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Ulevn Camp around 1915.

Ulven camp

16.06.2018 - 16:03

Os rectory

Os rectory

29.05.2019 - 15:12

Geologist William Helland-Hansen examining a quartz conglomerate in the Ulven Syncline on one of the hills by the north west end of Lake Ulvenvatnet.

Ulven

03.01.2019 - 15:16

In the region of Ulven phyllite occurs with Hordaland's youngest fossils, and a beautiful quartz conglomerate. The phyllite and conglomerate got squeezed into the bottom of an ancient oceanic crust, made of gabbro and greenstone, in the heart of the Caledonide mountain chain.

Store Milde, draft of the façade.

Store Milde

30.03.2018 - 08:38

Klosteret

12.06.2018 - 19:10

Model of the king’s estate around 1300

Bergenhus

12.05.2020 - 14:50

Marmorøyen

05.12.2018 - 16:24

From the mountainous rocks just below Sandvikshytte cabin on Sandviksfjellet.

Sandviksfjellet

06.03.2019 - 15:22

On Sandviksfjellet there are old boulders that have been made into mountains. The stones have been stretched out or squeezed together between huge slabs of rock, during slow, but powerfulprocesses of transport. This conglomerate shows, in quite a special way, the enormous powers that were active during the collision between Norway and Greenland over 400 million years ago.

At lake Gaupåsvatnet.

Gaupås

19.05.2018 - 19:24

«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.

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