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Glacier fall at Bondhusbreen.

Bondhusdalen

19.12.2018

The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018

On the trail toward Kyrkjedøri, a half hour walk from Finse station, we find these small ridges

Trail toward Kyrkjedøri

04.12.2018

Roughly 550 million years ago, what is now Finse lay at the bottom of the sea - the remains of mud and clay that were deposited in this sea have ended up on the roofs of Norway. Also the thrust sheet from the continental collision has found its way to Finse, after a several hundred kilometre-long, trek through the mountains, that took several tens of millions of years to complete.

The smallholding Træet, Askøy

Træet

30.03.2018

Fantasy drawing of the animal life that reigned when the Bjorøy layer was deposited during the younger part of the Jurassic Period.

Vatlestraumen

12.06.2018

There are coal bits hidden in the sand under Vatlestraumen. These remains from a geological layer from the Jurassic Period were discovered when the undersea Bjorøy Tunnel was built in 1994. Oil- and gas reservoirs in the Troll Field in the sea west of Hordaland are from the same time. It is, nonetheless, quite surprising to find bedrock from dinosaur time inside of the outer islands of western Norway. On the Scandinavian mainland north of Denmark, there are only a very few places where one f inds rock from this time in earth history.

Holmengrå

Holmengrå

07.12.2018

Holmengrå is the only place in Hordaland where we find traces of the abrasion that is supposed to have transformed Western Norway from a Himalaya-like high mountain landscape during the earth's Paleozoic Era, to a flat lowlands terrain during the Mezosoic Era. Just 400 million years ago, large and small stones plummeted down from the high mountains. Some of these stones became incorporated into the conglomerate bedrock on Holmengrå.

Ystebøtræet, Radøy

Ystebøtræet

18.06.2018

The trading post Godøysund at the end of the 1880s.

Godøysund

19.06.2018

The old hostelry centres were strategically placed with good harbours and anchoring conditions where people travelled. GODØYSUND, or Gøysundet, as it was called, was in the middle of Tysnes Parish, with easy access from the sea, also for the local population. Gøysundet is amongst the oldest hostelries in Sunnhordland.

The hotel in 1928.

Fleischers Hotel

19.06.2018

The second Stalheim Hotel

Stalheim

19.06.2018

Stalheim is situated between Stalheimsfossen and Sivlefossen, in a community with the farms Sivle and Brekke. The most likely explanation of the name is “the farm by Stadall”, from “standa” (stand), probably with background in the steep Stalheimskleivi. The farm has for a long time been divided into several units. At Stalheim there has been a transport exchange from the Middle Ages and the farm has been a postal farm since 1647.

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