| 1974 Lesser Antilles earthquake | |
| Timestamp: | 1974-10-08 09:50:58 |
| Isc-Event: | 736214 |
| Anss-Url: | iscgem736214 |
| Local-Time: | 05:50:58 |
| Magnitude: | 6.9 |
| Depth: | 35.20NaN0 |
| Location: | 17.3°N -62°W |
| Type: | Normal |
| Damage: | Moderate |
| Casualties: | 4 injured |
The 1974 Lesser Antilles earthquake occurred at on October 8 with a moment magnitude of 6.9 and a maximum Mercalli intensity of VIII (Severe). Four people were injured in what the United States' National Geophysical Data Center called a moderately destructive event.
See also: Volcanic arc.
While the northern and southern boundary of the Caribbean plate are complex and diffuse, with zones of seismicity stretching several hundred kilometers across, the eastern boundary is that of the Lesser Antilles subduction zone. This 850km (530miles) long subduction zone lacks a uniform curve and has an average dip of 50–60°. The largest known earthquake on the plate interface was a M7.5–8.0 event in 1843, but it did not generate a large tsunami. In opposition, the three largest events between 1950 and 1978 were intraplate normal faulting events.
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