The USGS has confirmed a magnitude 4.5 earthquake with its epicentre 60 km WNW of Colchani, Bolivia, occurring at 06:54 UTC on Tuesday, October 6, 2026. The event's focal depth — 191.7 km — is a key factor in understanding how this earthquake was experienced at the surface.
Why Depth Matters
With a focal depth of 191.7 km, this earthquake falls into the intermediate depth category (70–300 km). At this depth, seismic waves travel further before reaching the surface, spreading energy over a wider area. While shaking intensity at the epicentre is somewhat reduced compared to a shallow event of equal magnitude, an intermediate earthquake can be felt across a much larger region.
Depth is one of the most critical but least discussed parameters of any earthquake. Two earthquakes of identical magnitude can have dramatically different surface effects depending on how deep the rupture originates. Significant damage can occur to vulnerable structures — particularly unreinforced masonry, old adobe buildings, and poorly maintained older construction. Well-engineered modern buildings are designed to withstand this level of shaking with minimal structural impact, though contents may shift and non-structural elements (ceilings, partitions) can be damaged.
Magnitude 4.5: What the Science Says
On the moment magnitude scale, 4.5 represents a moderate earthquake. Moderate earthquakes are felt by virtually everyone near the epicentre. Strong shaking lasting 10–30 seconds can topple unsecured items, crack plaster, and cause poorly anchored objects to fall. Aftershocks are common following moderate events.
A magnitude 4.5 earthquake releases approximately roughly 500 tonnes of TNT of energy. For comparison, this exceeds the energy released by most conventional explosive events and is sufficient to shift tectonic stress in measurable ways across a wide region.
Tectonic Setting
Chile runs along the subduction boundary where the Nazca Plate dives beneath the South American Plate — one of the most seismically active convergent boundaries on the planet. This setting has produced the largest instrumentally recorded earthquake in history.
This region's seismic history is an important reminder that earthquake risk is a long-term reality that requires sustained preparedness. Chile holds the record for the strongest earthquake ever measured: the 1960 Valdivia earthquake at magnitude 9.5. More recently, the 2010 Maule earthquake (M8.8) and its associated tsunami caused widespread damage. Chileans have developed strong earthquake-preparedness culture over generations.
Practical Safety Information
Regardless of the earthquake's depth or magnitude, standard safety procedures apply. Keep an earthquake emergency kit accessible at home. It should include at least 72 hours of water (4 litres per person per day), non-perishable food, a first aid kit, torch, battery-powered radio, copies of important documents, and essential medications. Reviewing and restocking this kit annually is strongly recommended.
Agree on an out-of-area contact that family members can reach if local communications are disrupted. Identify two meeting points: one near your home and one further away. Practise earthquake drills, especially with children and elderly household members.
SHOA (Servicio Hidrográfico y Oceanográfico de la Armada) manages tsunami warnings for Chile, while SENAPRED coordinates national disaster response. Evacuation routes and tsunami inundation maps are posted in most coastal communities.
Track This Event
All seismic data for this event is being updated in real time as the USGS refines its measurements. Initial magnitude and depth estimates are sometimes revised as more seismograph stations report in — a process that typically completes within hours of the event. Follow updates on our live earthquake map and consider submitting a felt report if you experienced this earthquake directly.
The Science of Seismic Monitoring
Modern earthquake detection relies on a global network of seismographs — sensitive instruments that record ground motion in all three dimensions. When an earthquake occurs, the P-waves (primary, compressional waves) arrive first, followed by the slower S-waves (secondary, shear waves), and finally the surface waves that cause the most felt shaking. By comparing arrival times at multiple stations, scientists can triangulate the earthquake's location and calculate its magnitude within minutes of the event.
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