Journal
PURE AND APPLIED GEOPHYSICS
Volume 176, Issue 6, Pages 2203-2213Publisher
SPRINGER BASEL AG
DOI: 10.1007/s00024-019-02181-9
Keywords
Tsunami generated from landslide; tsunami deposit; field survey; PaluSulawesi 2018
Categories
Funding
- Coordinating Ministry for Marine Affairs of the Republic of Indonesia (Kemenkomar RI)
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On 28 September 2018, a Mw 7.5 earthquake struck Sulawesi Island, soon followed by a destructive tsunami. This study provides a case history of tsunami deposition where submarine landslides or coastal collapses have contributed to and intensified tsunami generation. The sedimentary features resulting from this complex tsunami mechanism are not yet well understood. We surveyed tsunami deposits at six locations along the coastline of Palu Bay, in addition to measuring tsunami flow depth, run-up height, and inundation distance at each site. In general, the tsunami height was less than 8m with a maximum inundation distance of 310m. The tsunami deposits are thin with simple sedimentary structures such as fining upward sequences. These sedimentary characteristics are typical of tsunami deposits elsewhere around the world. This work is a preliminary study, in that numerical modeling including sediment transport has not been performed. Further work is needed to distinguish tsunamis with different source mechanisms.
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