A Late-Night Jolt: The Bay Area’s Latest Reminder

At 1:40 AM PDT on April 2nd, the Bay Area received a sudden wake-up call. A 4.6 Mw earthquake centered near Boulder Creek, about 48 miles southeast of San Francisco—shook the region, with reports on the USGS "Did You Feel It?" map spanning from the Golden Gate down to Monterey1.

While a 4.6 isn't exactly a "Big One" on the scale of 1906 or 1989, it’s certainly more than a minor tremor. It originated within the San Andreas Fault system, perhaps the most famous transform boundary in the world, where the Pacific and North American plates relentlessly grind past one another.

Why This One Felt More Personal

For many, this was just another Northern California quirk, but for me, it triggered two specific points of interest:


The San Ramon Connection: It strikes while the well-publicized San Ramon swarm is still active. 2


A Moment of Déjà Vu: A mid-4.0 quake in this specific region was actually my first introduction to seismic life. On the evening of August 6, 1989, I felt my first rattle while staying in a shady hotel just north of Palo Alto. That quake—centered at Lake Elsman3—was located in the same 

general neighborhood as April 2nd’s Boulder Creek event. 


The August 6th 1989 Lake Elsman event was not thought terribly significant until October 17th, 1989, at 5:04 p.m. PDT  when the Loma Prieta 6.7 earthquake interrupted the World Series and more importantly Killed 63 people and injured another  3,7574. It is now seen that my August 6th shaker was a pre-shock, hindsight is wonderful. 


The Boulder Creek event does not necessarily mean another 6.7 is coming,  There have been quite a few >4Mw events since 1898 in the region with no knock on effect. But it quite often a release of stress in one part of a fault system can increase stress in another (see map 1)



Map 1

More Connected Than We Thought?

The geography here is telling. While the San Ramon swarm is typically associated with the Calaveras Fault, and the Boulder Creek/Lake Elsman events hug the San Andreas, the lines between these systems are blurring.


Recent USGS research suggests that many of these "separate" faults may actually be interconnected at much deeper levels. We are seeing evidence that major systems—like the San Andreas and Cascadia5, or the Hayward and Calaveras6—might share deeper structural links.

It’s a fascinating, if slightly unsettling, reminder that beneath the beautiful California landscape, the earth is far more integrated (and active) than it appears on the surface.


Footnote: Moment Magnitude vs. Richter Scale

The Richter scale measures earthquake size using the strength of seismic waves recorded by instruments, but it works best for small to moderate earthquakes and tends to underestimate very large ones because it “saturates.” The Moment Magnitude scale (Mw), now the standard used by scientists, measures earthquakes based on the physical characteristics of the fault rupture, including the area that slipped, the amount of movement, and the rigidity of the rocks, which directly reflects the total energy released. Moment Magnitude is preferred because it remains accurate for both small and extremely large earthquakes, allows consistent global comparison, and provides more reliable information for scientific studies, hazard assessment, and engineering design.

References:

  1. Did you feel it

  2. San Ramon Swarm

  3. LA Times August 1989 Earthquake Report

  4. October 1989 Loma Prieta Report
  5. Cascadia - San Andreas Connection
  6. Hayward - Calaveras Connection

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Bazza

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