Reviewed by USGSGreece22y ago
M2.7 earthquake 10 km S of Mégara, Greece
Tuesday, August 24, 2004, 19:00:17 UTC · 37.900°N, 23.330°E
A magnitude 2.7 earthquake struck 10 km S of Mégara, Greece on Tuesday, August 24, 2004, 19:00:17 UTC, at a depth of 25.0 km (shallow).
- Magnitude
- 2.7
- Minor · ml
- Depth
- 25 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
169 kg of TNT
That is about 1/88,990 of the Hiroshima bomb. A magnitude 5.0 releases about 2,818 times more energy.
Tectonic setting
67 km
from the nearest mapped plate boundary, between the Aegean Sea and Eurasian plates. Earthquakes cluster along boundaries like this one, where plates collide, pull apart or slide past each other.
Depth: shallow
25 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 13 M2.5+ earthquakes within 50 km in the following 30 days; the largest was M2.9 on September 3, 2004. Most nearby activity right after a large earthquake is aftershocks, which usually become less frequent over days and weeks.
- 2.58 km SW of Kaparéllion, Greece22y ago · 36 km NW of this epicenter
- 2.63 km SSW of Mándra, Greece22y ago · 21 km NE of this epicenter
- 2.66 km S of Sofikón, Greece22y ago · 30 km SW of this epicenter
- 2.67 km N of Kinéta, Greece22y ago · 18 km NW of this epicenter
- 2.59 km NNW of Póros, Greece22y ago · 37 km S of this epicenter
- 2.86 km NW of Galatás, Greece22y ago · 41 km S of this epicenter
- 2.57 km E of Áyios Adhrianós, Greece22y ago · 48 km SW of this epicenter
- 2.62 km SW of Fylí, Greece22y ago · 35 km NE of this epicenter
Regional history
Past M5+ earthquakes within 300 km
USGS lists 532 M5.0+ earthquakes within 300 km before this one (catalog from 1900; older records are less complete). The strongest:
- 7.9Southern GreeceAugust 11, 1903 · 213 km S of this epicenter
- 7.719 km SSE of Amorgós, GreeceJuly 9, 1956 · 270 km SE of this epicenter
- 7.34 km WNW of Koróni, GreeceOctober 6, 1947 · 174 km SW of this epicenter
- 7.2Aegean SeaNovember 8, 1905 · 268 km NE of this epicenter
- 7.261 km W of Eresós, GreeceDecember 19, 1981 · 222 km NE of this epicenter
- 7.29 km NNW of Karaburun, TurkeyJuly 23, 1949 · 289 km E of this epicenter
- 7.026 km SW of Lixoúri, GreeceJanuary 17, 1983 · 272 km W of this epicenter
- 7.055 km S of Mýrina, GreeceFebruary 19, 1968 · 218 km NE of this epicenter
History · NOAA
Deadliest earthquakes in this area
NOAA’s significant-earthquake database lists 157 damaging, deadly or tsunami-generating earthquakes within 300 km of this epicenter since 1700, which together caused about 28,367 recorded deaths. The most severe:
- 1883M7.3
Ayvalik, Izmir, Cesme
15 Oct 1883 · 255 km away · intensity X
15,000 deathsExtreme damage ($25M+)
- 1881M7.3
Khios; Turkey: Cesme
3 Apr 1881 · 259 km away · intensity XI
7,866 deathsExtreme damage ($25M+)tsunami
- 1750
Morea,Cerigo
7 Jun 1750 · 191 km away · intensity X
2,000 deaths
- 1953M7.2
Lixouri-Argostoli (Kephallenia)
12 Aug 1953 · 226 km away · intensity X
476 deaths$100 million damagetsunami
- 1820M6.9
Zakinthos (Zante)
29 Dec 1820 · 183 km away · intensity X
388 deathsSevere damage ($5–24M)tsunami
- 1886M6.8
Triphylie (Peleponese), Philiatra
27 Aug 1886 · 169 km away · intensity X
326 deathsSevere damage ($5–24M)tsunami
NOAA NCEI Global Significant Earthquake Database. Historical figures are estimates; older records are incomplete.