| Author | THE |
| Date and time | 2026-03-08 03:39:49.4 UTC |
| Latitude | 39.620 |
| Longitude | 20.640 |
| Depth | 12 |
| Magnitude | 3.6 ML |
| Region | GREECE |
| Latest update | 2026-03-08 08:33:09.8 UTC |
| rms | 0.17 s |
| N° phases used for the localisation | 20 |
| N° stations used for the localisation | 10 |
| Gap | 110.3 ° |
| 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 |
|---|---|---|---|---|---|---|---|---|---|
| HL | JAN | 0.165 | 77 | M | P | 2026-03-08 03:39:53.2 | -0.10 | T | THE |
| HL | JAN | 0.165 | 77 | M | S | 2026-03-08 03:39:56.4 | 0.20 | T | THE |
| HI | JAN3 | 0.166 | 67 | M | P | 2026-03-08 03:39:53.2 | 0.00 | T | THE |
| HI | JAN3 | 0.166 | 67 | M | S | 2026-03-08 03:39:56.2 | -0.10 | T | THE |
| HI | JAN2 | 0.170 | 75 | M | P | 2026-03-08 03:39:53.3 | 0.00 | T | THE |
| HI | JAN2 | 0.170 | 75 | M | S | 2026-03-08 03:39:56.5 | 0.20 | T | THE |
| HT | IGT | 0.255 | 250 | M | P | 2026-03-08 03:39:54.5 | -0.20 | T | THE |
| HT | IGT | 0.255 | 250 | M | S | 2026-03-08 03:39:58.9 | 0.10 | T | THE |
| 1Y | GR14 | 0.284 | 350 | M | P | 2026-03-08 03:39:55.2 | -0.10 | T | THE |
| 1Y | GR14 | 0.284 | 350 | M | S | 2026-03-08 03:40:00.2 | 0.30 | T | THE |
| HP | KSTR | 0.374 | 188 | M | P | 2026-03-08 03:39:56.8 | 0.10 | T | THE |
| HP | KSTR | 0.374 | 188 | M | S | 2026-03-08 03:40:02.7 | 0.30 | T | THE |
| 1Y | GR15 | 0.448 | 44 | M | P | 2026-03-08 03:39:58.3 | 0.00 | T | THE |
| 1Y | GR15 | 0.448 | 44 | M | S | 2026-03-08 03:40:05.6 | 0.40 | T | THE |
| AC | LSK | 0.530 | 357 | M | P | 2026-03-08 03:40:00.2 | 0.40 | T | THE |
| AC | LSK | 0.530 | 357 | M | S | 2026-03-08 03:40:07.6 | -0.30 | T | THE |
| AC | SRN | 0.557 | 298 | M | P | 2026-03-08 03:40:00.2 | 0.10 | T | THE |
| AC | SRN | 0.557 | 298 | M | S | 2026-03-08 03:40:08.8 | 0.40 | T | THE |