Tsunami from the Storegga Landslide
Chapter
Accepted version
Date
2019Metadata
Show full item recordCollections
- Import fra CRIStin [3580]
- Institutt for miljø- og naturvitskap [528]
Original version
Bondevik, S. (2019). Tsunami from the Storegga Landslide. In R. A. Meyers (Ed.), Encyclopedia of Complexity and Systems Science (pp. 1–33). Springer. 10.1007/978-3-642-27737-5_644-1Abstract
The Storegga tsunami was generated by the Storegga landslide off the Norwegian coast about 8150 years ago. The tsunami deposits show that the coasts of Scotland, Norway, Shetland, Faroe Islands and possibly also Eastern Greenland and Denmark was inundated, and that the tsunami ran up to heights ranging from 3 to more than 20 meters above sea level of that time. The Storegga tsunami is important for two reasons: First, it shows that big tsunamis have happened along passive margins and outside of the Pacific Ocean. Second, it is the only slide-generated tsunami of a basin-wide range where the run-up has been mapped out in the field and the tsunami simulated with numerical models.
Description
This is an accepted manuscript version of a book chapter published in the Encyclopedia of Complexity and Systems Science on 25 May 2019, and may be used under SpringerNature’s Terms of Use. The Version of Record can be found at https://doi.org/10.1007/978-3-642-27737-5_644-1