Highlights: 
The Blue Lagoon is a geothermal spa found on the Reykjanes Peninsula in southwest Iceland. It is the most popular attraction in Iceland drawing people from all across the world.
The Lagoon is just a fifteen-minute drive from Keflavík International Airport, or a thirty-minute drive from Reykjavík, located between the two. It is thus often visited straight after arrival to the country or right before departure.
There are few better ways to recharge after a long-flight or action-packed holiday.
History
The Blue Lagoon started as a pool of wastewater from the Svartsengi geothermal plant in 1976. The first person to bathe there was Valur Margeirsson in 1981. He was met with some resistance prior to taking the first dip as people thought he was mad for wanting to bath in a "blue mud pool". He and others soon began to notice the unusual but remarkable healing qualities of the azure waters.
Those with conditions such as psoriasis found the waters immediately soothing for their condition. News quickly spread, and by 1987, the first swimming facilities were officially opened.
Since then, the establishment has only grown, from an open pool with no surrounding buildings to a luxurious spa, research centre and hotel.
Today
The Blue Lagoon is considered to have such notable regenerative qualities because the water is rich in silica and sulphur. A research and development facility on site finds cures and remedies for skin ailments, and silica mud is available for free on the sides of the pool for guests to enjoy a facemask.
The temperature in the bathing and swimming area is very comfortable, averaging 37–39° C (98–102° F). The Blue Lagoon also boasts the LAVA Restaurant, the Blue Café and the Lagoon Spa: you can thus enjoy cocktails, health products, delicious meals and treatments such as massages without leaving the premises. Saunas, steam rooms and a small waterfall are also on site.
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 the water itself is opaque and vividly blue. Rising pillars of steam only add to the spa’s fantastic ambience.
Things to Note
The Blue Lagoon Spa is open throughout the year, and popular in every season. Due to the fact it has a maximum capacity for the comfort of its guests, it is essential that you book several months in advance to ensure your space. The vast majority of the time, you will be turned away at the door without a reservation.
More reserved guests might want to be aware that it is a requirement to shower naked in public before entering the lagoon, to ensure that the highest hygiene standards are maintained. Though uncomfortable for some, nudity has little taboo in Icelandic culture, so worry not; no-one’s looking.
Those who are travelling on a budget will note that the Blue Lagoon is quite pricey. There are other smaller spas and pools that can be entered for less, such as the Fontana Spa, Secret Lagoon, Mývatn Nature Baths and Krauma Spa. Of course, natural hot pools are free to enter.
For more information, you can read articles on the best pools in the country and the best natural hot springs.
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 other smaller geysers, Smiður and Litlí-Strokkur, that can be easily visited, as well as 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 Hvítá. 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, to which she and her sisters paved the first path, 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.
Thingvellir 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 it is located in 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-mans-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. For more natural beauty, you can visit the nearby Kerið crater lake.
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.
South Iceland is the most popular part of the country amongst travellers and contains some of Iceland’s most beautiful natural attractions.
Amongst these are the sites of the world famous Golden Circle, and the features of the South Coast, such as the beautiful Jökulsárlón glacier lagoon.
The south of Iceland can be roughly split into two areas, the lowlands in the west, and the east.
The South Icelandic lowlands
The South Icelandic lowlands stretch nearly 100 kilometres (over sixty miles) from Hellisheiði in the west to Eyjafjallajökull in the east. This region is flat and fertile farming land, and home to many Icelandic horses and sheep.
The whole area is geologically very young, formed during the last Ice Age by the lava flows from numerous volcanoes in the area. The lowlands are surrounded by volcanically active mountains, notably the aforementioned Eyjafjallajökull and Hekla.
The most notable features of the South Icelandic lowlands are the three on the Golden Circle, the country’s most popular sightseeing route.
These consist of the Geysir Geothermal Area, where geysers erupt and hot springs bubble, Gullfoss, a powerful two-stepped waterfall, and Þingvellir National Park, an oasis of forests and lava located between the tectonic plates.
The fissures and lava landscapes of this latter feature reveal the extent to which earthquakes and eruptions have shaped the region. The area is still very active; take, for example, the 1975 eruption in the Westman Islands that nearly destroyed the town and formed a new island.
It should be noted that Þingvellir is not just a site of natural, geological wonder. It was also the original site of the parliament Icelanders formed in 930 AD. This was a convenient place, considering the fertile lands of south Iceland meant that many settlers populated it.
Unlike most early Icelandic settlements, few of the communities formed in the south were based off fishing. The only town with a significant harbour in the south is Þorlákshöfn, where the ferry to the Westman Islands leaves.
Other towns in the lowlands are Selfoss, Hveragerði, Hella and Hvolsvöllur, all conveniently located by the Ring Road.
In terms of culture in the lowlands, it was once home to the ancient bishop seat of Skálholt. Also, Iceland's most famous saga, Njal's Saga, takes place in the region.
For sports, horse riding is popular, as is fishing for salmon and trout, hiking, snorkelling, sightseeing and river rafting.
Eastern South Iceland.
The areas south and east of Mýrdalsjökull, the glacier that covers the volcano Katla, are considered the eastern part of south Iceland. Glaciers, volcanoes and the Highlands dominate the view.
This landscape has also been shaped by volcanic eruptions, although these were much more recent, and thus the area looks dramatically different. Vast expanses of black sand stretch from the Highlands to the sea, part of several glacial outwash plains that flood during a volcanic eruption.
Some agriculture is found here, with farms nestled in the mountains, but because of the glacial floods, they are few and far between.
A few large glacial rivers flow through this area, creating incredible features such as Skógafoss and Seljalandsfoss. These are hardly the only sites in this part of the south worth seeing, however.
Sólheimajokull is a beautiful outlet glacier, a tongue of the greater Mýrdalsjökull, that you can hike on so long as you are with a guide. Skógar has a very interesting museum that discusses national traditions during Iceland’s development. One of Iceland’s most famous hiking routes, Fímmvörðuháls, cuts through the area.
Southwest of the village of Vík is one of Iceland’s most spectacular beaches, Reynisfjara. Near the promontory of Dýrholaey, and boasting incredible views of the Reynisdrangar sea stacks, it is a marvellous stretch of black sand.
Even further east is the Skaftafell preservation area, an area so beautiful it was once a national park in its own right. Today it is part of the greater Vatnajökull National Park, which covers parts of the south, east, north and much of the Highlands.
Just a little further from here is the incredible, world famous Jökulsárlón glacier lagoon, a deep lake that fills with icebergs. At the adjacent Diamond Beach, they wash upon the shore.
Reykjavík is the capital of Iceland and the northernmost capital of any sovereign state in the world.
Despite a small population (approximately 120,000, with just over 200,000 in the Greater Reykjavík area), it is a vibrant city that draws an ever increasing number of visitors every year. It is the financial, cultural and political centre of Iceland, and has a reputation of being one of the cleanest and safest cities in the world.
Geography
The city of Reykjavík is located in southwest Iceland by Faxaflói Bay. Throughout the ages, the landscape has been shaped by glaciers, earthquakes and volcanic eruptions and the area is geothermal; after all, its name translates to ‘Smoky Bay’.
Much of the current city area was subglacial during the Ice Age, with the glacier reaching as far as the Álftanes peninsula, while other areas lay under the sea. After the end of the Ice Age, the land rose as the glaciers drifted away, and it began to take on its present form.
The coastline of Reykjavík is set with peninsulas, coves, straits and islands, most notably the island of Viðey, and seabirds and whales frequent the shores. The mountain ring as seen from the shore is particularly beautiful.
Mount Esjan is the highest mountain in the vicinity of Reykjavík and the most distinctive feature of the coastline. This majestic summit is also highly popular amongst hikers and climbers. Other notable mountains that can be seen from the seaside are Akrafjall and Skarðsheiði.
On clear days, one may even see as far to the legendary Snæfellsjökull glacier, at the end of the Snæfellsnes peninsula.
The largest river to run through the city is Elliðaá in Elliðaárdalur valley, which is also one of Iceland’s best rivers for salmon fishing.
Transportation
There are no trains or trams in Iceland, but most people travel by car. The city also operates a bus system. There are two major harbours in town, the old harbour in the centre and Sundahöfn in the east.
The domestic Reykjavík Airport is located at Vatnsmýrin, not far from the city centre and close to the hill Öskjuhlíð and the restaurant, vantage point and exhibition centre Perlan. The international Keflavík Airport at Miðnesheiði heath then lies around 50 kilometres (31 miles) from the city.
Cars, jeeps and bicycles can be readily rented in the city and many organized tours are also being offered. It is, however, quite easy to walk between the major sites.
What to See & Do in Reykjavik
The local arts scene is strong in Iceland, with annual events and festivals, many of artists from which have hit the international stage.
Major events taking place in Reykjavík include Iceland Airwaves, Reykjavík Pride, RIFF (The Reykjavík International Film Festival), The Reykjavík Literature Festival, Culture Night, the Reykjavík Arts Festival, Food & Fun, the Reykjavík Fashion Festival and the Sónar music festival.
Amongst the famous people from Reykjavík are musicians like Björk Guðmundsdóttir and Sigur Rós, and writers Halldór Laxness (born on the main street, Laugavegur) and Arnaldur Indriðason.
Those eager to soak up the local culture should visit the city’s many museums, exhibitions and galleries, and check out live music at the cafés, bars, and concert venues dotted around. You could look at the programmes of what’s on at the Harpa music hall or the theatres, or else plan a few hours at the lighthouse at Grótta, the shopping street of Laugavegur, or the old harbour and the flea market.
You could even book a bird- and whale watching tour or a visit to Viðey island. There are a lot of things to do and the possibilities are endless.
Make sure to visit the public square of Austurvöllur, one of the city’s most popular gathering places, where you’ll also find the national parliament, the Alþingi, as well as the state church, a statue of independence hero Jón Sigurðsson, cafés, bars and restaurants.
Austurvöllur was central in the protests following the banking collapse of 2008, along with Lækjargata, home to the House of Government. You are also not likely to miss the great church of Hallgrímskirkja that towers over the city from the hill of Skólavörðuholt, from which you’ll get a great view of the city.
Try a walk by the city pond, Tjörnin, to greet the many birds that frequent the area and to visit the city hall, stationed by its banks. A beautiful park lies by the pond, ideal for a nice walk, and sometimes concerts get held there.
Further off is the campus of the University of Iceland, the Nordic house and the Vatnsmýrin wetland, a particularly pleasant place, but be mindful to not disturb the wildlife there by keeping to the pathways.
For a nice swim on a warm day, we particularly recommend Nauthólsvík beach, which is heated with geothermal water. Those who love a dip should also visit the Laugardalur valley, home to one of the city’s best swimming pools, which sits a short walk away from Ásmundarsafn gallery, a beautiful botanical garden and a domestic zoo.
A walk by the Ægissíða beach, with its old fishing sheds, in the west part of Reykjavík also holds a particular charm. From there, you can see all the way to president’s house at Bessastaðir, which is also a historical site in its own right, having been the educational centre of Iceland for centuries.
Another place that offers one of the city’s best views is Perlan, up on Öskjuhlíð hill. The hill itself is a popular place to spend a few hours, with over 176,000 trees and great opportunities for walking and cycling. Perlan also has and observation deck with great views, a café and an exhibition centre.
Furthermore, the city is a short drive from many of Iceland’s major attractions, most famously the Golden Circle and the Blue Lagoon. In close vicinity you’ll also find the Heiðmörk preservation area, a favourite local site of the people of Reykjavík, as well as the Blue Mountains, one of Iceland’s best skiing venues.
Finally, we’d like to stress that these are only some suggestions of the many things you might check out in Reykjavík. Whatever you choose to do, we hope you’ll be able to make the most of your visit and we wish you a pleasant stay in our capital.
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 their nesting 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 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 Vatnajokull
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 thousand 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 (northeast)
Jökulsá í Fljótsdal (northeast)
Jökulsá í Lóni (south)
Hornafjarðarfljót (south)
Jökulsá á Breiðamerkursandi (south)
Skeiðará (south)
Núpsvötn (south)
Hverfisfljót (south)
Skaftá (south)
Vatnajokull 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 Óðinn'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 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 Vatnajokull
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.
Vatnajokull and Jokulsarlon 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.
Snæfellsjökull is a glacier-capped volcano found on the tip of the Snæfellsnes Peninsula in west Iceland. It stands in a National Park of the same name, one of the only three National Parks in the country.
It stands at 1,446 metres (4,744 feet) tall, and on clear days, is visible across the bay from Reykjavík. The stratovolcano beneath Snæfellsjökull is 700,000-year-old.
The mountain is actually called 'Snæfell' (Snowy Mountain), though the 'jökull' (Glacier) is often added to help distinguish it from other mountains of the same name.
For the first time in recorded history, Snæfellsjökull had no snow or ice at its peak in August 2012, causing concern amongst locals that climate change is threatening the nature of the mountain.
History
Snæfellsjökull has several small villages surrounding it, including Hellissandur, Rif and Ólafsvík, all of which were some of the busiest commercial and fishing hubs in the country for much of the last millennium.
Fishing took off primarily in the 13th-Century, with fishing stations being built in all areas with easy access to the open ocean. The Snæfellsnes Peninsula was a notable centre of this industry, due to the fertile waters within Breiðafjörður bay.
One notable example would be the settlement of Dritvík; in spite of its minuscule size today, it once utilised around forty to sixty boats and employed up to six hundred people.
Fishing in the region declined during the 19th century due to change in Iceland’s industry and fish stocks, though it is still an important source of livelihood for those living on the Peninsula.
The Snæfellsjökull National Park was established in 2001, and tourism is rapidly changing the trade of the area.
In Folklore
Snæfellsjökull has, for centuries, been considered to be one of the world’s ancient power sites, a source of mysticism, energy and mystery for the peninsula’s superstitious population.
The feature takes a prominent role in Bárðar saga Snæfellsáss, a late 14th-century saga that tells the story of Bárður, half-human-half-troll, who became the 'guardian spirit of Snæfellsjökull'.
There are many rock formations on and around Snæfellsjökull that are said to be trolls petrified by sunlight, or else homes of the hidden people.
On November 5th, 1993, thousands of people came to Snæfellsjökull as some paranormal enthusiasts believed there would be an alien landing; CNN even showed up with a camera crew. Though the evening passed without a galactic invasion, the incident shows the strange significance of Snæfellsjökull to many.
In Literature
Snæfellsjökull serves as the entrance to a fantastical subterranean world in Jules Verne’s classic 1864 novel 'Journey to The Centre of The Earth.' Given its central place in the novel, Snæfellsjökull has become one of the most popular spots for visitors in Iceland and has inspired a wealth of writers, poets and artists.
Since 'Journey to The Centre of The Earth', Snæfellsjökull has appeared in the ‘Blind Birds’ trilogy by Czech science fiction writer Ludvík Souček (partially based on Jules’ work) and in ‘Under The Glacier’, a novel by Iceland’s only Nobel laureate, Halldór Laxness.
Nearby Attractions
Along with the glacier, attractions on the Snæfellsnes Peninsula include the two nearby basalt cliffs called Lóndrangar and the many fascinating lava formations at the beautiful Djúpalónssandur beach, such as the arch rock Gatklettur.
At Djúpalónssandur, one can also test their muscle as historic sailors once did with the four 'strength' stones, Amlóði ('Useless'), Hálfdrættingur ('Weakling'), Hálfsterkur ('Half Strength') and Fullsterkur ('Full Strength').
In the area, one can also explore the Saxhóll volcano crater and 'the singing cave' Sönghellir, which is named after the loud echoes inside.
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, it 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 miles) 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.
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 country's 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 pathway that stretches all the way around it. The cliffs behind the falls have 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 the 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.
Geysir is a famous hot spring in the geothermal area of Haukadalur Valley, found in south-west 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 a few 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“ Þorgilsson, 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.
Gullfoss (translated to ‘Golden Falls’) is one of Iceland’s most iconic and beloved waterfalls, found in the Hvítá river canyon in south-west Iceland.
The water in Hvítá river travels from the glacier Langjökull, before cascading 32 meters (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 became 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.
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 route, 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, Alþingi, 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.
Hraunfossar ('Lava Falls' in English) in Borgarfjörður district is a series of beautiful waterfalls formed by rivulets streaming out of the Hallmundarhraun lava field. It is located in West Iceland near another waterfall called Barnafoss.
Geography and Surroundings of Hraunfossar
The lava field that Hraunfossar trickles through flowed from an eruption of one of the volcanoes lying under the nearby glacier of Langjökull, the second largest ice-cap in Iceland. The waterfalls pour into the Hvítá river from ledges of less porous rock in the lava.
Because the area around Hraunfossar used to be the site of constant eruptions, the lava fields are known for their hidden caves. The country's longest cave, Víðgelmir, can be found near the waterfall. This amazing feature is 1,595 metres long (5,200 feet), up to 15.8 metres high (52 feet) and 16.5 metres wide (54 feet).
Its geological history may be fascinating, being just a thousand years old, though its human history stirs just as much intrigue as the lava field was once home to bandits and, according to folklore it is the home of trolls.
Another major site near Hraunfossar is an incredibly short walk away, and though also a waterfall, could not be more different. Barnafoss surges down a narrow, rocky valley with ferocious power, foaming and churning quite spectacularly. According to legend, however, the force of these rapids led to tragedy.
It was said that an old stone bridge once went over the falls, and two boys at a nearby farm, bored at home, attempted to cross it to catch up with their parents at church. However, they felt dizzy due to its height, fell, and drowned.
The legend ends in two different ways, with the least interesting saying the mother in grief simply ordered the bridge destroyed. Other tales say that she cursed the bridge using an Icelandic rune so that any who crossed would meet the same fate as her sons.
In this version, the bridge and curse were later broken by an earthquake.
The story led the waterfall its name; it translates to ‘Children’s Falls’.
Settlements near Hraunfossar
The nearest settlement of significance to Hraunfossar is Reykholt.
This tiny village has a huge history, being home to the legendary writer, chieftain, lawspeaker and poet Snorri Sturluson. Without Snorri, huge amounts of Icelandic, Nordic and even British history would be unknown.
He alone at the time catalogued a history of Norwegian kings and their relations with other monarchs through the work Heimskringla, as well as the Norse mythological beliefs through Prose Edda. It is also believed that Snorri first wrote many of the sagas still read today.
Reykholt has a centre dedicated to Snorri called Snorrastofa, which discusses his fascinating life as much as his works. Working during the times of Iceland’s tumultuous civil war as a chieftain, lawspeaker and spokesman of the Norwegian king, who had ambitions to take the country, it is a story with as much politics, betrayal, blood and sexual impropriety as Game of Thrones.
Hraunfossar is also reasonably close to Borgarnes, another town with a long history. Here, visitors can see the Settlement Centre with its two exhibitions on Iceland’s past, one is on the first people to reach this island over a thousand years ago, and the other is on Iceland’s most famous saga, Egil’s Saga.
Deildartunguhver is a hot spring located in Reykholtsdalur, a district of west Iceland. Deildartunguhver is the highest flowing hot spring in Europe and is widely known for its rapid flow rate of 180 litres (380 pints) per second.
Geothermal activity at Deildartunguhver
Reykholtsdalur is one of Iceland’s most popular places to see hot springs, along with the Geysir Geothermal Area, the Highlands, the Reykjanes Peninsula, Reykjadalur Valley and Námaskarð Pass. While each of these areas have their appeal, at no other does the water rise with such ferocity.
The water at Deildartunguhver hot spring emerges at a constant 97 degrees Celsius (207 degrees Fahrenheit), making it incredibly dangerous for those who venture too close. Thankfully, there are a number of wooden walkways and observation points that lead you around the hot springs without putting you at any risk.
Due to the sheer energy bubbling under Deildartunguhver, much of the water is used for heating Icelandic homes. One pipe travels 34 kilometres (21 miles) to Borgarnes, whilst another travels 64 kilometres (40 miles) to Akranes.
This means that if you’ve taken a shower or bath within a 64-kilometre radius of Deildartunguhver, you will have touched the water from the hot spring.
All Icelandic hot water comes from hot springs such as this, except in some parts of the Westfjords which are now geologically much older than the rest of the country, and thus less active.
This is a fantastic example of how Icelanders efficiently use the geothermal energy provided and is one of the major reasons as to why Iceland has such an excellent reputation for green energy.
Points of Interest at Deildartunguhver
Whilst in the area, many visitors choose to make a stop at Krauma Geothermal Bath & Spa, a fantastic and relaxing complex that makes for a cheaper, more isolated alternative to the Blue Lagoon.
Visitors to Kraua will experience the hot water of Deildartunguhver blended perfectly with glacial water from Iceland’s smallest ice cap, Ok (which rhymes with ‘talk’), creating the perfect bathing temperature.
Krauma has a total of six pools, a relaxation room and two steam baths.
Visitors to Deildartunguhver with an interest in botany will also be able to check out the Blechnum Spicant, aka; “deer fern”, a type of plant that grows nowhere else in Iceland.
Surroundings of Deildartunguhver
Deildartunguhver is located in west Iceland. The two most notable points of interest nearby are two waterfalls, Hraunfossar and Barnafoss.
Hraunfossar, or the ‘Lava Falls’, is, in fact, a series of tiny cascades that trickle through an old lava field. Barnafoss, or ‘the Children’s Falls’, is a more powerful rapid, steeped in a dark legend.
Deildartunghver is also near Víðgelmir, the longest lava cave in the country, trailing for 1,595 metres (5,200 feet) beneath the surface of the earth.
The most significant settlement near Deildartunghver is Reykholt, a beautiful village with a fascinating history. This settlement was once home to Snorri Sturluson, a historian, writer, chieftain and poet without whom we would know very little of the Nordic mythology, folklore and history at the time.
His works, and life--full of politics, betrayal, affairs and war--can be learnt about in the town at the Snorrastofa Centre.
Katla is one of Iceland’s most explosive volcanoes, located underneath Iceland’s fourth largest ice cap, Mýrdalsjökull. Since settlement, it has erupted, on average, once every fifty years, with the last eruption in 1918. It is long overdue.
Katla is connected to Eyjafjallajökull, which erupted in 2010 and caused widespread disruption to air traffic, as well as changes in climate. Usually, Katla is triggered by an eruption here, usually going off within the decade afterwards. Kristín Jónsdóttir said in 2016 that it was ‘a matter of when, not if’ Iceland would face the wrath of Katla once more.
Katla means ‘Kettle’ in Icelandic, and many women are named after the volcano with it being one of the more popular girl’s names.
Geography and geology of Katla
Katla is located on Iceland’s South Coast, north of the village of Vík. Its peak is 1,512 metres (4,961 feet) above sea level, and its crater is 10 kilometres (6.2 miles) wide. The ice of Mýrdalsjökull is, 700 metres (2,300 feet) thick at certain points over it.
Because of this huge amount of ice, some smaller eruptions do not even break the surface. However, even these can be very dangerous, as they can still cause unexpected floods as the melted water seeps from under the glacier. One only needs to see the black sand desert of Sólheimasandur to see how much life can thrive in the glacial outwash plain under Katla.
Because of the floods caused by Katla, Iceland’s South Coast has very few settlements. Floods such as these have wiped out entire villages before.
The floods following the 1918 eruption were particularly powerful, clearing away huge swathes of land. The lava that followed, however, was so voluminous that it extended the southern coastline over five kilometres (eight miles) out to sea.
Though Eyjafjallajökull and Katla have a relationship of exploding in quick succession, they are part of different volcanic systems. Katla’s system has an area of 595 square kilometres (230 square miles), and is connected to the Eldgjá canyon.
Tours on Katla
Katla is beneath the peak of Mýrdalsjökull, which is surrounded by outlet glaciers, making tours on it few and far between - after all, it is very difficult to reach. Some helicopter tours, however, will make a landing here. Some super jeep tours also take the bumpy but beautiful path to the top.
It should be noted that there are ice caves above Katla, which are accessible for longer throughout the year than the ice caves at Vatnajökull. These ones, however, do not have blue ice.
Where to see Katla
Katla can be seen from the Ring Road, which encircles Iceland, by travelling along the South Coast, so long as the weather is clear. It will be visible for much of the drive, which also takes you passed features such as the waterfall Seljalandsfoss and the black sand beach of Reynisfjara.
It can also be viewed when visiting one of the glacier tongues of Mýrdalsjökull, such as Sólheimajökull, the most popular outlet for glacier hiking.
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. Strokkur erupts more regularly than Geysir ever did, blasting water to heights of around fifteen to twenty metres every five to ten minutes, although it is known to reach up to forty metres.
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).
Snæfellsnes is a large peninsula extending from West Iceland, often nicknamed ‘Iceland in Miniature’ due to its wealth and diversity of natural features found there.
Home to the Snæfellsjökull National Park, at the centre of which is a subglacial volcano that towers over the scenery, this peninsula is home to waterfalls, rock formations, beautiful beaches, historic villages, and an intricate folklore.
In particularly clear weather, the Snæfellsnes Peninsula can sometimes be seen from Reykjavík, making views across the water from the capital of Iceland particularly beautiful. Those with an extended stay in Iceland are recommended to look into spending at least a day here.
Natural Sites of Snaefellsnes
The peninsula stretches 90 kilometres (56 miles) from West Iceland, between the Reykjanes Peninsula to the south and Westfjords to the north. A mountain range runs along it, consisting of both active and dormant volcanoes, culminating at the magnificent, ice-capped Snæfellsjökull volcano.
Starting along the south side of the Snæfellsnes Peninsula, you will first come to the Eldborg crater, which can be scaled for some incredible views, and the Gerðuberg basalt cliffs, where hundreds of hexagonal basalt columns are arranged with geometric precision. You will then start hugging the coast, where animal-lovers can find the Ytri-Tunga beach and its year-round seal colony.
The next site of particular natural beauty is the Rauðfeldsgjá Gorge, a cleft in a huge cliff face that it is possible to climb into. A stream runs through here, so those who want to plumb its depths will get wet. Those with decent clothing, sturdy shoes and reasonable fitness, however, will be able to get quite far.
After Rauðfeldsgjá, you will come to the mighty basalt plugs of Lóndrangar. All that remains of what was once a massive crater, these two enormous pillars are not only awe-inspiring in their scale, but home to thousands of nesting seabirds.
You will then enter Snæfellsjökull National Park, which, in spite of being the smallest of the country’s three national parks, is pregnant with destinations worth visiting.
The most historic of these is Djúpalónssandur beach. Comprised of black, volcanic sands, it is best-known for the four lifting stones that remain on the beach from a bygone age. Fishermen would use these stones to mark their strength, and gage their suitability to working on the dangerous waves.
Within the National Park are also two lava caves that can be entered in summer. Sönghellir is renowned for the musical qualities of its echoes, whereas Vatnshellir is favoured for its easy access and vivid colouration. There is a small entry fee to the latter and you cannot enter it without a guide.
Of course, however, the highlight of this part of the Peninsula is no doubt Snæfellsjökull itself. Even if you are not ascending it on a glacier hiking tour, it is worth stopping by to marvel at.
This is particularly the case for literature enthusiasts. The adventure in the Jules Verne novel ‘A Journey to the Centre of the Earth’ begins here, and it is the backdrop to the lesser-known novel ‘Under the Glacier’, by Nobel-Prize winning Icelander, Halldór Laxness.
On the north side of the peninsula is the haunting Berserkjahraun lava field, near the town of Bjarnarhöfn, the history of which weaves deception and murder. Most notable on this stretch, however, is the mountain Kirkjufell, often described as the most photographed mountain in Iceland, and known as "the mountain shaped like an arrowhead" from the popular HBO series, Game of Thrones.
Cultural Sites of Snaefellsnes
There are a few small and beautiful villages dotted across the peninsula, the majority of which are on the northern side, where the fishing is better. Most notable are Arnarstapi, Hellnar, Búðir, Hellissandur, Ólafsvík, Grundarfjörður and Stykkishólmur.
The last of these is highly popular for travellers, featuring a volcano museum and a ferry that takes you across the fascinating Breiðafjörður bay to the south border of the Westfjords with a stop at the remote island of Flatey.
Other museums of note are the Maritime Museum at Hellissandur, the regional museum at Ólafsvík, and, last but not least, the shark museum at Bjarnarhöfn, where you can taste the Icelandic ‘delicacy’, hákarl, or fermented shark.
Reykjanes is a peninsula in south-west Iceland, characterised by immense lava fields, volcanoes and heightened geothermal activity.
Volcanic & Geothermal Activity
The Reykjanes Peninsula runs along the Mid-Atlantic Rift, where the Eurasian and the North American tectonic plates are drifting apart. Due to this geological setting, the whole peninsula is extremely volcanically active, covered with lava fields, and eruptions and earthquakes are very common here.
During the Middle Ages, many eruptions occurred in Reykjanes, but no eruptions have been recorded here for the last 500 years. This is simply a period of dormancy, however; they could start again at any time.
Earthquakes are still common. In 2001, one occurred beneath the lake Kleifarvatn and drained it to the extent that it lost 25 per cent of its surface area. Since then, hot springs have been bubbling beneath its surface.
The main geothermal areas of Reykjanes, however, 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 water that gushes 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 eighty thousand seabirds. While puffins are not found here, it is an excellent place to spot cormorants, fulmar, and other such species.
North of Krýsuvíkurbjarg is the aforementioned Kleifarvatn, the largest lake on the peninsula and one of the deepest in Iceland. On the centre of the peninsula is lake Djúpavatn, a popular fishing destination.
Reykjanes is hammered by some of the most breath-taking breaker waves in the world. A short drive from Krýsuvík is Selvogur, where one can witness mighty waves shattering against the rocks. On Reykjanestá, the southwest tip of the peninsula, the waves are known to reach heights of thirty metres (nearly one hundred feet).
Because of this, coastal erosion is constantly ongoing at Reykjanes, and if it were not for the eruptions, it would either be much narrower or simply lost to the seas.
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. This is the port of arrival for the vast majority of travellers coming to Iceland.
The World-Famous Spa
On the southern tip of the peninsula is the Blue Lagoon geothermal spa, an ideal place for relaxing and bathing and one of the most-visited attractions in Iceland.
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 spot on which to take guided glacier walks, competing nationally for popularity only with Svínafellsjökull in the south-east.
Geography of Solheimajokull
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 Mýrdalsjökull, however, without a clear distinction between the two, it appears much bigger.
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.
The nearby Eyjafjallajökull erupted in 2010 causing widespread havoc at European airports. Throughout history, eruptions in Eyjafjallajökull mean that Katla will also erupt, and so the volcano is due to go off soon. However, volcanoes and all seismic activity in Iceland is highly monitored, meaning that it is perfectly safe to travel around the area and even take an ice cave tour in the glacier above.
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.
There are also 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 á Sólheimasandi. This river runs through a glacial outwash plain - otherwise known as a black-sand-desert - of Sólheimasandur to the nearby ocean.
Tours on Solheimajokull
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.
Mýrdalsjökull is a glacier in the south of the Icelandic highlands. It is the country's fourth largest ice cap, covering nearly 600 square kilometres (232 square miles), and its highest peak is almost 1500 meters tall. It is most well-known for sitting atop the notorious and explosive volcano, Katla.
Mýrdalsjökull is visible from Route 1 on the South Coast, sitting to the north of the village of Vík. It is visited on some snowmobiling, ice caving and helicopter tours, and one of its glacial outlets, Sólheimajökull, is the most popular place in the country for ice-climbing and glacier hiking.
Eruptions beneath Myrdalsjokull
Since 2010, the world has known of the volcano beneath Eyjafjallajökull; after all, it halted European air travel for over a week and stumped news readers everywhere. Few, however, are aware of the much larger volcano right beside it.
Mýrdalsjökull conceals Katla, one of the country’s most active volcanoes, having erupted, on average, once every fifty years since 930 AD. Because of the glacier above it, these eruptions tend to cause enormous ash clouds. It is these ash clouds that lead to flights being grounded, crops and livestock poisoned, and have the potential to change the world’s climate.
The last major eruption beneath Katla was in 1918, in which such huge lahar floods occurred that the southern coastline was extended five kilometres outwards. This area is also very susceptible to glacial floods, or 'jökulhlaup', during eruptions, even when the lava does not break through the surface of the ice. These are as dangerous as the lava itself, having wiped out whole Icelandic villages before.
Historically, the area was little settled for this reason.
Katla is connected to the same volcanic system as Eyjafjallajökull and usually erupts violently a few years after Eyjafjallajökull does. As the ex-president, Ólafur Ragnar Grímsson said in 2010:
‘The time for Katla to erupt is coming close… it is high time for European governments and airline authorities all over Europe and the world to start planning for the eventual Katla eruption’
So it is currently several years overdue. Katla is monitored heavily, and roads around it closed when seismic activity increases. All road closures around Iceland can be found on Road and Coastal Administration's website.
Tours on Myrdalsjokull
While there are no eruptions immediately imminent, tours continue to run onMýrdalsjökull, allowing visitors to enjoy the glacier. It is, for example, possible to snowmobile across its surface throughout the year and take ice caving tours beneath it throughout the year, with departures from both Reykjavík and Vík.
Considering the ice caves under Vatnajökull glacier are usually only accessible from November to March, this provides a wider window of opportunity for travellers to Iceland outside of the depths of winter. It should be noted that the caves in Mýrdalsjökull do not have the same blue ice, however.
Tours around Myrdalsjokull
Mýrdalsjökull can be seen on all South Coast tours that reach Vík and beyond in clear weather. It can also be seen from above on helicopter tours that depart from Reykjavík.
The best perspectives of the glacier, however, can be found on the popular Fimmvörðuháls hiking trail, which goes between Eyjafjallajökull and Mýrdalsjökull. Part of this hike can be done in a day, or you can take the complete route from Þórsmörk to Skógar on a three-day trek
Skaftafell is a nature reserve located in Vatnajökull National Park in the south-east of Iceland. It is an oasis of this nation’s diverse landscapes and features, so beautiful it was once a national park in its own right.
Nature of Skaftafell
Skaftafell is notable for its rich flora, growing between sands and glaciers, and for its amazing, contrasting scenery. Visitors will find a wealth of natural attractions, from cascading waterfalls to glacier lagoons, geological formations to black sand deserts.
The rugged region is known for its fantastic photo opportunities, with many awe-inspiring panoramic views.
Like many areas along the South Coast of Iceland, Skaftafell Nature Reserve is known for its glorious hiking trails, often called a ‘hiking paradise’. Unlike in the Highlands, where hikes tend to go on for multiple days, here there are far shorter. There are easy treks that lead to diverse sites such as the waterfall Svartifoss which is surrounded by bizarre and beautiful basalt columns, as well as to glaciers such as Svínafellsjökull.
With a qualified guide, it is 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.
The nature reserve 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.
Getting to Skaftafell
Just off the Ring Road in the south-east of the country, it takes approximately four hours to reach Skaftafell from Reykjavík. The South Coast, however, is one of the regions most popular sightseeing routes, so the journey usually takes much longer, as visitors will want to make several stops along the way.
Examples of the beautiful natural features found en route to Skaftafell include the waterfalls Seljalandsfoss and Skógafoss, the glaciers Mýrdalsjökull and Eyjafjallajökull, the black sand deserts of Sólheimasandur and Skeiðarársandur, as well as the dramatic coastal rock formations at Dyrhólaey and Reynisdrangar. The villages of Vík and Kirkjubæjarklaustur are also along Route 1 if you need to stop and refuel on refreshments.
Those who have made it all the way to Skaftafell will want to be sure to check out the Jökulsárlón glacier lagoon, a giant lake filled with enormous icebergs breaking from a glacial tongue, and slowly drifting to sea. At the nearby Diamond Beach you can watch them wash upon the shore, and in both the sea and lagoon are many seals which can routinely be spotted.
Skaftafell Visitor Center
You will find a Visitors Centre at Skaftafell which acts 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.
There is also a hotel at Skaftafell, though it tends to book up very early. Luckily, the south-east is dotted with hotels, cabins and cottages in which you can stay, and the area is not far from the settlements of Höfn or Kirkjubæklaustur.
Silfra is a fissure filled with fresh spring water within Þingvellir National Park, and one of the country’s most cherished wonders. Snorkelling and diving in its crystal-clear waters is an experience that is both thrilling and relaxing, and it is now considered to be one of the top five dive sites in the world. It takes around an hour to reach Silfra from Reykjavík.
Geography of Silfra
Silfra fissure opened in 1789, due to the movements of the tectonic plates that frame Þingvellir National Park. The North American and Eurasian plates, which run all the way through Iceland, separate at about 2 centimetres per year, and as they do, they tear open fissures in the land between them.
Some of the ravines fill with water travelling underground through the porous lava fields in the area, originating from Langjökull glacier about 60 kilometres north. It can take the water up to a century to reach Silfra and this long filtration process results in the water being both extremely clear and drinkable.
Because the water travels underground, it maintains a constant temperature of two to three degrees Celsius and does not freeze over immediately at the source of the spring. Snorkelling and diving tours are thus open throughout the year.
The clarity of the water is what draws most visitors. The visibility can extend to over 100 metres, allowing you to see the canyon walls and bottom like you are floating over a great cathedral.
The last colour that water absorbs is blue, which means that when you look forward in Silfra, it is as if you are looking into an ethereal, vivid, azure world. The clarity also means that sun-rays refract through the surface of the water, creating rainbows on Silfra’s bed when the weather allows.
Snorkelling in Silfra
Snorkelling in Silfra fissure is a highly enjoyable activity, but you must meet some prerequisites to be able to join. These are as follows:
- You must be able to swim
- You must be over 16
- You must be in good physical health
- You must be at least 145 centimetres and 45 kilograms
- If you are over sixty, you will need a medical waiver
- If you are over forty-five with a history of heavy alcohol use and pipe smoking, you will also need a waiver
The most common option for snorkelling is to conduct it in a drysuit. Drysuits work with a fluffy undersuit to keep your body free from water and insulated against the cold, making the task of swimming through the near-freezing temperature more than achievable.
While drysuit snorkelling is the most comfortable and popular option, a few tours allow you to go through Silfra wearing a wetsuit. Wetsuits, made of neoprene, allow water to surround your body in a thin layer, that your body then heats up and uses to protect you. Though they grant you more flexibility, they are not so warm, so this should be done by the daring; you will also need to be at least 50 kilograms to snorkel in a wetsuit.
In all tours, you wear neoprene on your head and hands to allow for better mobility, a mask and snorkel, and a pair of fins, all of which are provided on site. The course of Silfra takes approximately forty minutes, and there is a gentle current throughout, meaning it requires minimal energy to traverse.
Diving in Silfra
Diving through Silfra gives an extra dimension to its beauty, as you will be able to look up and see the sun glistening upon the surface as you cruise through the crystal clear waters. However, considering the risks associated with diving in cold water and cumbersome equipment, all who partake must meet all the requirements above, as well as one of the following:
- You must be a qualified diver with a certification in a drysuit speciality, OR
- You must be a qualified diver with at least 10 logged dives in a drysuit conducted over the past two years, signed by an instructor or divemaster.
Sólheimasandur is a vast area of sand and gravel along the South Coast of Iceland, between the cliffs of the interior and the modern shoreline. It was built up by immense glacier bursts sweeping from the mountains to the shore.
Geography of Sólheimasandur
Sólheimasandur is a glacial outwash plain, meaning when that when eruptions happen under the nearby glacier, Mýrdalsjökull, the floodwater rushes across this land for the sea.
A glacial flood, otherwise called Jökulhlaup (one of two words taken from Icelandic in the English language, the other being geyser) is perhaps the most dangerous immediate element of an Icelandic eruption. While individuals have been killed by lava flows and bombs, many more have lost their lives to the water.
For this reason, Sólheimasandur has no significant settlements, all the way from the village of Vík í Mýrdal to Kirkjubæjarklaustur. The whole area is vulnerable to glacial floods, which are still notoriously unpredictable to modern science.
This is especially the case considering that the volcano beneath Mýrdalsjökull, Katla, is Iceland’s most active volcano, which carries a reputation for violently erupting, seemingly at random.
Even if these eruptions do not break the surface of the ice, they can still cause devastating floods. In fact, these can even be more dangerous, as these eruptions are often not detected..
If Katla is showing signs of waking, then the Ring Road going south across Sólheimasandur is often closed.
In spite of its dark reputation, Sólheimasandur is a place of ethereal and haunting beauty. Entirely flat, composed of black sands, it is often compared to a lunar landscape, or else some kind fantastical desert. The views of Mýrdalsjökull, Vatnajökull, the Highlands and the South Coast are also magnificent in clear weather.
Sólheimasandur is easy to reach, laying on the Ring Road that encircles the country.
The DC-3 Plane Wreckage
Wikimedia, Creative Commons, Photo Credit: Sekeri
One of the most impressive sights on Sólheimasandur is the DC-3 plane wreckage. Lying abandoned in the sand, a deteriorating skeleton, with nothing but endless black sand surrounding it, it makes an eerie destination even more ominous.
It is a US Navy plane, that was flying across the area in 1973; until recently the US had a NATO base at Keflavík, as Iceland has no armed forces of its own. It seemed to run out of fuel - although it was later discovered that the pilot had, in fact, switched to the wrong fuel tank - and had to make an emergency landing.
Thankfully, no one was killed or injured, although the plane was far too damaged to be repaired.
Because there were no deaths or injuries, there is nothing tasteless about taking photos with the plane. In fact, it a popular addition to many South Coast tours. Because the wreckage is not expected to remain there for long - considering the regular glacial floods that rush through the area - it is fine to touch it. It is not recommended that you climb on it, however, for safety reasons.
To reach the plane requires a short walk across Sólheimasandur.
Höfn is an Icelandic fishing town of just over two thousand people in southeast Iceland. It is the most significant settlement on Route 1 between the village of Kirkjubæjarklaustur in the south and Egilsstaðir in the east.
Geography of Höfn
Höfn means ‘harbour,’ as the town is located in one of the few natural harbours of Iceland’s South Coast; unlike the rest of the country, this stretch is beachy and flat, and thus there are hardly any small coastal villages when compared to places such as the Snæfellsnes Peninsula.
The town is right at the tip of its own peninsula, which is easy to reach throughout the year. It sits at the base of Route 99, which detours off from Route 1. It is surrounded on three sides by the ocean, which has been known to freeze over in extreme conditions.
The town can also be reached by plane in good weather, as it is one of the few locations in the country with a domestic airport.
The largest glacier in Europe, Vatnajökull, which sits in a National Park of the same name, is within clear view of Höfn.
Nearby Locations to Höfn
Höfn is most often visited by those driving the full Ring Road of Iceland, as a place to stay just before or after visiting the South Coast or East Fjords.
It is also visited independently, however, by those seeking to spend enough time near the sites of southeast Iceland, most notably Vatnajökull National Park, the Jökulsárlón Glacier Lagoon, the Diamond Beach and Vestrahorn Mountain.
All of these sites are incredible. Vatnajökull, for example, is incredibly diverse, boasting a huge array of different sites to marvel over. In its southwestern corner, for example, it is home to the Skaftafell Nature Reserve, an oasis of unbelievable scenery, whereas to its west sits the mighty mountain Snæfell, renowned for its wildlife such as pink-footed geese and reindeer.
The Jökulsárlón Glacier Lagoon has recently been enveloped into the National Park, but warrants its own discussion. Out of all the sites listed, it is here where most visitors to Höfn want to spend the bulk of their time. This lagoon is, in fact, Iceland’s deepest lake, and renowned for being full of great icebergs throughout the year.
These bergs snap off of a tongue of Vatnajökull glacier, before slowly cruising through the waters towards the ocean. As they travel, they often become resting spots for some of the many seals who live in and around the lagoon.
The site is marvellous to behold, with a particular appeal for landscape photographers. Visitors, however, should not spend all their time in the lagoon. By following the channel from Jökulsárlón to the ocean, you will come onto the Diamond Beach, where these icebergs wash up on the shore and glisten against the black sands.
A final site in southeast Iceland, closer to Höfn than those previously listed, is Mount Vestrahorn. This jagged peak is ominous and dramatic, with two sharp peaks that have created the nickname ‘the Batman Mountain.’ Another favourite amongst photographers, it’s distinct silhouette and colouration make it the perfect subject regardless of the weather.
Culture at Höfn
Like many of Iceland’s small, coastal towns, Höfn has a surprising amount of culture. Its cuisine is particularly notable, with the celebration of it coming to a head at the annual Lobster Festival, held every July. This comes as little surprise, considering the town’s long history as an important fishing port.
Höfn also has several art museums where visitors can admire local handicrafts, although it should be noted, in spite of conflicting evidence on the internet, that the Höfn Glacier Museum is now closed.
Barnafoss is a rapid waterfall in West Iceland, just a short walk away from the serene Hraunfossar falls. It is best known for its dark history in folklore, and for how much it contrasts with its neighbour.
Folklore of Barnafoss
Barnafoss translates to ‘the Children’s Falls’ because of a legend long told about it. Back in Iceland’s early days, it was said that a family with two boys lived at the nearby farm of Hraunsás. The parents left home for church one morning, ordering the young ones to remain at home, but with nothing to entertain them, the children soon decided to follow.
They knew a shortcut to the church: a stone bridge, arching over the nearby rapid waterfall, that back then would have had a different name. They started to cross it, but found the heights and surging water below dizzying. In a tragic turn of events, neither boy made it across the bridge, and both fell to their deaths.
Though both parents were grief-stricken, the mother veered towards insanity. Some versions of the tale end with her demanding the bridge be torn down. Others say she turned to witchcraft, placing a rune on the bridge that made any who crossed it plummet to their deaths just like her beloved sons.
If the latter version is true, her spell was broken when an earthquake shattered the passage.
While Iceland’s tales of magic were, of course, exaggerated as they were passed down in oral tradition, it is very possible that this story is true; Barnafoss would kill whoever fell into it in all likelihood, and many Icelanders scratched runes to spread curses to their neighbours and rivals.
It is, of course, equally possible that like many Icelandic tales, it was simply created as a way to ensure that young children respected their parents, and feared the country’s unpredictable nature.
Surroundings of Barnafoss
Barnafoss is a magical site in and of itself, twisting, turning, foaming and churning as it races down a narrow valley, from which you can view it from above. It is even more fantastical, however, due to its contrast with Hraunfossar.
Rather than being a narrow rapids, Hraunfossar is a wide series of trickling waterfalls, flowing from a plateau of lava rock. Seeing the drama of one, followed by the peace of the other, is an excellent example of how Iceland’s scenery is ever-changing, and completely different spectacles can exist within mere metres of each other.
Other sites of the west near Barnafoss include the highest-flowing hot spring in Europe, Deildartunguhver, which is fascinating to admire but impossible to bathe in due to its extreme heat.
There are also the settlements of Reykholt and Borgarnes, both of which should be visited by those passionate about Icelandic history and culture. Reykholt hosts the Snorrastofa Exhibition, where you can learn about the village’s most famous resident, Snorri Sturluson. Snorri wrote many of the Icelandic texts that reveal huge amounts about Nordic kings, Norse mythology, and Icelandic folklore.
Borgarnes, meanwhile, has the Settlement Centre, where guests can learn about the brave first arrivals to this stark new home, and one of the country’s most famous sagas, Egil’s Saga.
The mighty Langjökull, the ‘Long Glacier’, is the second-largest glacier in Iceland, at 935 square kilometres (361 square miles). For jeep and snowmobile trips, Langjökull is the most popular glacier in Iceland, and skiing and hiking here is possible as well.
Highland tracks
Langjökull is located in the Highlands, and two main highland tracks, connecting the north and the south of Iceland, lie alongside it.
The Kaldidalur road stretches from Þingvellir National Park northwards to Húsafell. The Kjalvegur road, meanwhile lies east of Langjökull and west of Hofsjökull glacier, starting near the famous Gullfoss waterfall to the south, and passing through the beautiful Hveravellir geothermal area to the north.
The landscape of Langjokull
Langjökull is about 50 kilometres (31 miles) long and up to 20 kilometres (12 miles) wide, and the ice is around 580 metres (1,903 feet) deep at its thickest. The glacier reaches its highest point in its northernmost part, which is called Baldjökull, rising around 1,450 metres (4,757 feet) above sea level.
The glacier lies over a massif of hyaloclastite mountains. The tops of these mountains can be seen in certain places on the glacier. It also conceals at least two active volcanic systems, the calderas of which are visible from the air.
The best known of these systems fuels the geothermal area of Hveravellir, east of Baldjökull. Also in the east lies the Kjalhraun lava field, which formed about 7800 years ago.
To the northwest of the glacier is another system that produced the vast Hallmundarhraun lava field, through which the Hvítá river runs in the direction of Gullfoss waterfall. Also in the area is Iceland‘s longest lava cave, the fascinating Surtshellir.
Southwest of Langjökull is the Presthnúkur lava field, fissures of which creep under the ice. South of the glacier is the Lambahraun lava field and even further south lies the Skjaldbreiðarhraun lava field and the Skjaldbreiður shield volcano.
Compared to other regions in Iceland, the area is considered relatively calm, with only 32 eruptions in the last 10,000 years.
Into the glacier
Near the highest peaks of Langjökull exists a man-made ice tunnel, a true spectacle for any visitor passing by the glacier. Designed and constructed by geophysicist and presidential candidate Ari Trausti Guðmundsson, the tunnel exists to allow visitors to explore the inside of a glacier without having to come to Iceland in mid-winter for a chance to see the less-than-reliable ice caves.
Guests traverse beneath Langjökull's thick ice sheet, experiencing the vivid blue colouration within, and gaining an insight into the glacier's beauty, formation and processes. It is the only place in the world where this is possible. ‘Into the Glacier’ tours are often combined with adventure activities such as snowmobiling.
Nearby glaciers
The glaciers located nearest to Langjökull are Eiríksjökull, which conceals the highest mountain in west Iceland, and Þórisjökull. Hrútfellsjökull also lies on the east side of Langjökull.
Between Þórisjökull and Geitlandsjökull is a valley called Þórisdalur. Along with stunning views, it features prominently in Icelandic folk tales; the outlaw Grettir the Strong of Grettis Saga, for example, is reported to have resided here for one winter.
Langjokull and the Golden Circle
Iceland’s most popular sightseeing route, the Golden Circle, would not be possible if not for Langjökull glacier; none of its three iconic features would exist in their current state without the melting ice.
Gullfoss waterfall is the most obvious example of this. The river that feeds into it, the Hvítá, is a glacier river flowing straight from Langjökull; the scale of the ice cap is hinted at by the sheer volume of water that cascades here every second.
The hot springs at Geysir, meanwhile, are supplied with water underground. Meltwater from Langjökull feeds into the surrounding lava fields, which have very porous rock, and flows in a subterranean river to the geothermal area, where it comes bursting out of the naturally forms vents.
While Þingvellir would still have its National Park and World Heritage status without Langjökull, which it received for being the original site of what is now the longest-running representative parliament in the world, it would be notably less beautiful.
Many springs exist throughout the park, also formed by the underground meltwater of the glacier. Due to its long filtration process, the water emerges as some of the clearest naturally occurring water in the world.
Silfra fissure, therefore, is the best snorkelling and diving location in the country and consistently ranked as one of the top ten places for such activities in the world.
Global warming
Langjökull is shrinking fast and concerns have been raised about the glacier due to the effect of global warming. Some researchers fear that if climate change continues at its current rate the glacier may be gone in 150 years. Less optimistic scientists have said it could be gone in as few as 50.
Hallgrímskirkja is a Lutheran church, located on top of the Skólavörðuhæð hill in the centre of Reykjavík. At 74.5 metres (245 feet) tall, it is the largest church in Iceland, and its tower offers a spectacular panoramic view over the city.
History and Design
The church was designed by one of Iceland’s most renowned architects, Guðjón Samúelsson, who is said to have sought inspiration for his expressionistic design from elements of Icelandic nature.
These include glaciers, mountains and lava formations, particularly the hexagonal basalt columns that surround the waterfall Svartifoss in Skaftafell Nature Reserve, in Vatnajökull National Park. These have influenced the architecture of many structures in Iceland, as well as a whole host of other artistic projects.
It is also designed to resemble Thor’s hammer, with the handle facing up, as a nod to Iceland’s religious history.
The church took 41 years to build, with construction starting in 1945 and finishing in 1986. The leaders of the Church of Iceland wanted a building that would tower over the Catholic Church of Landakotskirkja, also designed by Samúelsson.
The large pipe organ inside Hallgrímskirkja, consisting of over 5000 pipes, was built by German Johannes Klais of Bonn and its construction was completed in December 1992.
Outside the church stands one of the most famous statues of one of Iceland’s most legendary children, Leifur Eiríksson, by American sculptor Alexander Stirling Calder; Eiríksson was a Norse explorer from Iceland who discovered the continent of North America in the year 1000, more than half a century before Christopher Columbus.
The statue was a gift from the United States in 1930, on the millennial anniversary of Iceland’s legislative body, the Alþingi, founded in Þingvellir in 930 AD. This was the world’s first democratically elected parliament and is now located in Reykjavík.
Culture
The church’s namesake is the Icelandic priest Hallgrímur Pétursson, a 17th-century poet and author of the Passion Hymns (Passíusálmar). These hymns are a vital part of Icelandic religious tradition and a staple of local literature, having been reprinted over 75 times since their original publishing in 1666.
The tower of the church is each day visited by hundreds of spectators who seek to enjoy its sweeping view of the capital. The observation tower can be accessed via a lift. There is a small fee to ascend above the clock, which goes towards the maintenance and running of the church.
Hallgrímskirkja counts as the most iconic landmark of the city of Reykjavík and is visible throughout most of the capital, challenged only by the concert hall and conference centre Harpa. It is a useful tool for navigating as visitors wander the streets.
It also serves as a focal meeting point for several cultural events, such as the annual gathering for watching the fireworks on New Year’s Eve. On this night, thousands of people set off dozens of fireworks in an ad-hoc, somewhat chaotic, yet unbelievably dazzling show.
In the lead-up to the night many shops sell protective goggles that are recommended for all observers, particularly children, due to a few incidents of debris falling from poorly aimed fireworks.
Perlan ('The Pearl') is a museum and rotating glass dome that stands on top of Öskjuhlíð Hill in Reykjavík; surrounded by forest, it is one of the capital's most distinctive landmarks. The site is built on top of six water tanks that together store 24 million litres of Reykjavík's hot water.
History & Construction
Architect Ingimundur Sveinsson originally designed the building in 1991; the hot water storage tanks that had stood on top of Öskjuhlíð since the mid-20th-century were updated when the hemispherical glass dome was added on top.
The project was largely curated by the beloved politician Davíð Oddsson, during his term as mayor of Reykjavík.
At night, the water tanks are lit up by floodlights that illuminate the construction for all of the city to see. On top of the dome is a rotating light which serves to signal the aeroplanes flying to and from the nearby Reykjavík Domestic Airport.
Museum & Sightseeing
Perlan has long been home to a viewing platform, restaurant and cafe, but more recently has become an educational site, boasting many exhibitions and displays.
The Glacier Exhibition of Iceland, for example, opened in Perlan in July 2017. The project contains a 100-metre long ice tunnel, where visitors are offered a glance into the past, present and future of the Iceland’s glaciers. It is the only museum in the world with such a feature.
To see the actual inside of a glacier, you can visit the ice caves in Vatnajökull between November and March, or else visit the manmade ice tunnel in Langjökull.
Since the Glacier Exhibition of Iceland, several more projects have been unveiled. Particularly of note is Áróra, the world’s first interactive planetarium film. A beautiful show that was compiled by some of the nation’s most celebrated photographers, writers and musicians, Áróra encourages its guests to dance as part of the piece and to choreograph their own Northern Lights experience.
The planetarium also educates guests on what creates this incredible phenomenon, and the stories people across the world had devised throughout history as a way to explain them.
Perlan also boasts a model of the Látrabjarg cliffs, which are located in the Westfjords; this incredible place is renowned as one of the world’s best places for birdwatching. The replica stands at ten metres tall and allows you to see lifelike figures of the birds that nest here without having to traverse all the way across the country.
This is part of the ‘Wonders of Iceland’ exhibition, which also includes a cinematic display of the country’s underwater world and a wealth of displays about Iceland’s geology, such as its volcanoes, tectonic plates, geothermal sites and earthquakes.
Furthermore, Perlan has an exhibition called ‘Water in Icelandic Nature’, which discusses everything about how water defines this country, from its weather patterns to its natural features, its wildlife to its chemistry. It uses cutting edge technology and interactive displays to bring these concepts to life.
Aside from its exhibitions, Perlan is renowned for its sightseeing opportunities. The observation deck here offers an impressive and panoramic view of the city and its surroundings, with adult tickets available for 490 ISK.
The surrounding woodland of Öskjuhlíð boasts of several scenic hiking trails and cycling routes, several of which lead to the remains military bunkers that were built by the US army during its WWII occupation in Iceland.
Restaurant and Shop at Perlan
At the top of the rotating dome of Perlan is a restaurant called Út í Bláinn, which boasts some of the best views in the city. It focuses on simple, seasonal, perfectly prepared Icelandic food, and has a friendly, lively atmosphere. Those looking for a bite without paying for the experience of the rotating restaurant will find the cafe Kaffitár below.
Perlan is also home to one of the oldest gift shops in Reykjavík, Rammagerðin, established in 1940. It has a range of products made by Icelandic designers and craftspeople that reflect the nature, culture and history of this beautiful nation.
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 Vik
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 glaciers Eyjafjallajökull and Mýrdalsjökull can also be seen on clear days; both of these cover volcanoes which 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 Dyrhólaey, 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 August.
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 Vik
Vík, due to its closeness to the Reynisfjall and Dyrhólaey 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 Vik
Vík has a wide variety of public services, due to its remoteness and its importance in 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.
Keflavík International Airport (KEF) is Iceland’s only international airport and the port of arrival for the vast majority of visitors to the country. In 2016 alone, almost seven million passengers went through its gates.
The History of Keflavík International Airport
Keflavík International Airport is a relic from the ‘invasion of Iceland’ in World War II, when Allied troops took over the island nation following the defeat of its colonial ruler, Denmark, at the hands of the Nazis.
The British laid out a landing strip in the town of Garður, but considering Iceland’s incredibly strategic position in the middle of the Atlantic Ocean, one strip was not quite enough.
After taking control of the ‘occupation’, US troops constructed and opened two airfields for military purposes in 1942 and 1943. Though they returned the property after the war, the United States reclaimed it in 1951 after a controversial defence alliance with Iceland.
This pact, and the general joining of NATO in 1949, caused decades of national protest, comparable to the ‘Women’s Day Off’ marches in 1975 and the ‘Kitchenware Revolution’ which followed the 2008 economic crash. The circumstances of it, however, also allowed decades of development at Keflavík Airport.
The airport first started to separate civilian and military use in 1987, with the opening of the Leifur Eríksson Terminal. Named after the first European to settle the Americas, it would go on to handle all the guests coming to or leaving Iceland.
The arrangement that the US would provide Iceland’s defences continues to this day, but their permanent bases at Keflavík were left at the expiration of the treaty in 2006. The airport was thus moved into full control of Icelanders and has expanded as a civilian hub ever since.
Keflavik International Airport Today
Keflavík International is located on the tip of the Reykjanes Peninsula, Iceland’s south-westernmost region. The drive to the capital city of Reykjavík is only about forty-five minutes, and there is a bus service that continuously runs between the locations, day and night.
This service provides guests with the option to stop at the Blue Lagoon en route in either direction, the iconic health spa renowned for its healing azure waters. The lagoon sits between the airport and the capital, refreshing guests after a long flight, or revitalising them in preparation for one.
The airport itself has all the modern amenities one would expect from a port that experiences so much traffic. It has restaurants, bars and cafés, banks and money transfers, car rental options available, a smoking area and, of course, many options for duty-free shopping.
Considering the price of and lack of availability of alcohol in Iceland, it is the best place to stock up on any tipple desired for your trip. Otherwise, you will have to locate specialist alcohol shops, which have limited opening hours, are sparse in the remote regions of the country, and have high taxes and duty.
The main airlines that arrive at and depart from Keflavík are the two national carriers, the prestigious Icelandair and budget airline WOW. Over thirty different carriers have chartered flights to the port, however, which head to over ninety different destinations. This is only ever increasing, with new travel routes emerging as Iceland’s popularity continues to skyrocket.
Fjaðrárgljúfur is a beautiful, dramatic canyon in South Iceland, close to the historic town of Kirkjubæjarklaustur.
Fjaðrárgljúfur is little known and is thus far less crowded than other sites in the area, such as Skaftafell nature reserve, and Jökulsárlón glacier lagoon. Its beauty and isolation make it a dream location for photographers and hikers alike.
Though the valley was only formed at the end of the last ice age approximately 10,000 years ago, the bedrock here is much older, dating back two million years. The ravine was created by the runoff from a glacial lake, which wore away the soft stone and left only the more resistant rocks behind.
Geography of Fjaðrárglúgur
Fjaðrárglúgur is about 100 metres (328 feet) deep and 2 km (1.25 mi) long, with sheer walls dotted with many waterfalls.
It is possible to walk along the ridges above, or in the valley itself. The site is popular amongst photographers for the contrasts between the dark rocks, foaming waters and verdant moss. Of course, if the midnight sun or northern lights are out, it is a shutterbug’s paradise.
If taking the route along ridges of the valley, look up as well as down, as, in clear weather, you will attain great views of the South Coast, Highlands, and surrounding glaciers.
If taking the latter route, know that the river Fjaðrá runs through the canyon, and though its waters are often shallow, those exploring may have to wade through it. While this is safe, you will want either waterproof, sturdy boots, or sandals with a strap on the back that you can easily change in and out of.
This tributary runs into the greater Skaftá river.
Fjaðrárglúgur’s Surroundings
The closest settlement to Fjaðrárglúgur is Kirkjubæjarklaustur, often nicknamed Klaustur by locals. This is a place with a long religious history; it was home to the country’s first convent, and is said to be the only place in the country that the Old Norse faith was never practiced.
Many local sites are named after the nuns who once lived in the area, such as Systrastapi (Sister’s Rock) and Systrafoss (Sister’s Falls).
Fjaðrárglúgur is a great place to stop for those travelling the South Coast as they make their way from Reykjavík or Vík towards Skaftafell and the Jökulsárlón Glacier Lagoon.
The South Coast itself is lined with other features to visit during your travel. These include the dramatic waterfalls Skógafoss and Seljalandsfoss; the former is famed for its scale, and the latter for the fact that you can walk all around it.
You will also see sites such the beach Reynisfjara, with its great sea-stacks, Reynisdrangar, said to be trolls frozen in the light of the morning sun. Other coastal features include the Dyrhólaey cliffs and arch, which is a paradise for birdwatchers in summer, due to the fact that it is home to thousands of nesting puffins.
The South Coast can be explored in a day, but to get to all the sites and enjoy them properly, visitors are encouraged to spend two or three days in the region.
Kirkjufell, or 'Church Mountain', is a distinctly shaped peak found on the north shore of Iceland’s Snæfellsnes Peninsula, only a short distance away from the town of Grundarfjörður. It is often called ‘the most photographed mountain in Iceland’, due to its dramatic formation and perfect coastal location.
Kirkjufell takes its name from its resemblance to a church steeple, sharpened at the top with long curved sides. From other angles, the mountain has been compared to a witch’s hat or even a freshly scooped ice cream.
Photography at Kirkjufell & Kirkjufellsfoss Waterfall
Peaking at 463 metres, 1519 feet, Kirkjufell is an impressive landmark. Throughout the centuries, Kirkjufell’s striking slopes have acted as a visual landmark for seafarers and travellers. More recently, it has attracted amateur and professional photographers alike.
Within walking distance from Kirkjufell is the serene and perfectly located waterfall Kirkjufellsfoss, or 'Church Mountain Falls', an excellent subject for photographers who can easily frame the mountain in the background. Despite its relatively diminutive height, Kirkjufellsfoss’ three-steps, gentle flow, and dramatic differences between seasons make it as impressive as some of Iceland’s larger waterfalls.
At the base of the mountain, visitors will also be able to find a lake; on calm and clear days, this lake reflects a perfect mirror image of Kirkjufell, only adding to the fantastic photo opportunities around this area.
On top of that, the colours of Kirkjufell change with the passing seasons; the summer sees it a lush green, full of life, whilst the winter months scar the mountain’s face with a mask of barren brown and white. Of course, it is more impressive under the midnight sun in the weeks surrounding the June equinox, and under the northern lights, best seen between September and April.
Fans of the HBO series Game of Thrones will recognise Kirkjufell as a shooting location from Season 7 of Game of Thrones. The mountain is showcased from the scenes ‘North beyond the Wall’ when Jon Snow, The Hound and Jorah Mormont, amongst others, brave the wilderness in hopes of catching an undead wight.
Having seen it in a vision, The Hound acknowledges Kirkjufell as “[...] the mountain like an arrowhead”, and the events that happen beneath it are some of the show’s most dramatic.
Hiking Kirkjufell
There is a fairly steep trail to the top of Kirkjufell, from where there are magnificent panoramas of the surrounding fields, coastlines and rivers. The mountain takes roughly an hour and a half to ascend, with another one and a half hours needed to get back to the bottom.
Given the steep elevation and treacherous trail, you should only hike Kirkjufell if you are a very experienced and confident mountain climber, preferably in the company of an expert guide. Sadly, there have been three fatal accidents on the mountain, most recently in 2018.
Getting to Kirkjufell
Kirkjufell is extremely close to Grundarfjörður, a small town on the Snæfellsnes Peninsula, which is just over two hours drive from Iceland's capital city, Reykjavík. From Grundarfjörður, one travels a few minutes west down Route Snaefellsnesvegur 54 to the base of Kirkjufell. Visitors have plenty of parking space to choose from, all free of charge.
Öxarárfoss is a waterfall situated within Þingvellir National Park in southwest Iceland.
The waterfall flows out the river Öxará, cascading in two drops over the cliffs of Almannagjá gorge, which marks the eastern boundary of the North American and Eurasian tectonic plates.
Description
The waterfall has a height of 13 metres (44 feet) and an average width of six metres (20 feet). The pool of water at the waterfall’s base is dotted with large, smooth rocks, which get especially icy in winter. The waterfall can be visited year round, but expect large crowds during the peak season of the summer.
During the depths of winter, the waterfall is entirely frozen over. Ice climbers have been known to scale it, but this should only be done with and by experts.
Surroundings and History
Öxarárfoss is one of the most popular attractions of Þingvellir Natural Park, which in turn, is one of the most popular attractions of Iceland. The National Park is one of the three famous sites of the Golden Circle along with Gullfoss waterfall and the Geyser Geothermal Area, for both geological and historical reasons.
The geological reason is that, as mentioned, Þingvellir lies between the tectonic plates. As they pull apart, the land is torn, and thus there are many beautiful ravines and lava fields to be found.
The most famous of these ravines is Silfra. Like the others, it is filled with crystal clear glacial water, which emerges from a spring, but unlike the others, it is possible to take snorkelling and diving tours here.
The water from the crevasses such as Silfra feed into the lake Þingvellavatn; in fact, the river Öxará, which feeds Öxarárfoss, is the only source of the lake that does not come from a spring.
The historical reason that makes Þingvellir so famous is that it was the original site of the Alþing, the Icelandic parliament founded in 930 AD. This parliament continues to exist in Reykjavík but for nine centuries flourished here.
Icelanders would meet annually to pass laws, settle disputes, and share news. It was both incredibly progressive, giving a voice to all people and granting women divorces long before many other nations were considering it, and barbaric, hosting many battles and the prosecution of dozens of witches.
It is thus featured in many sagas, and though not always mentioned in them, Öxarárfoss was a witness to this long history.
One notable piece of folklore about the waterfall was that it was said to have prophetic powers for the year ahead. At midnight on New Years Eve, it would run red with either wine or blood, with the former promising prosperity ahead, and the latter warning of war.
Haukadalur is a geothermal valley in South Iceland on the popular Golden Circle route.
Lying to the north of Lake Laugarvatn, it is home to hot springs, fumaroles, mud pots and geysers, including the famous Great Geysir and the active Strokkur. The area is noted for the vivid colouration of its surrounding hills, caused by elements deep in the earth being brought to the surface by the geothermal activity.
History of Haukadalur
Haukadalur has been mentioned in historic writings as far back as 1294, in which its geysers were described following an earthquake that activated them. Since the 18th Century, it has been drawing visitors to the island including two different Kings of Denmark in 1907 and 1922.
Throughout the 20th Century, images of the Great Geysir erupting at Haukadular began to symbolise Iceland. It’s activity, however, was unreliable, so unnatural efforts were made to stimulate it more regularly, such as lowering the water table in 1935 and pumping soap into it 1981.
These, however, limited the geyser’s long-term activity, so that it rarely goes off today, although, in the early 2000s, it did have a period where it was spouting water over 140 metres (459 ft) high. Even so, the geyser Strokkur is still very active, erupting to heights of 30 metres (98 ft) every five to ten minutes.
Today, most of the near-two million visitors to Iceland will see Haukadalur Valley on their travels.
Surroundings of Haukadalur
Haukadalur Valley is located about an hour and a half’s drive inland from Reykjavík, thus making many sites of the South and West easily accessible. The most notable of these are the other points on the Golden Circle: Gullfoss Waterfall (about five minutes away) and Þingvellir National Park (about forty minutes away).
It is also, however, within an easy driving distance of Flúðir, home of the Secret Lagoon, the Kjölur Highland Road, which leads into Iceland’s interior, Sólheimar eco-village, and Faxi Waterfall.
Wikimedia, Creative CommonsChensiyuan
Grundarfjörður is a small town found on the north coast of the Snæfellsnes Peninsula in the west of Iceland. It has an approximate population of 872 people and has been twinned with the French town Paimpol since 2004.
The town’s main industries lie in fishing and fish processing. Grundarfjörður also bears host to substantial ship traffic, a consequence of’ the settlement’s natural harbour.
More recently, it has become a centre for tourism, due to the incredible beauty of the features on the Snæfellsnes Peninsula. It is developing to meet the needs of those who travel through it.
Grundarfjörður boasts a public library, a historical centre, a resident’s café and a photography exhibition, Bæringsstofa, which is a collection of pictures by the late Icelandic photographer and honorary citizen of Grundarfjörður, Bærings Cecilsson.
Asides from accommodation and amenities, Grundarfjörður offers the opportunity to partake in numerous outdoor activities, ranging from horseback riding and camping to ice-climbing.
One can also find a nine-hole golf course beside the town.
Kirkjufell Mountain
Visitors to Grundarfjörður will likely visit the town’s main landmark, the photogenic Kirkjufell, which translates to ‘Church Mountain’. Clearly distinguishable, and standing alone on the edge of the sea, its dramatic slopes, steeple-like peak and surrounding shorelines make it one of the country’s most beautiful summits.
Kirkjufell is often called the most photographed mountain in Iceland, due to the variety of different way you can shoot it, and how starkly different it appears under different lights.
Besides the mountain itself, one can find Kirkjufellsfoss (Church Mountain Falls), a beautiful three-pronged waterfall, which is often favoured as a foreground.
Rock climbing is possible up Kirkjufell, but only for the very experienced as there have been accidents before.
Folklore & History
Nearby, one can find the town and municipality of Stykkishólmur, which has a population of 1,195, and is a centre of commerce and services for the region. The town, more than any other in the region, is considered mystical, with many folk stories and Sagas referencing it.
The road from Grundarfjörður to Stykkishólmur crosses a wide lava field known as Berserkjahraun. The name of this lava field is derived from the Eyrbyggja saga, in which it said two berserkers (Viking Warriors) were slaughtered by their master because one of them fell madly in love with own daughter.
It was said that the master had then pave the road across it before killing them.
Grundarfjörður is an important historical town in Iceland, having been a centre of trade for the Snæfellsnes Peninsula since at least the 15th century. The town was certified official as one the country’s six designated marketplaces in the year 1786.
There are a number of antiquity sites around the town, however, that point to the region being well-inhabited as far back as the Viking era.
Like many places on the peninsula, it is likely that it could have been one of the first inhabited places in the country, due to its harbour and the wealth of fish that live just off its shores.
Photo from Into the Underworld | Vatnshellir Caving Tour
Vatnshellir Cave is a lava tube on the Snæfellsnes Peninsula and a popular site for caving tours.
Geology of Vatnshellir Cave
Vatnshellir is one of Iceland’s older lava tubes that can be explored, having been formed in an eruption 8,000 years ago. To compare, Iceland’s other most popular lava tunnels for caving, Viðgelmir and Leiðarendi, are only one and two thousand years old respectively.
Like all lava tubes in Iceland, Vatnshellir was created when during an eruption, a river of molten rock began to cool from outside in. The effect left a crust over still-flowing lava, which, after flushing away, left a hollow tube.
The minerals of this lava can still be seen in Vatnshellir today. The rocks are vividly coloured, with reds representing deposits of iron, yellows representing sulphur, and greens representing copper.
Vatnshellir is 200 metres (656 feet) long, with a deepest point of 35 metres (114 feet).
Lava Caving in Vatnshellir
Lava caving is possible in Vatnshellir throughout the summer months with a guided tour. Taking such a tour is essential, as guides know the caves in and out, and will bring all the equipment you need. Alone, they are notoriously easy to get lost and hurt in.
Vatnshellir is easier to enter than its cousin Leiðarendi, as it has a staircase descending into it. Unlike Viðgelmir, however, the ground is not paved and the walls are not lit, so you need a reasonable level of fitness and confidence on your feet to traverse it comfortably. Even so, children as young as five can join the fun.
When travelling the cave, you will learn about Iceland’s geology and folklore, as trolls were said to make the caves their homes in many tales. You will also get to experience total darkness by shutting off your lights at the deepest point.
Location of Vatnshellir cave
Vatnshellir is a protected site, as it is within the Snæfellsjökull National Park. This park sits right on the tip of the Snӕfellsnes Peninsula, meaning you can include many nearby sites in a visit to it.
These include the basalt sea stacks of Lóndrangar, the fishing villages of Arnarstapi and Hellnar, and the pyramid-shaped peak Kirkjufell.
Djúpalónssandur is an arched-shaped bay of dark cliffs and black sand, located on the Snæfellsnes Peninsula in western Iceland.
History & Monuments
The location was once home to a prosperous fishing village, similar to other abandoned hamlets and ports of the area such as Búðir and Hellnar. These thrived back when the Snæfellsnes Peninsula functioned as one of the most active trading posts of the island, but now are simply centres for tourism.
Fascinating remnants of this period are found in the form of four ancient lifting stones that still occupy the beach. The stones range in weight from 23 kg (50 lbs) to 155 kg (342 lbs) and were used to test the strength of fishermen. Their names are Amlóði (useless), Hálfdrættingur (weakling), Hálfsterkur (half-strong) and Fullsterkur (full-strong). Even today, you can see how you would have fared working on Iceland's dangerous seas by trying your luck at lifting these stones.
In 1948, the English trawler Epine GY 7 from Grimsby shipwrecked on the shore, with fourteen dead and five survivors. The rusty iron remains of the vessel remain scattered on the beach, now protected as a monument to those who perished.
Environment & Surroundings
The Snæfellsnes Peninsula boasts countless natural wonders, where locals and travellers both flock on a daily basis to enjoy the unique landscape and stunning coastlines. Djúpalónssandur’s black pebble beach is particularly stunning with its rocky coastal lava formations, which include a large lava rock with a hole in the middle through which you can directly spot the Snæfellsjökull glacier volcano.
Behind the rocks are two freshwater lagoons called Djúpulón and Svörtulón, with the former serving as the namesake of the bay. Though believed in olden times to be bottomless, the water bodies were later revealed to reach the depth of just five metres.
Lagoons such as these are held in high regard amongst the Icelandic people, and Svörtulón is thought to possess healing properties, especially after having been blessed by Bishop Guðmundur góði ('the good') in the late 1100s.
A natural monument of the area is Söngklettur, or “singing rock”, a large lava rock with a reddish hue that resembles an elfish church. Other rock formations of folklorish appeal rest close by, including the alleged trolls-turned-to-stone Kerling and Lóndrangar.
Warning
When visiting Djúpalónssandur, take heed that these are treacherous waters and the Atlantic Ocean’s powerful suction can easily carry you out to sea. This beach is not one for wading, but enjoying from a safe distance, especially if the weather is stormy.
The video below shows the power and shocking speed of sneaker waves that occur at locations such as Djúpalónssandur and Reynisfjara in the south.
The glistening pebbles that make up the beach known as Djúpalónsperlur, or “pearls of the deep lagoon”, are gorgeous to look at and might seem appealing to stone collectors, but they are protected by law and should not be removed from the area by visitors.
Harpa is Rekjavík’s premier concert hall and conference centre. Opened in 2011, its design was a collaboration between Danish-Icelandic artist Ólafur Elíasson, and the Danish firm Henning Larsen Architects. Today, it is a cultural centre of Reykjavík and one of the city’s most iconic landmarks.
History
The idea for a purpose-built concert hall in Reykjavík had been tossed around since the 1880s, but it wasn't until this millennium that it began to gain traction. Construction finally began in 2007, with Icelanders as blissfully unaware as the rest of us as to the problems that year would bring.
The wake of the financial crash of 2008 hit Iceland far harder than most other countries; its banks far overstretched themselves across Europe and ended up heavily indebting the people when they collapsed.
The future of Iceland’s economy was uncertain, especially when the government declared they would not bail out the banks nor pay off their debts, much to the chagrin of countries like the Netherlands and the UK.
In this tumultuous period, Harpa was left partially constructed, with no funds to finish it. The Icelandic populace was divided between having a half-finished construction site facing their downtown—a humiliating reminder of their country’s financial state—or spending money no-one was sure they had.
The Icelandic government, however, decided that it was the only building in the country that warranted being raised, in spite of the dubious future of the economy, and fully financed its completion.
When the European Court of Justice ruled that Iceland did not have to bend to the will of its debtors, the country was united in supporting it.
Architecture
Harpa won the prestigious Mies van de Rohe award in 2013, otherwise known as the European Prize for Contemporary Architecture, and is featured heavily in any tour of the city. Its structure is beautiful and unique; it has a facade of 714 glass panels, all of which are a different shape and built with an LED light that allows for shows whenever the sky is dark.
Ólafur Elíasson is world-renowned for his large-scale installation art, and for the influences he draws from the natural world. This is clearly exhibited in Harpa. The building reflects the basalt landscapes of Iceland and the dark-coloured glass creates beautiful effects with the natural light. Considering the midnight sun and aurora borealis, this can be quite spectacular.
Studio Olafur Eliasson employs 90 people, from architects to graphic designers, craftsmen to art historians. Based in Berlin, they work across the world, and are well-known for works such as London's 2007 Serpentine Gallery Pavillion and the annual event Life is Space.
Henning Larsen Architects are similarly successful. They have collaborated on the construction of dozens of buildings in over twenty countries, such as the Copenhagen Opera House and Uppsala Concert Hall in Sweden. They are currently working on the creation of thirteen buildings around the world, many of which they scored the opportunity to work on due to their competition-winning designs.
Harpa Today
Today, Harpa is one of the jewels in Reykjavík’s crown. The hall hosts exhibitions, concerts, cultural events, meetings, and festivals such as Airwaves, Sónar and the Reykjavík Fashion Festival. Home of the Icelandic Symphony Orchestra and the offices of the Icelandic Opera, it is a centre of culture in Iceland’s capital.
Many internationally known artists from around the world have performed here, including people such as Eddie Izzard and Cyndi Lauper. It also regularly showcases native talent, such as Björk and Of Monsters and Men.
Below, you can see a video showing Harpa's construction:
Photo from: The Cave Explorer | Family Friendly Tour of Vidgelmir Lava Cave
Viðgelmir is the largest lava tube in Iceland at 1585 metres (5200 ft) long. It is located in the country’s west, and is one of the most popular destinations for lava tubing.
Geography and Geology of Viðgelmir
Viðgelmir is situated in the Borgarfjörður of west Iceland, beneath the Hallmundarhraun lava field. It was formed during a lava flow that occurred in the area in 900 AD.
Lava tubes are formed when a river of running lava cools from the outside, creating a solid shell. When the liquid lava within this flows out, a cave is left remaining.
This river must have been vast, as it left the largest cave in the country. Not only is it the longest, but also its widest, with the walls 16.5 metres (54 feet) apart at one point, and the highest, which the ceiling up to 15.8 metres (52 feet) above the ground.
As with many lava caves in Iceland, Viðgelmir has both lava stalactites, which come from the ceiling, and stalagmites, from the ground. The former were formed when lava at the top part of the cave cooled as it dripped from above, and the latter indicated where this lava landed, pooled and began to stack.
Unlike in limestone caves, these features never grow back if broken off, thus it is absolutely essential that you do not touch them or attempt to break them off. There are large fines for those who break these rules, and many of the more beautiful features are cordoned off.
Lava Caving in Viðgelmir
Viðgelmir is one of the country’s most popular lava caves, and the easiest to traverse for beginners.
Unlike lava caves such as Leiðerendi on the Reykjanes Peninsula, Viðgelmir has a paved walkway and installed lights. This means those who are less confident on their feet do not need to worry about the uneven lava or relying on their own torch.
The scale of the cave also makes walking it much less challenging, as there is no crawling, stooping or clambering needed to get through.
History of Viðgelmir
Viðgelmir is one of the many caves in Iceland that humans were known to have lived in.
Through Iceland’s medieval period, it was a common punishment for criminals to be outlawed from society. Many of these moved into caves and lived out their lives as notorious bandits.
It is very likely, considering the age of the evidence found, that this was the case in Viðgelmir. These artefacts are now kept in the National Museum of Iceland.
Breiðamerkurjökull is the glacial tongue that extends from southern Vatnajökull and into the glacier lagoon Jökulsárlón, creating the icebergs that define this beautiful landmark.
Breiðamerkurjökull is constantly retreating, breaking and melting, causing the Jökulsárlón glacier lagoon to increase in size; it is less than a century old, but already the deepest lake in Iceland.
This glacier tongue provides the lagoon with all of its enormous icebergs, which perpetually break from off its tip and tumble into the waters. Here they float for about five years until they are small enough to make their way towards sea. When they finally do escape the lagoon, most join the countless smaller ice chunks that adorn the nearby Diamond Beach.
Breiðamerkurjökull is beset with enormous cracks and crevices, and since it's virtually impossible to tell exactly when the next big block of ice will break from it, people should admire this enormous glacier tongue from a great distance.
The Diamond Beach is a strip of black sand belonging to the greater Breiðamerkursandur glacial plain, located by Jökulsárlón glacier lagoon on the South Coast of Iceland.
Here, the icebergs which fill Jökulsárlón glacier lagoon wash up on shore, standing dazzling and defiant in stark contrast to the black sand beach. It is, therefore, a favourite amongst photographers, nature-lovers, and wildlife-enthusiasts. Many seals call this beach home, and it is one of the best places in the country to see orcas from the shore.
Breiðamerkursandur
Breiðamerkursandur is a glacial outwash plain located in the municipality of Hornafjörður. The sand stretches approximately 18 kilometres along Iceland’s South Coast, more specifically from the foot of Kvíárjökull Glacier to the famed glacier lagoon Jökulsárlón, that nests by the foot of Breiðamerkurjökull Glacier.
Both glaciers make up part of the 30 outlets of Vatnajökull, Europe’s largest ice cap and the central feature of the Vatnajökull National Park. Many of these are seen en route to the Diamond Beach as you travel along the South Coast.
The outwash plain was formed when three of Vatnajökull’s outlet glaciers, Breiðamerkurjökull, Hrútárjökull and Fjallsjökull, flowed forward due to volcanic activity and ground the rocks of the underlying surface, creating and pushing forward the glacial sediments.
Such sand plains are a common part of the Icelandic landscape, due to the island being volcanically active as well as boasting numerous ice caps. The terminus (the tip of a given glacier) also dug deep into the ground and left what is now the Jökulsárlón glacier lagoon. Although now the deepest lake in all of Iceland, it only began to form in 1935.
The glacier lagoon and Diamond Beach are fantastical sites, however, the rate of their expansion is, unfortunately, a consequence of climate change. With the rate that the glaciers are melting, there may be no ice left at either site within decades.
Jökulsárlón Icebergs
Jökulsárlón glacier lagoon is one of the most famed and visited attractions in Iceland. Floating on the lagoon are enumerable icebergs that have broken off the resident glacier, creating an ever-changing scenery of incredible allure.
The river Jökulsá connects the lagoon to the Atlantic Ocean, meaning that these icebergs eventually drift out to sea where they are polished by the waves before floating back to the black sands of Breiðamerkursandur. The name ‘Diamond Beach’ thus comes from the white ice on the black sand appearing like gemstones or diamonds, as they often glisten in the sun and sharply contrast their jet black surroundings.
Safety at the Diamond Beach
The Diamond Beach is a safe place for any responsible traveller; unlike at Reynisfjara, another South Coast black-sand-beach, sneaker waves and rip currents are not notorious for whisking unwitting tourists out to sea. However, there are still dangers to consider.
The main one of these is the icebergs themselves. Under no circumstance should you climb upon an iceberg, due to their slippery surfaces and sharp edges.
This is especially the case if the iceberg is at all in the water, as it could flip and trap you underneath, or else be pulled out to sea by a current with you on it.
The risk of injury and illness in the form of hypothermia is so great that extortionate fines exist to deter any ‘rebels’ looking for a thrill-seek. These have only come about due to serious incidents, to protect not only tourists at the lagoon but guides and staff who may feel obligated to embark on a dangerous rescue if they see someone at risk.
The Krauma Spa is a geothermal bath and spa resort in West Iceland. It is located near Europe's highest flowing hot spring, Deildartunguhver.
Krauma Spa was opened to the public in late 2017 and offers five hot tubs, one cold tub and two steam baths, as well as a relaxation room where you can unwind to soothing music next to a crackling fireplace.
On-Site Facilities
To create the perfect bathing temperature, the spa pumps hot water straight from Deildartunguhver hot spring and cools it down by mixing freezing water from Iceland's smallest glacier Ok. The steam in the steam baths also comes directly from the hot spring and is scented with oils.
A restaurant and a bar are located on-site and provide views of the Deildartunguhver hot spring and the nearby valley. The restaurant serves Icelandic cuisine made from fresh farm-produced ingredients, and the bar offers a wide selection of drinks and snacks.
Krauma Spa and Resort is open all year round and accommodates up to 140 guests at a time. The restaurant seats 70 guests inside and another 60 on the outside terrace when the weather allows.
Nearby Attractions
Krauma Spa is located near some of West Iceland's most popular attractions. Aside from the powerful Deildartunguhver hot spring, visitors in the area can take a short drive to the waterfalls Hraunfossar and Barnafoss.
Iceland's largest lava cave, Víðgelmir in the Hallmundarhraun lava field is only a short drive away from Krauma Spa, and so is the country's second largest glacier, Langjökull.
Close by is the historical Reykholt area and the town of Borgarnes. Reykholt houses Snorrastofa, a centre for medieval studies, named after historian, poet and law-speaker Snorri Sturluson, and in Borgarnes, you'll find the Settlement Centre which focuses on the age of settlement in Iceland and Egill Skallagrímsson, a Viking-Era poet and warrior of the Egils Saga fame.
