3 dni, pakiet | Golden Circle, jaskinia lodowa, Jokulsarlon, zorza polarna, wędrówka po lodowcu

• Dostępna: Lis. - Mar.
• Czas: 3 dni
• Aktywności: Lodowiec, Zwiedzanie, Zorza polarna, Jaskinia lodowa
• Poziom trudności: Łatwy
• Minimalny wiek: 8 lat
• Języki: English
• Obszar:

  

  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.

  Złoty Krąg,

  South Iceland is the most popular part of the country and contains some of the most beautiful natural attractions in Iceland, among them the Golden Circle, some of Iceland's most famous active volcanoes as well as the beautiful Jokulsarlon glacier lagoon.

  Geography

  South Iceland is usually divided into the fertile South Icelandic lowlands between Hellisheidi and Eyjafjallajokull volcano on the one hand - and on the other hand the eastern part with the big volcanic glaciers Eyjafjallajokull and Myrdalsjokull (home of Katla) and flattened sands stretching towards the sea.

  The South Icelandic lowlands

  The South Icelandic Lowlands stretch nearly 100 km from Hellisheidi in the west towards Eyjafjallajokull in the east as a very flat and fertile farming land. From the shore the lowland stretches about km towards the inland. This is the best agriculture area in Iceland. The whole area is geologically very young, mainly of tuff type, formed during the Ice Age by the lava flows of the numerous volcanoes of the area. The area is indeed surrounded by volcanically active mountains on all sides. The glacier rivers of the area have helped filling the lavas with sand and clay, leaving it more and less smooth and fertile. Very strong earthquakes are found in this area as well.

  The most active volcanoes of the area are Hekla and Eyjafjallajokull. No less active and not far off, but on the east side, is Katla, which we’ll adress in the eastern part-section. South of the mainland are the volcanic Westman Islands, famous for the 1973 eruption as well as the eruption in 1963, when Surtsey island was formed. Closely linked to the volcanic activity in the south is the geothermal heat found in many places, the best known being the Geysir area, which forms a part of the famed Golden Circle, which also consists of Gullfoss waterfall , Iceland's most famous waterfall as well as one of its most beautiful, located in the popular rafting river Hvita and Thingvellir National Park, comprising three of Iceland's most beloved natural attractions.

  The earthquakes of the area bear witness to the fact that Iceland is still in shape. This is further evidenced by the endless number of fissures in the lavas, fractures in the mountains and certain pieces of lands sinking. The area of Thingvellir is the best known example of this, showcasing the continental drift. Thingvellir is a UNESCO World Heritage Site and the location of the old parliament, Althingi, (now situated in Reykjavik) and one of Iceland's most important sites.

  Another of Iceland's most popular attractions is the beautiful Thorsmork valley, situated between Myrdalsjokull and Eyjafjallajokull.

  Natural harbour-sites are hardly any on the South shore, due to sand produced by the glacier rivers. A few towns are found in the area, Selfoss being the biggest one, Hveragerdi is another, then there are Hella and Hvolsvollur, all conveniently located by the ring road. By the shore are three fishing villages; Thorlakshofn, Eyrarbakki and Stokkseyri. Thorlakshofn the only one of those that can accommodate modern ships and ferrys. The ferry to the Westman Islands sails from there. A new harbour has been built on the sandy coast opposite the Westman Islands. The whole south shoreline offers some of the most gigantic braker waves that you are likely to see.

  Culturewise, in addition to Thingvellir, we reccomend the ancient bishop seat of Skalholt (weekends at Skalholt further offer rich music life). Also, Iceland's most famous saga, Njal's saga takes place in the South lowlands. We further recommend the large reconstructed turfhouse near Stong and the ancient excavated ruins.

  For sports, horse riding is popular in the area as well as catching salmon or trout, hiking, and river rafting in Hvita. 

  The east part of South Iceland.

  This is the area south and east  of Myrdalsjokull. The volcanic glaciers Eyjafjallajokull (near the border of the eastern and western part) and Myrdalsjokull, dominate the view. The landscape has been shaped by volcanic eruptions and vast sands stretch to the sea. Some agriculture is found here, however, with the farms in a row alongside the mountains.  A few large glacial rivers fall down in this area which also has striking waterfalls, such as Skogafoss and Seljalandsfoss.

  Eyjafjallajokull is already well known for its 2010 eruption,  disturbing air communication all over Europe for many days. Much more serious,however, would be an eruption from Katla, a volcano in the eastern part og Myrdalsjokull. 

  Katla’s last eruption was in the year 1918, when an enormous flood of water exploded from the glacier in a matter of minutes, threatening the local farmers of the area. Large amounts of ash and muddy  material were brought to sea to form a new land of sand, Kotlutangi, later washed away by the sea. No people were killed in this eruption. Eruptions in Katla throughout the ages have further created the vast sand area Myrdalssandur. Sixteen eruptions have been recorded for Katla since 930 at intervals of 13-95 years and the volcano is being closely monitored, as time may draw near to its next eruption.

  In the same volcanic system as Katla (geologically speaking), are the Lakagigar craters, northeast of Myrdalsjokull. Those erupted in the years 1783-84; producing the largest amount of lava known in historic times. The ashes hindered the sunlight from reaching down to the surface of Earth, resulting in cold climate over northern Europe.

  In  this area – what we call the eastern part of South Iceland -, there are many places worth visiting: Solheimajokull is a beautiful glacier in a walking distance (an outlet of Myrdalsjokull); Skogar has a very interesting museum of older time traditions and Skogafoss is only a few km away from there. One of Iceland’s most famous hiking routes, Fimmvorduhals, starts from Skogar. Southwest of the village Vik is one of Iceland’s most spectacular beaches, Reynisfjara. Together with the promontory Dyrholaey, which is the southernmost tip of the mainland of Iceland, it offers a breathtaking view with amazing rock formations, a black pebble beach, an abundance of birds and the powerful waves of the North Atlantic Ocean crashing on the beach.

  Further east stretches the world's most vast sand plain, Skeidararsandur. North of the sand is the fascinating Skaftafell preservation area.  At its east end, south of Hvannadalshnukur, Iceland's highest peak, is Ingolfshofdi cape, with its rich birdlife, old fishermen's shacks and its lighthouse. Following the shore further east is the incredibly beautiful and ice-filled Jokulsarlon glacier lagoon. Not far off is the region of Sudursveit, featuring the culture center and heritage museum Thorbergssetur, erected in the memory of Icelandic author Thorbergur Thordarson.

  South Iceland,

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

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

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

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

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

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

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

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

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

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

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

  East Iceland,

  

  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.

   

   

  Jökulsárlón,

  

  Vatnajökull glacier is the largest glacier in Europe, covering 8% of Iceland’s landmass.

  It is the central feature of the Vatnajökull National park, found in the south west of Iceland, a popular spot for activities like glacier hiking from Skaftafell, boat tours in the Jökulsárlón glacier lagoon, and ice caving tours between November and March.

  Facts about Vatnajökull

  Vatnajökull has a surface area of approximately 8,100 square kilometres (3127 square miles); though it is rapidly shrinking due to climate change, its recession is not quite as advanced as at other glaciers, such as Langjökull and Mýrdalsjökull. In parts, it is a kilometre deep (over three million feet), and its average thickness is around half of that.

  Vatnajökull also holds the tallest peak in Iceland beneath its ice; Hvannadalshnjúkur is 2,200 metres tall (7,218 feet). It also conceals some of the most active volcanoes in the country, the most notable being Grímsvötn, Öræfajökull and Bárðarbunga.

  Volcanic activity in the region has occurred on and off throughout the centuries, and many geologists believe that several eruptions are overdue. If their calculations are correct, it would mean significant volcanic activity for Vatnajökull over the scope of the next half century.

  Depending on winds, this could result in worldwide consequences in terms of air-travel, agriculture and the general climate.

  The glacier boasts 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.

  Numerous rivers run out of Vatnajökull, making up some of the greatest glacial rivers in Iceland. The most notable are:

  • 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 was established in June 2008, and has slowly grown to include more and more areas. The park now covers an area of 14,141 square kilometres (5,460 square miles), 14% of the country. It is the second largest national park in Europe.

  Rivers divide the highland plateau to the north of the park. 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 Óðin's eight-legged 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 onto the lowlands. The sandy plains of Skeiðarársandur also lie to to the south, and the glacial river Skeiðará runs through this vast desert.

  One of Iceland's most visited landmarks in the National Park is the Jökulsárlón glacier lagoon, which sits at the base of the outlet glacier Breiðamerkurjökull. Here, large icebergs that have broken off the glacier float across a vast lake before ending up in the Atlantic Ocean, or washed ashore on the nearby Diamond Beach.

  This is one of the best seal-watching spots in the country.

  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, Vatnajökull has on average lost about a metre (three feet) of its thickness annually over the past 15 years.

  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.  

  Efforts are being made to prevent what some say is the inevitable, with reforestation projects going on all around the glacier, a proven method of cooling the area. Time will tell how successful they are.

  Vatnajökull and Jökulsárlón in Popular Culture

  The beauty of Vatnajökull National Park has not gone unnoticed by those in film or television. Many famous scenes have been shot here, starting with James Bond: A View to Kill in 1985. Other notable films with scenes here include Batman Begins, Lara Croft: Tomb Raider, and James Bond: Die Another Day.

  Most famously, however, many places in Vatnajökull have been used in the HBO Series Game of Thrones, north of the Wall. The Wall itself is constructed with CGI using shots of the glacier.
  Vatnajökull,

  

  Skógafoss is one of Iceland’s biggest and most beautiful waterfalls with an astounding width of 25 meters (82 feet) and a drop of 60 meters (197 feet).

  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 kilometre (14 mile) 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.
  

  Skógafoss,

  

  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 seven 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.
  Seljalandsfoss,

  

  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 20 metres (65 feet) up to 40 metres (130 feet) 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 feet).

  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 two kilometres (one 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 kilometre 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.

  Geysir,

  

  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 32 metre (105 feet) 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 11 metres (36 feet), whilst the second drop is 21 metres (69 feet). The canyon walls on both sides of the waterfall reach heights of up to 70 metres (230 feet), 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.

  Gullfoss,

  

  The glacier volcano of Eyjafjallajökull is notorious the world over for causing havoc to air travel in 2010, and stumping television anchors everywhere as they tried to pronounce it. 1651 metres (5427 feet) tall, it is one of the most dominant features of the South Coast.

  Geography

  The glacier of Eyjafjallajökull is approximately 100 square kilometres (39 square miles), making it the country’s sixth largest. It sits close to the fourth greatest, Mýrdalsjökull, which also conceals another notorious volcano, this one called Katla.

  While Eyjafjallajökull’s eruption was huge and disruptive, its pales in comparison to the potential of Katla. Far more explosive, and under much thicker ice, an eruption here in unfavourable wind conditions could have worldwide consequences.

  The magma chambers between both of these mighty volcanoes are connected, and, unfortunately for us, an eruption at Eyjafjallajökull is usually followed by one at Katla within a decade.

  Eyjafjallajökull has many glacial outlets, the most famous being Gígjökull. Many rivers flow from its meltwater, and one of these falls into the beautiful South Coast waterfall, Seljalandsfoss, which it is possible to fully encircle.

  Eruptions

  Eyjafjallajökull’s most recent eruption was no doubt the most famous in Iceland’s history (although the honour really should go to Laki, the 1783-4 eruption of which caused an ash cloud so great that Europe fell into a famine that many historians believe led to the French Revolution). On March 27th, 2010, magma began to bubble from beneath the surface, and by April 14th, ash was starting to billow from the peak.

  800 people were evacuated, in fears not of magma, but of equally dangerous glacial floods, which have decimated Icelandic towns in the past. Animals were ordered to be kept inside, and those with respiratory problems told they should also stay indoors.

  Air travel across Europe was halted, as by the evening of April 15th, the ash was already over the UK, Scandinavia, and parts of Germany. Holidaymakers were trapped, waiting for news, and would end up stuck for eight days; in Scotland and Ireland there were even flights delayed in May due to lingering effects.

  Thankfully, no one was injured, although the ash is thought to have caused respiratory issues for some in the south of the country. Many farms were also destroyed by the ash and floods, with some famers still struggling to recover today.

  Since settlement in 874, Eyjafjallajökull has also erupted in 900, 1612, and from 1821 to 1823. The latter released a huge amount of fluoride which is believed to have affected the bone health of humans and animals alike at the time.

  Eyjafjallajokull today

  Eyjafjallajökull is now entirely safe to visit, and is seen on most tours of the South Coast in clear weather. In the town of Hvolsvöllur, there is a visitor’s centre on the volcano, which focuses on the experience of one family whose farm, Þórvaldseyri, was one of the many destroyed by the floods, lava and ash.

  It is very unlikely that Eyjafjallajökull will erupt again any time soon, with hundreds of years between each eruption, but as mentioned, its neighbour Katla is rumbling...

  Eyjafjallajökull,

  

  Dyrhólaey Peninsula is a 120-metre promenade famed for its staggering views of Iceland’s South Coast, as well as its historic lighthouse and wealth of birdlife. 

  Dyrhólaey (Door Hill Island) is of volcanic origin and was once an island before joining up to the Icelandic mainland. In ancient times, passing sailors used to refer to Dyrhólaey as “Cape Portland”. It is also the most southernmost part of the Icelandic mainland, making it a popular stop for sightseers travelling along the Ring Road, and can be found close by the coastal village of Vík í Mýrdal. 

  One of Dyrhólaey’s instantly recognisable attractions is the promenade’s massive rock arch, a result of centuries of erosion. As a result, its name, (‘dyr’=door’) is in direct reference to this enormous arch. In fact, this natural feature is so large and dramatic that one daredevil pilot even flew through it, back in 1993. 

  Dyrhólaey has an abundance of birdlife, the most common sights being Eider Ducks and Iceland’s favourite winged resident, the migratory Atlantic Puffin, during the summer. 

  From your position atop the promenade, you can also enjoy staggering views over Iceland’s black sand beaches, complemented by the glittering waves of the Atlantic on one side, and distant mountainscapes to the other. To the north, you are also able to see the creeping glacier, Mýrdalsjökull, only proving that this is one of the most interesting panoramas in the whole of the country. 

  On top of Dyrhólaey stands Dyrhólaeyjarviti, a beautiful old lighthouse that consists of a white, square concrete tower. The first lighthouse in the area was built in 1919; the current construction was completed in 1927. Visitors here will be able to see the lighthouse flicking out beams of white light to sea every ten seconds. 

  

  Dyrhólaey,

  

  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.
  Þingvellir,

  

  Strokkur is Iceland’s most visited active geyser. One of the three major attractions on the world-famous Golden Circle sightseeing route, it is usually visited alongside Gullfoss Waterfall and Þingvellir National Park.

  Strokkur is found in the Geysir Geothermal Area, titled after the Great Geysir, which lent its name to all others across the world. It is the greatest active geyser on site; Geysir itself is in a period of inactivity. It erupts more regularly than Geysir ever did, however, blasting water to heights of up to forty metres every five to ten minutes.

  Strokkur and Haukadalur Valley

  

  Strokkur is the primary feature of the Haukadalur valley, and the main reason why it is one of the most visited sites in the country. While Geysir will very occasionally still erupt to enormous heights, it is nowhere near reliable enough to justify the area’s popularity.

  Haukadalur valley, however, has many other features that make it worth a visit. The natural beauty of the area is shaped by the forces of the earth; fumaroles, hot-springs, mud-pits and other little geysers are littered around, and the ground itself is dyed vividly by elements such as sulfur (yellow), copper (green) and iron (red).

  Opposite the main geothermal area in Haukadalur Valley is a restaurant, cafe, hotel and luxury gift shop.

  Science behind Strokkur

  

  Active geysers like Strokkur are rare around the world, due to the fact that many conditions must be met for them to form. They are thus only found in certain parts of highly geothermal areas.

  The first condition that is necessary is an intense heat source; magma must be close enough to the surface of the earth for the rocks to be hot enough to boil water. Considering that Iceland is located on top of the rift valley between the North American and Eurasian tectonic plates, this condition is met throughout most of the county.

  Secondly, you will need a source of flowing underground water. In the case of Strokkur, this comes from the second largest glacier in the country, Langjökull. Meltwater from the glacier sinks into the surrounding porous lava rock, and travels underground in all directions.

  Evidence of this flowing water can be found in Þingvellir National Park, where there are many freshwater springs flowing straight from the earth.

  Finally, you need a complex plumbing system that allows a geyser to erupt, rather than just steam from the ground like a fumarole. Above the intense heat source, there must be space for the flowing water to gather like a reservoir. From this basin, there must be a vent to the surface. This vent must be lined with silica so that the boiling, rising water cannot escape before the eruption.

  Environmental Issues with Strokkur

  One of the main reasons that Geysir entered a period of inactivity was due to the fact soap used to be pumped into the vents to make the eruptions more dramatic; it damaged the structure of the vent and prevented water building up. Strokkur, therefore, is guarded against all interference, with chains keeping visitors a good distance away.

  Unfortunately, however, there have been incidents where people have meddled with its natural state. For example, an artist called Marco Evaristti once poured food colouring into it to make the eruption pink. He defended himself by claiming that nature was open to artists to utiltise and the fact the colouring was all-natural, but he became a pariah amongst many Icelanders, and was arrested and fined (though never paid it).

   

  Strokkur,

  

  Sólheimajökull is an outlet glacier of the mighty icecap of Mýrdalsjökull on the South Coast of Iceland. It is one of the most easily accessible glaciers to reach from Reykjavík, just 158 kilometres (98 miles) away.

  For those who are based in Reykjavík, it is by far the favourite to take guided glacier walks on, competing nationally for popularity only with Svínafellsjökull in the south-east.

  Geography of Sólheimajökull

  About eight kilometres long and two kilometres wide (five miles long and just over a mile wide), Sólheimajökull is an impressive feature. Due to the way it descends from Mýdalsjökull, however, without a clear distinction between the two, it appears much vaster.

  Mýrdalsjökull itself has many other outlet glaciers; overall, it is the fourth largest ice cap in Iceland. Beneath its thick surface is one of the country’s most infamous volcanoes, Katla.

  Much larger than Eyjafjallajökull, which erupted in 2010 causing widespread havoc at European airports, its magma chamber is connected, and it is due to erupt at any time.

  Sadly, like all the glaciers in Iceland bar one, Sólheimajökull is shrinking rapidly. A glacier lagoon at its base reveals how quickly it is receding: the length of an Olympic swimming pool every year. It seems like this change is already an irreversible consequence of climate change, and it may be gone within decades.

  Visitors to Iceland should, therefore, make sure they witness the ice-cap while it is still with us.

  

  Sólheimajökull has several distinctive traits that separate it from other glaciers. Firstly, it is incredibly easy to find, laying just off of the Ring Road that encircles Iceland. Secondly, it is not surrounded by tall mountains, meaning those who ascend it can attain incredible views of the South Coast. Thirdly, it is home to many walls of ice that can be climbed up with ice axes on certain tours.

  All the traits that make Iceland’s glaciers so beloved can be found on Sólheimajökull. There are crevasses that snake across the surface, spectacular ice ridges and formations, and a vivid colouration that dances between a gleaming white, electric blue, and ash black. Occasionally, you will even find an ice cave, though these can never be guaranteed.

  A river runs from the meltwater of the glacier tongue, called the Jökulsá a Solheimasanður. This river runs through a glacial outwash plain - otherwise known as a black-sand-desert - of Sólheimasanður itself, to the nearby ocean.

  Tours on Sólheimajökull

  Many day tours run from Reykjavík to Sólheimajökull, for glacier hikes or as part of a greater South Coast tour.

  Greater South Coast tours include visits to other features, such as the incredible waterfalls of Skógafoss and Seljalandsfoss, the black sand beach Reynisfjara, and some even reach Vatnajökull National Park and the Jökulsárlón glacier lagoon.

  Hidden crevasses and ice caves, slippery surfaces, and the threat of rock- or ice-falls all pose dangers on glacier hikes, but glacier guides have to pass several training courses to deal with these eventualities, making the activity quite safe for those in a fit state of health.

  All guests are equipped with helmets, ice axes, and crampons, and should arrive wearing warm clothes and sturdy hiking boots.

  It is forbidden to ascend glaciers without the correct equipment or training, for your safety and the safety of others. There have been injuries and deaths on Sólheimajökull before, and glacier guides have had to risk their lives to rescue those who flouted the rules.

   

  Sólheimajökull,

  

  Mýrdalsjökull is a glacier in the south of the Icelandic highlands. It is the country's fourth largest ice cap, covering nearly 600 kilometres squared, and its highest peak is almost 1500 meters tall. It is most well-known for sitting atop the notorious and explosive volcano, Katla.Mýrdalsjökull is visible from Route 1 on the South Coast, sitting to the north of the village of Vík.

  Eruptions beneath Mýrdalsjökull

  Since 2010, the world has known of the volcano beneath Eyjafjallajökull; few, however, are aware of the much larger volcano right beside it. Mýdalsjökull conceals Katla, one of the country’s most active volcanoes, having erupted, on average, once every fifty years since 930 AD. Because of the glacier above it, these eruptions tend to cause enormous ash clouds.

  The last major eruption beneath Katla was in 1918, in which such huge lahar floods occurred that the southern coastline was extended five kilometres outwards. This area is also very susceptible to glacial floods, or jökulhlaups, during eruptions, even when the lava does not break through the surface of the ice.

  Historically, the area was little settled for this reason.

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

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

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

  Tours on Mýrdalsjökull

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

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

  Tours around Mýrdalsjökull

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

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

   

  Mýrdalsjökull,

  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.  

  Skaftafell,

  

  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.
  Reynisfjara Black Sand Beach,

  

  Vík í Mýdral, or just Vík, is the southernmost village on the Icelandic mainland, located 186 kilometres (110 miles) from the capital Reykjavík.

  Often visited by those travelling the popular sightseeing route along the South Coast, it is a wonderful place to stop, recharge, and if you are taking your time, rest for the night. Though it only has around 300 residents, the village is very popular amongst tourists for its convenience and beautiful surrounding landscapes.

  Features near Vík

  Reaching Vík from Reykjavík takes approximately two and a half hours, and en route, there are many marvellous features to admire. Two of the country’s most famous waterfalls, Skógafoss and Seljalandsfoss, lay between the two destinations; the former has awe-inspiring power, whereas the latter can be fully encircled.

  The subglacial volcanoes of Eyjafjallajökull and Katla can also be seen on clear days; both of these are particularly explosive, with Eyjafjallajökull famously disrupting European air travel in 2010. Out to sea in especially good weather, the Westman Islands can also be seen on the horizon.

  Just before Vík are the popular birdwatching cliffs of Dýrholaey, where you can also find an enormous rock arch curving out into the ocean. This is one of the best places for birdwatching in Iceland, with thousands of puffins nesting here from May to October.

  The village itself sits opposite one of the country’s most famous features: Reynisfjara black sand beach. Considered one of the world’s most beautiful non-tropical beaches, it boasts incredible geology.

  

  Particularly of note are the Reynisdrangar sea-stacks, said to be two trolls frozen in the light of the morning sun as they tried to pull a ship into shore.

  Though this beach makes for a lovely walk, particularly for those staying in Vík overnight, as they can see it under the midnight sun or northern lights, it has its dangers. Sneaker waves can be notorious here, so visitors should stay far from the water’s edge, and never go for a swim. Lives have been lost here before.

  The route to Vík from Reykjavík is beautiful, and continues to be so as you travel further along the South Coast, through the Skeiðarásandur black-sand-plains into Vatnajökull National Park. This beautiful region is often the final destination of those passing through Vík, as it is home to the largest glacier in Europe, the Skaftafell Nature Reserve, and Jökulsárlón Glacier Lagoon.

  Of course, ambitious travellers will carry on from here to encircle the full country.

  Wildlife around Vík

  Vík, due to its closeness to the Reynisfjall and Dýrholaey cliffs, has a rich birdlife. Short walks from the village will take you to the nesting grounds of gulls, fulmar, guillemots, and in summer, puffins.

  Due to its coastal location, visitors to Vík have a decent chance to see seals on the shore. There is also a slim chance to see whales or dolphins; the twenty or so species that live in Iceland’s waters can appear at any time.

  Services in Vík

  Vík has a wide variety of public services, due to its remoteness and its importance connecting the east and west of Iceland. There are gas stations, shops and cafes, a swimming pool, a wool factory that can be visited, and a wide range of accommodation options for all budgets.

  Please note, however, that as the village has such a small year-round population, those with special dietary requirements should purchase their food from Reykjavík before departing.

   

  Vík í Mýrdal,

  

  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.

  Reynisdrangar,

  

  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 this island, most notably being a favourite destination of Danish royals.

  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 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 from Svinafellsjokull Glacier Hiking Tour

  Svínafellsjökull in an outlet glacier of Vatnajökull, the largest ice cap in Europe, found within the Skaftafell Nature Reserve in Iceland's south-east.

  It is one of the most popular glacier tongues to hike, with some tours upon it lasting throughout the year; ice climbing is also possible here. Because of its dramatic ridges, plunging crevasses, spectacular views and vivid blue and white colouration, it was used in Game of Thrones Season 7 to represent the harsh lands North of the Wall.

  Skaftafell, part of the Vatnajökull National Park, is renowned for its glacier tongues, waterfalls, lava-landscapes and many hiking trails.

  Svínafellsjökull,

  

  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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  Południe,

  

  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

• Wszystkie noclegi w hotelach ze śniadaniem

• Wycieczka do jaskini lodowej

• Wędrówka po lodowcu

• Przewodnik mówiący po angielsku

• Transport

• Obiad

• Lunch

• Ciepłe ubrania, odporne na wiatr i deszcz

• Zimowe buty górskie

• Aparat fotograficzny i dodatkowe baterie

Ze względu na zwiększony popyt na usługi turystyczne w Islandii i niską dostępność, firmy oferujące wycieczki po Islandii nie mogą zagwarantować konkretnego zakwaterowania. Jednak zawsze zapewniamy najlepsze dostępne zakwaterowanie, w momencie dokonywania rezerwacji. Poniżej widać nasz pierwszy wybór noclegów. Pierwszy nocleg - pokój w hotelu Hvolsvöllur i Hótel Eyjafjallajökull. Druga noc - Hótel Höfn i Hótel Vatnajökull. Jeśli te miejsca są w pełni zarezerwowane w czasie trwania wycieczki, znajdziemy alternatywne rozwiązanie o tym samym standardzie.