Lo más destacado: The Reykjavík Capital Area is the country's largest and most populated city and currently home to 211.282 people, that's two-thirds of the entire Icelandic population!
Although it's one of the smallest capital cities in the world, it's still big enough to fit in six super-sized districts, with Reykjavík as the largest having a population of 121.230. Each district has its own elected council that governs the community and is responsible for the execution of legally determined projects.
A unique waterfall in the river Seljalandsá, about 30 km west from Skógar. It is 60 meters high with a foot path behind it at the bottom of the cliff, but with a thin cascade. It is the only known waterfall of its kind, where it is possible to walk behind it. The waterfall is very picturesque and therefore its photo can be found in many books and calendars.
Access to the waterfall is from the farm of Seljaland along the Ring Road, Iceland's main highway. A little further to the west there are several other falls, among them the interesting Gljúfrabúi which is partially masked by its own canyon. Access to it is from Hamragarðar farm along the road, east of Markarfljót.
Both of these "do-not-miss" attractions lie very close to the main Ring Road at the base of the Eyjafjallajökull Glacier, on the road leading in to Thorsmörk.
SKOGAFOSS - WATERFALL
Only a few kilometers away from the south shores of Iceland, lies the village of Skógar along the Southern Ring Road. It is a popular summer-resort centre surrounded by unusual scenic beauty. The breath-taking view of Skogáfoss waterfall and scenic surroundings and the snow-capped heights of two towering glaciers are Skógar's major summer attractions. There are two settlements by this name. One is Ytri-Skógar (outer or western Skógar) and the other Eystri-Skógar (eastern Skógar), located at a short distance from each other. Ytri-Skógar, commonly referred to as Skógar, is the main settlement. It is an old farm and has a church from 1890. It is located between the Skógá and Kverná rivers.
The greatest attraction of Skógar is of course the beautiful 60-metre high Skogáfoss waterfall in the river Skógá. Like the legends of buried treasures of Egill Skallagrímsson in Mosfell near Reykjavík and Ketilbjörn in Mosfell near Skálholt, there is a similar legend about the settler Þrasi who is believed to have buried his chest of gold under the Skogáfoss waterfall.
If the sun conditions are favourable - one can see a vivid rainbow in front of the waterfalls. The river below the falls holds a large salmon and char population and fisherman are seen here fishing July - October. The path leading to the top of the waterfalls continues following the river upstream - where numerous more dramatic waterfalls of sheer beauty are to be found. A great hike - to say the least!
One of the finest folk museums in Iceland is situated in extraordinarily beautiful natural surroundings. The interesting local folk museum has a collection of over 6000 artifacts and examples of various types of dwellings in Iceland since the early times. The collection of tools and equipment used at land and sea is outstanding. The museum also has an old turf farmhouse, where guests can experience the standards of living in Iceland in past centuries.
From Skógar the Ring Road runs eastwards along the foot of Mýrdalsjökull glacier, across the southern sandy plains and over glacial rivers, passes Seljavellir and continues along the soaring glaciated massive of Eyjafjöll and the two waterfalls Seljalandsfoss and Gljúfrabúi. From here runs a 10 km long trek along the river Skógá over the Fimmvörðuháls Pass between the Eyjafjallajökull and Mýrdalsjökull glaciers to the mountain oasis of Þórsmörk.
Skógar is a place to explore the natural diversity of the south or, if the weather is good, to spend a holiday amid beautiful and rugged landscapes. It is also very close to the ocean and the unique black beach.
DYRHOLAEY
Dyrhólaey is a 120-metre high promontory, not far from Vík. The place got its name from the massive arch that the sea has eroded from the headland. (The name literally means "door-hole"). When the sea is calm, big boats can sail through it. There has even been a maniacal daredevil pilot that flew through the arch with a small-craft airplane! From the top of Dyrhólaey there is a great view. The headland is thought to have been made in an underwater volcanic eruption late in the glacial period, not unlike the eruption of Surtsey. Several outcrops are in the sea, the highest one called Háidrangur ("High column") is 56 m. high. Dyrhólaey has been a natural reserve since 1978. The promontory is widely known among sailors as "Portland", and English trawler fishermen ubeach where one can climb (at your own risk). According to legend the Reynisdrangar needles were formed when two trolls were trying to drag a three-masted ship to land. When daylight broke they turned to stone. The Needles can be seen clearly from the village of Vík and are 66 meters above sea level at their highest. In one of the many caves here - there is a local legend about a monster having lived here for many centuries. The monster seems to have disappeared after a landslide over 100 years ago…sed to call it "Blow hole". There are also amazing rock formations all along the Birdlife here is abundant, with puffins and eider ducks being the most common species in the area. The lighthouse on the top of the cliff stands impressive and stoic in this often very windy area. Be careful not to go too close to the ledge of this dramatic cliff.
Reynisdrangar are basalt sea stacks situated under the mountain Reynisfjall near the village Vík í Mýrdal, southern Iceland which is framed by a black sand beach that was ranked in 1991 as one of the ten most beautiful non-tropical beaches in the world.
Legend says that the stacks originated when two trolls dragged a three-masted ship to land unsuccessfully and when daylight broke they became needles of rock.
Contemporary legends note the story of a husband who found his wife taken by the two trolls, frozen at night. The husband made the two trolls swear to never kill anyone ever again. His wife was the love of his life, whose free spirit he was unable to provide a home for; she found her fate out among the trolls, rocks, and sea at Reynisfjara.
Vatnajökull National Park was established in 2008. It includes the national parks in Skaftafell (est. 1967) and Jökulsárgljúfur (est. 1973) along with the Vatnajökull ice cap itself and extensive areas around it.
Vatnajökull National Park is characterised by diversity on all fronts, be it landscape, biosphere, cultural remains or service levels. For simplification, however, it may be placed into two categories: uninhabited highland areas with limited services and lowland areas with higher service levels.
The park‘s visitor centres are all located in lowland areas. Each of them has an exhibition about the park‘s nature and cultural heritage. Each also has a souvenir shop with special emphasis on local handicraft and products.
In 2018, Vatnajökull National Park was nominated for inclusion in the World Heritage List. The nomination [PDF - 28 MB]is currently being reviewed by UNESCO.
Jökulsárlón glacier lagoon is one of the most famed and visited attractions in Iceland. Floating on the lagoon are enumerable icebergs that have broken off the resident glacier, creating an ever-changing scenery of incredible allure.
The river Jökulsá connects the lagoon to the Atlantic Ocean, meaning that these icebergs eventually drift out to sea where they are polished by the waves before floating back to the black sands of Breiðamerkursandur. The name ‘Diamond Beach’ thus comes from the white ice on the black sand appearing like gemstones or diamonds, as they often glisten in the sun and sharply contrast their jet black surroundings.
The Diamond Beach is a strip of black sand belonging to the greater Breiðamerkursandur glacial plain, located by Jökulsárlón glacier lagoon on the South Coast of Iceland.
Here, the icebergs which fill Jökulsárlón glacier lagoon wash up on shore, standing dazzling and defiant in stark contrast to the black sand beach. It is, therefore, a favourite amongst photographers, nature-lovers, and wildlife-enthusiasts. Many seals call this beach home, and it is one of the best places in the country to see orcas from the shore.
Safety at the Diamond Beach
The Diamond Beach is a safe place for any responsible traveller; unlike at Reynisfjara, another South Coast black-sand-beach, sneaker waves and rip currents are not notorious for whisking unwitting tourists out to sea. However, there are still dangers to consider.
The main one of these is the icebergs themselves. Under no circumstance should you climb upon an iceberg, due to their slippery surfaces and sharp edges.
This is especially the case if the iceberg is at all in the water, as it could flip and trap you underneath, or else be pulled out to sea by a current with you on it.
The risk of injury and illness in the form of hypothermia is so great that extortionate fines exist to deter any ‘rebels’ looking for a thrill-seek. These have only come about due to serious incidents, to protect not only tourists at the lagoon but guides and staff who may feel obligated to embark on a dangerous rescue if they see someone at risk.
Breiðamerkurjökull (Icelandic pronunciation: [ˈpreːiðaˌmɛr̥kʏrˌjœːkʏtl̥]) is an outlet glacier of the larger glacier of Vatnajökull in southeastern Iceland. Emerging as a tongue of the Vatnajökull, it ends in a small lagoon, known as Jökulsárlón. Over time, it has gradually been breaking down.[1][2]
Breidamerkurjokull
As the icebergs break away from the tongue of the glacier, they drift slowly to the mouth of the lagoon and eventually join the ocean. They are stated to float in the deep lagoon for 5 years, which is around 300 m deep and spreads over an area of 17 km². It was near the ring road till 35 years ago before retreating rapidly and forming the Jökulsárlón lagoon. The 752 m high Breiðamerkurfjall Glacier was enclosed by the Breiðamerkurjökull and Fjallsjökull before the drifting started and formed the Breiðárlón lagoon, which is not as dramatic as the Jökulsárlón lagoon.[1][3]
The tongue of the Breiðamerkurjökull glacier is a major attraction for tourists. Tour operators conduct snowmobiles and jeep tours to visit the glacier along the winding iceberg studded Jökulsárlón Lagoon. The base station for visits to the area is at Jöklasel, which is approached from Höfn. It is termed as Tourist Conveyor belt. While walking on the shore, the isolated big blocks of icebergs on the sand beaches can be seen.[1][2][3]
The location has been used for many films and commercials. The glacier was used in Lara Croft: Tomb Raider as a stand-in for Siberia.[3]
VÍK
Mýrdalshreppur region is one of three municipalities in Katla UNESCO GLOBAL Geopark. Vik is the central town in the Geopark and has developed as an important local commercial centre and service for the travel industry. Mýrdalur is the southernmost district of Iceland, bordered by the glacial river Jökulsá to the west and the river Blautakvísl to the east. Its northern border is the Mýrdalsjökull glacier (700 km2, Iceland's fourth largest glacier). Approximately 600 metres below the ice lies the dormant subglacial volcano Katla which the Geopark is named after. Its southern limits are black sands and the rolling Atlantic waves. Vik is the only seaside settlement in Iceland left without a harbour due to natural circumstances. Nevertheless, Vík's inhabitants used to go fishing and got products from ship before the roads were imposed in 1939.
The natural beauty of the area is spectacular. There are many places of interest in the vicinity of Vik. Just east of the outskirts of the village lies one of Europe's biggest arctic tern breeding grounds. A short hike within the close vicinity of Vik is sure to satisfy all serious nature lovers and birds watchers. To the south of Reynisfjall mountain a spectacular set of rock columns called Reynisdrangar rise majestically out of the Atlantic Ocean. Dyrhólaey is a 120 meters high headland extending into the sea and forming an impressive natural arch located in the western part of the Mýrdalur district. In the summer, the peninsula is home to hosts of puffins.
Mýrdalshreppur region has a good travel services all year around and offers plenty of camping, hostels, guesthouses, apartments and hotels. We have over 1200 rooms to be precise. Among the many aspects of Vík that make it attractive to tourist are the hiking trails, bird watching, paragliding in the blue sky, snowmobile tour on Mýrdalsjökull glacier, ATV tour or horse riding on the black beach, glacier walk on Sólheimajökull glacier, short or long jeep tours around the region, a wool centre and a wool gallery, our local fish store where you can get both fresh and smoked Arctic char, to list but a few. Not many other places in Iceland offer as many contrast of nature as Mýrdalur. The area is therefore an ideal place to visit for travellers who want to enjoy good service and the best of what the country's natural environment has to offer.
Scenic landscape, favorable weather conditions and a selection of hiking trails make Skaftafell an ideal destination for those who like to enjoy outdoor activities in Icelandic nature.
Short and easy trails lead to waterfall Svartifoss and glacier Skaftafellsjökull, but for those who want to reach further out, the Morsárdalur valley and Kristínartindar mountain peaks are perfect in terms of distance and labour. Skaftfell is also the perfect base camp for those who seek to climb Iceland‘s highest mountain peak, Hvannadalshnjúkur.
In 1967, Skaftafell National Park was established, but in 2008 it became a part of the newly established Vatnajökull National Park.
Vestrahorn, Vesturhorn or Stokksnes, these are all names for this same place. The area is approximately a ten-minute drive away from Höfn. The Horn area is below Vestra-Horn, a 454-meter-high mountain. It is an interesting geological site composing of un-stratified plutonic rock, mostly gabbro but with some granophyre. East of the mountain is a strange-shaped outcrop called Brunnhorn that stretches out to sea.
One of the first settlement farms in Iceland was Horn, Built by Hrollaugur, son of Rögnvaldur earl of Møre in Norway. Hornafjörður Municipality and several natural sites are named after the settlement farm. In the Second World War, the Horn area became a base for the British army and later a NATO radar station was set up at Stokksnes, south of Horn. At Stokksnes you can feel the power of the Atlantic Ocean as the waves hit the rocky shore with massive force.
Vestrahorn is a photographer’s paradise. Come here to photograph the dramatic landscape, or just sit and enjoy the vast beauty. A very beautiful unspoiled natural site.
The shore features stunning lava dunes, that are constantly being shaped by the natural forces of water and wind. Down towards the sea, it is possible to get perfect reflections in the wet sand. Seals also tend to hang out on the stretch of sand, so if you’re lucky you can catch a picture of a lazing seal as well.
Þingvellir has always been popular, for obvious reasons. The history and striking landscape make the place an almost mandatory stopping point for tourists. In the middle of the 19th century, an idea was put forward in the US to conserve areas that are unique because of their beauty and grandeur. Settlers and others who travelled to uninhabited areas discovered places and natural phenomena at the sight of which they were spellbound. These were new ideas, a vision in which beauty and special characteristics started to be evaluated as wealth that mustn't be sacrificed, but instead, must be cared for and preserved for future generations. These ideas came to Iceland in the early 20th century.
In 1907, State Antiquarian Matthías Þórðarson wrote a magazine article entitled "Protection of Beautiful Places and Remarkable Natural Phenomena". There he discussed the necessity of preserving places that were remarkable and special because of their beauty; no less important, he maintained, than protecting ancient relics and old church objects. He suggested various places, but specified the Almannagjá fault and the area around Þingvellir by the river Öxará as an example of a site that deserved better care. He actually pointed out that Almannagjá had already been ravaged by the road work that by then was a fact. He cited examples of protection plans abroad and mentioned Yellowstone Park in the US as a place protected by law.
In 1913, teacher Guðmundur Davíðsson wrote an article that turned out to trigger the discussion of establishing a national park at Þingvellir. The article was published in a periodical called Eimreiðin, edited by University teacher Valtýr Guðmundsson. The article was explicit indeed and Guðmundur did not beat around the bush in depicting his countrymen's bad treatment and negligence of this most historic place in the country, Þingvellir. At beginning of the article he wrote: "Few Icelanders visit Þingvellir for the first time, without admiring the beauty of the landscape and being reminded of some of the major events that are interwoven into the history of this important place. These two factors, the historical events and the natural beauty, must stir the feelings of anyone standing in this sacred and legendary place. It brings together some of the most striking and beautiful aspects of Icelandic nature, while also being the site of many of the most important events of Icelandic history."
In the article, Guðmundur cited examples of national parks in the US and explained the necessity of protecting Þingvellir that, by then, had become a popular weekend destination for travellers. However, it wasn't until 1930 that the first national park in Iceland was established - Þingvellir National Park. In 1930, Guðmundur Davíðsson was appointed as the first National Park Warden at Þingvellir, living there until 1940, when he had to retire because of poor health. He then moved to Reykjavík and was an Alþing employee until 1948.
Today, Þingvellir is one of the most frequently visited tourist sites in the country. Each year, thousands of visitors go there to become better acquainted with Iceland's greatest historical site and jewel of nature.
The Golden Waterfalls (Gullfoss) are situated in the upper part of River Hvita. The water cascades down two steps, one 11 m high, and the other 22 m, into the 2,5 km long canyon below. This canyon was created at the end of the Ice Age by catastrophic flood waves and is lengthened by 25 cm a year by the constant erosion.
Above the waterfalls are dangerous rapids. History tells us about daredevils, who forded the river there. One of them was a young man, who watched his fathers sheep every summer on the west bank of the river. On the other side, a young woman did the same thing for her family. They started shouting across the river and became acquainted that way. Eventually the young man proposed to the girl across the river and she accepted on the condition, that he came right away across to seal their agreement. He did that and of course, they lived happily ever after.
In 1930 and 1948, the river was flooded to the brim of the canyons and both times bridges further down river were swept away. Early in the 20th century the farmer of Brattholt, who owned the water rights of the river contracted them to an English firm for a hydroelectric power station. The farmers daughter opposed this and even threatened to throw herself into the foaming water to prevent this accident. She fought bravely alone until a young lawyer, who later became the countries first president, came to her aid. Together they managed to save the waterfalls and she was commemorated by a monument in the canyon by the waterfalls in 1978.
In the canyon, alternating strata of lavas and moraines (till/tillite) are obvious and tell us about warm and cold epochs of the Ice Age.
This most famous and former largest spouting hot spring of the world probably was created during an extended earthquake period at the end of the 13th century. According to one of the annals, two large hot springs were created in the Haukadalur Valley in 1274, and many were ruined and disappeared. Silica deposits have created a mound around Geysir and its bowl measures about 18 metres across. The main natural shaft of the spring is 18 m deep and 2 m across.
For centuries on end, Geysir erupted and attracted tourists, but after the turn of the 19th century its activity diminished and after 1916 it has been very irregular. Scientists concluded that its cooling surface was too large and reduced it in size with good results for a spell. The highest measured eruptions reached over 80 m and before it erupted it rumbled and small tremors were felt. The hot spring area surrounding Geysir is about 500 m long and 100 m wide.
The ancient silica deposits cover a much larger area, close to 200 thousand square meters, which confirms the existence of a much larger hot spring area in the past. There are dozens of hot springs within the present active area and some of them spout as Geysir did. The most prominent one is Strokkur (The Churn), which spouts at intervals of 3-5 minutes. The hot spring area is fenced off and was declared inviolate in 1953.
A Geyser is a hot spring, which erupts intermittently in a column of steam and hot water. Some geysers erupt at regular intervals, but most erupt irregularly, the intervals ranging from a matter of minutes to years. The length of time of the eruption varies with the geyser, from seconds to hours. The height of the column ranges from about 1 m (3 ft) to about 100 m (328 ft), and the amount of water ejected in a single eruption varies from a few litres to hundreds of thousands of litres.
A geyser erupts when the base of a column of water resting in the earth is vaporized by hot volcanic rock. The force with which the water column is expelled depends on its depth. The weight of the water column increases with its depth. The weight, in turn, increases the pressure exerted on the base of the column, thereby increasing the boiling point of the water there. When the water finally boils, it expands, driving some water out into the air. With the weight of the column reduced, the pressure correspondingly drops, and the boiling point of the water remaining in the column falls below its actual temperature. Thereupon, the entire column instantly vaporizes, causing the geyser to erupt.
Almost all known geysers are located in three countries of the world—New Zealand, Iceland, and the United States. The most famous geyser in the world is Old Faithful in Yellowstone National Park in the United States, which expels about 38,000 to 45,000 litres (10,000 to 12,000 gallons) at each eruption. Old Faithful erupts at intervals of between 37 and 93 minutes, its column rising to a height of between 38 and 52 m (125 and 170 ft). The geyser gives warning of its impending activity by ejecting jets of water 3 to 7.6 m (10 to 25 ft) high.
Eruption intervals depend on such variables as the atmospheric pressure, the supply of heat, the amount and rate of inflow of subsurface water, and the nature of the geyser tube and its underground connections.
Katla is one of the largest volcanoes in Iceland. It is situated to the north of Vík í Mýrdal and to the east of the smaller glacier Eyjafjallajökull. Its peak reaches 1,512 metres (4,961 ft) and is partially covered by the Mýrdalsjökull glacier. The system has an area of 595 km2 (230 sq mi). The Eldgjá canyon is part of the same volcanic system.
The caldera of the Katla volcano has a diameter of 10 km (6.2 mi) and is covered with 200–700 metres (660–2,300 ft) of ice. The volcano normally erupts every 40–80 years. The flood discharge at the peak of an eruption in 1755 has been estimated at 200,000–400,000 m3/s (7.1–14.1 million cu ft/sec), comparable to the combined average discharge of the Amazon, Mississippi, Nile, and Yangtze rivers (about 266,000 m3/s (9.4 million cu ft/sec)).
The name Katla derives from the word ketill ("kettle"), referring to the form of the volcano. Katla is also used as a female first name.
It is thought that Katla is the source of Vedde Ash,[8] more than 6 to 7 cubic kilometers (1.4 to 1.7 cu mi) of tephra dated to 10,600 years BP found at a number of sites including Vedde in Norway, Denmark, Scotland and North Atlantic cores.
Sixteen eruptions have been recorded for Katla since 930. The last major eruption started on 12 October 1918 and lasted for 24 days. It was likely a VEI-5 level eruption. The 1918 eruption resulted in extending the southern coast by 5 km due to laharic flood deposits. Its present dormancy is among the longest in known history.
Minor eruptions occurred in:
2011 – VEI-1?
1999 – VEI-1?
1955 – VEI-1?
Major eruptions occurred in:
1918 – VEI-4
1860 – VEI-4
1823 – VEI-3
1755 – VEI-5
1721 – VEI-5
1660 – VEI-4
1625 – VEI-5
1612 – VEI-4
1580 – VEI-4
934 – VEI-5
Locations of caldera rim and previous eruptions
Most of these eruptions resulted in glacial floods. The severe fissure eruption in 934 was one of the largest lava eruptions in the past 10,000 years. Before the Hringvegur (Iceland's Ring Road) was constructed in 1974, people feared traversing the plains in front of the volcano because of the frequent jökulhlaup (or glacier bursts) and the deep river crossings. Especially dangerous was the glacier outburst that followed the eruption of 1918.
Present day activity
Schematic cross-section from west to east across the Eyjafjallajökull and Katla volcanoes. Magmatic intrusions are drawn in red, rhyolitic domes and the cryptodome in yellow; glaciers are shown in light blue.
Katla has been showing signs of unrest since 1999, and geologists have concerns that it might erupt in the near future.[15] Particularly, monitoring has been intensified following the March 2010 eruptions of a smaller neighbouring volcano, the Eyjafjallajökull glacier.[16] The eruption of this nearby long-dormant volcano in March and April 2010 prompted fears among some geophysicists that it might trigger an eruption at the larger and more dangerous Katla. In the past 1,000 years, all three known eruptions of Eyjafjallajökull have triggered subsequent Katla eruptions.
Following the 2010 Eyjafjallajökull eruptions, on 20 April 2010 Icelandic President Ólafur Grímsson said "the time for Katla to erupt is coming close ... we [Iceland] have prepared ... it is high time for European governments and airline authorities all over Europe and the world to start planning for the eventual Katla eruption".
Increased earthquake activity has been noticed on Katla since the eruption at Eyjafjallajökull, but no other signs of an imminent eruption have been observed. These quakes are located mainly on the northwestern rim of the caldera. On 9 October 2010, a sudden rise in harmonic tremor was observed in the stations around Katla, a sign of a possible impending eruption.
As of 2010, volcanologists are continuing to monitor Katla, aware that any eruption from Katla following an eruption from Eyjafjallajökull has historically occurred within months of the latter. The Icelandic Meteorological Office updates its website with reports of quakes both at Eyjafjallajökull and Katla.
2011 activity
In 2011, geologic activity led many to speculate that a very small subglacial eruption had taken place. In June 2011, harmonic tremor was again detected at Katla volcano. A few days later, an earthquake swarm took place in the caldera, indicating magma movement inside the volcano, leading to increased fears of an eruption in the near future.
On 8 and 9 July, another spike in harmonic tremors occurred, as a small eruption of Katla took place. Cracks formed on the Glacier, as well as a cauldron. Icelandic media reported a small subglacial eruption might have started. On the morning of 9 July, a glacier flood was reported in the river Múlakvísl, and also later in the river Skálm. The bridge across Múlakvísl was destroyed as well as other parts of the road, Route 1, on the Icelandic ring road. Helicopter pilots flying over the glacier also reported cracks in the glacier. Scientists monitoring the activity said speculation that it was caused by a "very small" subglacial eruption lacked confirmation by visual or seismic evidence.
2016 and 2017 activity
Tremors were detected under Katla in late August 2016.
A "Specialist Description" describing the activity on 29 August 2016 noted that:
There was "a seismic swarm in Mýrdalsjökull on the 29th of August with two events in the northern Katla caldera rim measured at magnitude 4.5. These are the biggest earthquakes in Katla volcano since 1977. Earthquake eruption checks confirmed that most earthquakes occurred between 0:40 and 1:50 PM. The big earthquakes were about thirty seconds apart at 1:47. They were followed by more than 50 aftershocks until 15:12 PM, when there was an earthquake of magnitude 3.3 and then the cycle and seismic activity in the region reduced again. No unrest was measured along these earthquakes. The geothermal has decreased in the following week and is now negligible."
Update Written by a specialist at 11 Sep 16:38 GMT "Today, shortly before 14:00, a small earthquake swarm began in Mýrdalsjökull. The largest earthquakes of the swarm were of magnitude 3.3 and 3.0 at 16:12 and 15:57. More than 10 smaller earthquakes were detected in the swarm. All of the earthquakes were shallow and located in the caldera of Katla volcano. It is not unusual for seismic swarms of this type to occur in this area."
In February 2017, seismic activity at the volcano continued.
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