70 results were found for Protect Your Funds: JZMOR’s Tools Against Crypto Scam.

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• 61. Fagradalsfjall eruption

  Real time dataOnly part of the data used by the IMO to monitor the Reykjanes Peninsula is shown here. Please note that information that the IMO publishes on web pages in real time has not been reviewed. Interpretation and processing of such data is done at your own risk. Here you can view the latest earthquakes.Seismic activity GPS Yfirlit yfir GPS kerfið má /volcanoes/fagradalsfjall-eruption/real-time-data/

• 62. Instructions for aurora forecast

  on a day or time. The upper-right box shows the forecast of auroral activity at midnight on the scale 0 to 9. The scale changes in accordance with the date selected under the cloud cover map. Aurora forecast shows expected activity at your selected date. Even grade 2 (low activity) can be beautiful and grade 3 (moderate) can be dazzling. The timing of sunset, darkness, sunrise and moonrise /weather/articles/nr/2588

• 63. 47th Nordic Seismology Seminar

  on the respective day. Poster presentations (during all three coffee breaks) Tuesday 11 October Arrival and check-in. Most flights will arrive in the afternoon, so you should be at your hotel around 17:00/18:00.19:00 Kickoff party at IMO (Bústaðavegur 7, 108 Reykjavík). We will meet you at 18:30 outside Grand Hotel and walk together to IMO. Should anybody prefer to get a lift by car, please /norsem/norsem2016/program/

• 64. Instructions on using meteograms

  to the corresponding forecast map and observation data are beneath each meteogram. Clicking reset, located at the lower right of each graph, removes it from the page. Pressing the reset all meteograms function near the top of the page removes all meteograms from the page. Note that the displayed graphs can be printed using the options available from your Internet browser. Go to the meteogram page /weather/articles/nr/1217

• 65. Registration

  In the registration mail please send your name and e-mail, name of the institution where you work or study, and dates of arrival and departure. Participation, including 2 lunches and a dinner, is free of charge. Participants, other than speakers, have to cover travel and hotel costs themselves. Approaching Reykjavík Recreation park Heiðmörk and Reykjavík in background. Photo: Guðrún Pálsdóttir /nonam/workshop/registration/

• 66. 47th Nordic Seismology Seminar

  buy a "Flybus Plus" ticket, further transportation from BSÍ terminal in central Reykjavík to the hotel is included. Get a return ticket for smooth transportation back to the airport, the same way you came. You do not need to book your ticket in advance. The Flybus operates for all arriving flights, and even in case of flight delays it will wait for the passengers.To get around in ReykjavíkCity /norsem/norsem2016/transportation/

• 67. VI_2009_012

  Distance corrected PGV. ......................... 14  Figure 3. Corrected magnitudes, Mw(v) plotted against log distance.. .................................. 17  Figure 4. Magnitude estimates as a function of Ci. ................................................................ 18  Figure 5. Observed/predicted PGV residuals for each station. .............................................. 20  Figure 6 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 68. Fractures in Svínafellsheiði and a potential rockslide on Svínafellsjökull

  ). Fractures in Svínafellsheiði and a potential rockslide on Svínafellsjökull Civil Protection advises against travel on Svínafellsjökull 22.6.2018 In the autumn of 2014, a surface fracture was discovered /about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull

• 69. Supporting structures stopped most of an avalanche

  the mountainside (see fig. 1). An avalanche slab was released inbetween the rows of supporting structures. The snow was mostly stopped by the structures and piled up against them (see fig. 2) but part of the snow jumped over the rows. A slab was also released below the lowermost row. The avalanche stopped near the foot of the slope to the west of the structures but before it reached the bottom of the slope /about-imo/news/nr/2476

• 70. Supporting structures stopped most of an avalanche

  near the mountainside (see fig. 1). An avalanche slab was released inbetween the rows of supporting structures. The snow was mostly stopped by the structures and piled up against them (see fig. 2) but part of the snow jumped over the rows. A slab was also released below the lowermost row. The avalanche stopped near the foot of the slope to the west of the structures but before it reached the bottom /avalanches/articles/nr/2475