The Ukiah Daily Journal

Who has the most quakes?

- LORI DENGLER

What is the most seismicall­y active spot in California? The answer depends on your perspectiv­e. If you are a regular reader of this column, you might say the North Coast and adjacent offshore area. That’s a good answer when you look at size. We have fairly frequent M6s and 7s. About 46% of all earthquake energy released in the State over the past fifty years comes from our neck of the woods.

Folks in Southern California might wave their arms. They are right if we defined “active” in terms of how many people feel earthquake­s. A 4.5 near El Monte last September produced nearly 39,000 Did You Feel It reports. If the criteria were lives lost, it would be the San Francisco Bay Area. 1906 alone accounts for 85% of the total U.S. earthquake and tsunami death toll in historic times.

What about just going by the numbers, regardless of size or impacts? Unless you are a close watcher of earthquake activity, I don’t think you will guess this one. The area of California with the most earthquake­s, sustained at a relatively steady rate for at least the past three decades is The Geysers geothermal area north of Santa Rosa. Over 200 earthquake­s were recorded near The Geysers in the past week, 730 in the past month and over 9800 in 2020 to date.

Why so little news coverage? Almost all of these earthquake­s are very small in magnitude. And by small, I mean miniscule. Of the 730 earthquake­s in the past month, only 23 were magnitude 2 or larger, the largest had a M3.2. The largest earthquake of the past year was a 4.1, and over the past 40 years, a 5.0. No historic earthquake­s have caused any damage.

The earthquake­s in The Geysers are unusual. They are not the typical mainshock — aftershock sequence where a large quake occurs followed by numerous smaller ones. They aren’t swarms where a burst of nearly equal size earthquake­s occurs over a period of days or weeks. The Geyser activity is sustained — 216 last week, 229 the week before and 237 the week before that.

The cause requires understand­ing the geologic setting and human activities. The Geysers is the world’s largest electricit­y producing geothermal field. Steam drawn from more than 350 wells power 18 geothermal power plants that produces about 6500 Gigawatt hours of electricit­y a year. In 2018, renewable energy sources provided 32% of California’s electric generation. 20% of that came from the Geysers, the single largest contributo­r to the renewable budget. A Calpine report in 2008 estimated The Geysers meets 60% of the total coastal electric power demand between Marin County and the Oregon border.

Energy production at The Geysers uses natural dry steam to drive turbines and convert the heat to electricit­y. The steam comes from a magma body about 4 miles beneath the surface. The Pomo, Wappo and Miwok peoples utilized the hot springs in the area for cooking, bathing and healing long before the entry of European peoples. In the mid 19th century spas and resort hotels were developed, a tradition that continues today in Calistoga. Electricit­y production began in 1921 when The Geysers Resort tapped the first geothermal well in the Western Hemisphere to power the hotel.

The Geysers steam field is fueled by a magma body that is part of the Clear Lake Volcanic Field. If you have driven through the Clear Lake area, you can’t help but notice Mount Konocti, a cinder cone on the south shore of Clear Lake. One of my closest friends in graduate school at Berkeley was Julie Donnely-nolan and her thesis project was to study Konocti and other volcanic centers to parse out volcanic history of the Clear Lake area. She and others ascertaine­d that volcanic activity began about 2.1 million years ago and the most recent eruptive phase was 10,000 years before present. The area is considered quite capable of producing future eruptions.

The modern era of power generation at The Geysers began in 1960 with PG&E’S first geothermal well. Calpine took over management in 1998. There are two features of The Geysers area that make it ideal for resource extraction. First, it produces steam and second, the steam is clean and contains almost no salts or contaminan­ts.

The natural flow of steam from The Geysers was in decline by the late 1980s, beginning to reduce the power generation capacity. Calpine partnered with Lake County to use wastewater to recharge the field. In 2004, a 42-mile long pipeline from Santa Rosa provided additional fluids for the recharge effort. Treated effluent is injected into deep wells where it is heated to steam by the magma body in the same way that natural ground water has fed the field for millennia.

There have always been earthquake­s in the region. It is difficult to quantify the relation between geothermal activity and earthquake­s prior to the commercial steam extraction era, as the seismic network wasn’t sensitive enough to detect very small earthquake­s. The process of withdrawin­g the steam and heat causes rock to contract and hence produce small quakes. I was certainly aware of Geysers seismicity as a grad student on the 1970s.

In the 1980s and 90s the seismic network was improved with the addition of borehole instrument­s and newer digital equipment. It is capable of recording earthquake­s as small as 0.1. The impact of waste fluid injection shows up clearly in the seismic date records, and has more than doubled the seismicity rate. And although the number has increased, the magnitudes are still modest. Each year, on average one or two quakes hit the low M4 range and most seismologi­sts don’t believe that heat extraction or waste fluid injection makes larger earthquake­s beneath the geothermal area any more likely.

Note: more about The Geysers and the Clear Lake Volcanic Field at https://www.usgs.gov/volcanoes/clear-lake-volcanic-field/geysers-geothermal-field

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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