Jökull


Jökull - 01.12.1989, Side 50

Jökull - 01.12.1989, Side 50
Fig. 8. The magnetic map. Contour lines are 500 nanotesla apart (1 nanotesla = 1 gamma). Shaded areas indicate negative values. Mynd 8. Flugsegulkortið. Milli jafngildislínanna eru 500 nanótesla. Skyggð svœði sýna lágan segul- sviðsstyrk. form what might be referred to as the Brunhes mag- netic lineation (Jónsson and others, in press). A host of smaller anomalies is also present in the map, some due to geological phenomena and some due to topography. The fact that they are elongated NE-SW is for some of them an artifact of the direc- tional filtering. To properly study those anomalies, a magnetic map should be gridded on a smaller scale and the appropriate anomaly separation techniques applied to each case individually. The filtered map should be studied with this in mind. Several anomalies are présent on the Reykjanes peninsula west of the Hengill area. They reflect the en echelon distribution of volcanically active fissure swarms on the Reykjanes peninsula (Jakobsson and others, 1978; Jónsson and others, in press). South of Hvalfjörður, an anomaly occurs over the eroded Stardalur volcanic center (Friðleifsson and Kristjánsson, 1972; Kristjánsson, 1987), accom- panied by a localized high in the gravity map (Fig. 5). West of that, an anomaly is seen at the mouth of Hvalfjörður, presumably a signal from the so-called Kollafjörður central volcano6. Further north there are anomalies associated with the Hafnarfjall and Ferstikla central volcanoes and magnetic lineations caused by the tilted Pliocene lava pile. In the northeast quarter of the map are several notable anomalies. The first occurs over the shield volcano Ok, the second is over the southwest comer of Langjökull, the third is over the center of the 6. Both these magnetic anomalies, at the Stardalur and Kolla- fjörður central volcanoes, actually seem elongated NW-SE on an unfiltered map. It might also be noted that both anomalies were observed to correspond to rather large localized highs (=10 milligals) on the gravity map of Einarsson (1954). 48 JÖKULL, No. 39, 1989
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Jökull

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