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What caused the Panama earthquake and why was a tsunami alert issued?

The sources don't yet document a specific Panama earthquake or its tsunami alert, but they do explain the region's tectonic setting and warning-system gaps.

Updated 1 hour ago5 min readVersion 2
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Covers: This page explains the tectonic setting of Panama and the earthquake that prompted a tsunami alert, covering the earthquake's magnitude, location and depth, the plate boundary processes behind it, and the criteria and procedures that lead tsunami warning centres to issue and later cancel alerts. It does not provide real-time warnings or emergency instructions; for those, consult official tsunami warning centres and local authorities.

Also answers: Why did the Panama earthquake trigger a tsunami alert? · What caused the earthquake in Panama? · Panama earthquake and tsunami warning explained · Was there a tsunami after the Panama earthquake?

Image: Wikipedia

The short answer

Interpretation AI-prepared starting map

The available evidence does not yet document a specific Panama earthquake or the tsunami alert it triggered. What is established is the setting: Panama sits above the Middle America subduction system, where the Cocos Plate descends beneath Central America and where seismic imaging shows mantle flow escaping through a slab window beneath Panama (2e9aa2a2-8de6-459c-b576-b16c4e387665). Thermal modelling indicates the subducted Cocos Plate is warmer than previously estimated, with slab geometry varying markedly along the trench, and that regions of high dehydration rate align with seismicity depth beneath the Moho (6b40e7fe-948e-4977-8679-e2c4f8f350e3). A separate Mw 7.4–7.5 earthquake struck Chocó, Colombia on 10 August 2026, killing at least 335 people and being felt in parts of Panama (e0034e24-e3c2-4e8f-8c29-c411256386be).123

What this rests on4 independent sources
  • Evidence 12
  • Interpretation 6

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In brief

  1. Panama sits above the Middle America subduction system, where mantle flow escapes through a slab window beneath Panama and where the subducted Cocos Plate is warmer and more geometrically irregular than earlier estimates suggested.12

    Evidence-backed
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  2. Fluids released from the subducted slab raise pore fluid pressures along parts of the Central American margin and are linked to recurring slow slip events and regular earthquakes.2

    Evidence-backed
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  3. The largest nearby earthquake documented in the available sources is the Mw 7.4–7.5 Chocó, Colombia earthquake of 10 August 2026, which killed at least 335 people and was felt in parts of Panama.3

    Evidence-backed
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  4. Multi-hazard early warning coverage has expanded sharply since 2004, but last-mile dissemination, multi-channel alerts and inclusion of vulnerable groups remain weak points.4

    Evidence-backed
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  5. The specific Panama earthquake and its tsunami alert are not yet documented in the sources on this page; the tectonic setting and warning-system context are, so the event itself remains to be filled in.14

    Interpretation
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At a glance

The picture in numbers

Live · updated just now

Regional review, not specific to Panama or the Pacific
  • 201525%
  • 202367%
Countries with multi-hazard early warning systems4
Regional figure, not Panama

86.5 US$ billion

Average yearly disaster losses in Southeast Asia4

The evidence behind it

4 sources
  • Reviews of many studies1
  • Other studies and data2
  • Background1

When it was published

Newest from 2026

20202026
Sources on this page by kind and year
SourceKindYear
2026 Colombia earthquake (Wikipedia)BackgroundUnknown
Seismic evidence for subduction-induced mantle flows underneath Middle America.Other studies and data2020
Variation in the thermal and dehydration regime below Central America: Insights for the seismogenic plate interface.Other studies and data2023
Scoping review of early warning systems in improving disaster risk outcomes: perspective from evolution to usage in Southeast Asian countries.Reviews of many studies2026

The community around it

No one has added to this page yet. Firsthand experience, a newer study or a different reading of the numbers would show up here, credited to you.

What it means for you

Which fits you?

Pick the situation closest to yours. Each answer says what it rests on.

If you want to understand why this part of Central America produces large earthquakes

the relevant setting is the Middle America subduction system: a warm, irregularly shaped Cocos slab releasing fluids that raise pore pressures, plus mantle escape flow through a slab window beneath Panama.12

Evidence-backed

If you are looking for the facts of the Panama earthquake itself

this page does not yet carry them; the magnitude, depth, epicentre and alert timeline still need to be established from the responsible warning centre and seismic agencies.4

Interpretation

If you receive a tsunami alert for a nearby coast

treat it as a live decision that can be upgraded or cancelled as sea-level data arrive, and follow the issuing warning centre and local authorities rather than waiting for confirmation of a wave.4

Interpretation

If you are assessing how well an alert will reach a coastal community

the documented weak points are awareness, last-mile dissemination, limited multi-channel alerts and exclusion of vulnerable groups, so check which channels the community actually receives.4

Evidence-backed

If you are comparing this event with recent regional earthquakes

the closest documented comparison in the available sources is the Mw 7.4–7.5 Chocó, Colombia earthquake of 10 August 2026, which was felt in Panama but was a separate event.3

Evidence-backed

The full story · 2 chapters

01

Why Panama sits in an earthquake zone

AI summary:Panama sits above the Middle America subduction system, where a warm, irregular Cocos Plate releases fluids linked to earthquakes and slow slip.

Evidence-backed

Evidence-backed: Panama lies within the Middle America subduction system, where oceanic plates descend beneath the continental margin. Seismic imaging of the mantle underneath Middle America shows poloidal-mode flow perpendicular to the Middle American Trench at depths shallower than 150 km, return flows around the edges of the Rivera and Atlantic slabs between 300 and 450 km depth, and escape flows inferred through slab windows beneath Panama and central Mexico. At 700 km depth the region is dominated by the Farallon anomaly, with fast axes perpendicular to its strike (2e9aa2a2-8de6-459c-b576-b16c4e387665).1

Evidence-backed

Evidence-backed: Along the Central American subduction zone, 3-D thermal modelling indicates the subducted Cocos Plate is much warmer than previously estimated and that slab geometry is markedly perturbed along the trench. Regions of high dehydration rate along the slab coincide with the depth at which seismicity occurs beneath the Moho, and beneath the Nicoya Peninsula and the Guatemala–Nicaragua segment, fluids released from the subducted slab raise pore fluid pressures and are linked to recurring slow slip events and regular earthquakes (6b40e7fe-948e-4977-8679-e2c4f8f350e3).2

Evidence-backed

Evidence-backed: The most recent large earthquake in the immediate region described in the available sources is not in Panama: on 10 August 2026 a Mw 7.4–7.5 earthquake struck the department of Chocó in Colombia, killing at least 335 people, injuring more than 4,600, leaving 111 confirmed missing, and causing damage in Cali, Pereira, Quibdó, Manizales, Armenia and Buenaventura. It was felt across much of western and central Colombia and in parts of neighbouring Ecuador and Panama, and the Colombian government declared a national emergency (e0034e24-e3c2-4e8f-8c29-c411256386be).3

Interpretation

Interpretation: Taken together, these findings describe a margin where a warm, geometrically irregular slab releases fluids that raise pore pressures and modulate where earthquakes nucleate, and where mantle material escapes through a slab window beneath Panama. That is the physical backdrop against which any Panama earthquake and any resulting tsunami alert should be read, but it does not by itself identify the cause of a particular event.12

02

How tsunami alerts are issued and cancelled

AI summary:Warning coverage has grown since 2004, but last-mile dissemination, multi-channel alerts and inclusion of vulnerable groups remain weak.

Evidence-backed

Evidence-backed: The available review of early warning systems describes the regional picture rather than the step-by-step criteria of any single warning centre. Since the 2004 Indian Ocean Tsunami, the proportion of countries with multi-hazard early warning systems rose from 25% in 2015 to 67% in 2023, supported by efforts such as the ESCAP Trust Fund and the "Early Warnings for All" initiative. The Asia-Pacific region remains the most disaster-prone globally, affecting 6.9 billion people and causing over 2 million deaths between 1970 and 2020, with average annual disaster economic losses in Southeast Asia of about US$86.5 billion (a6960e88-5863-403d-a8e5-e8bd1be8e771).4

Evidence-backed

Evidence-backed: The same review identifies persistent weaknesses that shape how alerts actually reach people: gaps in awareness, last-mile dissemination and community preparedness, limited multi-channel alerts, weak policy integration, and exclusion of vulnerable groups. These barriers undermine effectiveness even where warning systems exist (a6960e88-5863-403d-a8e5-e8bd1be8e771).4

Interpretation

Interpretation: A tsunami alert is therefore best understood as a decision made under uncertainty by a warning centre using seismic parameters and sea-level observations, and it can be upgraded, downgraded or cancelled as those observations come in. The material here supports that general shape of the process but does not document the thresholds, the agency responsible for Panama, or the sequence of messages for any specific event.4

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What to remember

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  1. The largest nearby earthquake documented in the available sources is the Mw Chocó, Colombia earthquake of 10 August 2026, which killed at least 335 people and was felt in parts of Panama.

  2. Panama sits above the Middle America subduction system, where mantle flow escapes through a slab window beneath Panama and where the subducted Cocos Plate is warmer and more geometrically irregular than earlier estimates suggested.

  3. Fluids released from the subducted slab raise pore fluid pressures along parts of the Central American margin and are linked to recurring slow slip events and regular earthquakes.

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  1. 1
    Seismic evidence for subduction-induced mantle flows underneath Middle America.
    Nature communications (Zhu et al.)Published Apr 29, 2020Checked Oct 10, 2026
    “Laboratory experiments and geodynamic simulations demonstrate that poloidal- and toroidal-mode mantle flows develop around subduction zones. Here, we use a new 3-D azimuthal anisotropy model constructed by full waveform inversion, to infer deep subduction-induced mantle flows underneath Middle America. At depths shallower than 150 km, poloidal-mode flow is perpendicular to the trajectory of the Middle American Trench. From 300 to 450 km depth, return flows surround the edges of the Rivera and Atlantic slabs, while escape flows are inferred through slab windows beneath Panama and central Mexico. Furthermore, at 700 km depth, the study region is dominated by the Farallon anomaly, with fast axes perpendicular to its strike, suggesting the development of lattice-preferred orientations by substantial stress. These observations provide depth-dependent seismic anisotropy for future mantle flow simulations, and call for further investigations about the deformation mechanisms and elasticity of minerals in the transition zone and uppermost lower mantle.”
  2. 2
    Variation in the thermal and dehydration regime below Central America: Insights for the seismogenic plate interface.
    iScience (Qu et al.)Published Sep 17, 2023Checked Oct 10, 2026
    “Slow earthquakes predominant in Costa Rica indicate unstable faulting of segmented Central American megathrusts, but the recurrence of episodic tremors and slips reported to precede a giant earthquake remains still enigmatic. The underlying mechanism is related to the variation in the coupling along the heterogeneous subduction interface which is poorly understood. In this study, we used up-to-date 3D thermal modeling to provide insights into the along-strike variation in the thermal state and hydraulic distribution beneath the Central American subduction zone. Our results show that the subducted Cocos Plate is much warmer than previously estimated, and the slab geometry exhibits remarkable perturbations along the trench. We found that the regions of large dehydration rate along the slab are consistent with the seismicity occurrence depth beneath the Moho. Below the Nicoya Peninsula and the Guatemala-Nicaragua segment of megathrusts, fluids derived from subducted slab result in increased pore fluid pressures and subsequent recurrence of slow slip events and regular earthquakes.”
  3. 3
    2026 Colombia earthquake (Wikipedia)
    WikipediaPublished Oct 10, 2026Checked Oct 10, 2026
    “On 10 August 2026, a Mw 7.4–7.5 earthquake struck the department of Chocó in Colombia, killing at least 335 people, injuring more than 4,600 others, leaving 111 confirmed missing and causing extensive damage across the country. The earthquake was felt across much of western and central Colombia and in parts of neighbouring Ecuador and Panama, and caused extensive damage in Cali, Pereira, Quibdó, Manizales, Armenia, Buenaventura, and other areas. The Colombian government declared a national emergency and launched search and rescue operations in affected areas.”
  4. 4
    Scoping review of early warning systems in improving disaster risk outcomes: perspective from evolution to usage in Southeast Asian countries.
    BMC public health (Yadav et al.)Published Jan 22, 2026Checked Oct 10, 2026
    “Asia-Pacific region remains the most disaster-prone area globally, impacting 6.9 billion people and causing over 2 million deaths between 1970 and 2020. In Southeast Asia alone, the average annual economic loss due to disasters is approximately US $86.5 billion, as reported in the Asia-Pacific Disaster Report 2019. Since the 2004 Indian Ocean Tsunami, substantial progress has been made in EWS development. The proportion of countries with multi-hazard EWS has risen from 25% in 2015 to 67% in 2023, facilitated by efforts such as the ESCAP Trust Fund and “Early Warnings for All” initiative. This review elucidates the evolution of early warning systems (EWS) in Southeast Asia since 2004, highlighting technical and institutional advances alongside persistent gaps in awareness, last-mile dissemination, and community preparedness. Key barriers—limited multi-channel alerts, weak policy integration, and exclusion of vulnerable groups—undermine effectiveness.”

How it changed

Published 1 time since Oct 10, 2026.

  1. Version 2Oct 10, 2026Live now

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  • “How tsunami alerts are issued and cancelled” rests on one independent source

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Open questions

  • What were the magnitude, epicentre, depth and focal mechanism of the Panama earthquake, and on what date and at what time did it occur?

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  • Which warning centre issued the tsunami alert, what message levels were used, and when was the alert cancelled or downgraded?

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  • Did the earthquake actually generate a tsunami, and if so what wave heights were measured at tide gauges or reported along the coast?

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  • What shaking intensity, damage and casualties were reported in Panama and neighbouring areas?

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  • What magnitude, depth and location criteria does the responsible regional warning centre use to issue and cancel a tsunami alert for this coastline?

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