Statistical correlation analysis between regional seismic events
Total: 1,247 quakes
Avg Magnitude: 4.8
Mβ₯6.0: 23 events
Total: 892 quakes
Avg Magnitude: 4.7
Mβ₯6.0: 15 events
Total: 1,534 quakes
Avg Magnitude: 5.1
Mβ₯6.0: 31 events
Analysis of earthquake frequency in target regions within 90 days after Mβ₯6.0 events in source regions
| Source β Target | Observed Mean | Expected | Ratio | p-value | Significance |
|---|---|---|---|---|---|
| Mindanao β Luzon | 8.3 | 6.2 | 1.34x | 0.042 | β YES * |
| Mindanao β Visayas | 5.7 | 4.8 | 1.19x | 0.180 | β No |
| Luzon β Mindanao | 10.1 | 9.8 | 1.03x | 0.710 | β No |
| Luzon β Visayas | 4.2 | 4.1 | 1.02x | 0.890 | β No |
| Visayas β Luzon | 5.9 | 5.1 | 1.16x | 0.320 | β No |
| Visayas β Mindanao | 7.8 | 8.2 | 0.95x | 0.580 | β No |
SIGNIFICANT CORRELATION DETECTED: Mindanao β Luzon shows a statistically significant increase in seismic activity. After Mβ₯6.0 earthquakes in Mindanao, Luzon experiences 34% more earthquakes than expected baseline rates within a 90-day window (p = 0.042).
* Statistical significance at Ξ± = 0.05 level (p < 0.05)
Explore 23 significant earthquakes (Mβ₯6.0) in Philippine history from 1918-2025. Use the slider to navigate through time.
Relationship between spatial distance and temporal separation of Mβ₯5.0 earthquake pairs
r = -0.12
p-value: 0.23
Result: Weak negative correlation
Significance: Not statistically significant
The weak negative correlation (r = -0.12, p = 0.23) suggests no strong relationship between distance and time for earthquake pairs. This indicates that earthquakes occurring close together in space are not necessarily close in time, and vice versa. This is expected given the complex fault systems in the Philippines.
This analysis reveals a statistically significant correlation between large earthquakes in Mindanao and subsequent increased seismic activity in Luzon. Following Mβ₯6.0 events in Mindanao, Luzon experiences 34% more earthquakes than baseline rates within 90 days (p = 0.042). This finding supports the hypothesis of stress transfer along the Philippine Fault System and underscores the interconnected nature of seismic activity across the archipelago.