Live Seismic Telemetry • REVIEWED Event

Micro 2.8 Earthquake – Bosnia And Herzegovina

9 days agoThursday, September 10, 2026 at 12:15:35 PM UTC

A micro magnitude 2.8 earthquake struck near Bosnia And Herzegovina on Thursday, September 10, 2026 at 12:15:35 PM UTC. This shallow crustal event (5.2 km depth) released energy equivalent to approximately 239 kg of TNT. Here is the verified EMSC telemetry, live epicenter map, and ground shaking assessment.

2.8MAG
Micro EarthquakeShallow Crustal Event
Bosnia And HerzegovinaBosnia And Herzegovina

Seismic Telemetry Specifications

Magnitude

2.8M

Micro Seismic Class

Focal Depth

5.2km

Crustal Layer

Epicenter

43.978° N, 18.212° E

GPS Coordinates

Energy Yield

239 kg

TNT Equivalent Power

Network Source

EMSC

USGS Real-time Feed

Epicenter Location & Tectonic Fault Map

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Is This Earthquake Dangerous?

A magnitude 2.8 event is classified as a micro earthquake. Micro-earthquakes are rarely felt by humans and are typically recorded only by sensitive seismometers.

Estimated Shaking Radius< 10 km
Potential Damage ZoneNone
Focal Depth EffectHigh Surface Energy (Crustal)

Estimated Shaking Across Nearby Communities

The epicenter occurred in a remote or offshore marine sector with no major population centers situated within the primary ground shaking perimeter.

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What Does Magnitude 2.8 Mean?

Earthquake strength is measured on a logarithmic scale. Compare this event with the full seismic scale:

1.0 – 2.9Micro
This Event
3.0 – 3.9Minor
4.0 – 4.9Light
5.0 – 5.9Moderate
6.0 – 6.9Strong
7.0 – 7.9Major
8.0+Great

Logarithmic Energy Multiplier

Because seismic scales are logarithmic, each whole integer increase represents:

10× Ground Motion Amplitude
The seismograph wave amplitude jumps tenfold for every 1.0 magnitude step.
~31.6× Radiated Kinetic Energy
Total energy release multiplies exponentially (101.5 &approx; 31.62 times per unit).

Why Did This Earthquake Happen?

Bosnia And Herzegovina's seismicity is fundamentally governed by its tectonic setting: Compressional deformation and thrust faulting across the Dinaric Alps caused by the northward push of the Adriatic microplate. Major regional fault structures include Banja Luka Fault Zone, Herzegovinian Thrust System.

Originating at a depth of 5.2 km (Earth's Crust (0–70 km)), this rupture occurred occurred within the brittle upper crust. shallow earthquakes produce the highest peak ground acceleration and the sharpest surface shaking.

Aftershock Outlook & Secondary Tremors

Micro-tremors and minor events of this scale are part of ongoing background tectonic relaxation. While isolated micro-aftershocks may occur, the likelihood of a damaging secondary event remains statistically low under normal seismic conditions.

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Earthquake Safety Action Plan

Complete Safety Guide →
During the Shaking
  • Drop, Cover, and Hold On: Take cover beneath a sturdy table or desk.
  • Stay indoors away from exterior glass windows and heavy unanchored fixtures.
  • If outdoors, move into an open area away from power lines and building facades.
Immediately After
  • Inspect utilities for damaged gas lines, water leaks, or electrical hazards.
  • Expect Aftershocks: Secondary tremors frequently strike after significant events.
  • Avoid damaged structures and listen to official emergency broadcasts.
Preparation & Kits
  • Maintain a 72-hour emergency go-bag with water, food, and first aid.
  • Anchor heavy furniture, water heaters, and appliances to structural studs.
  • Establish a family emergency communication protocol and meeting point.

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