| Author | |
| Date and time | 2016-01-13 18:33:41.0 UTC |
| Latitude | 44.706 |
| Longitude | -112.977 |
| Depth | 4 |
| Magnitude | 2.4 ML |
| Region | WESTERN MONTANA |
| Latest update | 2016-04-19 07:25:54.4 UTC |
| rms | 0.13 s |
| N° phases used for the localisation | 20 |
| N° stations used for the localisation | 20 |
| Gap | 120.0 ° |
| 95% confidence ellipse | |
| semi major | -- |
| semi minor | -- |
| Azimuth | -- ° |
| Location Type | manual |
Download data for this event
Note: links can take up to 20 minutes from the earthquake to become available
| Network | code | Distance° | EvAz | A/M | Phase | Pick time | Residual | T | Author |
|---|---|---|---|---|---|---|---|---|---|
| MCMT | 0.150 | 37 | M | P | 2016-01-13 18:33:45.4 | 0.10 | T | ||
| ICI | 0.380 | 176 | M | P | 2016-01-13 18:33:49.4 | 0.00 | T | ||
| MOMT | 0.430 | 105 | M | P | 2016-01-13 18:33:50.7 | 0.30 | T | ||
| BCYI | 0.500 | 218 | M | P | 2016-01-13 18:33:51.4 | -0.20 | T | ||
| EMI | 0.630 | 177 | M | P | 2016-01-13 18:33:53.9 | -0.10 | T | ||
| DLMT | 0.710 | 22 | M | P | 2016-01-13 18:33:55.4 | 0.10 | T | ||
| BGMT | 0.850 | 51 | M | P | 2016-01-13 18:33:57.8 | -0.10 | T | ||
| CNCI | 0.850 | 204 | M | P | 2016-01-13 18:33:58.0 | 0.20 | T | ||
| CMI | 0.980 | 100 | M | P | 2016-01-13 18:34:00.8 | 0.30 | T | ||
| DVCI | 1.060 | 253 | M | P | 2016-01-13 18:33:57.6 | 0.20 | T | ||
| QLMT | 1.110 | 83 | M | P | 2016-01-13 18:34:03.4 | 0.80 | T | ||
| HBMT | 1.120 | 13 | M | P | 2016-01-13 18:34:02.8 | 0.00 | T | ||
| LRM | 1.180 | 18 | M | P | 2016-01-13 18:34:03.9 | 0.00 | T | ||
| BOZ | 1.340 | 45 | M | P | 2016-01-13 18:34:05.9 | -0.20 | T | ||
| YWB | 1.340 | 94 | M | P | 2016-01-13 18:34:08.0 | 1.10 | T | ||
| LCCM | 1.370 | 34 | M | P | 2016-01-13 18:34:07.7 | 0.30 | T | ||
| MCID | 1.380 | 111 | M | P | 2016-01-13 18:34:07.7 | 0.00 | T | ||
| YMC | 1.400 | 87 | M | P | 2016-01-13 18:34:08.8 | 0.80 | T | ||
| YMR | 1.430 | 91 | M | P | 2016-01-13 18:34:08.9 | 0.40 | T | ||
| YHH | 1.520 | 86 | M | P | 2016-01-13 18:34:10.4 | 0.40 | T |