1964 Alaska earthquake

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1964 Alaska earthquake
AlaskaQuake-FourthAve.jpg
Fourth Avenue in Anchorage, Alaska, looking east from near C Street. The southern edge of one of several landslides in Anchorage, this one covered an area of over a dozen blocks, including five blocks along the north side of Fourth Avenue. Most of the area was razed and made an urban renewal district.
Relief map of USA Alaska.png
Green pog.svg
Anchorage
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UTC  time1964-03-28 03:36:16
ISC  event 869809
USGS-ANSS ComCat
Local dateMarch 27, 1964 (1964-03-27)
Local time17:36:16 AKST [a]
Duration4–5 minutes
Magnitude Mw 9.2–9.3
Depth25 kilometers (16 mi)
Epicenter 60°54′29″N147°20′20″W / 60.908°N 147.339°W / 60.908; -147.339
Type Megathrust
Areas affectedUnited States, Canada
Total damage$311 million (1964 USD) [$2.94 billion (2022 USD)]
Max. intensity MMI X (Extreme)
Peak acceleration~ 0.18 g [1]
TsunamiMajor. Run-up of 67 m (220 ft) at Shoup Bay, Alaska.
Casualties131

The 1964 Alaska earthquake, also known as the Great Alaska earthquake and Good Friday earthquake, occurred at 5:36 PM AKST on Good Friday, March 27, 1964. [2] Across south-central Alaska, ground fissures, collapsing structures, and tsunamis resulting from the earthquake caused about 131 deaths. [3]

Contents

Lasting four minutes and thirty-eight seconds, the magnitude 9.2–9.3megathrust earthquake remains the most powerful earthquake ever recorded in North America, [2] [4] and the second most powerful earthquake ever recorded in the world since modern seismography began in 1900. [5] Six hundred miles (970 km) of fault ruptured at once and moved up to 60 ft (18 m), releasing about 500 years of stress buildup. 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 (320 km) southwest, some areas near Kodiak were permanently raised by 30 feet (9 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 32 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. The 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. [6] Tsunamis also caused damage in Hawaii and Japan. Evidence of motion directly related to the earthquake was also reported from Florida and Texas.

Geology

On March 27, 1964, at 5:36 p.m. AKST (March 28, at 3:36 a.m. UTC), [a] 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 (20.0 km) north of Prince William Sound, 78 miles (126 km) east of Anchorage and 40 miles (64 km) west of Valdez. The focus occurred at a depth of approximately 15.5 mi (24.9 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. [7] Large rockslides were also caused, resulting in great property damage. Vertical displacement of up to 38 feet (12 m) occurred, affecting an area of 100,000 square miles (260,000 km2) within Alaska.

Studies of ground motion have led to a peak ground acceleration estimate of 0.14–0.18 g . [8] The earthquake was assigned a maximum Modified Mercalli intensity of X (Extreme). Shaking was felt across much of Alaska and parts of western Yukon and British Columbia in Canada. [9]

The Alaska earthquake was a subduction zone (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. [10] Uplift occurred across 520,000 km2 (200,000 sq mi) from southern Kodiak to Prince William Sound and further east of the sound. The maximum uplift was in Montague Island, where the ground was raised 13–15 m (43–49 ft) relative to sea level. The uplift also affected Kodiak, Sitkalidak, and Sitkinak islands. Subsidence was observed for 285,000 km2 (110,000 sq mi) from north and west of the sound, in Chugach Mountains, most of Kenai Peninsula, and almost all the Kodiak Island group. [9]

Tsunami

Calculated travel time map for the tectonic tsunami produced by the 1964 Prince William Sound earthquake in Alaska. Tsunami Travel Times computed using Tsunami Travel Times software v3.1 (P. Wessel). The map does not show the height or strength of the waves, only the calculated travel times. .mw-parser-output .plainlist ol,.mw-parser-output .plainlist ul{line-height:inherit;list-style:none;margin:0;padding:0}.mw-parser-output .plainlist ol li,.mw-parser-output .plainlist ul li{margin-bottom:0} @media screen{html.skin-theme-clientpref-night .mw-parser-output div:not(.notheme)>.tmp-color,html.skin-theme-clientpref-night .mw-parser-output p>.tmp-color,html.skin-theme-clientpref-night .mw-parser-output table:not(.notheme) .tmp-color{color:inherit!important}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output div:not(.notheme)>.tmp-color,html.skin-theme-clientpref-os .mw-parser-output p>.tmp-color,html.skin-theme-clientpref-os .mw-parser-output table:not(.notheme) .tmp-color{color:inherit!important}} Red: 1- to 4-hour arrival times Yellow: 5- to 6-hour arrival times Green: 7- to 14-hour arrival times Blue: 15- to 21-hour arrival times. Calculated Travel Time Map for 1964 Alaska Tsunami.jpg
Calculated travel time map for the tectonic tsunami produced by the 1964 Prince William Sound earthquake in Alaska. Tsunami Travel Times computed using Tsunami Travel Times software v3.1 (P. Wessel). The map does not show the height or strength of the waves, only the calculated travel times.

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

Two types of tsunami were produced by this subduction zone earthquake. There was a tectonic tsunami produced in addition to about 20 smaller and local tsunamis. These smaller tsunamis 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, Mexico, and in the continent of Antarctica. The largest tsunami wave was recorded in Shoup Bay, Alaska, with a height of about 220 ft (67 m). [3] [12]

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. Good Friday Earthquake at Turnagain Arm.jpg
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 Subsidence at portage.jpg
The ruin of Portage
A plank driven through a tire by the tsunami in Whittier AlaskaQuake-Tire.jpg
A plank driven through a tire by the tsunami in Whittier
The 5-story JCPenney department store in Anchorage in 1964, following the earthquake. 1964 Alaska Quake Penney Bldg.jpg
The 5-story JCPenney department store in Anchorage in 1964, following the earthquake.

As a result of the earthquake, 131 people are believed to have died: [3] Nine died as a result of the earthquake itself and another 122 died from the subsequent tsunamis all over the world. [13] Five died from the tsunami in Oregon, [14] and 12 died from the tsunami in Crescent City, California. [15] [16] Property damage was estimated at $116 million [3] ($0.87 billion in 2023 dollars). [17]

United States Geological Survey video explaining the earthquake and footage

Anchorage area

Most damage occurred in Anchorage, 75 mi (121 km) northwest of the epicenter. Anchorage was not hit by tsunamis, but downtown Anchorage was heavily damaged, and parts of the city built on sandy bluffs overlying "Bootlegger Cove clay" near Cook Inlet, most notably the Turnagain neighborhood, suffered landslide damage. The neighborhood lost 75 houses in the landslide, and the destroyed area has since been turned into Earthquake Park. [18] The Government Hill school suffered from the Government Hill landslide, leaving it in two jagged, broken pieces. Land overlooking the Ship Creek valley near the Alaska Railroad yards also slid, destroying many acres of buildings and city blocks in downtown Anchorage. Most other areas of the city were only moderately damaged. The 60-foot (18 m) concrete control tower at Anchorage International Airport was not engineered to withstand earthquake activity and collapsed, killing William George Taylor, the Federal Aviation Agency air traffic controller on duty in the tower cab at the time the earthquake began. [19]

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.

The hamlets of Girdwood and Portage, located 30 and 40 mi (48 and 64 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.

Elsewhere in Alaska

Kodiak before and after the earthquake 1964 Alaska Quake Kodiak Before and After.jpg
Kodiak before and after the earthquake
The Valdez townsite was abandoned and relocated following the 1964 earthquake and was used as a pipe yard for the construction of the Trans-Alaska Pipeline System, as shown in this 1974 photo Alaska pipeline route near Valdez River.jpg
The Valdez townsite was abandoned and relocated following the 1964 earthquake and was used as a pipe yard for the construction of the Trans-Alaska Pipeline System, as shown in this 1974 photo

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 with 32 dead was not totally destroyed, but after three years, the town relocated to higher ground four miles (6.4 km) west of its original site. Some Alaska Native villages, including Chenega and Afognak, were destroyed or damaged.[ citation needed ] The earthquake caused the ballistic missile detection radar of Clear Air Force Station to go offline for six minutes, [20] the only unscheduled interruption in its operational history. Near Cordova, the Million Dollar Bridge crossing the Copper River also suffered damage, with Span #4 slipping off its pylon and collapsing. 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. 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 covered by thousands of years of sediment and glacial deposits.[ citation needed ]

Canada

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. [21] The damage in British Columbia was estimated at CA$10 million ($96 million in 2023 Canadian dollars or $91 million in 2023 US dollars). [22] [23] [24]

Elsewhere

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 Portagetoday.JPG
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

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. [25] Other coastal towns in the U.S. Pacific Northwest and Hawaii were damaged. Minor damage to boats occurred as far south as Los Angeles. [26] Effects of the earthquake were even noted as far east as Freeport, Texas, where tide gauges recorded waves similar to seismic surface waves. [27] Seiches were detected in wells in countries around the world, including England, Namibia, and Australia. [28]

Aftershocks

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. [26]

1964 Alaska earthquake
Main shock and aftershocks from 1964-1-1 to 1964-12-31 (map data)

Recovery efforts

Alaska had never experienced a major disaster in a highly populated area before, and had very limited resources for dealing with the effects of such an event. In Anchorage, at the urging of geologist Lidia Selkregg, the City of Anchorage and the Alaska State Housing Authority appointed a team of 40 scientists, including geologists, soil scientists, and engineers, to assess the damage done by the earthquake to the city. [29] The team, called the Engineering and Geological Evaluation Group, was headed by Dr. Ruth A. M. Schmidt, a geology professor at the University of Alaska Anchorage. The team of scientists came into conflict with local developers and downtown business owners who wanted to immediately rebuild; the scientists wanted to identify future dangers to ensure that rebuilt infrastructure would be safe. [30] The team produced a report on May 8, 1964, just a little more than a month after the earthquake. [29] [31]

The United States military, which has a large active presence in Alaska, also stepped in to assist within moments of the end of the quake. The U.S. Army rapidly re-established communications with the lower 48 states, deployed troops to assist the citizens of Anchorage, and dispatched a convoy to Valdez. [32] On the advice of military and civilian leaders, President Lyndon B. Johnson declared all of Alaska a major disaster area the day after the quake.

The U.S. Navy and U.S. Coast Guard deployed ships to isolated coastal communities to assist with immediate needs. Bad weather and poor visibility hampered air rescue and observation efforts the day after the quake, but on Sunday the 29th the situation improved and rescue helicopters and observation aircraft were deployed. [32] A military airlift immediately began shipping relief supplies to Alaska, eventually delivering 2,570,000 pounds (1,170,000 kg) of food and other supplies. [33]

Broadcast journalist Genie Chance assisted in recovery and relief efforts, staying on the KENI air waves over Anchorage for more than 24 continuous hours as the voice of calm from her temporary post within the Anchorage Public Safety Building. [34] She was effectively designated as the public safety officer by the city's police chief. [34] Chance provided breaking news of the catastrophic events that continued to develop following the magnitude 9.2 earthquake, and she served as the voice of the public safety office, coordinating response efforts, connecting available resources to needs around the community, disseminating information about shelters and prepared food rations, passing messages of well-being between loved ones, and helping to reunite families. [35]

In the longer term, the U.S. Army Corps of Engineers led the effort to rebuild roads, clear debris, and establish new townsites for communities that had been completely destroyed, at a cost of $110 million. [33] The West Coast and Alaska Tsunami Warning Center was formed as a direct response to the disaster. Federal disaster relief funds paid for reconstruction as well as financially supporting the devastated infrastructure of Alaska's government, spending hundreds of millions of dollars that helped keep Alaska financially solvent until the discovery of massive oil deposits at Prudhoe Bay. At the order of the U.S. Defense Department, the Alaska National Guard founded the Alaska Division of Emergency Services to respond to any future disasters. [32]

See also

Notes

  1. 1 2 At the time of the disaster, Alaska was divided between four separate time zones, Anchorage was five hours behind Eastern Standard Time. See Time in Alaska.

Related Research Articles

<span class="mw-page-title-main">Alaska</span> U.S. state

Alaska is a non-contiguous U.S. state on the northwest extremity of North America. Part of the Western United States region, it is one of the two non-contiguous U.S. states, alongside Hawaii. Alaska is also considered to be the northernmost, westernmost, and easternmost state in the United States. It borders the Canadian territory of Yukon and the province of British Columbia to the east. It shares a western maritime border, in the Bering Strait, with Russia's Chukotka Autonomous Okrug. The Chukchi and Beaufort Seas of the Arctic Ocean lie to the north, and the Pacific Ocean lies to the south. Technically, it is a semi-exclave of the U.S., and is the largest exclave in the world.

<span class="mw-page-title-main">Valdez, Alaska</span> Town in Alaska

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<span class="mw-page-title-main">Prince William Sound</span> Sound of the Gulf of Alaska

Prince William Sound is a sound off the Gulf of Alaska on the south coast of the U.S. state of Alaska. It is located on the east side of the Kenai Peninsula. Its largest port is Valdez, at the southern terminus of the Trans-Alaska Pipeline System. Other settlements on the sound, which contains numerous small islands, include Cordova and Whittier plus the Alaska native villages of Chenega and Tatitlek.

<span class="mw-page-title-main">Cook Inlet</span> Inlet from the Gulf of Alaska

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<span class="mw-page-title-main">Girdwood, Anchorage, Alaska</span> Resort town in Alaska, United States

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<span class="mw-page-title-main">Cascadia subduction zone</span> Convergent plate boundary that stretches from northern Vancouver Island to Northern California

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The 2012 Haida Gwaii earthquake occurred just after 8:04 p.m. PDT on October 27. The shock had a moment magnitude of 7.8 and a maximum Mercalli Intensity of V (Moderate). The earthquake's epicentre was on Moresby Island of the Haida Gwaii archipelago. This was the second largest Canadian earthquake ever recorded by a seismometer, after the 1949 Queen Charlotte Islands earthquake, about 135 kilometres (84 mi) away. One person died due to a car crash related to the tsunami in Oahu, Hawaii.

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On November 30, 2018, at 8:29 a.m. AKST (17:29 UTC), a magnitude 7.1 earthquake hit Anchorage in South Central Alaska. The earthquake's epicenter was near Point Mackenzie, about 10 miles (16 km) north of Anchorage, and occurred at a depth of 29 miles (47 km). It was followed six minutes later by a magnitude 5.7 aftershock centered 2.5 miles (4.0 km) north-northwest of the municipality. The earthquake could be felt as far away as Fairbanks.

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The 1979 Saint Elias earthquake affected Alaska at 12:27 AKST on 28 February. The thrust-faulting Mw 7.5 earthquake had an epicenter in the Chugach Range. Though the maximum recorded Modified Mercalli intensity was VII, damage was minimal and there were no casualties due to the remoteness of the faulting. Damage also extended across the border in parts of Yukon, Canada.

References

Specific

  1. ↑ 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
  2. 1 2 ANSS. "iscgem869809 M 9.2 – The 1964 Prince William Sound, Alaska Earthquake". Comprehensive Catalog. U.S. Geological Survey.
  3. 1 2 3 4 Tsunami Events Search – sorted by Date, Country, National Geophysical Data Center, archived from the original on 2017-08-25, retrieved 2014-01-09
  4. ↑ Ichinose, Gene; Somerville, Paul; Thio, Hong Kie; Graves, Robert; O'Connell, Dan (2007). "Rupture process of the 1964 Prince William Sound, Alaska, earthquake from the combined inversion of seismic, tsunami, and geodetic data". Journal of Geophysical Research: Solid Earth. 112 (B7). doi:10.1029/2006JB004728. ISSN   0148-0227.
  5. ↑ ISC (2022), ISC-GEM Global Instrumental Earthquake Catalogue (1904–2018), Version 9.1, International Seismological Centre
  6. ↑ USC, Tsunami Research Group. "1964 Alaskan Tsunami". University of Southern California. Archived from the original on 8 May 2015. Retrieved 18 July 2015.
  7. ↑ Historic Earthquakes: Prince William Sound, Alaska Archived 2014-10-11 at the Wayback Machine
  8. ↑ National Research Council (U.S.). Committee on the Alaska Earthquake, The great Alaska earthquake of 1964, Volume 1, Part 1 Archived 2020-01-05 at the Wayback Machine , National Academies, 1968 p. 285
  9. 1 2 Stover, C. W.; Coffman, J.L. (1993). Seismicity of the United States, 1568-1989 (revised) (USGS Numbered Series). Professional Paper. doi:10.3133/pp1527.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  10. ↑ The Great Alaska Earthquake of 1964 and Its Legacy Archived 2018-12-01 at the Wayback Machine 27 March 2014
  11. ↑ "Geoware Tsunami Products". geoware-online.com. Archived from the original on 2018-06-28. Retrieved 2018-06-21.
  12. ↑ "Getting Ready to Rumble", Richard Conniff, The Wall Street Journal, August 26, 2017.
  13. ↑ The Great Alaskan Earthquake & Tsunamis of 1964, by the National Oceanic and Atmospheric Administration. Accessed 2009-06-23. Archived 2009-06-25.
  14. ↑ "Tsunami generated by Good Friday quake devastated Oregon Coast 50 years ago Thursday". OregonLive.com. 24 March 2014. Archived from the original on 28 July 2018. Retrieved 2018-07-27.
  15. ↑ "The day in 1964 when a tsunami ravaged Crescent City". San Francisco Chronicle. 23 January 2018. Archived from the original on 29 December 2019. Retrieved 2020-04-09.
  16. ↑ "Remembering the Deadly 75-Foot Tidal Wave that Leveled Crescent City in 1964". activenorcal.com. 20 August 2019. Retrieved 2020-04-09.
  17. ↑ Johnston, Louis; Williamson, Samuel H. (2023). "What Was the U.S. GDP Then?". MeasuringWorth . Retrieved November 30, 2023. United States Gross Domestic Product deflator figures follow the MeasuringWorth series.
  18. ↑ "Earthquake Park | Things to Do in Anchorage". ALASKA.ORG. Retrieved 2021-05-03.
  19. ↑ 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.
  20. ↑ McCann, Chris (24 March 2014). "50 YEARS since 1964 earthquake catastrophe: Military integral to recovery". Pacific Air Forces . Retrieved 12 May 2024.
  21. ↑ "Tsunami runups in Canada in 1964". National Oceanic and Atmospheric Administration. Archived from the original on 2017-11-07. Retrieved 2014-01-03.
  22. ↑ 1688 to 1923: Geloso, Vincent, A Price Index for Canada, 1688 to 1850 (December 6, 2016). Afterwards, Canadian inflation numbers based on Statistics Canada tables 18-10-0005-01 (formerly CANSIM 326-0021) "Consumer Price Index, annual average, not seasonally adjusted". Statistics Canada. Retrieved April 17, 2021. and table 18-10-0004-13 "Consumer Price Index by product group, monthly, percentage change, not seasonally adjusted, Canada, provinces, Whitehorse, Yellowknife and Iqaluit". Statistics Canada. Retrieved 2024-05-08.
  23. ↑ 1634–1699: McCusker, J. J. (1997). How Much Is That in Real Money? A Historical Price Index for Use as a Deflator of Money Values in the Economy of the United States: Addenda et Corrigenda (PDF). American Antiquarian Society. 1700–1799: McCusker, J. J. (1992). How Much Is That in Real Money? A Historical Price Index for Use as a Deflator of Money Values in the Economy of the United States (PDF). American Antiquarian Society. 1800–present: Federal Reserve Bank of Minneapolis. "Consumer Price Index (estimate) 1800–" . Retrieved February 29, 2024.
  24. ↑ "A brief history of the Canadian dollar". Archived from the original on 2016-12-25. Retrieved 2018-01-11.
  25. ↑ Oregon's pioneer spirit. Statesman Journal, December 26, 1999.
  26. 1 2 "USGS Release: 40th Anniversary of "Good Friday" Earthquake Offers New Opportunities for Public and Building Safety Partnerships (3/26/2004)". Archived from the original on 2006-09-27. Retrieved 2006-11-19.
  27. ↑ "Tsunami runups in Freeport". National Oceanic and Atmospheric Administration. Archived from the original on 2017-11-07. Retrieved 2014-01-04.
  28. ↑ Fountain, Henry (2017). The Great Quake: How the biggest earthquake in North America changed our understanding of the planet. New York: Crown. p. 145.
  29. 1 2 Friedel, Megan K. (2010). Guide to the Anchorage Engineering Geology Evaluation Group papers, 1964. UAA/APU Consortium Library Archives and Special Collections. HMC-0051. https://archives.consortiumlibrary.org/collections/specialcollections/hmc-0051/ Archived 2019-03-28 at the Wayback Machine
  30. ↑ "Ruth Anne Marie Schmidt Ph.D." Alaska Women's Hall of Fame. 2015. Retrieved November 23, 2015.
  31. ↑ Saucier, Heather (April 2014). "PROWESS Honors Historic Earthquake Survivor". American Association of Petroleum Geologists. Retrieved July 31, 2018.
  32. 1 2 3 Cloe, John Haile "Helping Hand" Military response to Good Friday earthquake Archived 2016-10-27 at the Wayback Machine Alaska Historical Society, 3/4/2014
  33. 1 2 Galvin, John Great Alaskan Earthquake and Tsunami: Alaska, March 1964 Archived 2016-10-27 at the Wayback Machine Popular Mechanics , 6/29/2007
  34. 1 2 "When a Quake Shook Alaska, a Radio Reporter Led the Public Through the Devastating Crisis". Smithsonian Magazine. Retrieved 2020-12-02.
  35. ↑ Barbaro, Michael (May 22, 2020). "Genie Chance and the Great Alaska Earthquake". The New York Times.

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