All archives · Papua New Guinea

Papua New Guinea · Earthquake archives July 2008

Explore earthquake activity year by year and month by month using the historical Quake Pulse database.

Events19
Largest magnitudeM 5.7
M6+0
M7+0
Average depth76.8 km

Strongest events

MagnitudeLocationDepthTime
M 5.7117 km SSE of Lorengau, Papua New Guinea23.7 km2008-07-11 09:58:49 UTCView event →
M 5.5102 km ENE of Kainantu, Papua New Guinea39.1 km2008-07-25 20:11:07 UTCView event →
M 5.5135 km S of Kavieng, Papua New Guinea10.0 km2008-07-20 21:13:36 UTCView event →
M 5.3177 km NNE of Rabaul, Papua New Guinea10.0 km2008-07-29 18:54:35 UTCView event →
M 5.126 km NW of Madang, Papua New Guinea215.8 km2008-07-06 17:36:29 UTCView event →
M 5.1158 km ENE of Angoram, Papua New Guinea35.0 km2008-07-04 10:18:02 UTCView event →
M 4.9143 km SE of Kokopo, Papua New Guinea26.6 km2008-07-21 11:37:56 UTCView event →
M 4.877 km SSE of Panguna, Papua New Guinea84.6 km2008-07-02 01:52:35 UTCView event →
M 4.798 km SSE of Finschhafen, Papua New Guinea44.9 km2008-07-30 09:23:34 UTCView event →
M 4.646 km SSE of Kimbe, Papua New Guinea69.5 km2008-07-26 11:37:38 UTCView event →
M 4.6114 km SW of Kokopo, Papua New Guinea150.1 km2008-07-24 21:55:41 UTCView event →
M 4.6153 km ESE of Kimbe, Papua New Guinea52.3 km2008-07-24 08:04:07 UTCView event →
M 4.6179 km N of Madang, Papua New Guinea35.0 km2008-07-23 20:32:12 UTCView event →
M 4.6124 km E of Madang, Papua New Guinea220.9 km2008-07-09 19:32:26 UTCView event →
M 4.652 km W of Kimbe, Papua New Guinea136.0 km2008-07-03 04:59:59 UTCView event →
M 4.5209 km N of Madang, Papua New Guinea35.0 km2008-07-28 07:42:48 UTCView event →
M 4.5139 km W of Panguna, Papua New Guinea36.7 km2008-07-16 09:13:32 UTCView event →
M 4.5198 km ENE of Madang, Papua New Guinea134.2 km2008-07-13 20:31:27 UTCView event →
M 4.571 km ESE of Ambunti, Papua New Guinea100.5 km2008-07-07 06:35:07 UTCView event →

Historical small-earthquake detection varies through time. Long-term comparisons are most robust at higher magnitude thresholds.

Historical small-earthquake detection varies through time. Long-term comparisons are most robust at higher magnitude thresholds.

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