type, surface condition and weather
was noted. In total more than 100 point measure-ments were made during three days (2 and 3 August2006 and 7 August 2007). Measurements weremade on different surface types: ice, snow and firn,
as well as on different surface conditions (dry, wet,clean, dirty). Some of the measurements will be re-ferred to in this paper.
Meteorological observations outside
/media/ces/GA_2009_91A_4_Andreassen.pdf
behavior towards
a public good based on individual preferences, and provides insights into the type of indi-
viduals who best serve the social interest and those to avoid in institutional settings. This
distinction helps us to understand why, with the same incentives, the provision of public
goods works better in some populations than in others. In addition, our use of a sequential
public good
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
Dashed lines encompass the V-shaped zone of tephra deposition. (c)
Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall
from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November.
The top portion shows its projection on an EW-vertical plane. The minimum detection height for
Grímsvötn is seen at 6 km, and the plume extends
/media/jar/myndsafn/2005EO260001.pdf
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111
/about-imo/the-web/iframes/wind-temp-precip/
be copied to your html file where the frame should appear:
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To show other areas, a different digit must be entered after 'Vi.ifrm.area
/about-imo/the-web/iframes/wst-txt-obs/
during the 12 hours preceding the earthquake, so its fault plane
could not have been envisaged with this method.
Figure 2. (Left) Map view of the foreshock distribution on the Ingólfsfjall (eastern) fault
of the 29 May 2008 Mw6.3 earthquake; a total of 25 foreshocks occurring until 15
minutes before the large event. (Right) Vertical cross-section viewed from the north,
showing the event
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
northwest of Geysir geothermal field, continues. Around 50 earthquakes have been detected in that area since 9am yesterday. The largest was M2.5 at 01:11 this morning. They originate at a depth of 2 - 3 km.
23 December 2014 10:00 - from geoscientist on duty
The largest earthquakes since 9am yesterday were M4.3 at 11:15 and 17:42 (22 Dec.). Five more were over 4 in magnitude. In total, a little less
/earthquakes-and-volcanism/articles/nr/3055
northwest of Geysir geothermal field, continues. Around 50 earthquakes have been detected in that area since 9am yesterday. The largest was M2.5 at 01:11 this morning. They originate at a depth of 2 - 3 km.
23 December 2014 10:00 - from geoscientist on duty
The largest earthquakes since 9am yesterday were M4.3 at 11:15 and 17:42 (22 Dec.). Five more were over 4 in magnitude. In total, a little less
/earthquakes-and-volcanism/articles/nr/3055/
quakes were between magnitude 3 and 4. In total,
35 quakes have been observed during the past 24 hours. In the dyke intrusion, 10 quakes were
observed, all below magnitude 2. In Tungnafellsjökull area ten quakes were observed, all also
below magnitude 2. Clear view has been of the eruption site through web cameras this
morning and yesterday.
The earthquakes in the Geysir area seem to be fading
/media/jar/Bardarbunga-2014_December-events.pdf