8日夏季套餐｜格陵兰一日游＋冰岛南岸＋斯奈山＋杰古沙龙＋黄金圈

• 运营日期 6月. - 8月.
• 长度 8 天
• 项目 冰川徒步, 浮潜, 岩洞, 雪地摩托, 骑马, 观鲸, 观光, 船游, 温泉, 文化, 观鸟, 飞机
• 难度 容易
• 最低年龄 10 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,

   

  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,

  

  Hvíta is a glacier river in Arnessysla in South Iceland. It is one of the most popular rivers in Iceland for rafting, salmon fishing, and it is home to Iceland's most famous waterfall.

  Gullfoss Waterfall

  The river has its source in Hvítarvatn, by the roots of Langjökull. Many tributaries join it as it travels towards the ocean, making Gullfoss waterfall, which lays on its course, mightily powerful.

  At 32 metres (105 feet) tall, it falls in two steps into a magnificent canyon. There are several viewing platforms around it, and a café and visitors centre a short distance away.

  It can be seen in all seasons, with rainbows flying from its mists in summer and ice cladding the rocks around it in winter.

  Rafting in Hvíta

  Downstream from Gullfoss is the part of Hvíta that is most popular for kayaking, canoeing and rafting. To participate in rafting tours here, no experience is needed.

  These tours are not only exhilarating but expose guests to beautiful nature and geology.

  Hvítá River,

  

  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,

  

  Snæfellsjökull (1446 m) is an ice-capped volcano found on the tip of the Snæfellsnes Peninsula in West Iceland.

  Though many consider Snæfellsjökull to simply be a particularly impressive ice cap, it is, in fact, a 700,000-year-old glacier-capped stratovolcano. The mountain is actually called "Snæfell" (Snowy Mountain), though the “jökull” (Glacier) is often added to help distinguish it from other mountains of the same name. For the first time in recorded history, Snæfellsjökull had no snow or ice at its peak in August 2012, causing concern amongst locals that climate change is threatening the nature of the mountain.

  On clear days, one can see Snæfellsjökull from Iceland’s capital city, Reykjavik, approximately 120 kilometres away over Faxa Bay, making for an impressive sight—and a tick off the bucket list if you can’t make it to travelling across the Peninsula itself. The volcano makes up just a small part of the larger Snæfellsjökull National Park.

  History

  Nearby villages include Hellissandur, Rif and Ólafsvík, all of which were commercial and fishing hubs throughout the peninsula’s long history of human inhabitance. Fishing took off primarily in the 13th-Century, with fishing stations being built in all areas with easy access to the open ocean.

  One notable example would be the settlement of Dritvík, one of the largest fishing stations in Iceland at the time, utilising around 40–60 boats and employing between 200–600 people. Fishing in the region declined during the 19th century due to a change in Iceland’s fishing practises, though it is still an important source of livelihood for those living on the Peninsula.

  Snæfellsjökull has, for centuries, been considered to be one of the world’s ancient power sites, a source of mysticism, energy and mystery for the peninsula’s superstitious population. This likely has something to do with the stratovolcanoes place in the Icelandic sagas; the feature takes a prominent role in Bárðar saga Snæfellsáss, a late 14th-century saga that tells the story of Bárður, half-human-half-troll, who became the “guardian spirit of Snæfellsjökull.”

  In Literature

  Snæfellsjökull serves as the entrance to a fantastical subterranean world in Jules Verne’s classic 1864 novel “Journey to The Centre of The Earth.” Given its central place in the novel, Snæfellsjökull has become one of the most popular spots for visitors in Iceland and has inspired a wealth of writers, poets and artists.

  Since “Journey to The Centre of The Earth”, Snæfellsjökull has appeared in the Blind Birds trilogy by Czech SF writer Ludvík Souček (partially based on Jules’ work) and in Under The Glacier, a novel by Iceland’s only Nobel laureate, Halldor Laxness.

  Nearby Attractions

  Along with the glacier, attractions include the two nearby basalt cliffs called Lóndrangar and the many fascinating lava formations at the beautiful Djúpalonssandur beach, such as the arch rock Gatklettur. At Djúpalonssandur, one can also test their strength just as the ancient sailors once did with the four "strength" stones, Amlóði ('Useless'), Hálfdrættingur ('Weakling'), Hálfsterkur ('Half Strength') and Fullsterkur ('Full Strength'). In the area, one can also explore the Saxhóll volcano crater and 'the singing cave' Sönghellir, which is named after the loud echoes inside.

  斯奈菲尔冰川,

  

  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),

   

  Hraunfossar in Borgarfjordur district is a series of beautiful waterfalls  formed by rivulets streaming from a short distance out of the Hallmundarhraun lava field.

  The lava field flowed from an eruption of one of the volcanoes lying under the glacier Langjokull. The waterfalls pour into the Hvita river from ledges of less porous rock in the lava. These are some of the most magnificent falls found in Iceland and not to be missed.

  赫伦瀑布群(熔岩瀑布),

  Deildartunguhver, by Reykholt, in Borgarfjordur district, has the highest flow rate for a hot spring in Europe.

  The flow rate of Deildartunguhver is 180 liters/second and water emerges at 97 °C. The place is also unique for being the only place in the country where the hard fern grows.

  德尔达图赫菲,

   

  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,

  Snaefellsnes is a large peninsula extending to the west from West Iceland ending with a national park, Snaefellsjokull National Park, where the glacier towers over the scenery, as can sometimes be seen from Reykjavik, lending its beauty to the area. 

  Snaefellsnes peninsula

  The peninsula stretches over 100 km to the west as a mountain ridge that includes active volcanoes and is unique in the variety of mountains found. 

  A few small and beautiful villages are located on the south side and a few fishing villages are on the north side: Rif, Hellissandur, Olafsvik, Grundarfjordur and Stykkisholmur. The last one is highly popular for travelers, featuring a volcano museum and a ferry that takes you across the fascinating Breidafjordur bay to Brjanslaekur on the south border of the Westfjords.

  Other museums you might want to check out are the Maritime Museum at Hellissandur, the regional museum Pakkhusid at Olafsvik, and, last but not least, the shark museum at Bjarnarhofn, indeed listed as the nr. 1 Snafellsnes attraction by Lonely Planet Travelers. Also, many of the Icelandic sagas take place at Snaefellsnes.

  Snaefellsnes has an abundance of interesting sights. At the national park, you can witness the impressive lava formations of Djupalonssandur creek and test your strength on its four stones, see the two massive lava formations that compries Londrangar, explore the Saxholl volcanic crater and enjoy the echo of 'The Singing Cave', Songhellir. You may also hike on the majestic Snaefellsjokull glacier. The glacier has strong ties with folklore and was the setting for Jules Verne's Journey to the Center of the Earth.

  Other sights we can recommend at Snaefellsnes recommend include Raudfeldsgja canyon, east of the national park and the rugged and colourful Berserkjahraun lava field, near Bjarnarhofn, on the north side of the peninsula.

  Last, but not least, Snaefellsnes is one of the main setting for Laxdaela saga. Chieftain Snorri godi, Gudrun Osvifursdottir, Bolli Thorlakssson all lived there as well as his namesake Bolli Bollason, the first West Norse member of the Varangian guard, an elite unit of the Byzantine army. Iceland's most famous mass murderer, Axlar-Bjorn, also lived at Snaefellsnes. 

  斯奈山半岛,

  Wikimedia, Creative Commons, Photo Credit: Axel Kristinsson

  Hválfjörður is a fjord in southwest Iceland. The fjord is approximately 30 kilometres (19 miles) long and five (three miles) kilometres wide.

  Nature and Landscape

  The landscape of Hválfjörður is varied and beautiful, with wide areas of flat land along majestic mountains, green vegetation in summer and beaches cut with by creeks.

  The area is rich in birdlife and is home to seals, but despite its name, which translates to ‘Whale Fjord’, it is not known for its whale or dolphin population. Two theories exist on how it got its name; either that it was once home to whales before fish stocks moved away, or because of the general shape of the bay.

  The area has recently been part of Iceland’s successful reforestation effort. 

  Natural attractions in the area are plentiful, but most significant is Iceland's highest waterfall, Glýmur, in the river Botnsá. There are also plenty of interesting hiking trails in the area, such as Sildarmannagotur, leading north, and Leggjabrjotur, leading east towards the area of Þingvellir National Park. 

  History and Culture

  Historically, Hválfjörður was home to one of the main whaling stations in Iceland, with ships heading out into Fáxaflói Bay. It was one of the most important naval stations in the North Atlantic during World War Two, when Iceland was occupied by the Allies, after the Nazis conquered Denmark.

  The old whaling station and a war museum can be found in the fjord. 

  Iceland's main psalm poet, Hallgrímur Pétursson, writer of the ‘Passia Hymns' lived in Hválfjörður. The area was also the home of the late Sveinbjörn Beinteinsson, rhymes poet and performer and head of the Icelandic pagan association. 

  Economy

  Most inhabitants of the fjord live in rural areas, and there is some farming in the area. Until the 1990s those travelling between Borgarnes and Reykjavík had to take a long detour around the fjord, but this was solved with a tunnel that travels beneath it, finished in 1998.

  Grundartangi spit in Hválfjörður has one of the largest harbours in the country and two industrial plants. One is a ferrosilicon plant, operated since 1979, the other an aluminium smelter, operated since 1998.

  Both of these were controversial during their construction, and continue to be controversial during their ongoing operation. Along with whaling and hydroelectric dams, smelters and silicone plants are the hottest environmental debates going on in Iceland.

   

  Hvalfjörður,

   

  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,

  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,

  

  Silfra is a fissure filled with fresh spring water within Þingvellir National Park, and one of the country’s most cherished wonders. Snorkelling and diving in its crystal-clear waters is an experience that is both thrilling and relaxing, and it is now considered to be one of the top five dive sites in the world. It takes around an hour to reach Silfra from Reykjavík. 

  Geography of Silfra

  

  Silfra fissure opened in 1789, due to the movements of the tectonic plates that frame Þingvellir National Park. The North American and Eurasian plates, which run all the way through Iceland, separate at about 2 centimetres per year, and as they do, they tear open fissures in the land between them. 

  Some of the ravines fill with water travelling underground through the porous lava fields in the area, originating from Langjökull glacier about 60 kilometres north. It can take the water up to a century to reach Silfra and this long filtration process results in the water being both extremely clear and drinkable.

  

  Because the water travels underground, it maintains a constant temperature of two to three degrees Celsius and does not freeze over immediately at the source of the spring. Snorkelling and diving tours are thus open throughout the year.

  The clarity of the water is what draws most visitors. The visibility can extend to over 100 metres, allowing you to see the canyon walls and bottom like you are floating over a great cathedral.

  The last colour that water absorbs is blue, which means that when you look forward in Silfra, it is as if you are looking into an ethereal, vivid, azure world. The clarity also means that sun-rays refract through the surface of the water, creating rainbows on Silfra’s bed when the weather allows. 

  Snorkelling in Silfra

  

  Snorkelling in Silfra fissure is a highly enjoyable activity, but you must meet some prerequisites to be able to join. These are as follows:

  • You must be able to swim
  • You must be over 16
  • You must be in good physical health
  • You must be at least 145 centimetres and 45 kilograms
  • If you are over sixty, you will need a medical waiver
  • If you are over forty-five with a history of heavy alcohol use and pipe smoking, you will also need a waiver

  The most common option for snorkelling is to conduct it in a drysuit. Drysuits work with a fluffy undersuit to keep your body free from water and insulated against the cold, making the task of swimming through the near-freezing temperature more than achievable. 

   

  While drysuit snorkelling is the most comfortable and popular option, a few tours allow you to go through Silfra wearing a wetsuit. Wetsuits, made of neoprene, allow water to surround your body in a thin layer, that your body then heats up and uses to protect you. Though they grant you more flexibility, they are not so warm, so this should be done by the daring; you will also need to be at least 50 kilograms to snorkel in a wetsuit.

  In all tours, you wear neoprene on your head and hands to allow for better mobility, a mask and snorkel, and a pair of fins, all of which are provided on site. The course of Silfra takes approximately forty minutes, and there is a gentle current throughout, meaning it requires minimal energy to traverse.

  Diving in Silfra

  

  Diving through Silfra gives an extra dimension to its beauty, as you will be able to look up and see the sun glistening upon the surface as you cruise through the crystal clear waters. However, considering the risks associated with diving in cold water and cumbersome equipment, all who partake must meet all the requirements above, as well as one of the following:

  • You must be a qualified diver with a certification in a drysuit speciality, OR
  • You must be a qualified diver with at least 10 logged dives in a drysuit conducted over the past two years, signed by an instructor or divemaster.

   

  Silfra,

  Photo from Thrihnukagigar Volcano Tour

  Þríhnúkagígur is a dormant volcano in west Iceland, famous for its enormous magma chamber. It is the only magma chamber in the world that can be entered, and has a depth of 213 metres (699 feet).

  Formation of Þríhnúkagígur

  Þríhnúkagígur was a normal volcano in Iceland’s Blue Mountain range, also call Bláfjöll. However, its last eruption, almost 2,000 years ago, had some very unusual consequences.

  After an eruption, the magma chamber of a volcano, now free of pressure, usually remains full of lava that cools into solid rock until the next eruption. If the magma chamber is fully emptied, the volcano will usually collapse in on itself.

  To the bewilderment of scientists, however, neither of these things happened to Þríhnúkagígur.

  It seems that a rift beneath the chamber drained it of all remaining lava, leaving behind an enormous chamber, that covered an area of 3,270 square metres (35,200 square feet). To give some idea of the scale of this, the Statue of Liberty could stretch her limbs within it, and it could comfortably fit Hallgrímskirkja church.

  Unusually, the volcano did not collapse, and it has remained unchanged since.

  Discovery and Exploration of Þríhnúkagígur

  The vast magma chamber under Þríhnúkagígur would not be discovered until 1974, by an Icelandic cave explorer. Its discovery made world news, as volcanologists had not seen anything like it before, and were fighting to try to explain its existence.

  In 2012, it was opened for tourism. A lift, akin to those used in mining, was installed, and visitors were now allowed to join tours plumbing its depths.

  Its popularity comes not only from the uniqueness of the tour and the scale of the chamber, but the incredible colouration within it. Mineral deposits dye the walls vivid shades of red, yellow, green and blue, making the incredible space that much more ethereal.

  Reaching Þríhnúkagígur requires a short but uphill hike, which can be done by any steady on their feet with a reasonable level of fitness. Tours only operate in summer.

   

  Þríhnúkagígur,

  

  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,

   

  Hellnar is an old fishing village on the westernmost part of the Snaefellsnes peninsula. It used to be one of the largest fishing stations of the peninsula, the oldest record of seafaring there being from 1560.

  At the shore are spectacular rock formations. Among them is a protruding cliff called Valasnos. Tunneling into the cliff is a cave renowned for its changing colourful hues, according to the light and sea movement. Large colonies of birds also nest in the area.

  At Gvendarbrunnar a.k.a. Mariulind you can taste excellent spring water which is said to have healing powers.

  Hellnar hosts the guesthouse for Snaefellsnes National Park and has a very interesting exhibition about the economy of former times and on the geology, flora and fauna of the national park.

  海勒那尔小镇,

  

  Reykholt is a tiny village in west Iceland, which was once home to one of the world’s greatest medieval writers. Packed with history and culture, this little settlement should not be overlooked

  Reykholt: Home of Snorri Sturluson

  Reyholt’s fame comes from the fact that it was the home of the legendary writer, historian, chieftain and lawspeaker Snorri Sturluson. Though his name is not well-known outside of the Nordic world, without him we would know much less about medieval northern European history than we do today.

  His two most famous works are Prose Edda and Heimskringla. The former is an account of the Old Norse Mythology, which was otherwise kept alive only by oral tradition.

  It tells about how the pagans thought the world was created and how it would end, and the deities that sparked fear and awe in them, most famously Odin, Thor and Loki. Considered an epic poem akin to Homer’s Odyssey to many, it has inspired the fantasy genre perhaps more than any other work in the world.

  Heimskringla is an account of Norwegian kings, told as sagas. It depicts what most historians consider to be an accurate depiction of relations across northern Europe from the 9th Century to the end of the 12th.

  It is through this work, therefore, that we can learn about how the Vikings related to the kings of places such as the not-yet United Kingdom, how the jarls and clans disputed, and how they formed governments that have lasted to this day.

  Though Snorri is best remembered for his works, his life was also a fascinating tale somewhat similar to that of a Game of Thrones character.

  Aside from being a beloved poet and writer, he was a chieftain and later lawspeaker for Icelandic parliament, as well as a spokesperson, agent and, to some, lackey of the Norwegian king.

  His influence and actions propelled Iceland’s civil war into chaos, and he met betrayal from every side, resulting in his eventual assassination. The taboo of this execution, however, meant that Snorri was remembered as a hero, rather than the divisive figure he often was.

  To add to the Game of Thrones flavour, he was also notorious for infidelity, and fathering children up and down the country.

  In honour of Snorri’s life and works, Reykholt is home to Snorrastofa, a centre on his contribution to medieval studies.

  Reykholt and Surroundings

  

  Even if you have little interest in Snorri, Reykholt is a beautiful town, well worth a visit. It has a wealth of geothermal activity, and one of the country's oldest structures, Snorralaug geothermal pool, can be found here.

  Reykholt is also the closest settlement to the popular waterfalls of Hraunfossar and Barnafoss. The former of these, the ‘Lava Falls’, are serene and unique, while the latter, the ‘Children’s Falls’, is rapid and dramatic.

  It is also close to Deildartunghver, the highest flowing hot spring in Europe.

  If you're looking to stay more than a day in Reykholt or nearby, there are several hotels in the vicinity, among them the the beautifully built boarding school that functions as an Edda-hotel in the summer. There are also a wealth of cabins and bungalows to be rented here.

   

  Reykholt,

  Barnafoss ('Children's Waterfall') is a waterfall in Hvita river in Borgarfjordur.

  The waterfall runs through a narrow rocky gorge and legend has it that there once was a natural stone arc over the river, that was demolished after two children fell from it to their death. Not far away is the stunning series of waterfalls Hraunfossar, flowing out of a lava field into Hvita. 

  儿童瀑布群,

  The mighty Langjokull (“The Long Glacier“), in the midwest highlands is the second-largest glacier in Iceland, at 935 km2. For jeep and snowmobile trips, Langjokull is the most popular glacier in Iceland and skiing and hiking is possible as well. We stress that under no circumstances should one travel alone on Langjokull, as there are many cracks in the glacier. Experience of the area, whether that of yourself or of those traveling with you is all important.

  Highland tracks

  Two main highland tracks, connecting the north and the south, lie alongside the glacier, Kaldidalur road and Kjalvegur (a.k.a. Kjolur road). The Kaldidalur road stretches from Thingvellir northwards to Husafell (in Borgarfjordur district), between Langjokull and Ok shield volcano. Kjalvegur lies east of Langjokull and west of Hofsjokull glacier, starting near the famous Gullfoss waterfall to the south and the Svartakvisl stream by the Hveravellir geothermal area to the north.

  The Landscape of Langjokull

  Langjokull is about 50 km long and 15-20 km wide. The volume of the glacier is 195 km3 and the ice is around 580 m thick. The glacier reaches its highest point at the northernmost part of the glacier, which is called Baldjokull, rising around 1450 m above sea level.

  Counting west and southwards from there, outlets extending from the main glacier are Thristapajokull, Flosajokull, Geitalandsjokull, Flosajokull, Geitlandsjokull and West- and East Hagafellsjokull furthest south, separated by Mt. Hagafell. On the eastside from north to south are Leidarjokull, Kirkjujokull, Nordurjokull, and Sudurjokull.

  The glacier lies over a massif of hyaloclastite mountains that rise highest in the south and the east. The tops of these mountains can be seen in certain places on the glaciers. To the northeast are Hyrningur (1320 m), Peturshorn (1358) m), Fjallkirkja (1248 m) and Thursaborg (1315 m), a mighty series of immense rock pillars rising high to the sky. In the southern part of Langjokull, between Lonsjokull and Vestri-Hagafellsjokulll is the 995 high Klakkur.

  Notable nearby mountains

  The main mountains that lie close to Langjokull to the north are Krakur and the Burfjoll mountain range, slightly eastwards. East of Baldjokull are Hafjall and the Thjofadalafjoll mountain range. Hrutfell with the Hrutfellsjokull glacier cap (1396 m) lies east of Fjallkirkja and is the most impressive mountain of the Kjolur area, along with Kjalfell (1008 m), further northeast.

  On the south eastern side of Langjokull, between the outlets Nordurjokull and Sudurjokull lies Mt. Skridufell (1235 m) and south of Sudurjokull is the shield volcano Skalpanes. Further east, i.e. south of Hvitarvatn is the 1204 m high Blafell and south of Skalpanes is the impressive palagonitic mountain range Jarlhettur. Among the most prominent mountains south of the Langjokull glacier is Hlodufell at 1186 meters and the Skjaldbreidur shield volcano further east.

  Among the most prominent mountains to the west of Langjokull are Hafrafell,  south of Eiriksjokull,  North- and South Hadegisfell, Ok volcano, Prestahnukur volcano, and Stora- and Litla Bjornsfell.

  Nearby glaciers

  Glaciers located near to Langjokull are Eiriksjokull, to the west, the highest mountain of West Iceland, and Thorisjokull, further southwest. Hrutfellsjokull lies on the east side of Langjokull.

  Between Thorisjokull and Geitlandsjokull is a valley called Thorisdalur. Along with stunning views it features prominently in Icelandic folk tales and the outlaw Grettir the strong of Grettis saga fame is further reported to have resided there for one winter.

  Glacier-fed rivers & lakes

  Two glacier rivers, both bearing the name of Hvita (‘White River’) trace their sources to Langjokull. The first is the mighty Hvita in Arnessysla county, home to Iceland‘s most famous waterfall, Gullfoss, the beautiful Bruarhlod canyon and one of Iceland‘s most popular rafting rivers. The source of this river is Hvitarvatn lake, east of Langjokull. The outlet Nordurjokull reaches the lake and lends it a distinctly glacial colour. Sudurjokull used to reach it as well but has retreated in recent times.

  The other Hvita glacier river, in Borgarfjordur, also has its source in the area, by Eiriksjokull glacier. In this river are the beautiful waterfalls Hraunfossar and Barnafoss. Indeed, many of the hot springs in Borgarfjordur receive ground water from Langjokull. Sub-surface water also flows south to Lake Thingvallavatn, reappearing in springs in and around the lake. A few rivers flowing north to Hunafloi bay also have their sources there.

  To the south, Eystri-Hagafellsjokull feeds a lake called Hagavatn and several smaller river flow from there to lake Sandvatn. In turn, rivers flow from this lake to two major rivers i.e. Hvita in Arnessysla  & Tungufljot. Tungufljot later joins up with Hvita and Hvita itself merges with Sogid river as Olfusa and this river then flows towards the sea.

  Volcanism

  There are at least two active volcanic systems under Langjokull glacier, whose calderas are visible from the air. The best known of these is the geothermal area of Hveravellir, east of Baldjokull. Also to the east lies the Kjalhraun lava field, which flowed about 7800 years ago.

  To the northwest of the glacier is another system that produced the vast Hallmundarhraun lava field, through which Hvita in Borgarfjordur runs, with its stunning falls. Also in the area is Iceland‘s longest lava cave, the fascinating Surtshellir.

  Southwest of Langjokull is the Presthnukur lava field, its fissures extending under Langjokull. South of the glacier is the Lambahraun lava field and further east, i.e. south of Thorisjokull, lies the Skjaldbreidarhraun lava field and the Skjaldbreidur  shield volcano.

  Compared to other regions in Iceland, the area is considered relatively calm, with only 32 eruptions in the last 10.000 years.

  Global warming

  Langjokull is shrinking fast and concerns have been raised about the glacier due to the effect of global warming. Some researchers feared that if climate change continues at its current rate the glacier may be gone in about 150 years.

  朗格冰川,

  Wikimedia, Creative Commons, Photo Credit: Geri340

  Gerðuberg is a row of perfectly shaped hexagonal basalt columns that run along a cliff on the southern side of the Snӕfellsnes Peninsula, in west Iceland.

  Geology of Gerðuberg

  The cliff on which the Gerðuberg columns reside is over a kilometre long, with columns between seven and 14 metres (23 to 46 feet) tall and up to one and half metres (five feet) wide. Many have compared the feature to a fortress wall.

  The most unusual thing about Gerðuberg is how the columns are so geometrically symmetrical that they seem to be carved by hand. Such features are rare around Iceland and the rest of the world, but easily explained by science.

  During an eruption thousands of years ago, rivers of lava ran off the cliffs here, in very equal flows. The sea rapidly cooled them, causing them to take this unique and unusual shape.

  Other places in Iceland that they can be found include Hofsós, in north Iceland, and from the river Hvíta on a rafting tour.

  The Snӕfellsnes Peninsula is defined by a long range of volcanoes, with the Snӕfellsjökull glacier volcano being the most renowned. Lava flows like those that cause Gerðuberg have not occurred in the area for hundreds of years.

  Getting to Gerðuberg

  Gerðberg is usually the first major site visitors to the Snӕfellsnes Peninsula see as they as they approach it from Reykjavík, and travel along its southern side (excluding the Eldborg crater, which is a little inland). The cliffs with these strange columns runs adjacent to the road and sea, making them impossible to avoid.

  While a marvellous feature to see, they are just one of many on the peninsula. Travelling clockwise from Gerðuberg, guests will get to marvel over the Ytri Tunga seal-watching beach; Rauðsfeldja gorge; the Lóndrangar sea-stacks; Snӕfellsjökull National Park; and Mount Kirkjufell, to say nothing of the many fishing villages, swimming pools and cultural sites along the way.

   

  Gerðuberg,

   

  Arnarstapi is a village in the southern part of the Snaefellsnes peninsula. The area has several old and charming houses with interesting stories to them and is furthermore renowned for its beautiful nature. 

  The beach holds a particular attraction. It has an eroded circular stone arch, called Gatklettur, and three rifts, Hundagja,Midgja and Musagja. The interplay of spectacular waves and the light of the sun creates a fascinating spectacle. Large colonies of the arctic tern also nest in the area.

  An old horse trail through the lava field Hellnahraun is highly popular for hiking, due to the impressiveness of the surrounding landscape.

  阿尔纳斯塔皮,

  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,

  

  Gljúfrabúi (or Canyon Dweller) is a beautiful waterfall located at Hamragarðar in South Iceland, close to its better known counterpart, Seljalandsfoss waterfall. It is one of the hidden gems of the South Coast, and thus a great spot for photographers and those seeking to admire nature in peace.

  ---

  Image from Regína Hrönn Ragnarsdóttir

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  Nature of Gljúfrabúi

  The 40 metre (131 feet) high Gljúfrabúi is hidden behind a huge cliff which faces out towards Iceland’s South Coast and the Atlantic Ocean. Because of its decent ‘hiding place’, it is overlooked by most travellers, in spite of the fact that thousands of people visit Seljalandsfoss, less than a kilometre away, every day.

  A stream, the Gljúfurá, runs through a cleft in the cliff, and those who wish to approach the falls must do so by wading through these waters.

  After a few metres of travelling through a narrow valley, the space will open, and here, Gljúfrabúi tumbles before a great boulder, which it is possible to climb upon for some great photos. With the open sky above, mossy walls, silver mist and black lava, it is one of Iceland’s most breathtaking gems, seemingly from a fantasy story.

  This is especially the case on sunny days, where rainbows curve through the water’s spray.

  It is also possible to see Gljúfrabúi from above. There is a steep path that allows you to clamber up the cliff, at some points with the aid of ropes.

  Both these routes are mildly challenging and have their dangers, so only attempt to reach Gljúfrabúi if you are in a decent state of health and confident on your feet. They should only be attempted when there is not ice on the ground, and in the case of the path up the cliff, when it is wet and slippery.

  Surroundings of Gljúfrabúi

  

  Gljúfrabúi is in one of the most travelled regions of Iceland, on the South Coast along the Ring Road. This means that it is very easy to reach, either alone or on a guided tour, just an hour and a half’s drive from the capital.

  As mentioned, Gljúfrabúi is about ten minutes walk north Seljalandsfoss. Interestingly, this is one of the country’s most famous and photographed waterfalls, due to the fact it falls from a concave cliff which allows visitors to fully encircle the cascade.

  Seljalandsfoss is taller than Gljúfrabúi at 60 metres (196 metres), with a similar waterflow. Both are fed by the meltwater of the glacier Eyjafjallajökull, the volcano beneath which caused widespread problems to air traffic across Europe when it erupted in 2010.

  A much more powerful waterfall can be found just half hour’s drive or so along the Ring Road, called Skógafoss. This is a similar height to Seljalandsfoss, but up to 30 metres (98 feet) wide after a heavy rain.

  Another popular site in the area is Sólheimajökull, the most popular glacial outlet in Iceland for glacier hiking. This feature is on Sólheimasandur, a vast expanse of volcanic ash that resembles a black sand desert.

  Those who travelling a little further along the South Coast will reach the cliffs of Dyrhólaey, with their beautiful rock arch and resident puffins in summer, and the beach of Reynisfjara, renowned for it powerful waves and basalt sea-stacks, called Reynisdrangar.

  All these sites can be visited with ease within a day.

   

  Gljufrabui,

   

  

  Reykjavík Airport refers to the predominantly domestic airport within Iceland’s capital, often shortened to RVK or BIRK.

  While Keflavík International Airport deals with flights abroad, planes from Reykjavík Domestic Airport only fly to select towns around Iceland, as well as to the Faroe Islands and Greenland. It will, however, serve as a landing place for international flights if conditions are problematic at Keflavík.

  History of Reykjavík Airport

  Flights had been going in and out of Reykjavík to an extent before 1940, but this was the year when construction began at the airport.

  It was built by the British Troops who invaded the country after Denmark (the colonial ruler of Iceland at the time) was invaded by the Nazis. Initially, it was called RAF Reykjavík but received its current name when it was handed back to Icelanders in 1946.

  In 2000, the airport underwent two years of renovation. During this time, there was a successful referendum in which the people spoke in favour of moving the airport out of the city centre, but due to complications in voting and the fact that the vote was not binding, these plans are yet to move forward.

  The renovations were finished in 2002, and the airport has not changed much since, other than becoming much busier with the dramatic increase of tourism.

  Reykjavík Airport Today

  

  Today, Reykjavík Airport has four airlines that operate from it. They head to the following destinations in Iceland:

  • Akureyri

  • Egilsstaðir

  • Húsavík

  • Ísafjörður

  • The Westman Islands

  • Bíldudalur

  • Gjögur

  This means that guests who are pressured for time, fearful of driving on the icy roads, or have come in the depths of winter and roads are closed, can still reach all corners of the country.

  Flights also go to Nuuk, Kulusuk and Ilulissat in Greenland, and Vágar in the Faroe Islands.

  Very occasionally, flights will go back and forth to Copenhagen.

  The airport is also regularly visited by tourists staying in Reykjavík, however, as it is the departure location for many helicopters and small plane excursions, which allow guests to have incredible aerial views of Iceland.

  Some of these tours take guests as far out as to remote parts of the Highlands, while others are short flightseeing trips around the greater Reykjavík area. These, however, are still exhilarating and rewarding; there is no better way to see Reykjavík than from above, witnessing the patchwork quilt of colourful tin roofs unfold beneath you, and landmarks such as Hallgrímskirkja church from a whole new angle.

  It also provides a great chance to see the nature around Reykjavík. In clear weather, you will be able to see the Snæfellsnes and Reykjanes Peninsulas, the flat-topped mountain Esjan, the bay of Faxaflói and the Bláfjöll Mountain Range.

  The airport is located about two kilometres from Reykjavík’s city centre, putting it within easy walking, bus or taxi distance from all downtown hotels. It is right beside the forested hill Öskuhlíð, home to the popular restaurant, viewing point and exhibition centre, Perlan.

   

  Reykjavík Airport,

  

  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,

  Kirkjufell (“Church Mountain”) is a distinctly shaped mountain found on the north coast of Iceland’s Snæfellsnes Peninsula, only a short distance away from the town of Grundarfjörður.

  Kirkjufell takes it’s name from its resemblance to a church steeple, sharpened at the top with long curved sides. From other angles, the mountain can resemble a witch’s hat or even a freshly scooped ice cream.

  Photography at Kirkjufell

  Peaking at 463 m, Kirkjufell holds the honour of being Iceland’s most photographed mountain. Throughout the centuries, Kirkjufell’s striking slopes have acted as a visual landmark for seafarers and travellers.

  Walking distance from Kirkjufell, one can find the photogenic waterfall Kirkjufellsfoss (“Church Mountain Falls”), an excellent subject for photographers who can easily frame the mountain in the background. Despite its relatively diminutive height, Kirkjufellsfoss’ three-pronged falls make the waterfall particularly stunning, even for Iceland.

  At the base of the mountain, visitors will also be able to find a lake; on calm and clear days, this lake reflects a perfect mirror image of Kirkjufell, only adding to the fantastic photo opportunities around this area. On top of that, the colours of Kirkjufell change with the passing seasons; the summer see it a lush green, full of life, whilst the winter months scar the mountain’s face with a mask of barren brown and white.

  Fans of the HBO series Game of Thrones will recognise Kirkjufell as a shooting location from Season 7 of Game of Thrones. The mountain is showcased from the scenes ‘beyond the wall’ when Jon Snow, The Hound and Jorah Mormont, among others, brave the wilderness in hopes of catching an undead wight. Having seen it in a vision, The Hound acknowledges Kirkjufell as “[...] the mountain like an arrowhead.” Even the Games of Thrones producers can’t resist capturing the mountain on celluloid!

  Hiking Kirkjufell

  There is a fairly steep trail to the top of Kirkjufell, from where there are magnificent panoramas of the surrounding fields, coastlines and rivers. The mountain takes roughly an hour and a half to ascend, and one and a half hours back to the bottom.

  Alongside this mountain-track is a steeper route to the peak which involves two points where one needs to rope-climb. This route should never be attempted in the winter, and never without a certified guide. Given the steep elevation, it is highly recommended that you bring a sturdy pair of hiking boots, snacks and water to the trail.

  Getting to Kirkjufell

  Kirkjufell is extremely close to Grundarfjörður, a small town on the Snæfellsnes Peninsula, approximately two hours drive from Iceland's capital city, Reykjavik. From Grundarfjörður, one travels ten minutes west down Route Snaefellsnesvegur 54 to the base of Kirkjufell. Visitors have plenty of parking space to choose from, all free of charge.

  教会山(草帽山),

  

  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,

  

  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,

   

  Photo by Regína Hrönn Ragnarsdóttir.

  Eldborg is a 60 m (197 ft) high volcanic crater, located north of Borgarnes in West Iceland.

  Eldborg is the largest crater on a 200 m (650 ft) long volcanic rift. It last erupted between 5000 and 6000 years ago, but according to medieval manuscripts, it also erupted during the time of Iceland's settlement, 1000 years ago. 

  The easiest way to approach Eldborg is from its southern side, by walking 2.5 km (1.5. mi) from Snorrastaðir, across the lava field.

  Eldborg,

  Photo from Into the Underworld | Vatnshellir Caving Tour

  Vatnshellir Cave is a lava tube on the Snæfellsnes Peninsula and a popular site for caving tours.

  Geology of Vatnshellir Cave

  Vatnshellir is one of Iceland’s older lava tubes that can be explored, having been formed in an eruption 8,000 years ago. To compare, Iceland’s other most popular lava tunnels for caving, Viðgelmir and Leiðarendi, are only one and two thousand years old respectively.

  Like all lava tubes in Iceland, Vatnshellir was created when during an eruption, a river of molten rock began to cool from outside in. The effect left a crust over still-flowing lava, which, after flushing away, left a hollow tube.

  The minerals of this lava can still be seen in Vatnshellir today. The rocks are vividly coloured, with reds representing deposits of iron, yellows representing sulphur, and greens representing copper.

  Vatnshellir is 200 metres (656 feet) long, with a deepest point of 35 metres (114 feet).

  Lava Caving in Vatnshellir

  Lava caving is possible in Vatnshellir throughout the summer months with a guided tour. Taking such a tour is essential, as guides know the caves in and out, and will bring all the equipment you need. Alone, they are notoriously easy to get lost and hurt in.

  Vatnshellir is easier to enter than its cousin Leiðarendi, as it has a staircase descending into it. Unlike Viðgelmir, however, the ground is not paved and the walls are not lit, so you need a reasonable level of fitness and confidence on your feet to traverse it comfortably. Even so, children as young as five can join the fun.

  When travelling the cave, you will learn about Iceland’s geology and folklore, as trolls were said to make the caves their homes in many tales. You will also get to experience total darkness by shutting off your lights at the deepest point.

  Location of Vatnshellir cave

  Vatnshellir is a protected site, as it is within the Snæfellsjökull National Park. This park sits right on the tip of the Snӕfellsnes Peninsula, meaning you can include many nearby sites in a visit to it.

  These include the basalt sea stacks of Lóndrangar, the fishing villages of Arnarstapi and Hellnar, and the pyramid-shaped peak Kirkjufell.

   

  Vatnshellir火山洞穴,

  

  The Lóndrangar basalt cliffs are amongst the many geological wonders of the Snæfellnes peninsula.

  Geology of Lóndrangar

  Once a volcanic crater, all that remains after aeons of ocean battering are two great pillars upon a cliff, one 75 metres (246 ft) high and the other 61 metres (200 ft).

  Their dramatic scale earning this incredible formation the nickname ‘the rocky castle’.

  The cliffs can be accessed easily from the Visitor’s Centre, through fields of mossy lava, but they can also be seen from the sea. Surfing is relatively popular in the area and doing so in the shadows of these great peaks only adds to the experience.

  Folklore at Lóndrangar

  The surrounding lands are steeped in folklore; farmers have never made use of the fields around the Lóndrangar basalt cliffs due to the elves that are rumoured to live there.

  Nearby, at Þúfubjarg, another cliff on the Snӕfellsnes Peninsula, it was said that the poet Kolbeinn Jöklaskáld met the devil and struck a deal with him.

  Lóndrangar,

  

  Djúpalónssandur is an arched-shaped bay of dark cliffs and black sand, located on the Snæfellsnes Peninsula in western Iceland.

  History & Monuments

  The location was once home to a prosperous fishing village, along with other abandoned hamlets and ports of the area such as Búðir and Hellnar, from back when the Snæfellsnes Peninsula functioned as one of the most active trading posts of the island.

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  • See a selection of exciting Snæfellsnes Tours

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  Fascinating remnants of this period are for instance found in the form of four ancient lifting stones that still occupy the beach. The stones range in weight from 23 kg (50 lbs) to 155 kg (342 lbs) and were used to test the strength of fishermen. Their names are Amlóði (useless), Hálfdrættingur (weakling), Hálfsterkur (half-strong) and Fullsterkur (full-strong).

  In 1948, the English trawler Epine GY 7 from Grimsby shipwrecked on the shore, with fourteen dead and five survivors. The rusty iron remains of the vessel remain scattered on the beach, now protected as a monument to those who perished.

  Environment & Surroundings

  The Snæfellsnes Peninsula boasts countless natural wonders, where locals and travellers both flock on a daily basis to enjoy the unique landscape and stunning coastlines. Djúpalónssandur’s black pebble beach is particularly stunning amidst rocky coastal lava formations, including the elusive Gatklettur, a large lava rock with a hole in the middle through which you can directly spot the Snæfellsjökull Glacier Volcano.

  Behind the rock are two freshwater lagoons called Djúpulón and Svörtulón, with the former serving as the namesake of the bay. Believed in olden times to be bottomless, the water bodies were later revealed to reach the depth of five metres. Lagoons such as these are held in high regard amongst the Icelandic people, and Svörtulón is thought to possess healing properties, especially after having been blessed by Bishop Guðmundur góði ('the good') in the late 1100s.

  A natural monument of the area is Söngklettur, or “singing rock”, a large lava rock with a reddish hue that resembles an elfish church. Other rock formations of folklorish appeal rest close by, including the alleged trolls-turned-to-stone Kerling and Lóndrangur.

  Warning

  When visiting Djúpalónssandur, take heed that these are treacherous waters and the Atlantic Ocean’s powerful suction can easily carry you out to sea. This beach is not one for wading, but enjoying from a safe distance, especially if the weather is stormy.

  The glistening pebbles that make up the beach known as Djúpalónsperlur, or “pearls of the deep lagoon”, are gorgeous to look at and might seem appealing to stone collectors, but they are protected by law and should not be removed from the area by visitors.

  Djúpalónssandur黑沙滩,

  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

• 首都雷克雅未克6晚住宿 (多种级别可选，超级经济、经济级别不含早餐，舒适级别、品质级别含早餐，具体请阅读住宿信息部分)

• 冰岛国际机场往返首都雷克雅未克市中心住宿的机场大巴

• 蓝湖温泉舒适门票(可在预定时选择升级至高级)＋往返巴士交通

• 南岸2日小巴游＋冰川徒步

• 冰岛南岸1晚住宿 (含早餐，私人卫浴根据酒店情况而定)

• 格陵兰Kulusuk一日游（含雷克雅未克往返Kulusuk机票）

• 黄金圈小巴一日游 (可在预定过程中选择升级增加特色项目)

• 斯奈山半岛小巴一日游

• 详细、实用又有趣的行程单，覆盖了行程中涉及到的冰岛自然、历史和文化

• 冰岛旅行网专业客服确认行程

• 税

• 除雷克雅未克往返格陵兰Kulusuk的的机票外，不含其它机票

• 午餐

• 晚餐

• 登山鞋

• 温暖、防风、防水衣物

• 泳衣、浴巾

• 相机

下面我们列出了这个行程套餐中的可选住宿级别。在每日行程中，您可以看到每一天具体的首选酒店。 您在预订过程中可以选择不同的住宿标准。超级经济级别住宿将安排青旅床位。经济级别和舒适级别的住宿为单人预订安排单人间住宿，多人预订将安排双人间或三人间的组合。如果您多人同时出行但是希望安排单人间，请分开预订，或联系客服进行单间差升级。品质住宿会为单数人数预订提供一个单人间，余下提供双人间。 青少年、儿童与家长共享房间时，可享受产品的青少年、儿童价格。如果因为人数超额需要额外安排房间，需按成人价格计算。 注：行程中的多日游提供首都外的乡间住宿，此类住宿无法选择级别，这里列出的级别只针对行程中首都地区的住宿。 我们会从Guide to Iceland优选的住宿中为您安排您预订时可选的最佳选择。冰岛酒店质量水平差异较大，且严重的供不应求，您定的越早，效果越为理想。 注：特别安排将会有额外的房型或服务费用。选择日期即可查询位置并预订。

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