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Monday, August 24, 2026

Costa Rica Latest News

Two Costa Rica Earthquakes Shake Coronado Area, No Injuries

By · August 24, 2026 · 6 min read

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Key Facts

  • What happened Two Costa Rica earthquakes struck the Coronado area early Monday, causing minor local damage.
  • How big The first quake measured M5.4 per RSN, with aftershock M4.8 about two minutes later.
  • The catch Different agencies reported conflicting magnitudes for the first quake, from M4.9 to M5.4.
  • Who pays Local residents face repair costs, while the National Emergency Commission (CNE) manages response.
  • What comes next Monitoring continues as more than 30 aftershocks were recorded following the initial pair.
  • Tsunami risk No tsunami warning was issued because these Costa Rica earthquakes struck inland, not offshore.

A pair of quakes rattled central Costa Rica before dawn, leaving only minor damage despite more than 30 aftershocks.

Two Costa Rica earthquakes hit the Coronado area early Monday 24 August 2026, with the first striking at 1:37 a.m. local time. Authorities confirmed no deaths or injuries, though minor damage was reported across several neighborhoods.

Pedestrians on a shopping street in downtown San José, Costa Rica.
Two Costa Rica Earthquakes Shake Coronado Area, No Injuries. (Photo internet reproduction)
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The sequence of events early Monday

Two Costa Rica earthquakes jolted the Coronado area before dawn on 24 August 2026. The first tremor hit at 1:37 a.m. local time, followed by a second about two minutes later.

The Red Sismológica Nacional (RSN) reported the first quake as M5.4 at a depth of 7 kilometers. Its epicenter was located 11 kilometers north of Cascajal, Vázquez de Coronado.

The second quake measured M4.8 at a depth of 10 kilometers, according to RSN. Both tremors occurred in the same general area of central Costa Rica.

Seismologists recorded more than 30 aftershocks after the initial pair of quakes. Residents reported feeling several strong shakes throughout the early morning hours.

How different agencies measured the first quake

The three main monitoring institutions gave different magnitudes for the first tremor. The RSN revised its reading to M5.4, while the Volcanological and Seismological Observatory of Costa Rica (OVSICORI) initially reported M5.0.

The United States Geological Survey (USGS) listed the event as M4.9 near the town of Cot at a depth of 10 kilometers. OVSICORI placed its epicenter near San Isidro de Coronado at 11 kilometers depth.

These discrepancies are common because agencies process preliminary data differently. The RSN later revised its reading, which is considered the most consistent final local value.

All agencies agreed the quake was shallow, between 7 and 11 kilometers deep. Such shallow depth typically increases shaking intensity near the epicenter.

Damage reports from affected communities

Damage from these Costa Rica earthquakes was minor and localized, according to emergency officials. The National Emergency Commission (CNE) reported only isolated incidents across the affected region.

A damaged house wall was reported in Dulce Nombre de Jesús, a community near the epicenter. A fallen utility pole was confirmed in San Vicente de Moravia, disrupting local power briefly.

Debris on Route 32 near kilometre 30 caused traffic delays for early commuters. Road crews cleared the material quickly, restoring normal flow within hours.

No deaths or injuries were confirmed by any agency following the earthquake sequence. The relatively minor damage reflects the moderate size of these tremors.

Why no tsunami warning was issued

No tsunami warning was issued for these Costa Rica earthquakes, and none was expected. Both quakes struck inland, not beneath the ocean floor where tsunamis can form.

The United States Tsunami Warning System explicitly stated no tsunami statement was issued for the event. This is standard procedure for earthquakes that occur on land.

Tsunami alerts are reserved for undersea quakes capable of displacing large water volumes. The Coronado area sits inland in the central highlands of Costa Rica.

Residents along the Pacific and Caribbean coasts experienced no unusual sea activity. The lack of an ocean connection made any tsunami threat virtually impossible.

Aftershock activity and ongoing monitoring

Seismologists recorded more than 30 aftershocks following the main quakes on Monday morning. These smaller tremors continued for several hours after the initial pair.

Most aftershocks were too weak to be felt by residents, according to RSN. A few reached magnitudes that caused additional minor shaking in nearby communities.

The RSN and OVSICORI continue to monitor the seismic swarm closely. Both agencies are analyzing data from the sequence to understand the fault behavior.

Costa Rica sits in a seismically active region where such earthquake sequences are common. The country experiences hundreds of tremors each year, most too small to notice.

Public response and emergency coordination

The CNE activated its emergency protocols shortly after the first tremors were detected. Officials assessed damage across the Coronado area and surrounding districts.

Emergency crews inspected infrastructure including roads, bridges, and utility lines. They found only the fallen pole in Moravia and debris on Route 32.

Local authorities urged residents to remain calm and follow safety guidelines. Many people in San José and nearby cities felt the shaking and took precautions.

No evacuation orders were issued because damage levels did not warrant them. The response focused on quick damage assessment and restoring normal services.

Context of seismic activity in Costa Rica

Costa Rica Earthquakes are frequent because the country sits atop several active tectonic plate boundaries. The Cocos plate subducts beneath the Caribbean plate along the Pacific coast.

This collision zone generates frequent tremors of varying intensity across the country. The Coronado area has experienced earthquakes before due to local fault lines.

Scientists at OVSICORI and RSN continuously monitor these fault systems. Their early warning systems provide valuable seconds of notice before strong shaking arrives.

Monday’s pair of Costa Rica earthquakes was moderate compared to historic major events. The country’s building codes have improved significantly since destructive quakes in the past.

What residents should do after the quakes

Residents should check their homes for cracks in walls and damage to gas lines. The CNE recommends reporting any structural issues to local authorities promptly.

People should be prepared for possible continued aftershocks in coming days. Having an emergency kit with water, food, and flashlights is always advisable.

Those living near steep slopes should watch for landslides after heavy rain or shaking. Route 32 authorities will monitor the area for new debris falls.

Stay informed through official channels like CNE, RSN, and OVSICORI for updates. These Costa Rica earthquakes serve as a reminder to review personal emergency plans.

Frequently Asked Questions

What time did the two Costa Rica earthquakes occur on Monday?

The first quake struck at 1:37 a.m. local time, followed by the second about two minutes later. Both tremors hit the Coronado area of central Costa Rica.

How big were the earthquakes according to different agencies?

The RSN measured the first quake at M5.4, while OVSICORI reported M5.0 and the USGS listed M4.9. The second quake was measured at M4.8 by RSN.

Was there any damage from these earthquakes?

Damage was minor: a damaged house wall in Dulce Nombre de Jesús and a fallen utility pole in San Vicente de Moravia. No injuries or deaths were confirmed.

Was a tsunami warning issued after the quakes?

No tsunami warning was issued because both earthquakes struck inland, not under the ocean. Such warnings are only necessary for undersea quakes that can displace water.

How many aftershocks were recorded after the main quakes?

Seismologists recorded more than 30 aftershocks following the initial pair of tremors. Most were weak but some caused additional minor shaking in nearby areas.

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Sources

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