70 results were found for 제주제원레깅스〈Օ1Օ＝751ვ＝Օ3Օ4〉 제주레깅스룸 제주도레깅스룸з제주시레깅스룸㏶제주공항레깅스룸 ENd/.

Results:

• 1. News

  of IMO, Magnus Jonsson, is at the right end of the row. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 2012 2011 2010 2009 2008 2007 2006 /about-imo/news/bigimg/1302

• 2. Grimsvotn_status_2011-05-30_IES_IMO

  Since Thursday the tremor had been intermittent. Today, Monday 30 May, it has been confirmed by the participants of Iceland Glaciological Society's spring expedition that the eruption has ended. The end of the Grímsvötn eruption is set to 7 UTC Saturday morning 28 May 2011. /media/jar/Grimsvotn_status_2011-05-30_IES_IMO.pdf

• 3. Update on Fagradalsfjall

  a deep reservoir which was feeding the eruption.However, since the end of September, inflation has been detected on Reykjanes Peninsula (following the end of eruptive activity). The signal has been identified on both GNSS and InSAR observations and broadly correlates to the area that was deflating throughout the eruption. The most likely cause of the current inflation is renewed magma inflow /about-imo/news/update-on-fagradalsfjall

• 4. News

  News © Richard Yeo In the aftermath. A field trip after the end of the eruption had been declared. IMO‘s staff /about-imo/news/bigimg/3124

• 5. Sea ice in January 2009

  attention to the proceedings on satellite images and put information in that regard three times on the web. Easterly and northeasterly winds were dominant in the Greenland Strait. No dispatches were received from ships and the Coast Guard did not go on an exploration flight. By the end of the month sea ice maps from the Norwegian Met Office were made accessible on the IMO's web site (originally hafis /sea-ice/monthly/2009/nr/2323

• 6. Sea ice in January 2011

  in the following locations: 80 nm WNW of Bjargtangar, 46 nm NW of Barði, 40 nm NW of Straumnes and 41 nm N of Kögur. No icebergs were to be seen near the ice edge. On the Greenland Strait, northeasterly wind directions were dominant to begin with, and most of the month, but at the end of the month there were a few days with southwesterly wind /sea-ice/monthly/2011/nr/2348

• 7. Trausti_Jonsson_(IMO,_Ice)

  of large natural events in the 1960s and early 1970s showed that this line of thought was at the best wrong, but possibly also dangerous. Since then the need for natural hazard management in the broad sense has become more and more obvious in Iceland. The assessment of Icelandic natural hazards fit very well into the frame proposed by the WMO at the end of the International Decade for Natural /media/loftslag/Trausti_Jonsson_(IMO,_Ice).pdf

• 8. norsem_gunnar

  by the SIL system in 2015 was about 24000 and about 17000 in 2016, end of September. Following the seismicity from south to north, the northern most part of the Reykjanes ridge had large seismic swarms in June and July 2015. The largest earthquake in the swarms occurred on 1 July and had a magnitude Mlw5.0. Reykjanes peninsula had occasionally some small swarms, mainly at the tip of the peninsula /media/norsem/norsem_gunnar.pdf

• 9. The eruption has come to an end

  The eruption has come to an end The volcanic eruption in Holuhraun lasted six months 15.3.2015 The volcanic eruption in Holuhraun has come to an END, see a declaration from the Scientific Advisory Board, 28 February 2015. For the first time in six months /about-imo/news/nr/3097

• 10. Earthquake sequence offshore North Iceland

  Earthquake sequence offshore North Iceland 22.10.2012 An earthquake sequence at the southern end of the Eyjafjarðaráll graben has been ongoing since Saturday 20 October. The source region of the events is approximately 20 km north-northeast of Siglufjörður /about-imo/news/nr/2555