Jökull


Jökull - 01.12.1985, Page 44

Jökull - 01.12.1985, Page 44
gravel cutting below Melar, some 3 km N of Bessa- staðaá, at an altitude of about 35 km. The best exposure is on the W side of the cutting with current-bedded sands and pebbles, (No. 80/1 in Fig. 6), covered by a layer of variable thickness which is much less well- sorted, No. 80/2 in Fig. 6. The base of the bedded deposit is obscured by debris, but the visible thickness is about 2.5 m, while that of the unsorted deposit above is usually about 0.5 m but some large stones, up to a third of a metre across, occur in this material. Similar deposits are suggested at many places along the W shore of Lagarfljót by banks of rounded stones near Brekka, Brekkugerði, FIús and Geitagerði, all at about 35 m, and just N of the Arnheiðarstaðir homefields, where a long bank of rounded material is visible at about 50 m. There are, however, no good exposed sections in this general area. A little further to the N of Arnheiðarstaðir, however, a better section is visible in another road gravel quarry, just above the positions of Stekkhús and Parthús on the 1:100 000 Icelandic map, at about 50 m altitude. In both the exposed faces layered and sometimes cross-bedded sands are covered by about a metre of unsorted mate- rial, (Fig. 12). The exposures are about 4 m deep in each case, with the lower parts obscured by debris. As in many of the exposures of this material the top nearby is cultivated as hayfield. From about this point north- wards the slope bordering the Fellaheiði plateau, which has so far risen close to the W shore of the lake, begins to swing away to the W along the flank of the Lagarfljót flexure zone, and channels begin to show on it. As mentioned previously the houses and cultivated ground of the next pair of farms to the N, Droplaugar- staðir and Hrafnsgerði are on two platforms at 50m and 70 m, the latter probably the strandline referred to in Hjartarson et al. (1981, p.80). A very prominent bank of rounded material lies just above the houses, between the Hrafnsgerðisá stream and the foot of the Hrafns- gerðisbjarg cliff to the W, then up into a channel between Hrafnsgerðisbjarg and the slope up to the plateau above. Similar material is visible in a roadcut just to the N of Hrafnsgerði but no good exposures are visible. Hovever, a good exposure of current-bedded sands, again covered by about a metre of unsorted material, occurs in a road gravel quarry just below the farm of Teigaból a little further to the N. This material appears to continue N without interrup- tion to the group of farms at Skeggjastaðir and most of the cultivated ground between 60 and 80 m lies on it. These farms lie in an embayment between the Hnaus spur to the E and the Fellaheiði plateau slope to the W and, as mentioned previously, channels lead N over the Hnaus spur, (Fig. 2). This leads directly to the question of the origin of the material at Skeggjastaðir. If it is the result of sub-aerial delta formation from the short streams flowing from the channels, then this flow was in a precisely opposite direction to that of the main water and ice movement in the district. It seems reasonable to Fig. 11. Bedded sands and coarse gravels at about 70 m altitude above and to the N of Skriðu- klaustur. The varying angle of dip could suggest origin in an esker. The grassy slope above covers the bank of coarse, relatively unsort- ed material running from the base of the Tröllkonustígur, left, to Bessastadaá, rt. of the picture. The contact between the two mat- erials is not visible. - 11. mynd. Setlög í um 70 m hœð yfir og norðan við Skriðuklaustur. 42 JÖKULL 35. ÁR
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