- Remove Quarns and mills filter Quarns and mills
- Remove Hydro power filter Hydro power
- Remove Mountain plants filter Mountain plants
- Remove Wetland filter Wetland
- Remove Sediments filter Sediments
- Remove Sedimentary rocks filter Sedimentary rocks
- Remove Conservation area filter Conservation area
![Langavassmyrane looking towards Langavatn.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_39.jpg?itok=TWhBEzeV)
Langavassmyrane
The Ruff lek on Langvassmyrane is the only known phenomenon of its kind on Hardangervidda. Every year it attracts hens from the whole plateau. The marsh is also the richest wetland in the county. This green oasis is located in a rocky moraine landscape a few hours walking distance south of Dyranut.
![Sysendammen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_37.jpg?itok=ibwv5qBG)
![The delta at the outflow of Storelvi in Granvinsvatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_1.jpg?itok=er1kEGup)
Granvinsvassdraget
After the ice age, Granvin Fjord reached all the way up under Skjervsfjossen waterfall. Just a thousand years later, as a result of the rising of the land after the ice melted, this whole inner part of the fjord freed itself of the sea and became Granvinsvatnet lake. In spite of this rise in elevation, this waterway is still navigable for fish: Sea trout have wandered into Granvinsvatnet in more recent times and evolved to become freshwater trout. And salmon and sea trout made the journey 13 kilometres up the Storelvi river.
![Lime forest at Joberget](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_22.jpg?itok=pd1PXGzQ)
Joberget
Flowering lime is one of nature's blessings: The nectar gives clear honey. The flower is used as folk medicine. From the inner bark of the lime tree one can make strong rope. Elderly folk can still tell how they got a weather report from the lime tree. If it smelled strong, it was probably going to rain. Lime often grows together with elm, ash and other tree species of the deciduous forest. Pure lime forests are rarer. Granvin has Hordaland's biggest lime forests.
![From Lussand toward Håfjell.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_23.jpg?itok=JA0Ck0TM)
Uranes
One of the most magnificent deciduous forests in Hordaland grows along the border with Kvam. The rich growth comes from the phyllite and mica schist bedrock, together with a good climate. Along the fjord the summer is warm but not too dry, and in winter it is not too cold for plants that do not tolerate the frost.
![In the background Nordrenut and Vesle Finsenuten, from the south-east.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_3.jpg?itok=nFVp8uAU)
Finse
Many mountain plants are well prepared to face cold and wind. Some would surely rather face an easier life in the lowlands, but they cannot compete with the higher-growing plants living there. Most mountain plants manage to compete for light and space only if they cling to the bedrock and gravel in the harsh high alpine climate.
![Glacial river plain at Lake Klevavatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_32.jpg?itok=duW0R_ur)
Rallarvegen
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](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_12.jpg?itok=gpoawGzE)
Trail toward Kyrkjedøri
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](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_13.jpg?itok=ufHTN52m)
Ulvikapollen
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.
![Ramnagjelet, Ulvik](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_45.jpg?itok=pbWriFAE)
Ulvik-village
The ice cap that covered the land during each of the 40 past ice ages over the past 2 million years of Earth's history pressed down the crust of the earth - like a finger on a rubber ball. And when the ice finally loosened its grip 11,000 years ago, the earth's crust rose again, most where the ice was thickest, least where it was thin, quickly in the beginning, and later more slowly. To this day, the land in the inner part of Norway continues to rise by perhaps one millimetre per year. By and large, however, the crust in Hordaland has again reached equilibrium after the weight of the ice was removed.