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• 61. Nordic Seismology Seminar in Iceland

  field trip will be made to the Reykjanes peninsula to see the faults of the Reykjanes oblique rift and some pillow lavas near the ocean. Also lake Kleifarvatn, Seltún geothermal field and Gunnuhver, a hot-spring famous for its steam. News 2023 2022 2021 /about-imo/news/nordic-seismology-seminar-in-iceland

• 62. The earthquake swarm on Reykjanes ridge

  for Eldey volcano from "green" to "yellow". IMO is monitoring the activity closely. Seafarers and people by the sea shore are asked to please contact IMO in case of any unusual observations in the water, such as an increase of water temperature, change of surface color, steam or dead fish. All information may be valuable. The earthquake swarm on the Reykjanes ridge, preliminary results, (see /about-imo/news/nr/3163

• 63. The eruption continues with little changes

  causing some water discharge into river Hvanná, steam plumes and low frequency tremor bursts. Water level (cm) of Hvanná Two outburst of water discharge into river Hvanná on Easter Sunday, caused by lava melting ice. At the Institute of Earth Sciences, University of Iceland, a preliminary report has been written on gas composition and flux from the Fimmvörðuháls eruption /about-imo/news/nr/1860

• 64. Magma splatters ejected

  of this phenomenon at IMO yet. Magma splatters have have accumulated on the crater's rim. Splatters of magma have also fallen on the ice around the crater and this gives rise to steam plumes. In spite of the ejected batches of liquid magma, no lava flow from the craters was detected. South of the eruptive site, the ash clouds reached 5-6 km hight. Eyjafjallajökull ash cloud - two days ago /about-imo/news/nr/1883

• 65. The eruption continues with little changes

  On April 4th, lava flowing to the west encountered some patches of glacial ice, causing some water discharge into river Hvanná, steam plumes and low frequency tremor bursts. Water level (cm) of Hvanná Two outburst of water discharge into river Hvanná on Easter Sunday, caused by lava melting ice. At the Institute of Earth Sciences, University of Iceland, a preliminary report has been written /about-imo/news/nr/1860/

• 66. Articles

  Articles © Einar Kjartansson A plume of steam rises where the lava front melts snow and ice. The eruption crater /earthquakes-and-volcanism/articles/bigimg/1852

• 67. Eyjafjallajokull_status_2010-06-01_IES_IMO

  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. We continue to monitor the volcano closely. /media/jar/Eyjafjallajokull_status_2010-06-01_IES_IMO.pdf

• 68. Grimsvotn_status_2011-05-26_IES_IMO

  monitoring; IMO hydrological data; weather radar; ash-fall reports; scientific overflights; UK Met Office ATDnet; MODIS and NOAA satellite images. Eruption plume: Height (a.s.l.): Plume not detected on radar at 70 km distance from the eruption site.. Minor steam explosion observed in the crater. Heading: -- Colour: -- Tephra fallout: Only in the vicinity of the eruption site. Lightning: No lightning /media/jar/Grimsvotn_status_2011-05-26_IES_IMO.pdf

• 69. Articles

  o'clock. Steam is caused by lava melting snow. Aerial photo of Fimmvörðuháls on Eyjafjallajökull. Aerial photo of Fimmvörðuháls /earthquakes-and-volcanism/articles/bigimg/1851