Jökull


Jökull - 01.12.1984, Side 5

Jökull - 01.12.1984, Side 5
Further examination of available records (Jóhannesson 1983) shows firm evidence for eruptions in 1902-1904, 1922, 1933, 1934, 1938, 1945 and 1954 and possible eruptions in 1939, 1941 and 1948. The definite eruptions were actually observed or conditions at the volcano after a jökulhlaup show signs of an eruption. For the otheT ones the indications for an eruption are jökulhlaups at unusually short intervals which suggests that the frequency may have been influ- enced by eruptions. Jökulhlaups without accom- panying eruptions took place in 1960, 1965, 1972, 1976, and 1982. Little can be said about the volume of these eruptions but the apparently short duration and the thin or no tephra layers suggest that each eruption had fairly small volume but this is com- pensated by high eruption frequency. This high eruption frequency makes the petrology of the products interesting because they are likely to interrupt the evolution process of the magma that feed the volcano. To explain the 5000 MW Fig. 2. The Grímsvötn caldera showing the eruption site and the ash layers formed in the 1983 eruption. Mynd 2. Staðsetning gosstöðv- anna í Grímsvötnum 1983 og öskugeirarnar þrír sem þá mynduðust. geothej-mal activity 50 million m3 of mágma need to be cooled down to 400°C (Björnsson et al. 1982). This large volume may either be steadily supplied into high level magma reservoirs or large magma volumes already present in the upper crust may be the source. Both possibilities may affect the magma about to be erupted and since the products are instantly quenched at the time of eruption the state of the magma at that time is further reflected in the glass and minerals of the tuffs. THE 1983 ERUPTION In the morning of May 28th 1983 several seismometers of the Icelandic seismic network recorded unusually intense seismic activity originating in Grímsvötn. This lasted from early in the morning until noon and was followed by a continuous volcanic tremor which was most intense on May 28th and 29th but lasted until just JÖKULL 34. ÁR 3
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Jökull

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