Latest magnitude 4 and higher event index
Recent moderate events are organized for rapid review. Confirm exact origin time, coordinates, depth and magnitude with the reporting seismic agency.
A focused archive for moderate seismic events worldwide, with clear reminders that magnitude alone does not determine shaking, damage or local risk.
This index presents representative archive summaries reviewed during the last 18 months. Locations and values on a live seismic feed may change after agency analysis.
Recent moderate events are organized for rapid review. Confirm exact origin time, coordinates, depth and magnitude with the reporting seismic agency.
Shallow depth and proximity to communities can make an event more noticeable, while local soil and building conditions influence reported intensity.
An offshore location does not by itself establish tsunami danger. Follow official warning centers and local emergency guidance rather than drawing conclusions from magnitude alone.
Aftershocks can continue as a fault zone adjusts. Their frequency generally declines, but individual events remain possible and early classifications may be revised.
Magnitude measures the earthquake at its source. Intensity describes effects at a particular place, so reports can vary considerably across the affected region.
Initial solutions rely on the first available signals. Additional stations and analyst review can improve the estimated hypocenter and alter the published values.
Magnitude 4 events can occur near plate boundaries or within plates. Each report needs geographic and tectonic context before broader meaning is assigned.
Past earthquake records help describe regional seismicity, but they do not identify the exact date, location and magnitude of a future event.
Early earthquake summaries are useful, but no single field provides a complete account of what happened on the ground.
A logarithmic measurement of earthquake size. A small numerical change represents a substantial change in released energy.
The estimated distance below the surface. Shallow events can produce stronger nearby shaking, though other factors remain important.
A description of observed shaking and effects at a location. It varies with distance, ground conditions and the built environment.

Earthquake Report treats the first automatic solution as a starting point rather than a final conclusion.
Impact cannot be determined from magnitude alone. Depth, distance, local geology, building vulnerability and secondary hazards all affect consequences.
An event may be deep, remote or offshore. Human perception also varies with ground conditions, distance, building height and ambient activity.
Automatic estimates use limited early data. Agencies refine the solution as more seismic stations and analyst reviews become available.
Magnitude alone is not enough to assess tsunami risk. Use official tsunami-warning centers and local evacuation instructions after strong or long coastal shaking.
No. Seismologists consider timing, location and the relationship to the earlier rupture. Event labels may change as a sequence is analyzed.
A cluster does not provide an exact prediction. Seismicity is monitored probabilistically, and no reliable method specifies a future event’s precise time, place and magnitude.
The magnitude 4+ category helps readers find moderate earthquake entries without implying that every event has the same effect. Earthquake Report combines archive organization with plain-language explanations of preliminary seismic data.
For corrections, accessibility feedback or archive questions, email info@earthquakereport.com-html.com.
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