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Skogafoss is one of the biggest and most beautiful waterfalls of the island with an astounding width of 25 meters and a drop of 60 meters.
This is one of the most popular waterfalls in Iceland for travellers to visit. It is located in South Iceland, not far from Skogar, which itself features a highly interesting regional museum. Due to the amount of spray the waterfall often produces a single or double rainbow on sunny days.
Seljalandsfoss in the river Seljalandsa in South Iceland is one of the most sought waterfalls in the country.
Seljalandsfoss has a narrow cascade but is one of Iceland's highest waterfalls, at 63 meters. The waterfall is highly picturesque and has the rare distinction that one can actually walk behind it.
Mýrdalsjökull is a glacier in the south of the Icelandic highlands. It is the country's fourth largest ice cap, covering nearly 600 square kilometres (232 square miles), and its highest peak is almost 1500 meters tall. It is most well-known for sitting atop the notorious and explosive volcano, Katla.
Mýrdalsjökull is visible from Route 1 on the South Coast, sitting to the north of the village of Vík. It is visited on some snowmobiling, ice caving and helicopter tours, and one of its glacial outlets, Sólheimajökull, is the most popular place in the country for ice-climbing and glacier hiking.
Eruptions beneath Myrdalsjokull
Since 2010, the world has known of the volcano beneath Eyjafjallajökull; after all, it halted European air travel for over a week and stumped news readers everywhere. Few, however, are aware of the much larger volcano right beside it.
Mýrdalsjökull conceals Katla, one of the country’s most active volcanoes, having erupted, on average, once every fifty years since 930 AD. Because of the glacier above it, these eruptions tend to cause enormous ash clouds. It is these ash clouds that lead to flights being grounded, crops and livestock poisoned, and have the potential to change the world’s climate.
The last major eruption beneath Katla was in 1918, in which such huge lahar floods occurred that the southern coastline was extended five kilometres outwards. This area is also very susceptible to glacial floods, or 'jökulhlaup', during eruptions, even when the lava does not break through the surface of the ice. These are as dangerous as the lava itself, having wiped out whole Icelandic villages before.
Historically, the area was little settled for this reason.
Katla is connected to the same volcanic system as Eyjafjallajökull and usually erupts violently a few years after Eyjafjallajökull does. As the ex-president, Ólafur Ragnar Grímsson said in 2010:
‘The time for Katla to erupt is coming close… it is high time for European governments and airline authorities all over Europe and the world to start planning for the eventual Katla eruption’
So it is currently several years overdue. Katla is monitored heavily, and roads around it closed when seismic activity increases. All road closures around Iceland can be found on Road and Coastal Administration's website.
Tours on Myrdalsjokull
While there are no eruptions immediately imminent, tours continue to run onMýrdalsjökull, allowing visitors to enjoy the glacier. It is, for example, possible to snowmobile across its surface throughout the year and take ice caving tours beneath it from October to April, with departures from both Reykjavík and Vík.
Considering the ice caves under Vatnajökull glacier are usually only accessible from November to March, this provides a wider window of opportunity for travellers to Iceland outside of the depths of winter. It should be noted that the caves in Mýrdalsjökull do not have the same blue ice, however.
Tours around Myrdalsjokull
Mýrdalsjökull can be seen on all South Coast tours that reach Vík and beyond in clear weather. It can also be seen from above on helicopter tours that depart from Reykjavík.
The best perspectives of the glacier, however, can be found on the popular Fimmvörðuháls hiking trail, which goes between Eyjafjallajökull and Mýrdalsjökull. Part of this hike can be done in a day, or you can take the complete route from Þórsmörk to Skógar on a three-day trek
Sólheimasandur is a vast area of sand and gravel along the South Coast of Iceland, between the cliffs of the interior and the modern shoreline. It was built up by immense glacier bursts sweeping from the mountains to the shore.
Geography of Sólheimasandur
Sólheimasandur is a glacial outwash plain, meaning when that when eruptions happen under the nearby glacier, Mýrdalsjökull, the floodwater rushes across this land for the sea.
A glacial flood, otherwise called Jökulhlaup (one of two words taken from Icelandic in the English language, the other being geyser) is perhaps the most dangerous immediate element of an Icelandic eruption. While individuals have been killed by lava flows and bombs, many more have lost their lives to the water.
For this reason, Sólheimasandur has no significant settlements, all the way from the village of Vík í Mýrdal to Kirkjubæjarklaustur. The whole area is vulnerable to glacial floods, which are still notoriously unpredictable to modern science.
This is especially the case considering that the volcano beneath Mýrdalsjökull, Katla, is Iceland’s most active volcano, which carries a reputation for violently erupting, seemingly at random.
Even if these eruptions do not break the surface of the ice, they can still cause devastating floods. In fact, these can even be more dangerous, as these eruptions are often not detected..
If Katla is showing signs of waking, then the Ring Road going south across Sólheimasandur is often closed.
In spite of its dark reputation, Sólheimasandur is a place of ethereal and haunting beauty. Entirely flat, composed of black sands, it is often compared to a lunar landscape, or else some kind fantastical desert. The views of Mýrdalsjökull, Vatnajökull, the Highlands and the South Coast are also magnificent in clear weather.
Sólheimasandur is easy to reach, laying on the Ring Road that encircles the country.
The DC-3 Plane Wreckage
Wikimedia, Creative Commons, Photo Credit: Sekeri
One of the most impressive sights on Sólheimasandur is the DC-3 plane wreckage. Lying abandoned in the sand, a deteriorating skeleton, with nothing but endless black sand surrounding it, it makes an eerie destination even more ominous.
It is a US Navy plane, that was flying across the area in 1973; until recently the US had a NATO base at Keflavík, as Iceland has no armed forces of its own. It seemed to run out of fuel - although it was later discovered that the pilot had, in fact, switched to the wrong fuel tank - and had to make an emergency landing.
Thankfully, no one was killed or injured, although the plane was far too damaged to be repaired.
Because there were no deaths or injuries, there is nothing tasteless about taking photos with the plane. In fact, it a popular addition to many South Coast tours. Because the wreckage is not expected to remain there for long - considering the regular glacial floods that rush through the area - it is fine to touch it. It is not recommended that you climb on it, however, for safety reasons.
To reach the plane requires a short walk across Sólheimasandur.
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.
The DC Plane Wreck is a famous site located in South Iceland, its rusting shell laying on haunting black sands. The wreckage is a particularly beloved spot by local and visiting photographers alike thanks to its sparse and wild surrounding landscape and its incredible visual contrast to the aircraft’s gnarled metal.
History
The aircraft, a Douglas R4D-8, a Super DC-3, was originally in possession of the US Navy and considered to be a symbol of the golden age of air travel.
Originally utilised as a cargo aircraft, the US Navy was routinely flying over Iceland during the 1970s as a part of its unilateral defence agreement with the country. Iceland is a NATO member, and US forces had a permanent base on the island until 2005.
The aircraft crashed into Sólheimasandur on Wednesday, November 21st, 1973, at around 14:00 as reported by the Aviation Safety Network. It was flying from Höfn in Iceland's east coast and onboard were seven crew members.
No one is quite sure why the plane crashed, with several theories flying about. Some blame it on icing damaging the plane’s structure; others say that the thrusters were not working correctly. Some say that it was a mishap of the pilot who believed the thrusters were not working when they were.
Regardless, it little matters as no one was injured in the crash. The forced landing was made on an icy river by the coast, and though the ice broke, the plane didn't sink.
In the years since its rocky landing, the DC Plane Wreck has borne the brunt of Iceland’s tempestuous weather; heavy rainfall, freezing and powerful gales. Today, the aircraft’s wings are no longer attached, and it has only half a tail (rumours stipulate that a local farmer cashed in on the tail long ago.)
It is not expected that the plane wreck will be there forever. Sólheimasandur is a glacial outwash plain, meaning when there is an eruption underneath the glacier Mýrdalsjökull, there is a chance floodwater could wash it away.
It truly is a case of ‘when there is an eruption’, not if, as Mýrdalsjökull covers Katla, one of the country’s most explosive and regular volcanoes.
Getting There
If you are looking to visit the DC Plane Wreck, you could join an organised hiking, horse riding or ATV riding tour that takes you right up to the site.
Alternatively, you could choose to find the wreckage yourself. To reach it requires a walk, however, as driving over the sands is considered to be driving off-road, and incredibly heavy fines are attached to this.
A recently built car park by the main road allows visitors to leave their vehicles and proceed their way over to the wreck, taking approximately two hours.
It should also be noted that as this is not a natural attraction, nor is it a permanent feature, and thus visitors should not be too concerned about climbing it for photographs. Icelanders themselves are not sensitive about this, and will likely be seen clambering up it for a shot themselves.
However, do take extra precautions when moving around the wreck in order not to hurt yourself on the metal.
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