46 results were found for JZMOR mette fine alla frode nel mondo delle criptovalute.

Results:

• 1. VI_2016_006_rs

  a debris cone in the run-out zone. The source of the material is either within in the channel or in the talus slope above the channel. Most of the landslides that occur in Strandartindur are debris flows of this type. B Debris slides that are not confined to gullies and occur near a concave break of slope. The main type of material is debris mixed with fine-grained material. Most of the landslides /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 2. Festive forecast

  News Festive forecast Fine weather forecast /about-imo/news/nr/3053

• 3. Supercomputer in Iceland

  Hafdís Þóra Karlsdóttir, the Danish Ambassador Mette Kjuel Nielsen, the Minister for the Environment Sigrún Magnúsdóttir and Dir. General of DMI, Marianne Thyrring. Photographer: Bjarne Keinicke. Facts The partnership Partnership centered around making use of each other‘s competences The supercomputer is acquired by DMI and is installed at IMO Operations obligations are diveded among parties, so /about-imo/news/nr/3309

• 4. VI_2021_008

  of minutes. Depending on the specific window lengths, the appropriate triggering signal-to-noise ratio falls somewhere between 1.1 and 1.4. Logarithmic scaling on the vertical axis enhances weak tremor signals, making them easier to identify at an early time. When logarithmic scaling was applied to the STA and LTA averages, however, it became clear that this would require very fine tuning, as many /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 5. The August glacial outburst - one of the larger jökulhlaups to have affected Skaftá in recent decades

  station, showing collapse of the ice-surface.Infilling of lava fields by fine sediment, resulting in stream contamination and sandstormsDuring the height of the flood, fine-grained sediment was deposited on young, porous lava fields adjacent to the river, both in the highlands and the lowlands. Such sedimentation progressively fills the lava, allowing subsequent jökulhlaups to expand further /about-imo/news/the-august-glacial-outburst-one-of-the-larger-jokulhlaups-to-have-affected-skafta-in-recent-decades

• 6. EUMETNET meeting in Reykjavík

  modelling and satellite information. In Reykjavik, the status and funding of various projects will be discussed. Future guidelines and organization of the weather community in Europe will, however, be the main topic of discussion. In fact, EUMETNET is often seen as a fine example of international co-operation. Members intend to develop their collective capability to serve environmental /about-imo/news/nr/1302

• 7. QA on the eruption in Eyjafjallajökull 2010

  or no volcanic activity has been observed since 23rd May but scientists have not yet declared that the eruption is over. What kind of an eruption is it? The eruption is an explosive eruption beneath a glacier. The ash is fluorine rich, of intermediate silica content and the particles are very fine. Is the ash dangerous? Yes, the fluorine is dangerous to livestock. The fine ash can also effect human /earthquakes-and-volcanism/articles/nr/1880

• 8. Eyjafjallajokull_status_2010-05-17_IES_IMO-1

  is drifting east. Colour: Dark-gray at 6 km (seen on webcam). Tephra fallout: Ash has fallen in the Gnúpverjahreppur area, on the road to Stultartangi Power Station and in the Biskupstungur area (very fine- particled and gray). Lightning: Constant lightning (up to 10 flashes per hour) has been detected. Noises: In Hafnarfjörður. Meltwater: Low water discharge at Gígjökull. Conditions /media/jar/Eyjafjallajokull_status_2010-05-17_IES_IMO-1.pdf

• 9. Eyjafjallajokull_status_2010-05-26_IES_IMO

  in the last couple of days. Overall assessment: There is still a considerable amount of steam coming from the crater. The tremor is still higher than before the onset of the eruption, and small tremor pulses have been detected on the lowest frequency. Very fine ash has been blown up, but it does not go very high up in the air, but covers the volcano so it can not be seen on webcameras.. /media/jar/Eyjafjallajokull_status_2010-05-26_IES_IMO.pdf

• 10. Eyjafjallajokull_status_2010-05-28_IES_IMO

  and or degassing from the craters. Visibility to the bottom limited due to steam. The crater rim is coated with fine ash that extends me 20 m from the edge. Strong smell of sulfur around the craters. At 20:45 the steam plume was measured to be at the altitude of 2.8 km. Seismic tremor: Volcanic tremor is still more than before the eruption and has been rather steady since 22nd May, but small pulses /media/jar/Eyjafjallajokull_status_2010-05-28_IES_IMO.pdf