Comprehensive specification of 18 independent global and regional seismological networks, structural geology catalogs, NOAA SWPC space weather, astronomical tidal models, and emergency alert channels.
Parallel polling of leading global institutes with 1–2 minute cycle times
Comprehensive planetary earthquake catalog from the USGS ComCat system. Delivers global M≥4.0 baseline coverage and continental US high-density hypocenters.
Major European hub aggregating real-time bulletins from 85+ national agencies across the Mediterranean, Anatolia, and Caucasus down to microseismicity.
The world's definitive global seismological archive based in the United Kingdom. Provides peer-reviewed, relocated hypocenters for scientific validation.
Operational tsunami warning authority under UNESCO/IOC and NOAA. Ingests deep-ocean DART® buoys and coastal tide gauges to issue real-time warning tiers, coastal ETA forecasts, wave amplitudes, and cancellation bulletins.
Italy's national research agency monitoring seismic hazard, volcanic activity (Etna, Stromboli, Vesuvius), and tectonic faulting along the Apennine ridge.
Boğaziçi University Kandilli Observatory and AFAD national seismic network providing dense coverage of the Anatolian extrusion wedge and Marmara Sea.
The Institute of Geodynamics at NOA monitors the most active subduction arc in Europe, spanning the Hellenic Trench, Corinth Rift, and Cyclades volcanic arc.
Federal agency at ETH Zurich operating ultra-sensitive borehole broadband arrays monitoring Alpine crustal deformation and geothermal induced seismicity.
German Research Centre for Geosciences (GFZ) operating a premier global seismic network with automated fast moment tensor solutions and virtual networks.
World-renowned high-density network combining JMA express bulletins and NIED borehole sensors across the 4-plate junction of Japan.
State monitoring authority tracking continental intraplate collision, the Tibetan orogenic belt, Sichuan Basin fault systems, and eastern China seismicity.
Government agency monitoring the active subduction trenches flanking both sides of the Philippine archipelago and the 1,200 km transcurrent strike-slip fault.
Federal Research Center Geophysical Survey of the Russian Academy of Sciences (GS RAS, Obninsk). Authoritative nationwide monitoring of all Russian seismic belts: Kamchatka, Kurils, Sakhalin, Baikal Rift, Altai-Sayan, Caucasus, and Arctic.
Authoritative national seismological center of Chile monitoring the fastest-slipping oceanic-continental subduction zone on Earth along the Nazca plate boundary.
National seismic network operated by UNAM Institute of Geophysics, monitoring the Cocos/North American plate subduction interface and Trans-Mexican Volcanic Belt.
Federal seismic monitoring network of Canada tracking Cascadia megathrust locked zones, Haida Gwaii strike-slip boundary, and intraplate eastern seismicity.
National geophysical agency of Indonesia. Monitors the high-hazard Sunda Megathrust across Sumatra, Java, Bali, and Sulawesi with rapid automated tsunami warnings.
High-resolution geological hazards network monitoring the Hikurangi Subduction Zone, Alpine Fault, and volcanic centers with instrumental ground shaking (MMI).
Australia's national geoscience agency monitoring continental intraplate seismicity, Joint Australian Tsunami Warning Centre feeds, and the Macquarie Ridge plate boundary.
Fault-isolated ingestion with automated twin-event reconciliation
Each seismic provider is isolated by a dedicated circuit breaker. If a remote agency experiences temporary downtime, the system automatically isolates the stream, allowing the remaining networks to continue delivering uninterrupted coverage.
Parallel incoming feeds are reconciled using a multidimensional spatiotemporal clustering algorithm. When duplicate detections occur, coordinates and magnitudes from the authoritative regional network take precedence, while event identifiers are linked into a unified profile.
Structural geology baselines coupled with dynamic planetary parameters
Global Earthquake Model database containing trace geometry, kinematic slip mechanism (strike-slip, normal, thrust), and annual slip accumulation rates (mm/yr).
Digital model of Earth's 52 tectonic plates classifying boundary dynamics into subduction zones, oceanic rifts, continental collisions, and transform boundaries with relative velocities.
The Smithsonian Institution’s authoritative catalogue of Holocene volcanoes, powering the volcano map layer and the volcanic-setting card on every event page. Coordinates, edifice type, summit elevation and last known eruption are taken from it.
9 Aviation Centers • Plumes & Flight Levels (FL000–FL600)
Official bulletins and dispersion polygons from the 9 international ICAO VAAC centers (Tokyo, London, Darwin, Toulouse, Montreal, Buenos Aires, Washington, Anchorage, Wellington) monitoring ash hazards for global aviation.
Planetary geomagnetic index Kp (0–9) and interplanetary magnetic field Bz utilized to monitor electrodynamic triggering interactions during intense geomagnetic storms.
Astronomical Algorithms • Tidal Shear Stress
High-precision solar/lunar ephemeris computing topocentric positions and syzygy alignment (New/Full Moon). Gravitational tidal deformation shifts Earth's crust by 20–40 cm vertically, generating modulating shear stresses on critically stressed faults.
Zero-friction alert delivery across personal channels and high-availability feeds for emergency response.
Direct cryptographic push notifications dispatched straight to iOS, Android, and Desktop browsers without requiring app store installation.
Interactive bot service (@EarthquakeLiveOrg_bot) offering customizable radius triggers, minimum magnitude thresholds, and localized language alerts.
Dedicated low-latency streams, automated civil protection webhooks, and private API integrations available for universities, researchers, and emergency agencies.
Rigorous theoretical foundations grounded in international seismological literature
"Aki, K. (1965). Maximum likelihood estimate of b in the formula log N = a - bM and its confidence limits. Bulletin of the Earthquake Research Institute, Tokyo University, 43, 237–239."
Pipeline Role: Evaluates frequency-magnitude distribution slope across Uber H3 Res 4 cells; identifies acute shear stress concentration anomalies (b < 0.8).
"Gutenberg, B., & Richter, C. F. (1944). Frequency of earthquakes in California. Bulletin of the Seismological Society of America, 34(4), 185–188."
Pipeline Role: Fundamental physical constraint scaling expected recurrence rates across regional catalogs.
"Benioff, H. (1951). Earthquakes and rock creep (Part I: Creep characteristics of rocks and the origin of aftershocks). Bulletin of the Seismological Society of America, 41(1), 31–62."
Pipeline Role: Computes cumulative acoustic energy and Benioff strain rebound S = ∑10^(0.75 M_i) to detect seismic quiescence or accelerating moment release.
"Wald, D. J., Jaiswal, K. S., Allen, T. I., & Hearne, M. G. (2008). USGS Prompt Assessment of Global Earthquakes for Response (PAGER). U.S. Geological Survey Fact Sheet 2008-3093."
Pipeline Role: Underpins the calibrated log-normal fatality and building vulnerability assessment curves.
"Esteva, L. (1974). Geology and predicting extreme ground motion for earthquake-resistant design. In Proceedings of the 2nd International Conference on Seismic Risk."
Pipeline Role: Isoseismal radius calculation mapping Modified Mercalli Intensity (MMI V–VIII) attenuation.
"Lundberg, S. M., & Lee, S.-I. (2017). A Unified Approach to Interpreting Model Predictions. Advances in Neural Information Processing Systems (NeurIPS 30), 4765–4774."
Pipeline Role: Decomposes ensemble hazard forecasts into exact Shapley values, ensuring full transparency.
"Bird, P. (2003). An updated digital model of plate boundaries. Geochemistry, Geophysics, Geosystems, 4(3), 1027."
Pipeline Role: Spatial distance to plate boundaries, relative motion rates, and plate convergence kinematics.
"Meeus, J. (1998). Astronomical Algorithms (2nd ed.). Willmann-Bell, Richmond, VA."
Pipeline Role: Computes lunar and solar gravitational tidal potential and syzygy alignment cycles.
"Titov, V. V., & Synolakis, C. E. (1998). Numerical modeling of tidal wave runup. Journal of Waterway, Port, Coastal, and Ocean Engineering, 124(4), 157–171."
Pipeline Role: Underpins NOAA MOST tsunami simulation and deep-ocean DART buoy wave inversion models.
"Kajiura, K. (1970). Tsunami source, energy and the ratio of wave energy to seismic energy. Bulletin of the Earthquake Research Institute, Tokyo University, 48, 835–869."
Pipeline Role: Formulates the ratio of seismic radiated energy to tsunami potential energy in shallow subduction megathrust ruptures.
"OASIS Standard. (2010). Common Alerting Protocol Version 1.2. OASIS Open Standard."
Pipeline Role: International interoperable XML standard for real-time ingestion of NOAA PTWC/NTWC multi-agency hazard bulletins.
Strict scientific reproducibility adhering to international seismological standards
100% of raw seismological waveform solutions and earthquake event records are ingested in real-time from open public institutions: USGS, EMSC FDSNWS, ISC, BMKG, GeoNet NZ, INGV, and GA. Raw data is never modified or fabricated.
All machine learning forecast models are evaluated on frozen, out-of-time test folds (CSEP standard). The full verification ledger with Brier Skill Score (+0.354) and ROC-AUC (0.814) is publicly auditable via the open metrics API.
We reject unscientific deterministic prediction claims. Fault nucleation obeys non-linear continuum mechanics. EarthquakeLive models strictly calibrated conditional probabilities P(M ≥ 4.5) to empower emergency preparedness.
Verified scientific, operational, and emergency protocols
Switch to the interactive WebGL map with real-time fault lines, recent quakes, and calibrated hazard cells.