West Iceland, is a direct run off river. Fig. 4 shows the effect of low precipitation on such rivers. During a dry spell in late summer, water discharge was very low. In preceding years, it was also rather low except during the summer of 2005 (red line). The black line (2010) shows that hardly any rain fell on the drainage area last summer.
Location
A map which shows the location of various rivers
/hydrology/articles/nr/2110
A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from the gully to the west of the hillside and into supporting structures that have been installed as protection measures to reduce avalanche danger in the settlement near
/about-imo/news/nr/2476
A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from the gully to the west of the hillside and into supporting structures that have been installed as protection measures to reduce avalanche danger in the settlement
/avalanches/articles/nr/2475
September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge.
The first two weeks as an example
Total subsidence from 12 Sept 2014 until 1 March 2015
The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment
/earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera
of a town in north Iceland in 2012
27.4.2012
A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from the gully
/about-imo/news/nr/2476/
in north Iceland in 2012
Tómas Jóhannesson
25.4.2012
A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from
/avalanches/articles/nr/2475/