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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.

Landmannalaugar, or the 'People's Pools', is a vast area of stunning and unique beauty in the heart of Iceland's southern Highlands. Throughout the summer, it is one of the most popular places for hiking -- either over one day or several -- and natural hot spring bathing.

Geology

Landmannalaugar is a truly rare area, both geologically and aesthetically. The dramatic region can be found nestled beside the raven-black Laugahraun lava field, a sweeping expanse of dried magma which originally formed in an eruption in 1477.

Landmannalaugar itself is made up of windswept rhyolite mountains, a rock type that creates a full spectrum of dazzling colour. Shades of red, pink, green, blue and golden yellow make for an ethereal location.

Landmannalaugar was historically best known for its natural geothermal baths, hence its name the People's Pools. For centuries, it served as an area of shelter and respite for weary travellers who use these soothing springs as a means to relax after tiring excursions.

Originally, those attending were settlers crossing the barren highlands, but today, they are tourists after an exciting trip.

Today, visitors to the Highlands should always bring a swimsuit and towel, just in case one of these naturally occurring hot pools should crop up along the hiking trail.

The most popular road leading to Landmannalaugar, Sigölduleið, has such springs, and takes you past multiple stunning natural features, including Bláhylur lake, a magnificent body of water nestled in a dormant volcanic crater.

Landmannalaugar can be reached by car in one of two ways. The quickest is driving through West Iceland, either via Selfoss or Þingvellir National Park. A longer but more scenic route would take you along the South Coast of Iceland. This is Iceland’s most popular sightseeing route, aside from the Golden Circle, due to its wealth of sites.

Of course, like many of Iceland’s destinations, Landmannalaugar can also be reached via helicopter, for those who are travelling with less of a concern for budget. Those on more of a shoestring can buy a bus pass that will take them to the region.

Hiking

Landmannalaugar marks the northern end of the Laugavegur, one of Iceland's most popular hiking trails. This route connects Landmannalaugar and Þórsmörk, the ‘Valley of Thor’, ending at the beautiful Skógafoss waterfall.

It is also home to many other notable trails, however, including the path onto the mighty Mt. Brennisteinsalda, the ‘Sulphur Wave’ crater. Visitors can also traverse the trail up the Bláhnjúkur volcano, the 'Blue Peak', whose summit allows for a sweeping view of up to five glaciers on clear days.

Multiple operators run daily tours to Landmannalaugar from mid-June to mid-September, during which time the Icelandic Touring Association operates a small shop, three campsites and a mountain hut equipped with sleeping bags and accommodation for up to 80 visitors.

It is only recommended you take a multi-day hike with an operator. If visiting Landmannalaugar without a guide, you will need a four-wheel-drive.

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.

Hekla, nicknamed ‘the Gateway to Hell’ in the Middle Ages, is one of Iceland’s most explosive, unpredictable and powerful volcanoes. It has erupted twenty to thirty times since settlement, and remains active to this day.

Geography of Hekla

Hekla is located in the south of Iceland, just north of the country’s most famous volcano, Eyjafjallajökull, which last erupted in 2010, causing planes to be grounded and reporters to be tongue-tied for weeks. A dominant peak, standing at 1,491 metres tall (4,892 feet), it can be seen for miles around.

Hekla is part of a 40 kilometre (25 mile) rift, the most active part, called Heklugjá, being under the volcano itself. There are many craters at the peak, two of which are known to erupt more than the others.

Unlike Eyjafjallajökull and Iceland’s other most active volcano, Katla, Hekla does not sit underneath any significant glacier, meaning its eruptions should not cause ash clouds to the same degree. In spite of this, some have been so great that the ash produced was still enough to change the climate of the northern hemisphere for years.

Hekla has also produced one of the greatest lava flows of this millenium of any volcano in the world, at eight cubic kilometres. Approximately 10 percent of Iceland’s landmass was brought up by lava from Hekla.

History of Hekla

The first recorded eruption at Hekla was in 1104, and it was so great and significant that it drew attention across Europe; the effects it had on the weather, on people’s breathing, and on agriculture lasted for years.

This, however, was not the first time it had done so; undiscovered by man, it had contributed to a third of all volcanic ash across northern Europe for the past seven millenia.

It would not significantly erupt again until 1300, although it had been recorded going off several times in between; one of the most notorious things about Hekla is its unpredictability, sometimes exploding within a decade of its last eruption, sometimes laying dormant for nearly a century.

For this reason, the farms around it were largely abandoned, partly explaining why today there are few settlements in Iceland’s south.

Further serious eruptions occurred in 1693 and 1845 with international consequences, but none as significant as the one that began in 1947. Lava bombs weighing over 20 kilograms (44 pounds) landed 32 kilometres away; some as large as 50 square metres (538 square feet) were thrown a kilometre. It took just 52 two hours before the enormous cloud of ash was covering Helsinki.

It would be thirteen months before the eruption stopped, ebbing and flowing with power, but constantly pouring ash into the atmosphere, poisoning crops and livestock.

It is likely many died of respiratory problems as a result, but Hekla even directly killed one person. A scientist filming the great lava flows from the crater, some of which were 15 metres (49 feet) tall, was struck by a block of lava.

Hekla erupted again in 1970 for two months, but since has only gone off for a few days at a time, in 1981, 1982, 1991 and 2000.

Though the 2000 one seemed inconsequential, it was later discovered that it proved that Hekla was even more frightening than was already thought. The remains of a pyroclastic flow, the most dangerous element of an eruption, where searing ash and rock travel at enormous speeds and raze all they meet, had occured for over five kilometres (three miles).

Hekla today

In spite of its volatile nature, Hekla can still be considered a safe place to visit; there are hiking opportunities all around it, and some tour operators embark in super jeeps journeys to its slopes. Visitors should not be afraid of the volcano’s potential, just aware of it.

Of course, before heading to Hekla if travelling without a guide, ensure you check the meteorological office’s website to ensure that there are no alerts that an eruption may be imminent. The volcano is monitored constantly.

In spite of this, Hekla remains as unpredictable as it ever was, and visitors are warned that in spite of every good measure, there is always a chance an eruption could start without being noticed.

Volcanologists also warn that it is overdue, and due to this volcano’s patterns, the warning time between knowing an eruption is imminent and it occurring will often be just an hour or less.

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.

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

Geography

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

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

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

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

Eruptions

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

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

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

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

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

Eyjafjallajokull today

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

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

Dyrhólaey Peninsula is a 120-metre promenade famed for its staggering views of Iceland’s South Coast, as well as its historic lighthouse and wealth of birdlife. It is home to a rock arch of the same name.

Dyrhólaey, which translates to Door Hill Island, is of volcanic origin and was once an island before joining up to the Icelandic mainland. In ancient times, passing sailors used to refer to Dyrhólaey as ‘Cape Portland’.

It is also the southernmost part of the Icelandic mainland, making it a popular stop for sightseers travelling along the Ring Road, and can be found close by the coastal village of Vík í Mýrdal.

Other features along the South Coast en route to Dyrhólaey from Reykjavík include the waterfalls Seljalandsfoss and Skógafoss, and the glacier Eyjafjallajökull.

Dyrhólaey Arch

Dyrhólaey’s most instantly recognisable attraction is the promenade’s massive rock arch, a result of centuries of erosion. As a result, its name is in direct reference to this enormous arch. In fact, this natural feature is so large and dramatic that one daredevil pilot even flew through it, back in 1993. Boats can easily cruise through its opening.

Dyrhólaey Wildlife

Dyrhólaey has an abundance of birdlife, the most common year-round being Eider Ducks. Iceland’s favourite winged resident, the migratory Atlantic Puffin, can be found here from May to September.

It is one of the best places to reliably locate them, and one of the closest to Reykjavík after the islands in Faxaflói Bay which can be visited by boat from the Old Harbour.

While watching puffins, it is striking how little they seem to fear people, as they allow you to get very close. Be aware, however, they do not like to be touched, and if one flies off in a panic, the whole flock might follow it, so be respectful.

Features at and around Dyrhólaey

From your position atop the promenade of Dyrhólaey, you can enjoy staggering views over Iceland’s black sand beaches, complemented by the glittering waves of the Atlantic on one side, and distant mountainscapes to the other.

The most notable stretch of coast here is called Reynisfjara, renowned for its incredible geology, with the sea-stacks of Reynisdrangar jutting up out to sea. If you visit this beach while seeing Dyrhólaey as part of a South Coast adventure, be sure to follow the warning signs and stay away from the water as dangerous sneaker waves here are commonplace.

To the north, you will also able to see the creeping glacier, Mýrdalsjökull. This amazing ice cap conceals a secret; beneath its surface is one of the most explosive and notorious volcanoes in all of Iceland, Katla. Long overdue, experts say that it is a matter of when - not if - it will erupt over the coming years.

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

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.

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.

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.

Þingvallavatn (anglicised to Thingvallavatn, ‘the Lake of the Fields of Parliament’) is a rift valley lake located roughly forty-minutes drive from Iceland’s capital city, Reykjavík.

Features of Thingvallavatn

Þingvallavatn is partially within the boundaries of Þingvellir National Park, Iceland’s oldest National Park and only one with UNESCO World Heritage Site status.

Covering an area of 84 square kilometres (32 square miles), Þingvallavatn is the largest natural lake in Iceland with its greatest depth measuring at 114 metres (374 feet). Þingvallavatn is situated on the Mid-Atlantic Rift, on a part of the ridge known as the Reykjanes Ridge.

The lake has only one outflow, the river Sog.

Of particular note to biologists and fishermen are the four morphs of Arctic Char that inhabit the lake. The lake’s char are an excellent example of species evolving to fit and adapt to a secluded environment; over ten thousand years, one species of Char has transformed into four different-sub branches. Other fish in the lake include the the Brown Trout and the Three-Spine Stickleback.

History and Geology

Þingvallavatn takes its name from the historical founding of the Alþingi, which occurred in 930 AD at what is now known as Þingvellir National Park. Þingvellir literally translates to ‘Fields of Parliament’.

The Alþingi was the first democratically elected representative parliament in world history (examples such as Ancient Athens were direct, not representative, democracies); Icelanders used to travel by foot or horseback simply to congregate at Þingvellir where they would hear the latest laws and judgements of the island.

Þingvellir National Park is also notable for its geology. Given its position on the Mid Atlantic Ridge, the park is one of the only places on the planet where visitors can see both the North American and Eurasian tectonic plates standing exposed from the earth.

Footpaths allow you to get up close and personal to the plates, standing right where the ancient settlers once did. In between the tectonic plates lies fields of dried volcanic rock, blanketed with a thick, yet fragile layer of Icelandic moss.

Scuba Diving in Thingvallavatn

Scuba diving around Þingvallavatn revolves around two sites, Silfra Fissure and Davíðsgjá (David’s Crack), the former being one of the most popular spots on the planet for snorkelling and underwater exploration.

Silfra Fissure is situated between the North American and Eurasian tectonic plates and is filled with crystal-clear glacial water originating from the Langjökull ice cap. The water measures at between two degrees Celsius all year round, with a slight current preventing the fissure from ever freezing over.

Davíðsgjá is found within Þingvallavatn and is often considered the darker and more dramatic cousin of Silfra Fissure, resembling the gorge formation so prevalent across the Mid Atlantic Rift.

Only certain tour operators provide tours into Davíðsgjá, so make sure to do some research beforehand if you are looking to access this dive site during your time in Iceland.

Húsafell is a large farm and church site in the Borgarfjörður district of West Iceland. With incredible natural beauty, it has been a popular resting spot for travellers since the earliest days of the country.

History of Húsafell

Húsafell is quite inland for an Icelandic settlement, made possible due to the fertile lands and relative lack of eruptions in the area. In spite of its distance from the coast, fishing has always been popular due to the trout lakes and salmon rivers within it.

A rectory once stood on the farm, gaining it fame as a location across the country when it was in its deepest religious throes, although all that remains now is a church.

The settlement was also well known for being somewhat of an oasis for weary travellers. Those travelling from regions such as the north, the Westfjords, and the Snæfellsnes Peninsula, on their way to and from Reykjavík or Þingvellir National Park, would often find that this was one of the very few places en route they could comfortably find refuge and food.

Due to Iceland’s harsh conditions, it became very taboo to turn down a houseguest, although to counter this, due to its scarcity of resources it was also taboo to stay longer than three days.

Húsafell gained a new reputation in the 19th Century when a colony of artists, including Jóhannes S. Kjarval, perhaps the country’s most important painter, lived and worked there. It has continued this tradition for art, with sculptor and musician Páll Guðmundsson being its most famous current resident.

Guðmundsson is best known for his carvings of stone faces, and for the stone harps he has created. He has played these alongside the internationally acclaimed Icelandic band, Sigur Ros.

Services and Features of Húsafell

Today, Húsafell is most popular and well-known as a camping location. There are many campsites, cabins, bungalows and holiday homes to be rented in the area, making it very popular amongst both locals and travellers. The old farmhouse, dating back to 1904, is also now a hotel.

Hiking is very popular, due to the beautiful birch forest of Húsafellsskógur; due to the fact that Húsafell is reasonably sheltered, the trees here can reach four metres (13 feet) tall, which is unusual in Iceland. Because of the force of the wind, Icelandic birch tends to form more like a gnarled bush.

This forest grows from a lava field, where geothermal pools can be found.

The dramatic mountain Tengil also provides many hiking opportunities; it was this mountain that named the area, with ‘húsa’ meaning home and ‘fell’ meaning ‘mountain’.

Húsafell is also blessed with its proximity to many incredible natural features of Iceland. Two of the most significant of these are the waterfalls Hraunfossar and Barnafoss, which are located right beside each other. Hraunfossar trickles in many tiny streams from a wide plateau of jagged lava rock, while Barnafoss rushes down a narrow valley with daunting force.

The highest flowing hot spring in Europe, Deildartunghver, is also found nearby.

For those seeking to explore the Snæfellsnes Peninsula or Westfjords, Húsafell provides a great location to spend the night before, putting you closer to both locations.

Reynisfjara is a world-famous black-sand beach found on the South Coast of Iceland, just beside the small fishing village of Vík í Mýrdal.

With its enormous basalt stacks, roaring Atlantic waves and stunning panoramas, Reynisfjara is widely considered to be the most beautiful example of Iceland’s black sand beaches. In 1991, National Geographic voted Reynisfjara as one of the Top 10 non-tropical beaches to visit on the planet.

Reynisfjara is found around 180 kilometers (112 miles) from Iceland’s capital city, Reykjavík, and is a popular stop-off for those taking a sightseeing tour along the popular South Coast.

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

Folklore

Upon visiting the beach, travelers will immediately observe rocky sea stacks sitting off the shoreline, known as Reynisdrangar.

According to local Icelandic folklore, these large basalt columns were once trolls trying to pull ships from the ocean to shore. However, these trolls were dim and went out too late in the night; dawn broke on the horizon, turning the trolls into solid stone.

Another legend tells of a husband whose wife was kidnapped and killed by two trolls. The man followed the trolls down to Reynisfjara where he froze them, ensuring that they would never kill again.

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

The sea stacks themselves are home to thousands of nesting seabirds. Species that can be found here include puffins, fulmars and guillemots, making it a must-see location for all birdwatchers out there.

Surrounding Sites

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

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

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

Potential Dangers

Visitors to Reynisfjara must be made well aware of the potential dangers present at the beach. First of all, the rolling, roaring waves of Reynisfjara are particularly violent, often pushing far further up the beach than many would expect.

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

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

Aside from these sudden and dramatic shifts in the tide, the rip currents offshore are infamous for their strength and ability to drag helpless people out into the freezing cold open ocean. A number of fatal accidents have occurred at Reynisfjara, the last of which occurred in January 2017.

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

History of Hellnar

Historically, the settlement was a hub of activity, with many trading and fishing vessels pulling in and out of the harbour daily. There were many farms around the area, and by 1703, 38 houses.

Though by modern international standards this was nothing, it was rather significant for Iceland at the time.

Throughout the nineteenth and twentieth centuries, however, Iceland began to develop and industrialise, and its fishing and trading industries began to move to Reyjavík, bringing with them many people.

Hellnar, therefore, rapidly lost its population and importance, like many other places in Iceland particularly on the Snӕfellsnes Peninsula. The change in the economy hit Hellnar particularly hard, however, considering it was increasingly neglected for the neighbouring village of Arnarstapi, which was favoured by the ruling Danish.

The settlement was abandoned but for a few farms and a few resilient locals, until tourism began to boom in Iceland. Now, it is a centre for visitors in the area, with many options for rural accommodation.

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

Sites near Hellnar

At the shores of Hellnar are spectacular rock formations; much of the Snӕfellsnes Peninsula is incredibly dramatic along its coast, due to the previous volcanism of the area and the waves shattering the brittle lava rock that makes up the land.

Most notable amongst these that can be reached on foot is a protruding cliff called Valasnös. It has tunnels into the cliff, and its colouration is affected by the time of the day, the movements of the sea, and the prevailing weather conditions.

Large colonies of birds nest in the area, although it should be noted that puffins do not.

Hellnar, located at the tip of the peninsula, is a convenient hub for those travelling in their own car, offering easy access to the incredible natural sites nearby. These include the Lóndrangar sea stacks, the mountain Kirkjufell, and the Ytri Tunga seal watching beach.

Like many other places on Snӕfellsnes, it is easy to see the beautiful glacial capped volcano Snӕfellsjökull from the village.

Arnarstapi is a village on the southern side of the Snæfellsnes peninsula, once a fishing hub and now a place for travellers to refuel before entering Snæfellsjökull National Park. The area has several old and charming houses with interesting stories to them and is renowned for its beautiful nature.

History of Arnarstapi

Records of settlements around Arnarstapi date back to the Bárðar saga Snæfellsáss, an ancient Icelandic Saga that tells of the half-human, half-ogre who once lived on the Snæfellsnes peninsula. Since his death, he has been considered the area's guardian spirit.

The region was popular with settlers due to its natural harbour, meaning fishing in the rich herring grounds of the surrounding waters was easy. When Norway, and to a much greater extent when they took over, Denmark, were in control of Iceland, Arnarstapi grew increasingly as a trading port.

Denmark invested a lot of money into Arnarstapi throughout the eighteenth and nineteenth centuries (for their own interests, unfortunately not those of the Icelanders). Many of the resulting buildings still stand today, being some of the oldest in the country, such as the Danish Prefect’s Residence, which was built in the 1770s.

In the industrial revolution, Arnarstapi’s population radically shrunk which was common in the countryside at this time. The vast majority of Iceland’s jobs were now centralised in Reykjavík, reducing opportunities for small-time fishermen and their businesses, and the town became little more than a hamlet as a result.

As Iceland’s infrastructure rapidly improved after independence in 1943, and more people abroad began to see the many wonders of this island as a travel destination; Arnarstapi, like many other settlements in the area, got a new lease on life.

Fishing and trade remain vital parts of the economy, but they now play second fiddle to tourism and services. The village has essential services for those travelling on the peninsula, a wide array of accommodation options, and tour companies operating from it.

Nature and Sites around Arnarstapi

The beach at Arnarstapi holds a particular attraction. It has an eroded circular stone arch, called Gatklettur, and here, the interplay of spectacular waves and the light of the sun create a fascinating spectacle. Large colonies of the arctic tern also nest in the area, and both these features make it very popular amongst photographers.

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

Arnarstapi, however, should never be too long a stop on a tour of the peninsula. As lovely as it is, the natural attractions nearby simply warrant more time. The village, for example, sits on the cusp of Snæfellsjökull National Park, home to the Snæfellsjökull glacier and volcano, the beauty of which has inspired writers and artists for centuries.

This is one of only three National Parks in the country, but it is to the credit of the peninsula’s beauty that it is far from the only must-see destination around. Very close to Arnarstapi is the Lóndrangar basalt cliffs, huge towers of lava that from a distance look like a fortress.

Vatnshellir and Sönghellir and two nearby lava caves (the former of which can only be entered on a guided tour). There is also a beautiful cleft in a mountainside called Rauðfeldsgjá Gorge that it is possible to climb into.

Though a little further away, on the north of the peninsula, Kirkjufell mountain is also a wonderful site to behold.

Kerið is a volcanic crater lake in the Grímsnes area of South Iceland. It is close to the three major sites that comprise Iceland’s world-famous Golden Circle sightseeing route and thus makes for the perfect detour for those on visiting these landmarks.

Kerid and the Golden Circle

The Golden Circle is Iceland’s most popular tourist route. Its three main highlights are Gullfoss, or the ‘Golden Waterfall’; the Haukadalur Geothermal Valley, with its many springs and geysers; and Þingvellir National Park, the only UNESCO World Heritage Site on Iceland’s mainland and the birthplace of the country’s parliament.

There are several tour operators who offer trips to the Golden Circle. Many of those define their tours from others with extra stops, and Kerið crater is the most popular of these. It is approximately 40 minutes drive from Þingvellir and Haukadalur in different directions, providing visitors with two routes by which they can return to Reykjavík.

If travelling to Kerið crater alone, please be aware that there is a small entrance fee, of 400 ISK (about two Euros, or three US dollars). This is only to help the landowners preserve and protect the crater; after all, it is on privately owned land.

Other sites you may want to detour on when travelling the Golden Circle are the Sólheimar ecovillage, the Fontana Spa in Laugarvatn, the Secret Lagoon in Flúðir, and the Friðheimar tomato and horse farm.

Geology of Kerid

Kerið is approximately three thousand years old, making it roughly half the age of most volcanic calderas found in Iceland. This is the major reason as to why Kerið’s slopes are red in colour, rather than a volcanic black; the iron deposits are, geologically speaking, fresh.

This vivid redness is part of the appeal of visiting this crater. The crimson rocks contrast dramatically with their surroundings, particularly the intense azure colour of the waters within the crater lake, and the verdant bursts of vegetation.

Kerið is approximately 55 metres (180 feet) deep, 170 metres (558 feet) wide and 270 meters (886 feet) in circumference. It is possible to take a path right to the crater’s edge, to fully encircle it, and to descend down to the pristine waters of the crater lake.

Many crater lakes can be found in nearby, a region known as Iceland's Western Volcanic Zone. The area surrounding it is of barren, stark lava fields, further illustrating the volcanism of the region.

Scientists believe that Kerið was once a cone-shaped volcano. Upon eruption, it is widely believed that the volcano depleted its magma reserve, causing the foundation to fall in upon itself and result in the formation it has today. Of course, this was two thousand years before settlement, so no one is quite certain.

At some point in the centuries following the collapse, Kerið crater filled with water. The resulting lake is between seven and fourteen metres deep, depending on the time of year and the amount of rainfall.

The reason why the lake is so vividly coloured is that of the minerals from the rocks, seeping into and dyeing the water the aquamarine colour for which it is renowned.

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

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

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

Dangerous Waves

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

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

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

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

Folklore

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

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

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

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

Surroundings & Wildlife

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

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

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