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Overview of landslide hazard and possible
mitigation measures in the settlement
southeast of Fjarðará River in Seyðisfjörður
Daniel Illmer
Jón Kristinn Helgason
Tómas Jóhannesson
Eiríkur Gíslason
Sigurjón Hauksson
VÍ 2016-006
Report
Cover photo: Jón Kristinn Helgason, 11 September 2015
Overview of landslide hazard and possible
mitigation measures in the settlement
southeast of Fjarðará River
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
in Holuhraun 31 August 2014. This photo is taken 31 January 2015 of the lava field, by then closely approaching 85 square kilometers. A month later, 28 February 2015, the eruption is declared over.
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/about-imo/news/bigimg/3097
at the Reykjanes peninsula during the period from January 2000 until June 2015. Blue lines represent known faults which have been active in Holocene or Recent Epoch, i.e. after the ice age (Páll Einarsson, 2015). Also shown in yellow are volcanic systems with fissure swarms (Páll Einarsson and Kristján Sæmundsson, 1987). Enlarge
/about-imo/news/bigimg/3150
A GPS station was mounted there on 10th July 2015 in order to monitor displacements at Bárðarbunga in the aftermath of the Holuhraun eruption. Further adjustments and maintainance took place in November 2015 (see photos).
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/about-imo/news/bigimg/3345
; fax: +358 20 490 2590.
E-mail address: Noora.Veijalainen@ymparisto.fi (N. Veijalainen).
Journal of Hydrology 391 (2010) 333–350
Contents lists available at ScienceDirect
Journal of Hydrology
journal homepage: www.elsevier .com/ locate / jhydrol
Author's personal copy
narios from GCMs or RCMs, and with different emission scenarios
(e.g. Menzel et al., 2006; Minville et al., 2008; Prudhomme and Da
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
Seismic activity in Iceland 2015 – 2016
and testing of near-real time automatic relative locations
Gunnar B. Guðmundsson¹ and the Natural Hazards monitoring team
¹Icelandic Meteorological Office, Bústaðavegi 7-9, 108 Reykjavík, Iceland, gg@vedur.is
At present, in September 2016 the SIL seismic monitoring network consists of around 70 seismic
stations. The number of earthquakes located
/media/norsem/norsem_gunnar.pdf