Tsunamis are unpredictable and infrequent but potentially large impact natural disasters. To
prepare, mitigate and prevent losses from tsunamis, probabilistic hazard and risk analysis …

Assessing initiation of rock-slope deformation and paleo-slip rates of rockslides is important
to understand the impact of climate variability-in particular permafrost changes-on rockslide …

Landslides are the second most frequent tsunami source worldwide. However, their complex
and diverse nature of origin combined with their infrequent event records make prognostic …

Abstract The Glacier Bay area in southeastern Alaska and British Columbia, encompassing
Glacier Bay National Park and Preserve, has experienced rapid glacier retreat since the end …

An unstable rock volume of more than 50 million m 3 has been detected in the Åkerneset
rock slope in the narrow fjord, Storfjorden, Møre & Romsdal County, Western Norway. If …

Destructive tsunamis are most often generated by large earthquakes occurring at subduction
interfaces, but also other “atypical” sources—defined as crustal earthquakes and non …

We have compiled recently published and unpublished cosmogenic 10 Be exposure ages of
rock-avalanche deposits and break away scars in western and southern Norway in order to …

Large catastrophic rock slope failures are difficult to predict because the underlying
mechanisms causing slope accelerations are difficult to study under in-situ conditions. For …

For quantitative hazard assessment it is necessary to define the magnitude–frequency
distribution and a temporal model of the landslide frequency. This is often complicated for …

Instrumental monitoring of displacement rates of slow-moving rockslides is limited to an
insufficient length of the pre–catastrophic failure deformation time. Prehistorical slip rates …