February 14, 1934 Tsunami: South China Sea, Philippines
A tsunami caused by a magnitude 7.9 earthquake began at South China Sea, Philippines on February 14, 1934 at 03:59:34 UTC. 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
- February 14, 1934, 03:59:34 UTC
- Source
- South China Sea, Philippines
- Cause
- Earthquake
- Earthquake
- Magnitude 7.9, 55 km deep
- Runups recorded
- 1
- Tsunami intensity (Soloviev-Imamura)
- 0.5
- Waters
- Ocean
- How certain
- Definite tsunami
- Source location
- 17.500° N, 119.000° E
The toll
- Damage
- Limited (under about $1 million) with the earthquake or eruption that caused it
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:
1934, February 14, 12:00 local time (17.5 N, 119 E, magnitude 7.6), there was a strong earthquake in the South China Sea, off the western coast of Luzon Island. The earthquake was accompanied by a small tsunami, which was observed at San Estaban. According to reports, the sea first retreated so markedly that the residents rushed to the dry strip of bottom to collect fish. Some of them almost drowned when the reflux was succeeded by a tidal wave.
Almost immediately during the earthquake (at 12:01), the Manila - Shanghai cable was cut. A ship sent from Shanghai to fix it found breaks at the following points: 17 deg 26 min 24 sec N., 119 deg 16 min 50 sec E., and 17 deg 25 min 45 sec N., 119 deg 16 min 50 sec E. The cable was repaired on February 23-25, but broke again on March 2 about in the middle between these two points, but this time the seismic stations did not register any earthquake. The bottom in the region of the break previously had an average depth of 2,465 m. Measurements of the bottom during repairs showed that the depth of the sea had diminished to 2,366 m 4 km south of the break, and had increased to 2,563 another 2 km further south.
The distinctive feature of the earthquake was the presence of very intensive long-period (20-30 sec.) waves between P and S onsets on the records of the stations at Hong Kong, Fulyan, Tsi Ka Vei (China) and others. The earthquake was accompanied by numerous recurrent shocks
Reference #1187:
1934, February 14, 11:59 a.m. Luzon 17o20'N - 119o20'E: It was perceptible over all of Luzon. The shaken area was approximately 1,885,900 sq km or 723,400 sq miles. In the coast towns nearest the centre of the earthquake, the motion was perceptible for 90 to 120 seconds, while in Manila, some 350 kms from the epicentre, the motion lasted about 60 seconds. Although the earthquake caused considerable alarm, the damage done on land was negligible... This epicentre is about 115 kms due west of San Esteban where a sea disturbance was observed. The first movement of the sea was reported to have been a recession and to such a noticeable extent that the people hurried out onto the exposed shore to gather fish which had been left stranded. Some persons narrowly escaped drowning when the water returned.
Reference #132:
1934, February 14. China Sea, 18o N, 118o E. Wave felt on northwest coast of Luzon.
Reference #10958:
1934, February 14. In the Ilocos Sur town of San Esteban, sea disturbance was reported (SEASEE, 1985) and some people narrowly escaped drowning when they tried to retrieve exposed fishes. Some surges were noted at sea south of Vigan shores (Repetti, 1934; Heck, 1947; Berninghausen, 1969). Tsunami probability is ranked as “positive”.
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 |
|---|---|---|---|---|---|---|---|
| San Estaban, Luzon Island | Philippines | 155 | Eyewitness observation of water height |
More
Every tsunami in 1934The 1900sTsunamis of PhilippinesThe 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 2026-10-01. NCEI tsunami event 1669.