Frå Grønafjellet mot Kattnakken. (Svein Nord)

From Grønafjellet toward Kattnakken.

From Grønafjellet toward Kattnakken. (Svein Nord)

Grønafjellet

MOUNTAIN PLANTS FAR TO THE WEST

Mountain plants with their beautiful, colourful flowers are common in high altitude areas in Norway. On the coast there are not so many of them. But, here and there one nonetheless finds mountain plants, and this makes some coastal mountainsides a little bit different. Perhaps the growth on these mountainsides gives us a little glimpse of a distant past?

Grønafjellet is just such a mountainside. The mountainside here is the easterly part of a larger mountainous region in Fitjar. Mountain avens is the most stunning of these mountain plants. With its big, white flowers, it is a beautiful sight, especially in early June. There are also other alpine species that grow especially where the gabbro is a bit crumbly and gravelly. Moss campion and alpine bartsia belong to these. Other parts of Grønafjellet are more barren with moors, where only a few species are able to make a living.

The alpine plants probably came to Grønafjellet quite early. Perhaps some of the first plants put down roots just as the coastal area in the west became ice-free roughly 15 000 years ago. The glacial surge in Younger Dryas times (the period is named after mountain avens, since it has the word "Dryas" as its generic name: Dryas octopetala). about 12,000 years ago did not reach this far west. One can therefore presume that these hardy alpine plants managed just fine during this cold period. Many mountain species have probably disappeared because of the unfavourable climate with warm periods and too dense vegetation in the 11 000 years that have passed to reach our time. But, on Grønafjell the mountain avens survived, and dwarf birch and other alpine species have also right up until today.

Storbjønnskjegg, vanleg i fjellheia på Stordøya. (Bjørn Moe)

Reinrose har sin vestlegaste vekseplass i Hordaland på Grønafjellet. (Jan Rabben)

I tysnesgabbroen, som òg dekkjer den nordaustlege delen av Fitjar, trengde det inn granittiske smelter og varme væsker då austevollgranittane kom på plass for 430–440 millionar år sidan. Nokre av dei danna pegmatittgangar – gangar med store mineralkrystallar, først og fremst feltspat, kvarts og glimmer. I fjellet i Fitjar fann studenten Ståle Raunaholm i 1997 ein spesiell jernfattig, rosa turmalin med namnet rubelitt. Denne steinen er av økonomisk interesse i mineralsamlarmiljøet, jamvel om han ikkje har smykkesteinkvalitet. Dei avlange krystallane vart bøygde og delvis knekte i bitar under den kaledonske kontinentkollisjonen.

See also

Places in muncipality