4天3夜冬季行程｜蓝湖＋蓝冰洞＋杰古沙龙｜梦幻冰岛蓝＋彩色北极光

• 运营日期 11月. - 3月.
• 长度 4 天
• 项目 观光, 船游, 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 Blue Lagoon is a geothermal spa and is the single most popular attraction in Iceland.

  The water is rich in silica and sulphur that helps make your skin shine like a baby. The Blue Lagoon also operates a Research and Development facility that helps find cures for skin ailments using the mineral-rich water.

  The temperature in the bathing and swimming area is very comfortable, and averages 37–39 °C (98–102 °F). There´s a restaurant there and it´s a truly romantic and beautiful place one should not miss while in Iceland.

  蓝湖温泉,

   

  West Iceland is home to Europe's most powerful hot spring, Iceland's most significant lava tube, fascinating glaciers, beautiful waterfalls, some of Iceland's most important historical sites and more. It has three main districts:

  Borgarfjordur

  Borgarfjordur has rich history, with Reykholt where Snorri Sturluson, author of Snorra-Edda and Heimskringla lived and featuring a medeval and cultural museum dedicated to his memory. In Borgarnes, the main village of Borgarfjordur, the Settlement Center can be found.The landscape is magnificent and includes the magical Hraunfossar waterfalls, Surtshellir lava cave, Deildartunguhver hot spring and Eiriksjokull glacier.

  Snaefellsnes

  The Snaefellsnes peninsula has its unique mountain ridge with the majestic Snafellsjokull glacier at its west end. The region around it is a national park, named after the glacier.

  Breidafjordur

  Breidafjordur is a natural reserve, a wide bay with countless small islands and home of thousands of birds. The inner part of Breidafjordur is the agricultural area Dalir. In Haukadalur is the old farm site Eiriksstadir, the home of Eric the Red, the first European to land in Greenland (in the year 984 AD). His son was Leif Ericsson, the first European to land in America (in the year 1000).

  西部冰岛,

  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 

  ---

  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. 

  ---

  • 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,

   

  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,

  

  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,
  

  Sólheimasandur is a vast area of sand and gravel along the South Coast of Iceland, between the cliffs of the interior and the modern shoreline. It was built up by immense glacier bursts sweeping from the mountains to the shore.

  Geography of Sólheimasandur

  Sólheimasandur is a glacial outwash plain, meaning when that when eruptions happen under the nearby glacier, Mýrdalsjökull, the floodwater rushes across this land for the sea.

  A glacial flood, otherwise called Jökulhlaup (one of two words taken from Icelandic in the English language, the other being geyser) is perhaps the most dangerous immediate element of an Icelandic eruption. While individuals have been killed by lava flows and bombs, many more have lost their lives to the water.

  For this reason, Sólheimasandur has no significant settlements, all the way from the village of Vík í Mýrdal to Kirkjubæjarklaustur. The whole area is vulnerable to glacial floods, which are still notoriously unpredictable to modern science.

  This is especially the case considering that the volcano beneath Mýrdalsjökull, Katla, is Iceland’s most active volcano, which carries a reputation for violently erupting, seemingly at random.

  Even if these eruptions do not break the surface of the ice, they can still cause devastating floods. In fact, these can even be more dangerous, as these eruptions are often not detected..

  If Katla is showing signs of waking, then the Ring Road going south across Sólheimasandur is often closed.

  In spite of its dark reputation, Sólheimasandur is a place of ethereal and haunting beauty. Entirely flat, composed of black sands, it is often compared to a lunar landscape, or else some kind fantastical desert. The views of Mýrdalsjökull, Vatnajökull, the Highlands and the South Coast are also magnificent in clear weather.

  Sólheimasandur is easy to reach, laying on the Ring Road that encircles the country.

  The DC-3 Plane Wreckage

  Wikimedia, Creative Commons, Photo Credit: Sekeri

  One of the most impressive sights on Sólheimasandur is the DC-3 plane wreckage. Lying abandoned in the sand, a deteriorating skeleton, with nothing but endless black sand surrounding it,  it makes an eerie destination even more ominous.

  It is a US Navy plane, that was flying across the area in 1973; until recently the US had a NATO base at Keflavík, as Iceland has no armed forces of its own. It seemed to run out of fuel - although it was later discovered that the pilot had, in fact, switched to the wrong fuel tank - and had to make an emergency landing.

  Thankfully, no one was killed or injured, although the plane was far too damaged to be repaired.

  Because there were no deaths or injuries, there is nothing tasteless about taking photos with the plane. In fact, it a popular addition to many South Coast tours. Because the wreckage is not expected to remain there for long - considering the regular glacial floods that rush through the area - it is fine to touch it. It is not recommended that you climb on it, however, for safety reasons.

  To reach the plane requires a short walk across Sólheimasandur.

   

  Sólheimasandur,

  

  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,

  

  Hallgrímskirkja is a Lutheran church, located on top of hill Skólavörðuhæð in the centre of Reykjavík. At 74,5 metres tall, it is the largest church in Iceland, and its tower offers a spectacular panoramic view over the city.  

  History and design

  The church was designed by one of Iceland’s most renowned architects, Guðjón Samúelsson, who is said to have sought inspiration for his expressionistic design from elements of the Icelandic nature. These include glaciers, mountains and trap rocks, such as the hexagonal basalt columns that surround the waterfall Svartifoss in Skaftafell National Park. 

  The church took 41 years to build, with construction starting in 1945 and finishing in 1986. The leaders of the Church of Iceland wanted a building that would tower over the Catholic church of Landakotskirkja, also designed by Samúelsson. The large pipe organ inside Hallgrímskirkja, consisting of over 5000 pipes, was built by German Johannes Klais of Bonn and its construction was completed in December 1992. 

  Outside the church stands its predecessor; a statue of Leifur Eiríksson by American sculptor Alexander Stirling Calder. The statue was a gift from the United States in 1930, on the millennial anniversary of Iceland’s first legislative body Alþingi, founded in Þingvellir in 930 AD. Leifur Eiríksson was a Norse explorer from Iceland who discovered the continent of North America in the year 1000, more than half a century before Christopher Columbus. 

  Culture 

  The church’s namesake is Icelandic priest Hallgrímur Pétursson, a 17th-century poet and author of The Passion Hymns (Passíusálmar). The hymns are a vital part of Icelandic religious tradition and a stable of local literature, having been reprinted over 75 times since their original publishing in 1666. 

  The tower of the church is each day visited by hundreds of spectators who seek to enjoy its sweeping view of the capital. The observation tower can be accessed via a lift. Hallgrímskirkja counts as the most iconic landmark of the city of Reykjavík and is visible throughout most of the capital. It serves as a focal meeting point for several cultural events, for example, an annual gathering for watching the fireworks on New Year’s Eve. 

  哈尔格林姆斯大教堂,

  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,

  

  Keflavík International Airport (KEF) is Iceland’s only international airport and the port of arrival for the vast majority of visitors to the country. In 2016 alone, almost seven million passengers went through its gates.

  The History of Keflavík International Airport

  Keflavík International Airport is a relic from the ‘invasion of Iceland’ in World War II, when Allied troops took over the island nation following the defeat of its colonial ruler, Denmark, at the hands of the Nazis.

  The British laid out a landing strip in the town of Garður, but considering Iceland’s incredibly strategic position in the middle of the Atlantic Ocean, one strip was not quite enough.

  After taking control of the ‘occupation’, US troops constructed and opened two airfields for military purposes in 1942 and 1943. Though they returned the property after the war, the United States reclaimed it in 1951 after a controversial defence alliance with Iceland.

  This pact, and the general joining of NATO in 1949, caused decades of national protest, comparable to the ‘Women’s Day Off’ marches in 1975 and the ‘Kitchenware Revolution’ which followed the 2007 economic crash. The circumstances of it, however, also allowed decades of development at Keflavík Airport.

  The airport first started to separate civilian and military use in 1987, with the opening of the Leifur Eríksson Terminal. Named after the first European to settle the Americas, it would go on to handle all the guests coming to or leaving Iceland.

  The arrangement that the US would provide Iceland’s defences continues to this day, but their permanent bases at Keflavík were left at the expiration of the treaty in 2006. The airport was thus moved into full control of Icelanders and has expanded as a civilian hub ever since.

  Keflavik International Airport Today

  

  Keflavík International is located on the tip of the Reykjanes Peninsula, Iceland’s south-westernmost region. The drive to the capital city of Reykjavík is only about forty-five minutes, and there is a bus service that continuously runs between the locations, day and night.

  This service provides guests with the option to stop at the Blue Lagoon en route in either direction, the iconic health spa renowned for its healing azure waters. The lagoon sits between the airport and the capital, refreshing guests after a long flight, or revitalising them in preparation for one.

  The airport itself has all the modern amenities one would expect from a port that experiences so much traffic. It has restaurants, bars and cafés, banks and money transfers, car rental options available, a smoking area and, of course, many options for duty-free shopping.

  Considering the price of and lack of availability of alcohol in Iceland, it is the best place to stock up on any tipple desired for your trip. Otherwise, you will have to locate specialist alcohol shops, which have limited opening hours, are sparse in the remote regions of the country, and have high taxes and duty.

  The main airlines that arrive at and depart from Keflavík are the two national carriers, the prestigious Icelandair and budget airline WOW. Over thirty different carriers have chartered flights to the port, however, which head to over ninety different destinations. This is only ever increasing, with new travel routes emerging as Iceland’s popularity continues to skyrocket.

   

  Keflavik International Airport,

  

  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.

  ---

  • 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.

  ---

  • See also: Puffin Watching Tours

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  Reynisdrangar石柱群,

  Wikimedia. Creative Commons. Credit: Praveen Kumar Bodigutla

  Skaftafellsjökull is a glacier tongue spurting off from Iceland's largest ice cap, Vatnajökull.

  Skaftafellsjökull itself

  The glacier tongue of Skaftafellsjökull sits in Skaftafell, a nature reserve in Öræfi, Vatnajökull National Park. It is one of many tongues stretching from the largest glacier in Europe, Vatnajökull itself. This ice cap covered eleven percent of the surface area of Iceland.

  This reserve was once a national park in its own right, before it was enveloped into a new, much greater one. The Vatnajökull National Park was created to incorporate many other protected areas, including the Jökulsárlon glacier lagoon in the south and the Jökulsárgjlúfur canyon in the north.

  It is now the largest national park in Iceland.

  Skaftafellsjökull is an excellent but concerning example of how climate change is steadily affecting the glaciers in Iceland.

  Over the last decade, Skaftafellsjökull has been receding dramatically, only strengthening the argument that environmental policies must look to preserve Iceland's unique, important and beautiful natural features.

  Many trees have been planted in the area to help absorb carbon dioxide around the glaciers, but tragically, many scientists believe that this is too little, too late.

  It is possible to hike Skaftafellsjökull's surrounding area in order to secure a fantastic perspective of this glacier tongue. After checking in with the Skaftafell Visitors Centre as to the best hiking trails and conditions, guests will follow an eight kilometre (five miles) trail (there and back), up 390 metres (1,280 feet) to the waterfall, Svartifoss.

  From here, you will be able to look out on the glacier and its adjacent lagoon.

  Svínafellsjökull

  Skaftafellsjökull and Svínafellsjökull are both glacier tongues of Vatnajökull within Skaftafell, and are often mistake for each other. For ease, the latter is often referred to as the former, though both are distinct features.

  The majority of glacier hiking tours in this part of the country are in fact done on Svínafellsjökull.

   

  Skaftafellsjökull,

  

  Breiðamerkurjökull is the glacial tongue that extends from southern Vatnajökull and into the glacier lagoon Jökulsárlón, creating the icebergs that define this beautiful landmark.

  Breiðamerkurjökull is constantly retreating, breaking and melting, causing the Jökulsárlón glacier lagoon to increase in size; it is less than a century old, but already the deepest lake in Iceland.

  This glacier tongue provides the lagoon with all of its enormous icebergs, which perpetually break from off its tip and tumble into the waters. Here they float for about five years until they are small enough to make their way towards sea. When they finally do escape the lagoon, most join the countless smaller ice chunks that adorn the nearby Diamond Beach.

  Breiðamerkurjökull is beset with enormous cracks and crevices, and since it's virtually impossible to tell exactly when the next big block of ice will break from it, people should admire this enormous glacier tongue from a great distance.

  Breiðamerkurjökull,

  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. 

  ---

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

  ---

   

  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.

  ---

   

  Diamond Beach

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