1797 Sumatra earthquake

Background

The island of Sumatra lies on the convergent plate boundary between the Indo-Australian plate and the Eurasian plate. The convergence between these plates is highly oblique near Sumatra, with the displacement being accommodated by near pure dip-slip faulting along the subduction zone, known as the Sunda megathrust, and near pure strike-slip faulting along the Great Sumatran fault. The major slip events on the subduction zone interface are typically of the megathrust type.

Historically, great or giant megathrust earthquakes have been recorded in 1797, 1833, 1861, 2004, 2005 and 2007, most of them being associated with devastating tsunamis. Smaller (but still large) megathrust events have also occurred in the small gaps between the areas that slip during these larger events, in 1935, 1984, 2000 and 2002.

Damage

The earthquake caused the collapse or damage of many houses. The tsunami surge drove an English sailing ship of 150–200 t, moored in the Arau River, about 1 km inland, destroying several houses as it went. Smaller boats were driven up to 1.8 km upstream. In Air Manis, the whole town was flooded and the bodies of several people who had climbed trees to escape the surge were found the next day in the branches. Only two fatalities were reported from Padang itself but many more from Air Manis. The Batu Islands were also reported to be affected.

Characteristics

Earthquake

The shaking lasted up to seven minutes. The magnitude of the earthquake has been estimated from uplift patterns determined from eroded coral microatolls in the range 8.6–8.8. Reports in 1845 and 1847 said either that this was the strongest earthquake in the memory of the residents of Padang or the strongest for forty years.

Tsunami

The run-up of the tsunami at Padang and the village of Air Manis is estimated to be in the range of 5-10 m. Modelling of tsunami effects using source parameters estimated from the uplift of microatolls, provide a reasonable match to the sparse historical records.

The tsunami reports for this event are localised around Padang and it has been suggested that the tsunami may have been caused by an underwater landslide triggered by the earthquake.

References

References

1. (1972). "Significant Earthquakes Information". [[National Centers for Environmental Information]].
2. (2014). "Rupture and variable coupling behavior of the Mentawai segment of the Sunda megathrust during the supercycle culmination of 1797 to 1833". Journal of Geophysical Research: Solid Earth.
3. Natawidjaja, D. H.. (2006). "Source parameters of the great Sumatran megathrust earthquakes of 1797 and 1833 inferred from coral microatolls". Journal of Geophysical Research.
4. Borrero, J.C.. (December 26, 2006). "Tsunami inundation modeling for western Sumatra". Proceedings of the National Academy of Sciences.
5. Permana, H.. (2010). "Submarine mass movement and localized tsunami potentiality of Mentawai Basin, Sumatera, Indonesia".
6. (2022). "Gempa Nusantara: A Database of 7380 Macroseismic Observations for 1200 Historical Earthquakes in Indonesia from 1546 to 1950". Bulletin of the Seismological Society of America.