Shortly before noon on Wednesday, April 13, 1949, an earthquake rocked the area from British Columbia to Oregon and caused extensive damage. Seven people died and at least 64 were injured in the heaviest shock ever recorded in the region. In Seattle, downtown streets and buildings were jammed with people but no deaths occurred. As soon as the ground began to shake, photographer Ken Harris headed out the door for Pioneer Square, where he predicted damage would be extensive. His front page photo shows the bricks that cascaded from the cornice of the Seattle Hotel at First and Yesler Way, damaging at least five automobiles. At least a half a dozen buildings in the Pioneer Square area had damage to cornices or walls. Ken Harris/Seattle Post-Intelligencer
Take a look at three key indicators of how well Seattle neighborhoods will survive a serious earthquake. First, these Seattle neighborhoods are most likely to see liquefaction in a major shaker.
GENNA MARTIN/SEATTLEPI.COM
Alki – Higher risk of land movement during an earthquake. GRANT HINDSLEY/SEATTLEPI.COM
Blue Ridge – Higher risk of land movement during an earthquake. Courtesy Tere Foster and Moya Skillman/Windermere Real Estate
Loyal Heights – Higher risk of land movement during an earthquake. Scott Eklund/Seattle Post-Intelligencer
Magnolia – Higher risk of land movement during an earthquake. DANIEL DEMAY/SEATTLEPI.COM
Queen Anne – Higher risk of land movement during an earthquake.
South Park – Higher risk of land movement during an earthquake. JOSHUA TRUJILLO/SEATTLEPI.COM
Sunset Hill – Higher risk of land movement during an earthquake. Seattle Municipal Archive
The Duwamish industrial area – Highest risk of land movement
during an earthquake.
Elliott Bay waterfront – Highest risk of land movement during an earthquake.
Georgetown – Higher risk of land movement during an earthquake. GRANT HINDSLEY/SEATTLEPI.COM
Harbor Island – Highest risk of land movement during an earthquake. GRANT HINDSLEY/SEATTLEPI.COM
Interbay – Highest risk of land movement during an earthquake. JORDAN STEAD/SEATTLEPI.COM
Montlake – Highest risk of land movement during an earthquake. (That's the moment the Montlake Cut joined Lake Washington and Lake Union.) Asahel Curtis / Courtesy of the Washington State Archives
Pioneer Square – Highest risk of land movement during an earthquake. MIKE URBAN/SEATTLE POST-INTELLIGENCER
Sodo – Highest risk of land movement during an earthquake.
Grant Hindsley/SEATTLEPI.COM
University of Washington – Highest risk of land movement during an earthquake. JOSHUA TRUJILLO/SEATTLEPI.COM
Seattle is rotten with unreinforced brick buildings. Continue on for a look at how the city’s neighborhoods rank when it comes to the riskiest masonry buildings.
Wallingford – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. rutlo, Creative Commons Flickr
Sunset Hill/Loyal Heights – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. JOSHUA TRUJILLO/SEATTLEPI.COM
Seward Park – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. PAUL JOSEPH BROWN/P-I
Rainier Beach – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. GENNA MARTIN/SEATTLEPI.COM
North Capitol Hill – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. JORDAN STEAD/SEATTLEPI.COM
Mount Baker – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. Gilbert W. Arias/Seattle Post-Intelligencer
Fremont – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records.
GRANT HINDSLEY, SEATTLEPI.COM
Fauntleroy/Seaview – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. JORDAN STEAD/SEATTLEPI.COM
Cascade/Eastlake – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. P-I file
Beacon Hill – This Seattle neighborhood has one large unreinforced masonry building that appears to not have been retrofitted, according to city records. GRANT HINDSLEY/SEATTLEPI.COM
Whittier Heights – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records. JORDAN STEAD/SEATTLEPI.COM
Ravenna/Bryant – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records. JOSHUA TRUJILLO/SEATTLEPI.COM
North Beacon Hill/Jefferson Park – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records. Seattle Municipal Archive
Miller Park – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records. Karen Ducey/Seattle Post-Intelligencer
Madrona/Leschi – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records.
Madison Park – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records. Seattle Municipal Archive
Judkins Park – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records. JOSHUA TRUJILLO/SEATTLEPI.COM
Greenwood/Phinney Ridge – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records. GENNA MARTIN/SEATTLEPI.COM
Belltown – This Seattle neighborhood has two large unreinforced masonry building that appears to not have been retrofitted, according to city records. GRANT HINDSLEY/SEATTLEPI.COM
Central Area/Squire Park – This Seattle neighborhood has three large unreinforced masonry building that appears to not have been retrofitted, according to city records. GENNA MARTIN/SEATTLEPI.COM
Pioneer Square/Chinatown-International District – This Seattle neighborhood has four large unreinforced masonry building that appears to not have been retrofitted, according to city records. JORDAN STEAD/SEATTLEPI.COM
Green Lake – This Seattle neighborhood has four large unreinforced masonry building that appears to not have been retrofitted, according to city records. JOSHUA TRUJILLO/SEATTLEPI.COM
Downtown – This Seattle neighborhood has four large unreinforced masonry building that appears to not have been retrofitted, according to city records. LACEY YOUNG/SEATTLEPI.COM
Ballard – This Seattle neighborhood has four large unreinforced masonry building that appears to not have been retrofitted, according to city records.
GRANT HINDSLEY, SEATTLEPI.COM
First Hill – This Seattle neighborhood has five large unreinforced masonry building that appears to not have been retrofitted, according to city records. GRANT HINDSLEY/SEATTLEPI.COM
Duwamish/SODO – This Seattle neighborhood has five large unreinforced masonry building that appears to not have been retrofitted, according to city records.
GRANT HINDSLEY, SEATTLE PI.COM
University District – This Seattle neighborhood has eight large unreinforced masonry building that appears to not have been retrofitted, according to city records. GENNA MARTIN/SEATTLEPI.COM
Queen Anne – This Seattle neighborhood has 11 large unreinforced masonry building that appears to not have been retrofitted, according to city records. GRANT HINDSLEY/SEATTLEPI.COM
Capitol Hill – This Seattle neighborhood has 12 large unreinforced masonry building that appears to not have been retrofitted, according to city records. GENNA MARTIN/SEATTLEPI.COM
Finally, the U.S. Geological Survey has identified nine key infrastructure areas at risk in a large Puget Sound quake. Take a look at them. JOSHUA TRUJILLO/SEATTLEPI.COM
Water – The USGS notes that all three of the region’s largest water systems are supplied by long pipelines to lakes in the Cascades. Most cross river valleys with soft, shifty soils.
Waste – Sewage in the Seattle area also has a long way to go. Most of south King County’s sewage flows in pipe along the Duwamish. Snohomish and Pierce counties have similar systems, and all are susceptible to break in a large quake.
Seattle Municipal Archives
Power – The USGS notes that there is a “significant level of redundancy” in the Puget Sound electrical grid. Roy Musitelli/AP
Natural gas – The region’s natural gas is piped south from Canada. The main lines pass east of the urban centers, though distribution lines are everywhere. Phil H. Webber/Seattle Post-Intelligencer
Liquid fuel – Fuel from northwest Washington refineries is piped south through Bellevue and much of the Eastside. About 75 percent of the region’s gas moves through them. GRANT HINDSLEY/SEATTLEPI.COM
Highways – And you thought traffic was bad now. GRANT HINDSLEY/SEATTLEPI.COM
Railroads – Many of the region’s railroad bridges are more than a century old, and most of the Seattle-Tacoma line was built on liquefiable fill. Landslides are already common north of Seattle, and could intensify in a quake.
Airports – Boeing Field sits on loose dirt, but the rest of the region’s airports sit on what the USGS describes approvingly as “competent soils.” JOSHUA TRUJILLO/SEATTLEPI.COM
Ports – The ports at Seattle and Tacoma were both built on old estuaries. They’re highly unstable and will not do well in a large quake. GENNA MARTIN/SEATTLEPI.COM
Click through the slideshow to see the most powerful earthquakes in U.S. history.
American Stock Archive/Getty Images
Near Islands earthquake 1975 Magnitude: 7.6
No one died in this quake off of sparsely populated Attu Island, Alaska, but Shemya Air Force Base (now Eareckson Air Station) suffered major damage.
Google Maps
Lituya Bay earthquake 1958 Magnitude: 7.8
This quake in a fjord on the Alaskan panhandle triggered a massive rock slide in narrow Lituya Bay. The rock slide caused the largest tsunami in modern-day history, which killed five people.
Historical/Corbis via Getty Images
Alaska earthquake 2018 Magnitude: 7.9
Tuesday's earthquake near Kodiak Island prompted tsunami warnings and evacuations along the West Coast and in Hawaii, but there were no immediate reports of any injuries.
AP
Aleutian Islands earthquake 2014 Magnitude: 7.9
This quake off Alaska's Little Sitkin Island was too deep to produce a significant tsunami and, therefore, significant damage.
Google Maps
Denali earthquake 2002 Magnitude: 7.9
The largest U.S. earthquake in nearly 50 years, there were only a few injuries caused by the Denali quake, which caused minor damage to the Trans-Alaska Pipeline.
Kevin Fujii/Chronicle
San Francisco earthquake 1906 Magnitude: 7.9
The deadliest earthquake in U.S. history, the San Francisco quake -- and the fires it caused -- killed more than 3,000 people.
American Stock Archive/Getty Images
Hawaii earthquake 1868 Magnitude: 7.9
With an epicenter on Hawaii's big island, the largest earthquake in the state's history led to 77 deaths: 46 from tsunamis and 31 from landslides.
Google Maps
Fort Tejon earthquake 1857 Magnitude: 7.9
The largest earthquake in California history was felt as far away as Las Vegas. Scars along a 225-mile stretch of the southern San Andreas fault still remain.
Scott Haefner/AP
Andreanof Islands earthquake 1957 Magnitude: 8.6
A Hawaii-based pilot and photographer were killed when trying to document the tsunami caused by this huge Alaska quake.
Google Maps
Aelutian Islands earthquake 1946 Magnitude: 8.6
This Alaska quake triggered a massive tsunami that killed 165 people, including the unfortunate man pictured here in Hilo, Hawaii.
Historical/Corbis via Getty Images
Rat Islands earthquake 1965 Magnitude: 8.7
Another shake-up in the Aleutians, the Rat Islands quake was massive, but the only damage reported was cracked runways.
Smith Collection/Gado/Getty Images
Cascadia earthquake 1700 Magnitude: 8.7-9.2
A deadly tsunami in Japan wasn't connected to this U.S. quake -- which suddenly dropped the coastlines of Northern California, Oregon and Washington 36 feet -- until the 1990s.
Pacific Northwest Seismic Network
If you've noticed a quiet in the region's seismic activity, you're not alone. According to a new paper by researchers at the Pacific Northwest Seismic Network , researchers have also picked up on a strange lack of significant earthquakes in the region -- and they're not sure why .
Advertisement
Article continues below this ad
The last big quake to hit the area was the Nisqually quake, with a magnitude of 6.8, back in 2001. Washington hasn't had a major earthquake in a while, and that seems unusual to researchers .
Though there have been rumbles, tremors, and even swarms of quakes , there have only been nine earthquakes at magnitude 4 or grater since 2009 in the Pacific Northwest, outside of those at Mount St. Helens or on the Cascadia Subduction Zone.
That's significantly less than the decade before that, which had 14 -- which is already less in turn than between 1989 and 1999, when there were 24.
Advertisement
Article continues below this ad
"The largest event in the past decade was also smaller than the largest event in any previous decade," wrote Stephen Malone, professor at the University of Washington's Earth and Space Sciences department. "It seems inescapable that strong seismicity has taken a break."
What the paper can't conclude is exactly what the cause is. Malone, who is also a former director of the PNSN, noted that it is "beyond the purview of this opinion piece" to say confidently what the possible causes for the calm is.
He does note a number of possibilities though, including differing kinds of seismograms and ranges of magnitude between PNSN and other agencies that monitor this sort of thing, or a general lack of historical data to see a larger pattern forming. There's also a slight correlation in leadership at the PNSN, which could affect how data is read and reported.
Advertisement
Article continues below this ad
"Although the recent quiescence in the PNW described here may be just random chance, it is possible that it fits into some model of seismicity variability on a regional scale," Malone wrote. "Alternatively, with a new director (Harold Tobin) having just taken over leadership of the PNSN, we have the opportunity to test the hypothesis that regime change can have a profound effect on seismicity."
In an interview with Northwest Public Broadcasting, Tobin told reporters that scientists are coming around to the idea that there may be a non-random cycle for earthquakes to follow.
Advertisement
Article continues below this ad
"The essential question is, does that mean we're in a quiet period now and what was before that was normal?" Tobin told NWPB last week . "Or have we returned to normal after a decade or so of an unusually large numbers of earthquakes?"
Either way, the report isn't meant to be read as a prelude to greater seismic activity in order to make up for a quiet period; as the Seismological Research letters wrote ahead of the opinion paper, "this observation is little more than a curiosity and not an indication of likely lower or higher earthquake rates in the future."