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![Sketch showing the process of formation of an esker.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/skisse.jpg?itok=dTA78127)
![Scythes used to be made in the brick house just across the motorway through Folkedal](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_367-3.jpg?itok=Q7DufBD1)
Nedre Folkedal
For many years the Folkedal scythe had a good reputation. Immediately above the highway through Folkedal there is a long brick building, on the inner side of the river. Here production of scythes went on to the beginning of the 1950s.
![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.
![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.
![Sandy beach to the west of Kallsøyna, outermost Valen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_353_herdla_150.jpg?itok=XcEOtEry)
Herdla – glacial deposits
The shift in the landscape is striking between the barren craggy moors north on Askøy and the green fields of Herdla, which has the county's biggest farm. The majority of Herdla, such as the island appears today, is a gift from the glacier: The glacier that advanced here over 12,000 years ago stopped at the northern tip of Askøy and took its time building up the moraine on Herdla. Since then, Herdla has been under continual transformation. The re-organisation of the loose sediment deposits continues today.
![Section of the lid of the chest painted around 1830, by Nils Johannesson Tveiterås](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_250-_4xy.jpg?itok=CgKmtwUv)
![Litlematre](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mas_10.jpg?itok=wpTaAy0K)
![Door](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_319-4.jpg?itok=-5nryjpy)
![The smithy at Odland, Meland](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_297-1_0.jpg?itok=n38ypKHf)
Odland
The auger smithies in Odland and Fosse were amongst those which had the largest production of augers in the period between the Wars. Martinus Fosse built a smithy in 1877, and this was in operation right up to the 1980s - one of the centres for auger production in Meland. In 1930 yet another smithy was built here. There was a smithy at Fossesjøen as early at the 18th century, and at the end of the 19th century they went over to auger smithing. There is still a market for hand-forged augers.
![View in over Mostraumen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_16.jpg?itok=GnR34JLO)
Mostraumen
Until 1743 the people from Modal had to wait for a flood in MOSTRAUMEN before they could draw their boats up the river current, and then row back across Lake Movatnet. But, that year the flood opened a free passageway all the way to Mo. Hordaland had gained a new tidal waterway.