Jökull

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Jökull - 01.12.1984, Qupperneq 150

Jökull - 01.12.1984, Qupperneq 150
1955). Another cauldron approximately 4 km west of the 1955 cauldron was first noticed in 1971. H. Björnsson (1977) was of the opinion that the jökulhlaups in Skaftá are caused by a draining of a water cupola formed by geothermal meltwa- ter trapped beneath a depression in the glacier surface. Since 1954 16 Skaftárhlaups have occur- red, 12 draining the eastern (1955) cauldron and 4 draining the western cauldron (Björnsson 1983). None of these jökulhlaups have been accompanied by increased seismic activity (Fig. 2), and nothing in the seismic data indicates that the Skaftárhlaups could be related to volcanic activity in the cauldron area, at the time of each jökulhlaup. It is noteworthy, that the increase in the Vatnajökull seismicity since 1954 is followed by a volume increase in Skeiðarárhlaups since 1955. INTERPRETATION AND CONCLUSIONS The Vatnajökull seismicity during this century can be divided into two periods, a low seismicity period from 1909—1914 and 1925—1953 and a higher seismicity period from 1954 (Table 1, Fig.2). None of the earthquakes recorded since seismic observations began in 1909 were felt in inhabitated areas, not even the largest ones, such as the Bárðarbunga earthquakes in 1974—1980 with M > 5.0. The higher seismicity period from 1954 coincides with increased geothermal activity northwest of Grímsvötn, most likely resulting from increased magmatic activity at shallow levels. Jökulhlaups are generally not found to be accompanied by earthquakes. Two eruptions in western Vatnajökull this century have pro- duced earthquakes with M 3= 3.5, i.e. the erup- tions in Grímsvötn in 1934 and 1983 (see Table 2). The Reykjavík seismometers were not in operation during the eruption in 1922. The erup- tion of 1910, and the probable eruptions of 1938, 1945 and 1954 were not accompanied by signifi- cant earthquakes. Before 1957 eruptions in Vatnajökull could occur undetected by seismometers. ACKNOWLEDGEMENTS Páll Einarsson provided unpublished data and suggested several improvements on the manu- script.. Ragnar Stefánsson at the Meteorological Office permitted access to old seismograms. Beg Month Year Seismometers in operatioa uj^^2n:i/)cokh>h-.cqli_ cc<>lolooi/)cc5é:5:<o Earthq. felt rec. Eruption Grímsv. other SkeiSarár- hlaup km3 May 1903 ? ? X 5 June 1910 | ? x No April 1913 I ? 6 Sept. 1922 X 6 Sept. 1927 ? No Nov. 1933 ? ? No Mar. 1934 X x 6-7 Dec. 1934 9 9 No May 1938 ? 6-7 June 1939 ? -1 May 1941 ? 1-2 Sept. 1945 ? 2-3 Feb. 1948 ? 2-3 July 1954 ? 3.5 Jan. 1960 3.0 Aug. 1965 3.0 Mar. 1972 3.2 Sept. 1976 24 Feb. 1982 1.3 May 1983 x X No Dec. 1983 I I I 0.55 Table 2. The table lists the beginning month and year of all Skeiðarárhlaups, possible eruptions in Grímsvötn and in other volcanic areas in SW-Vatnajökull, during this century. Principal seismometers in operation during each event and available data on the eartquake activity is also shown. (Reykjavík (REY), Akureyri (AKU), Vík (VIK), Kirkjubæjarklaustur (SID), Skamma- dalshóll (SK), Grímsstaðir (GS), Snæbýli (SB), Reynihlíð (RI), Kvísker (KV), Miðfell (MI), Að- alból (AB) and Grímsfjall (GF)). Note that no reliable reports are of earthquakes felt during these events and only twice have the been accom- panied by earthquakes M & 3.5. Tafla 2. Taflan sýnir öll Skeiðarárhlaup og eldgos sem vitað er um á þessari öld, einnig alla tiltæka vitneskju um jarðskjálfta. Athyglisvert er, að eng- ar áreiðanlegar heimildir eru um að skjálftar hafi fundist í þessum umbrotum og einungis tvisvar hafa skráðst skjálftar M 3= 3.S. í bœði skiptin fylgdu skjálftarnir eldgosi í Grímsvötnum. REFERENCES Áskelsson, Jóhannes 1934: Á Vatnajökli. Ferða- sögubrot eftir Jóhannes Áskelsson. (An excursion at Vatnajökull, in Icelandic). Les- bók Morgunblaðsins 9. árg. 24. og 25. tbl. 185-187 og 193-196. Askelsson, Jóhannes 1936: On the Last Eruptions in Vatnajökull. Soc. Sci. Islandica 18: 55p. Áskelsson Jóhannes 1938: Rannsókn eldstöðv- anna í Vatnajökli, ferðasaga. (The Vatna- jökull expedition May—June 1938, in Ice- landic). Morgunblaðið 9 júní 1938. Björnsson, H. and M. Hallgrímsson 1976: Mælingar í Grímsvötnum við Skeiðarárhlaup 1972 og 1976. (Measurements in Grímsvötn 148 JÖKULL 34. ÁR
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