Seljaveitingar

The Merkjá River has several beautiful waterfalls, but the most outstanding is Gluggafoss or Window Falls. (also known as Merkjárfoss) The upper half of the cliff is palagonite or tuff rock and the lower ledge is basalt. The river has formed tunnels and grooves through the soft rock and a series of 'windows' in the tunnels, thereby earning the name 'Gluggafoss'. At the very top of the falls, the river passes under a stone arch. As the rock is rather soft, the waterfall has changed over time. Around 1947 the upper half of the waterfall could hardly be seen, as the water flowed into a vertical tunnel behind the cliff. It was only visible through three different openings or 'windows' one above the other. The water came out through the bottom 'window', forming a beautiful arch, except when the water rose in the river, forcing it through all three windows. Further changes occurred when Hekla erupted in 1947, causing a 20 cm thick layer of volcanic ash to be carried downstream by the river. The vertical tunnel formation nearly disappeared as it filled with ash. It has taken nearly 50 years for the falls to return to its former glory.

More geosites in the neighbourhood: www.katlageopark.com

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.

Great Dímon is the name of a landmark that landmark East Landeyjar, Fljótshlíð and West Eyjafjöll. Great Dimon has a sister mountain called Litla Dimon or Little Dimon. The name is thought to come from Latin, meaning twin mountains or two alike. It has also been said that the word means haystack and it certainly is reminiscent of a haystack surrounded by golden fields. Near the mountain a sign has been erected by the Saga Center of Hvolsvöllur which tells of battles fought in the area during the times of the settlement of Iceland in the most famous of Icelandic sagas, Njálssaga. The mountain is only 178 meters high and is a fun hike for both adults and children.

At the Saga Centre in Hvolsvöllur, guests are invited into a medieval world of Icelandic culture in the early centuries of Iceland's history. The exhibition covers such subjects as ocean travel and navigation, religion, Viking cosmology, and the literary art of the sagas, Iceland's most important contribution to world literature. Prominence is given to Njáls Saga, the masterpiece of Icelandic sagas, which takes place in the Rangárvellir region. The saga tells of the close friendship between the hero, Gunnar of Hlídarendi, and the sage, Njáll of Bergthórshvoll; and it tells of their wives, who are sworn enemies and think nothing of sacrificing the lives of slaves and labourers in the service of their own virulent disputes, it tells of powerful love, conflicts and deceit, battles and holy reconciliation. The pagan way of thinking and complicated intrigues, gives Gunnar´s enemies the right to kill him and the sage Njáll and his wife are burned to death in their home with their sons. In the Viking Hall, a replica of a medieval longhouse, its walls paneled with timber, and the benches are clad with horsehide, the guest can sit down or continue to the model of the assembly site at Þingvellir around 1000 AD. The Centre also houses an interesting exhibition on the history of commerce and the cooperative movement in South of Iceland.

Open summer 09:00 - 19:00 from June 1. - Septemer 1.

The Eyjafjallajökull glacier is a 1666 m high glacier-capped stratovolcano. It is one of the smaller glaciers of Iceland. It is situated to the north of Skógar and to the south and west of the bigger glacier Mýrdalsjökull. The icecap of the glacier covers a volcano (1666m in height) which has erupted relatively frequently since the Ice Age. The crater of the volcano has a diameter of 3-4 km and the glacier covers an area of about 100 km². In June 1994 an earthquake swarm lasting for nearly a month occurred below the active volcano Eyjafjallajökull in South Iceland. It is otherwise a relatively quiet volcano - although it is not listed as being inactive. Eyjafjallajökull erupted last in 1821-1823. The south end of the mountain was once part of the Atlantic coastline. As the sea has since retreated some 5 km, the former coastline has left behind sheer cliffs with a multitude of beautiful waterfalls, the best known of them being Skógafoss and Seljalandsfoss. In strong winds, the water of some of the smaller falls can even be blown up the mountain. It is one of the three glaciers that surround the Thorsmörk area - the other 2 being Myrdalsjökull and Tindfjallajökull. Specialized tours are arranged on the glacier for both skiing, superjeep tour and hiking. One should never venture onto the glacier without guides and good knowlege of these kind of activities as this is a very dangerous area for unexperienced visitors.

Eyjafjöll is a beautiful region of south Iceland, which is easily accessible and popular with visitors.

Check out www.eyjafjoll.is Eyjafjoll's website aims to provide a wide range of useful information for visitors to the area: we tell you about walking routes, places of interest, and tourist services in the Eyjafjöll region.

The caves in Efra-Hvol (Upper Hvol) have histarically been referred to as "the Irish Caves" which are set into the so-called, "Irish Heath". It was originally thought that many of these man-made or artificial caves were madein the 19th century, but in fact, their histofical names appear to confirm they originated even beforr the settlement period.

More geosites in the neighbourhood: www.katlageopark.com