Reviewed by USGSGreece31y ago
M3.1 earthquake 6 km W of Aianí, Greece
Tuesday, August 8, 1995, 22:43:43 UTC · 40.157°N, 21.749°E
A magnitude 3.1 earthquake struck 6 km W of Aianí, Greece on Tuesday, August 8, 1995, 22:43:43 UTC, at a depth of 10.0 km (shallow).
- Magnitude
- 3.1
- Minor · md
- Depth
- 10 km
- Shallow
- 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
674 kg of TNT
That is about 1/22,353 of the Hiroshima bomb. A magnitude 5.0 releases about 708 times more energy.
Tectonic setting
174 km
from the nearest mapped plate boundary, between the Aegean Sea and Eurasian plates. Earthquakes this far from a boundary happen on faults inside a plate, often less frequently but sometimes strongly.
Depth: shallow
10 km
Shallow earthquakes (under 70 km) produce the strongest surface shaking for their size, so they are the ones most likely to cause damage near the epicenter.
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 33 M2.5+ earthquakes within 50 km in the following 30 days; the largest was M4.4 on August 20, 1995. Most nearby activity right after a large earthquake is aftershocks, which usually become less frequent over days and weeks.
- 2.910 km SW of Aianí, Greece31y ago · 8 km S of this epicenter
- 2.58 km E of Siátista, Greece31y ago · 16 km NW of this epicenter
- 2.911 km ESE of Grevená, Greece31y ago · 21 km SW of this epicenter
- 2.85 km ESE of Deskáti, Greece31y ago · 29 km S of this epicenter
- 4.07 km SW of Aianí, Greece31y ago · 4 km S of this epicenter
- 3.013 km SE of Grevená, Greece31y ago · 24 km SW of this epicenter
- 3.116 km ENE of Grevená, Greece31y ago · 12 km W of this epicenter
- 2.83 km W of Aianí, Greece31y ago · 3 km E of this epicenter
Regional history
Past M5+ earthquakes within 300 km
USGS lists 495 M5.0+ earthquakes within 300 km before this one (catalog from 1900; older records are less complete). The strongest:
- 7.2Aegean SeaNovember 8, 1905 · 245 km E of this epicenter
- 7.07 km SE of Stara Kresna, BulgariaApril 4, 1904 · 218 km NE of this epicenter
- 7.026 km SW of Lixoúri, GreeceJanuary 17, 1983 · 271 km SW of this epicenter
- 7.055 km S of Mýrina, GreeceFebruary 19, 1968 · 289 km E of this epicenter
- 6.97 km NNE of Ágios Nikólaos, GreeceSeptember 26, 1932 · 170 km E of this epicenter
- 6.86 km W of Stara Kresna, BulgariaApril 4, 1904 · 216 km NE of this epicenter
- 6.815 km ENE of Póros, GreeceAugust 12, 1953 · 230 km S of this epicenter
- 6.86 km SW of Galaxídhion, GreeceMarch 31, 1965 · 208 km S of this epicenter
History · NOAA
Deadliest earthquakes in this area
NOAA’s significant-earthquake database lists 177 damaging, deadly or tsunami-generating earthquakes within 300 km of this epicenter since 1700, which together caused about 7,318 recorded deaths. The most severe:
- 1851M6.6
Vlore (Valona),Berat; Turkey
12 Oct 1851 · 178 km away · intensity XI
2,000 deathsExtreme damage ($25M+)tsunami
- 1963M6.0
Macedonia: Skopje
26 Jul 1963 · 219 km away · intensity X
1,070 deaths$1.0 billion damage
- 1953M7.2
Lixouri-Argostoli (Kephallenia)
12 Aug 1953 · 222 km away · intensity X
476 deaths$100 million damagetsunami
- 1851
Berat
17 Oct 1851 · 178 km away · intensity X
400 deathsSevere damage ($5–24M)
- 1820M6.9
Zakinthos (Zante)
29 Dec 1820 · 271 km away · intensity X
388 deathsSevere damage ($5–24M)tsunami
- 1767M6.7
Kefalonia
11 Jul 1767 · 237 km away · intensity X
303 deathsSevere damage ($5–24M)
NOAA NCEI Global Significant Earthquake Database. Historical figures are estimates; older records are incomplete.