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1955 Lanao earthquake

Coordinates:7°40′N123°10′E / 7.66°N 123.16°E /7.66; 123.16
From Wikipedia, the free encyclopedia
Earthquake in Mindanao, Philippines
1955 Lanao earthquake
1955 Lanao earthquake is located in Mindanao mainland
1955 Lanao earthquake
Show map of Mindanao mainland
1955 Lanao earthquake is located in Philippines
1955 Lanao earthquake
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UTC time1955-03-31 18:17:13
ISC event889384
USGS-ANSSComCat
Local dateApril 1, 1955
Local time02:17:13 (UTC+8)
Magnitude7.4Mw
Depth35 km (22 mi)
Epicenter7°40′N123°10′E / 7.66°N 123.16°E /7.66; 123.16
FaultCotabato-Sindangan Fault
TypeStrike-slip
Areas affectedMindanao
Total damage$5 million (1955 rate)
Max. intensityMMI VIII (Severe)
Casualties465 deaths
898 injured

The1955 Lanao earthquake struckLanao del Sur on April 1 at 02:17 local time. The earthquake measuring 7.4 on themoment magnitude scale and assigned a maximum intensity of VIII (Severe) on theModified Mercalli intensity scale was one of the largest to hitMindanao. It caused immense damage around the northern and central parts of Mindanao, as well as the southern reaches ofVisayas. It killed at least 465 individuals and injured a further 898.[1][2]

Geological setting

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Both provinces ofLanao del Sur andLanao del Norte run along two main faults, the western extension of the Mindanao Fault (Cotabato–Sindangan) and the northern segment of theCotabato Trench. The two faults were formed by the collision of thePhilippine Sea Plate andSunda Plate. In between the two faults lie thePhilippine Mobile Belt, a region the takes up most of the western regions of the Philippines.[3] It hosts multiple faults and active seismic blocks from southern Luzon to the Cotabato Trench.[4] The Cotabato Trench itself caused two earthquakes in1918 (Mw  8.3) and1976 (Mw  8.0). The last significant earthquake to happen in the same area as the 1955 event was a magnitude 6.0 earthquake on April 12, 2017.[4]

Earthquake

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The earthquake struck at dawn. Multiple magnitudes vary from moment magnitudes of 7.4–7.6 by local seismographs. It was assigned an intensity of VIII on theRossi–Forel scale. Most earthquakes that occur along the Cotabato Trench displays a strike-slip mechanism, which may be that of the 1955 earthquake.[5]

Multiple foreshocks preceded the mainshock, the largest measuring 6.3 occurred 6 hours earlier. It was first believed to be a double earthquake with the mainshock, however it was later confirmed to be a foreshock. Aftershocks also struck the area with varying magnitudes.[6]

Damage and casualties

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Most damage was centered aroundLanao Lake, more specifically the city of Dansalan (now known asMarawi). Numerous mosques were damaged or destroyed completely. Local houses and infrastructures collapsed due to the strong acceleration of ground movement. Towns southwest of theLanao Lake were said to have been submerged underwater for a few years due to ground displacement by a few meters in a southward direction, causing a miniature tsunami to that permanently flood the towns. The death toll from ranged from 225 to 465 according to multiple accounts, and injuries were counted near a thousand. InMisamis Occidental, the city ofOzamiz was also greatly affected. The earthquake caused the destruction of both the city's parish church and the southwest bastion of theFuerte de la Concepcion y del Triunfo, a Spanish fort that was built in the 18th-century. Thepresident at the time of the event,Ramon Magsaysay, declared a state of calamity in theprovinces ofMisamis Occidental,Misamis Oriental,Lanao, andSurigao.[7][2][8]

Religious implications

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The earthquake was deemed a sign fromGod towards those who sinned against him. This was due to the large religious Muslim and Christian populations that were present in the areas near the epicenter. TheBible andQuran were often cited and repeated during the aftermath by preachers and locals. During the earthquake itself, cries of children were heard along with chanting and prayers.[7]

See also

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References

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  1. ^"M 7.4 - Mindanao, Philippines".earthquake.usgs.gov. Retrieved2022-05-21.
  2. ^ab"NCEI Global Historical Hazard Database".www.ngdc.noaa.gov. Retrieved2022-05-21.
  3. ^Gervasio, F. C. (1967-10-01)."Age and nature of orogenesis of the philippines".Tectonophysics.4 (4–6):379–402.Bibcode:1967Tectp...4..379G.doi:10.1016/0040-1951(67)90006-6.ISSN 0040-1951.
  4. ^ab"A PRIMER ON THE 12 APRIL 2017 MAGNITUDE 6.0 LANAO DEL SUR EARTHQUAKE (relative to the 1955 Lanao quake)".PHIVOLCS. 12 April 2017. Retrieved22 May 2022.
  5. ^Wu, W.N.; Lo, C.-L.; Lin, J.-Y. (2017). "Spatial variations of the crustal stress field in the Philippine region from inversion of earthquake focal mechanisms and their tectonic implications".Journal of Asian Earth Sciences.142:109–118.Bibcode:2017JAESc.142..109W.doi:10.1016/j.jseaes.2017.01.036.
  6. ^"M 6.3 - 7 km W of Marogong, Philippines".earthquake.usgs.gov. Retrieved2022-05-22.
  7. ^abLanto, Macabangkit B."The 1955 Lanao del Sur earthquake".Daily Tribune. Archived fromthe original on 2022-05-25. Retrieved2022-05-22.
  8. ^"Proclamation No. 142, s. 1955 | GOVPH".Official Gazette of the Republic of the Philippines. Retrieved2022-05-22.

External links

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