1953 Suva earthquake
  | |
| Date | September 14, 1953 |
|---|---|
| Magnitude | 6.8 Ms[1] |
| Depth | 60 km |
| Epicenter | 18°12′S 178°18′E / 18.2°S 178.3°ECoordinates: 18°12′S 178°18′E / 18.2°S 178.3°E[1] |
| Areas affected | Fiji |
| Max. intensity | VII |
| Tsunami | local |
| Casualties | 8 |
The 1953 Suva earthquake occurred on September 14 at 00:26 UTC near Suva, Fiji, just off the southeast shore of Viti Levu. This earthquake had a magnitude of Ms 6.8. The earthquake triggered a coral reef platform collapse and a submarine landslide that caused a tsunami.[2][3] Eight people were reported killed;[4] a wharf, bridges, and buildings were severely damaged in Suva.[2]
Tectonic setting
Fiji lies in a complex tectonic setting along the boundary between the Australian Plate and the Pacific Plate. Southwards from Fiji the Pacific Plate is subducting beneath the Australian Plate along the Tonga Trench forming the Tonga Ridge island arc system and the Lau Basin back-arc basin. To the southwest of Fiji the Australian Plate is subducting beneath the Pacific Plate forming the Vanuatu Ridge island arc system and the North Fiji back-arc basin.[2] Hence, the region has undergone a complex process of plate convergence, subduction, and arc volcanism from the Middle Eocene to the Early Pliocene.[5] Many of the larger islands, such as Viti Levu, are of volcanic origin.[6] Volcanism still exists, and there are Holocene volcanos in Fiji.[7]
The Fiji Platform lies in a zone bordered with active extension fault lines around which most of the shallow earthquakes were centered. These fault lines are the Fiji Fracture Zone (FFZ) to the north, the 176° Extension Zone (176°E EZ) to the west, and the Hunter Fracture Zone (HFZ) to the east.[5]
Earthquake
The earthquake lasted between 25 and 30 seconds and had an estimated magnitude of 6.75 on the surface wave magnitude scale. The calculated focal mechanism is consistent with slightly oblique dextral (right lateral) strike-slip on a NW-SE trending fault plane, matching the orientation of other fault planes measured in the area and a marked bathymetric lineament. The fault parameters calculated for the earthquake are a length of 30 km, a width of 27 km and a slip of one metre.[2] The NW trending nodal plane of this earthquake coincides with the strike of the NW trending Naqara Fault on the southeast coast of Viti Levu.[8]
Tsunami
The first sign of the tsunami was observed about one minute after the earthquake when a disturbance of the sea surface was noticed by the captain of the cutter Adi Tirisa "beyond the reef some 4 to 5 miles southwest of Suva…she was badly shaken and a little later three great spouts burst out of the sea, carrying mud, stones, and part of a long-wrecked vessel…" The location of this disturbance was at the western end of the entrance to the Suva Passage.[2]
Origin
From the type of fault displacement and the magnitude of the event it was clear that the tsunami was not caused by any displacement of the seabed associated with the earthquake. The shaking triggered collapse of part of the barrier reef at Suva into the Suva Canyon. The current reef edge shows the effects of repeated slope failure. The characteristics of the 1953 landslide scar were investigated using a high resolution multibeam echo sounder. The area immediately offshore from the reef is a composite failure surface, within which a fresh scar was identified with a width of 800 m, defining an estimated slide volume of 60 million cubic metres. Numerical modelling of this as the likely source was able to reproduce many aspects of the observed development of the tsunami.[2]
Damage
This earthquake was the most destructive in Fiji's recorded history, the tremor itself killing three people and seriously injuring twenty others. The most serious damage occurred in the southeastern part of Viti Levu. The tsunami caused particular damage to coastal areas not protected by barrier reefs, devastating the villages of Nakasaleka and Makaluva. There were five deaths from the tsunami, three at Suva and two at Nakasaleka.[2] Had the tsunami occurred at high tide, rather than low tide it would have been more damaging.[3]
The landslide that caused the tsunami generated turbidity currents that damaged several underwater cables in the Suva Canyon.[2] The total damage caused by earthquake and tsunami was estimated as $500,000 (at 1953 values in U.S. dollars).[4]
See also
References
- 1 2 NGDC. "Comments for the Significant Earthquake". Retrieved 2 November 2010.
- 1 2 3 4 5 6 7 8 Rahiman, T.I.H.; Pettinga J.R. & Watts P. (2007). "The source mechanism and numerical modelling of the 1953 Suva tsunami, Fiji". Marine Geology. 237 (1–2): 55–70. doi:10.1016/j.margeo.2006.10.036. Retrieved 21 March 2011.
- 1 2 Pacific Disaster Center. "Summary of Earthquakes and Tsunamis Affecting Fiji 1850–2004" (PDF). Tsunami Awareness Kit. Retrieved 22 March 2011.
- 1 2 Fiji Mineral Resources Department. "Earthquake in Fiji". Retrieved 22 March 2011.
- 1 2 Greenbaum, D.; Bowker, M. R; Dau, I; Drospy, H; Greally, K. B; McDonald A. J. W; Marsh, S. H; Northmore, K. J; O'Connor, E. A; Prasad, R. S & Tragheim, D. G. (1995). "Landslide hazards in Fiji" (PDF). Technical Report WC/95/28 Rapid methods of landslide hazard mapping : Fiji case study. British Geological Survey. Retrieved 23 March 2011.
- ↑ Government of Fiji (2009). "Government of Fiji Country Report on Pacific Adaptation to Climate Change (PACC) Inception Meeting Samoa, from 29th June – 3rd July 2009." (PDF). p. 2. Retrieved 23 March 2011.
- ↑ Global Volcanism Program. "Volcanoes of New Zealand to Fiji: Fiji Islands". Volcanoes of the World. Retrieved 23 March 2011.
- ↑ Rahiman, Tariq I.H.; Pettinga, Jarg R. (2009). "Fracture lineaments, fault mesh formation and seismicity: Towards a seismotectonic model for Viti Levu, Fiji" (PDF). Bulletin of the New Zealand Society for Earthquake Engineering. 42 (1): 63–72. Retrieved 3 February 2013.
Sources
- Houtz, R. E., "The 1953 Suva earthquake and tsunami", Bulletin of the Seismological Society of America, Seismological Society of America, 52 (1): 1–12