Okinawa Plate
| Okinawa Plate | |
|---|---|
| 1Relative to the African Plate |
The Okinawa Plate, or Okinawa Platelet, is a minor continental
Kyūshū.[1][2] The Okinawa Plate hosts typical earthquakes, like the 1911 Kikai Island earthquake, and various types of slow earthquakes, including low frequency earthquakes,[3] very low frequency earthquakes,[4] tremor,[5] and slow slip events.[6]
Boundaries
The eastern side of the Okinawa Plate forms a
Amur Plate
.
References
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