Brú Guesthouse

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

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.

The waterfall Gljúfrabúi tumbles down from the Gljúfurá River. Its source is just north of Tröllagil (Troll Gorge) Canyon in the heath Hamragarðaheiði. It is a spring-fed river and less voluminous than its neighbour Seljalandsá River. The river runs from Tröllagilsmýri (Troll Gorge Marsh), a picturesque and fertile marsh in the heath. When the river emerges out of the marsh, it runs into the northern edge of a lava field which was formed in the volcanic eruptions in Eyjafjallajökull at the beginning of Holocene. There are several little waterfalls to be found in the river in the area.

Gljúfrabúi, which is 40 m tall, is on the land of the uninhabited farmstead Hamragarðar which the Rangá Foresty Society received as a gift in 1962 and is now owned by the municipality of Rangárþing eystra. There is a certain mystique over the waterfall because it falls into a deep chasm, while in front of it there is much palagonite rock that blocks the waterfall so that only the very top of it is visible. The boulder that blocks the waterfall is called Franskanef. Previously, people believed that it and the surrounding cliffs were the residences of huldufólk or hidden people. It is possible to climb onto Franskanef and see the waterfall from above. On the most risky parts there is a chain with which it is possible to support oneself; however, care must be taken if one climbs up and it is not for everybody. It is also possible to take off your shoes and wade the river down in the canyon. It's an amazing experience. Caution must be taken when travelling in the canyon because there is a risk of falling rocks. There is an old bath basin below Franskanef and at the inner end of the basin there is a little cave called Ömpuhellir, named after a hermit woman who lived there. Gljúfrabúi is a protected natural monument.

A little south of Gljúfrabúi there is a small canyon in the cliff face from which it is possible to ascend onto the heath above where there is a spectacular view of the neighbouring area. People referred to it as going up Stígurinn (the Path) and thus the river in that canyon is named Stígslækur (Path Brook). The path is still rather clear, with some stairs where it is steepest. Right above the edge, there are ruins of old sheepcotes from Hamragarðar.

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.

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

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