Jökull


Jökull - 01.12.1988, Side 8

Jökull - 01.12.1988, Side 8
TABLEIV. List of molluscs and localities Partly based on Askelsson (1934) and Kjartansson (1958). TAFLA IV. Listi yfir skeljar og aðrar lífrœnar leifar og fundarstaði þeirra. SPECIES/TEGUND Pododesmus squamula • • • • Chlamys islandica • • • Crenella decussata • Nucula tenuis • • Nuculana pernula • • • Mytilus edulis • • • Tridonta montagui • Arctica islandica • • • • • • • Macoma calcarea • • • • • • Hiatella arctica • • • • • • • • Panopea norvegica • Mya truncata • • • • • Zirfaea crispata • Puncturella noachina • Natica pallida • Natica ajfnis • Boreotrophon clathratus • • Buccinum undatum • Thracia myopsis • • Balanus sp. • • • • • • • • • • • • Bryozoa • • • Crustacea fragments • • Mollusca fragments, unidentified • • • • • HREPPHÓLAR (Lu-2401, Lu-2402) Close to Hrepphólar the river Stóra-Laxá has found its way through the Búði moraines, at about 65 m a.s.l. The section exposed in the northem bank is about 1000 m long and c. 20 m high (Fig. 5). The following stratigraphy was observed: Lowest is unit A which consists of silty diamic- ton, irregularly stratified, with abundant outsized clasts which are rich in rhyolite. It resembles the Búðaberg diamicton, but contains more dropstones. In the section this unit has a ridge-like appearance, with maximum thickness of c. 15 m. The diamicton has been deformed by a glacial push. Fragments of Balanus sp. are widespread in the diamicton. A radiocarbon dating of a Balanus sample gave the value of 9.745±140 BP (Table II: Lu-2401). This is a maximum age for the disturbance of this diamicton. The diamicton is unconformably overlain by unit B, a 5 m thick unit of crudely stratiíied, coarse gravel, which constitutes the upper part of the 6 JÖKULL, No. 38, 1988
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