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1964 Alaska earthquake

1964 Alaska earthquake
Fourth Avenue in Anchorage, Alaska, looking east from near Barrow Street. The southern edge of one of several landslides in Anchorage, this one covered an area of over a dozen blocks, including 5 blocks along the north side of Fourth Avenue. Most of the area was razed and made an urban renewal district.
Date 27 March 1964 (1964-03-27) (AKST)
Magnitude 9.2 Mw[1]
Depth 14 miles (23 km)
Type Megathrust
Areas affected United States, Canada
Total damage $311 million
Max. intensity XI (Extreme)
Peak acceleration 0.18 g
Casualties 139 killed

The 1964 Alaskan earthquake, also known as the Great Alaskan earthquake and Good Friday earthquake, occurred at 5:36 P.M. AST on Good Friday, March 27.[2] Across south-central Alaska, ground fissures, collapsing structures, and tsunamis resulting from the earthquake caused about 139 deaths.[3]

Lasting four minutes and thirty-eight seconds, the magnitude 9.2 megathrust earthquake was the most powerful recorded in North American history, and the second most powerful recorded in world history. Soil liquefaction, fissures, landslides, and other ground failures caused major structural damage in several communities and much damage to property. Anchorage sustained great destruction or damage to many inadequately earthquake engineered houses, buildings, and infrastructure (paved streets, sidewalks, water and sewer mains, electrical systems, and other man-made equipment), particularly in the several landslide zones along Knik Arm. Two hundred miles southwest, some areas near Kodiak were permanently raised by 30 feet (9.1 m). Southeast of Anchorage, areas around the head of Turnagain Arm near Girdwood and Portage dropped as much as 8 feet (2.4 m), requiring reconstruction and fill to raise the Seward Highway above the new high tide mark.

In Prince William Sound, Port Valdez suffered a massive underwater landslide, resulting in the deaths of 30 people between the collapse of the Valdez city harbor and docks, and inside the ship that was docked there at the time. Nearby, a 27-foot (8.2 m) tsunami destroyed the village of Chenega, killing 23 of the 68 people who lived there; survivors out-ran the wave, climbing to high ground. Post-quake tsunamis severely affected Whittier, Seward, Kodiak, and other Alaskan communities, as well as people and property in British Columbia, Washington, Oregon, and California.[4] Tsunamis also caused damage in Hawaii and Japan. Evidence of motion directly related to the earthquake was reported from all over the earth.


  • Geology 1
  • Tsunamis 2
  • Death toll, damage, and casualties 3
    • Anchorage area 3.1
    • Elsewhere in Alaska 3.2
    • Canada 3.3
    • Elsewhere 3.4
  • Aftershocks 4
  • See also 5
  • References 6
    • General references 6.1
  • External links 7


At 5:36 p.m. Alaska Standard Time (3:36 a.m. March 28, 1964 UTC), a fault between the Pacific and North American plates ruptured near College Fjord in Prince William Sound. The epicenter of the earthquake was 12.4 mi (20 km) north of Prince William Sound, 78 miles (125 km) east of Anchorage and 40 miles (64 km) west of Valdez. The focus occurred at a depth of approximately 15.5 mi (25 km). Ocean floor shifts created large tsunamis (up to 220 feet (67 m) in height), which resulted in many of the deaths and much of the property damage.[5] Large rockslides were also caused, resulting in great property damage. Vertical displacement of up to 38 feet (11.5 m) occurred, affecting an area of 100,000 miles² (250,000 km²) within Alaska.

Studies of ground motion have led to a peak ground acceleration estimate of 0.14 - 0.18 g.[6]

The Alaska Earthquake was a subduction zone earthquake (megathrust earthquake), caused by an oceanic plate sinking under a continental plate. The fault responsible was the Aleutian Megathrust, a reverse fault caused by a compressional force. This caused much of the uneven ground which is the result of ground shifted to the opposite elevation.


Calculated travel time map for the tectonic tsunami produced by the 1964 Prince William Sound earthquake in Alaska. Tsunami Travel Times computed using TTT v3.1 (P. Wessel). Map does not show the height or strength of the waves, only the calculated travel times.

  • Red: 1-4 hour arrival times
  • Yellow: 5-6 hour arrival times
  • Green: 7-14 hour arrival times
  • Blue: 15-21 hour arrival times.

Two types of tsunamis were produced by this subduction zone earthquake. There was a tectonic tsunami produced in addition to about 20 smaller and local tsunamis. These smaller tsunami were produced by submarine and subaerial landslides and were responsible for the majority of the tsunami damage. Tsunami waves were noted in over 20 countries, including: Peru, New Zealand, Papua New Guinea, Japan, and Antarctica. The largest tsunami wave was recorded in Shoup Bay, Alaska, with a height of about 220 ft (67 m).[3]

Death toll, damage, and casualties

The largest landslide in Anchorage occurred along Knik Arm between Point Woronzof and Fish Creek, causing substantial damage to numerous homes in the Turnagain-By-The-Sea subdivision.
The ruin of Portage
A 2x6 plank driven through a ten-ply tire by the tsunami in Whittier.

As a result of the earthquake, 139 people are believed to have died:[3] Fifteen died as a result of the earthquake itself, 106 died from the subsequent tsunami in Alaska,[7] 5 died from the tsunami in Oregon, and 13 died from the tsunami in California. The quake was a reported XI on the modified Mercalli Intensity scale "indicating major structural damage, and ground fissures and failures".[8] Property damage was estimated at about $311 million[3] ($2.28 billion in current U.S. dollars).

USGS video explaining the earthquake and footage

Anchorage area

Most damage occurred in Anchorage, 75 mi (120 km) northwest of the epicenter. Anchorage was not hit by tsunamis, but

  • 1964 Good Friday Great Alaskan Earthquake – University of Arizona, Department of Geosciences
  • 1964 Great Alaska Earthquake – United States Geological Survey
  • The Effects of the March 28, 1964 Alaska Tsunami in British Columbia, Canada – George Pararas-Carayannis
  • The Great Alaska Earthquake of 1964 – Alaska Earthquake Information Center
  • The short film ALASKAN EARTHQUAKE (1966) is available for free download at the Internet Archive
  • Anchorage, AK Good Friday Earthquake, Mar 1964 –
  • Tsunami Anniversary – Oregon Field Guide
  • Fifty Years Since the Great Alaska Earthquake: The Role of First Responders in Catastrophic Disaster Planning – 113th United States Congress

External links

  • National Research Council, Committee On The Alaska Earthquake (1971–73). The Great Alaska Earthquake Of 1964. Washington: National Academy of Sciences. 
  • Geology, Seismology and Geodesy, Hydrology, Biology, Oceanography And Coastal Engineering, Engineering, Human Ecology, Summary and Recommendation

General references

  1. ^ USGS. "M9.2 - The Great Alaska Earthquake and Tsunami of March 27, 1964".  
  2. ^ US Geological Survey report on the earthquake
  3. ^ a b c d Tsunami Events Search - sorted by Date, Country,  
  4. ^ USC, Tsunami Research Group. "1964 Alaskan Tsunami". University of Southern California. Retrieved 18 July 2015. 
  5. ^ Historic Earthquakes: Prince William Sound, Alaska
  6. ^ National Research Council (U.S.). Committee on the Alaska Earthquake, The great Alaska earthquake of 1964, Volume 1, Part 1, National Academies, 1968 p. 285
  7. ^ The Great Alaskan Earthquake & Tsunamis of 1964, by the National Oceanic and Atmospheric Administration. Accessed 2009-06-23. Archived 2009-06-25.
  8. ^ Great Alaskan Quake of 1964- Retrieved 2014-06-10
  9. ^ Sozen, Mete A. and N. Norby Nielsen, 1973: Analysis of the failure of the Anchorage International Airport control tower. The great Alaska earthquake of 1964, Volume 3, Part 2, National Research Council (U.S.). Committee on the Alaska Earthquake, National Academy of Sciences, ISBN 0-309-01606-1.
  10. ^ "Tsunami runups in Canada in 1964". National Oceanic and Atmospheric Administration. 
  11. ^ Oregon’s pioneer spirit. Statesman Journal, December 26, 1999.
  12. ^ a b USGS Release: 40th Anniversary of "Good Friday" Earthquake Offers New Opportunities for Public and Building Safety Partnerships (3/26/2004)
  13. ^ "Tsunami runups in Freeport".  
  14. ^ "Everglades Chekika: Fountain".  


See also

There were hundreds of aftershocks in the first weeks following the main shock. In the first day alone, eleven major aftershocks were recorded with a magnitude greater than 6.0. Nine more struck over the next three weeks. In all, thousands of aftershocks occurred in the months following the quake, and smaller aftershocks continued to strike the region for more than a year.[12]


Twelve people were killed by the tsunami in or near Crescent City, California, while four children were killed on the Oregon coast at Beverly Beach State Park.[11] Other coastal towns in the U.S. Pacific Northwest and Hawaii were damaged. Minor damage to boats occurred as far south as Los Angeles.[12] Effects of the earthquake were even noted as far east as Texas. Tide gauges in Freeport recorded waves similar to seismic surface waves.[13] In the Florida Everglades, an artesian aquifer located near Lake Chekika saw its water flow rate double from 3 million gallons per day to 6 million gallons per day, 60 to 90 minutes after the first shock of the earthquake.[14]

A winter scene of a "Ghost forest" that was killed and preserved by salt water along with ruined buildings at the site of the former town of Portage, 2011


A 4.5 ft (1.4 m) wave reached Prince Rupert, British Columbia, just south of the Alaska Panhandle, about three hours after the earthquake. The tsunami then reached Tofino, on the exposed west coast of Vancouver Island, and traveled up a fjord to hit Port Alberni twice, washing away 55 homes and damaging 375 others. The towns of Hot Springs Cove, Zeballos, and Amai also saw damage.[10] The damage in British Columbia was estimated at $10 million Canadian (or $77.6 million in today's Canadian dollars, or $76 million in today's U.S. dollars).


Most coastal towns in the Prince William Sound, Kenai Peninsula, and Kodiak Island areas, especially the major ports of Seward, Whittier and Kodiak were heavily damaged by a combination of seismic activity, subsidence, post-quake tsunamis and/or earthquake-caused fires. Valdez was not totally destroyed, but after three years, the town relocated to higher ground 7 km (4 mi) west of its original site. Some Alaska Native villages, including Chenega and Afognak, were destroyed or damaged. The earthquake caused the Cold-War era ballistic missile detection radar of Clear Air Force Station to go offline for six minutes, the only unscheduled interruption in its operational history. Near Cordova, the Million Dollar Bridge crossing the Copper River also collapsed. The community of Girdwood was also confined to the southern side of the Seward Highway when water rushed into Turnagain Arm and flooded or destroyed any buildings left standing to the north of the highway. Interestingly, only the ground immediately along the highway and that on the north side of the road dropped, prompting geologists to speculate that Girdwood may rest upon an ancient cliff face, now covered by countless thousands of years of sediment and glacial deposits.

Elsewhere in Alaska

The hamlets of Girdwood and Portage, located 30 and 40 mi (60 km) southeast of central Anchorage on the Turnagain Arm, were destroyed by subsidence and subsequent tidal action. Girdwood was relocated inland and Portage was abandoned. About 20 miles (32 km) of the Seward Highway sank below the high-water mark of Turnagain Arm; the highway and its bridges were raised and rebuilt in 1964-66.

One house on W. 10th Avenue suffered peripheral damage, but only one block away the recently completed (and still unoccupied) Four Seasons Building on Ninth Avenue collapsed completely, with the concrete elevator shafts sticking up out of the rubble like a seesaw.


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