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Ølve

Ølve

04.01.2019 - 15:57

Ølve has a special soil type. Here one finds an extra hard clay soil. This is especially noticed by those who work with excavating for building foundations and the like. Often it is necessary to use especially big digging machines and sometimes even dynamite in order to break up the compact masses. The reason for this is the growth of the glaciers toward the end of the Ice Age: The clay, that was first deposited in front of the glacier, came under great pressure when the glacier later grew and slid out over the clay.

Ådlandsstova, as it stood at Nedre Ådland, Stord

Ådlandsstova

31.03.2018 - 14:36

The Ådland house is one of the biggest medieval houses still existing in West Norway. It is constructed from unusually large, hard fir wood, beautifully oval-cut. One story links the cottage to the Gildeskålbakken at Orninggård (Lower Ådland); thus indicating that the cottage has been the medieval banqueting hall. The building has been dated back to the 13-1400s by carbon dating.

Portrait of Jonas Lie

Undarheim

19.06.2018 - 16:18

Toward Støle and Sørheim, 1920.

The village of Etne

18.12.2018 - 20:39

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

The main building at Huglo, Stord

Sørhuglo

26.06.2018 - 09:59

The tax collector’s farm at Sørhuglo is one of the many farms for state employees in Hordaland. According to history, “Futastovo” was built by the tax collector Gram in the second half of the 17th century. In 1943 the building was moved to Sunnhordland Folk Museum.

Støle church

Støle church

18.06.2018 - 20:27

The stone church at Støle may have been built around 1160 probably as a private chapel for the mighty Stødle clan. It is likely that it was Erling Skakke, the king’s representative and father of king Magnus Erlingsson, who built the church.

Den flate terrassen på moreneryggen på garden Tjedla viser kor høgt havet stod på slutten av den siste istida.

Skånevik- moraine

06.03.2019 - 14:58

In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.

Skorpo (Svein Nord)

Skorpo

29.03.2018 - 11:25

Skorpo - Polished by glaciers and meltwater

Selsøya

19.05.2018 - 20:37

The hayshed in Håvik, Bømlo

Outer Håvika

16.11.2022 - 13:19

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