64 results were found for kone娱乐香港报130【┃咨询Ｑ２17431】】.

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• 41. VI_2009_013

  the last two decades, in 1994, 1996 and 1999. The 1994 swarm began on 11 May and lasted until 27 June. Between 120 and 130 earthquakes were located during that period, mostly beneath the northern flank of the volcano. Dahm and Brandsdóttir (1997) analyzed 15 selected earthquakes from the 1994 swarm which were also recorded on a temporary network. Lacking a velocity model for Eyjafjallajökull /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 42. Bárðarbunga 2015 - January events

  in Westman islands archipelago south of Iceland (Heimaey, Vestmannaeyjar) lasted for 130 days, from 23 February 1973 until 3 July same year. 31 January 2015 12:00 - from geoscientist on duty No significant changes have taken place during the last 26 hours. Around six o‘clock this morning visibility improved and since then the glow from Holuhraun can be seen on webcams and there do not seem to be any /earthquakes-and-volcanism/articles/nr/3071

• 43. Bárðarbunga 2015 - January events

  in Westman islands archipelago south of Iceland (Heimaey, Vestmannaeyjar) lasted for 130 days, from 23 February 1973 until 3 July same year. 31 January 2015 12:00 - from geoscientist on duty No significant changes have taken place during the last 26 hours. Around six o‘clock this morning visibility improved and since then the glow from Holuhraun can be seen on webcams and there do not seem to be any /earthquakes-and-volcanism/articles/nr/3071/

• 44. Bardarbunga-2015_January-events

  and has therefore lasted for 167 days. For comparison, the volcanic eruption in Westman islands archipelago south of Iceland (Heimaey, Vestmannaeyjar) lasted for 130 days, from 23 February 1973 until 3 July same year. 31 January 2015 12:00 - from geoscientist on duty No significant changes have taken place during the last 26 hours. Around six o‘clock this morning visibility improved and since /media/jar/Bardarbunga-2015_January-events.pdf

• 45. VI_2022_006_extreme

  Three watersheds are clustered together on the north- eastern flank of Vatnajökull: Hálslón, Ufsarlón, and Hraunaveita, while Blönduvirkjun extends between Langjökull and Hofsjökull. The hydropower catchments vary in size, ranging from about 130 km2 (Hraunaveita) to almost 1,800 km2 (Hálslón), and two of them have a mean elevation above 1,000 meters (Hágöngulón and Hálslón). Only Búðarháls has /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 46. VI_arsskyrsla2020

  til 2000. Mest snjódýpt á árinu mældist 130 cm við Skeiðsfossvirkjun þ. 23., 24. og 25. desember. Sólskinsstundir, loftþrýstingur og vindhraði Árið var óvenjusólríkt á suðvesturhluta landsins á árinu. Sólskinsstundir í Reykjavík mældust 1582,2 sem er 314 fleiri en í meðalári 1961 til 1990. Árið var það þriðja sólrík- asta frá upphafi sólskinsstundamælinga í Reykjavík. Á Akureyri mældust /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 47. Bárðarbunga 2014 - November events

  the last measurement (4 Nov.) corresponds to a magmaflow of 130 m³/s. This is less than the first month, when the estimated flow was close to 200 m³/s. Institute of Earth Sciences, 27 November 2014. 29 November 2014 12:30 - from geoscientist on duty Since 10:00 AM yesterday, 28 November, around 40 earthquakes have been detected within Bárðarbunga. Most of the recorded seismicity occurred /earthquakes-and-volcanism/articles/nr/3023

• 48. Bardarbunga-2014_November-events

  of the caldera has decreased slowly but the subsided area has also broadened. The change in volume since the last measurement (4 Nov.) corresponds to a magmaflow of 130 m³/s. This is less than the first month, when the estimated flow was close to 200 m³/s. Institute of Earth Sciences, 27 November 2014. 29 November 2014 12:30 - from geoscientist on duty Since 10:00 AM yesterday, 28 November, around 40 /media/jar/Bardarbunga-2014_November-events.pdf

• 49. Bárðarbunga 2014 - November events

  the last measurement (4 Nov.) corresponds to a magmaflow of 130 m³/s. This is less than the first month, when the estimated flow was close to 200 m³/s. Institute of Earth Sciences, 27 November 2014. 29 November 2014 12:30 - from geoscientist on duty Since 10:00 AM yesterday, 28 November, around 40 earthquakes have been detected within Bárðarbunga. Most of the recorded seismicity occurred /earthquakes-and-volcanism/articles/nr/3023/

• 50. 2010_012rs

  characterized by parallel, N-S oriented, vertical strike- slip faults. In the last 19 years of SIL network operation, over 130 thousand microearthquakes have been recorded in southwest Iceland, and in the last nine years, three M>6 and six M>5 events have occurred in the SISZ and Reykjanes peninsula (stars in Figure 1). Figure 1. A map of south-west Iceland showing Reykjanes Peninsula /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf