The 1833 Sumatra earthquake, occurring on November…
November 1833 CE
There are no reliable records of the loss of life, with the casualties being described only as 'numerous'.
The magnitude of this event has been estimated using records of uplift taken from coral microatolls.
The earthquake shaking lasts five minutes in Bengkulu and three minutes in Padang; combined with the severity this suggests a very large source rupture.
Modelling of the tsunami suggests that most of the energy would have been radiated out into the Indian Ocean, sparing most coastal population centers outside Sumatra itself.