Reviewed by USGSGuam24y ago
M7.1 earthquake 20 km SSW of Merizo Village, Guam
Friday, April 26, 2002, 16:06:07 UTC · 13.088°N, 144.619°E
A magnitude 7.1 earthquake struck 20 km SSW of Merizo Village, Guam on Friday, April 26, 2002, 16:06:07 UTC, at a depth of 85.7 km (intermediate). It is the strongest earthquake within 300 km since an M7.8 on August 8, 1993.
- Magnitude
- 7.1
- Major · mwc
- Depth
- 86 km
- Intermediate
- Felt reports
- 0
- Did You Feel It?
- Est. shaking
- VII
- Very strong (ShakeMap)
- PAGER alert
- None
- Not issued
- Tsunami
- No flag
- USGS feed
Outlined circle: this earthquakeDashed circle: 200 km aftershock search areaColoured lines: estimated shaking intensity (USGS ShakeMap)
In context
How big was it, and why here?
Energy released
674 kilotons of TNT
That is about 45 times the Hiroshima bomb. It released about 1,413 times the energy of a magnitude 5.0.
Tectonic setting
93 km
from the nearest mapped plate boundary, between the Philippine Sea and Mariana plates. Earthquakes cluster along boundaries like this one, where plates collide, pull apart or slide past each other.
Depth: intermediate
86 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 200 km
USGS lists 5 M2.5+ earthquakes within 200 km in the following 30 days; the largest was M5.4 on May 21, 2002. Most nearby activity right after a large earthquake is aftershocks, which usually become less frequent over days and weeks.
- 4.0207 km SW of Merizo Village, Guam24y ago · 190 km SW of this epicenter
- 5.4Rota region, Northern Mariana Islands24y ago · 114 km N of this epicenter
- 4.2133 km SSW of Merizo Village, Guam24y ago · 114 km SW of this epicenter
- 4.440 km SE of Inarajan Village, Guam24y ago · 40 km E of this epicenter
- 4.131 km SSE of Inarajan Village, Guam24y ago · 24 km E of this epicenter
Regional history
Past M5+ earthquakes within 300 km
USGS lists 487 M5.0+ earthquakes within 300 km before this one (catalog from 1900; older records are less complete). The strongest:
- 7.832 km S of Inarajan Village, GuamAugust 8, 1993 · 23 km SE of this epicenter
- 7.2265 km S of Merizo Village, GuamJanuary 28, 1931 · 247 km S of this epicenter
- 7.1261 km S of Merizo Village, GuamMay 9, 1917 · 243 km S of this epicenter
- 7.0176 km ESE of San Jose Village, Northern Mariana IslandsMay 18, 1913 · 297 km NE of this epicenter
- 7.098 km SSE of Inarajan Village, GuamDecember 9, 1909 · 84 km SE of this epicenter
- 7.032 km NNE of Yigo Village, GuamOctober 26, 1912 · 89 km NE of this epicenter
- 7.069 km SSE of Inarajan Village, GuamOctober 12, 2001 · 59 km SE of this epicenter
- 6.5276 km SW of Merizo Village, GuamOctober 23, 1971 · 261 km SW of this epicenter
History · NOAA
Deadliest earthquakes in this area
NOAA’s significant-earthquake database lists 13 damaging, deadly or tsunami-generating earthquakes within 300 km of this epicenter since 1700. The most severe:
- 1993M7.8
Tuman Bay, Apra Harbor
8 Aug 1993 · 23 km away · intensity IX
$250 million damagetsunami
- 1849M7.5
Guam
25 Jan 1849 · 175 km away · intensity IX
Severe damage ($5–24M)tsunami
- 1909M8.0
Guam
9 Dec 1909 · 77 km away · intensity VIII
Moderate damage ($1–5M)tsunami
- 1892M7.5
Guam
16 May 1892 · 175 km away · intensity VIII
Moderate damage ($1–5M)tsunami
- 2001M7.0
Guam
12 Oct 2001 · 59 km away · intensity VIII
Moderate damage ($1–5M)
- 1825
Ladrones Island
Apr 1825 · 175 km away · intensity VIII
Moderate damage ($1–5M)tsunami
NOAA NCEI Global Significant Earthquake Database. Historical figures are estimates; older records are incomplete.