Reviewed by USGSGreece22y ago
M3.0 earthquake 4 km W of Río, Greece
Sunday, June 20, 2004, 23:53:21 UTC · 38.290°N, 21.730°E
A magnitude 3.0 earthquake struck 4 km W of Río, Greece on Sunday, June 20, 2004, 23:53:21 UTC, at a depth of 21.0 km (shallow).
- Magnitude
- 3.0
- Minor · md
- Depth
- 21 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
477 kg of TNT
That is about 1/31,575 of the Hiroshima bomb. A magnitude 5.0 releases about 1,000 times more energy.
Tectonic setting
13 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
21 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 15 M2.5+ earthquakes within 50 km in the following 30 days; the largest was M3.6 on July 14, 2004. Most nearby activity right after a large earthquake is aftershocks, which usually become less frequent over days and weeks.
- 2.819 km SSE of Chalandrítsa, Greece22y ago · 40 km S of this epicenter
- 2.816 km N of Goúmero, Greece22y ago · 43 km S of this epicenter
- 2.97 km ENE of Náfpaktos, Greece22y ago · 21 km NE of this epicenter
- 3.25 km NE of Rododáfni, Greece22y ago · 31 km E of this epicenter
- 3.622 km NE of Lálas, Greece22y ago · 48 km S of this epicenter
- 2.68 km WSW of Mesolóngi, Greece22y ago · 34 km W of this epicenter
- 2.82 km ESE of Gavaloú, Greece22y ago · 30 km NW of this epicenter
- 3.214 km E of Chalandrítsa, Greece22y ago · 27 km SE of this epicenter
Regional history
Past M5+ earthquakes within 300 km
USGS lists 528 M5.0+ earthquakes within 300 km before this one (catalog from 1900; older records are less complete). The strongest:
- 7.9Southern GreeceAugust 11, 1903 · 278 km SE of this epicenter
- 7.34 km WNW of Koróni, GreeceOctober 6, 1947 · 166 km S of this epicenter
- 7.026 km SW of Lixoúri, GreeceJanuary 17, 1983 · 135 km W of this epicenter
- 6.97 km NNE of Ágios Nikólaos, GreeceSeptember 26, 1932 · 284 km NE of this epicenter
- 6.815 km ENE of Póros, GreeceAugust 12, 1953 · 70 km W of this epicenter
- 6.86 km SW of Galaxídhion, GreeceMarch 31, 1965 · 52 km E of this epicenter
- 6.828 km SSE of Karyes, GreeceJanuary 18, 1982 · 294 km NE of this epicenter
- 6.7Ionian SeaNovember 15, 1959 · 113 km SW of this epicenter
History · NOAA
Deadliest earthquakes in this area
NOAA’s significant-earthquake database lists 160 damaging, deadly or tsunami-generating earthquakes within 300 km of this epicenter since 1700, which together caused about 5,835 recorded deaths. The most severe:
- 1750
Morea,Cerigo
7 Jun 1750 · 258 km away · intensity X
2,000 deaths
- 1953M7.2
Lixouri-Argostoli (Kephallenia)
12 Aug 1953 · 81 km away · intensity X
476 deaths$100 million damagetsunami
- 1820M6.9
Zakinthos (Zante)
29 Dec 1820 · 73 km away · intensity X
388 deathsSevere damage ($5–24M)tsunami
- 1886M6.8
Triphylie (Peleponese), Philiatra
27 Aug 1886 · 132 km away · intensity X
326 deathsSevere damage ($5–24M)tsunami
- 1767M6.7
Kefalonia
11 Jul 1767 · 111 km away · intensity X
303 deathsSevere damage ($5–24M)
- 1894M6.7
Locride, Malesina-Martinon (Lokris)
20 Apr 1894 · 133 km away · intensity X
255 deathsSevere damage ($5–24M)
NOAA NCEI Global Significant Earthquake Database. Historical figures are estimates; older records are incomplete.