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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.

Ground up bedrock in the Valen Fault, seen under a microscope.

The Valen Fault

04.01.2019 - 12:59

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

Gjønavatnet and Kikedalen

Gjønavatnet and Kikedalen

16.06.2018 - 14:03

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Vinnesleira

Vinnesleira

06.12.2018 - 11:03

Bays that are shallow far out into the sea, with fine sand and clay, are rare in Hordaland. Where they are found, the reason is usually that the edge of the glacier made smaller advances or stopovers when it calved back at the end of the last Ice Age. This is what happened at Vinnesleira.

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.

Ulvikapollen

Ulvikapollen

27.05.2018 - 15:53

When the lush beach area innermost in Ulvikapollen was protected, the bird life was instrumental to the decision. The plant diversity is just as impressive. In Hordaland sea meadows such as this are rare small in size - they are more common in coastal environments.

Smooth lungwort

Herdla- botany

25.06.2018 - 18:05

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

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