Earthquakes & seismic hazard

Earthquakes as data from USGS: Gutenberg-Richter b-values and recurrence, ShakeMap stations and Did You Feel It? reports, ground motion against distance, faults, plate boundaries, focal mechanisms, slab depth, hazard curves and maps, and the unit, time and distance traps.

Left, the PB2002 plate boundaries, subduction and convergent boundaries in red, with every earthquake of magnitude 7.5 or more from 1900 to 2024 in the USGS catalogue as a dark circle sized by magnitude, crowding the subduction zones of the Pacific rim and Indonesia; right, M3 and larger earthquakes in Oklahoma each year from 1990 to 2024, near zero until 2009, rising to 887 in 2015 and falling back after disposal limits. where the great earthquakes happen, and a rise made by people19902024Oklahoma M3+ per year: 887 in 2015M7.5+ since 1900 on plate boundaries

Earthquakes are among the best-documented natural hazards: the USGS catalogue lists every significant event worldwide, each large one comes with a ShakeMap, thousands of Did You Feel It? reports and a moment tensor, and the national hazard model can be queried for any point in the country. The guides here turn that into numbers: b-values and recurrence probabilities, shaking against distance, faults and plate boundaries, focal mechanisms, slab geometry, hazard curves, disaggregation and exposure maps, and the unit, time and distance traps that catch everyone once.

Every number comes from a run. The Ridgecrest M7.1 was felt 744 km away; its strongest recording was 56.9% of g; Oklahoma went from 1.4 M3+ earthquakes a year to 887 in 2015 and back down; and the three largest earthquakes of 2000 to 2024 released 46% of the seismic moment of all 12,334 M5.5+ events, which is what a b-value of 1.03 implies.

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