they pulled, the ring broke off, and the treasure was lost forever. The ring was then given to the local church before it made its way to the museum.

  斯科加瀑布(森林瀑布),

  塞里雅兰瀑布是冰岛南部最著名的一个瀑布，瀑布的水流相对比较苗条，但高度在冰岛名列前茅，高达63米。瀑布非常美丽，最特别之处在于一条通向瀑布水帘背面的小径，让人可以走道瀑布后面。

  塞里雅兰瀑布,

   

  Geysir is a famous hot spring in Haukadalur valley in South Iceland. Part of the ‘Golden Circle', Geysir gives its name to hot springs all over the world.

  Though Geysir itself is hardly active anymore, the area features spectacular hot springs such as the powerful Strokkur, which spouts a vast amount of water every 10 minutes, around 15-20 meters into the air, Smidur and Litli-Strokkur.           

  North of Geysir are fumaroles, i.e. unlike the hot springs the emit hot water, only steam and gas emanate from these. You may be able to observe bright yellow stains at the fumaroles, this is native sulphur, which crysallizes from the steam. At the southern part of the geothermal area, called Thykkuhverir, you‘ll find various mud pots. Such mud pots are actually fumaroles that boil up through surface water/groundwater and may become steaming fumaroles during dry spells, rather than the usual boiling mudpots.

  About 2 km from Geysir is an old preserved natural pool called Marteinslaug. One can bathe in it and it has room for 3-5 people at a time, but care should be taken, as the area around the pool is very delicate. The temperature is 39-43°C, depending on how you are positioned in the pool. The water is slightly muddy, as the pool is built on soil, and the bottom is slippery due to algae, so caution is advised.

  In Haukadalur there has also been tree planting in recent times and today the forest Haukadalsskogur is one of the largest in South Iceland. Aspen, various types of pine, and other plants have been tried out there and experiments and research continue.  We also recommend visiting the tree museum, built in the memory of forester Gunnar Freysteinsson. There are good paths and roads in the forest and the wood is specially designed to accommodate wheelchairs.

  Haukadalur has been a church site since ancient time. The current wooden church was last rebuilt in 1938 but the variety and appearance of the church dates back to 1842, making it one of the oldest of its kind in Iceland.

  Haukadalur is indeed a historical place. It was settled during the age of settlement and scholar Ari “The Wise“ Thorgilsson grew up there. The first pastoral school in Iceland was also built there.

  For accommodation, Hotel Gullfoss is about 7 km from the Geysir area, and closer still is the Hotel Geysir.

  盖歇尔间歇泉,

  

  Gullfoss (translated to ‘Golden Falls’) is one of Iceland’s most iconic and beloved waterfalls, found on the Hvítá river canyon in south Iceland. The water in Hvítá river travels from the glacier Langjökull, finally cascading 32m down Gullfoss’ two stages in a dramatic display of nature’s raw power. 

  Because of the waterfall’s two stages, Gullfoss should actually be thought of as two separate waterfalls. The first, shorter stage of the waterfall is 11m, whilst the second stage is 21m. The canyon walls on both sides of the waterfall reach heights of up to 70m, descending into the 2.5km long Gullfossgjúfur canyon (geologists indicate that this canyon was formed by glacial outbursts at the beginning of the last age.)

  In the summer, approximately 140 cubic metres of water surges down the waterfall every second, whilst in winter that number drops to around 109 cubic metres. With such energy, visitor’s should not be surprised to find themselves drenched by the waterfall’s mighty spray-off. 

  Gullfoss makes up a part of the highly popular Golden Circle tour, alongside Geysir geothermal area and Þingvellir National Park.

  History

  In the early days of the last century, Gullfoss was at the centre of much controversy regarding foreign investors and their desire to profit off Iceland’s nature. In the year 1907, an English businessman known only as Howells sought to utilise the waterfall’s energy and harboured ambitions to use its energy to fuel a hydroelectric plant.

  At the time, Gullfoss was owned by a farmer named Tómas Tómasson. Tómas declined Howell’s offer to purchase the land, stating famously “I will not sell my friend!” He would, however, go on to lease Howells the land, inadvertently beginning the first chapter of Icelandic environmentalism.

  It was Tómas’ daughter, Sigríður Tómasdóttir, who would lead the charge. Having grown up on her father’s sheep farm, she sought to get the lease contract nullified, hurriedly saving her own money to hire a lawyer. The ensuing legal battle was an uphill struggle; the case continued for years, forcing Sigríður to travel many times by foot to Reykjavík if only to keep the trial moving. Circumstances became so difficult that Sigríður threatened to throw herself into the waterfall if any construction began.

  Thankfully, in 1929, the waterfall fell back into the hands of the Icelandic people. Today, Sigríður is recognised for her perseverance in protecting Gullfoss and is often hailed as Iceland’s first environmentalist. Her contribution is forever marked in stone; a plaque detailing her plight sits at the top of Gullfoss. 

  Restaurant / Cafe

  Besides Gullfoss, visitors can enjoy the views from Gullfoss Cafe, a locally run delicatessen that serves a wide variety of refreshments and meals. The menu has options to tantalise everyone’s taste buds; hot soups, sandwiches, salads and cakes. There is also a shop on site where visitors’ can browse and purchase traditional Icelandic souvenirs. 

  黄金瀑布(居德瀑布),

   

  The glacier volcano of Eyjafjallajokull (1651 m) is located at the borders of the South Icelandic highlands. It featured prominently in world news in 2010 when ash from its eruption halted air traffic in Europe.

  An ice cap of about 100 km with several outlet glaciers covers the caldera of Eyjafjallajökull that stands at the height of 1651 meters. The diamaeter of its highest crater is around 3-4 km2 wide and the rim has several peaks.

  Eyjafjallajokull glacier volcano lies north of Skogar, and to the west of Myrdalsjokull glacier and the massive volcano there; Katla.

  Eyjafjallajokull is thought to be related geologically to Katla in Myrdalsjokull and eruptions in the former have often been followed by eruptions in the latter.

  The 2010 eruptions

  The end of 2010 saw some small seismic activity that gradually increased and resulted in a small eruption in March of 2010, characterized by a flow of alkani-olivine basalt lava.

  This first stage lasted until April 12th and created the volcanic craters Magni and Modi at the Fimmvorduhals trail. They are so far Iceland's newest vocanic craters, and still eminate steam with lava glowing under the surface.

  However it was the second phase of the eruption that started on April 14th that created the huge ash cloud that rose about 9 km into the skies.

  This eruption halted air traffic in Europe for days, and its estimated that as many as 107.000 flights may have been cancelled during the week it lasted.

  The ejected tephra measured around 250 million cubic meters. This ash cloud lasted for six days and some more localized disruption continued into May. The eruption was officially declared to be over in October 2010, as the snow on the glacier had ceased to melt.

  Future volcanic developments?

  Eyjafjallajokull erupted in years 920, 1612 and again 1821-1823.

  Its latest eruptions were the two that occurred in 2010.

  Future volcanic developments remain unclear. The area is still highly active and can be quite unpredictable. It continues, however, to be closely monitored by The Icelandic Meterological Office.

  埃亚菲亚德拉冰盖(艾雅法拉火山),

   

  The 120 meter high promontory Dyrholaey is the southernmost part of the mainland, only a short drive south of the Ring Road. It offers a breathtaking view and features spectacular outcrops and rock formations. 

  A notable attraction is the massive arch that the sea has eroded from the heartland, giving the island its name (‘dyr’=door’). One daredevil pilot even flew through it!

  Dyrholaey has an abundance of birdlife, the most common being puffins and eider ducks. You can also enjoy the black beach, where the waves can provide an impressive sight. As these can be very wild, we do however advise uttermost caution.

  迪霍拉里,

   

  Thingvellir  is one of the most important sites to visit in Iceland for its landscape, history and cultural value.

  The Icelandic parliament was founded in Thingvellir in 930 and remained there for centuries.Thingvellir is surrounded by a beautiful mountain range and is the site of a rift valley, marking the crest of the Mid-Atlantic range. Today it is a natural park, listed as a World Heritage Site by UNESCO and considered a vital part of the ‘Golden triangle’ (with Geysir and Gullfoss). Of particular note is the magnificent gorge Almannagja, which marks the eastern boundary of the north American plate and into which the beautiful waterfall Oxararfoss falls.

  Other notable attractions within the park include the beautiful lake Thingvallavatn, the largest lake in Iceland, the Silfra fissure, one of the world's top dives, and Gjabakkahellir, one of Iceland's most interesting lava tubes. 

  辛格维利尔(辛格韦德利),

   

  Strokkur (Icelandic for "churn") is one of the most famous hot springs in Iceland and belongs to the famous Golden Circle.

  Strokkur is a fountain geyser in the Geysir geothermal area in the southwest part of the country, east of Reykjavik. Strokkur is a powerful hot spring and an impressive sight. It erupts about every 4–8 minutes and spouts water to a height of 15 – 20 m, sometimes up to 40 m.

  史托克间歇泉,

   

  Solheimajokull is a beautiful outlet glacier of the Myrdalsjokull icecap.

  Solheimajokull is a rugged glacial tounge riddled with crevasses and spectacular ever-changing ice formations, jagged ridges and sinkholes and is popular for hiking and ice climbing.

  The glacier river Jokulsa a Solheimasandur has its source at the glacier, flowing over the sand plain of Solheimasandur towards the sea.

  索尔黑马冰川,

  

  Mýrdalsjökull is a glacier in the south of the Icelandic highlands. It is the country's fourth largest ice cap, covering nearly 600 square kilometres (232 square miles), and its highest peak is almost 1500 meters tall. It is most well-known for sitting atop the notorious and explosive volcano, Katla.

  Mýrdalsjökull is visible from Route 1 on the South Coast, sitting to the north of the village of Vík. It is visited on some snowmobiling, ice caving and helicopter tours, and one of its glacial outlets, Sólheimajökull, is the most popular place in the country for ice-climbing and glacier hiking.

  Eruptions beneath Myrdalsjokull

  Since 2010, the world has known of the volcano beneath Eyjafjallajökull; after all, it halted European air travel for over a week and stumped news readers everywhere. Few, however, are aware of the much larger volcano right beside it.

  Mýrdalsjökull conceals Katla, one of the country’s most active volcanoes, having erupted, on average, once every fifty years since 930 AD. Because of the glacier above it, these eruptions tend to cause enormous ash clouds. It is these ash clouds that lead to flights being grounded, crops and livestock poisoned, and have the potential to change the world’s climate.

  

  The last major eruption beneath Katla was in 1918, in which such huge lahar floods occurred that the southern coastline was extended five kilometres outwards. This area is also very susceptible to glacial floods, or 'jökulhlaup', during eruptions, even when the lava does not break through the surface of the ice. These are as dangerous as the lava itself, having wiped out whole Icelandic villages before.

  Historically, the area was little settled for this reason.

  Katla is connected to the same volcanic system as Eyjafjallajökull and usually erupts violently a few years after Eyjafjallajökull does. As the ex-president, Ólafur Ragnar Grímsson said in 2010:

  ‘The time for Katla to erupt is coming close… it is high time for European governments and airline authorities all over Europe and the world to start planning for the eventual Katla eruption’

  So it is currently several years overdue. Katla is monitored heavily, and roads around it closed when seismic activity increases. All road closures around Iceland can be found on Road and Coastal Administration's website.

  Tours on Myrdalsjokull

  While there are no eruptions immediately imminent, tours continue to run onMýrdalsjökull, allowing visitors to enjoy the glacier. It is, for example, possible to snowmobile across its surface throughout the year and take ice caving tours beneath it from October to April, with departures from both Reykjavík and Vík.

  Considering the ice caves under Vatnajökull glacier are usually only accessible from November to March, this provides a wider window of opportunity for travellers to Iceland outside of the depths of winter. It should be noted that the caves in Mýrdalsjökull do not have the same blue ice, however.

  Tours around Myrdalsjokull

  Mýrdalsjökull can be seen on all South Coast tours that reach Vík and beyond in clear weather. It can also be seen from above on helicopter tours that depart from Reykjavík.

  The best perspectives of the glacier, however, can be found on the popular Fimmvörðuháls hiking trail, which goes between Eyjafjallajökull and Mýrdalsjökull. Part of this hike can be done in a day, or you can take the complete route from Þórsmörk to Skógar on a three-day trek

   

  Mýrdalsjökull,

  斯卡夫塔山是冰岛Öræfasveit地区的一个自然保护区，它曾经是一个国家公园，2008年，和杰古沙格鲁夫尔(Jökulsárgljúfur)国家公园合并为如今的瓦特那冰川国家公园(Vatnajökull National Park)。

  斯卡夫塔山地区的植被非常有特色，它们生长在沙地与冰川形成的特色地貌上，给整个地区带来盎然生机和独特的自然风光。从斯卡夫塔山游客中心可以沿徒步路径通向斯瓦蒂瀑布(Svartifoss，意为黑瀑布，又译为魔鬼瀑布)、Hundafoss瀑布，以及斯卡夫塔山冰川，远处是Kristinartindar山和Morsardalur山谷。

  对于户外爱好者，斯卡夫塔山是前往冰岛最高峰－华纳达尔斯赫努克火山(Hvannadalshnjúkur)的最佳营地选择。

  斯卡夫塔山游客中心(Skaftafell Visitor Center)

  在斯卡夫塔山的游客中心，您可以找到此地区最完备的信息，以及它的历史、地理知识。您可以了解以此为出发地的各个徒步线路、观光建议、住宿选择等。

  斯卡夫塔山,

  

  Þingvallavatn (anglicised to Thingvallavatn, ‘the Lake of the Fields of Parliament’) is a rift valley lake located roughly forty-minutes drive from Iceland’s capital city, Reykjavík.

  Features of Thingvallavatn

  Þingvallavatn is partially within the boundaries of Þingvellir National Park, Iceland’s oldest National Park and only one with UNESCO World Heritage Site status.

  Covering an area of 84 square kilometres (32 square miles), Þingvallavatn is the largest natural lake in Iceland with its greatest depth measuring at 114 metres (374 feet). Þingvallavatn is situated on the Mid-Atlantic Rift, on a part of the ridge known as the Reykjanes Ridge.

  The lake has only one outflow, the river Sog.

  Of particular note to biologists and fishermen are the four morphs of Arctic Char that inhabit the lake. The lake’s char are an excellent example of species evolving to fit and adapt to a secluded environment; over ten thousand years, one species of Char has transformed into four different-sub branches. Other fish in the lake include the the Brown Trout and the Three-Spine Stickleback.

  History and Geology

  Þingvallavatn takes its name from the historical founding of the Alþingi, which occurred in 930 AD at what is now known as Þingvellir National Park. Þingvellir literally translates to ‘Fields of Parliament’.

  The Alþingi was the first democratically elected representative parliament in world history (examples such as Ancient Athens were direct, not representative, democracies); Icelanders used to travel by foot or horseback simply to congregate at Þingvellir where they would hear the latest laws and judgements of the island.

  Þingvellir National Park is also notable for its geology. Given its position on the Mid Atlantic Ridge, the park is one of the only places on the planet where visitors can see both the North American and Eurasian tectonic plates standing exposed from the earth.

  Footpaths allow you to get up close and personal to the plates, standing right where the ancient settlers once did. In between the tectonic plates lies fields of dried volcanic rock, blanketed with a thick, yet fragile layer of Icelandic moss.

  Scuba Diving in Thingvallavatn

  Scuba diving around Þingvallavatn revolves around two sites, Silfra Fissure and Davíðsgjá (David’s Crack), the former being one of the most popular spots on the planet for snorkelling and underwater exploration.

  Silfra Fissure is situated between the North American and Eurasian tectonic plates and is filled with crystal-clear glacial water originating from the Langjökull ice cap. The water measures at between two degrees Celsius all year round, with a slight current preventing the fissure from ever freezing over.

  Davíðsgjá is found within Þingvallavatn and is often considered the darker and more dramatic cousin of Silfra Fissure, resembling the gorge formation so prevalent across the Mid Atlantic Rift.

  Only certain tour operators provide tours into Davíðsgjá, so make sure to do some research beforehand if you are looking to access this dive site during your time in Iceland.

   

  Þingvallavatn,

  

  Reynisfjara is a world-famous black-sand beach found on the South Coast of Iceland, just beside the small fishing village of Vík í Mýrdal.

  With its enormous basalt stacks, roaring Atlantic waves and stunning panoramas, Reynisfjara is widely considered to be the most beautiful example of Iceland’s black sand beaches. In 1991, National Geographic voted Reynisfjara as one of the Top 10 non-tropical beaches to visit on the planet.

  Reynisfjara is found around 180 km from Iceland’s capital city, Reykjavik, and is a popular stop-off for those taking a sightseeing tour along South Coast. Driving to the beach is particularly easy, taking an approximate two and a half hours from the capital.

  Folklore

  Upon visiting the beach, travellers will immediately observe rocky sea stacks sitting off the shoreline, known as Reynisdrangar. According to local Icelandic folklore, these large basalt columns were once trolls engaged in trying to pull ships from the ocean. However, as bad luck would have it, the dawn quickly arose, turning the trolls into solid stone.

  Another legend tells of a husband whose wife was kidnapped and killed by two trolls. The man followed the trolls down to Reynisfjara where he froze them, ensuring that they would never kill again.

  The sea stacks themselves are home to thousands of nesting seabirds. Species that can be found here include Puffins, Fulmars and Guillemots, making it a must-see location for all birdwatchers out there.

  Potential Dangers

  Visitors to Reynisfjara must be made well aware of the potential dangers present at the beach. First of all, the rolling, roaring waves of Reynisfjara are particularly violent, often pushing far further up the beach than many would expect.

  Visitors are advised to never turn their back on the waves, don't go chasing after them and keep a safe distance of 20-30 metres.

  Aside from these sudden and dramatic shifts in tide (known as “sneaker waves”), the currents off the shore are infamous for their strength and ability to drag helpless people out into the freezing cold open ocean. A number of fatal accidents have occurred at Reynisfjara, the last of which occurred in January 2017.

  Reynisfjara黑沙滩,

  Vik in Myrdalur valley is the southernmost village on the Icelandic mainland, located around 180 km from the capital Reykjavik.

  Vik is important as a service center for the inhabitants and visitors of the marvellous Reynisfjara beach.

  Reynisfjara is widely considered one of the most beautiful beaches on earth (see for example Islands Magazine). This black pebble beach boasts an amazing cliff of regular basalt columns called Gardar, which resembles a rocky step pyramid and out in the sea are the spectaculary shaped basalt sea stacks Reynisdrangar. The area has rich birdlife, including puffins, fulmars  and guillemots.

  维克镇,

  Hvolsvöllur is a small town of 950 people in south Iceland, conveniently located by the ring road. The local airport has flights to the Westman Islands.

  Economy and transport

  Hvolsvöllur’s main economy is services to the surrounding agricultural area, which has an additional 600 people, meat processing and tourism. 

  Museum

  The area features prominently in one of the most famous Icelandic sagas, Njál’s saga. There is indeed an excellent Icelandic Saga Centre in the town that we recommend checking out. It has two exhibitions, ‘The exhibition of Njála, introducing guests to the characters of the sagas along with the Viking cosmology and the literary art and one on the history of trade, commerce and the cooperative movement in the 20th century. You can also view a model of Alþingi, Iceland’s parliament, founded at Þingvellir in 930. There is also a nice gallery there and a good restaurant in the Saga Hall, a replica of a medieval longhouse.

  Nearby attractions

  Hvolsvöllur has a number of interesting hiking routes in its vicinity. Among interesting sights is the large and peculiar rock Drangurinn by the farm Drangshlíð, under the Eyjafjöll mountains. Hvolsvöllur is also a short drive from many other interesting attractions, among them some of Iceland’s top ones. One of Iceland’s oldest swimming pools, Seljavallalaug, is about 44 km from the town. At a 14 km distance is the rural area of Fljótshlíð and the farm Hlíðarendi. According to Njal's Saga, its hero, Gunnar, lived there.

  There is good trout and salmon fishing in the nearby rivers. Several interesting caves, both natural and man-made are in driving distance from Hvolsvöllur, 18-40 km. There is also a number of beautiful waterfalls not far off, the most well known being Seljalandsfoss, which you can walk behind, and Skógafoss, one of Iceland’s highest and most beautiful falls. Forests and groves can be found no further than  9-18 km from Hvolsvöllur.

  科沃尔斯瓦特鲁,

  

  Reynisdrangar are rock formations situated near the shore of Reynisfjara beach by the coastal village Vík í Mýrdalur on the South Coast of Iceland.

  The formations are large and impending sea cliffs, made up of the rock type basalt, that serve as a vital part of the area’s allure as they shoot dramatically out of the ocean under the looming cliffs of Mt. Reynisfjall.

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  • Visit Reynisfjara and Reynisdrangar on these South Coast Tours

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  Dangerous Waves

  The village of Vík only houses around 300 permanent inhabitants, but on a daily basis, travellers scouting the South Coast make their way there to visit what has been voted as one of the most beautiful non-tropical beaches in the world. The beach of Reynisfjara, however, can be highly dangerous if proper caution is not taken. As is evident from how the waves of the Atlantic Ocean crash upon Reynisdrangar, the currents here are strong, and sneak waves can easily carry anyone that’s standing too close out to sea. The beach is not for wading, but for admiring, and especially the mighty surf bursting on the base of these rocky cliffs.

  Folklore

  There is an Icelandic folk tale that explains the origin of the pillars’ eerie appearance. According to legend, a couple of trolls were busy dragging a stranded three-masted ship to shore when the sunlight hit them and turned them into pillars of rock for all eternity. In fact, numerous rock formations in Iceland carry with them tales of trolls or elves, and one has only to look at them to fathom why.

  Surroundings & Wildlife

  An alternative view of the bewitching cliffs and their surrounding sea can be enjoyed by venturing up Mt. Reynisfjall, by a road to the west of the village. The mountain furthermore functions as a puffin colony every summer, from April to September, meaning guests can enjoy the view in good company. Other birds can be seen gliding around the cliffs such as Arctic terns, fulmars and seagulls.

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  • See also: Puffin Watching Tours

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  Reynisdrangar石柱群,

  

  Öxarárfoss is a waterfall situated within Þingvellir National Park in southwest Iceland. 

  The waterfall flows out the river Öxará, cascading in two drops over the cliffs of Almannagjá gorge, which marks the eastern boundary of the North American and Eurasian tectonic plates. 

  Description

  The waterfall has a height of 13 metres (44 feet) and an average width of six metres (20 feet). The pool of water at the waterfall’s base is dotted with large, smooth rocks, which get especially icy in winter. The waterfall can be visited year round, but expect large crowds during the peak season of the summer. 

  During the depths of winter, the waterfall is entirely frozen over. Ice climbers have been known to scale it, but this should only be done with and by experts.

  Surroundings and History

  Öxarárfoss is one of the most popular attractions of Þingvellir Natural Park, which in turn, is one of the most popular attractions of Iceland. The National Park is one of the three famous sites of the Golden Circle along with Gullfoss waterfall and the Geyser Geothermal Area, for both geological and historical regions

  The geological reason is that, as mentioned, Þingvellir lies between the tectonic plates. As they pull apart, the land is torn, and thus there are many beautiful ravines and lava fields to be found.

  The most famous of these ravines is Silfra. Like the others, it is filled with crystal clear glacial water, which emerges from a spring, but unlike the others, it is possible to take snorkelling and diving tours here.

  The water from the crevasses such as Silfra feed into the lake Þingvellavatn; in fact, the river Öxará, which feeds Öxarárfoss, is the only source of the lake that does not come from a spring.

  The historical reason that makes Þingvellir so famous is that it was the original site of the Alþing, the Icelandic parliament founded in 930 AD. This parliament continues to exist in Reykjavík but for nine centuries flourished here.

  Icelanders would meet annually to pass laws, settle disputes, and share news. It was both incredibly progressive, giving a voice to all people and granting women divorces long before many other nations were considering it, and barbaric, hosting many battles and the prosecution of dozens of witches.

  It is thus featured in many sagas, and though not always mentioned in them, Öxarárfoss was a witness to this long history.

  One notable piece of folklore about the waterfall was that it was said to have prophetic powers for the year ahead. At midnight on New Years Eve, it would run red with either wine or blood, with the former promising prosperity ahead, and the latter warning of war.

   

  Öxarárfoss,

  

  Haukadalur is a geothermal valley in South Iceland on the popular Golden Circle route. 

  Lying to the north of Lake Laugarvatn, it is home to hot springs, fumaroles, mud pots and geysers, including the famous Great Geysir and the active Strokkur. The area is noted for the vivid colouration of its surrounding hills, caused by elements deep in the earth being brought to the surface by the geothermal activity.

  History of Haukadalur

  Haukadalur has been mentioned in historic writings as far back as 1294, in which its geysers were described following an earthquake that activated them. Since the 18th Century, it has been drawing visitors to the island including two different Kings of Denmark in 1907 and 1922.

  Throughout the 20th Century, images of the Great Geysir erupting at Haukadular began to symbolise Iceland. It’s activity, however, was unreliable, so unnatural efforts were made to stimulate it more regularly, such as lowering the water table in 1935 and pumping soap into it 1981. 

  These, however, limited the geyser’s long-term activity, so that it rarely goes off today, although, in the early 2000s, it did have a period where it was spouting water over 140 metres (459 ft) high. Even so, the geyser Strokkur is still very active, erupting to heights of 30 metres (98 ft) every five to ten minutes.

  Today, most of the near-two million visitors to Iceland will see Haukadalur Valley on their travels.

  Surroundings of Haukadalur

  Haukadalur Valley is located about an hour and a half’s drive inland from Reykjavík, thus making many sites of the South and West easily accessible. The most notable of these are the other points on the Golden Circle: Gullfoss Waterfall (about five minutes away) and Þingvellir National Park (about forty minutes away).

  It is also, however, within an easy driving distance of Flúðir, home of the Secret Lagoon, the Kjölur Highland Road, which leads into Iceland’s interior, Sólheimar eco-village, and Faxi Waterfall.

   

  Haukadalur,

  

  Svínafellsjökull in an outlet glacier of Vatnajökull, the largest ice cap in Europe. It is one of the country’s most popular places for glacier hiking due to its incredible formations and excellent views.

  Getting to Svínafellsjökull

  Svínafellsjökull is part of the Skaftafell Nature Reserve, a place of popularity amongst hikers, photographers, and those with a passion for raw natural beauty.

  This reserve was even a National Park in its own right, before the creation of the enormous Vatnajökull National Park which absorbed it.

  The reserve is easy to reach throughout the year if travelling from the capital of Iceland, Reykjavík, as it is located just off the Ring Road which encircles the country. Travelling on this route east for four hours, you will come to a left turn onto Route 998, which will take you to the car park and visitors’ centre.

  Most tours onto Svínafellsjökull start here, although some go from Reykjavík and the village of Vík. Reaching the glacier requires a short hike.

  If travelling yourself, the villages of  Vík and Kirkjubæjarklaustur are good for stopping off for fuel, rest and refreshment. There are also many significant attractions en route to admire, such as the waterfalls of Seljalandsfoss and Skógafoss and the black sand beach of Reynisfjara.

  

  Features of Svínafellsjökull

  Svínafellsjökull competes with Sólheimajökull for the country’s most popular glacier for hiking. While Sólheimajökull is closer to Reykjavík, and has better walls for ice-climbing, Svínafellsjökull has distinct appeals of its own.

  Firstly is in its surface. While Sólheimajökull, as mentioned, has walls,  Svínafellsjökull is made up of many sharp ridges that, while not possible to climb on, are much more beautiful to behold.

  Secondly, it boasts even more beautiful views from its heights. From Sólheimajökull, you can achieve magnificent panoramas over the wastelands of Sólheimasandur and the black sand beaches of the south coast, but from Svínafellsjökull, you are able to see across Vatnajökull National Park with its many other glacier outlets and mountains, the forested beauty of Skaftafell, and the ocean.

  Both glaciers, however, are matched when it comes to surrounding attractions, meaning a visit to them can incorporate many other sites. Svínafellsjökull, for example, is near to Jökulsárlón, a magnificent glacier lagoon filled with giant icebergs, while Sólheimajökull is close to the aforementioned waterfalls.

  Both also have beautiful colouration, with deep blue ice, gleaming white snow, and veins of black ash, memories of eruptions centuries past.

  If glacier hiking in summer, the colouration is less vivid but the journey easier and the views usually clearer. If hiking in winter, the intensity of the blue ice is mesmerising, and there is a greater chance of finding an ice cave on the glacier that is safe to enter.

  Svínafellsjökull’s beauty has not just been appreciated by Icelanders and visitors; it, like many other destinations in the country, was noticed by the producers of Game of Thrones.

  Many of the scenes filmed ‘North of the Wall’ in Season 7, during the dramatic battle of the penultimate episode, were shot on Svínafellsjökull. The greater Vatnajökull was used throughout the series as the base to which the Wall itself is built with CGI.

   

  斯维纳山冰川,

  The South Coast of Iceland is the country's most visited sightseeing route, along with the Golden Circle. 

  The famed South Coast shoreline stretches from the greater Reykjavík area and is dotted with natural wonders such as cascading waterfalls, volcanoes both active and dormant, black sand beaches and glacier lagoons. 

  Geography, Nature & Wildlife

  Iceland is divided into eight geographical regions. Out of these, the Southern Region is the largest, as it spans over 24.000 square kilometres with its administrative centre in the municipality of Selfoss. 

  What is known as the South Coast embodies the shoreline of this particular region. The area consists of a lowland that is mostly composed of marshlands, bays and cultivated pastures that are met by a series of black beaches where the estuaries to the east and west of the district close off the coastal body. 

  Underneath the soil rests a vast lava field, known as Þjórsárhraun. Its edges reach several hundred metres offshore where the ocean waves crash upon them, thereby protecting the lowland from the invasion of the sea. This results in the South Coast being unusually lacking in the deep fjords that so distinctly characterise the rest of Iceland's shore line. 

  The region boasts vibrant bird life during all seasons. It is not only rich with both marshland birds and seabirds but also migrating birds such as the North Atlantic puffin. Some species stay throughout the harsh Icelandic winter, including the northern diver, the loom and various species of gulls and ducks.  

  Highlights of the South Coast 

  The South Coast offers an unprecedented array of natural wonders that draw thousands of visitors each day. When driving the route from Reykjavík City, the highlights in their correct order are: 

  • Seljalandsfoss Waterfall
  • Vestmannaeyjar; The Westman Islands
  • Eyjafjallajökull Glacier Volcano
  • Skógafoss Waterfall
  • Sólheimajökull Glacier 
  • Dyrhólaey Peninsula
  • Reynisfjara Black Sand Beach
  • Reynisdrangar Sea Stacks
  • Coastal Village Vík í Mýrdal
  • Skeiðarársandur Glacial Sand Plain
  • Vatnajökull National Park
  • Jökulsárlón Glacier Lagoon 

  These attractions count for but a fraction of what the South Coast has to offer. The vast sand plains of Sólheimasandur are home to a crashed DC-3 Plane Wreck, and close to Seljavellir by the Skógar Village there's Seljavallalaug, one of the oldest swimming pools in Iceland. 

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  • Explore the many wonders of the area on these South Coast Tours

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  南岸,

  

  The Diamond Beach is a strip of black sand belonging to the greater Breiðamerkursandur glacial plain, located by Jökulsárlón glacier lagoon on the South Coast of Iceland.

  Here, the icebergs which fill Jökulsárlón glacier lagoon wash up on shore, standing dazzling and defiant in stark contrast to the black sand beach. It is, therefore, a favourite amongst photographers, nature-lovers, and wildlife-enthusiasts. Many seals call this beach home, and it is one of the best places in the country to see orcas from the shore.

  Breiðamerkursandur

  Breiðamerkursandur is a glacial outwash plain located in the municipality of Hornafjörður. The sand stretches approximately 18 kilometres along Iceland’s South Coast, more specifically from the foot of Kvíárjökull Glacier to the famed glacier lagoon Jökulsárlón, that nests by the foot of Breiðamerkurjökull Glacier.

  Both glaciers make up part of the 30 outlets of Vatnajökull, Europe’s largest ice cap and the central feature of the Vatnajökull National Park. Many of these are seen en route to the Diamond Beach as you travel along the South Coast.

  The outwash plain was formed when three of Vatnajökull’s outlet glaciers, Breiðamerkurjökull, Hrútárjökull and Fjallsjökull, flowed forward due to volcanic activity and ground the rocks of the underlying surface, creating and pushing forward the glacial sediments.

  Such sand plains are a common part of the Icelandic landscape, due to the island being volcanically active as well as boasting numerous ice caps. The terminus (the tip of a given glacier) also dug deep into the ground and left what is now the Jökulsárlón glacier lagoon. Although now the deepest lake in all of Iceland, it only began to form in 1935.

  The glacier lagoon and Diamond Beach are fantastical sites, however, the rate of their expansion is, unfortunately, a consequence of climate change. With the rate that the glaciers are melting, there may be no ice left at either site within decades.

  Jökulsárlón Icebergs

  

  Jökulsárlón glacier lagoon is one of the most famed and visited attractions in Iceland. Floating on the lagoon are enumerable icebergs that have broken off the resident glacier, creating an ever-changing scenery of incredible allure.

  The river Jökulsá connects the lagoon to the Atlantic Ocean, meaning that these icebergs eventually drift out to sea where they are polished by the waves before floating back to the black sands of Breiðamerkursandur. The name ‘Diamond Beach’ thus comes from the white ice on the black sand appearing like gemstones or diamonds, as they often glisten in the sun and sharply contrast their jet black surroundings.  

  Safety at the Diamond Beach

  The Diamond Beach is a safe place for any responsible traveller; unlike at Reynisfjara, another South Coast black-sand-beach, sneaker waves and rip currents are not notorious for whisking unwitting tourists out to sea. However, there are still dangers to consider.

  The main one of these is the icebergs themselves. Under no circumstance should you climb upon an iceberg, due to their slippery surfaces and sharp edges.

  This is especially the case if the iceberg is at all in the water, as it could flip and trap you underneath, or else be pulled out to sea by a current with you on it.

  The risk of injury and illness in the form of hypothermia is so great that extortionate fines exist to deter any ‘rebels’ looking for a thrill-seek. These have only come about due to serious incidents, to protect not only tourists at the lagoon but guides and staff who may feel obligated to embark on a dangerous rescue if they see someone at risk.

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  Diamond Beach

• 两晚住宿，私人卫浴，含早餐

• 蓝冰洞探秘旅行团

• 冰川徒步

• 英文向导

• 所有交通

• 晚餐

• 午餐

• 温暖的衣服、防水外衣

• 登山鞋和冰面防滑鞋套

• 相机＋备用电池

这个旅行团包含沿途两晚的住宿，我们为您安排了人口稀少的冰岛南岸最优秀的一些住宿选择。 第一晚您的住宿将被安排在以龙虾而著名的霍芬镇Höfn(又名赫本镇)，您将有机会在镇上选择品尝最鲜美的冰岛龙虾。在繁忙的节日期间，比如圣诞节，我们还准备了备选住宿地点－杰古沙龙冰河湖景区不远处的乡间酒店Smyrlabjörg。 第二晚您的住宿将被安排在艾雅法拉冰川附近的Hótel Eyjafjallajökull，或者维克镇的Hotel Katla，两个地区都风景秀丽宜人。