July 4, 1904 Tsunami: Banda Sea, Indonesia
A tsunami caused by an earthquake began at Banda Sea, Indonesia on July 4, 1904. Its effects were recorded at 1 place.
Where the waves reached
The source (white) and every runup with a place, colored by the water height recorded there. A ring is a runup NCEI marks doubtful.
- Under 1 m
- 1 to 3 m
- 3 to 10 m
- 10 to 30 m
- 30 m and more
- Height not recorded
Travel times
How long the first wave took to reach each part of the ocean, one line for each hour up to 24, estimated from the source and the depth of the sea.
The travel times are computed in your browser, which needs JavaScript.
- 1 to 4 hours
- 5 to 6 hours
- 7 to 14 hours
- 15 hours and more
Computed in your browser the way NOAA’s own travel time maps are: the wave travels at the square root of gravity times the depth, over NOAA’s ETOPO1 depths averaged to a 10 arc-minute grid. Checked against NOAA NCEI’s maps for 21 tsunamis over the first 24 hours, these lines fall within 10 minutes of NCEI’s at half the points compared and within 52 minutes at 9 in 10. They give when the first wave could arrive, not how high it is; bays, harbors and island chains finer than the grid can see it later. Not for use in a warning: see tsunami.gov.
The tsunami
- Date
- July 4, 1904
- Source
- Banda Sea, Indonesia
- Cause
- Earthquake
- Earthquake
- The earthquake
- Runups recorded
- 1
- Tsunami intensity (Soloviev-Imamura)
- 1
- Waters
- Ocean
- How certain
- Very doubtful tsunami
- Source location
- 3.600° S, 128.700° E
The toll
- Damage
- Limited (under about $1 million)
Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.
What the record says
NCEI’s account, from the sources it cites.
Reference #414:
July 5, 1904, early morning. The sea was very stormy in Saparua Bay and outside of it, although there had been no storm there before. Part of the pier was smashed and washed off. At 2:00, a tidal wave fell on the coast at Sirisori; one proa, loaded with goods, ran aground and was smashed, but the passengers were saved. On other areas of the coast, as far as is known, nothing similar was observed. The cause of the waves is unclear. The last known earthquake had occurred on the 4th after 13:00 and was felt at Piru, Amahai and Wahai.
Reference #1188:
July 5,1904. Siri-Siri: West Sumatera - a part of the pier was destroyed and sailing boats on the coast of Siri-Siri sank as a result of the high waves.
Reference #3831:
July 5, 1904. The earthquake seemed to have a submarine origin. A part of the pier was destroyed and a sailing boat just off the Siri-Sori coast sank as a result of the high waves.
Reference #42:
July 4, 1904. Sumatra. Waves generated by a submarine shock off the Siri-Sori coast sank a sailing boat and damaged a pier,(Soetadi, 1962).
Note: reference #42, #12917 and #4659 lists this event in West Sumatra. However, location Siri-Sori (or Siri-Siri) only found in E. Indonesia. All sources point to reference #3831, which does not provide any details beyond "Siri-Sori". Reference #13384 lists an earthquake on 04 July 1904 07:00 (local) in South Maluku.
Every runup
Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.
| Where | Country | Km from source | Water height, m | Inland, m | Measured by | First wave, UTC | Deaths |
|---|---|---|---|---|---|---|---|
| Siri-Sori, Saparua | Indonesia | 16 | Eyewitness observation of water height |
More
Every tsunami in 1904The 1900sTsunamis of IndonesiaThe earthquakeThis day in weather historyAlerts in force
Sources
Tsunami events and runups from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI tsunami event 1315.