: 115 km towards SW and 55 km towards NNE from Bárðarbunga
Trend: Veidivötn fissure swarm NE-SW, Dyngjuháls fissure swarm NNE-SSW
Ice cover: Partial
Type of activity: Lava effusion, explosive phreatomagmatic
Magma type: Basalt
Eruption characteristics:
Type of products: Airborne tephra, lava flows, water transported tephra
VEI Max: VEI 5-6; most freq: VEI 1-2
Bulk volume
/media/jar/Bardarbunga_kafli20140825.pdf
but several small slides were released from rim of the slope. Fixed points were installed on
boulders after 2001 to detect future surface movements and these points have been remeasured
regularly with a GPS with a 1–2 year interval (Esther H. Jensen, 2002) (see Maps 6 and 7). The
movements were particularly rapid for a couple of years after 2001 but have been slower during
the last decade. Total/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
J600v berg 2.utg) were also used in this study.
Table 1. Main characteristics of river basins used in this study.
River Name Type Area Mean Percentage Mean annual Period
/ (km2) elevation glacier precipitation for
Gauging (m a.s.l) (mm) streamflow
station (1961-2014) data
vhm59 Ytri-Rangá L 622 365 0 1564 1961–2014
vhm64 Ölfusá L+D+J+S 5687 480 12.2 2003 1950–2014
vhm66 Hvítá (Borgarfirði) L+J 1577
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
The
investment amount for new roads is about the same as the maintenance budget4. The relative
significance of the maintenance budget will rise as investment in new roads will stagnate of
decrease. The total value of the Finnish road system is in the order of magnitude of 36 billion euro
(approx. current replacement value; Uimonen 2008).
Last but not least adverse weather causes reduction
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
Fault plane solutions of the earthquakes in Nordland, Norway
Ilma Janutyte(1), Jan Michalek(2), Conrad Lindholm(1), and Lars Ottemoller(2)
(1) NORSAR, Kjeller, Norway, (2) University of Bergen, Bergen, Norway
This study is a part of the ongoing NEONOR2 project which is carried out in Nordland, norther
Norway. This work aims to define the fault plane solutions (FPS) of the earthquakes
/media/norsem/norsem_janutyte.pdf