| 1 |
STRONG
|
90
|
↓ DOWN
|
web_search |
UCERF3 (the authoritative USGS/CGS model) estimates a 7.0% probability of an M8.0+ earthquake in California over the next 30 years, implying roughly 0.23%/year annual rate, well below the 1%/year threshold in sq1. |
Yes |
| 2 |
STRONG
|
85
|
↓ DOWN
|
web_search |
Regional USGS breakdown shows Northern California ~2% and Southern California ~3% probability of M8.0+ over 30 years, summing to roughly 5% combined (with overlap), consistent with an annual rate of ~0.17–0.23%/yr—far below 1%/yr. |
Yes |
| 3 |
STRONG
|
88
|
↓ DOWN
|
code_execution |
Poisson calculation at the UCERF3-implied rate (~0.23%/yr) over 9.63 years yields roughly 2.2% cumulative probability; only at rates ≥1%/yr does the 9.63-year probability reach ~9%, confirming sq1 likely resolves NO under mainstream models. |
Yes |
| 4 |
STRONG
|
88
|
↓ DOWN
|
web_search |
California has not experienced a confirmed M8.0+ earthquake since 1906 (~120 years), consistent with a long recurrence interval and a low annual rate well under 1%/yr. |
Yes |
| 5 |
MODERATE
|
75
|
↑ UP
|
wikipedia_lookup |
The Cascadia subduction zone extends into Northern California, capable of M9.0+ events; its southern terminus lies offshore near Cape Mendocino, CA, which could contribute to the M8+ probability for 'California territorial waters' depending on resolution scope. |
Yes |
| 6 |
STRONG
|
85
|
↑ UP
|
web_search |
The southern San Andreas Fault (Carrizo, Mojave, Coachella segments) has not ruptured in a major event since the 1857 Fort Tejon M7.9 earthquake—168 years ago—while the estimated recurrence interval is 140–160 years, meaning the fault is overdue for a large rupture. |
Yes |
| 7 |
MODERATE
|
80
|
↑ UP
|
web_search |
The Mojave segment of the San Andreas carries a 19% probability of M7.5+ in 30 years (highest of any California fault segment), but this is for M7.5+, not M8.0+, limiting its direct relevance to the question threshold. |
Yes |
| 8 |
WEAK
|
55
|
NEUTRAL
|
article_search |
A swarm of M4.5 earthquakes hit Imperial County (Southern California) near Brawley in May 2026, proximal to the San Andreas Fault system, but these are minor events not indicative of imminent M8+ rupture. |
Yes |
| 9 |
WEAK
|
55
|
NEUTRAL
|
article_search |
In January 2026, a M4.9 earthquake near Indio prompted seismologist Dr. Lucy Jones to warn of continued seismic activity due to proximity to the San Andreas, but no expert commentary linked this to elevated M8+ probability. |
Yes |
| 10 |
MODERATE
|
72
|
↑ UP
|
wikipedia_lookup |
The San Andreas Fault accumulates slip at 0.79–1.38 inches/year; with 168 years since the last major southern rupture, substantial elastic strain energy has accumulated on multiple locked segments. |
Yes |
| 11 |
MODERATE
|
82
|
↑ UP
|
web_search |
UCERF3's increased M8+ probability versus UCERF2 (7% vs 4.7% over 30 years) reflects inclusion of multi-fault rupture scenarios—suggesting that connecting fault ruptures could reach M8+ even if individual segments are unlikely to do so alone. |
Yes |
| 12 |
STRONG
|
85
|
↓ DOWN
|
web_search |
California's confirmed M8+ events in the historical/instrumental record are limited: the 1906 San Francisco earthquake (estimated M7.9–8.3) and possibly Fort Tejon 1857 (M7.9), suggesting recurrence intervals of many decades to over a century between M8+ events statewide. |
Yes |
| 13 |
STRONG
|
85
|
↓ DOWN
|
web_search |
UCERF3's 30-year M8+ probability of 7% implies a mean recurrence interval of roughly 400+ years for M8+ events in California, consistent with a 10-year probability of approximately 2–2.5%—well below the >10% threshold asked about in sq3. |
Yes |
| 14 |
MODERATE
|
70
|
↑ UP
|
wikipedia_lookup |
The Cascadia subduction zone has a paleoseismic record of full-margin M9+ ruptures roughly every 200–500 years; its southern end off Cape Mendocino could qualify as California territorial waters, potentially adding to M8+ recurrence—but the epicenter would typically be offshore Oregon/Washington for full-margin events. |
Yes |
| 15 |
STRONG
|
88
|
↓ DOWN
|
code_execution |
For the 10-year window probability to exceed 10%, the annual rate would need to be approximately 1.05%/yr or higher—roughly 4–5x the UCERF3 central estimate of ~0.23%/yr—indicating the historical record does not support sq3 resolving YES under mainstream models. |
Yes |
| 16 |
MODERATE
|
55
|
↑ UP
|
kalshi_data |
The Kalshi market for M8+ California before 2028 is priced at 11%, implying roughly a 1.1–1.3%/yr annual rate over the ~2 remaining years—somewhat higher than UCERF3 central estimates, possibly reflecting market uncertainty or upward bias. |
Yes |
| 17 |
MODERATE
|
50
|
↑ UP
|
kalshi_data |
The Kalshi market for M8+ California before 2035 is currently priced at 32%, which is dramatically higher than the ~2–2.5% implied by UCERF3 for a ~10-year window, suggesting significant market overpricing relative to seismological models or a much broader interpretation of the question. |
No |
| 18 |
MODERATE
|
60
|
↓ DOWN
|
kalshi_orderbook |
The orderbook spread is extremely wide ($0.95) with yes_bid at only $0.01 and no_bid at $0.04, suggesting very thin real buy-side support and that the 32% 'price' may not reflect genuine informed trading activity. |
Yes |