Los Angeles County and Many Others Are Mostly Exposed to Earthquakes, Leading to Disrupted Travel and a Grind to a Halt - Travel And Tour World

Los Angeles County and Many Others Are Mostly Exposed to Earthquakes, Leading to Disrupted Travel and a Grind to a Halt

Anamika Talukder Written by Anamika Talukder

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16 mins to read
Los angeles Image generated with Ai

American counties facing the greatest risk of severe earthquake-related travel disruption are concentrated in California, Alaska, Washington, Oregon, Hawaii and Utah, with additional concern around Memphis in Tennessee. Los Angeles, San Bernardino, Riverside, Alameda, San Francisco, King, Pierce, Multnomah, Anchorage, Salt Lake and Shelby counties or county-equivalent areas stand out because strong earthquake exposure overlaps with major airports, interstate highways, bridges, ports, rail systems and tourism corridors. California has the strongest concentration of urban transport risk, while the Cascadia Subduction Zone in the Pacific Northwest could create the widest multi-state disruption if a major earthquake strikes.

U.S. Counties Most Exposed to Severe Earthquakes That Could Disrupt Travel

County / county equivalentStateMain earthquake sourceTravel-disruption exposureMain transport assets at riskWhy travellers could face major disruptionHistorical event / official scenario
Los Angeles CountyCaliforniaSan Andreas, Sierra Madre, Puente Hills and numerous basin faultsVery HighLAX, I-5, I-10, I-405, Metrolink, LA Metro, Port-area connectionsFreeway bridges, rail corridors and airport access sit within one of America’s most exposed urban transport systems. The 1994 Northridge earthquake damaged freeway bridges and overpasses, disrupting major arteries for months.1994 M6.7 Northridge; USGS ShakeOut M7.8 scenario.
San Bernardino CountyCaliforniaSan Andreas, San Jacinto faultsVery HighI-15/Cajon Pass, I-10, I-215, freight rail, Ontario-region accessThis is one of Southern California’s most important inland gateways. Government earthquake scenarios show severe disruption to Cajon Pass and highway connections into Los Angeles.USGS ShakeOut scenario predicts particularly strong effects in San Bernardino and Riverside counties.
Riverside CountyCaliforniaSan Andreas and San Jacinto fault systemsVery HighI-10, I-215, SR-60, Palm Springs access, freight routesThe San Andreas crosses the Coachella Valley and approaches the San Gorgonio Pass transport bottleneck. Road, rail and utility corridors converge in narrow passes.M7.8 ShakeOut scenario models damaging shaking across Riverside County.
Orange CountyCaliforniaNewport-Inglewood and regional Southern California faultsHighI-5, I-405, SR-55, John Wayne Airport, MetrolinkDense freeway and commuter-rail infrastructure means even damage outside the county could create severe network congestion and access problems.Included in the official eight-county ShakeOut impact area.
Ventura CountyCaliforniaVentura, San Cayetano and regional faultsHighUS-101, SR-126, Pacific Coast routes, railMountains, bridges and coastal corridors create relatively few alternatives if highways or rail lines are damaged by shaking or landslides.Included in the USGS Southern California ShakeOut study.
Alameda CountyCaliforniaHayward FaultVery HighOakland International Airport, BART, I-80, I-880, I-580, Port of Oakland, Bay Bridge accessThe Hayward Fault runs directly through the urban East Bay. Surface rupture, liquefaction and strong shaking could simultaneously affect roads, BART and port/airport access.USGS HayWired M7.0 scenario places the hypothetical epicentre in Oakland.
Contra Costa CountyCaliforniaHayward/Rodgers Creek and nearby faultsVery HighI-80, I-680, BART, Richmond-San Rafael and Benicia-Martinez corridorsBridges and cross-Bay travel make transport highly interconnected. A disruption can propagate throughout the Bay Area.HayWired modelling identifies Contra Costa among counties exposed to major Hayward Fault consequences.
San Francisco CountyCaliforniaSan Andreas and Hayward regional systemVery HighSFO approaches, BART, Muni, Bay Bridge, Golden Gate approaches, ferriesPeninsula geography makes travellers dependent on bridges, tunnels, rail and a limited number of highway corridors. Liquefaction-prone bayfront areas increase infrastructure vulnerability.1989 Loma Prieta damaged the original Bay Bridge East Span; regional plans specifically address earthquake recovery.
Santa Clara CountyCaliforniaSan Andreas, Hayward and Calaveras faultsVery HighSan José airport, US-101, I-280, I-880, Caltrain, VTASilicon Valley lies between several major fault systems. Transport interruptions could isolate employment centres and interfere with links between San José and San Francisco.Included in USGS HayWired modelling; 1868 Hayward earthquake affected what is now Santa Clara County.
Napa CountyCaliforniaWest Napa Fault and regional faultsHighSR-29, SR-121, wine-tourism road networkNapa has fewer alternative transport corridors than major metropolitan counties. Earthquake damage can directly interfere with tourism access and local roads.2014 M6.0 South Napa earthquake is one of the significant modern California events used in USGS hazard assessments.
Kern CountyCaliforniaEastern California shear zone, Garlock and nearby fault systemsHighSR-178, US-395 approaches, I-5 connections, Mojave transport corridorsMountain passes and long-distance highway connections make earthquake-related rockfall and pavement damage particularly disruptive.2019 Ridgecrest earthquake sequence occurred in the region; Kern is also included in the ShakeOut study area.
Anchorage MunicipalityAlaskaAlaska-Aleutian subduction system and intraslab faultsVery HighTed Stevens Anchorage International Airport, Glenn Highway, Seward Highway, Alaska RailroadAnchorage is Alaska’s principal air and road hub. Ground failure and liquefaction can damage highway approaches and sever connections between the state’s population centres.2018 M7.1 Anchorage earthquake caused widespread infrastructure inspections and road disruption.
Matanuska-Susitna BoroughAlaskaAlaska-Aleutian seismic systemVery HighGlenn and Parks highways, roads around Wasilla/PalmerThe 2018 earthquake produced road failures and lateral spreading in the Matanuska Valley. Aftershocks continued aggravating road damage.Municipality of Anchorage and Mat-Su both declared local disaster emergencies after the 2018 quake.
Hawaiʻi CountyHawaiiKīlauea/Mauna Loa volcanic seismicity and regional faultsVery HighHawaiʻi Belt Road, Saddle Road/Daniel K. Inouye Highway, Hilo and Kona airportsEarthquake risk combines with volcanic deformation, landslides and limited island road alternatives. A highway closure can force very long detours.USGS updated Hawaiian seismic modelling partly because of earthquake activity associated with volcanic processes.
King CountyWashingtonCascadia Subduction Zone, Seattle FaultVery HighSeattle-Tacoma regional network, I-5, I-90, ferries, Link light rail, Port of SeattleThe Seattle metropolitan area contains bridges, elevated roadways, port facilities and areas susceptible to liquefaction. Cascadia damage could affect transport over a broad region simultaneously.Washington modelling evaluates highway-bridge damage under a M9.0 Cascadia event.
Pierce CountyWashingtonCascadia Subduction Zone, Tacoma-area faultsVery HighI-5, SR-16, Tacoma Narrows corridor, Port of Tacoma, SEA regional accessMajor freight and passenger corridors cross waterways and soft sedimentary areas. Regional bridge failures could restrict north-south mobility.Included in Washington’s M9.0 Cascadia bridge-damage scenario.
Clallam CountyWashingtonCascadia Subduction ZoneVery HighUS-101, Port Angeles ferry connectionsCoastal shaking would be accompanied by tsunami danger. The Olympic Peninsula has comparatively limited alternate road access.Washington Cascadia scenario identifies western counties and highway bridges exposed to serious damage.
Grays Harbor CountyWashingtonCascadia Subduction ZoneVery HighUS-12, US-101, coastal roads, port facilitiesDirect coastal exposure raises both shaking and tsunami risks. Road and bridge failures could isolate coastal communities.Included in statewide Cascadia transportation modelling.
Pacific CountyWashingtonCascadia Subduction ZoneVery HighUS-101, coastal bridges and local evacuation routesVery strong shaking plus tsunami inundation could simultaneously remove coastal roads and evacuation routes.Washington’s M9.0 Cascadia model includes Pacific County.
Multnomah CountyOregonCascadia Subduction Zone and Portland Hills faultsVery HighPortland International Airport access, I-5, I-84, I-205, MAX, Willamette/Columbia bridgesPortland depends heavily on river crossings. Strong shaking, liquefaction and bridge damage could break east-west and north-south travel connections.Oregon places Multnomah in the mid-range Cascadia impact area; detailed Portland regional impact modelling exists.
Clackamas CountyOregonCascadia and Portland-area crustal faultsVery HighI-5, I-205, bridges across Willamette tributariesODOT says the I-5 Boone Bridge, a key West Coast route carrying more than 126,000 vehicles daily, is at risk of failure in a Cascadia earthquake.Cascadia and Portland M7 scenario modelling.
Washington CountyOregonCascadia Subduction ZoneHighUS-26, OR-217 and western Portland routesStrong shaking and ground failure could restrict access between the Oregon Coast and Portland metropolitan area.Oregon regional impact study specifically covers Washington, Multnomah and Clackamas counties.
Clatsop CountyOregonCascadia Subduction ZoneVery HighUS-101, US-26, Columbia River/coastal routesOregon identifies Clatsop as a high-impact Cascadia county. Tsunami arrival could occur shortly after prolonged strong shaking.State Cascadia planning expects 4–6 minutes of shaking and tsunami arrival in some coastal areas within about 15 minutes.
Lincoln CountyOregonCascadia Subduction ZoneVery HighUS-101, OR-18, OR-20Narrow coastal roads and bridges make alternative travel difficult. Tsunami damage could compound earthquake-related bridge and landslide failures.Official Oregon list places Lincoln County in the high-impact Cascadia area.
Coos CountyOregonCascadia Subduction ZoneVery HighUS-101, port and coastal roadsCoastal highways, bridges and port infrastructure face combined shaking, liquefaction and tsunami exposure.Listed among Oregon’s high-impact Cascadia counties.
Curry CountyOregonCascadia Subduction ZoneVery HighUS-101 and coastal bridgesRemote geography and dependence on one principal north-south road increase the potential for traveller isolation following bridge or landslide damage.One of Oregon’s designated high-impact Cascadia counties.
Salt Lake CountyUtahWasatch FaultVery HighSalt Lake City International Airport, I-15, I-80, I-215, TRAX, FrontRunnerUtah’s main population and transport corridor lies directly within the Intermountain Seismic Belt. An earthquake could damage roads, bridges and utilities across the Wasatch Front.State M7.0 scenario estimated enormous infrastructure and economic disruption; USGS has modelled multiple M7 Wasatch scenarios.
Shelby CountyTennesseeNew Madrid Seismic ZoneHigh–Very HighMemphis International Airport, I-40, I-55, Mississippi River bridges, freight rail and river shippingMemphis is a national freight crossroads. Strong shaking and liquefaction could damage bridge approaches, highways and Mississippi River transport.USGS says a major New Madrid event could make roadways impassable and river navigation impossible for weeks in severe scenarios.
Charleston CountySouth CarolinaCharleston seismic zoneHighI-26, US-17, Charleston International Airport, Port of CharlestonSeismic hazard is unusually significant for the eastern U.S.; soft coastal sediments can amplify shaking and liquefaction risk around transportation infrastructure.The 1886 Charleston earthquake underpins current state intensity planning.

Why Are California Counties So Vulnerable to Earthquake Travel Disruptions?

California carries the country’s most concentrated combination of seismic activity, population density and transport infrastructure. Los Angeles, San Bernardino, Riverside, Alameda, Contra Costa, San Francisco and Santa Clara counties all sit near major fault systems while supporting some of the busiest airports, highways and rail corridors in the United States. The danger is not limited to ground shaking. Earthquakes can damage bridges, buckle highways, trigger landslides, interrupt rail service and block access to airports.

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Past disasters show how quickly mobility can collapse. The 1994 Northridge earthquake damaged freeway structures around Los Angeles and disrupted major commuter routes. The 1989 Loma Prieta earthquake damaged transportation infrastructure across the San Francisco Bay Area. These cases show why California remains central to national earthquake travel planning. In highly connected urban regions, a damaged interchange or bridge can affect travel well beyond the immediate disaster zone.

Why Does Los Angeles County Remain One of the Biggest Travel Risk Zones?

Los Angeles County combines extensive earthquake exposure with one of America’s largest transportation systems. The region depends heavily on highways including Interstate 5, Interstate 10 and Interstate 405, while Los Angeles International Airport serves as one of the country’s most important gateways for domestic and international travel. Metro rail, commuter rail, bus networks and port connections add more infrastructure that could be affected by strong shaking.

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The county is surrounded by several active fault systems. These include the San Andreas system as well as faults beneath or close to the metropolitan area. A major earthquake could therefore create road closures, bridge inspections, rail suspensions and airport access problems at the same time.

The Northridge earthquake demonstrated this vulnerability when freeway overpasses were damaged and commuters faced major detours. For travelers, the greatest problem may not be the earthquake itself but the loss of reliable connections between airports, hotels, tourist districts and neighboring counties.

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Why Are San Bernardino and Riverside Critical to Southern California Travel?

San Bernardino and Riverside counties are particularly important because they contain major transport corridors linking Southern California with Arizona, Nevada and the wider interior West. Interstate 15, Interstate 10 and Interstate 215 cross these counties, while Cajon Pass and San Gorgonio Pass funnel highways, rail lines and utilities through narrow geographic corridors.

Both counties also lie close to major segments of the San Andreas and San Jacinto fault systems. If a powerful earthquake damages roads through one of these passes, there may be relatively few practical alternatives for long-distance traffic.

This makes the two counties strategically important even for travelers who never plan to stop there. Tourists heading between Los Angeles, Las Vegas, Palm Springs and desert destinations rely on these routes. Freight transport also shares the same infrastructure. A major disruption could create widespread delays, road closures, fuel-delivery problems and pressure on alternate highways, extending the effect far beyond the earthquake’s immediate epicenter.

Why Is the San Francisco Bay Area So Exposed to Transport Failure?

The San Francisco Bay Area faces a different type of earthquake travel problem because movement depends heavily on bridges, tunnels, ferries and rail networks crossing or surrounding the bay. Alameda, San Francisco, Contra Costa and Santa Clara counties are particularly significant because they contain major airports, Interstate corridors, Bay Area Rapid Transit lines and port infrastructure.

The Hayward Fault creates one of the region’s most serious concerns. A strong earthquake on this fault could damage roads, utilities and rail connections in densely populated East Bay communities. Liquefaction is another major hazard in areas built on soft ground near the shoreline.

Travel disruption could spread rapidly because the region functions as one interconnected transport system. A bridge closure in one county could increase congestion in several others. Damage affecting BART or airport access could disrupt both local commuters and international visitors. This interconnected geography makes the Bay Area one of America’s most complex earthquake transportation challenges.

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Why Could Cascadia Cause the Largest Regional Travel Shutdown?

The Cascadia Subduction Zone represents one of the most serious earthquake threats in North America because a very large event could affect vast sections of Washington, Oregon and northern California simultaneously. Unlike a localized urban earthquake, a major Cascadia rupture could damage hundreds of miles of highways, bridges, railways, ports and airports across several states.

Washington counties such as King, Pierce, Clallam, Grays Harbor and Pacific face different but connected risks. Seattle and Tacoma could experience severe infrastructure disruption, while coastal counties may face both intense shaking and tsunami danger. Oregon counties including Multnomah, Clatsop, Lincoln, Coos and Curry also contain vulnerable transport corridors.

The scale is what makes Cascadia unique. Interstate 5, coastal Highway 101, railway networks and numerous river crossings could all be affected. Travelers could face extended detours, ferry disruptions, airport problems and isolated coastal communities, making recovery considerably more complicated than after a smaller urban earthquake.

Why Are Oregon’s Coastal Counties Especially Difficult for Travelers?

Oregon’s coastal counties face a dangerous combination of strong earthquake shaking, tsunami exposure and limited road alternatives. Clatsop, Lincoln, Coos and Curry counties depend heavily on U.S. Highway 101, which runs along the coast and crosses numerous bridges, rivers and landslide-prone areas. Several east-west routes link the coast with the Willamette Valley, but mountainous terrain limits alternatives.

A major Cascadia earthquake could therefore isolate communities even when individual towns avoid catastrophic damage. Bridges may require inspection before reopening, landslides could block roads and tsunami inundation could damage low-lying transport infrastructure.

This matters directly to tourists. Oregon’s coast is popular for road trips, state parks and small seaside communities. Visitors unfamiliar with tsunami evacuation routes could face additional challenges during a major event. Travel disruption would likely involve more than temporary traffic delays. In the worst-hit areas, access could remain difficult while authorities inspect bridges, clear debris and restore essential services.

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Why Is Anchorage One of America’s Most Important Earthquake Travel Hubs?

Anchorage is unusually significant because it is both Alaska’s largest population center and its main transportation gateway. Ted Stevens Anchorage International Airport connects Alaska with the rest of the United States and international markets, while the Glenn Highway, Seward Highway and Alaska Railroad provide critical links to other communities.

The 2018 magnitude 7.1 Anchorage earthquake showed how quickly transport infrastructure can be affected. Roads cracked, ramps failed and authorities conducted widespread bridge and highway inspections. Although major transportation systems recovered relatively quickly, the event demonstrated the vulnerability of the region.

Alaska’s geography increases the consequences of disruption. Many communities depend on a small number of roads or air connections, so losing a highway can create much larger problems than in a city with multiple alternate routes. The neighboring Matanuska-Susitna Borough also remains important because highways connecting Anchorage with Palmer, Wasilla and interior Alaska pass through earthquake-prone terrain.

Why Should Travelers Pay Attention to Salt Lake County and the Wasatch Front?

Salt Lake County may receive less earthquake attention than California, but its exposure is significant. The Wasatch Fault runs close to the heavily populated urban corridor stretching along northern Utah. Interstate 15, Interstate 80 and Interstate 215 converge around Salt Lake City, while Salt Lake City International Airport is a major regional aviation hub.

A strong earthquake could damage bridges, highway interchanges, rail infrastructure and utilities across the Wasatch Front. Because so much of Utah’s population and economic activity is concentrated in this narrow corridor, transportation disruption could become widespread.

Tourism would also be affected. Salt Lake City functions as a gateway to Utah’s ski resorts, national parks and mountain destinations. Road closures or airport access problems could disrupt travel plans across the state. The area’s vulnerability illustrates a wider lesson: earthquake travel risk is not limited to coastal regions. Inland cities located beside major active faults can face equally serious mobility challenges.

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Why Does Memphis Face a Major Earthquake Travel Threat?

Memphis and Shelby County stand out because they sit near the New Madrid Seismic Zone while also functioning as one of America’s most important freight and transport centers. Interstate 40 and Interstate 55 cross the region, major railway lines converge there and Mississippi River bridges carry enormous volumes of passenger and commercial traffic.

A strong New Madrid earthquake could therefore affect transportation far beyond Tennessee. Geological conditions in the central United States allow earthquake waves to travel over wider areas than they often do in the western United States. That means one powerful event could affect infrastructure across several states.

Bridge damage would be especially disruptive because alternative Mississippi River crossings are limited. Memphis International Airport, freight facilities and river shipping could also experience interruptions. The region receives less public attention than California or Cascadia, but its national logistical importance makes Shelby County one of the most consequential inland earthquake travel-risk locations in the country.

What Should Travelers Understand About Earthquake Risk Across America?

Earthquake travel risk depends on more than how often earthquakes occur. The biggest disruptions happen where strong shaking intersects with dense infrastructure, important transport hubs and limited alternative routes. That is why Los Angeles, the San Francisco Bay Area, Anchorage, Seattle, Portland, Salt Lake City and Memphis deserve particular attention.

Travelers should understand that even an airport left physically undamaged can become difficult to reach if highways, rail lines or bridges close. Coastal areas may also face tsunami warnings that stop road movement and trigger evacuations. After a major earthquake, authorities may close infrastructure temporarily for safety inspections even when there is no obvious visible damage.

The broad pattern is clear. California carries America’s greatest concentration of urban earthquake transportation exposure. Cascadia presents the largest potential multi-state disruption. Alaska combines intense seismicity with limited alternative routes. Utah and Memphis show that significant travel risk also exists well beyond the Pacific Coast.

America’s earthquake threat is ultimately a transportation problem as much as a geological one. Strong shaking becomes especially disruptive when active faults cross crowded cities, mountain passes, bridges, ports, airports, and interstate corridors. California remains the clearest hotspot because seismic exposure overlaps with enormous travel networks. Cascadia could create the broadest regional shutdown, affecting Washington and Oregon simultaneously. Anchorage, Salt Lake City, Hawaii, and Memphis add major risks beyond those areas. The answer is stronger infrastructure planning, emergency preparation, and traveler awareness. These measures matter because damaged connections can isolate communities and disrupt journeys long after shaking has stopped.

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