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From Ingahogg.

Ingahogg

20.12.2018 - 12:19

At nearly 1000 metres over sea level, on the north side of INGAHOGG mountain, the remains of a soapstone quarry have been discovered. It is said, according to the Sagas, that Inga collected the big soapstone that lies in front of the Åkra Church from here.

From Upper Musland toward Geitadalen.

Ulvanosa

04.01.2019 - 11:02

Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.

A rainy day at the Fish market, in the 1930s. (Alf Adriansen)

Bergen- Rain City

05.12.2018 - 09:21

"With its strange situation (surrounded by high mountains), this city has the advantage of a beautiful port and considerable shipping, but also the disadvantage that once on land one cannot get to the city without great inconvenience. This is because the weather in the vicinity of these high mountains is extremely unpleasant and rainy. There has even evolved an expression that is always rains in Bergen, and we have not experienced anything to counteract this saying." (a quote by the Dutch professor Fabricius after a visit to Bergen in ca. 1780).

Skytjedalen in Eidfjord.

Skytjedalen

03.01.2019 - 14:57

The contrast between phyllite and Precambrian basement is clearly visible at Lussand.

Lussand- geology

30.11.2018 - 12:16

Hardangerfjorden kløyver Hordaland i to. Den etter måten rettlinja fjorden skjer seg liksom på skeive inn i landet. Ikkje som Sognefjorden og Nordfjord – dei krokar og buktar seg innover meir eller mindre vinkelrett på kysten. Hardangerfjordens utforming har røter 400 millionar år tilbake i tida, då den veike sona i fjellet, der isen seinare tok grådig for seg, vart danna. Denne sona stig på land ved Lussand.

Glacial river plain at Lake Klevavatnet.

Rallarvegen

04.12.2018 - 14:30

They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.

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

Trail toward Kyrkjedøri

04.12.2018 - 15:04

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.

Stone quarry in Kollevågen, 1922

Hanøy

12.06.2018 - 16:56

The saw tooth pattern is clearly visible from Skora Mountain southwards toward Tellnes and Skogsvågen.

Haganes

12.06.2018 - 19:59

The gneiss landscape west and north of Bergen viewed in profile can remind us of a saw blade of the kind that has long, slanted sides that get broken off shorter transverse sides. It has taken several hundred million years to file this saw blade, an enduring interplay between various geological processes.

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 - 20:06

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.

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