2018
DOI: 10.1088/1742-6596/979/1/012020
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Study of characteristic of tsunami base on the coastal morphology in north Donggala, Central Sulawesi

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Cited by 3 publications
(3 citation statements)
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“…According to an earlier study by Horspool et al [7], who conducted a national probabilistic tsunami hazard assessment in Indonesia, which included Sulawesi Island among the study areas, over the last 100 years, the eastern part of Indonesia has experienced more massive tsunami events than has the western part. The northern arm of Sulawesi may generate earthquakes and tsunamis as a result of the subduction zone in the Sulawesi Sea [8]. Rahmadaningsi [8] constructed a simulation using a single fault method and simulated tsunami inundation using raster calculator functions in ArcGIS software, based on the 1996 earthquake that occurred at Toli-Toli, North Sulawesi.…”
Section: Introductionmentioning
confidence: 99%
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“…According to an earlier study by Horspool et al [7], who conducted a national probabilistic tsunami hazard assessment in Indonesia, which included Sulawesi Island among the study areas, over the last 100 years, the eastern part of Indonesia has experienced more massive tsunami events than has the western part. The northern arm of Sulawesi may generate earthquakes and tsunamis as a result of the subduction zone in the Sulawesi Sea [8]. Rahmadaningsi [8] constructed a simulation using a single fault method and simulated tsunami inundation using raster calculator functions in ArcGIS software, based on the 1996 earthquake that occurred at Toli-Toli, North Sulawesi.…”
Section: Introductionmentioning
confidence: 99%
“…The northern arm of Sulawesi may generate earthquakes and tsunamis as a result of the subduction zone in the Sulawesi Sea [8]. Rahmadaningsi [8] constructed a simulation using a single fault method and simulated tsunami inundation using raster calculator functions in ArcGIS software, based on the 1996 earthquake that occurred at Toli-Toli, North Sulawesi. The result shows that bay-shaped shorelines are associated with higher tsunami run-ups than straight or cape-shaped shorelines.…”
Section: Introductionmentioning
confidence: 99%
“…In addition, a tsunami is not always produced by an earthquake. [16] [4] further explains that underwater volcanic eruptions (for example the Krakatau eruption in 1883), hilly coastal landslides (for example Landslides in Lituya Bay in 1958), and the impact of meteors from outer space are other potential factors causing a tsunami on the coast. Therefore, given the tsunami that can spread rapidly in the high seas without losing much of its energy, coastal regions in the vast oceans such as the Indian Ocean, the Pacific Ocean and the Atlantic Ocean are very vulnerable to the impact of the tsunami.…”
Section: Introductionmentioning
confidence: 99%