Jökull


Jökull - 01.12.1984, Page 96

Jökull - 01.12.1984, Page 96
 a 1 a b c d C b a 4 a b a 2 a b c d e d c b a 5 a b c b a 3 a b c d e f i r~ ! i 1 1 e d c b a 6 Fig. 19. Formation of a dyke which is composed of 12 col- umnar rows. (1) Intrusion of the first magma phase (a). This magma phase cools enough to form columns before the next magma phase (b) splits (a) in two parts (2) . The process continues (3) -(5) until the final magma phase (f) is intruded (6). The columns of (f) are slightly bent, thereby indicating the direction of movement of the magma. The section can be either vertical or lateral. Mynd 19. Myndun gangs sem samanstendur af 12 stuðlaröð- um. Stuðlaröð (a) er elst, stuðlaröð (f) yngst. í hvert skipti sem kvika treðst inn klýfur hún nœstu stuðlaröð á undan í tvennt. Yngsta stuðla- röðin (f) er sveigð í miðju í flæðistefnu kvikunnar. Sniðið getur verið hvort sem er lárétt eða lóðrétt. is essentially the same as the tensile strength of the country rock. Thus there must be some time limit between successive magma phases of a single dyke. Using the conduction cooling models of Jaeger (1968), it can be shown (Gudmundsson 1984) that the cooling of a two meter thick magma phase from the initial temperature of 1200°C down to 800°C (i.e. when columnar joints start to form (Jaeger 1961)) takes about 270 days. Thus the time between successive magma phases, for a typical dyke, should be of the order of a few hundred days. This time is comparable with the time between successive phases of intrusion in the Krafla volcano in northern Iceland (Björnsson et al. 1979). DISCUSSION The present results of dyke studies in north- western Iceland are generally similar to those of eastern Iceland (Gudmundsson 1983a). Nevertheless, there are some dissimilarities. For instance, although the average dyke thickness for northwestern and eastern Iceland is essentially the same (4.3 m and 4.1 m respectively), the thickness distribution is different. Thus thin dykes are relatively more common in northwest- ern Iceland compared with eastern Iceland. About 17% of the dykes in northwestern Iceland are less than 1 m in thickness, but only about 10% of the dykes in eastern Iceland. Also, dyke strike and dip is more variable in northwestern Iceland. These differences are associated with the trend of individual dyke swarms in northwestern Iceland, which varies, whereas the dyke swarms of eastern Iceland all have a similar trend. The dyke swarms of northwestern Iceland are not as well defined as those of eastern Iceland, a fact that is at least partly explained by greater degree of erosion (referring to the original surface of the lava pile) in eastern Iceland. 94 JÖKULL 34. ÁR
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