Latest from the Met Office, posted about 6 pm:
Seismic activity around the magma dyke has remained fairly steady in recent days. At 5 pm today, around 1,400 earthquakes had been recorded since midnight, the largest 2.9 by Hagafell shortly after 1 pm. Most earthquakes were smaller than 2 and the most concentrated activity was seen by Hagafell.
Land deformation related to the magma dyke continues, though it has slowed a little since yesterday. The latest models based on GPS measurements and satellite data still show that the most significant tectonic divergence is north of Grindavík, near Helgafell. If magma manages to break the surface, it is still most likely to occur in this area.
Today sulphur dioxide was detected from a borehole at Svartsengi, just north of Þorbjörn. The borehole goes diagonally underneath Grindavíkurvegur and extends into the crust towards the Sundhnúkur craters. The end of the borehole is therefore near the part of the crust where the magma dyke is believed to be. Further measurements will be taken tomorrow, but the fact that sulphur dioxide was detected from the borehole confirms that magma is present north of Hagafell, as models have suggested.
The likelihood of an eruption is still considered high. The Met Office continues to monitor signs of seismic activity becoming shallower and sudden divergence, which could precede an eruption. There are no signs of an imminent eruption at this time.
They'll probably translate it themselves soon, but that's basically what it says.
https://www.vedur.is/um-vi/frettir/jardskjalftahrina-nordan-vid-grindavik-hofst-i-nott