Latvia Earthquakes Today: Live Tracker & Map

Track every Latvia earthquake today with live seismic updates, refreshed every 60 seconds using verified data from USGS and EMSC. Latvia sits in a very low seismic risk zone, with no earthquakes recorded in the last 30 days. While seismic activity is currently quiet, our real-time monitor remains active 24/7 to detect any emerging tremors or shifts.

Live Seismology Clock:
UTC Synchronized
Regional Seismic Profile
Risk LevelVery Low (Baltic Sedimentary Basin)
Major FaultsLiepaja-Riga-Pskov Fault Line, Sloka-Talsi Tectonic Zone
Notable Quakes1821 (M3.5), 2004 (M5.2)
Population Exposed1.9 million
Tectonic SettingDeep Precambrian crystalline crust covered by undisturbed Paleozoic sediments on the stable East European Craton.
Historical Insight: The strongest recorded earthquake in Latvia was the 1821 Koknese earthquake, reaching magnitude 3.5.
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Latvia Earthquakes Today — Live Map

Interactive map of recent seismic activity in Latvia. Each colored radar ring marks an earthquake epicenter.

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Latest Earthquakes in Latvia

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All Quiet in Latvia!

No earthquakes of magnitude 2.5 or greater have been recorded in the past 30 days. This is great news for seismic stability!

Check the sidebar for historical activity statistics.

Magnitude Color Guide:
M1–M2.9M3–M4.9M5–M5.9M6–M6.9M7.0+
Activity Analytics

Seismic frequency telemetry in Latvia

Past 7 DaysWeekly
0recorded quakes
Past 30 DaysMonthly
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Past 12 MonthsAnnual
recorded quakes
10-Year TotalDecade
seismic events

Earthquake in Latvia Right Now — Live Updates & Seismic Activity

Latvia experiences very low (baltic sedimentary basin) seismic activity, primarily governed by its tectonic setting: Deep Precambrian crystalline crust covered by undisturbed Paleozoic sediments on the stable East European Craton.. Historically, the 2004 Kaliningrad Regional Felt Shaking earthquake (M5.2) demonstrated the region's immense seismic hazard potential.Major geological fault structures include Liepaja-Riga-Pskov Fault Line, Sloka-Talsi Tectonic Zone. This page provides continuous, verified seismic telemetry sourced directly from the U.S. Geological Survey (USGS) and the European-Mediterranean Seismological Centre (EMSC).

Earthquakes Today in Latvia — Live USGS & EMSC Tracker

Was there an earthquake in Latvia today or just now? No significant earthquakes have been detected in Latvia within the past 24 hours. However, tectonic stress can shift without warning. Our live Today's Earthquakes tracker monitors real-time telemetry from the USGS and EMSC around the clock to detect and report every tremor the second it occurs. If you recently felt unexpected ground motion or tremors, check the interactive map above for recent verified seismic activity, depth measurements, and localized epicenter reports. With an exposed population of approximately 1.9 million, timely seismic tracking is crucial for emergency awareness.

Why Does Latvia Experience Earthquakes?

Seismic activity in Latvia is fundamentally driven by its tectonic setting: Deep Precambrian crystalline crust covered by undisturbed Paleozoic sediments on the stable East European Craton.. As tectonic plates continuously converge, slide past one another, or diverge, frictional forces along fault planes lock the crust until the strain exceeds rock strength. When a fault suddenly slips, stored elastic energy is released as seismic waves that radiate outward, causing the ground motion recorded on seismographs. To see the latest seismic events worldwide, visit our earthquake today tracker for live updates.

Key Facts About Latvia Seismicity

  • Seismic Risk: Very Low (Baltic Sedimentary Basin)
  • Major Faults: Liepaja-Riga-Pskov Fault Line, Sloka-Talsi Tectonic Zone
  • Tectonic Setting: Deep Precambrian crystalline crust covered by undisturbed Paleozoic sediments on the stable East European Craton.
  • Notable Historical Quakes: 1821 Koknese (M3.5), 2004 Kaliningrad Regional Felt Shaking (M5.2), 1908 Ilukste (M3.2)
  • Population Exposed: 1.9 million

Earthquake Magnitude & Impact Reference

M1.0–M2.9
Minor Tremor
M3.0–M4.9
Light Shaking
M5.0–M5.9
Moderate
M6.0–M6.9
Strong Shaking
M7.0+
Major Quake
Shallow (< 70 km)
Causes the highest surface ground shaking and structural risk.
Intermediate (70–300 km)
Widely felt across regions with moderate ground acceleration.
Deep (> 300 km)
Seismic wave energy is largely dissipated through the mantle.

Staying Safe During an Earthquake in Latvia

If you feel sudden shaking in Latvia, remember the official safety protocol: Drop, Cover, and Hold On. Take cover under a sturdy table, shield your head and neck, and hold on until ground shaking completely subsides. Afterwards, check for gas leaks, stay alert for aftershocks, and review our step-by-step earthquake survival guide .

Stay informed with our earthquake today homepage for a global overview of seismic activity. Explore other regions on our global countries directory, check our earthquake near me radar, set up instant seismic alerts, or read our scientific breakdown on why earthquakes happen.

Regional Seismic Navigation

Explore Seismic Activity & Cities in Latvia

Monitor localized live tremors across Latvia's provinces, explore neighboring fault lines, and access critical earthquake survival guides.

Neighboring Tectonic & Seismic Zones

Earthquake tremors frequently cross national borders. Explore active subduction zones and fault networks in adjacent countries.

Underlain by the stable crystalline basement of the East European Platform (Baltic monocline), with negligible natural tectonic activity.

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Straddles the Trans-European Suture Zone (Teisseyre-Tornquist Line) separating ancient cratonic crust from younger Paleozoic Europe, with localized tectonic activity in the Sudetes/Carpathians and frequent mining tremors.

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Precambrian Baltic (Fennoscandian) Shield characterized by stable intraplate lithosphere, where low-magnitude seismic activity is driven primarily by post-glacial isostatic uplift.

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Occupies the thick, ultra-stable core of the Archean-Proterozoic Fennoscandian Craton, recording rare, low-magnitude seismic adjustments due to post-glacial rebound.

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Sits upon the Sorgenfrei-Tornquist Zone separating the Baltic Shield from the North German Basin, subject to minor post-glacial rebound adjustments.

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Central Western Carpathians alpine orogenic belt, deformed during Cretaceous-Tertiary collision and undergoing transpressional block movements adjacent to the Pannonian Basin.

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Seismic Preparedness & Real-Time Radar Tools

Essential emergency resources, live proximity scanning, and life-saving safety guides.

Earthquakes Near Me

Use your device GPS to scan for earthquakes within 100km to 1,000km of your current location.

Launch Proximity Radar
What to Do During Shaking

Immediate survival steps: Drop, Cover, and Hold On rules for indoors, vehicles, and open areas.

Read Survival Guide
72-Hour Emergency Kit

Comprehensive checklist: drinking water, emergency rations, trauma medical supplies, and power backup.

View Kit Checklist
Pacific Ring of Fire

Deep dive into the 40,000 km subduction belt responsible for 90% of global tremors and megaquakes.

Explore Ring of Fire
Frequently Asked Questions

Frequently Asked Questions

Live seismic intelligence, historical frequency trends, and safety tips for Latvia.

To check if an earthquake just occurred in Latvia, view our live interactive map and real-time feed at the top of this page. Any tremors detected within the last 24 hours are displayed instantly with verified magnitude, focal depth, exact epicenter coordinates, and distance from major cities, updated directly via USGS and EMSC sensor networks.