Jökull


Jökull - 01.12.1978, Page 7

Jökull - 01.12.1978, Page 7
Fig. 3. Fluvioglacial sediments in the Vatnsskard-Saemundar- hlíd area. The southernmost part is a remnant of a medial moraine, but north of the farm Fjall the moraine transforms into a kame terrace. Some large eskers are situated to the north of the terrace. Inside the areas covered with fluvioglacial sedi- ments contours are shown with broken lines. Key: 1. Eskers, 2. Mounds, 3. Fluvioglacial sedi- ments covered with bog, 4. Ket- tles, 5. Lake in a kettle, 6. Inner limit of a kame terrace, 7. Ter- races, 8. Dry meltwater chan- nels, 9. Lateral channels, 10. Large meltwater channels, 11. Recent fluvial sendiments. Mynd 3. Jökulárset í Vatnsskarði og Sœmundarhlíð. Syðsti hlutinn er leifar urðarrana en við bœinn Fjall tekur við jaðarhjalli. Nyrst eru svo nokkrir stórir malarásar. Hœðarlínur eru sýndar með brotnum línum á svœðum sem þakin eru jökulárseti. Skýringar: 1. malarásar, 2. haugar, 3. jökulárset hulið mýri, 4. jökulker, 5. stöðuvatn í jökulkeri, 6. innrimörk jaðarhjalla, 7. hjallar, 8. þurrir far- vegir, 9. jaðarrásir, 10. stórir far- vegir, 11. ungt árset. areas are covered by ablation till. In the mouth of the Djúpidalur valley the deposits consist entirely of ablation till and no eskers or fluvioglacial material are observed. On Hlídarfjall, however, the eskers consist of fluvioglacial gravel with a mantle of ablation till. This difference must be due to different meltwater supply on the surface of the glacier. LATE GLACIAL MARINE FEATURES AND ICE RECESSION Three major raised delta deposits are found JÖKULL 28. ÁR 5
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