サマーバケーション3泊4日｜ゴールデンサークルと南海岸

• ツアー時期: 4月. - 8月.
• 所要時間: 4 日間
• アクティビティ: 氷河ハイキング, シュノーケリング, ハイキング, スノーモービル, 乗馬, 観光, 温泉, カルチャー, 野鳥観察
• 難易度: ☆
• 最低年齢: 2 歳
• ツアーガイド言語: English
• ハイライト:

  

  The Blue Lagoon is a geothermal spa found on the Reykjanes Peninsula in southwest Iceland. The Blue Lagoon is the single most popular visitor attraction in Iceland, drawing people in from across the world. It is located approximately fifteen minutes drive from Keflavík International Airport, or a thirty minutes drive from Reykjavík, the country’s capital.

  History

  People first began bathing in the waters beside Svartsengi power plant in 1981, quickly realising that it had amazing healing qualities for the skin (the original lagoon was a result of a project of the power plant in 1976).

  People, such as those suffering from psoriasis, found the waters immediately soothing for their condition. News quickly spread of this miraculous lagoon, and by 1987, the first swimming facilities were officially opened.

  Today

  The reasons as to why the Blue Lagoon is considered to be such a regenerative spot is because the water is rich in silica and sulphur. This is greatly complemented by the fact that the Blue Lagoon also operates a Research and Development facility, finding cures and remedies for skin ailments using the mineral-rich water.

  The temperature in the bathing and swimming area is very comfortable, and averages 37–39° C (98–102° F). The Blue Lagoon also boasts the LAVA Restaurant, the Blue Café and the Lagoon Spa, from where you can buy a range of cocktails, health products, delicious meals and book an in-water massage. Saunas, steam rooms and a small waterfall are also on the premises.

  For all of these reasons and more, the Blue Lagoon is considered to be one of the most enjoyable and romantic spots in the country. It is surrounded by a plethora of fantastic volcanic landscapes and sports a stunning aquamarine colour in the water, as well as rising pillars of steam that only add to the spa’s fantastic ambience. Guests can also enjoy silica face masks and massages. Most visitors to the Blue Lagoon will arrive there either on their first or last day in the country due to its proximity to the airport.

  • See Blue Lagoon Tours Here. 
  ブルーラグーン,

  

  The Golden Circle is a 300 kilometre (186 mile) route to the three most popular natural attractions in Iceland: the Geysir Geothermal Area, Gullfoss Waterfall and Þingvellir National Park.

  This sightseeing trail is easy to do within half a day from Reykjavík, either by self drive or on one of many tours. Some of these tours have additional activities, such as snorkelling or snowmobiling, or are conducted in a unique style, such as by helicopter, or under the midnight sun.

  Within the three locations of the Golden Circle are some of the clearest examples of Iceland’s fascinating geological forces, magnificent landscapes, and rich culture.

  The Geysir Geothermal Area

  

  The Geysir Geothermal Area is a hot-spring haven in Haukadalur Valley. As could be guessed, it is home to a famous geyser, the name of which has named all others: Geysir itself.

  Though this feature is currently in a phase of inactivity, its neighbour Strokkur more than makes up for it. Every five to ten minutes, it blasts a column of boiling water to heights that can reach over 40 metres (131 feet).

  The surrounding area is dotted with fumaroles, hot springs, and mud-pits. There are also two more smaller geysers, Smiður and Litlí-Strokkur, that can be easily visited. There is also a hotel, restaurant, cafe and gift shop across the road.

  Gullfoss waterfall

  The 'Golden Waterfall', Gullfoss one of the most beautiful and powerful waterfalls in Iceland, plummeting 32 metres (105 feet) in two tiers into the river gorge of the popular rafting river Hvíta. It is just a ten minute drive from Geysir, and is the furthest point on the Golden Circle from Reykjavík.

  Gullfoss was very almost lost in the early 20th Century, when British developers sought to harness its incredible power for geothermal energy. Though they got the lease to the land, allowing them to go ahead with their plans, they met an unlikely adversary: the daughter of the farmer who owned it, Sigríður Tómasdóttir.

  This resilient woman refused to see the waterfall, which she and her sisters paved the first path to, destroyed. She, therefore, walked over 200 kilometres (124 miles) to Reykjavík and back multiple times to meet with a lawyer in order to help change the decision.

  Though the process was arduous and took years, eventually Sigríður managed to exhaust the resources of the businessmen and they withdrew their plans. Because of her, all Icelandic waterfalls are now protected from foreign investors, and she is considered one of Iceland’s first environmentalists and most important historical people.

  Þingvellir national park

  

  The largest attraction of the Golden Circle is Þingvellir National Park. The Icelandic parliament was founded here in 930 and remained until the year 1798 before moving to Reykjavík, making it the original site of what is now the world’s longest ongoing parliament.

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

  Þingvellir is surrounded by a beautiful mountain and volcanic ranges, as is the site of a rift valley directly between the North American and Eurasian tectonic plates. This makes it one of the few places in the world where you can walk between the continents, in the Mid-Atlantic rift.

  The daring and qualified even have opportunities to snorkel or scuba dive in this no-man’s-land, in a ravine filled with crystal-clear spring water called Silfra. The visibility here can exceed 100 metres (328 feet), revealing incredible geological sites. Though it never freezes over due to the constant flow of water into it, it is 2°C (35°C) throughout the year, thus underwater explorers are always equipped with protective suits.

  Other sites of note are the magnificent Almannagjá gorge, which you can walk down into to reach the rift valley from the North American tectonic plate, and the beautiful lake Þingvallavatn, the largest lake in Iceland, which gleams to the south of the National Park.

  Surrounding sites

  Due to its convenient location in south-west Iceland, it is easy to visit the Golden Circle alongside with many other sites. Those seeking relaxation could head to the Secret Lagoon in Flúðir or Fontana Spa in Laugarvatn, those seeking adventure could book a trip to the ice tunnels of Langjökull glacier, and those seeking culture could visit the Sólheimar ecovillage.

  There are many tours that include such bonuses, but if driving yourself, you should check out this guide to great detours off the Golden Circle.

  ゴールデンサークル,

  

  Reykjavík is the capital of Iceland and the northernmost capital of any sovereign state in the world.

  Despite a small population (approximately 120,000, with just over 200,000 in the Greater Reykjavík area), it is a vibrant city that draws an ever increasing number of visitors every year. It is the financial, cultural and political centre of Iceland, and has a reputation of being one of the cleanest and safest cities in the world.

  Geography

  The city of Reykjavík is located in southwest Iceland by a creek of the same name. Throughout the ages, the landscape has been shaped by glaciers, earthquakes and volcanic eruptions and the area is geothermal; after all, its name translates to ‘Smoky Bay’.

  Much of the current city area was subglacial during the Ice Age, with the glacier reaching as far as the Álftanes 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 Reykjavík is set with peninsulas, coves, straits and islands, most notably the island of Viðey, and seabirds and whales frequent the shores. The mountain ring as seen from the shore is particularly beautiful.

  Mount Esjan is the highest mountain in the vicinity of Reykjavík and the most distinctive feature of the coastline. This majestic summit is also highly popular amongst hikers and climbers. Other notable mountains that can be seen from the seaside are Akrafjall and Skarðsheiði.

  On clear days, one may even see as far to the legendary Snæfellsjökull glacier, at the end of the Snæfellsnes peninsula.

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

  Transportation

  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 centre and Sundahöfn in the east.

  The domestic Reykjavík Airport is located at Vatnsmyrin, not far from the city centre and close to the hill Öskjuhlíð and the restaurant, vantage point and exhibition centre Perlan. The international Keflavík Airport at Miðnesheiði heath then lies around 50km (31 miles) from the city.

  Cars, jeeps and bicycles can be readily rented in the city and many organized tours are also being offered. It is, however, quite easy to walk between the major sites.

  What to See & Do in Reykjavik

  The local arts scene is strong in Iceland, with annual events and festivals, many of artists from which have hit the international stage.

  Major events taking place in Reykjavík include Iceland Airwaves, Reykjavík Pride, RIFF (The Reykjavík International Film Festival), The Reykjavík Literature Festival, Culture Night, the Reykjavík Arts Festival, Food & Fun, the Reykjavík Fashion Festival and the Sónar music festival.

  Amongst the famous people from Reykjavík are musicians like Björk Guðmundsdóttir and Sigur Rós, and writers Halldór Laxness (born on the main street, Laugavegur) and Arnaldur Indriðason.

  Those eager to soak up the local culture should visit the city’s many museums, exhibitions and galleries, and where to check out live music. You could look at the programmes of what’s on at the the Harpa music hall or the theatres, or else plan a few hours at the lighthouse at Grótta, the shopping street of Laugavegur, or the old harbour and the flea market.

  You could even book a bird- and whale watching tour or a visit to Viðey island. Be sure to check out our list of the top ten list of things to do.

  

  Make sure to visit the public square of Austurvöllur, one of the city’s most popular gathering places, where you’ll also find the national parliament, the Alþingi, as well as the state church, a statue of independence hero Jón Sigurðsson, cafés, bars and restaurants.

  Austurvöllur was central in the 2008 protests, along with Lækjargata, home to the House of Government. You are also not likely to miss the great church of Hallgrímskirkja that towers over the city from the hill of Skólavörðuholt, from which you’ll get a great view of the city.

  Try a walk by the city pond, Tjörnin, to greet the many birds that frequent the area and to visit the city hall, stationed by its banks. A beautiful park lies by the pond, 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 Vatnsmyrin wetland, a particularly pleasant place, but be mindful to not disturb the wildlife there by keeping to the pathways.

  For a nice swim on a warm day, we particularly recommend Nauthólsvík beach, which is heated with geothermal water. Those who who love a dip should also visit the Laugardalur valley, home to one of the city’s best swimming pools, which sits beside Ásmundarsafn gallery, a beautiful botanical garden and a domestic zoo.

  A walk by the Ægissíða beach, with its old fishing sheds, in the west part of Reykjavík also holds a particular charm.

  Another place that offers one of the city’s best (and free) views is Perlan, up on Öskjuhlíð hill. The hill itself is a popular place to spend a few hours, with over 176,000 trees and great opportunities for walking and cycling. Perlan also has a rotating restaurant with great views and an exhibition centre.

  Travel to Álftanes to see the president’s house at Bessastaðir, which is also a historical site in its own right, having been the educational centre of Iceland for centuries. Nearby is a beautiful lava field, Galgahraun, well worth a visit.

  Furthermore, the city is 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 Heiðmörk preservation area, a favourite local site of the people of Reykjavík, as well as the Blue Mountains, one of Iceland’s best skiing venues.

  Finally, we’d like to stress that these are only some suggestions of the many things you might check out in Reykjavík. 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. For more information, check out the Best of Reykjavík.

  レイキャビク,

  

  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 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 of 248 metres (814 feet). With a surface area of 18 square kilometres (7 square miles), 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. In 1975, it had less than half its current surface area.

  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.

   

   

  ヨークルサロン氷河湖,

  

  Vatnajökull glacier is the largest ice cap in Iceland and the third largest glacier in Europe, covering 8% of the island's landmass. Vatnajökull National park can be found in the south west of Iceland and is a popular spot for activities like glacier hiking from Skaftafell, boat tours and ice caving tours from Jökulsárlón glacier lagoon, both of which are part of Vatnajökull national park. 

  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 a stratovolcano known as Öræfajökull. 

  Underneath the glacier rests some of the most active volcanoes in the country, the most notable being Grímsvötn, Öræfajökull and Bárðabunga. Volcanic activity in the region has occurred on and off throughout the centuries, and many geologists believe that such a period is overdue for immediate future. If their calculations are correct, it would mean 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 of the valley. The major outlet glaciers of Vatnajökull include Dyngjujökull in the north, Breiðamerkurjökull and Skeiðarárjökull to the south. To the west, one can find the outlet glaciers Síðujökull, Skaftárjökull and Tungnaárjökull. 

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

  • Click here for a selection of Ice Cave tours 

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

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

  Vatnajökull National Park 

  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. Vatnajökull National Park has 14% coverage over the whole island of Iceland.

   

  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, one can find wetlands and ranges, 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) 
  ヴァトナヨークル氷河,

  

  Skógafoss is one of Iceland’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, at least one 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. This will get you drenched, although on a summer’s day, can be quite tempting.

  Skógafoss can also be viewed from the top as a steep staircase leads to an observational platform above the cascade. Many nesting seabirds can be found on the route up.

  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.

  Skógafoss is often visited alongside the waterfall Seljalandsfoss, which is just a little further along the South Coast. Both fall from cliffs of the same height, and while Skógafoss is much more powerful, Seljalandsfoss has a cave behind it, which means it can be fully encircled. It is also next to a much lesser known but still awe-inspiring waterfall, Gljúfrabúi.

  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, who by some accounts was a giant. 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.
  

  スコゥガフォスの滝,

  

  Seljalandsfoss is a waterfall that can be fully encircled, situated on the South Coast of Iceland with a drop of 60 metres (200 feet).

  Due to the waterfall’s close proximity to the Ring Road and impressive natural features, it is one the country's most famous and visited falls. Majestic and picturesque, it is one of the most photographed features in all of Iceland.

  Geology and Surroundings

  Seljalandsfoss waterfall, part of the river Seljalandsá, has its origins underneath the glacier Eyjafjallajökull. The volcano beneath this ice cap was the one that erupted in 2010 and caused havoc at airports across Europe.

  The cascade of the falls is relatively narrow, but falls from a tall cliff that once marked the coastline: the sea is now located across a stretch of lowlands, and is visible from the site.

  

  The most distinguishing feature of Seljalandsfoss is a natural pathway that stretches all the way around it. The cliffs behind the falls has a wide cavern, and rocks and paths allow guests to fully encircle it in summer.

  Though a mesmerising opportunity, visitors should be prepared to get dampened due to the perpetual mist of the falls, which also tends to make the rocks of the pathway slippery. 

  Floodlights have been set up on both sides of the waterfall, which impressively illuminate the scene during the night when the midnight sun is not out. The lights were installed in 2001 due to the growing popularity of the falls as a tourist destination.

  After visiting Seljalandsfoss, it is common for visitors to continue north to the waterfall Gljúfrabúi, which is found partially hidden behind a rock face. Because of Seljalandsfoss extreme popularity, Gljúfrabúi is widely considered an additional hidden gem of the scene, as it is too often overlooked.

  Seljalandsfoss is also usually visited alongside the nearby Skógafoss. The waterfall falls from the same height, and while it cannot be encircled, it is much more powerful, and steeped in the legend of a giant’s hidden treasure.

  Visitor Centre Controversy

  In 2017, it was announced that a visitor’s centre was to be constructed near the falls. The design of the building indicated that it would be 7 metres (23 feet) high and 2,000 square metres (21,500 square feet) in size. Landowners in the area opposed to the idea, proclaiming that the centre would greatly alter the natural appearance of the waterfall’s renowned scenery.

  The project has neither been fully approved nor wholly cancelled, with ideas surfacing of either significantly reducing the size of the construction, or moving the visitor centre’s location further away, for instance to the nearby farmstead Brekkuhorn.

  Seljalandsfoss in Popular Culture

  Along with a multitude of South Iceland’s most famous natural attractions, Seljalandsfoss can be seen in Justin Bieber’s music video for his song ‘I’ll Show You’. Please enjoy the video without emulating any antics that will endanger yourself or the environment.

  The waterfall was also a featured waypoint during the first leg of the sixth season of The Amazing Race, an American reality TV series.
  セリャランズフォスの滝,

  

  Geysir is a famous hot spring in the geothermal area of Haukadalur Valley, found in South Iceland.

  Making up just one of the attractions along the world-renowned Golden Circle sightseeing route, alongside Þingvellir National Park and the mighty Gullfoss waterfall, Geysir is most well-known for having lent its name to geysers all around the world.

  Geography 

  Though Geysir itself is rarely active these days, Haukadalur Valley boasts a plethora of hot springs and geysers, including the powerful Strokkur, Smiður and Litli-Strokkur.

  Strokkur is, arguably, the country’s most famous hot spring, shooting vast jets of boiling water from 20m (65ft) up to 40m (130ft) high. Don’t worry about missing this incredible spectacle of nature, as Strokkur erupts every five to ten minutes; just make sure to have your camera ready.

  

  Geysir is much larger, but years can go by between eruptions here; it is currently in an inactive phase. When it does erupt, the water can shoot up in the air as high as 70 metres (230 ft).

  Just five minutes walk north of Geysir are a wealth of fumaroles emanating steam and gas into the cool Icelandic air. Aside from watching the hypnotic pillars of steam, you will also be able to observe the yellow sulphuric stains along the fumaroles themselves, a result of the earth’s minerals crystallising around the rock bed.

  At the southern part of the valley, Þykkuhverir, you’ll find various bubbling mud pots. These spooky brown cauldrons are actually fumaroles that boil up through the loose ground; after a dry spell, these mud pools are likely to transform into a hardened fumarole.

  Nearby Attractions 

  About 2km (1 mile) from Geysir is a preserved natural pool called Kúalaug. It has room for three to five people at a time, but care should be taken, as the area around the pool is very delicate. The temperature is 39-43°C (102-109°F), depending on where 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 when relaxing here.

  Haukadalur has also seen a rise in reforestation in recent times thanks to continued experiments and research in the area. Today, Haukadalsskógur is one of the largest forests in South Iceland, boasting accessible walking paths (also for wheelchair users), fascinating vegetation and The Tree Museum, built in the memory of forester Gunnar Freysteinsson.

  History 

  Haukadalur has been inhabited and used as a church site since the Age of Settlement. Given its historic value, it should be noted that scholar, Ari “The Wise“ Þórgilsson, grew up here; it was also where the first pastoral school in Iceland was built.

  The current wooden church was last rebuilt in 1938 but its architectural style dates back to 1842, making it well worth a visit to see how Iceland looked before industrialisation.

  For accommodation, Hotel Gullfoss is approximately 7 km from the Geysir area, and closer still is Hotel Geysir on the other side of the road from the attraction, where you will also find a restaurant, café and a souvenir shop.

  ゲイシールの間欠泉,

  

  Gullfoss (translated to ‘Golden Falls’) is one of Iceland’s most iconic and beloved waterfalls, found in the Hvítá river canyon in south Iceland.

  The water in Hvítá river travels from the glacier Langjökull, before cascading 32m (105ft) down Gullfoss’ two stages in a dramatic display of nature’s raw power. This incredible site is seen by most visitors, as it is on the Golden Circle sightseeing route.

  Because of the waterfall’s two stages, Gullfoss should actually be thought of as two separate features. The first, shorter cascade is 11m (36ft), whilst the second drop is 21m (69ft). The canyon walls on both sides of the waterfall reach heights of up to 70m (230ft), descending into the great Gullfossgjúfur canyon. Geologists believe that this canyon was formed by glacial outbursts at the beginning of the last age.

  In the summer, approximately 140 cubic metres (459 cubic feet) of water surges down the waterfall every second, whilst in winter that number drops to around 109 cubic metres (358 cubic feet). With such energy, visitors should not be surprised to find themselves drenched by the waterfall’s mighty spray.

  As mentioned, Gullfoss makes up a part of the highly popular Golden Circle sightseeing route, alongside Geysir geothermal area and Þingvellir National Park. Many Golden Circle tours include additional activities that can be taken from Gullfoss, such as ascending the mighty nearby glacier Langjökull and entering its ice tunnels, or snowmobiling along its gleaming surface.

  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, Howell, 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 Howell the land without the knowledge of a loophole that would allow him to proceed with his plans.

  It was Tómas’ daughter, Sigríður Tómasdóttir, who would lead the charge to stop Howell’s ambitions. Having grown up on her father’s sheep farm where she helped pave the first road to Gullfoss, she sought to get the 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, a distance of over 100 kilometres (62 miles). Circumstances became so difficult that Sigríður threatened to throw herself into the waterfall if any construction began.

  Her tenacity, however, resulted in success. In 1929, Howell’s withdrew from the lease, unable to keep up with the costs and difficulties of his plan. 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. As such, she is one of the most famous figures in Iceland’s history. Her contribution is forever marked in stone; a plaque detailing her plight sits at the top of Gullfoss.

  Interestingly, the lawyer who assisted Sigríður, Sveinn Björnsson, went on to go down in history too; he become the first president of Iceland in 1944.

  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.

  グトルフォスの滝,

   

  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.

  エイヤフィヤットラヨークル火山,

  

  Þingvellir National Park is the only UNESCO World Heritage site on the Icelandic mainland and one of the three stops on the world famous Golden Circle sightseeing tour, alongside the Haukadalur Geothermal Valley (Geysir) and Gullfoss Waterfall. Just to the south of the park is Þingvallavatn, Iceland’s largest natural lake.

  Geography 

  The first thing that visitors to the National Park notice is its sheer aesthetic beauty; dried magma fields, covered in Icelandic moss, sit carved by glacial springs and surrounded by a bowl of ancient mountain peaks.

  Two of the greatest attractions in the park are the exposed North American and Eurasian tectonic plates; it is one of the only regions in the world where you can see geology such as this on land.

  Visitors are encouraged to walk along the North American tectonic plate, where they can read more about the area’s fascinating formation and history, before descending into the valley below.

  History 

  

  Þingvellir can be anglicised to ‘Fields of Parliament’, a nod to the area’s fascinating history and relevance to Icelandic culture. It is here, after all, that the world’s first democratically elected parliament that remains functioning, the Althing, was formed in 930 AD.

  It may seem unlikely that Vikings would want to be under such an uncombative government, but the thirty or so clans that lived in Iceland at the time sought to prosper in their harsh new environment.

  The first gathering was such a success that the meetings became annual, and it became a place where disputes were settled, criminals were tried, and laws to the benefit of all were laid down.

  This saw the birth of the Icelandic Commonwealth, a time of independence and freedom for the Icelandic people before they became constituents of the Norwegian monarchy. Sessions would continue to be held at Þingvellir until 1798.

  Though the parliament was removed by the Danish at this time, it returned 1845 to Reykjavík.

  Another major reason as to why Þingvellir is considered so important to Icelanders is the fact that this is where the decision was made to abandon the belief of Paganism and the Norse Gods; the people adopted Christianity in 1000 AD under threat of invasion from Norway.

  This turning point in history was left to the pagan lawspeaker, Þorgeir Þorkelsson, who rested on the choice for one day and one night before reappearing to share his decision.

  To symbolise the country’s change, he threw idols of his old deities into the northern waterfall Goðafoss, the name of which translates to ‘Waterfall of the Gods’.

  Silfra Fissure 

  Þingvellir is one of the most widely visited attractions in Iceland, in large part due to the fact that it is home to the glacial spring, Silfra fissure, one of the top ten sites in the world for snorkellers and scuba divers.

  Silfra (meaning ‘Silver’) is a submerged ravine within the park, boasting visibility of up to 100 metres (328 feet) and a temperature just above freezing. Participants in these tours will be attired at the Silfra carpark in neoprene hoodies and gloves, as well as an undersuit and drysuit for thermal protection.
  シングヴェトリル国立公園,

  

  Reykjanes is a peninsula in Southwest Iceland, characterised by immense lava fields, volcanoes and strong geothermal activity.

  Volcanic & Geothermal Activity

  The peninsula runs along the Mid-Atlantic Ridge where the Eurasian and the North American tectonic plates are drifting apart. Because of this geological setting, the whole peninsula is extremely volcanically active, covered with lava fields and volcanoes and small earthquakes are very common there. 

  During the middle ages, many eruptions occurred in Reykjanes, but no eruptions have been recorded there for the last 500 years.

  The main geothermal areas of Reykjanes are Gunnuhver, Krýsuvik and Svartsengi. Various mud pools and fumaroles can be seen at Gunnuhver while Krýsuvik is characterised by hot springs and mud pots that bestow multicoloured hues upon the soil. The green crater lake Grænavatn is also an impressive sight.

  Svartsengi is home to a geothermal power station that produces 76.5 MW of electricity from the 475 litres of 90° C warm water that gush from the earth per second. The mineral-rich surplus water fills up the Blue Lagoon spa.

  Nature & Wildlife

  Reykjanes' cliffs are teeming with birdlife. Its best-known bird colony resides in Krýsuvikurbjarg which is the nesting place of approximately 80 thousand seabirds. North of Krýsuvíkurbjarg is Kleifarvatn, the largest lake on the peninsula and one of the deepest in Iceland and on the centre of the peninsula is lake Djúpavatn, a popular fishing destination. 

  Reykjanes is hammered by some of the most breathtaking breaker waves in the world. A short drive from Krýsuvík is Selvogur where one is able to witness some of the country's greatest waves. On Reykjanestá, the southwest tip of the peninsula, the waves are known to reach heights of 20-30 meters.

  The peninsula's north side is dotted with fishing villages and towns, most notably Keflavík, Sandgerði, Garður and Vogar. Grindavík town is located on the south shore of the peninsula. Together, the towns and towns Keflavík, Njarðvík, Hafnir and Ásbrú make up the municipality Reykjanesbær which consists of just under 16,000 residents, making it the fifth largest municipality in Iceland.

  Miðnesheiði

  Near Keflavík is the Miðnesheiði heath, where the international airport, Leifsstöð (also known as Keflavíkurflugvöllur or ‘Keflavík Airport’) is located. 

  The World-Famous Spa

  On the southern tip of the peninsula is the Blue Lagoon geothermal spa, an ideal place for relaxing and bathing.
  Reykjanes,

  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.

  ソゥルヘイマヨークトル氷河,

  Photo from Tour to Skaftafell from Reykjavik. 

  Skaftafell Nature Preserve can be found in Öræfasveit, the western region of Austur-Skaftafellssýsla in Iceland. Skaftafell once used to be a national park in its own right but was merged with the far larger Vatnajökull National Park in 2008.

  Skaftafell is notable for its rich flora, growing between sands and glaciers, and for its amazing and contrasting scenery. At Skaftafell, visitors will find a wealth of natural attractions, from cascading waterfalls to panoramic views over this picturesque region.

  Like many areas along the South Coast of Iceland, Skaftafell Nature Preserve is known for its glorious hiking trails. You can take short and easy treks to the waterfalls Svartifoss and Hundafoss, as well as to the gorgeous Skaftafell glacier. A little further along, guests will stumble on the mountain, Kristinartindar, as well as the scenic Morsardalur Valley. 

  Skaftafell is also the perfect base camp for those seeking to climb Iceland’s highest peak, Hvannadalshnúkur, or for those wishing to spend a number of days exploring the region's attractions, including Vatnajökull glacier, Jökulsárlón glacial lagoon and the nearby Diamond Beach. It is also an excellent region to try your hand at a spot of either ice climbing or glacier hiking; both activities are two of the most authentically Icelandic experiences you can partake in whilst in the country. 

  Skaftafell Visitor Center

  Skaftafell also boasts a Visitors Centre, acting as the main information and meeting point for tour operators and independent travellers. At the Skaftafell Visitor Centre, you will find answers to virtually any questions you might have about the greater Skaftafell area, including its history and geology. The Visitors Centre also contains information about nearby hiking trails, recreational options and accommodation.  

  スカフタフェットル,

  

  Silfra is a fissure filled with fresh springwater 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. 

  ---

  • See this article on Diving and Snorkelling in Iceland

  ---

  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 when they do, tear open fissures in the land between them. 

  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 like is done on this tour. 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,

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

  The glacier bursts would come via the glacier river Jokulsa a Solheimasandi which runs from the Solheimajokull outlet glacier and towards the sea.  

  The beach of Solheimasandur is astonishing. It is quite common as far as sands and pebbles go but the colour stands out, a dark greenish, sometimes reddish grey, turning pure black when it turns wet. Mixed with the crashing waves of the Atlantic Ocean it becomes an amazing sight.

  Another impressive sight is the plain wreck of a DC-3 belonging to the US Navy that ran out of fuel and crashed on the sand in 1973, and is still located at the very same spot. It is also seen in Icelandic band Sigur Ros's film Heima.

  Sólheimasandur,

  The crater Thrihnukagigur, east of the Blue Mountains in Southwest Iceland offers the unique experience of exploring the inside of a volcano.

  Go here for the tour: Inside the volcano.

  Through the crater's opening you will enter a humongeous magma chamber. Vibrant in colours and remnicent of a citadel, it is considered the most amazing natural phenomenon of its kind.

  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 kilometres (112 miles) from Iceland’s capital city, Reykjavík, and is a popular stop-off for those taking a sightseeing tour along the popular South Coast.

  Driving to the beach is particularly easy, taking an approximate two and a half hours from the capital, so can easily be done within half a day, or a full one combined with other features.

  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 trying to pull ships from the ocean to shore. However, these trolls were dim and went out too late in the night; dawn broke on the horizon, turning the trolls into solid stone.

  So mesmerising are these features that they featured in Season 7 of the HBO Series Game of Thrones; you can spot them in a few scenes shot ‘North of the Wall’.

  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.

  Surrounding Sites

  

  Reynisfjara beach is located conveniently in the middle of the South Coast, adjacent to the village of Vík. This means that those taking the Ring Road around the country, or else those heading to the Jökulsárlón glacier lagoon, will pass it, and are encouraged to make a stop.

  The closest major landmark is the Dyrhólaey rock arch and cliffs. While many seabirds are found at Reynisfjara, it is nothing compared to the numbers here. From May to August, it is one of the best places to see puffins from land.

  En route to Reynisfjara from Reykjavík, you will discover waterfalls, such as Seljalandsfoss and Skógafoss, and glaciers, such as Eyjafjallajökull and Mýrdalsjökull. Further along the South Coast, you will reach the Vatnajökull National Park, with its many glacier tongues, glacier lagoons, black sand deserts, and the incredible Skaftafell Nature Reserve.

  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.

  These are called sneaker-waves, and they can appear when least expected, even on incredibly still days. There are no significant landmasses in between Antarctica and the shores of Reynisfjara, meaning waves have thousands of kilometres to build.

  Visitors are advised to never turn their back on the waves, and keep a safe distance of at least 30 metres (98 feet).

  Aside from these sudden and dramatic shifts in tide, the rip currents offshore 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.
  レイニスフィヤラのブラックサンドビーチ,

  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.

  ラングヨークトル氷河,

  

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

  The formations are the remains of large and imposing sea cliffs, made up of basalt, that serve as a vital part of the area’s allure; they shoot dramatically out of the ocean under the looming cliffs of Mt. Reynisfjall, making for a beautiful site, and have a folklore that is equally impressive.

  More modern visitors will be excited to know that these pillars also feature in Season 7 of Game of Thrones, at Eastwatch by the Sea.

  Dangerous Waves

  

  Before getting into the wonders of Reynisdrangar, it is important for potential visitors to be aware of the dangers at the site.

  These majestic rock pillars rise from the sea just off of Reynisfjara, a famous black sand beach on the South Coast, by the village of  Vík. Though incredible due to its diverse and dramatic geology, Reynisfjara is gaining a notorious reputation for its sneaker waves.

  There are no significant landmasses between Antarctica and Reynisfjara, giving waves the entire length of the Atlantic Ocean to build strength. This means that even on still, summer days, they can rise from seemingly nowhere and chase far further up the sand than would ever be expected.

  It is absolutely imperative, therefore, that guests stay at least 30 metres (98 feet) from the water’s edge. Those who flout these rules put their lives and the lives of others at risk; people have died here before.

  Folklore

  

  As with almost all bizarre features in this country, there is an Icelandic folk tale that explains the origin of the Reynisdrangar pillars and their eerie appearance.

  According to legend, a couple of trolls saw a ship out to sea by night, and waded out to reach it. They got hold of it, and began to drag it to shore, but as so often happens in troll stories, they got their timing wrong.

  Before they were even close to getting to the shade, dawn broke. The trolls and ship were instantly frozen into stone, and they have remained immortalised since, as a warning to their kin.

  This is not the only folk tale in this area. According to local legend, two other trolls murdered a woman, whose husband hunted them down, tricked them into coming out at night, and ensured they too were turned to stone. Their remains can be found inland.

  Surroundings & Wildlife

  Most visitors will only see the Reynisfjara sea-stacks from the shore of Reynisfjara, although there is an incredibly rewarding alternative view of them from above. Those with a reasonable level of fitness can venture up the bewitching cliffs of Mt. Reynisfjall, by a road to the west of Vík.

  The mountain furthermore holds thousands of puffins every summer, from May to August. These adorable creatures have very little fear of people, and can be approached within metres (although you should never try to touch them). Other birds can be seen gliding around the cliffs such as Arctic terns, fulmars and seagulls.

  The oceans of Iceland are pregnant with life, so lucky visitors may also see seals in the water, or even one of Iceland’s twenty species of whale and dolphin.

  レイニスドランガル,

  

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

  This incredible shoreline stretches from the greater Reykjavík area in the west to the magnificent Jökulsárlón glacier lagoon in the east, and is lined with countess natural wonders such as cascading waterfalls, volcanoes, black sand beaches and glaciers.

  Geography, Nature & Wildlife

  The South Coast is the most easily accessible part of the country’s southern region, found along the Route 1 highway, which encircles Iceland. The area consists of a diverse lowland that transitions between, marshlands, bays, cultivated pastures, estuaries and black sand deserts.

  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. Freshwater birds nest in the marshlands and around the estuaries, while seabirds flock around the cliffs of Reynisdrangar and Dyrhólaey, including the North Atlantic puffin between May and August. Some species stay throughout the harsh Icelandic winter, including the northern diver, the loom and various species of gulls and ducks.  

  Seals are often found along the shore, particularly around the Jökulsárlón Glacier Lagoon and Diamond Beach. As with everywhere in Iceland, you should always keep an eye out to sea, as whales and dolphins reside all along its coastline.

  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 first major features are the two great waterfalls of Seljalandsfoss and Skógafoss, which sit beneath the notorious subglacial volcano, Eyjafjallajökull. On clear days from these beautiful cascades, the Westman Islands can be seen across the ocean.

  A little further down the route is the glacier Mýrdalsjökull, which covers one of Iceland’s most explosive volcanoes, Katla. Many glacier hikes are taken here upon the outlet of Sólheimajökull.

  The aforementioned Dýhólaey cliffs are next, home to many seabirds. Even if you come outside of puffin season, they are well worth a visit; jutting out to sea is an enormous rock arch of the same name, which you can marvel at from many angles.

  

  Adjacent to the village of Vík is the famous black-sand beach, Reynisfjara, home to the rock pillars of Reynisdrangar, said to be two trolls frozen by the light of the sun. Though beautiful, this area is gaining notoriety for its dangerous sneaker waves, so visitors should be sure to stay well away from the edge of the water, even on a calm, still day.

  There are no landmasses between Reynisfjara beach and the continent of Antarctica, so you can imagine how the waves can build momentum.

  After passing through Vík, you will cross the glacial sand plain of Skeiðarársandur, before entering Vatnajökull National Park, home to the largest ice cap in Europe, Vatnajökull itself, dozens of glacial outlets and the magnificent Jökulsárlon glacier lagoon.

  While almost all of these sites can be seen from Route 1, they make up 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 within the Vatnajökull National Park is the dramatic Skaftafell Nature Reserve.

  Less than a kilometre from Seljalandsfoss is hidden gem of Gljúfrabúi waterfall, and short walks from Jökulsárlón will take you to the Diamond Beach, where icebergs wash on the black-sand shore, and another glacier lagoon, Fjallsárlón.

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  南海岸,

  

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

  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 count amongst the 30 outlets of Vatnajökull, Iceland’s largest ice cap.  

  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.

  Jökulsárlón Icebergs

  The Jökulsárlón glacier lagoon is one of the most famed and visited attractions in Iceland. Floating on the lagoon are enumerable ice bergs 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" 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.  

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  • Find Jökulsárlón Tours here
  • Find South Coast Tours here

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  Diamond Beach,

  Mt. Keilir is a volcanic mountain, southwest of Hafnarfjörður, and is the most recognisable landmark on the Reykjanes Peninsula. For visitors travelling from Keflavik Airport, it is arguably their first introduction to the beautiful landscapes around Iceland. 

  Formation

  Mt. Keilir is a hyaloclastite mountain, meaning it is made from angular, glassy rock formed by volcanic eruptions underneath an ice sheet. These rock formations can create dazzling shapes and colours. Mt. Keilir was formed during the last Ice Age, leading to the mountain’s distinctive, cone-shaped appearance. This relatively early eruption also means the mountain is far older than the lava fields that surround it. Scientists now strongly believe that Mt. Keilir acts as a ‘plug’ for an incredibly large crater below. 

  Origins

  Long before the introduction of lighthouses, seaman used Mt. Keilir’s prominence on the landscape as a way of navigating the Icelandic coastal waters. As to the origins of the mountains’ name, however, very little is known. Keilir is a masculine word used nowhere else in the Icelandic language. The feminine alternative, keila - meaning cone - was, for reasons now lost, deemed unsuitable, despite the mountain's cone shape. The mountains north to Mt. Keilir are named Keilisbræður, meaning Keilir’s brothers. 

  Hiking

  Mt. Keilir can be visited easily whilst travelling between Reykjavik and Keflavik airport and makes for an excellent 2-3 hour hike. The terrain is loose, but not too steep; still rugged enough to pose a challenge for leisurely mountaineering. The summit peaks at 379m, but for those who make it to the top, there are unbelievable 360-degree views of the surrounding area. Views include steam rising from the nearby Blue Lagoon, the Atlantic Ocean, Snæfellsjökull glacier, Reykjavik city, and other neighbouring towns. Just make sure to climb Mt. Keilir on a clear and sunny day. There is also a bench, for some much-needed respite, and an information board describing the sights and directions from the mountain.

  Mt. Keilir is a 3km walk from Höskuldarvellir. The road leading up to the mountain car park is a gravel road, Road 41, roughly halfway between Reykjavik and Keflavik. A 4x4 jeep is recommended to make the journey. 

  Keilir

• レイキャビクで3泊(ホテルグレードの選択可。朝食の有無や施設については下記宿泊施設詳細をご覧ください。）

• ケプラビーク空港⇔レイキャビク市内の送迎バス

• ブルーラグーンのコンフォート入場券(アップグレード可)と送迎バス

• ゴールデンサークルツアー：小型バス、追加オプション有り

• 南海岸ツアー：追加オプション有り

• 日本語で旅程表を作成、メールでお送りします

• 経験豊富なスタッフが対応します

• 消費税込み

• 夕食

• 昼食

• カメラ

• 水着とタオル（ブルーラグーンでレンタル可能）

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