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við strik
sprungunnar í heild, en þó er hún samhangandi við botninn. Hestvatnssprungan er einnig
nær lóðrétt og um 15,5 km löng og með strikstefnu N179°A. Hún er ólík Holtasprungunni
að því leyti að hún dýpkar til suðurs, úr 6 í 9 km en jafnframt virðist hún mynduð úr
tveimur mishallandi flötum. Rétt sunnan skjálftamiðjunnar er sprungan nær lóðrétt (88°
halli) en norðan upptakanna hallar
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
).
The implications of the present analysis are twofold. Firstly, a risk commu-
nication strategy based on providing scientifically sound information alone, even
if tailored to individuals’ perceptions of the issue and geared towards correcting
88 I. LORENZONI AND N. F. PIDGEON
misinformed opinions (Kempton, 1997), whilst clearly outlining feasible actions
individuals can undertake
/media/loftslag/Lorenzoni_Pidgeon_2006.pdf
.................... 85
8
Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86
Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87
Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88
Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf