81 results were found for gpt header corruption has(🏅xnseo.cc🏅)gpt header corruption has.SVD.

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• 51. Gauging stations

  Gauging stations 6.1.2010 The operation of a network of gauging stations provides the basic information for knowledge of the hydrology of Iceland. As the importance of monitoring and mediating information has been growing, the network has been updated /hydrology/stations/

• 52. Eyjafjallajökull eruption

  Eyjafjallajökull eruption Heard and not seen 20.4.2010 As said earlier, the eruption in Eyjafjallajökull has apparently entered a new phase with less interaction of magma with ice and melt water. It seems that the ice cauldrons over /about-imo/news/nr/1887

• 53. Eyjafjallajokull_status_2010-05-24_IES_IMO

  : Similar as yesterday, estimated through a webcamera. Seismic tremor: Volcanic tremor is still decreasing and is approaching the level it had before the eruption. Earthquakes: Earthquake activity has decreased since yesterday. One earthquake has been recorded since midnight. GPS deformation:Horizontal displacements toward the centre of Eyjafjallajökull volcano and subsidence. Overall assessment /media/jar/Eyjafjallajokull_status_2010-05-24_IES_IMO.pdf

• 54. Gyrite_Brandt_(Local_Government_Denmark,_DK)

  and this was done by stakeholder involvement with different levels of involvement. The climate adaptation plan has been presented to the general public and has been used as a basis for integrating climate adaptation measures in the Municipal plan. Lolland is now an pilot study area for two Interreg projects SUSCOD and BLAST, both dealing with the coastal zone and climate adaptation. /media/loftslag/Gyrite_Brandt_(Local_Government_Denmark,_DK).pdf

• 55. Katla and Mýrdalsjökull

  Activity, interpretation and monitoring 31.8.2016 Since mid-June, heightened earthquake activity has been registered in the Katla caldera. Summertime increases in caldera seismicity are an almost annual occurrence at Katla, often associated with the drainage /about-imo/news/katla-and-myrdalsjokull

• 56. Monitoring Öræfajökull – update 22. Dec. 2017

  – update 22. Dec. 2017 22.12.2017 Real-time surveillance around Öræfajökull has been improved in the last month to better monitor the seismicity (significantly increased since September this year) and the release of geothermal water from the caldera (detected /about-imo/news/monitoring-oraefajokull-update-22-dec-2017

• 57. Seismic activity around Mt. Þorbjörn has decreasing

  Along with reduced deformation, seismic activity has decreasing significantly. The picture shows an overview of the earthquake activity in April. Seismic activity around Mt. Þorbjörn has decreasing significantly The area is now most likely recovering after the large induced stress /about-imo/news/seismic-activity-around-mt-thorbjorn-has-decreasing-significantly

• 58. Eyjafjallajökull

  volcanic system is located on the Eastern Volcanic zone, approximately 25 km west of Katla volcano. Eyjafjallajökull volcano is a 1666 m high stratovolcano with an east-west elongated direction, the system is about 25 km long and 15 km wide. The volcano is mostly covered by ice and has an ice-filled caldera of about 2.5 km wide.In the last 8000 years Eyjafjallajökul has been moderately active /volcanoes/about-volcanoes/eyjafjallajokull/

• 59. Hekla

  on the Eastern Volcanic zone and consists of a central volcano rising to 1490 m.a.s.l. and is about 60 km long fissure swarm. The volcano has been highly active during Holocene and has erupted 23 times in historical time, with its last eruption occurring in 2000. It is considered the third most active volcano in Iceland. About 100 eruptions are known from the system in the past 9000 years, both effusive /volcanoes/about-volcanoes/hekla/

• 60. Further information on the seismicity in Northern Iceland

  Further information on the seismicity in Northern Iceland 26.10.2012 Seismic activity at Eyjafjarðaráll is continuing although it has slightly decreased since yestarday evening. On 25 October, the largest events in the source region of Sunday's M 5.6 earthquake /about-imo/news/nr/2561