Fagradalsfjall is a tuya with NS structure due to earthquake faults having that alignment. Besides that, the volcanic systems have left NE-SW oriented slopes, as can be expected in that area. Thirdly, perpendicular lines can be detected shaping the other sides pointing NW-SE. That is a bit unexpected, except keeping the convection rolls underneath in mind. The result looks like this, when sharpened with inserted lines:
The shape of Fagradalsfjall area.
This diamond shape is quite apparent, when pointed out. The NS structure is also exaggerated with inserted lines. The red line indicates the site of eruption.
The eruption that started March 19th ein the Geldingadalir valley at Fagradalsfjall on the Reykjanes Peninsula of Iceland is the first to occur within the area since the year 1240. No one can predict for how long it will proceed, but it has been found that the lava is rather hot, or between 1180-1190°C, as can be seen here: https://www.mbl.is/frettir/innlent/2021/03/22/likist_dyngjugosbergi/
The lava is therefore of the category found in shield volcanoes. Therefore the possibility that this eruption will go on for some time can not be ruled out. The crater of Thrainsskjoldur (Þráinsskjöldur) is found nearby, a large shield volcano covering the central parts of the peninsula. Now we consider this as the smallest eruptions we have seen in Iceland. If this is really an effusive eruption of ‘shield volcano category’, it surely comes as a surprise.
The dyke of Geldinigadalir eruption.
The dyke extends about 8 km over the theoretical area of the seismic zone as extended from South Iceland Seismic Zone over the Reykjanes Peninsula, bending towards the Reykjanes Ridge. It is assumed according to the model that the main part of magma is originated from NW, and when the dyke propagates to the SW, it encounters the division line of the polygon.
The different composition of this lava compared with the lavas erupted around 1000 years ago, can be explained according to this model with influx through the ductile mantle (below the brittle crust) from the NW division line of the Reykjanes polygon, reaching underneath the dyke into a conduit leading to the eruption site at Geldingadalir.
The material of the dyke might have propagated from the NW, and outflow could be found into the mantle at the SW end of the dyke. At least, no clue of either depletion or accumulation of magma within the earth is being measured for the moment.
As magma is entering the brittle crust with a flow rate of perhaps about 20 cubic meters per second, a dyke is forming in the southern half of the Reykjanes Peninsula. Geoscientists are therefore in the difficult position of explaining what is going on, and at the same time trying to predict what will happen. No one can foresee an eruption, but different scenarios are studied. Here I will show you a simple map with the main features. Convection rolls model divisions are marked with red lines. The tensional vectors are parallel to those lines. A red arrow indicates the present scope of the dyke being formed. Information from the Icelandic Met Office is found here: https://www.vedur.is/um-vi/frettir/skjalfti-m57-a-reykjanesi
Dyke formation at Reykjanes Peninsula in 2021
We are aware that, where the dyke has already formed, the magma might make its way upwards. The triggering effect might be extra heat entering the dyke, and that might originate from the convection rolls division lines found south-west of it. As the dyke propagates farther in that direction, the more likely it is that an eruption will occur according to this model. In 2014, the Holuhraun eruption started under similar circumstances.
On this map, I have superimposed the grid on the original map from the Icelandic Land Survey showing tectonic drift vectors.
Reykjanes Peninsula in context with convection rolls grid and tectonic drift vectors.
The drift vectors show the rotation taking place within the Reykjanes polygon. Further analysis provides this drawing:
The Reykjanes Earthquake Zone and a few relevant dynamic factors.
The small black arrows indicate the unaltered drift directions measured directly with GPS stations. It can be reasoned that the rifting process of the volcanic systmes is perpendicular to the main tensional effect within the area, indicated with light gray arrows. Similarly, pressure is excerted, creating the earthquake faults with NS alignment. The western half of the polygon seems to rotate in a semi-circular way with center at its western corner, but is at the same time subject to rifting process to the west. Similarly, the eastern half is subject to rifting to the east as compared to the NS axis of the polygon.
The earthquakes at Reykjanes Peninsula show resemblance to the volcanic systems, but occur on NS faults. This should be due to an interplay between tension and pressure within the polygon.
To realize what forces are affecting the earthquake zone of Reykjanes, a 3D model can be useful. The convection rolls below interact with the basic tectonic drift. Layer A has direct contact with the ductile part of the tectonic plate. Layer B has a certain degree of coupling effect with layer A, also affecting the tectonic plate. The ductile part is twisted as a result, turning anti-clockwise. Therefore, the polygon forms a rupture along the NS-axis from one corner to the other. This leads to the fact that the brittle part above may be affected by the twisting effect from below at different points of time at each side of the NS-axis.
The earthquake zone of Reykjanes Peninsula
The convection rolls are nearly perpendicular to each other. Drawn to scale. The coupling effect between layers leads to different pressure and tectonic drift directions, besides earthquakes.
The relevant earthquake swarm is shown in the previous post.
Magic Magma 