Steven Philley
Local Earthquakes Liquefaction Weather Site contents

Local desk · Seismic history

Bay Area earthquakes — history underfoot

Educational essay · USGS / history · Not a live alert · Updated Sep 2026

The South Bay sits inside a living plate boundary. This page is a calm reading of the faults we live with and the quakes that shaped memory — Peninsula, East Bay, Santa Cruz Mountains, Calaveras country — with Campbell and Santa Clara Valley in view. History and literacy only. Live feelables belong on the Local desk; ground-failure detail lives on liquefaction.

Why the Bay Area shakes

Northern California sits where the Pacific Plate slides northwest past the North American Plate along the San Andreas system. Motion is not one clean knife-cut; it is a braid of right-lateral faults that share the load across the Coast Ranges and under the Bay. When a locked patch fails, stored elastic strain releases as an earthquake — seconds of shaking that can last longer on soft valley fill than on bedrock hills.

Four names dominate Bay Area conversation: the San Andreas (Peninsula and Santa Cruz Mountains), the Hayward (East Bay urban corridor), the Calaveras (East Bay into the South Bay and Morgan Hill country), and the San Gregorio (offshore and coast-side west of the Peninsula). Together they explain most of the region’s historic damage — and why Campbell feels distant from the epicenter yet still rattles when a South Bay or Santa Cruz Mountains event lights up the valley floor.

Not a forecast. Nothing here predicts the next quake, its size, or its timing. Magnitudes below are well-known public figures from USGS and standard historical summaries. Treat older nineteenth-century sizes as estimates. For current seismicity, use USGS products and official alerts — not this essay.

Faults underfoot

USGS hazard models treat these as a connected system: stress and slip transfer among strands over decades and centuries. For map literacy, start with the USGS Earthquake Hazards Program and California Geological Survey fault maps — then zoom out before you zoom into any single street.

Historical timeline

A selective shelf of major and notable Bay Area events — enough to orient Campbell and Peninsula readers without pretending to be a complete catalog. Magnitudes use common USGS / historical shorthand (~ for older estimates).

  1. 1838

    Peninsula / San Andreas

    ~M6.8–7.4 (historical estimate)

    A large San Andreas earthquake on the Peninsula, known from contemporary accounts of strong shaking and damage in the young Mexican- and early American-era settlements. It remains a key pre-instrumental marker that the Peninsula strand can fail in a major way — a century of context for 1906 rather than a precise catalog entry.

  2. October 21, 1868

    Hayward — “great quake of the East Bay”

    ~M6.8–7.0

    The classic Hayward Fault rupture. East Bay towns took the brunt; the event still frames why Hayward scenarios dominate modern East Bay planning. For South Bay readers it is the reminder that the next regional “big one” is not automatically a San Andreas rematch of 1906.

  3. April 18, 1906

    San Francisco earthquake and fire

    ~M7.9

    The defining San Andreas rupture of the twentieth-century Bay Area: violent shaking from the North Coast through the Peninsula and beyond, followed by the fire that remade San Francisco’s built memory. Ground failure and liquefaction in lowland and fill settings are documented in USGS historic compilations; the cultural story of the fire often overshadows the geologic one. See also this site’s liquefaction desk for 1906 lowland notes.

  4. July 1, 1911

    Calaveras — Coyote / Morgan Hill country

    ~M6.5

    A strong Calaveras earthquake centered in the Coyote area south of San Jose — an early modern reminder that South Bay residents live next to an active East Bay–South Bay strand, not only the more famous San Andreas and Hayward names.

  5. March 22, 1957

    Daly City / San Francisco

    ~M5.3

    A sharp Peninsula / San Francisco jolt centered near Daly City. Modest by 1906 standards, memorable for mid-century residents and a teaching example of how a mid-magnitude event on soft ground can still feel dramatic in the city.

  6. April 24, 1984

    Morgan Hill

    M6.2 (Calaveras)

    A South Bay–relevant Calaveras rupture near Morgan Hill. Strong shaking across Santa Clara Valley communities made this a local memory event — the kind of quake that empties aisles for a few minutes and then becomes a neighborhood story. Useful context for later Alum Rock and valley floor feelables.

  7. October 17, 1989 · 5:04 p.m. PDT

    Loma Prieta

    M6.9

    The modern South Bay and Santa Cruz Mountains reference quake. Rupture in the Santa Cruz Mountains sent strong shaking across Monterey Bay, the South Bay, and — on soft fill and deep sediments — San Francisco and Oakland. The Cypress Structure collapse on the I-880 double-deck freeway and the Bay Bridge deck failure became the region’s most iconic infrastructure images; the Marina District’s liquefaction remains the Bay Area’s textbook urban ground-failure case (see liquefaction). Campbell and Santa Clara Valley felt a hard jolt during Game 3 of the World Series — a shared calendar memory as much as a geologic one.

    Public archival broadcast clip via YouTube (privacy-enhanced youtube-nocookie embed). Opens with regional coverage including Bay Bridge damage. Source: KTVU / YouTube.

    Collapsed upper deck section of the San Francisco–Oakland Bay Bridge after the 1989 Loma Prieta earthquake, looking west toward Pier E-9
    Bay Bridge — failed ~15 m span at Pier E-9, looking west. USGS photo by E.V. Leyendecker (public domain via Wikimedia Commons).
    Collapsed Cypress Street Viaduct double-deck freeway in Oakland after the 1989 Loma Prieta earthquake
    Cypress Structure (I-880 approach, Oakland) — double-deck collapse. USGS (public domain via Wikimedia Commons).
    Close view of the collapsed section of the San Francisco–Oakland Bay Bridge after Loma Prieta
    Bay Bridge collapsed section, alternate USGS view by C.E. Meyer (public domain via Wikimedia Commons).
  8. October 30–31, 2007

    Alum Rock / South Bay

    M5.6 (Calaveras area)

    A widely felt South Bay event near Alum Rock / east San Jose, with aftershocks that kept nerves up for days. Not a regional catastrophe — a modern example of how a mid-5s Calaveras quake can rattle Campbell, San Jose, and neighbors without rewriting the skyline. Useful as “recent memory,” not as a swarm forecast.

  9. August 24, 2014

    South Napa

    M6.0

    The largest Bay Area–adjacent damaging quake since Loma Prieta for many residents’ living memory. Centered in Napa County, it damaged older buildings and wine-country infrastructure and was felt widely around the Bay. A reminder that “Bay Area risk” is a regional system — North Bay strands matter even when you live in Campbell.

  10. Recent feelables

    Smaller jolts, careful framing

    Typically M3–M4+ · felt unevenly

    Most years bring a handful of widely felt but non-catastrophic Bay Area quakes — often on Calaveras, Hayward, or smaller strands. They are ordinary plate-boundary housekeeping, not secret previews of “the big one.” If your phone buzzes or the hanging lamp sways, check earthquake.usgs.gov or official ShakeAlert / wireless emergency alerts. This page will not duplicate the Local desk’s live quake blurbs.

South Bay & Campbell angle

Campbell sits on the Santa Clara Valley floor — soft sediments that can amplify shaking relative to nearby hills. That does not make every distant quake catastrophic; it does explain why a Morgan Hill, Alum Rock, or Santa Cruz Mountains event can feel sharper here than a similar magnitude far up the East Bay.

Calaveras proximity puts 1911, 1984 Morgan Hill, and 2007 Alum Rock in the local scrapbook. Loma Prieta (1989) remains the shared South Bay trauma and teaching case: World Series timing, valley-wide shaking, and the long commute home when freeways and bridges failed farther north.

For ground failure specifically — creek corridors, young fill, shallow water tables — use the liquefaction essay and its USGS northern Santa Clara scenario maps. History of shaking and maps of soil behavior are sibling literacies, not substitutes for each other.

Weather and air quality on the Local hub are day-to-day; this page is the longer seismic shelf. Cross-check Local and Weather when you want live conditions — not earthquake predictions.

SF & the Peninsula

San Francisco’s earthquake story is usually told as 1906 (shake + fire) and 1989 (Cypress, Bay Bridge, Marina). Both are fair anchors. Soft-bay mud and historic fill concentrate damage; hillside rock generally does better. Daly City 1957 sits between them as a mid-century Peninsula jolt that city residents still mention when comparing “how hard it felt.”

Infrastructure lessons from 1989 — double-deck freeways, older bridge spans, unreinforced masonry, and poorly compacted fill — drove decades of retrofit policy. The geology did not change; the building stock and emergency systems did. That is the useful Peninsula takeaway for South Bay readers too: risk is geology plus what we built on top of it.

Living with risk

Preparedness is ordinary, not apocalyptic. High-level habits that USGS and emergency managers repeat for a reason:

Drop, Cover, and Hold On during shaking — do not run outside through falling debris. Secure tall furniture and water heaters; know how to shut off gas if you smell it after a quake (and only then). Keep water, meds, shoes, and a flashlight where you can reach them in the dark. Agree on an out-of-area contact; local phones may jam.

Alerts. ShakeAlert-powered wireless alerts can give seconds of warning before strong shaking arrives from a detected rupture — enough to drop and cover, not enough to evacuate a city. Enable official alerts on your phone; treat unofficial social posts as unverified.

After. Expect aftershocks. Check on neighbors if you can do so safely. Use text or data when voice circuits are busy. Follow city and county emergency accounts for shelter, water, and road status — not rumor threads.

Literacy, not engineering. This page does not rate your house, school, or office. For retrofit, insurance, or site geology, talk to licensed professionals and use current USGS / California Geological Survey products. Pair this history with the liquefaction desk if soft ground is your question.

Sources

Disclaimer. Educational history only. Not a forecast, not a live alert feed, and not engineering or insurance advice. Magnitudes for nineteenth-century events are approximate. For property, retrofit, or emergency planning decisions, use current USGS / CGS products, local hazard disclosures, and licensed professionals. Official alerts beat any essay.