Near the Cotabato Trench, two of the largest 20th century Philippine earthquakes: the 1918 Celebes Sea earthquake (8.3 Mw) and the 1976 Moro Gulf earthquake (8.0 Mw). Also included is the recent 2002 Mindanao earthquake (7.5 Mw). The Moro Gulf, part of the Celebes Sea, is labeled for context.
The 1918 Celebes Sea earthquake occurred on August 15 at 12:18 UTC near the Moro Gulf coast of Mindanao.[1] It had a magnitude of 8.3 on the moment magnitude scale[3] and a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. It triggered a tsunami of up to 7 m in height and the combined effects of the earthquake and tsunami led to the deaths of 52 people.
The earthquake had a magnitude of 8.3 on the moment magnitude scale, it had an estimated depth of 20 kilometers. The earthquake was 75 kilometers South southwest of Palimbang, Sultan Kudarat.[2] A station at Butuan in northern Mindanao registered over 600 aftershocks before the end of August, with 250 recorded by the end of August 16.[1][6]
The earthquake has been associated with rupture along the active east-dipping Cotabato Trench subduction zone beneath Mindanao.[4] The epicenter is interpreted to be in the same part of the plate interface as the 1976 Moro Gulf event. The distribution of effects suggests that fault rupture extended for 200 km along the coast. The average slip is estimated to be 4.1 m.[7]
Tsunami
This event in the southern Philippines triggered a large tsunami, with a maximum run-up of 7.2 m,[8] which affected the coasts of the Celebes Sea, causing widespread damage. The combined effects of the earthquake and the tsunami caused 52 casualties. With some sources stating that the tsunami alone caused up to 1,000 casualties.[9][better source needed]
Damage
The earthquake caused widespread damage in the coastal parts of southwestern Mindanao, with all houses destroyed around Sarangani Bay. The effects of the earthquake were compounded by the tsunami that particularly affected 150 km of coast between Lebak and Glan. A major landslide was also reported from one of the mountains around Saragani Bay.[1]
The number of casualties is uncertain as there is no definitive total.[7] Several sources refer to 52 deaths.[1]
The estimated losses were up to 5-25 million dollars. There was damage to a stone bridge at Paleleh, Central Sulawesi.[6]
^ abcdeNational Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information (1972). "Significant Earthquake Information". Significant Earthquake Database. doi:10.7289/V5TD9V7K. Retrieved June 28, 2024.
^Beck, Susan L.; Ruff, Larry. J. (1985). "The rupture process of the 1976 Mindanao Earthquake". Journal of Geophysical Research: Solid Earth. 90 (B8): 6773–6782. Bibcode:1985JGR....90.6773B. doi:10.1029/JB090iB08p06773.
^ abOkal, E.A.; Synolakis, C.E.; Kalligeris, N. (2011). "Tsunami Simulations for Regional Sources in the South China and Adjoining Seas". Pure and Applied Geophysics. 168 (6–7): 1153–1173. Bibcode:2011PApGe.168.1153O. doi:10.1007/s00024-010-0230-x.
^National Geophysical Data Center / World Data Service: NCEI/WDS Global Historical Tsunami Database. NOAA National Centers for Environmental Information. "Tsunami Event Information". NOAA National Centers for Environmental Information. doi:10.7289/V5PN93H7. Retrieved June 28, 2024.