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• 41. Bardarbunga-2014_December-events

  in the northwestern Vatnajökull area with a series of small quakes around Tungnafellsjökull and Herðubreiðartögl. A few small ones were also detected in the dyke intrusion. 30 December 2014 - now confirmed 82.8 km² Two days ago, difficulties in approaching the lava led to doubts about the newest estimate of its size. The Institute of Earth Sciences has now confirmed that the lava is almost 83 km², see /media/jar/Bardarbunga-2014_December-events.pdf

• 42. 47th Nordic Seismology Seminar

  and then click on "Registration" on top of that page (see screenshot). Conference costs are 30.000 ISK (~220€), to be paid upon registration. See details on cancellation policies on the registration page. Rooms at Grand Hotel Reykjavík can be booked during the registration process. Participants are free to book other potentially cheaper hotels in the vicinity.Conference costs include coffee /norsem/norsem2016/registration/

• 43. Registration

  to give an oral or poster presentation, whether you intend to participate in the excursion to Langjökull on Friday afternoon, and whether you arrive on June 19 or 20. A block booking of rooms has been made at the Reykholt hotel. Potential participants are encouraged to register early due to limited number of hotel rooms. The deadline for registration was: April 15 – abstract, registration /lidar/lidar-2013/registration/

• 44. Gyrite_Brandt_(Local_Government_Denmark,_DK)

  and this was done by stakeholder involvement with different levels of involvement. The climate adaptation plan has been presented to the general public and has been used as a basis for integrating climate adaptation measures in the Municipal plan. Lolland is now an pilot study area for two Interreg projects SUSCOD and BLAST, both dealing with the coastal zone and climate adaptation. /media/loftslag/Gyrite_Brandt_(Local_Government_Denmark,_DK).pdf

• 45. Monitoring Öræfajökull – update 22. Dec. 2017

  the volcano, as assessed by the temporal changes on the ice-surface are not suggesting an increase. There are no clear indications that water is accumulating beneath the ice in the cauldron and, given the trend of the activity until now, it is unlikely to expect a flood in the next months. However, it is very important to keep following this process with regular measurements of the caldera /about-imo/news/monitoring-oraefajokull-update-22-dec-2017

• 46. A new low pressure record for July in Iceland

  21:30 to 22:30, 972.4 hPa. The pressure in Iceland has only on three occasions dropped down to 975 hPa or lower in the entire record extending back to the 1820s. These cases were 974.1 hPa in Stykkishólmur on 18 July 1901, 974.3 hPa in Stykkishólmur on 19 July 1923 and 975.0 hPa in Reykjavík 11 July 1912. It should be kept in mind that although the pressure was recorded at a few stations all /about-imo/news/nr/2504

• 47. Bardarbunga_Daily_status_report_250814

  Bárðarbunga update 25082014 2014-08-25 13:58 UTC Bárðarbunga update Compiled by Hildur María Friðriksdóttir, Benedikt G. Ófeigsson, Melissa Anne Pfeffer, Sara Barsotti, Kristjana Eyþórsdóttir Based on Seismic, GPS, Hydrology Eruption plume Height (a.s.l.) No eruption and no eruption cloud. Heading No eruption and no eruption cloud. Colour No eruption and no eruption cloud. Tephra fallout /media/jar/Bardarbunga_Daily_status_report_250814.pdf

• 48. Bardarbunga_Daily_status_report_260814

  a significant part, or all, of the fissure is beneath the glacier. This would most likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity. Other scenarios cannot be excluded. For example, an eruption inside the Bárdarbunga caldera is possible but presently considered to be less likely. /media/jar/Bardarbunga_Daily_status_report_260814.pdf

• 49. Eyjafjallajokull_status_2010-06-11_IES_IMO

  water to flow up onto a road west of a bridge, as there it now not much difference between the height of the bridge and the river channel. Conditions at eruption site: A lake, about 300 m in diamenter, has formed at the bottom of the big crater. Steam is rising from the rims, especially from the north side. In the morning the steam cloud only rose about 100 m over the crater /media/jar/Eyjafjallajokull_status_2010-06-11_IES_IMO.pdf

• 50. norsem_voss

  monthly bulletin was that of April 2015. Apart from the destructive earthquake in Italy and the nuclear explosion in the DPRK, the most significant seismic events recorded by the seismic service at GEUS in the recent period, are a sequence of earthquakes in the Disko Bay area in West Greenland. Since the beginning of the sequence on April 5th 2016, 95 earthquakes have been /media/norsem/norsem_voss.pdf