Reviewed by USGSAlaska18y ago
M2.6 earthquake 109 km WSW of Adak, Alaska
Wednesday, August 27, 2008, 10:04:24 UTC · 51.602°N, 178.156°W
A magnitude 2.6 earthquake struck 109 km WSW of Adak, Alaska on Wednesday, August 27, 2008, 10:04:24 UTC, at a depth of 70.9 km (intermediate).
- Magnitude
- 2.6
- Minor · ml
- Depth
- 71 km
- Intermediate
- Felt reports
- 0
- Did You Feel It?
- Est. shaking
- —
- No ShakeMap
- PAGER alert
- None
- Not issued
- Tsunami
- No flag
- USGS feed
Outlined circle: this earthquakeDashed circle: 50 km aftershock search area
In context
How big was it, and why here?
Energy released
120 kg of TNT
That is about 1/125,702 of the Hiroshima bomb. A magnitude 5.0 releases about 3,981 times more energy.
Tectonic setting
123 km
from the nearest mapped plate boundary, between the North American and Pacific plates. Earthquakes this far from a boundary happen on faults inside a plate, often less frequently but sometimes strongly.
Depth: intermediate
71 km
Intermediate-depth earthquakes usually break inside a plate that is sinking into the mantle. Shaking spreads over a wide area but is gentler at the epicenter than a shallow quake of the same size.
Did You Feel It?
Where it was felt
No “Did You Feel It?” reports have been published for this event yet. If you felt it, you can add your report on the USGS website.
I felt it — report to USGS ↗USGS PAGER estimate
Who was exposed to shaking
USGS publishes PAGER impact estimates for significant earthquakes, usually within an hour. No PAGER estimate is available for this event.
After the main event
Aftershocks within 50 km
USGS lists 8 M2.5+ earthquakes within 50 km in the following 30 days; the largest was M5.2 on September 15, 2008. Most nearby activity right after a large earthquake is aftershocks, which usually become less frequent over days and weeks.
- 2.6134 km W of Adak, Alaska18y ago · 31 km NW of this epicenter
- 5.2129 km WSW of Adak, Alaska18y ago · 26 km SW of this epicenter
- 2.974 km W of Adak, Alaska18y ago · 42 km NE of this epicenter
- 2.8108 km SW of Adak, Alaska18y ago · 39 km SE of this epicenter
- 3.5128 km WSW of Adak, Alaska18y ago · 37 km S of this epicenter
- 2.8103 km SW of Adak, Alaska18y ago · 47 km SE of this epicenter
- 4.4135 km SW of Adak, Alaska18y ago · 49 km S of this epicenter
- 2.5114 km SW of Adak, Alaska18y ago · 43 km S of this epicenter
Regional history
Past M5+ earthquakes within 300 km
USGS lists 1,060 M5.0+ earthquakes within 300 km before this one (catalog from 1900; older records are less complete). The strongest:
- 8.71965 Western Aleutian Islands (Hawadax/Rat Islands) EarthquakeFebruary 4, 1965 · 220 km W of this epicenter
- 8.61957 Atka, Alaska EarthquakeMarch 9, 1957 · 175 km E of this epicenter
- 8.31906 Western Aleutian Islands (Hawadax/Rat Islands) EarthquakeAugust 17, 1906 · 254 km W of this epicenter
- 8.01986 Atka, Alaska EarthquakeMay 7, 1986 · 234 km E of this epicenter
- 7.977 km WSW of Adak, AlaskaJune 10, 1996 · 36 km E of this epicenter
- 7.8Rat Islands, Aleutian Islands, AlaskaNovember 17, 2003 · 227 km W of this epicenter
- 7.65 km WNW of Adak, AlaskaFebruary 14, 1905 · 105 km E of this epicenter
- 7.4265 km WSW of Adak, AlaskaFebruary 4, 1965 · 157 km W of this epicenter
History · NOAA
Deadliest earthquakes in this area
NOAA’s significant-earthquake database lists 14 damaging, deadly or tsunami-generating earthquakes within 300 km of this epicenter since 1700, which together caused about 2 recorded deaths. The most severe:
- 1957M8.6
Alaska
9 Mar 1957 · 175 km away
2 deathsSevere damage ($5–24M)tsunami
- 1986M8.0
Aleutian Islands: Adak
7 May 1986 · 234 km away · intensity VI
Moderate damage ($1–5M)tsunami
- 1965M8.7
Aleutian Islands: Rat Islands
4 Feb 1965 · 220 km away · intensity VI
Under $1 million damagetsunami
- 1906M8.3
Aleutian Islands: Rat Islands
17 Aug 1906 · 254 km away
- 1905M7.9
Andreanof Islands
14 Feb 1905 · 101 km away
- 1996M7.9
Andreanof Islands
10 Jun 1996 · 36 km away · intensity VI
tsunami
NOAA NCEI Global Significant Earthquake Database. Historical figures are estimates; older records are incomplete.