SeismoScope PH

Data source: SQL Server

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Magnitude trend (map window)

Seismic activity · past 24 hours

25 Feb 2026 22:10 – 26 Feb 2026 22:10 (Asia/Manila)

Magnitude trend (3D window)

Depth distribution (3D)

25 Feb 2026 22:10 – 26 Feb 2026 22:10 (Asia/Manila)

Weekly Seismic Overview

Seismic Activity Report: Philippines (Last 7 Days)

Overview:

This report summarizes the seismic activity in the Philippines over the past week, covering a total of 252 recorded events. The data indicates a diverse range of magnitudes and depths, with notable clusters primarily in the Mindanao and Visayas regions.

Magnitude Trends:

The recorded magnitudes ranged from 1.0 to 4.7, with the majority of events falling between 1.0 and 3.0. The highest magnitude event was a 4.7 quake on February 22, 2026, located 34 km north of Dalupiri Island in Cagayan. This event was significant, indicating a potential shift in tectonic activity in the region.

Cluster Analysis:

1. Mindanao Region:

- Mindanao exhibited a high frequency of seismic events, particularly in the Davao Occidental and Davao Oriental provinces. The most significant clusters occurred around February 21 and 22, with multiple events recorded in quick succession. For instance, on February 21, there were three notable events: a 3.5 magnitude quake at 21 km depth, a 3.4 magnitude quake at 16 km depth, and a 3.3 magnitude quake at 5 km depth.

- The area near Sarangani Island also showed increased activity, with several events of magnitudes between 2.0 and 3.1 occurring within a short time frame.

2. Visayas Region:

- The Visayas region recorded a series of moderate earthquakes, particularly around Negros Occidental and Eastern Samar. The highest recorded magnitude in this region was 3.3 on February 23, near San Policarpo, Eastern Samar.

- A notable cluster was observed on February 23, with several events around 2.5 to 2.9 magnitudes occurring within hours of each other, indicating a potential fault line activity.

3. Luzon Region:

- Luzon experienced fewer significant events, but notable occurrences included a 4.3 magnitude quake on February 22, located 384 km south-east of Balut Island. This event, while distant from populated areas, highlights the ongoing tectonic activity in the region.

Depth Analysis:

The depth of the recorded earthquakes varied significantly, with most events occurring at shallow depths of less than 30 km. The shallow depth of many of these quakes, particularly in Mindanao, suggests a close relationship with tectonic plate boundaries and fault lines. Notably, the 4.7 magnitude quake on February 22 had a depth of 18 km, which is consistent with the shallow nature of seismic activity in this region.

Trench Involvement:

The Philippines is situated along the Pacific Ring of Fire, characterized by numerous tectonic trenches and fault lines. The activity observed in Mindanao aligns with the presence of the Philippine Trench, which is known for its seismic activity. The clustering of events in this region indicates ongoing tectonic stress and potential for larger seismic events.

Conclusion:

The seismic activity in the Philippines over the past week reflects a dynamic geological environment, particularly in Mindanao and the Visayas. The presence of multiple clusters, varying magnitudes, and shallow depths underscores the importance of continuous monitoring. Further analysis is recommended to assess potential risks and prepare for future seismic events.

AI-generated report created on 2026-02-26T20:00:31.511066+08:00 (gpt-4o-mini).

Magnitude & Slip Summary

Latest AnalysisMath snapshot · 2026-02-26T00:30:01.137841+00:00 UTC · Window 30 days

Events analysed
1781
Mean magnitude
2.34
Strongest magnitude
5.90
Events M ≥ 4.0
80
Events M ≥ 5.0
15
Gutenberg–Richter b-value
0.69
Total seismic moment
3.91 ×10¹⁸ Nm
Radiated energy
219813.80 GJ
Equivalent slip
1.55 cm
Slip rate (approx.)
0.53 mm/day
Moment rate
0.13 ×10¹⁸ Nm/day
Energy proxy
195445.18 GJ
Data coverage
29.3 days

Slip estimates assume a 120 × 70 km fault and shear modulus of 30 GPa.

Daily earthquakes (30 days)

Daily seismic moment release

7-day Seismic Heat Map

Trench Contribution

The pie chart highlights which trenches account for the bulk of recent seismic activity.

Depth Distribution Histogram

Depth bins highlight how seismicity concentrates from shallow crustal levels to deep subduction zones.

Philippines 3D Cross-Section

The analysis of fracture clusters beneath the Philippines reveals critical insights into the region's tectonic dynamics and associated seismic hazards. Our examination here, based on event clusters, centroids, and depth ranges, identifies key characteristics of nine clusters across the area, each with distinct implications for seismic activity and hazard evaluation.

Cluster Overview:

Centroid located at 157.7 km along-strike and -40.6 km across-strike. This cluster is the most active, indicating a significant concentration of seismicity. Geographically, it aligns closely with the Manila Trench, suggesting it may be influenced by subduction processes.

Positioned at approximately 392.7 km along-strike, this cluster is situated in the eastern region near the Philippine Trench. The deeper average depth (26.3 km) suggests a relationship with the trench's activity and potential for larger subduction zone earthquakes.

Cluster 3, at -171.4 km along-strike (near the Mindanao region), shows a range of depths (2.0–101.0 km) indicating more complex tectonic interactions. In contrast, Cluster 4, located at -193.9 km, has a similar depth range (1.0–59.0 km) but lacks significant seismicity, perhaps indicating a less active tectonic environment.

These are less active, with clusters occurring at spatially more distant positions from major trenches. Clusters 5 (-107.2 km) and 6 (-191.9 km) have depths of about 6.0–30.0 km and 7.0–37.0 km, respectively, yet they may represent evolving stress fields rather than stable fault lines.

Clusters 7 (273.1 km) and 9 (-279.5 km) demonstrate mild seismicity, with narrower depth ranges, possibly indicating minor tectonic adjustments. For instance, Cluster 9’s location in a complex region suggests intricate interactions between nearby geological formations. Cluster 8 is very localized and characterized by shallow depths (1.0–33.0 km), indicating potentially minor, shallow crustal faults.

With shallow depths, Cluster 11 (266.4 km) shows less seismic activity and could suggest a stable area or insufficient data coverage.

Tectonic Implications:

The presence of these clusters indicates that the Philippines is situated at a critical convergent boundary with the Eurasian Plate and the Philippine Sea Plate. The more active clusters (1 and 2) align with significant geological features that drive earthquake generation, while the less active clusters can indicate areas of stress accumulation or tectonic quiescence.

Hazard Implications:

The primary risk from the identified clusters, particularly from Clusters 1 and 2, is the likelihood of significant seismic events affecting densely populated regions. As such, a better understanding of these clusters can aid in informing earthquake preparedness and risk mitigation strategies.

In conclusion, the analysis provided here illustrates not only the seismicity of the Philippines but the importance of monitoring these clusters to improve hazard assessments and readiness. This understanding can facilitate better urban planning and disaster response strategies in an earthquake-prone region.

This analysis was generated by the AI model GPT-4.

  • Cluster 1 (3012 events, depth range 1.0–51.0 km):
  • Cluster 2 (2040 events, depth range 1.0–79.0 km):
  • Clusters 3 and 4 (196 and 95 events, respectively):
  • Clusters 5 and 6 (27 and 18 events):
  • Clusters 7, 8, and 9 (58, 15, and 70 events):
  • Cluster 11 (25 events):

Seismic Activity Forecast (24 hours)

Mappa di previsione sismica nelle Filippine
Ultimo aggiornamento blob: 2026-02-26T12:00:06+00:00 · 450.0 KB

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EarthquakesPH · 11629 records

2025-10-01T08:01:00+08:00 – 2026-02-27T05:20:00+08:00

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Data source: DOST-PHIVOLCS (Department of Science and Technology – Philippine Institute of Volcanology and Seismology).