Rit (Vísindafélag Íslendinga) - 01.08.1930, Side 5

Rit (Vísindafélag Íslendinga) - 01.08.1930, Side 5
5 nemoralis, Deschampsia cæspitosa, D. flexuosa and Festuca rubra were most abundant. These vegetation- groups, which have already been men- tioned, covered the forestless tracts of land, but now ITl turn to the forest-vegetation itself, which, as aforementioned, was the only forms of vegatation I found time to examine closely. The Forest of Ásólfsstaðir. This forest, as mentioned above, is in the valley through which Hvammsá flows. The forest-land is not continuous, but frequently dissected, both by fairly deep ravines, of which several are forest-grown, and in places by landslips from the mountain slopes. These are forestless, but have scanty clayep- flat-vegetation. Besides this, there are fairly big clearances in the forest, mostly covered with heather-vegetation. The forest is mostly a low and stunted copsewood of various density. In some places it is hard to break through, but in others sparse and far between the branches. The height is also uneven. Up in the mountain slopes the copse- wood was frequently not more than ab. 1 metre in height, but there were also places where it was 2 or 3 metres, and I even measured several branches reaching over 4 metres. On the whole, the copsewood was stunfed and showed traces of heavy snow masses and grazing. The slopes are very arid. Above the forest the Grimmia heath and the fell-fields begin immediately; in some places the forest-turfs were left close to denuded pafches, but this occurred with greater frequency in the forest of Skriðufell. In the lowland the copsewood was higher, mostly ab. 2 metres, and in oíher places even more, in Vatnsás the forest is fairly high and erect. As mentioned before, I used the circling method of Prof. Raunkiær, cf. p. 2. I chose the circling-stations in copsewood of medium density and in different altitudes, the lowest on the Iowland beyond Hvammsá, but the others in the mountain slope above Ásólfsstaðir, at the bottom of Skóggil and at the top of Stórólfshlíð. Here follows a table showing the resuits of the circlings.

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