The Full Monty Private Helicopter Tour
Visit South Iceland's most astonishing natural highlights with this amazing private helicopter tour! This is the perfect option for guests looking for a truly eclectic experience, including adrenaline pumping action, epic travel and truly gorgeous scenery.
Your 9-hour tour will begin on location at Hangar 6, Reykjavík Airport (note that there is no pickup available for this tour.) There, you will meet your highly experienced pilot and friendly guide, both of whom have received the highest level of professional training. They will run through the tour's itinerary and the helicopter itself, choosing the best fit from their fleet of their excellently maintained aircraft. Your safety and comfort are of the highest concern, meaning the best modern equipment and training protocols are guaranteed.
When everyone is ready, it's all aboard for the adventure of a lifetime!
This tour will take you across a wide array of diverse, mesmerising landscapes. You will visit the largest volcanoes, the longest rivers, the highest mountains and the most staggering glaciers this island has to offer. You will be flown to such destinations as the stunning Þingvellir National Park, the awe-inspiring Katla volcano, the kaleidoscopic hills of Landmannalaugar and even the mighty glacier Vatnajökull, to name only a handful. This tour encapsulates what's best about travelling in Iceland, and neatly includes many other tour packages that are popular in Iceland. But why travel by bus when you can fly by helicopter?
Weather permitting, the pilot will make a number of scheduled stops along the way to take photographs and enjoy the immersive experience of your destinations. In Höfn, you and your group will take a gourmet meal break... preferably fresh lobster! Only luxury on this tour!
So what are you waiting for? Visit the website today to make sure you don't miss out on this incredible, once in a lifetime aerial adventure, visiting the highlights of South Iceland by chopper! Check the booking availability by choosing a date.
- Duration: 10 hours
- Difficulty: Easy
- Languages: English
Reykjavik is the capital of Iceland and the northernmost capital of a sovereign state in the world.
Despite a small population (120.000 and more than 200.000 in the Greater Reykjavik area), it is a vibrant city that draws an ever increasing number of visitors. It is the financial, cultural and governmental centre of Iceland. It also has a reputation of being one of the cleanest and safest cities in the world.
The city of Reykjavik is located in southwest Iceland by the creek of the same name. Throughout the ages, the landscape has been shaped by glaciers, earthquakes and volcanic eruptions and the area is geothermal. Much of the current city area area was subglacial during the Ice Age, with the glacier reaching as far as the Álftanes peninsula, while other areas lay under the sea. After the end of the ice age the land rose as the glaciers drifted away, and it began to take on its present form.
The coastline of Reykjavik is set with peninsulas, coves, straights and islands, most notably the island of Videy, and seabirds and whales frequent the shores. The mountain ring as seen from the shore is particularly beautiful. Mount Esja is the highest mountain in the vicinity of Reykjavik and lends its distinct feature to the whole area. This majestic mountain is also highly popular for climbing. Other notable mountains that can be seen from the seaside are Akrafjall and Skardsheidi and on clear days one may even see as far to the legendary Snaefellsjokull glacier, at the end of the Snafellsnes peninsula.
The largest river to run through the city is Ellidaa in Ellidaardalur valley, which is also one of Iceland‘s best rivers for salmon fishing.
There are no trains or trams in Iceland, but most people travel by car. The city also operates a bus system. There are two major harbours in town, the old harbour in the centre and Sundahofn in the east. The domestic Reykjavik Airport is located at Vatnsmyrin, not far from the city centre and close to Oskjuhlid and Perlan. The international Keflavik Airport at Midnesheidi heath then lies around 50 km from the city. Cars, jeeps and bicycles can be readily rented in the city and many organized tours are also being offered.
What to See & Do in Reykjavik
The local arts scene is strong in Iceland, with both annual events and single ones, many of whom have hit the international stage. For the annual ones please check our articles Best Annual Events in Iceland and the Top Ten Festivals in Iceland. Major events taking place in Reykjavik include the Iceland Airwaves, Gay Pride, RIFF (The Reykjavik International Film Festival), The Reykjavik Literature Festival, Cultural Night, the Reykjavik Arts Festival, Food & Fun, the Reykjavik Fashion Festival and the Sónar music festival.
Among famous people from Reykjavik are artists Bjork Gudmundsdottir, Sigur Ros, writers Halldor Laxness (born in Laugavegur) and Arnaldur Indridason and mayor Jon Gnarr. For more well-known and fairly-well known Icelanders, check our article on the subject.
You might also want to check our article on some of the many things to see and do in Reykjavik, such as visiting the city‘s many museums, exhibitions and galleries, checking out live music, visiting the Harpa music hall or the theatres, visiting the lighthouse at Grotta, the main shopping street of Laugavegur, visiting the old harbour and the flea market, going on a bird- and whale watching tour or visiting Videy island. We also have a top ten list of things to do.
Make sure to visit the public square of Austurvollur, one of the city‘s most popular gathering places, where you‘ll also find the national parliament, Althingi, the state church a statue of independence hero Jon Sigurdson, as well as cafés, bars and restaurants. Austurvollur was central in the 2008 protests, along with Laekjargata, home to the House of Government. You are also not likely to miss the great church of Hallgrimskirkja that towers over the city from the hill of Skolavorduholt, wherefrom you‘ll get a great view of the city.
Try a walk by the city pond, greet the many birds that frequent the area and visit the city hall, stationed by its banks. The Hljomaskalagardur is a beautiful park that lies by the pond, it ideal for a nice walk and sometimes concerts get held there. Further off is the campus of the university of Iceland, the Nordic house and the Vatnsmyri wetland, a particularly pleasant place, but be mindful of not disturbing the wildlife there and keep to the pathways.
For a nice swim on a warm day, we particularly recommend Nautholsvik beach.
Visit the Laugardalur valley, home to one of the city‘s best swimming pools, as well as the Asmundarsafn gallery, a beautiful botanical garden and a domestic zoo. A walk by the Aegissida beach, with it‘s old fishing sheds, in the west part of Reykjavik also holds a particular charm. The aforementioned Elllidaardalur valley is also a popular resort.
Another place that offers one of the city‘s best (and free) views is Perlan, up in Oskjuhlid hill. The hill itself is a popular resort, with over 176.000 trees and great opportunities for walking and cycling.
Travel to Alftanes to see the president‘s house at Bessastadir, which is also a historical site in it‘s own right, having been the educational centre of Iceland for centuries. Nearby is a beautiful lava field, Galgahraun, well worth a visit, though there is currently an environmental struggle going on as to it‘s future state.
The city is furthermore a short drive from many of Iceland‘s major attractions, most famously the Golden Circle and the Blue Lagoon. In close vicinity you‘ll also find the Heidmork preservation area, a favourite pastime resort of the people of Reykjavik, as well as the Blue Mountains, one of Iceland‘s most beloved skiing venues.
Check our Best of Reykjavik guide further for tips on the best cheap things to do in Reykjavik, some of the best restaurants in the city, happy hours, the top ten value places to eat and our two articles on the famous Reykjavik nightlife; Nightlife in Reykjavik and Nightlife and mating.
Finally, we‘d like to stress that these are only some suggestions of the many things you might check out in Reykjavik. Whatever you choose to do, we hope you‘ll be able to make the most of your visit and we wish you a pleasant stay in our capital.
Vatnajökull is the largest ice cap in Iceland and the third largest glacier in Europe, covering 8% of the island's landmass. Vatnajökull Glacier can be found in the south west of Iceland and is a popular spot for glacier hiking and ice caving tours.
Facts about Vatnajökull
- Surface: 8,100 km2
- Average thickness: 400 - 600 m
- Maximum thickness: 1,000 m
- Height: 1,400 - 1,800 m
- Highest peak: 2,200 m (Hvannadalshnjúkur)
Information about Vatnajökull
Vatnajökull Glacier belongs to the greater Vatnajökull National Park, which encompasses the former national parks Skaftafell, in the southwest, and Jökulsárgljúfur, in the north. Vatnajökull's highest summit is Hvannadalshnjúkur which rests on top of a stratovolcano known as Öræfajökull.
Underneath the glacier rests some of the most active volcanoes in the country, the most notable being Grímsvötn, Öræfajökull and Bárðabunga. Volcanic activity in the region has occurred on and off throughout the centuries, and many geologists believe that such a period is overdue for immediate future. If their calculations are correct, it would mean significant volcanic activity for Vatnajökull over the scope of the next half century.
The glacier boasts of over 30 outlet glaciers, which are channels of ice that flow out of ice caps but remain constrained on the sides of the valley. The major outlet glaciers of Vatnajökull include Dyngjujökull in the north, Breiðamerkurjökull and Skeiðarárjökull to the south. To the west, one can find the outlet glaciers Síðujökull, Skaftárjökull and Tungnaárjökull.
Glaciers are in constant motion underneath their weight; as they form over the centuries, the accession of snow exceeds its melting, creating a constant "push" on the ice cap. Each year, due to the melting ice water, new ice caves form that disappear come spring.
- Click here for a selection of Ice Cave tours
Numerous rivers run out of Vatnajökull, making up some of the greatest glacial rivers in Iceland:
- Tungnaá (west)
- Köldukvísl (west)
- Þjórsá (west)
- Jökulsá á Fjöllum (north)
- Skjálfandafljót (north)
- Jökulsá á Brú (north east)
- Jökulsá í Fljótsdal (north east)
- Jökulsá í Lóni (south)
- Hornafjarðarfljót (south)
- Jökulsá á Breiðamerkursandi (south)
- Skeiðará (south)
- Núpsvötn (south)
- Hverfisfljót (south)
- Skaftá (south)
Vatnajökull National Park
Vatnajökull National Park, in its current state, was established in June 2008. The park now covers an area of 14.141 km2, making it the second largest national park in Europe. Vatnajökull National Park has 14% coverage over the whole island of Iceland.
Rivers divide the highland plateau to the north of the park; an area that sees massive glacial flows in the summertime. The volcanic table mountain Herðubreið towers over this particular region, along with volcanoes Askja, Snæfell and Kverkfjöll.
The canyon Jökulsárgljúfur was carved out by glacial floods centuries ago. At the upper end of the canyon, you'll find Dettifoss, the most powerful waterfall in Europe. Further north, the horseshoe-shaped canyon Ásbyrgi is believed to have formed when Óðinn's horse, Sleipnir, stepped his foot down from the heavens.
East around Snæfell, one can find wetlands and ranges, home to roaming herds of wild reindeer and abundant birdlife. Steep mountain ridges make up the south side of Vatnajökull, where outlet glaciers crawl in between the ridges onto the lowlands. The sandy plains of Skeiðarársandur also lie to the south as they reach out to sea. The glacial river Skeiðará runs through this vast desert.
One of Iceland's most visited landmarks is the Jökulsárlón glacier lagoon, which sits at the head of outlet glacier Breiðamerkurjökull. There, large icebergs that have broken off the glacier gather to float in the lake before ending up in the Atlantic Ocean, or on the nearby Diamond Beach.
- Click here for a selection of Jökulsárlón tours
The Future of Vatnajökull
The volume of Vatnajökull reached its peak around 1930 but has since been in a steady process of decline. Because of rising levels of global temperature, approximately over the last 15 years, Vatnajökull has on average lost about a metre of its thickness annually.
If temperature levels continue to rise, the glacier could be all but gone nearing the end of the next century, leaving only small ice caps on top of the highest mountain summits.
Vatnajökull and Jökulsárlón in Popular Culture
- HBO's Game of Thrones (season 2, 2012)
- Batman Begins (2005)
- James Bond: Die Another Day (2002)
- James Bond: A View to a Kill (1985)
Landmannalaugar ("The people's pools") is a vast area of stunning and unique beauty, the true heart of Iceland's southern Highlands.
Landmannalaugar is a truly rare area, both geologically and aesthetically. The area can be found nestled beside the raven-black Laugahraun lava field, a sweeping expanse of dried magma which originally formed in 1477. Landmannalaugar itself is made up of windswept rhyolite mountains, a rock type that creates a full spectrum of dazzling colour on the mountainside. Shades of red, pink, green and golden yellow all change their tone, keeping in movement with the sun rays and creating an area of wilderness that resembles no place else on earth.
Landmannalaugar is primarily known for its natural geothermal baths, hence its name "The People's Pools". For centuries, Landmannalaugar has served as an area of shelter and respite for weary travellers who use these soothing springs as a means to relax after tiring excursions. 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 area marks the northern end of the Laugavegur, one of Iceland's most popular hiking trails. It is also home to many other notable trails, however, including the path onto the mighty Mt. Brennisteinsalda ("Sulphur Wave"). Visitors can also traverse the trail up the Bláhnjúkur ("Blue Peak") volcano, 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 camp sites and a mountain hut equipped with sleeping bags and accommodation for up to 80 visitors.
- Find Highland Tours here
Thingvellir is one of the most important sites to visit in Iceland for its landscape, history and cultural value.
The Icelandic parliament was founded in Thingvellir in 930 and remained there for centuries.Thingvellir is surrounded by a beautiful mountain range and is the site of a rift valley, marking the crest of the Mid-Atlantic range. Today it is a natural park, listed as a World Heritage Site by UNESCO and considered a vital part of the ‘Golden triangle’ (with Geysir and Gullfoss). Of particular note is the magnificent gorge Almannagja, which marks the eastern boundary of the north American plate and into which the beautiful waterfall Oxararfoss falls.
Other notable attractions within the park include the beautiful lake Thingvallavatn, the largest lake in Iceland, the Silfra fissure, one of the world's top dives, and Gjabakkahellir, one of Iceland's most interesting lava tubes.
Myrdalsjokull is a glacier in the south of the Icelandic highlands. It is the country's fourth largest glacier, covering nearly 600 km2. It's highest peak reaches around 1500 meters. Under the icecap is the volcano Katla.
Katla is active and has had at least 16 eruptions since the year 936, usually erupting every 40-80 years. It's latest eruption was in 1918. Myrdalsjokull is to the north of the village Vik and east of the famous Eyjafjallajokull glacier volcano. The popular Fimmvorduhals trail lies between the two glaciers. Due to Eyjafjallajokull's eruption in 2010 the area is closely monitored.
Þingvallavatn (anglicised as Thingvallavatn, “Lake of the Parliament”) is a rift valley lake located roughly forty minutes drive from Iceland’s capital city, Reykjavik.
Features of Þingvallavatn.
Þingvallavatn is partially within the boundaries of Þingvellir National Park, Iceland’s largest national park and only one with UNESCO World Heritage Site status. Covering an area of 84 km², Þingvallavatn is the largest natural lake in Iceland with its greatest depth measuring at 114 m. 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 Althingi, which occurred in 930 AD at what is now known as Þingvellir National Park. Þingvellir literally translates to “Fields of Parliament.” The Althingi was the first democratically elected parliament in world history; 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 at Silfra / David's Crack
Scuba diving around Þingvallavatn revolves around two sites, Silfra Fissure and 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 Langjokull ice cap. The water measures at between 2-3 degrees Celsius all year round, a slight current preventing the fissure from ever freezing over.
David’s Crack 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 David’s Crack, so make sure to do some research beforehand if you are looking to access this dive site during your time in Iceland.
Header Photo: Wikimedia. Creative Commons. Credit: Axel Kristinsson.
Hofn a Hornafirdi, is a fishing town in southeast Iceland, with a population of 1641 (as of 2011). It has a strong harbour and its main industries are fishing and tourism.
Of note are several interesting museums and the annual Humarhatid (lobster festival). The area is also rich and varied birdlife and migratory birds from Scotland land here around April and leave around August/September.
Katla (meaning “Kettle”) is one of Iceland's largest and most active volcanos. Situated in south Iceland, Katla is partially buried underneath Mýrdalsjökull glacier and has a summit of 1512 metres.
The volcano sits within Katla Geopark, a nature reserve covering 9542 square kilometres (roughly 9% of the country), stretching east from Hvolsvöllur to the black desert sands of Skeiðarársandur, and south from Vatnajökull to Reynisfjara beach. The area contains such natural attractions as the neighbouring ice-cap and volcano, Eyjafjallajökull and the Craters of Laki, in Vatnajokull National Park.
Of all the volcanoes in Iceland, Katla is of the greatest concern to the Icelandic people, having erupted roughly twice per century since 930 AD. As of the present day, Katla’s eruption is long overdue. Over recent years, scientists have measured an increase in seismicity and an inflation of the volcano’s caldera—clear warning signs that an eruption is on its way. The last eruption to break the glacier ice was in 1918, unleashing five times the amount that Eyjafjallajökull—its closest volcanic neighbour—did in 2010.
Local residents receive routine evacuation training for the day Katla erupts. All mobile phones within the scope of a broadcast tower will receive an electronic warning alerting them to the present danger. Afterwards, farmers must shut down their electric fences, allow their cattle to escape to higher ground and, finally, hang a notice on their door stating that they have moved to an evacuation centre in Hella, Hvolsvöllur or Skógar.
When Katla finally erupts again, days of ashfall, tephra clouds, lightning and glacial flash floods are expected to impact the environment immediately. Past eruptions have even caused tidal waves, a concern for the residents of Vik who live in the potential fallout zone. Given the wind direction, it is also a high possibility that Katla’s ash cloud might affect European air travel, as Eyjafjallajökull did at the beginning of the decade. National TV station, RUV, constantly updates Katla’s activity at www.ruv.is/katla.
Reykjavík domestic airport - Hangar 6
What to bring: