The map shows quakes of M1.5 and up from the last 90 days, the 8 biggest on record, and always the very latest quake — even if it was smaller than M1.5. The list below can include smaller ones the map leaves out. Tap any dot for details.
In the last 30 days, 280 earthquakes of M1.5 or bigger were recorded within 100 km of Diamond Ridge, the biggest of them M4.3. Over the past year, M3.0+ quakes near Diamond Ridge came at 1.5× the usual pace — busier than normal for this area. The biggest quake on record near Diamond Ridge — records go back to 1980 — was the M6.4 of Jul 29, 2015, 02:35 UTC: 52 km ENE of Pedro Bay, Alaska.
How we figure this: 106 quakes of M3.0 or bigger within 100 km in the last 12 months (Nov 04, 2025 – Nov 04, 2026), compared with an average of 70.5 a year across the full calendar years 2016–2025, counted the same way. This compares how often quakes happened in two past periods. It is not a forecast, and it does not mean a big earthquake is on its way — nobody can predict earthquakes.
Does a busier spell mean a bigger earthquake is coming?
Short answer: nobody can tell — and a busier spell by itself is not a warning sign. Bunches of small quakes are common around Diamond Ridge, and most settle down on their own. Small quakes also do not “let off steam” that would prevent a big one: a single M7 releases roughly as much energy as 32,000 M4 quakes added together. Earthquakes cannot be predicted. What can be measured is the long-term pattern — the biggest quakes on record near Diamond Ridge are listed further down this page.
Latest earthquakes near Diamond Ridge
| Mag | Location | Local time | Depth | Distance |
|---|---|---|---|---|
| M3.0 | 55 km ENE of Pedro Bay, Alaska | Nov 03, 2026, 09:57 PM | 132 km | 92 km WNW |
| M2.5 | 47 km WNW of Nanwalek, Alaska | Nov 03, 2026, 06:06 PM | 78 km | 70 km WSW |
| M2.7 | 34 km SSW of Nanwalek, Alaska | Nov 03, 2026, 05:26 PM | 62 km | 76 km SSW |
| M2.2 | 36 km W of Anchor Point, Alaska | Nov 03, 2026, 02:52 PM | 81 km | 52 km W |
| M2.4 | 52 km W of Anchor Point, Alaska | Nov 03, 2026, 07:56 AM | 100 km | 70 km WNW |
| M2.3 | 56 km WNW of Nanwalek, Alaska | Nov 03, 2026, 03:37 AM | 97 km | 73 km W |
| M2.6 | 54 km WNW of Nanwalek, Alaska | Nov 03, 2026, 03:37 AM | 98 km | 72 km WSW |
| M2.4 | 55 km W of Nanwalek, Alaska | Nov 02, 2026, 07:12 PM | 91 km | 85 km WSW |
| M2.3 | 49 km WNW of Anchor Point, Alaska | Nov 02, 2026, 10:57 AM | 92 km | 68 km WNW |
| M2.7 | 52 km WNW of Ninilchik, Alaska | Nov 02, 2026, 10:40 AM | 112 km | 79 km NW |
Earthquakes per year near Diamond Ridge (M3.0 and up, within 100 km)
M3.0–3.9 M4.0+
Each bar is one year; taller means more quakes (M3.0 and up). The dark red part is the bigger ones (M4.0+), counted inside the number above each bar — not added on top. These may be felt, depending on how far away and how deep they are. 2026 is not a full year yet — it only counts up to today. Source: USGS Earthquake Catalog.
What the last year looked like near Diamond Ridge
Every quake of M1.5 or bigger within 100 km over the last year — 2841 in total. A quake of exactly M2.0 counts in the M2.0–3.0 group.
The 8 biggest earthquakes on record near Diamond Ridge (M4.0 and up, since 1980)
| Mag | Location | Date (UTC) | Distance |
|---|---|---|---|
| M6.4 | 52 km ENE of Pedro Bay, Alaska | Jul 29, 2015, 02:35 UTC | 95 km |
| M5.9 | Southern Alaska | Jan 24, 2009, 18:09 UTC | 80 km |
| M5.9 | 66 km ENE of Pedro Bay, Alaska | Nov 20, 1993, 19:24 UTC | 91 km |
| M5.8 | 23 km WNW of Happy Valley, Alaska | May 10, 2014, 14:16 UTC | 49 km |
| M5.7 | 30 km ESE of Port Graham, Alaska | May 05, 1999, 10:30 UTC | 51 km |
| M5.6 | 48 km WNW of Nanwalek, Alaska | Mar 02, 2017, 02:11 UTC | 63 km |
| M5.6 | 67 km SE of Pedro Bay, Alaska | Feb 12, 1995, 20:13 UTC | 92 km |
| M5.5 | 6 km WNW of Nanwalek, Alaska | Feb 10, 2004, 20:33 UTC | 43 km |
Nearby places
Homer, AK (4 km) · Fritz Creek, AK (16 km) · Anchor Point, AK (19 km)
USGS data fetched Nov 04, 2026, 19:45 UTC · page built Nov 04, 2026, 19:45 UTC. How to read this page: recent-window counts cover M1.5+ events within 100 km, measured from the center of the place, not the city limits; the 10-year layer is based on M3.0+ and the history layer on M4.0+ since 1980. Recording completeness varies by era and region — small quakes from early decades are under-recorded, so “no record” does not prove “never happened”. Depths are relative to sea level and can be slightly negative for shallow events in elevated terrain. Method: data & methodology.