Rit (Vísindafélag Íslendinga) - 01.06.1967, Side 196

Rit (Vísindafélag Íslendinga) - 01.06.1967, Side 196
192 composition. The volume of rhyolitic tephra as fresh fallen is four to five times and the volume of the basaltic tephra about three times the volume of dense rock of the same com- position. Studies of Hekla (Thorarinsson 1954, 1967, Tómasson 1967) have revealed that the bulk of the tephra produced by an eruption which may last a year or more is produced during an initial, Plinian phase of the eruption, lasting usu- ally only a few hours, and this tephra is to a great extent rhyolitic or dacitic, whereas the tephra produced later in the eruption is mainly andesitic. The first historical eruption of Hekla, 1104 A.D., produc- ed about 0.5 km3 of tephra (2.5 km3 as fresh fallen) and that tephra was rhyolitic or nearly so. The second biggest tephra production was in the 1300 eruption, 0.125 km3 (0.5 km3 as fresh fallen). The 1766/68 eruption ranks as third with 0.1 km3. Altogether the 14 Hekla eruptions have produced a little more than 1 km3 of tephra, whereof nearly 50% is rhyolitic, the rest dacitic and andesitic. We know less about the volume of Hekla’s historical lava flows as lava of only 7 eruptions has been identified. The total volume of the lava produced by the last three eruptions is about 2.7 km3 or an average 0.9 km3 per eruption. This is doubtless more than the average of all 14 eruptions (the 1104 eruption probably did not produce any lava) and the total volume of lava produced by Hekla in historical times is probably not far from 8 km3. A part of this lava is dacite, but the bulk of it is andesitic. The biggest lava production was by the 1766/68 eruption, about 1.3 km3, and the vo- lume of lava and tephra of this eruption is the third biggest in Iceland in historical times, the biggest ones being the Laki 1783 (12.5 km3) and Öræfajökull 1362 (2 km3). Let us then turn to Katla, the second biggest producer. The total number of historical eruptions in Katla or the Katla area is according to Thoroddsen 14. Tephrochronological stu- dies have revealed that Katla had a big eruption about 1000
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Rit (Vísindafélag Íslendinga)

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