Strong correlation of major earthquakes with solid-earth tides in part of the eastern United States
January 1, 1989
East of the eastern American continental divide and south of fat 42.5°N, moderate to large historic earthquakes correlate strongly with times of high and low solid-earth tides. This effect is most pronounced when solar declination lies between 17°N and 17°S. Significant correlations also exist between major earthquakes, time of day, lunar declinations, and lunar phase.
Citation Information
| Publication Year | 1989 |
|---|---|
| Title | Strong correlation of major earthquakes with solid-earth tides in part of the eastern United States |
| DOI | 10.1130/0091-7613(1989)017<0661:SCOMEW>2.3.CO;2 |
| Authors | R. E. Weems, W.H. Perry |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Geology |
| Index ID | 70015656 |
| Record Source | USGS Publications Warehouse |