PAGER: Prompt Assessment of Global Earthquakes for Response
MMI | Mag | Location | Lat | Lon | Depth | Version |
---|---|---|---|---|---|---|
IV | 5.4 | NEW BRITAIN REGION, PAPUA NEW GUINEAEvent time UTC: 2009-05-05 22:26:07 | -4.79 | 151.78 | 103km | 3 |
III | 3.8 | 24.7 miles E of TalkeetnaEvent time UTC: 2009-05-05 21:31:18 | 62.25 | -149.35 | 24km | 3 |
I | 3.9 | 41.4 miles WNW of HomerEvent time UTC: 2009-05-04 11:46:42 | 59.78 | -152.70 | 86km | 4 |
VI | 5.5 | PAPUA, INDONESIAEvent time UTC: 2009-05-04 03:33:51 | -3.55 | 135.52 | 51km | 4 |
IV | 4.2 | 0.5 km (0.3 mi) NE of Pine Hills, CAEvent time UTC: 2009-05-03 17:54:05 | 40.75 | -124.16 | 21km | 4 |
V | 6.2 | GUATEMALAEvent time UTC: 2009-05-03 16:21:47 | 14.58 | -91.15 | 127km | 3 |
I | 3.6 | 91.5 miles SSW of KodiakEvent time UTC: 2009-05-02 21:50:46 | 56.65 | -153.65 | 3km | 4 |
I | 3.6 | 50.1 miles SE of King CoveEvent time UTC: 2009-05-02 02:28:35 | 54.50 | -161.49 | 17km | 2 |
IV | 5.3 | 50.8 miles SE of King CoveEvent time UTC: 2009-05-02 02:19:11 | 54.48 | -161.53 | 5km | 7 |
V | 4.4 | 3.6 mi ENE of Leo Carrillo State Beach, CAEvent time UTC: 2009-05-02 01:11:13 | 34.07 | -118.88 | 14km | 6 |
III | 3.5 | 11.4 mi SE of Taft, CAEvent time UTC: 2009-05-01 15:39:25 | 35.02 | -119.31 | 17km | 3 |
VIII | 5.9 | SOLOMON ISLANDSEvent time UTC: 2009-05-01 06:03:06 | -10.75 | 162.31 | 21km | 2 |
III | 3.4 | NEW MEXICOEvent time UTC: 2009-05-01 01:34:03 | 36.77 | -104.72 | 5km | 2 |
IV | 3.5 | 14.1 km (8.8 mi) N of Morgan Hill, CAEvent time UTC: 2009-04-30 22:50:54 | 37.25 | -121.64 | 7km | 4 |
V | 5.2 | SOUTHEASTERN IRANEvent time UTC: 2009-04-30 10:04:27 | 27.75 | 61.43 | 70km | 3 |
III | 4.9 | 33.6 miles SSE of SeldoviaEvent time UTC: 2009-04-30 04:54:57 | 58.99 | -151.31 | 53km | 5 |
PAGER Archive
For earthquakes larger than magnitude 5.5, PAGER results are generally available on the Internet within 30 minutes of the earthquake's occurrence. However, information on the extent of shaking will be uncertain in the minutes and hours following an earthquake and typically improves as additional sensor data and reported intensities are acquired and incorporated into models of the earthquake's source. Users of PAGER exposure estimates should account for uncertainty and always seek the most current PAGER release for any earthquake.