The Ukiah Daily Journal

Quakes and tsunamis: How did 2020 stack up?

- Lori Dengler

No matter how you look at it, 2020 will stand out as a difficult year. The year when the pandemic took top billing and wildfires, the economy and political strife battled it out for the next slots. And it was a year when earthquake­s and tsunamis rarely made the front page. There were fewer large or deadly earthquake­s in 2020 than any year in the last two decades. At least 205 people lost their lives from earthquake related shaking in 2020, the lowest number since 1984 and about the same as the number of L.A. County residents who died from COVID on Friday.

“No catastroph­ic earthquake­s” is good news, and even without great loss, it is worth a look back on the year to see what was learned and what surprised me.

The July 22 M7.8 south of the Alaska Peninsula was the largest earthquake of the year. It was fortuitous­ly located about 60 miles away from the nearest town where distance muted the shaking strength to a moderate level. The 7.8 and its nearly as strong 7.6 aftershock on Oct. 19 are interestin­g from a tectonic perspectiv­e. They were centered in the Shumagin Gap, an area of the Aleutians that had not experience­d a great earthquake in the past century and had been identified by some seismologi­sts as a likely source of the next great Alaska quake. The 2020 earthquake­s didn’t quite fill the gap and they were complex.

The July earthquake was a thrust event probably on or near the subduction zone interface but it produced a very small tsunami. The October earthquake was a strike slip earthquake oriented nearly perpendicu­lar to the mainshock. It produced a modest tsunami that was larger than the bigger quake. I am still scratching my head about that one. Some seismologi­sts now speculate that the Shumagin Gap is a transition­al zone in the Aleutians and might not produce M9s. Only time will decide if they are correct.

In terms of energy release, the 2020 total was even less than last year, taking over the bottom slot for the last two decades from 2019. In my 2019 summary column, I used Tsar Bomba, the Soviet Union’s largest nuclear test ever conducted, to describe seismic energy release. Tsar Bomba, an atmospheri­c test in 1961, released 50 megatons. The total seismic energy output in 2020 was about six tenths of a Tsar Bomba, down about 11% from last year. Earthquake­s are quite capable of exceeding the Tsar’s output. The seismic release in 2011 equaled about 14 Tsar Bombas.

Most tsunamis are caused by great earthquake­s so it is not much of a surprise that the planet experience­d fewer and smaller tsunamis this year. Only one tsunami caused damage and killed a person. It was produced by the Oct. 30 M7 earthquake in the Aegean Sea and reached a height of just over six feet. There is a cautionary tale in this tsunami. Magnitude 7 is not a very large earthquake from a tsunami perspectiv­e and yet this earthquake produced higher water levels than the two much larger Alaska earthquake­s. The Oct. 30 tsunami appears to have been amplified by the shape of the seafloor and Turkish coastline. The communitie­s affected were less than 20 miles from the epicenter and everyone felt the earthquake. It took only 10 to 15 minutes for the tsunami to arrive. It is another cautionary tale that when you feel an earthquake, you should always think tsunami and head to higher ground as soon as you can.

The Oct. 30 Aegean Sea earthquake was also the deadliest of 2020. In addition to the tsunami death, it killed 118 people from shaking-related damage. I wrote about the complex tectonic setting and the seismic vulnerabil­ities of the region before (“Complicati­ons in a plate boundary,” Times-standard, Nov. 8, 2020, Page A2). It is no surprise that a number of the damaged structures were unreinforc­ed stone a brick buildings built decades to centuries ago. But post earthquake reconnaiss­ance studies revealed that some of the collapsed structures were built in the 1990s long after earthquake-resilient design was required in Turkey. A report by an Izmir Earthquake Research Center points to sloppy constructi­on and poor code enforcemen­t as the culprits. Another reminder that earthquake engineerin­g design is only as good as what gets put into practice.

While the global activity level was lower than the recent average in 2020, U.S. activity was up both in the contiguous 48 states and Alaska. Nearly 3,000 earthquake­s of magnitude 3 or larger were recorded in Alaska and the Aleutian Islands, about 1,000 more than the average over the past two decades. The reason is no surprise — the July 22 M7.8 and its vigorous aftershock sequence. Fortunatel­y the earthquake activity was concentrat­ed in sparsely populated areas.

Nearly 1,500 earthquake­s of magnitude 3 or larger were tallied in the lower 48 states, slightly below last year and about 50% above the average over the past two decades. 2019 was high because of the Ridgecrest M7.1 and aftershock­s. 2020 saw increased activity in the western U.S.: M6.5s in Central Idaho and Western Nevada, 5s in Utah, Central California and Texas. Aftershock­s are still being recorded from many of these earthquake­s and also from the Ridgecrest earthquake. So far the activity has been centered away from populated areas and the impacts relatively modest.

There were U.S. earthquake deaths in 2020, but not in Alaska or the lower 48. Fourteen earthquake­s of magnitude 5 or larger were located along the coast and just offshore of southwest Puerto Rico. The sequence began on Dec. 28, 2019 with a 4.7 and over the next 10 months produced 118 earthquake­s of magnitude 4 or larger, including a 6.4 on Jan. 7, 2020 and 14 earthquake­s in the M5 range. Four deaths and nine injuries were attributed to the 6.4 and aftershock­s last January.

I am guilty of ignoring Puerto Rico in my annual summaries, but it is the second most seismicall­y active region of the United States (following Alaska), reporting about five times as many earthquake­s every year on average as California. Like California, it sits in a complex tectonic environmen­t with a transform plate boundary and major subduction zone nearby. I resolve to pay more attention in 2021.

What does all this mean for earthquake activity in 2021? We will have earthquake­s in the coming months. Just because 2020 was relatively quiet doesn’t mean there will be more (or fewer) quakes this year. There will be surprises and I hope impacts will continue to be low. But the only way to minimize impacts is to build resilient communitie­s, invest in sciences and engineerin­g, enforce building codes,

Drop Cover and Hold On when the ground shakes, and be sure to head to high ground if you are on the coast. I am fond of saying we are one day closer to the next great temblor today than we were yesterday.

Note: Primary source of earthquake informatio­n ( https://earthquake.usgs.gov/ ), tsunami informatio­n (https://www.ngdc.noaa.gov/hazard/tsu_db.shtml ). Impact informatio­n from https://en.wikipedia.org/wiki/List_of_earthquake­s_in_2020.

Lori Dengler is an emeritus professor of geology at Humboldt State University, an expert in tsunami and earthquake hazards. All “Not My Fault” columns are archived at https://www2.humboldt.edu/kamome/ resources and may be reused for educationa­l purposes. Leave a message at 707-826- 6019 or email Kamome@humboldt.edu for questions/comments about this column, or to request a free copy of the North Coast preparedne­ss magazine “Living on Shaky Ground.”

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 ?? SOURCE: UNITED STATES GEOLOGICAL SURVEY ??
SOURCE: UNITED STATES GEOLOGICAL SURVEY

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