Strong M6.6 earthquake registered in Molucca Sea, Indonesia

Strong M6.6 earthquake registered in Molucca Sea, Indonesia

A strong earthquake measuring M6.6 on the Richter scale was registered in Molucca Sea, Indonesia at 11:34 UTC on December 21, 2014. USGS is reporting depth of 54.6 km (34 miles). Geoscience Australia is reporting Mwp 6.6 at depth of 60 km.

Epicenter was located 157 km (98 miles) WNW of Tobelo, 168 km (104 miles) NNW of Ternate and 179 km (111 miles) ENE of Bitung, Indonesia.

There are no people living within 100 km radius. Based on all available data, there is no tsunami threat from this earthquake, PTWC said.

USGS issued green alert for shaking-related fatalities and economic losses. There is a low likelihood of casualties and damage.

Overall, the population in this region resides in structures that are vulnerable to earthquake shaking, though some resistant structures exist.

Today's quake is a part of ongoing swarm of earthquakes being registered in Molucca Sea. In last 30 days, USGS registered 60 strong earthquakes in this region with magnitudes ranging from 4.0 - 6.8. See the map and a list below.

Additionally, Mount Gamalama in North Maluku province of Indonesia which erupted at 13:41 UTC on Thursday, December 18, 2014, is located about 168 km SSE from the epicenter of today's M6.6 earthquake. The eruption sent ash and rocks 2 km into the sky and forced the authorities to close an airport and issue warnings to planes. Nine people were injured, 4 of them seriously. As of press time, 1 person is still missing.

Map showing earthquakes registered in last 30 days. Credit: USGS

  1. 6.6157km WNW of Tobelo, Indonesia2014-12-21 11:34:14 UTC54.6 km
  2. 4.374km WSW of Tobelo, Indonesia2014-12-15 17:49:53 UTC136.7 km
  3. 4.8135km ENE of Bitung, Indonesia2014-12-14 14:14:36 UTC48.2 km
  4. 5.0150km NW of Kota Ternate, Indonesia2014-12-13 09:17:49 UTC28.7 km
  5. 4.534km NNW of Kota Ternate, Indonesia2014-12-12 11:39:20 UTC153.8 km
  6. 4.8123km ENE of Bitung, Indonesia2014-12-10 21:18:46 UTC27.6 km
  7. 4.4147km ENE of Bitung, Indonesia2014-12-10 02:22:24 UTC58.0 km
  8. 5.9132km E of Bitung, Indonesia2014-12-09 03:09:23 UTC36.8 km
  9. 5.4140km ENE of Bitung, Indonesia2014-12-08 07:35:51 UTC10.0 km
  10. 4.6115km NW of Kota Ternate, Indonesia2014-12-08 04:41:58 UTC40.6 km
  11. 5.2119km NNW of Ternate, Indonesia2014-12-08 01:28:18 UTC112.9 km
  12. 4.6159km NW of Kota Ternate, Indonesia2014-12-06 11:03:01 UTC35.0 km
  13. 4.670km NW of Tobelo, Indonesia2014-12-05 17:57:32 UTC67.2 km
  14. 5.2159km NNW of Kota Ternate, Indonesia2014-12-05 15:39:06 UTC66.8 km
  15. 4.8156km WNW of Tobelo, Indonesia2014-12-05 14:55:54 UTC53.3 km
  16. 4.7120km ENE of Bitung, Indonesia2014-12-03 00:27:07 UTC29.7 km
  17. 4.8146km ENE of Bitung, Indonesia2014-12-01 16:36:57 UTC35.0 km
  18. 4.3139km NW of Kota Ternate, Indonesia2014-12-01 04:39:55 UTC33.3 km
  19. 4.0123km WNW of Tobelo, Indonesia2014-12-01 03:33:11 UTC35.0 km
  20. 4.1125km WNW of Tobelo, Indonesia2014-12-01 03:15:33 UTC35.0 km
  21. 4.8155km NW of Kota Ternate, Indonesia2014-11-29 21:23:58 UTC45.7 km
  22. 5.6133km WNW of Tobelo, Indonesia2014-11-29 19:40:09 UTC31.1 km
  23. 4.2133km WNW of Tobelo, Indonesia2014-11-29 06:12:52 UTC35.0 km
  24. 4.558km NW of Tobelo, Indonesia2014-11-29 00:30:54 UTC47.7 km
  25. 4.1125km NW of Kota Ternate, Indonesia2014-11-28 23:07:53 UTC41.0 km
  26. 4.0172km WNW of Tobelo, Indonesia2014-11-28 21:13:10 UTC59.5 km
  27. 5.2154km ENE of Bitung, Indonesia2014-11-28 19:29:30 UTC24.2 km
  28. 4.694km NW of Kota Ternate, Indonesia2014-11-28 00:22:03 UTC39.5 km
  29. 4.5158km ENE of Bitung, Indonesia2014-11-27 23:22:13 UTC42.2 km
  30. 4.499km NW of Kota Ternate, Indonesia2014-11-27 17:17:35 UTC47.8 km
  31. 4.7144km ENE of Bitung, Indonesia2014-11-27 05:26:38 UTC35.0 km
  32. 4.8158km NNW of Kota Ternate, Indonesia2014-11-26 22:05:41 UTC35.0 km
  33. 4.5147km WNW of Tobelo, Indonesia2014-11-26 21:28:49 UTC39.3 km
  34. 4.6149km ENE of Bitung, Indonesia2014-11-26 21:07:55 UTC31.6 km
  35. 4.3152km NNW of Kota Ternate, Indonesia2014-11-26 19:47:53 UTC46.4 km
  36. 4.4154km ENE of Bitung, Indonesia2014-11-26 17:43:53 UTC35.0 km
  37. 5.0150km NW of Kota Ternate, Indonesia2014-11-26 17:16:01 UTC21.1 km
  38. 4.573km W of Tobelo, Indonesia2014-11-26 16:40:46 UTC109.6 km
  39. 4.1139km WNW of Tobelo, Indonesia2014-11-26 16:03:50 UTC38.2 km
  40. 4.5124km ENE of Bitung, Indonesia2014-11-26 15:34:25 UTC35.0 km
  41. 4.6146km W of Tobelo, Indonesia2014-11-26 15:33:54 UTC35.0 km
  42. 4.1145km ENE of Bitung, Indonesia2014-11-26 15:31:56 UTC35.0 km
  43. 4.2153km WNW of Tobelo, Indonesia2014-11-26 15:30:43 UTC35.0 km
  44. 4.2139km ENE of Bitung, Indonesia2014-11-26 15:20:24 UTC35.0 km
  45. 4.6155km NW of Kota Ternate, Indonesia2014-11-26 15:18:49 UTC35.0 km
  46. 4.1146km NW of Kota Ternate, Indonesia2014-11-26 15:11:54 UTC35.0 km
  47. 5.0150km NW of Kota Ternate, Indonesia2014-11-26 15:02:47 UTC35.0 km
  48. 5.6153km NW of Kota Ternate, Indonesia2014-11-26 14:49:50 UTC38.9 km
  49. 5.1152km ENE of Bitung, Indonesia2014-11-26 14:48:30 UTC35.0 km
  50. 4.9162km WNW of Tobelo, Indonesia2014-11-26 14:46:36 UTC35.0 km
  51. 6.8156km NW of Kota Ternate, Indonesia2014-11-26 14:33:43 UTC39.0 km
  52. 4.4137km ENE of Bitung, Indonesia2014-11-25 19:57:02 UTC43.2 km
  53. 5.1132km WNW of Tobelo, Indonesia2014-11-25 16:29:52 UTC46.7 km
  54. 4.7152km ENE of Bitung, Indonesia2014-11-25 14:59:17 UTC52.3 km
  55. 4.534km N of Ternate, Indonesia2014-11-24 05:07:56 UTC10.0 km
  56. 4.8109km WNW of Tobelo, Indonesia2014-11-24 05:02:29 UTC43.3 km
  57. 4.1138km ENE of Bitung, Indonesia2014-11-22 05:20:21 UTC35.0 km
  58. 4.5146km NNW of Kota Ternate, Indonesia2014-11-21 20:40:23 UTC49.5 km
  59. 4.5148km ENE of Bitung, Indonesia2014-11-21 17:07:02 UTC58.7 km
  60. 4.7160km WNW of Tobelo, Indonesia2014-11-21 12:43:47 UTC32.0 km
Data source: USGS (Updated: 12:27 UTC on December 21, 2014)

 

Population exposure (data for M6.6 on December 21, 2014)

Population per ˜1 sq. km. from LandScan

Selected cities exposed

from GeoNames Database of Cities with 1,000 or more residents

MMI CityPopulation
IVTobelo10k
IVBitung137k
IVManado452k
IVTondano33k
IVTernate102k
IIIKota Ternate<1k
IIILaikit, Laikit II (Dimembe)  8k
IIITomohon28k
IIITompasobaru<1k
IIIPoigar<1k
IIIDumoga<1k

(k = x1,000)

Seismotectonics of the Philippine Sea and Vicinity

The Philippine Sea plate is bordered by the larger Pacific and Eurasia plates and the smaller Sunda plate. The Philippine Sea plate is unusual in that its borders are nearly all zones of plate convergence. The Pacific plate is subducted into the mantle, south of Japan, beneath the Izu-Bonin and Mariana island arcs, which extend more than 3,000 km along the eastern margin of the Philippine Sea plate. This subduction zone is characterized by rapid plate convergence and high-level seismicity extending to depths of over 600 km. In spite of this extensive zone of plate convergence, the plate interface has been associated with few great (M>8.0) ‘megathrust’ earthquakes. This low seismic energy release is thought to result from weak coupling along the plate interface (Scholz and Campos, 1995). These convergent plate margins are also associated with unusual zones of back-arc extension (along with resulting seismic activity) that decouple the volcanic island arcs from the remainder of the Philippine Sea Plate (Karig et al., 1978; Klaus et al., 1992).

South of the Mariana arc, the Pacific plate is subducted beneath the Yap Islands along the Yap trench. The long zone of Pacific plate subduction at the eastern margin of the Philippine Sea Plate is responsible for the generation of the deep Izu-Bonin, Mariana, and Yap trenches as well as parallel chains of islands and volcanoes, typical of circum-pacific island arcs. Similarly, the northwestern margin of the Philippine Sea plate is subducting beneath the Eurasia plate along a convergent zone, extending from southern Honshu to the northeastern coast of Taiwan, manifested by the Ryukyu Islands and the Nansei-Shoto (Ryukyu) trench. The Ryukyu Subduction Zone is associated with a similar zone of back-arc extension, the Okinawa Trough. At Taiwan, the plate boundary is characterized by a zone of arc-continent collision, whereby the northern end of the Luzon island arc is colliding with the buoyant crust of the Eurasia continental margin offshore China.

Along its western margin, the Philippine Sea plate is associated with a zone of oblique convergence with the Sunda Plate. This highly active convergent plate boundary extends along both sides the Philippine Islands, from Luzon in the north to the Celebes Islands in the south. The tectonic setting of the Philippines is unusual in several respects: it is characterized by opposite-facing subduction systems on its east and west sides; the archipelago is cut by a major transform fault, the Philippine Fault; and the arc complex itself is marked by active volcanism, faulting, and high seismic activity. Subduction of the Philippine Sea Plate occurs at the eastern margin of the archipelago along the Philippine Trench and its northern extension, the East Luzon Trough. The East Luzon Trough is thought to be an unusual example of a subduction zone in the process of formation, as the Philippine Trench system gradually extends northward (Hamburger et al., 1983). On the west side of Luzon, the Sunda Plate subducts eastward along a series of trenches, including the Manila Trench in the north, the smaller less well-developed Negros Trench in the central Philippines, and the Sulu and Cotabato trenches in the south (Cardwell et al., 1980). At its northern and southern terminations, subduction at the Manila Trench is interrupted by arc-continent collision, between the northern Philippine arc and the Eurasian continental margin at Taiwan and between the Sulu-Borneo Block and Luzon at the island of Mindoro. The Philippine fault, which extends over 1,200 km within the Philippine arc, is seismically active. The fault has been associated with major historical earthquakes, including the destructive M7.6 Luzon earthquake of 1990 (Yoshida and Abe, 1992). A number of other active intra-arc fault systems are associated with high seismic activity, including the Cotabato Fault and the Verde Passage-Sibuyan Sea Fault (Galgana et al., 2007).

Relative plate motion vectors near the Philippines (about 80 mm/yr) is oblique to the plate boundary along the two plate margins of central Luzon, where it is partitioned into orthogonal plate convergence along the trenches and nearly pure translational motion along the Philippine Fault (Barrier et al., 1991). Profiles B and C reveal evidence of opposing inclined seismic zones at intermediate depths (roughly 70-300 km) and complex tectonics at the surface along the Philippine Fault.

Several relevant tectonic elements, plate boundaries and active volcanoes, provide a context for the seismicity presented on the main map. The plate boundaries are most accurate along the axis of the trenches and more diffuse or speculative in the South China Sea and Lesser Sunda Islands. The active volcanic arcs (Siebert and Simkin, 2002) follow the Izu, Volcano, Mariana, and Ryukyu island chains and the main Philippine islands parallel to the Manila, Negros, Cotabato, and Philippine trenches.

Seismic activity along the boundaries of the Philippine Sea Plate (Allen et al., 2009) has produced 7 great (M>8.0) earthquakes and 250 large (M>7) events. Among the most destructive events were the 1923 Kanto, the 1948 Fukui and the 1995 Kobe (Japan) earthquakes (99,000, 5,100, and 6,400 casualties, respectively), the 1935 and the 1999 Chi-Chi (Taiwan) earthquakes (3,300 and 2,500 casualties, respectively), and the 1976 M7.6 Moro Gulf and 1990 M7.6 Luzon (Philippines) earthquakes (7,100 and 2,400 casualties, respectively). There have also been a number of tsunami-generating events in the region, including the Moro Gulf earthquake, whose tsunami resulted in more than 5000 deaths. (USGS) More information on regional seismicity and tectonics

Featured image credit: USGS

Tags: molucca sea

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