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Hunkubakkar offers accommodation with or without a private bathroom in five two-room chalets, each with a small veranda. They are all suitable for 2-3 people. Accommodation is also available in the farmhouse. Cooking facilities are available on request. The chalets are just a short distance from the restaurant, where guests can order breakfast and evening meals.
Meals are served in the conservatory, with seating for up to 30 guests, or in the dining room where there is space for a further 20 people. The restaurant is licensed to serve beers, wines and spirits.
Groups of up to 50 people are welcome, be it for a meal, for a party or for overnight accommodation.

The district around Hunkubakkar is well-known for its natural beauty and mild climate.
There are countless attractions for nature lovers with something new around every corner. Enticing footpaths criss-cross the countryside with spectacular views all around. Bird life is abundant close to the farm and further afield.



GPS Points N63° 46' 9.738" W18° 7' 49.015"


Accommodation 17 Rooms / 40 Beds / 6 Houses
Opening period All year
Service Smoking not allowed Cottage rental Hotel / guesthouse Coffe shop Restaurant Fishing permits Cooking facilities Credit cards accepted Bar
Categories Farm Holidays , Cottages , Cafés

Travel directory for Hunkubakkar

The official travel index of Iceland


Hörgsland Travel Service
Sleeping bag accommodation
  • Hörgsland I
  • 880 Kirkjubæjarklaustur
  • 487-6655, 894-9249
Guesthouse at Seglbudir Landbrot
  • Seglbúðum
  • 880 Kirkjubæjarklaustur
  • 697-6106
Laki Golf Club
Golf Courses
  • Efri-Vík
  • 880 Kirkjubæjarklaustur
  • 487-4694, 899-4694
Tour Operators
  • Mörtunga I
  • 880 Kirkjubæjarklaustur
  • 852-2012
Flandur Trips
Tour Operators
  • Túngata 2
  • 880 Kirkjubæjarklaustur
  • 899-8767
2.22 km

Fjaðrárgljúfur is a magnificent and massive canyon, about 100 meters deep and about two kilometres long. The canyon has sheer walls, and is somewhat serpentine and narrow. The bedrock in Fjaðrárgljúfur is mostly palagonite from cold periods of the Ice Age and is thought to be about two million years old. The river Fjaðrá has its source in the mountain Geirlandshraun and falls off the heath edge in this stunning canyon until it makes it down into Skaftá river. Fjaðrá has changed a lot in the course of time. Today Fjaðrá is often rather low in water and therefore hikers can safely choose to walk inside the canyon. However, wading is necessary fairly often. Deep in the canyon there are waterfalls so one needs to walk the same way back. Most people choose to walk along a walking path up on the canyon's edge while simultaneously enjoying the view above the canyon.

Formation of the Fjaðrárgljúfur canyon

It is believed that Fjaðrárgljúfur formed at the end of the last Ice Age, about nine thousand years ago. When the glacier retreated, a lake formed in the valley behind a hard resistant rock. The run-off from the lake flowed to where Fjaðrárgljúfur is today. Glacial rivers from the glacier's edge carried a lot of sediment into the lake and the river which ran from it dug itself down into the rock and down onto the palagonite in front of it. Because the cascade has been so large, it was powerful in digging out the canyon. Eventually the lake filled with sediments and the river's strength dwindled. When the lake filled up completely, the river began to dig itself into the sediment layers which it had previously left in the valley. Fluvial terraces on both sides in the valley give an indication about the original height and location of the lake while a deep channel in the palagonite serves as a silent reminder to the power of nature.

More geosites in the neighbourhood:

19.00 km
Dverghamrar / Dwarf Rocks

Dverghamrar (Dwarf Rocks), just east of Foss, are peculiar and beautiful formations of columnar basalt. On top of the columns there is cube-jointed basalt. The landscape is thought to have been moulded at the end of the Ice Age. The sea level was higher at that time and it is believed that the waves caused the peculiar look of the rocks. Dverghamrar are a protected natural monument. Columnar basalt is formed when lava flow gets cooled and contraction forces build up. Cracks then form horizontally and the extensive fracture network that develops results in the six sided formation of the columns.

South Iceland

Towns & Villages

The south of Iceland has several towns and villages, each with its own style, charm and points of interest. Selfoss is the largest town and has a variety of shops, services, many restaurants and fast food places. Most towns are close to the main route, making them accessible and enjoyable.

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Map Höfn Kirkjubæjarklaustur Vík Vestmannaeyjar Hvolsvöllur Flúðir Laugarvatn Reykholt Laugarás Borg Brautarholt Hveragerði Árnes Selfoss Hella Stokkseyri Eyrarbakki Þykkvibær Þórlákshöfn