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Bogota Seismic Zone • 250 km Monitoring Radius

Real-Time Earthquakes in Bogota, Colombia

Live seismic telemetry, active fault rupture tracking, and ground motion hazard monitoring for the Bogota metropolitan area.

TECTONIC SETTING:Eastern Frontal Fault System (Fallas del Borde Llanero) & Altiplano Cundiboyacense
METRO POPULATION:8.0 Million (11M Metro)
OBSERVATORY:SGC →

BOGOTA EVENTS (250 KM)

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NEAREST ACTIVE FAULT

Servitá-Bogotá Fault System (25 km)

TELEMETRY WINDOW

Live Telemetry Feed

SEISMIC INTENSITY

LOW SEISMICITY (24H)

Landmark Historical Earthquakes in Bogota

Significant seismic benchmarks, cataloged damage, and engineering lessons shaping modern safety standards.

2023M 6.1

El Calvario, Meta

2023-08-17•50 km from Bogota•MMI VI in Bogotá

Vigorously shook high-rise buildings and residential towers across Bogotá; triggered citywide building alarms and evacuations of tens of thousands, cracked structures, dislodged decorative plaster in the Colombian Congress chamber, and caused 1 fatality.

1917M 6.9

Villavicencio / Bogotá Foothills

1917-08-31•55 km from Bogota•MMI VIII in Bogotá

Known as the "Terremoto de 1917"; severely damaged churches, the presidential palace, and over 400 buildings across Bogotá.

Seismic Geology & Soil Amplification in Bogota

Plate boundaries, tectonic kinematics, and local geotechnical ground response characteristics.

PLATE BOUNDARY:South American Plate & North Andean Block Convergence
SLIP RATE:5–10 mm/year crustal shortening
STRESS REGIME:Compressional Reverse Thrusting

Bogotá sits on an elevated lacustrine plateau (the Sabana de Bogotá) at 2,640 meters altitude within the Eastern Cordillera of the Colombian Andes. The city is flanked on the east by the Eastern Frontal Fault System (Servitá, Bogotá, and Guaycaramo faults) and subjected to deep intermediate slab seismicity from the Bucaramanga Nest to the north.

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Local Soil Profile & Ground Motion Resonance

The Sabana de Bogotá is filled with deep soft lacustrine clay deposits of ancient Lake Humboldt, exceeding 500 meters thickness in western and northern districts. This generates resonant amplification of low-frequency seismic waves.

Major Active Fault Systems Near Bogota

Seismogenic fault lines, maximum credible magnitudes (MCE), and proximity to the metropolitan center.

25 KM FROM CITYM 7.2

Servitá-Bogotá Fault System

Reverse Thrust2–4 mm/year

Major frontal thrust system along the eastern Andean escarpment separating the mountains from the eastern plains (Llanos).

60 KM FROM CITYM 7.0

Guaycaramo Fault Zone

Sinistral Transpressive Thrust3 mm/year

Active tectonic boundary driving uplift of the Eastern Cordillera.

Seismic Safety, Observatory & Building Codes

Official seismological monitoring, building construction standards, early warnings, and emergency response.

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OFFICIAL SEISMIC OBSERVATORY

Servicio Geológico Colombiano (SGC) (SGC)

SGC National Seismological Telemetry Network
BUILDING CODE STANDARD:Reglamento Colombiano de Construcción Sismo Resistente (NSR-10)
Visit Official Observatory (SGC) →
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EMERGENCY HOTLINE
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Agáchate, Cúbrete y Sujétate. In older brick buildings in La Candelaria and Chapinero, protect against falling decorative masonry.

Frequently Asked Questions About Earthquakes in Bogota

Authoritative answers to common questions regarding seismic risks, building safety, and preparedness in Bogota.

Is Bogotá vulnerable to earthquakes despite being far from the coast?▾

Yes. Bogotá faces strong seismic hazards from the active Eastern Frontal Fault system less than 30 km east, and its soft ancient lakebed clay amplifies seismic waves by up to 4 times.