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![](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/byparken_bergen_norway_20050516.jpg?itok=r7clF_UH)
Byparken
It isn't true that hungry students have hunted down basking ducks in the city park Byparken in their spring fervour, as rumours may have it. But, it is not unusual to see students throw themselves over the park's wild birds, and hold on to them tight. They ring the birds. Because of this, we know quite a lot about the birds in Byparken.
![Fjøsanger](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_49.jpg?itok=x0vBKTNz)
Fjøsanger
Fjøsanger is known among ice age researchers from around the world. Under an excavation in 1975-77, geologists from the University of Bergen found layers from the last interglacial, ca. 115 000 to 130 000 years old.
![At lake Gaupåsvatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_334_gaupas_koronitt_150.jpg?itok=Wq7ffNPu)
![](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_12_0.jpg?itok=hv7XxFE6)
![Up to the 1870s Osøyra was a military training area.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_236-1.jpg?itok=dIxgmecK)
Osøyro
The coastal settlement of Os begins to take form in the middle of the 1800s. This is when craftsmen and traders begin to settle at the river delta.
![Ulevn Camp around 1915.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_237-2.jpg?itok=_5pK0Vd7)
![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.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/os_31.jpg?itok=kdZe21Du)
Ulven
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.
![From the mountainous rocks just below Sandvikshytte cabin on Sandviksfjellet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/sandviksfjellet_berg_42_0.png?itok=ojW0mG7e)
Sandviksfjellet
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.
![Model of the king’s estate around 1300](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_254-3.jpg?itok=epp8SSrJ)