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Key Words: Avalanche, avalanche accident, evacuation, res-

cue

ABSTRACT

This presentation will be case histories of two avalanche
disasters in Iceland in the year 1995, resulting in the death
of 34 people. Each avalanche hit a small fishing village,
destroying many houses in the middle of the night. On
January 16th the village of Sudavik was partly destroyed
by an avalanche, killing 14 people, and on October 26th
the village of Flateyri was hit, killing 20 people. Those
villages are both on the North-West peninsula of Iceland,
named Vestfirdir, whose history has during the centuries
proved to be very prone to avalanches. Both avalanches
happenedduring severe northerly snowstorms, thatcaused
widespread avalanche activity and damages. Both ava-
lanches went much further than the hazard zone line had
indicated, which is also true for 5 other avalanches in the
area in the last two years. The size of the accidents and
the bad weather had a big effect on the rescue operations,
and the rescue efforts were a test for the whole Icelandic
rescuesystem. Those two disasters affected the avalanche
warningandprotection system in Iceland, which hassince
been reorganized and strengthened. In the future one of
the villages will be protected by defense structures and
the other will be moved to a safer place.
INTRODUCTION

Iceland is an island in the middle of the North-Atlantic,
around 103,000 km 2 in size, with a little over 260,000 in-
habitants. Most of the settlements are along the coast, on a
narrow strip between the seaand themountains (600-1000
meter high a.s.l. in coastal areas), or in deep valleys
extending from the fjords. A landscape made by the gla-
ciers during the last ice-age are in many cases ideal run-
ways for avalanches. Until the 19th century most of the
Icelanders lived on small farms, spread all over the coun-
try, but then small fishing villages were established along
the coast. Most often this was on reefs extending into the
fjords, where it was easy to safely land the small fishing
boats. In the beginning of the 20th century new technol-
ogy led to greatdevelopment in thefishing industry, which
causedthose villages to grow rapidly. This meant that they
extended from the reef up the mountainsides above it and
along the narrow coast, often into areas which were not
safe from avalanches.
The climate in Iceland is a maritime one, variable, with
relatively mild weather, but very changeable. The weather
is mostly controlled by pressure lows and fronts, passing
NW along the North-Atlantic, resulting in (often sudden)
changes in the weather.
From the moment the first settler set his foot on Ice-
land, in the year 874, avalanches have been a threat. The
oldest description of an avalanche accident comes from
Sturlungu, one of the old Sagas:
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"Snorri hada good stock of sheep and livedin Svinadalur,
where now is called Snorrastadir. He dr owned in
Saelingsdalsa, where now is called Snorravad. Then went
Sighvatur Ulfsson, his brother-in-law, to look for him and
four men with him and they were hit by an avalanche and
all killed."
This was in the year 1118.
From that year, chronicles tells of around 680 fatalities
as a result of avalanches, and one can assume that many
accidents are missing, specially before the year 1600. Of
those 680 fatalities, 164 happened during thiscentury, 107
of them in houses and villages, but 57 on roads and in the
backcountry. No other natural hazard has claimed more
human lives, exceptbad weather sinking boats anddrown-
ing fishermen. All the earlier accidents were relatively
small, since the people lived on small individual farms.
After the villages started to form, bigger avalanche acci-
dents followed. 24 people died in Seydisfjordur in the
year 1885, 20 people in Hnifsdalur in 1910, 12 people in
Neskaupstadur in 1974, 14 people in Sudavik in 1995 and
20 people in Flateyri in 1995.
THE TWO AVALANCHES

On the morning of January 14th 1995 a pressurelow could
be seen on weather charts, far SWof Iceland. At that time
its influence on the weather in Icelandwasnot certain, but
as it came closer the computer forecasts indicated that it
would lead to a full force winter storm. On Sunday the
13th the windspeedstarted to increase, with snowfall and
heavy drifting snow. That day a general avalanchewarn-
ing was issued and people started to evacuate the houses
that were within avalanchehazard zones in the villages in
northern and western parts of Iceland.
At 6:25 in the morning of January 16th a big avalanche
started high in the mountain above the small village of
Sudavik (230 inhabitants) in the NW part of Iceland (Fig-
ure 1). The avalanche is believed to have started at the
mountain edge (elevationof 580 m.a.s.l.), possibly as a col-
lapse of a cornice, but gained size as it ran further down
the mountain slope. This is only assumed, since the four
day storm that followed theavalancheeliminatedall marks
of the start of it. The starting zone is expected to have
been about 200 meters wide, but further down the ava-
lanche spread out to the width of 430 meters. The total
length of the avalanche path was 1,400 meters and the
estimated size around 150,000 m 3.
The avalanchehit 17 buildings in the village and ranfar
beyond the avalanchehazardzone line. All of those build-
ings, except two, were homes and at that time there were
48 people in them, all asleep. Only 3 of those houses were
within the avalanchehazardzone, but had notbeen evacu-
ated at that time. The force of the avalanchewas enough
to totally wipe out some of the houses, but other were
damaged, some severely and others less so. Of those 48
people, 21 people got out the avalanche on their own or
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