Etne og Etnedeltaet kring 1900. (Etne Kommune)

Etne and the Etne delta around 1900.

Etne and the Etne delta around 1900, when the delta had a much more natural appearance than it does today. (Etne Municipality)

Etnedeltaet

FROM MAGNIFICENT BIOTOPE TO INDUSTRIAL SITE

During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.

Where bigger rivers meet the sea and form sand banks, there is always a high level of biological activity. The rivers are a constant source of rich nutrients and sediments. By the river mouth there are usually many different forms of life waiting to exploit this runoff. Animals and plants that thrive here are adapted for an environment in which the salinity, temperature, tidal waters and currents in the river are constantly changing.

This zone of outflow, which is also called an estuary, Characteristically introduces great challenges both with respect to the seasons and the changing tides. The whole time there are life forms that die off because they cannot keep up with the fluctuating conditions. These organisms then become nourishment for others. Nature responds by increasing production, such that the number of smaller fish, mussels and other small crustaceans can become exceptionally large. This in turn leads to a high diversity of animal species, and most estuaries also have an unusually rich bird life.

But, the delta sands, which are both flat and nutrient-rich, are well suited also for agriculture. This is how it came to be that the first strips of field were cultivated. Later, these were the preferred areas for settlement. With settlement, followed flood-control and obstructions in the river, mass removal, and often, changes in the usage aimed at meeting the goals of business and industry, since construction costs invariably were low in such areas.

This is how the land was developed in Bolstadøyri, where the Vosso runs out. And this is how things developed also in Eidfjord, Odda and Eikelandsosen, and similarly, on the delta flats in Sogn and Fjordane. The delta in the Etneelva river met with the same fate. But, parts of the sand flat here are still biologically quite rich. On the north side of Etne river mouth, there is a little, undisturbed area that is an important rest stop for wading birds under migration, and for the over-wintering ducks, kittiwakes and grey herons, who all find food in the ice-free river mouth.

Dei gamle grekarane kalla området der elvar når innsjø eller hav, delta etter forma på bokstaven Δ (delta). Møtestaden dannar ofte eit trekanta område med avsetjing av mykje sediment. I osen minkar straumen, elva misser transportevna og legg frå seg sedimenta i form av eit delta ut i fjorden.

 

Dei finaste partiklane (leir og silt) held seg lengst svevande og fell sakte til botnen langt ute. Nærare land, innanfor botnlaga, rullar og hoppar sand og gruskorn langs elvebotnen til dei når deltaskråninga og blir avsette som skrålag. Dei største partiklane som elva fraktar med seg, legg ho att som flate topplag i grus- og steinbankar ytst i deltaet, der elva gjerne forgreinar seg. Når deltaet byggjer seg ut i fjorden, vil laga etter kvart koma oppå kvarandre, med botnlaga nedst, så skrålaga og øvst topplaga. Seinare heving av landet, slik vi har hatt i Noreg etter den siste istida, kan resultera i at vi no ser gamle deltaavsetjingar på tørt land med botn-, skrå- og topplag.

Tørrlagt delta i terrassen på Austreim, tre kilometer aust for Etne sentrum. For om lag 12 000 år sidan vart deltaet avsett i fjorden, men landhevinga har lyfta det 70–80 meter over havet. I det store grustaket kan vi studera lagdelinga i eit slikt delta med horisontale topplag over skrålaga. I nærleiken, nede ved elva, kan vi òg finna dei gamle botnlaga. (Inge Aarseth)

See also

Places in muncipality