Lakagigar Day Tour by Super Jeep

South Iceland is the most popular part of the country and contains some of the most beautiful natural attractions in Iceland, among them the Golden Circle, some of Iceland's most famous active volcanoes as well as the beautiful Jokulsarlon glacier lagoon.

Geography

South Iceland is usually divided into the fertile South Icelandic lowlands between Hellisheidi and Eyjafjallajokull volcano on the one hand - and on the other hand the eastern part with the big volcanic glaciers Eyjafjallajokull and Myrdalsjokull (home of Katla) and flattened sands stretching towards the sea.

The South Icelandic lowlands

The South Icelandic Lowlands stretch nearly 100 km from Hellisheidi in the west towards Eyjafjallajokull in the east as a very flat and fertile farming land. From the shore the lowland stretches about km towards the inland. This is the best agriculture area in Iceland. The whole area is geologically very young, mainly of tuff type, formed during the Ice Age by the lava flows of the numerous volcanoes of the area. The area is indeed surrounded by volcanically active mountains on all sides. The glacier rivers of the area have helped filling the lavas with sand and clay, leaving it more and less smooth and fertile. Very strong earthquakes are found in this area as well.

The most active volcanoes of the area are Hekla and Eyjafjallajokull. No less active and not far off, but on the east side, is Katla, which we’ll adress in the eastern part-section. South of the mainland are the volcanic Westman Islands, famous for the 1973 eruption as well as the eruption in 1963, when Surtsey island was formed. Closely linked to the volcanic activity in the south is the geothermal heat found in many places, the best known being the Geysir area, which forms a part of the famed Golden Circle, which also consists of Gullfoss waterfall , Iceland's most famous waterfall as well as one of its most beautiful, located in the popular rafting river Hvita and Thingvellir National Park, comprising three of Iceland's most beloved natural attractions.

The earthquakes of the area bear witness to the fact that Iceland is still in shape. This is further evidenced by the endless number of fissures in the lavas, fractures in the mountains and certain pieces of lands sinking. The area of Thingvellir is the best known example of this, showcasing the continental drift. Thingvellir is a UNESCO World Heritage Site and the location of the old parliament, Althingi, (now situated in Reykjavik) and one of Iceland's most important sites.

Another of Iceland's most popular attractions is the beautiful Thorsmork valley, situated between Myrdalsjokull and Eyjafjallajokull.

Natural harbour-sites are hardly any on the South shore, due to sand produced by the glacier rivers. A few towns are found in the area, Selfoss being the biggest one, Hveragerdi is another, then there are Hella and Hvolsvollur, all conveniently located by the ring road. By the shore are three fishing villages; Thorlakshofn, Eyrarbakki and Stokkseyri. Thorlakshofn the only one of those that can accommodate modern ships and ferrys. The ferry to the Westman Islands sails from there. A new harbour has been built on the sandy coast opposite the Westman Islands. The whole south shoreline offers some of the most gigantic braker waves that you are likely to see.

Culturewise, in addition to Thingvellir, we reccomend the ancient bishop seat of Skalholt (weekends at Skalholt further offer rich music life). Also, Iceland's most famous saga, Njal's saga takes place in the South lowlands. We further recommend the large reconstructed turfhouse near Stong and the ancient excavated ruins.

For sports, horse riding is popular in the area as well as catching salmon or trout, hiking, and river rafting in Hvita. 

The east part of South Iceland.

This is the area south and east  of Myrdalsjokull. The volcanic glaciers Eyjafjallajokull (near the border of the eastern and western part) and Myrdalsjokull, dominate the view. The landscape has been shaped by volcanic eruptions and vast sands stretch to the sea. Some agriculture is found here, however, with the farms in a row alongside the mountains.  A few large glacial rivers fall down in this area which also has striking waterfalls, such as Skogafoss and Seljalandsfoss.

Eyjafjallajokull is already well known for its 2010 eruption,  disturbing air communication all over Europe for many days. Much more serious,however, would be an eruption from Katla, a volcano in the eastern part og Myrdalsjokull. 

Katla’s last eruption was in the year 1918, when an enormous flood of water exploded from the glacier in a matter of minutes, threatening the local farmers of the area. Large amounts of ash and muddy  material were brought to sea to form a new land of sand, Kotlutangi, later washed away by the sea. No people were killed in this eruption. Eruptions in Katla throughout the ages have further created the vast sand area Myrdalssandur. Sixteen eruptions have been recorded for Katla since 930 at intervals of 13-95 years and the volcano is being closely monitored, as time may draw near to its next eruption.

In the same volcanic system as Katla (geologically speaking), are the Lakagigar craters, northeast of Myrdalsjokull. Those erupted in the years 1783-84; producing the largest amount of lava known in historic times. The ashes hindered the sunlight from reaching down to the surface of Earth, resulting in cold climate over northern Europe.

In  this area – what we call the eastern part of South Iceland -, there are many places worth visiting: Solheimajokull is a beautiful glacier in a walking distance (an outlet of Myrdalsjokull); Skogar has a very interesting museum of older time traditions and Skogafoss is only a few km away from there. One of Iceland’s most famous hiking routes, Fimmvorduhals, starts from Skogar. Southwest of the village Vik is one of Iceland’s most spectacular beaches, Reynisfjara. Together with the promontory Dyrholaey, which is the southernmost tip of the mainland of Iceland, it offers a breathtaking view with amazing rock formations, a black pebble beach, an abundance of birds and the powerful waves of the North Atlantic Ocean crashing on the beach.

Further east stretches the world's most vast sand plain, Skeidararsandur. North of the sand is the fascinating Skaftafell preservation area.  At its east end, south of Hvannadalshnukur, Iceland's highest peak, is Ingolfshofdi cape, with its rich birdlife, old fishermen's shacks and its lighthouse. Following the shore further east is the incredibly beautiful and ice-filled Jokulsarlon glacier lagoon. Not far off is the region of Sudursveit, featuring the culture center and heritage museum Thorbergssetur, erected in the memory of Icelandic author Thorbergur Thordarson.

Vatnajökull glacier is the largest ice cap in Iceland and the third largest glacier in Europe, covering 8% of the island's landmass. Vatnajökull National park can be found in the south west of Iceland and is a popular spot for activities like glacier hiking from Skaftafell, boat tours and ice caving tours from Jökulsárlón glacier lagoon, both of which are part of Vatnajökull national park. 

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) 

Lakagígar, in the south of the Icelandic highlands, is a row of craters, formed during one of the largest eruptions in recorded history, known as the fires of the River Skafta, or ‘Skaftareldar’ in Icelandic. The area has some of the most stunningly attractive landscapes in Iceland.

The majority of the craters are today covered in moss.The total area of the lava field is 565 km² and the estimated volume of volcanic material is over 12 km². The Skaftáreldar eruption that formed the craters in the 18th century led to crop failure, disease and disasters in Iceland. Some believe that the airborne haze from the eruption, blocking the sunlight in the northern hemisphere, may have contributed to the French revolution in 1789.

Eldgja is the largest volcanic canyon in the world, 270m deep, 600m at its widest and around 40 km long. 

The canyon lies paralel with the Lakagigar craters. The first documented eruption of Eldgja, in 934, was the largest flood basalt in historic time.

A beautiful watefall, Ofaerufoss in the river Ofaerua falls into in the Eldgja canyon. This is a two-spilt waterfall and the lower part used to have a natural bridge, but the bridge collapsed in the early nineties.

Mýrdalsjökull is a glacier in the south of the Icelandic highlands. It is the country's fourth largest ice cap, covering nearly 600 kilometres squared, 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.

Eruptions beneath Mýrdalsjökull

Since 2010, the world has known of the volcano beneath Eyjafjallajökull; few, however, are aware of the much larger volcano right beside it. Mýdalsjökull 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.

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 jökulhlaups, during eruptions, even when the lava does not break through the surface of the ice.

Historically, the area was little settled for this reason.

Katla is connected to the same volcanic system as Eyjafallajökull and usually erupts violently a few years after. As the ex-president, Ólafur Ragnar Grímsson said in 2010:

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 Mýrdalsjökull

While there are no eruptions immediately imminent, tours continue to run on Mýrdalsjökull, 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 Mýrdalsjökull

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.

Oraefajokull is a glacier volcano in South-East Iceland. On its north-western side is Iceland's highest peak, Hvannadalshnjukur (2109 m).

Oraefajokull, which has several glacier tounges of its own, is considered a part of the larger Vatnajokull and thus belongs to Vatnajokull National Park. It has erupted twice, in 1362 and 1727.

The vast Eldhraun lava field (“Fire Lava“), in the south of the Icelandic highlands was created in one of the greatest eruptions in recorded history and is of the largest of its kind in the world. The Lakagigar craters were also created during this eruption.

This eruption lasted from 1783 to 1784 and is known as the Skaftareldar (The skafta River Fires). This was a cataclysmic event for Iceland and beyond. In Iceland it lead to diease, crop failure and disasters.

The eruption affected Europe as well. In Great Britain, that summer known as the Sand-Summer in Great Britain due to the fallout of ash and it is believed that the airborne haze and blocking of sunlight may have contributed to the French Revolution.

Despite the abysmal effect the eruption had, this lava field of 565 km2 is today one of the most stunningly attractive ones in Iceland.

The area features one of the most magnificent lava tube systems in the country, located north of the Lake Laufbalavatn. More than 200 caves have been found there, extending for more than five kilometers and 14 cu. meters.

Credit: Wikimedia, Creative Commons. Photo by ptj56.

Fjaðrárgljúfur is a beautiful, dramatic canyon in South Iceland, close to the historic town of Kirkjubæjarklaustur.

Though the valley was only formed at the end of the last ice age approximately 10,000 years ago, the bedrock here is much older, dating back two million years. The ravine was created by the runoff from a glacial lake, which wore away the soft stone and left only the more resistant rocks behind.

Geography of Fjaðrárglúgur

Fjaðrárglúgur is about 100 metres deep and two kilometres long, with sheer walls dotted with many waterfalls. 

It is possible to walk along the ridges above, or in the valley itself. The site is popular amongst hikers and photographers for the contrasts between the dark rocks, foaming waters and verdant moss. If taking the former route, look up as well as down, as, in clear weather, you will attain great views of the South Coast, Highlands, and surrounding glaciers.

If taking the latter route, know that the river Fjaðrá runs through the canyon, and though its waters are often shallow, those exploring may have to wade through it. This tributary runs into the greater Skaftá river. 

Fjaðrárglúgur’s Surroundings

The closest settlement to Fjaðrárglúgur is Kirkjubæjarklaustur, often nicknamed Klaustur by locals. This is a place with a long religious history, behind home to the country’s first convent. Many local sites are named after the nuns who once lived in the area, such as Systrastapi (Sister’s Rock) and Systrafoss (Sister’s Falls).

Fjaðrárglúgur is a great place to stop for those travelling the South Coast as they make their way from Reykjavík or Vík towards Skaftafell and the Jökulsárlón Glacier Lagoon. The South Coast itself is lined with other features to visit during your travel, such as the waterfalls Skógafoss and Seljalandsfoss, the beach Reynisfjara, and the Dyrhólaey cliffs and arch.

Kirkjubæjarklaustur (referred to locally as ‘Klaustur’) is a village of approximately 120 inhabitants in the Skaftárhreppur municipality of south of Iceland. Situated by the Ring Road, approx. 250 km east of Reykjavík, Klaustur is one of the few villages providing amenities—eg. fuel, post office, bank, supermarket— between Vík í Mýrdal and Höfn.

History

The history of Kirkjubæjarklaustur differs, in many respects, to the traditional Icelandic settlement. “Papar”, the Icelandic title for travelling Irish monks, were thought to have settled the area long before the Norsemen. In that tradition, it was claimed that pagans of no kind would set foot in Klaustur; this was a strictly Christian area.

Stories have permeated, with one telling of a pagan, Hildir Eysteinsson, who attempted to move there in the 10th Century. Upon setting foot across the border, he fell instantly dead and was buried on the neighbouring hill, Hildishaugur (“Hildir’s Mound.”)

Despite twisting the tongue, the full village name 'Kirkju-bæjar-klaustur' actually tells the story of the area well; 'Kirkju' means church, 'bæjar' means farm and 'klaustur' means convent. The word 'Klaustur' was added to the original name 'Kirkjubær' in 1186 AD when a convent of Benedictine nuns settled there. 

In the 364 years leading to the Reformation in 1550 AD, Klaustur did much for the oral history of south Iceland. Systrastapi (Sister’s Rock), the Systrafoss waterfall and lake Systravatn all take their names from the nun’s settlement. 

Folklore

The folklore relating to these sites are rich in tales of religious heresy, superstition and death. Sister’s Rock, for instance, has been said to be the burial site of two nuns executed for sinful behaviour. Selling their soul to the devil, removing communion bread from church, carnal knowledge with men, blasphemy toward the pope; these were just some of the accusations brought against them. Guilty or not, the nuns were swiftly burnt at the stake. 

Following the Reformation, one of the nuns was vindicated for her actions, and it is said that flowers soon bloomed on top of her grave. The other’s grave has remained barren, a continuing reminder of the lady’s ethereal disapproval.

Nearby attractions

Despite its petite size, Klaustur is an important crossroads to the attractions nestled at the centre of the island, namely the Laki Craters in Vatnajokull National Park and the Landmannalaugar hiking trails in the scenic Fjallabak Nature Reserve. Only a few kilometres from the village itself lies the spectacular Fjaðrárgljúfur canyon.

A short walk east of Kirkjubæjarlaustur will take you to the fascinating Kirkjugólfið “Church Floor”, an 80 square metre flat of basalt columns, shaped and formed naturally by tide and glacial melts. 

Wikimedia. Creative Commons. Credit: Praveen Kumar Bodigutla

Skaftafellsjökull is a glacier tongue spurting off from Iceland's largest ice cap, Vatnajökull.

The glacier tongue sits in Skaftafell, a nature reserve in Öræfi, Vatnajökull National Park. 

Skaftafellsjökull is an excellent but concerning example of how climate change is steadily affecting the glaciers over the growing years. Over the last decade, Skaftafellsjökull has been receding dramatically, only strengthening the argument that environmental policies must look to preserve Iceland's unique, important and beautiful natural features.

It is possible to hike Skaftafellsjökull's surrounding area in order to secure a fantastic perspective of this glacier tongue. After checking in with the Skaftafell Visitor's Centre as to the best hiking trails and conditions, guests will follow an 8 km (5 mi) trail (there and back) up 390 m (1,280 ft) to the waterfall, Svartifoss. From here, you will be able to look out on the glacier and its adjacent lagoon. 

Mýrdalssandur is an outwash plain located between the rivers of Kúðafljót, in the east, and Múlakvísl, in the west, both of which carry water down from the glacier, Mýrdalsjökull. Mýrdalssandur has a 35km (22mi) long coastline which includes Kötlutangi, the southernmost point of the Iceland's mainland. 

Culture

Around the year 1000, many farmers set up shop on Mýrdalssandur. By the 15th century, however, most of these farmsteads were abandoned due to violent eruptions originating from Katla volcano. Today, the area is a 700 square kilometre desert of black sand, made up of the deposits from Mýrdalsjökull ice cap and the sudden glacial floods (or jökulhaup) that run from the glacier down to the sea. Evidence of these prior floods can be seen throughout Mýrdalssandur, be it the washed out bridges or the peculiar rock erosions. Even today, farmers close to Mýrdalssandur worry that receding glaciers will cause rivers to change direction and overflow. It’s no wonder Icelanders left this region a long time ago.

The barren landscape of Mýrdalssandur has done much for folklore and superstition, with many still claiming (albeit, with a twinkle in their eye) that the black sand desert is haunted by ghosts and witches. Birdlife and arctic foxes are a relatively common sight in the region.

Attractions 

There are a number of attractions to preoccupy oneself with in Mýrdalssandur. At the beginning of the western edge, visitors can head to Sólheimasandur beach to see the famous Navy DC plane wreck. The plane crashed in 1973 after the pilot, incorrectly, assumed the plane had run out of fuel. Still, he managed to land the plane on the black sands with no casualties. The plane wreck still exists today and makes for a great stop for photographers. 

Roughly 15km east of Vik, visitors will arrive at the inselberg mountain, Hjörleifshöfði. Rising 221m (725ft) above sea level, Hjörleifshöfði was once an island though by the time of the settlement of Iceland, it was already connected to the mainland. Today, it offers a well-paced trail hike with sweeping views across the Mýrdalssandur region.

The mountain is named in a number of sagas, particularly that of Hjörleifur Hróðmarsson, of whom the mountain is named after. The brother of Ingólfur Arnarson, it was told that Hjörleifur settled at the base of the mountain in the 9th Century, but was eventually murdered by his Irish slaves. Vengeance was swift as Ingólfur pursued the assailants to Vestmannaeyjar, where they were eventually killed. Hjörleifur is said to be buried at the summit of Hjörleifshöfði. 

Driving across Mýrdalssandur will take approximately an hour, with stunning views of Vatnajökull glacier and regular picnic stops. Recently, Mýrdalssandur was used as a filming location for the opening scenes of Star Wars: Rogue One, depicted as the planet Lah’mu. 

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.​

Geography

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.

Activity

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. 

Precautionary measures

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.

Credit: Wikimedia, Creative Commons. Photo by Nave111.

Fagrifoss (the Beautiful Waterfall) is located in southeast Iceland near the Lakagígar volcanic region. The falls rest along the 4x4 road F206, approximately 24 km (15 mi) from the small town Kirkjubæjarklaustur and 40 km (25 mi) from the Laki crater. 

What makes Fagrifoss particularly attractive is its smooth brink and the segmented plunge in which its lower end slants, giving the falling water at its base a beautiful fan shape. Only adding to the falls beauty is its contrast with the raw landscapes in which it is nestled.

To reach the Fagrifoss, travellers must cross a small river and a 4x4 vehicle is needed for the crossing.