Wycieczka helikopterem - wulkany, lodowce

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.

Nestled between the glaciers Eyjafjallajökull, Mýrdalsjökull, and Tindfjallajökull is Þórsmörk, the Valley of Thor. A nature reserve in the southern Icelandic highlands, Þórsmörk is one of the country's most popular hiking destinations and a favourite location for photographers and nature lovers alike.

Strictly speaking, Þórsmörk is a valley and a mountain range between the Krossá, Þröngá, and Markarfljót rivers.

Locals, however, often use the name ‘Þórsmörk’ when referring to a much larger region that is composed of the area between Þórsmörk proper, and the Eyjafjallajökull glacier volcano, the peak that notoriously erupted in 2010 and caused widespread disruption to air traffic in Europe.

Landscapes and Geology

The contrasting vistas of lush oases and roaring glacier rivers cutting through black desert expanses not only make Þórsmörk unique in Iceland but to the entire world. Parts of the valley are rich with moss, fern, and birchwood, while jagged mountain ridges and ice-capped peaks crown the horizon.

The valley's climate is warmer and calmer than usual in south Iceland, which often causes Þórsmörk's mountains to be cloaked in a veil of mist that materialises when the warm valley air ascends and mixes with the descending cold breath of the glaciers above. This is due to the colossal peaks that both surround and shelter it.

In spite of being warmer, Þórsmörk is also wetter than the rest of the country. This, however, only brightens the vegetation, giving the area a lush, emerald hue.

Activities

Þórsmörk's surrounding hills, slopes and mountains are beset with small valleys and gullies that make for some of Iceland's most astonishing hiking routes.

Experienced hikers, therefore, have a wealth of trails to trek, varying in distances and difficulty. In fact, Þórsmörk offers two of the most popular trails in Iceland, the Fimmvörðuháls and the Laugavegur routes.

Fimmvörðuháls is a 30 kilometres (19 miles) trail that takes you into the hills beneath the Eyjafjallajökull glacier volcano and to the volcanic craters Magni and Móði, which erupted during the 2010 eruption. You can feel the lingering effects of the volcano by feeling heat still rising from the lava rock.

The 55 kilometre (34 miles) Laugavegur path takes you from Þórsmörk to the Landmannalaugar geothermal area, which is home to an incredible wealth of hot springs and rhyolite mountains of vibrant colours.

A short but demanding hike from Þórsmörk up Mt. Útigönguhöfði is suitable for those who are looking for stunning views and don't mind a little physical challenge.

Accommodation and How To Get There

During winter (October 16th to April 30th) the road into Þórsmörk is impassable. In summer (May 1st to October 15th) a special four-wheel-drive mountain bus runs three times per day from the BSÍ bus terminal in central Reykjavík.

Once there you have the choice of setting up base in a small hut in Húsadalur valley, a private room or a dormitory in Langidalur valley, or to camp in Þórsmörk's campsite. Please note that the huts, private rooms and dormitories must be booked well in advance.

Of course, when the roads are clear, it is possible to drive there yourself. As with all cases with driving in Iceland, however, ensure that you are comfortable with the vehicle you have and your driving skills before setting off.

The Westman Islands, or Vestmannaeyjar, are an archipelago of 15 islands and 30 rock stacks off the South Coast of Iceland. Aside from their incredible natural beauty, the islands have the world’s largest population of nesting puffins in summer, and a fascinating history.

History of the Westman Islands

The history of the Westman Islands is as dark as it is intriguing, beginning at the very start of Iceland’s history, with the first family to settle here.

The first person renowned for permanently settling Iceland was a man called Ingólfr Arnarson (although it should be noted that he hardly came alone; he was accompanied by his wife Hallveig Fróðadóttr and several slaves). His half-brother joined him in the country, a few years later, but met his death at the hands of two of his own captured men.

These slaves attempted to flee and hide, to escape Arnarson’s vengeance. They reached the Westman Islands, but unfortunately, were found by ‘Iceland’s father’ and killed in retribution.

The islands since have been named after these men; they were Irish slaves, and at the time, the Irish were called ‘Westmen’, as Ireland was thought to be the westernmost landmass before Iceland’s discovery.

This brutal beginning would be a hint at the later events to occur on and shape the archipelago.

The largest island, Heimaey, was settled in the early era, and the people on it lived off the fertile oceans, puffins, and eggs. Life was challenging but manageable, until a terrible tragedy occured in 1627.

At the height of the Ottoman Empire, it was Barbary Pirates from Algiers who ruled the seas, and they managed to find their way to this little island. They took control of it for three days, before setting off back home with 237 slaves.

The vast majority of these lived out the rest of their lives in bondage, though some were ransomed back in 1638.

The trials of the voyage and their captivity was captured in a novel by a priest who managed to escape in 1628.

Unfortunately, this was not the last major calamity to befall the islands.

In the 20th Century, it seemed that the Westman Islands had overcome their hardships, modernising and better connecting to the mainland. That, however, was to be overturned in 1974.

At 01.55, on January 20th, a fissure tore open in the middle of the town of Heimaey and the previously unknown Eldfell volcano began to violently erupt. In hours, it had torn across the island, spurting fountains of lava height in the air and pouring noxious gasses into the atmosphere.

Unbelievably, however, no-one was killed. There was an emergency plan for a situation such as this, and thankfully, storms the days before meant that the whole fishing fleet was docked in the harbour. The entire population of the island was taken to safety.

That is not to say, however, that the work was done. 5,300 peoples’ homes were in the town, and the Icelandic authorities were desperate to do what they could to help protect them. At the time, the US had a NATO base in the country, and their help was enlisted.

By pumping seawater onto the great lava fronts, it was possible to cool the molten rock, slow it, and change its direction.

This innovative, previously unused technique was particularly effective when it came to protecting the harbour. It seemed at one point that the eruption may have closed it entirely, effectively destroying the island’s economy, yet by spraying the lava, the harbour was actually enclosed more and improved.

When the eruption ended, the island slowly repopulated to about 85 percent of its previous population; about one fifth of the buildings were destroyed.

The town, however, now had a long stretch of new land to build a runway on, and a volcano in its centre to draw guests. Ever since, the Westman Islands have recovered as a popular tourist destination.

The Westman Islands today

Today, the Westman Islands attract thousands of visitors of years, for a variety of reasons. Many wish to visit the Eldborg crater and learn about the eruption in depth at the Eldheimar Museum. Others come for the incredible nature opportunities.

First and foremost amongst these are the chances for puffin watching. Ten million puffins nest in Iceland between May and September, and more of them come to the Westman Islands than anywhere else.

They nest in the cliffs, crags and sea-stacks, and can be easily seen by travelling on foot or by boat. Towards the end of the season, many of the pufflings get confused by the lights of the town as they try to make their way to the ocean, and end up in the streets; it is thus a local tradition amongst the children to collect them and throw them in the sea.

Some business-savvy young ones used to even collect them up, and ‘sell’ them to tourists to release.

The puffins are just one of the thirty or so species that nest on the islands but by far the most abundant.

The Westman Islands also boast some of the best whale-watching opportunities in the country, with Fin, Minke and Humpback Whales seen often in summer, and Orcas throughout the year.

Heimaey itself is home to the worlds first beluga whale sanctuary. In exchange for a donation fee to the charity, visitors can meet Little White and Little Grey in their home in Klettsvik Bay.

Getting to the Westman Islands

The ferry Herjolfur sails to the Westman Islands from the town of Landeyjahöfn, on the south shore of Iceland, for the shortest journey. In poor conditions, particularly between November and March, it may instead leave from  Þorlákshöfn. It is also possible to fly to the islands from Reykjavík Domestic Airport.

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.

Hengill is an enormous mountain in south-west Iceland, covering an area of about 100 square kilometres. It is a vital source of energy for south Iceland

Energy at Hengill

Hengill is an active volcano, although there has not been an eruption here for about 2,000 years. In spite of that, there is still lava close to the surface, evidenced by the steaming fumaroles and many hot springs dotted across it.

Iceland’s electricity and heated water comes from entirely renewable sources, taken from places such here. There are two power stations harnessing the energy potential at Hengill, called Nesjavellir and Hellisheiði.

Certain Golden Circle tours include stops at these.

Popular sites at Hengill

The energy beneath Hengill does not only help Iceland with its electrical and heating needs; it also helps with tourism. The geothermal activity of the volcano has created some of the country’s most popular sites.

Most significant of these are Hveragerði town and the adjacent Reykjadalur valley. Hveragerði is often named the ‘hot spring town’ or the ‘earthquake town’ because of the amount of volcanic activity Hengill creates here.

Boiling water runs mere feet beneath the surface of the earth, meaning there are steaming fumaroles all around. Chefs cook simply by burying their food into the earth, leading to an interesting restaurant culture. There is also an exhibition on the town’s earthquake history.

On that note, activity at Hengill has historically caused no end of trouble for the residents of Hveragerði. Though the houses are built to be earthquake proof now, there is little that can be done about the boiling water when it rises. It regularly causes surprise hot springs to rise inside people’s homes.

Reykjadalur can be hiked through from Hveragerði, and is one of Iceland’s easiest, most accessible, and rewarding trails. After walking for an hour or so through a beautiful range of mountains, visitors will come to a river fed by both boiling and rain water.

This mix means that guests can find the perfect points to bathe, based on how warm they want it. The surrounding area is dotted with boiling mud pits and steaming vents.

Hengill is located south of Þingvellir National Park, one of the sites of the Golden Circle. One of the best ways to see the scale of it is to approach the park from Reykjavík, and stop on top of the Almannagjá Gorge.

This gorge runs from north to south, and looking south, there is no missing the slopes of the volcano across the lake Þingvallavatn.

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...

Fimmvörðuháls Pass is one of Iceland's most popular hiking trails. It made the world news when the Eyjafjallajökull eruption started here in 2010, but now is best renowned for its incredible, stark nature.

Hiking at Fimmvörðuháls

Fimmvörðuháls is located in south Iceland, and is part of the highly popular, multi-day hike, the Laugavegur trail. It can be trekked as part of this, which goes from from Landmannalaugar to Þórsmörk valley, or independently in a day.

The trail is located between glaciers Eyjafjallajökull and Mýrdalsjökull and lies from Skógar to Þórsmörk valley. It is about 22 kilometres (14 miles) long, and requires a 1000 metres (0.6 miles) ascent.

It is therefore only recommended that those with a good level of fitness, with decent hiking boots and adequate supplies, take the route. It is also not recommended you hike without a guide, unless you are a very experienced hiker and people know where you are going and when to expect your return.

The trail offers breathtaking and diverse scenery. The view down to the verdant and dramatic Þórsmörk, and of the many waterfalls of the river Fossá, are being particularly of note. Part of the trail is often snowy, as the glaciers meet it at either side.  

The Morinsheiði plateau offers a stunning view of the ice cap Mýrdalsjökull, which conceals one of the country’s most dangerous and unpredictable volcanoes, Katla.

The weather can be unpredictable in these parts so caution is advised; it is important to check the forecast before leaving for any destination in Iceland, but, due to the difficult terrain here, it is especially vital.

The 2010 eruption at Fimmvörðuháls

In 2010, the world watched as the glacier Eyjafjallajökull erupted, pouring vast amounts of ash into the atmosphere. Farms were poisoned across the south of the county, those with respiratory problems were confined indoors, flights were grounded and newscasters everywhere twisted their tongues trying to pronounce it.

Few know, however, that this eruption succeeded a smaller one at Fimmvörðuháls.

On the 20th of March, at 23:00, a 0.5 kilometre (0.3 mile) fissure opened to the north of the pass. A week later, it started again, and began to form in two craters near Þórsmörk.

The lava flow died down, but were unfortunately only a sign of what was to come on the 14th of April. Air traffic all but halted across Europe for six days, and some routes were closed even into May.

The new craters were named Móði and Magni on the 15th of June, after the sons of Thor, a fitting name considering they were situated next to ‘the Valley of Thor’. They are two of the youngest craters in the country.

They are visited on most hikes through the area, and particularly interesting due to the face that they still emanate heat. Snow cannot settle on the rocks here, and on cold days, they often appear to be steaming.

This is due to the fact lava takes years to fully cool. If you put your hands on the stone here, you’ll find them warm even in cool weather.

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

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

Geography, Nature & Wildlife

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

Underneath the soil rests a vast lava field, known as Þjórsárhraun. Its edges reach several hundred metres offshore where the ocean waves crash upon them, thereby protecting the lowland from the invasion of the sea. This results in the South Coast being unusually lacking in the deep fjords that so distinctly characterise the rest of Iceland's shoreline.

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

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

Highlights of the South Coast

The South Coast offers an unprecedented array of natural wonders that draw thousands of visitors each day.

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

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

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

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

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

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

While almost all of these sites can be seen from Route 1, they make up a fraction of what the South Coast has to offer. The vast sand plains of Sólheimasandur are home to a crashed DC-3 Plane Wreck, and within the Vatnajökull National Park is the dramatic Skaftafell Nature Reserve.

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