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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.
The Golden Circle is a 300 km route to the 3 most popular natural attractions in Iceland. The Golden Circle consists of Geysir, Gullfoss and Thingvellir.
See this for Golden circle tours.
Geysir area
Geysir is a geyser that gives its name to hot springs all over the world. But although Geysir itself is not active anymore the area features spectacular hot springs such as the powerful Strokkur (spouting a vast amount of water every 10 minutes, regularly about 15-20 meters into the air), Smidur and Litli-Strokkur.
Gullfoss waterfall
The 'Golden Waterfall', is the second part of the Golden Circle, and one of the most beautiful and powerful waterfalls in Iceland, plummeting 32 meters into the river gorge of the popular rafting river Hvita. It is Iocated about 10 km from Geysir.
Thingvellir national park
The largest attraction of the Golden Circle is Thingvellir National Park. The Icelandic parliament was founded there in 930 and remained until the year 1798.
Today it is a UNESCO World Heritage Site and one of the most important places to visit in Iceland, not just for its historical and cultural values, but for also its magnificent landscape.
Thingvellir is surrounded by a beautiful mountain and volcano range and is the site of a rift valley, where the tectonic plates meet, marking the crest of the Mid-Atlantic ridge.
Of particular note at Thingvellir are the magnificent Almannagja gorge, and the beautiful lake Thingvallavatn, the largest lake in Iceland. The popular Gjabakkahellir lava cave is also in the area.
The fissure Silfra is located by Thingvallavatn, Iceland's largest lake, and is famous for its clear waters and popular for diving and snorkeling, as you can literally swim between continents.
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.
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.
North Iceland is very popular area in Iceland and contains some of the best attractions on the island. Akureyri is the capital of North Iceland and is the second largest "city" in Iceland. Around 20.000 people live in North Iceland.
The North coast has four major fjords (or bays) with mountain ridges between them and each of the fjords has corresponding agricultural districts.
The main districts are: Hunathing, Skagafjordur district, Eyjafjordur district and the amazing Thingeyjarsysla county, home to Lake Myvatn.
More attractions in the amazing Thingeyjasysla are mentioned below. Note that the first three areas are geologically speaking ancient formations, while Thingeyjasysla is recent and full of volcanic activity, young lava fields and tuff mountains.
Siglufjordur and Grimsey island are also part of the north but listed separately.
Eyjafordur
In Eyjafjörður is the capital of the North, Akureyri with 17.000 inhabitants. It is a very charming town and highly popular with travelers, so we advise you not to miss it. Many cruisers land in the port of the town.
The older part of Akureyri is particularly worth a stroll. If you like skiing or snowboarding, one of the best skiing sites in the country is located nearby.
We also recommend the botanical gardens there, fine restaurants and many interesting museums, such as Davidshus and Nonnahus, dedicated to the memory of poet David Stefansson and Jon Sveinson, author of the Nonnabaekur ('Nonni’s books').
Not far from Akureyri is the unique turf framhouse of Laufas, a museum and a prime example of the old architecture and farmlife. Also not far from Akureyri are the submarine geothermal silica cones of Strytur, a natural wonder and an excellent place for a dive.
One of Iceland's most beloved poets, Jonas Hallgrimsson was born in Eyjafjordur, at the farm Hraun in Oxnadalur valley and the knife-edged lava peaks there are particularly stunning. Also essential when traveling in the area is the beautiful and peaceful island Hrisey, often called 'The Pearl of Eyjafjordur'.
Siglufjordur
Siglufjordur has the distinction of not falling under the regular four part division, as it straddles the border of Eyjafjordur and Skagafjordur. Here we highly recommend the herring era museum and the folk music museum. Indeed, Siglufjordur hosts an annual folk music festival that is truly worth experiencing.
Hunathing
Among major attractions in Hunathing are the Regional Museum at Reykir in Hrutafjordur, the Seal Watching Center at Vatnsnes and the Arnarvatnsheidi heath, with a large numbers of ponds and lakes full of trout.
Skagafjordur
In Skagafjordur, the largest town of which is Saudarkrokur, we particularly recommend the historical bishop’s seat of Holar and the agricultural university there, the Glaumbaer museum, and Drangey island.
Thingeyjarsysla
Thingeyjarsysla county is the home of the beautiful waterfalls Godafoss and Aldeyjarfoss as well as the amazing Lake Myvatn with its fascinating pseudocraters and rich birdlife.
Near Myvatn is the chaotic lava field Dimmuborgir, a truly amazing sight (and paid homeage to by the Norwegian Black Metal band of the same name).
Husavik is the whale watching capital of the North so don’t miss that one either.
The Jokulsargljufur National Park is home to some of Iceland's most beloved natural attractions, Holmatungur, Hljodaklettar and the Asbyrgi canyon. In the river Jokulsa a Fjollum is Europe's most powerful waterfall, Dettifoss.
At the Melrakkasletta peninsula you can see fascinating birdlife and there is good trout fishing to be made there. Seals may be sighted as well as whales off the coast. The vegetation is rich and this is an ideal place to enjoy the midnight sun. Northern lights may also be spotted from late August to early April.
Grimsey
Far north, straddling the Arctic Circle is Grimsey island, the northernmost inhabited territory of Iceland, with a population of about 100 people. It is renowned for its fishermen, its rich vegetation and birdlife.
Reykjavik is the capital of Iceland and the northernmost capital of a sovereign state in the world.
Despite a small population (120.000 and more than 200.000 in the Greater Reykjavik area), it is a vibrant city that draws an ever increasing number of visitors. It is the financial, cultural and governmental centre of Iceland. It also has a reputation of being one of the cleanest and safest cities in the world.
Geography
The city of Reykjavik is located in southwest Iceland by the creek of the same name. Throughout the ages, the landscape has been shaped by glaciers, earthquakes and volcanic eruptions and the area is geothermal. Much of the current city area area was subglacial during the Ice Age, with the glacier reaching as far as the 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 Reykjavik is set with peninsulas, coves, straights and islands, most notably the island of Videy, and seabirds and whales frequent the shores. The mountain ring as seen from the shore is particularly beautiful. Mount Esja is the highest mountain in the vicinity of Reykjavik and lends its distinct feature to the whole area. This majestic mountain is also highly popular for climbing. Other notable mountains that can be seen from the seaside are Akrafjall and Skardsheidi and on clear days one may even see as far to the legendary Snaefellsjokull glacier, at the end of the Snafellsnes peninsula.
The largest river to run through the city is Ellidaa in Ellidaardalur valley, which is also one of Iceland‘s best rivers for salmon fishing.
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 Sundahofn in the east. The domestic Reykjavik Airport is located at Vatnsmyrin, not far from the city centre and close to Oskjuhlid and Perlan. The international Keflavik Airport at Midnesheidi heath then lies around 50 km from the city. Cars, jeeps and bicycles can be readily rented in the city and many organized tours are also being offered.
What to See & Do in Reykjavik
The local arts scene is strong in Iceland, with both annual events and single ones, many of whom have hit the international stage. For the annual ones please check our articles Best Annual Events in Iceland and the Top Ten Festivals in Iceland. Major events taking place in Reykjavik include the Iceland Airwaves, Gay Pride, RIFF (The Reykjavik International Film Festival), The Reykjavik Literature Festival, Cultural Night, the Reykjavik Arts Festival, Food & Fun, the Reykjavik Fashion Festival and the Sónar music festival.
Among famous people from Reykjavik are artists Bjork Gudmundsdottir, Sigur Ros, writers Halldor Laxness (born in Laugavegur) and Arnaldur Indridason and mayor Jon Gnarr. For more well-known and fairly-well known Icelanders, check our article on the subject.
You might also want to check our article on some of the many things to see and do in Reykjavik, such as visiting the city‘s many museums, exhibitions and galleries, checking out live music, visiting the Harpa music hall or the theatres, visiting the lighthouse at Grotta, the main shopping street of Laugavegur, visiting the old harbour and the flea market, going on a bird- and whale watching tour or visiting Videy island. We also have a top ten list of things to do.
Make sure to visit the public square of Austurvollur, one of the city‘s most popular gathering places, where you‘ll also find the national parliament, Althingi, the state church a statue of independence hero Jon Sigurdson, as well as cafés, bars and restaurants. Austurvollur was central in the 2008 protests, along with Laekjargata, home to the House of Government. You are also not likely to miss the great church of Hallgrimskirkja that towers over the city from the hill of Skolavorduholt, wherefrom you‘ll get a great view of the city.
Try a walk by the city pond, greet the many birds that frequent the area and visit the city hall, stationed by its banks. The Hljomaskalagardur is a beautiful park that lies by the pond, it ideal for a nice walk and sometimes concerts get held there. Further off is the campus of the university of Iceland, the Nordic house and the Vatnsmyri wetland, a particularly pleasant place, but be mindful of not disturbing the wildlife there and keep to the pathways.
For a nice swim on a warm day, we particularly recommend Nautholsvik beach.
Visit the Laugardalur valley, home to one of the city‘s best swimming pools, as well as the Asmundarsafn gallery, a beautiful botanical garden and a domestic zoo. A walk by the Aegissida beach, with it‘s old fishing sheds, in the west part of Reykjavik also holds a particular charm. The aforementioned Elllidaardalur valley is also a popular resort.
Another place that offers one of the city‘s best (and free) views is Perlan, up in Oskjuhlid hill. The hill itself is a popular resort, with over 176.000 trees and great opportunities for walking and cycling.
Travel to Alftanes to see the president‘s house at Bessastadir, which is also a historical site in it‘s own right, having been the educational centre of Iceland for centuries. Nearby is a beautiful lava field, Galgahraun, well worth a visit, though there is currently an environmental struggle going on as to it‘s future state.
The city is furthermore a short drive from many of Iceland‘s major attractions, most famously the Golden Circle and the Blue Lagoon. In close vicinity you‘ll also find the Heidmork preservation area, a favourite pastime resort of the people of Reykjavik, as well as the Blue Mountains, one of Iceland‘s most beloved skiing venues.
Check our Best of Reykjavik guide further for tips on the best cheap things to do in Reykjavik, some of the best restaurants in the city, happy hours, the top ten value places to eat and our two articles on the famous Reykjavik nightlife; Nightlife in Reykjavik and Nightlife and mating.
Finally, we‘d like to stress that these are only some suggestions of the many things you might check out in Reykjavik. Whatever you choose to do, we hope you‘ll be able to make the most of your visit and we wish you a pleasant stay in our capital.
Akureyri, ‘The Capital of the North’ is a town in the fjord Eyjafjordur in North Iceland. It lies just 100 km away from the Arctic Circle. It is Iceland’s second-largest urban area with a population of about 17,800.
Read Akureyri | Iceland's "Capital of the North" for more information.
Economy
Akureyri is an important fishing centre and port, but in the last few years tourism, industry, higher education and services have become the fastest growing sectors of the economy.
An international airport is located about 3 km from the center. A large number of cruisers also stop at Akureyri. One of Iceland's best skiing sites is found by Akureyri, at Hlidarfjall.
Traditionally Akureyri has survived on fisheries and some of Iceland’s largest fishing companies, like for example Samherji, have their headquarters there. Other large companies include Brim, Nordurmjolk, and Vifilfell hf, the largest brewery in Iceland.
FSA/Akureyri Hospital is a major employer in the area and is one of two major hospitals in Iceland.
Akureyri has excellent facilities for travelers and is located a short drive from many of Iceland’s top natural, cultural and historical attractions.
Nature & Landscape
Akureyri is surrounded by mountains, the highest one being Kerling (1538 m). The area around it has rich agriculture and a beautiful mountain ring.
The innermost part of the fjord, Pollurinn ('The Pool') further lends the town a special character. The climate in Akureyri is generally very pleasant.
The islands Hrisey in the middle of Eyfjordur and Grimsey, straddling the Artic Circle, both belong to the municipality of Akureyri. Hrisey is often called 'The Pearl of Eyjafjordur' and Grimsey 'The Pearl of the Artic' and these beautiful and peaceful islands are highly popular with travelers.
History & Culture
During World War II the town was an important site for the Allies and the town grew considerably after the war, as people increasingly moved to urban areas.
Akureyri has a strong cultural scene, with several bars and renowned restaurants. Folk culture in general is more prevalent there than in Reykjavik. During the summer there are several notable festivals in Akureyri and its surroundings.
Sites of interest in Akureyri include the brand-new Hof concert hall and Akureyri’s many museums, The Nature Museum, Nonnahus, a.k.a. Jon Sveinsson Memorial Museum, for the writer, David's house or David Stefansson Memorial Museum, for the poet, Akureyri Art Museum.
Akureyri also has several churches, Akureyrarkirkja being the most notable, as well as beautiful botanical gardens. The old town is particularly charming, ideal for a nice walk.
Jökulsárlón is Iceland’s most famous glacier lagoon. Conveniently located in the southeast by Route 1, about halfway between the Skaftafell Nature Reserve and Höfn, it is a popular stop for those travelling along the South Coast or around the circular ring road of the country.
Geography
As a glacier lagoon, Jökulsárlón is a lake that is filled with the meltwater from an outlet glacier. In this case, it is Breiðamerkurjökull, a tongue of Europe’s largest ice cap, Vatnajökull.
It stands out, however, due to the fact that it also fills with icebergs breaking from the glacier, some of which tower several stories high.
These icebergs, other than their scale, are notable for their colouration. Although they are, as expected, largely white, most are also dyed electric blue in part, with black streaks of ash from eruptions centuries past.
When the icebergs finally make it across the lagoon, they either drift out to sea or wash up on the nearby shore. Because of the way they glisten against the black sands of Breiðamerkursandur, this area has been nicknamed ‘the Diamond Beach’.
In spite of being a rather recent formation, Jökulsárlón is the deepest lake in the country, with depths reaching 248 metres. With a surface area of 18 square kilometres, it is also growing to be one of the largest.
History
Jökulsárlón has not been around since Iceland’s settlement; it only formed around 1935. This was due to rapidly rising temperatures in the country from the turn of the twentieth century; since 1920, Breiðamerkurjökull has been shrinking at a dramatic rate, and the lagoon has begun to fill its space.
Today, the expansion of Jökulsárlón is accelerating. As recently as 1975, it was just 8 square kilometres, and now that size has more than doubled.
In the relatively near future, it is expected that the lagoon will continue to grow until it becomes a large, deep fjord.
Though a dark omen for Iceland’s glaciers and ice caps in general, the retreat of Breiðamerkurjökull has resulted in an incredibly beautiful, if temporary, site. This has not been overlooked by Hollywood.
Jökulsárlón has been featured in the James Bond films A View to Kill in 1985 and Die Another Day in 2002, 2001’s Lara Croft: Tomb Raider, and 2005’s Batman Begins.
In 2017, Jökulsárlón was enveloped into the Vatnajökull National Park, thus it is now fully protected by Icelandic law.
Wildlife
Because of the wealth of herring and capelin that the tides bring into the lagoon, Jökulsárlón is somewhat of a hot-spot for Iceland’s wildlife.
In summer, it is a nesting site for Arctic Terns; stay well away from this area, as these birds are notorious for the fierceness with which they protect their eggs, dive-bombing the heads of any they see as a threat. Skuas also nest on the lake’s shores in this season.
Seals can be reliably spotted here throughout the year, swimming amongst or else hauling out on the icebergs. Jökulsárlón provides them with a safe haven to rest and socialise, especially considering the waters of southeast Iceland are renowned for their population of orcas.
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.
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.
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)
Myvatn is a beautiful lake with many small islands in the north of Iceland, the fourth largest lake in the country. Along with its surrounding area, the lake is one of Iceland's most amazing natural attractions.
Some of the islands in Myvatn are pseudocraters, formed by steam explosions. The lake has rich birdlife and more species of ducks than anywhere else in the world. As for vegetation, it is one of the few places in the world that grows Marimo, also known as Cladophora ball, Lake ball, or Moss Balls in English, a species of filamentous green algae (Chlorophyta).
The Myvatn nature baths are also renowned throughout the world, a perfect place to relax, surrounded by breathtaking landscape.
Close to the lake is Dimmuborgir, a fascinating area of dramatic and chaotic lava. Norwegian symphonic metal band Dimmu Borgir takes its name from the the lava field, and it continues to inspire travellers from all over the world.
The Myvatn area is definitely one of the most beautiful places in Iceland. Don´t miss it!
Dimmuborgir (e. ‘Black Forts') is a large area of chaotic lava, situated right east of Lake Myvatn, in North Iceland. With its dramatic view, Dimmuborgir is one of Iceland's most popular attractions.
The area is composed of various volcanic caves and rock formations, reminiscent of an ancient collapsed citadel. In folklore the Dimmuborgir lava field has been connected with hell, Satan was to have landed there after being cast from heaven and the Norwegian symphonic black metal band derives its name from the region.
Husavik in Skjalfandi Bay in North Iceland is called the whale watching capital of the world.
Whale watching is highly recommended from Húsavík and visiting the village whale museum. Other places that visitors might like to visit are the wooden Húsavíkurkirkja church, built in 1907, and the civic museum for culture and biology, which amongst other things features a stuffed polar bear and ancient boats, bearing witness to the history of seafaring in Iceland.
In Húsavík you'll find cute cafés and restaurants offering tasty treats, and you'll have a gorgeous view over the Skjálfandi Bay from this small town of about 2,000 inhabitants.
Skógafoss is one of the country’s biggest and most beautiful waterfalls with an astounding width of 25 meters (82 ft) and a drop of 60 meters (197 ft). Due to the amount of spray the cascade produces, a rainbow is present any time the sun emerges from behind the clouds.
Located on the Skógá river, this mighty cascade is clearly visible from Route 1 and is an excellent place to stop and stretch the legs while travelling Iceland’s South Coast. The river below Skógafoss holds a large char and salmon population and is thus a favourite spot for fishermen in the summer.
The land underneath the waterfall is very flat, allowing visitors to walk right up to the wall of water. Keep in mind, however, that this will get you drenched. Skógafoss can also be viewed from the top as a steep staircase leads to an observational platform above the cascade.
Geography
Skógafoss is located near the small village of Skógar, south of the Eyjafjallajökull glacier volcano. There you’ll find the Skógasafn folk museum, an open-air museum with both old wooden houses and turf houses, as well as a regional museum with various artefacts from this area.
A part of the Skógasafn Regional Museum is the Museum of Transportation, which showcases the history and evolution of transportation, communication and technologies in Iceland. There, you can see how this nation evolved from the age of the working horse to the digital communications of the 21st century.
The Skógasafn museum also includes a café and a museum shop, and in the village of Skógar, you will find both a hotel and a restaurant.
At the eastern side of Skógafoss, you will find one of Iceland’s most famed hiking routes; the Fimmvörðuháls pass. The 22 km (14 mi) trail takes you along Skógá river, between two glaciers, Mýrdalsjökull and Eyjafjallajökull, before ending in the beautiful Þórsmörk valley.
Folklore
A gold ring is on display at the Skógasafn museum. According to legend, the ring is from a chest that was owned by Þrasi Þórólfsson, one of the first Viking settlers in the area. Folklore states that before his death in 900 AD, Þrasi buried a chest filled with gold in a cave behind Skógafoss waterfall.
Many attempts were made to retrieve the chest after Þrasi’s death, and years later, locals managed to grasp a ring on the side of the chest. As they pulled, the ring broke off, and the treasure was lost forever. The ring was then given to the local church before it made its way to the museum.
Seljalandsfoss is a waterfall, 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 of the most famous and visited falls in the whole country. Majestic and picturesque, the waterfall is one of the most photographed features in the whole of Iceland.
Geology and Surroundings
Seljalandsfoss waterfall, part of the river Seljalandsá, has its origins underneath the glacier volcano Eyjafjallajökull. The cascade of the falls is relatively narrow. However, it used to be wider until a flood in 1976 altered the shape of the cliffs from which the waterfall tumbles. The rainfall during the day of the flood measured 101 millimetres (4 inches), which caused a significant rise in the water levels of rivers in the area. This event caused a new crack to form in the cliffs, that subsequently redirected the width of the falls.
The cliffs themselves are the remnants of a former coastline, which now separates the lowlands from the Highlands of Iceland. The same can be said of Seljalandsfoss’s equally famous neighbour, Skógafoss waterfall.
The most distinguished feature of Seljalandsfoss is a natural pathway that stretches all the way around it. The cliffs behind the falls, therefore, form an accessible cave. Visitors can easily walk this path, although they 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. During the winter season, it is highly advised not to walk around the falls since the icing makes the walk too hazardous.
However, floodlights have been set up on both sides of the waterfall, which impressively illuminate the scene during dark winter nights. 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.
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 indicates 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’.
The waterfall was also a featured waypoint during the first leg of the sixth season of The Amazing Race, an American reality TV series.
Geysir is a dormant hot spring in the geothermal area, Haukadalur Valley, found in South Iceland. Making up just one of the attractions along the world famous 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 around the world.
Geography
Though Geysir itself is rarely active these days, Haukadalur Valley boasts a plethora of hot springs, 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 twenty metres (65 ft) up to forty metres (130 ft) 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 at Geysir. 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 a wealth of fumaroles emanating steam and gas into the cool Icelandic air can be found. 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 steam 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 2 km from Geysir is a preserved natural pool called Kúalaug. It has room for 3-5 people at a time, but care should be taken, as the area around the pool is very delicate. The temperature is 39-43°C, depending on 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 re-forestation 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 a church site since ancient times and has been inhabited since the Age of Settlement. Given its historic value, it should be noted that scholar, Ari “The Wise“ Thorgilsson, grew up there; 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 one of the oldest of its kind in Iceland.
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.
Gullfoss (translated to ‘Golden Falls’) is one of Iceland’s most iconic and beloved waterfalls, found on the Hvítá river canyon in south Iceland. The water in Hvítá river travels from the glacier Langjökull, finally cascading 32m down Gullfoss’ two stages in a dramatic display of nature’s raw power.
Because of the waterfall’s two stages, Gullfoss should actually be thought of as two separate waterfalls. The first, shorter stage of the waterfall is 11m, whilst the second stage is 21m. The canyon walls on both sides of the waterfall reach heights of up to 70m, descending into the 2.5km long Gullfossgjúfur canyon (geologists indicate that this canyon was formed by glacial outbursts at the beginning of the last age.)
In the summer, approximately 140 cubic metres of water surges down the waterfall every second, whilst in winter that number drops to around 109 cubic metres. With such energy, visitor’s should not be surprised to find themselves drenched by the waterfall’s mighty spray-off.
Gullfoss makes up a part of the highly popular Golden Circle tour, alongside Geysir geothermal area and Þingvellir National Park.
History
In the early days of the last century, Gullfoss was at the centre of much controversy regarding foreign investors and their desire to profit off Iceland’s nature. In the year 1907, an English businessman known only as Howells sought to utilise the waterfall’s energy and harboured ambitions to use its energy to fuel a hydroelectric plant.
At the time, Gullfoss was owned by a farmer named Tómas Tómasson. Tómas declined Howell’s offer to purchase the land, stating famously “I will not sell my friend!” He would, however, go on to lease Howells the land, inadvertently beginning the first chapter of Icelandic environmentalism.
It was Tómas’ daughter, Sigríður Tómasdóttir, who would lead the charge. Having grown up on her father’s sheep farm, she sought to get the lease contract nullified, hurriedly saving her own money to hire a lawyer. The ensuing legal battle was an uphill struggle; the case continued for years, forcing Sigríður to travel many times by foot to Reykjavík if only to keep the trial moving. Circumstances became so difficult that Sigríður threatened to throw herself into the waterfall if any construction began.
Thankfully, in 1929, the waterfall fell back into the hands of the Icelandic people. Today, Sigríður is recognised for her perseverance in protecting Gullfoss and is often hailed as Iceland’s first environmentalist. Her contribution is forever marked in stone; a plaque detailing her plight sits at the top of Gullfoss.
Restaurant / Cafe
Besides Gullfoss, visitors can enjoy the views from Gullfoss Cafe, a locally run delicatessen that serves a wide variety of refreshments and meals. The menu has options to tantalise everyone’s taste buds; hot soups, sandwiches, salads and cakes. There is also a shop on site where visitors’ can browse and purchase traditional Icelandic souvenirs.
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.
Þingvellir National Park is Iceland’s only UNESCO World Heritage site and one of the major stops on the world famous Golden Circle sightseeing tour, alongside Haukadalur Geothermal Valley (Geysir) and Gullfoss Waterfall. Just to the south, as well as a part 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.
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.
This saw the birth of the Old 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.
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, instead adopting Christianity in 1000 AD. This turning point in history was left to the pagan lawspeaker, Thorgeir Thorkelsson, who rested on the choice for one day and one night before reappearing to share his decision.
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 10 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 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.
Katla is an active volcano situated under the glacier Myrdalsjokull in South Iceland. It is one of Iceland's most well known volcanoes.
Katla's eruptions have produced many massive glacier bursts, with enormous amounts of water flowing, as the fire melts the ice. Its latest eruption was 1918. That eruption created the spit Kötlutangi, which is the mainland's southernmost tip.
Strokkur (Icelandic for "churn") is one of the most famous hot springs in Iceland and belongs to the famous Golden Circle.
Strokkur is a fountain geyser in the Geysir geothermal area in the southwest part of the country, east of Reykjavik, near Hvítá river.
Strokkur is a powerful hot spring and an impressive sight. It erupts about every 4–8 minutes and spouts water to a height of 15 – 20 m, sometimes up to 40 m.
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.
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.
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.
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.
Reynisfjara is a world-famous black-sand beach found on the South Coast of Iceland, just beside the small fishing village of Vík í Mýrdal.
With its enormous basalt stacks, roaring Atlantic waves and stunning panoramas, Reynisfjara is widely considered to be the most beautiful example of Iceland’s black sand beaches. In 1991, National Geographic voted Reynisfjara as one of the Top 10 non-tropical beaches to visit on the planet.
Reynisfjara is found around 180 km from Iceland’s capital city, Reykjavik, and is a popular stop-off for those taking a sightseeing tour along South Coast. Driving to the beach is particularly easy, taking an approximate two and a half hours from the capital.
Folklore
Upon visiting the beach, travellers will immediately observe rocky sea stacks sitting off the shoreline, known as Reynisdrangar. According to local Icelandic folklore, these large basalt columns were once trolls engaged in trying to pull ships from the ocean. However, as bad luck would have it, the dawn quickly arose, turning the trolls into solid stone.
Another legend tells of a husband whose wife was kidnapped and killed by two trolls. The man followed the trolls down to Reynisfjara where he froze them, ensuring that they would never kill again.
The sea stacks themselves are home to thousands of nesting seabirds. Species that can be found here include Puffins, Fulmars and Guillemots, making it a must-see location for all birdwatchers out there.
Potential Dangers
Visitors to Reynisfjara must be made well aware of the potential dangers present at the beach. First of all, the rolling, roaring waves of Reynisfjara are particularly violent, often pushing far further up the beach than many would expect.
Visitors are advised to never turn their back on the waves, don't go chasing after them and keep a safe distance of 20-30 metres.
Aside from these sudden and dramatic shifts in tide (known as “sneaker waves”), the currents off the shore are infamous for their strength and ability to drag helpless people out into the freezing cold open ocean. A number of fatal accidents have occurred at Reynisfjara, the last of which occurred in January 2017.
The Skutustadagigar are pseudocraters at the southern shore of Lake Myvatn.
The craters were formed by steam explosions, when boiling lava flowed over the wetlands. The wetlands are preserved and are popular for birdwatching.
Vik in Myrdalur valley is the southernmost village on the Icelandic mainland, located 186 km from the capital Reykjavik.
Vik is important as a service centre for the inhabitants and visitors of the marvellous Reynisfjara beach.
Reynisfjara is widely considered one of the most beautiful beaches on earth (see for example Islands Magazine). This black pebble beach boasts an amazing cliff of regular basalt columns called Gardar, which resembles a rocky step pyramid and out in the sea are the spectaculary shaped basalt sea stacks Reynisdrangar. The area has rich birdlife, including puffins, fulmars and guillemots.
Svartifoss, in the area of Skaftafell in Vatnajokull National Park, is one of Iceland’s most scenic waterfalls.
This narrow 20 metre high waterfall is located in a horse-shoe shaped gorge and derives its name, ‘Dark waterfall’, from the fact that it is framed by dark hexagonal basalt columns. These are very pronounced and make for a truly spectacular sight. At the base you’ll see notably sharp rocks that have broken from the columns, as new column sections break faster than the water wears down the edges.
Architect Guðjón Samúelsson was inspired by the basalt columns of Svartifoss when designing the exterior of Hallgrímskirkja church, which towers over Iceland's capital, Reykjavík, from Skólavörðuhæð hill, and when designing the ceiling of the National Theatre, also in Reykjavík. Likewise the world-renowned sculptor Richard Serra drew inspiration from the columns for his sculpture Milestones, located in Viðey Island in Kollafjörður bay, near Reykjavik.
Egilsstadir is the largest town in East Iceland, with a population of 2257 people as of 2011. It is located on the banks of the river Lagarfljot in the wide valley of the fertile Fljotsdalsherad district.
Egilsstadir is the main centre for service, transportation and administration in East Iceland.
Airport and Services
The town provides all basic services and features an airport which is mostly used for domestic flights, although some international airlines sometimes fly there. The town also boasts a college and a health centre. Egilsstadir also has an annual jazz festival that we can recommend. The town is furthermore close to many of East Iceland's and indeed Iceland's main attractions and as a centre of the area, many East Iceland tours are directed from there.
The area of Fljotsdalsherad has many notable points of interest, whether natural, historical or cultural. Click here for further information about those.
Hella is a small town of around 781 people (as of 2011), located in South Iceland, around 94 km from the capital. It is an important regional centre for the area.
Hella's economy mainly consists of commerce, services and industry. Tourism is an ever-growing sector as well.
The river Ytri-Ranga on the east bank of which Hella is located, is one of the best salmon rivers in Iceland. Hella has excellent lodgings and for recreational activities there is plenty to choose from; sightseeing tours, horse rentals, dog sledge tours and fishing. Horse shows are held regularly and in July the town hosts an annual family festival. Hella is furthermore located near to many of Iceland's major attractions, such as Hekla volcano, Iceland's most famous volcano and one of its most active, as well as the nature wonders of Thorsmork valley and Landmannalaugar geothermal area.
Keflavík International Airport (KEF) is Iceland’s only international airport and the port of arrival for the vast majority of visitors to the country. In 2016 alone, almost seven million passengers went through its gates.
The History of Keflavík International Airport
Keflavík International Airport is a relic from the ‘invasion of Iceland’ in World War Two, when Allied troops took over the island nation following the defeat of its colonial ruler, Denmark, at the hands of the Nazis. The British laid out a landing strip in the town of Garður, but considering Iceland’s incredibly strategic position in the middle of the Atlantic Ocean, one strip was not quite enough.
After taking control of the ‘occupation’, US troops constructed and opened two airfields for military purposes in 1942 and 1943. Though they returned the property after the war, the United States reclaimed it in 1951 after a controversial defence alliance with Iceland.
Though this pact, and the general joining of NATO in 1949, caused decades of national protest, the circumstances also allowed decades of development at Keflavík Airport.
The airport first started to separate civilian and military use in 1987, with the opening of the Leifur Eríksson Terminal. Named after the first European to settle the Americas, it would go on to handle all the guests coming to or leaving Iceland.
The arrangement that the US would provide Iceland’s defences continues to this day, but their permanent bases at Keflavík were left at the expiration of the treaty in 2006. The airport was thus moved into full control of Icelanders and has expanded as a civilian hub ever since.
Keflavík International Airport Today
Keflavík International is located on the tip of the Reykjanes Peninsula, Iceland’s south-easternmost region. The drive to the capital city of Reykjavík is only about forty-five minutes, and there is a Flybus service that continuously runs between the locations, day and night.
This service provides guests with the option to stop at the Blue Lagoon en route in either direction, the iconic health spa renowned for its healing azure waters. The lagoon sits between the airport and capital, refreshing guests after a long flight, or revitalising them in preparation for one.
The airport itself has all the modern amenities one would expect from a port that experiences so much traffic. It has restaurants, bars and cafés, banks and money transfers, car rental options available, and of course, many options for duty-free shopping.
Considering the price of and lack of availability of alcohol in Iceland, it is the best place to stock up on any tipple desired for your trip.
The main airlines that arrive at and depart from Keflavík are the two national carriers, the prestigious Icelandair and budget airline WOW. Over thirty different carriers have chartered flights to the port, however, which head to over ninety different destinations. This is only ever increasing, with new travel routes emerging as Iceland’s popularity continues to skyrocket.
Reynisdrangar are rock formations situated near the shore of Reynisfjara beach by the coastal village Vík í Mýrdalur on the South Coast of Iceland.
The formations are large and impending sea cliffs, made up of the rock type basalt, that serve as a vital part of the area’s allure as they shoot dramatically out of the ocean under the looming cliffs of Mt. Reynisfjall.
Dangerous Waves
The village of Vík only houses around 300 permanent inhabitants, but on a daily basis, travellers scouting the South Coast make their way there to visit what has been voted as one of the most beautiful non-tropical beaches in the world. The beach of Reynisfjara, however, can be highly dangerous if proper caution is not taken. As is evident from how the waves of the Atlantic Ocean crash upon Reynisdrangar, the currents here are strong, and sneak waves can easily carry anyone that’s standing too close out to sea. The beach is not for wading, but for admiring, and especially the mighty surf bursting on the base of these rocky cliffs.
Folklore
There is an Icelandic folk tale that explains the origin of the pillars’ eerie appearance. According to legend, a couple of trolls were busy dragging a stranded three-masted ship to shore when the sunlight hit them and turned them into pillars of rock for all eternity. In fact, numerous rock formations in Iceland carry with them tales of trolls or elves, and one has only to look at them to fathom why.
Surroundings & Wildlife
An alternative view of the bewitching cliffs and their surrounding sea can be enjoyed by venturing up Mt. Reynisfjall, by a road to the west of the village. The mountain furthermore functions as a puffin colony every summer, from April to September, meaning guests can enjoy the view in good company. Other birds can be seen gliding around the cliffs such as Arctic terns, fulmars and seagulls.
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.
The Capital Region refers to Reykjavík and its bordering towns. It holds well over half of the country’s population, in spite of taking up less than 1% of the country’s landmass.
The towns surrounding the capital are Kópavogur, Hafnafjörður, Garðabær, Mosfellsbær, Seltjarnarnes and Kjósarhreppur. Combined with Reykjavík city itself, these municipalities account for around 220,000 people.
Although each area is its own municipality, they cooperate on issues like transport, and by doing so, keep the region well connected.
The South Coast of Iceland is the country's most visited sightseeing route, along with the Golden Circle.
The famed South Coast shoreline stretches from the greater Reykjavík area and is dotted with natural wonders such as cascading waterfalls, volcanoes both active and dormant, black sand beaches and glacier lagoons.
Geography, Nature & Wildlife
Iceland is divided into eight geographical regions. Out of these, the Southern Region is the largest, as it spans over 24.000 square kilometres with its administrative centre in the municipality of Selfoss.
What is known as the South Coast embodies the shoreline of this particular region. The area consists of a lowland that is mostly composed of marshlands, bays and cultivated pastures that are met by a series of black beaches where the estuaries to the east and west of the district close off the coastal body.
Underneath the soil rests a vast lava field, known as Þjórsárhraun. Its edges reach several hundred metres offshore where the ocean waves crash upon them, thereby protecting the lowland from the invasion of the sea. This results in the South Coast being unusually lacking in the deep fjords that so distinctly characterise the rest of Iceland's shore line.
The region boasts vibrant bird life during all seasons. It is not only rich with both marshland birds and seabirds but also migrating birds such as the North Atlantic puffin. Some species stay throughout the harsh Icelandic winter, including the northern diver, the loom and various species of gulls and ducks.
Highlights of the South Coast
The South Coast offers an unprecedented array of natural wonders that draw thousands of visitors each day. When driving the route from Reykjavík City, the highlights in their correct order are:
These attractions count for but a fraction of what the South Coast has to offer. The vast sand plains of Sólheimasandur are home to a crashed DC-3 Plane Wreck, and close to Seljavellir by the Skógar Village there's Seljavallalaug, one of the oldest swimming pools in Iceland.
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.
Iceland has one main ring road: Route 1. This ring road goes all around the island and is 1332 km long (828 miles). The road connects the capital, Reykjavík, to the second biggest city in Iceland, Akureyri, in the north of the country. Other notable towns that are connected via the ring road are Borgarnes, Blönduós, Egilsstaðir, Höfn, Kirkjubæjarklaustur, Vík, Hella, Hvolsvöllur, Selfoss and Hveragerði.
A number of popular tourist attractions are also found by the ring road, such as Jökulsárlón glacier lagoon, Lake Mývatn and the waterfalls Seljalandsfoss, Skógafoss and Goðafoss.
The ring road consists mainly of paved two lanes road (one each direction). Some parts of the ring road are still unpaved however. In various places the road contains single lane bridges, especially in the east part of the country. The speed limit is 90km per hour on the paved section of the road (lower when it passes through towns), but 80km per hour on gravel.
The road was only completed in 1974, with the opening of Iceland's longest bridge, that crosses Skeiðará river in southeast Iceland. In 1998 a tunnel below the fjord Hvalfjörður shortened the drive around Iceland by about one hour (or 45km along a winding fjord). Hvalfjörður tunnels are the biggest tunnels in Iceland, 5,8 km and 165m below sea level. The ring road has another tunnel called Almannaskarð in the southeast by Höfn and by 2017 the Vaðlaheiðar tunnels should be open in north Iceland, shortening the distance between Akureyri and Mývatn.
Some sections of the ring road are original 1940's country roads, and a number of sharp curves, blind curves, blind summits as well as single lane bridges mean that people need to drive cautiously. In wintertime most of the ring road is kept open, with the exception of a short passage in the east part of the country that may be closed due to heavy snow (a detour is needed to travel from the north to the east during wintertime).
Guide to Iceland would advise people to drive cautiously on the ring road both in summer and wintertime, but also to explore other roads leading from it to multiple attractions.
