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Prospect of Alvøen, Bergen

Alvøen

12.06.2018 - 19:13

Alvøen is one of the oldest industrial places in Norway. As early as the 1620s a gunpowder mill was built here. The place itself was well situated for industrial activity, lying only 100 m from the waterfall, which provided power for the mill, and a good harbour wherefrom the products were shipped. The success of the gun-powder mill varied in the 1600s and 1700s, but what made Alvøen best known was its paper production.

Prospectus Damsgård, Bergen

Damsgård

12.06.2018 - 19:20

As a fairytale castle Damsgård Hovedgård lies on the slope rising up from the Puddefjord. The old connection between the farm and the sea, as we see it on Dreier’s prospectus from 1810, has been broken up by roads and encroachments in the building mass. But the main building itself is a central monument in Norwegian architecture from the 1700s – one of the finest representatives for the rococo period, with a magnificent and rich décor both in its interior and exterior.

Reppadalen (Svein Nord)

Reppadalen

31.03.2018 - 19:33

The unusual bog landscape, with enormous peat deposits surrounded by steep mountainsides, makes Reppadalen in Arna an exciting, but little visited tour destination for most of Bergen's inhabitants. Those who live in Arna, however, know to make the most of its beautiful natural splendour.

«Steene Gaard». Prospectus by J.F.L. Dreier, 1816

Stend

12.06.2018 - 19:21

Garden Stend høyrde i mellomalderen til Nonneseter kloster. Etter reformasjonen var han i eiga til Vincents Lunge fram til 1680. Då overtok generaltollforvaltar Hans Christophersøn Hiorth eigedommen. Hiorth vart adla i 1682, og Stend fekk status som adeleg setegard. Truleg fekk den staselege hovudbygningen si form i Hiorths embetstid.

Store Milde, draft of the façade.

Store Milde

30.03.2018 - 08:38

Årstad in the 1890s

Årstad

12.06.2018 - 17:18

Alrekstad (later Årstad) is the birthplace of Bergen. The estate was an estate for Harald Hårfagre and several of his descendants: Eirik Blodøks, Håkon den gode og Olav Tryggvason. These first kings moved with their courts and guardsmen from estate to estate. From these estates the king ruled the country.

The delta at the outflow of Storelvi in Granvinsvatnet.

Granvinsvassdraget

24.06.2018 - 15:36

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

Joberget

26.05.2018 - 11:37

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.

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.

Skjervet toward the east. Jørdre Farm up to the left.

Skjervet- river theft

02.12.2018 - 20:59

At the end of the last ice age the ice flowed out of Hardanger fjord in such a fury that it forced the meltwater from Voss to run back uphill toward Granvin. The glacier from Raundalen down the windy valley along the Vosso to Bolstadøyri went too slow to make the turn.

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