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1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

2. Monitoring of Hekla

are reliably recorded has improved since 2000. Increased earthquake activity at Hekla results in an automated audio warning in IMO's monitoring room in Reykjavík, which is staffed around the clock every day of the year. The warning system, which is used for all regions in Iceland, is based on earthquake size, earthquake rate and energy release relative to predefined thresholds. In addition /about-imo/news/monitoring-hekla

3. Reports and publications

et al. 3 2005 Seismic hazard in the Hengill area based on the SIL earthquake catalogue - First results (PDF) Kristján Ágústsson, Páll Halldórsson 42 0,8 2005 A model of the release of the two June 2000 earthquakes based on all available observations (PDF) Sigurlaug Hjaltadóttir, Kristín S. Vogfjörð, Þóra Árnadóttir, Páll Einarsson, Peter Suhadolc 8 8,2 2005 /earthquakes-and-volcanism/reports-and-publications/

4. News

News © Oddur Sigurðsson The western cauldron on 19 August 2000, shortly after a jökulhlaup in Skaftá /about-imo/news/bigimg/3142

5. Articles

Articles © Veðurstofa Íslands The lowering of the surface of the Snæfellsjökull ice cap between 1999 and 2008 /weather/articles/bigimg/1618

6. An earthquake in South Iceland

that the earthquake is an aftershock following a strong earthquake in the same region in June 2000. This is because not all the strain in the bedrock was released during the 2000 earthquakes. It cannot be excluded that a similiar-sized earthquake could occur in the same region in the near future. The lowland in South Iceland is one of the most seismically active regions of the country, where /about-imo/news/nr/2888

7. norsem_ingi

may have caused preseismic velocity changes in the crust. The original design of the network had a high clock accuracy (±1 ms). S-waves tend to be very clear, and successful 1D velocity model (SIL model) has been used to locate earthquakes in the area, suggesting relatively simple velocity structure in spite of active tectonic setting. Earthquakes in Southern Iceland during the period /media/norsem/norsem_ingi.pdf

8. News

9. News

at the Reykjanes peninsula during the period from January 2000 until June 2015. Blue lines represent known faults which have been active in Holocene or Recent Epoch, i.e. after the ice age (Páll Einarsson, 2015). Also shown in yellow are volcanic systems with fissure swarms (Páll Einarsson and Kristján Sæmundsson, 1987). Enlarge /about-imo/news/bigimg/3150

10. Earthquakes shake Bláfjöll ski-area

around M4 occurred, only 5 seconds apart, 6 km south of Bláfjöll mountains. Several smaller aftershocks were recorded. The earthquakes were felt widely in the capital area, and also in Ölfus and Akranes. The earthquakes are located on the tectonic plate boundary that lies eastwards along the Reykjanes peninsula where earthquakes of magnitude around M6 can occur. Largest known earthquakes /about-imo/news/earthquakes-around-blafjoll-ski-are

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