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International Symposium on Mitigative Measures against Snow ...

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<str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> <str<strong>on</strong>g>Symposium</str<strong>on</strong>g> <strong>on</strong> <strong>Mitigative</strong> <strong>Measures</strong> <strong>against</strong> <strong>Snow</strong> Avalanches<br />

Egilsstaðir, Iceland, March 11–14, 2008<br />

two 100 m l<strong>on</strong>g and 10 m high earth filled deflecting dams which form a wedge shaped<br />

structure directly above the facility (figure 2). The fr<strong>on</strong>t of the wedge (the “bow”) is steep<br />

over a 50 m l<strong>on</strong>g secti<strong>on</strong> but the rest of the dams is built with rock fill and a c<strong>on</strong>venti<strong>on</strong>al<br />

slope of the fill material used. C<strong>on</strong>structi<strong>on</strong> of the steep part of the dams was completed in<br />

1998 and the complete structure in 2002.<br />

Figure 2 Deflecting dams in Engidalur, Ísafjörður. The dams form a wedge shaped<br />

structure (photos: Hallgrímur D. Indriðas<strong>on</strong>).<br />

The dams have repeatedly been hit by avalanches from Kirkjubólshlíð. The first <strong>on</strong>e fell in<br />

February 1999 prior to the full completi<strong>on</strong> of the dams, followed by avalanches in: April<br />

2001, January 2004, January 2005 and March 2007. The dams have <strong>on</strong> all occasi<strong>on</strong>s<br />

prevented accidents to employees and damages to the facility (IMO, 2003; Arnalds and<br />

others, 2007; IMO, 2005).<br />

4.3 Neskaupstaður<br />

4.3.1 Drangagil area<br />

The town of Neskaupstaður is located in the east fjords of Iceland. A large part of the<br />

residential area is threatened by avalanches from several well defined avalanche paths.<br />

Preparati<strong>on</strong> for the c<strong>on</strong>structi<strong>on</strong> of avalanche defences in the Drangagil area was initiated in<br />

1997. Defence structures in the Drangagil area are of three types: 1) Supporting structures, 2)<br />

braking mounds and 3) a catching dam. The supporting structures are located in the starting<br />

z<strong>on</strong>e of Drangagil and include approximately 1000 m of 3.5−4.0 m high avalanche nets. The<br />

braking mounds are positi<strong>on</strong>ed in two rows above the residential area, a total of 13 mounds<br />

(Tómass<strong>on</strong> and others, 1998a). The mounds have a steep fr<strong>on</strong>t facing the mountain, are 10 m<br />

high and each mound is approximately 10−12 m wide at the top. The 400 m l<strong>on</strong>g catching<br />

dam is located at a distance of 100 m from the residential area. The dam is 17 m high with a<br />

steep fr<strong>on</strong>t facing the mountain (see figure 3). The total volume of earth fill comprising the<br />

catching dam and the braking mounds is approximately 260,000 m 3 . The steep dam fr<strong>on</strong>ts<br />

facing the mountain are built with earth reinforcement system made of steel. The avalanche<br />

defences were inducted in 2002.<br />

4.4 Tröllagil area<br />

The most extensive appraisal study yet, carried out by VST, is a proposal for the Tröllagilarea<br />

in Neskaupstaður, which was completed in 2003 (Sigurðss<strong>on</strong> and others, 2003). Following<br />

c<strong>on</strong>structi<strong>on</strong> of avalanche defences in the Drangagil area in Neskaupstaður, defence<br />

opti<strong>on</strong>s in the Tröllagil area (western most part of the residential area) were c<strong>on</strong>sidered. Emp-<br />

Indriðas<strong>on</strong>, Sigurðss<strong>on</strong>, Tómass<strong>on</strong> and Hák<strong>on</strong>ardóttir 127

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