Tracing the Hayward Fault in Fremont
 Lecture by
Dr. Joyce R. Blueford, Geologist, Math Science Nucleus

   (510)790-6284
http://msnucleus.org       msn@msnucleus.org


Commemorating the 150th Anniversary of the Great Quake of 1868

An overview of what is known about the Hayward Fault in the East Bau Hills.  A look at the the science and history of the Hayward Fault.

funding from a grant from Lam Research Foundation

Where:  Fremont Main Library, Stevenson Blvd
When: September 24, Monday
Time:   7-8 pm lecture;  come early and see the new display

FREE  

PUBLIC LECTURE (NOT APPROPRIATE FOR LITTLE ONES)

Eventbrite - Earthquakes and Volcanoes - Lam Research Science at the Library
(for reminder only)

The Hayward Fault has shaped the landscape of the East Bay for the last million years.  The last large earthquake was on October 21, 1968, when a 6 foot offset was ripped from Milpitas to San Leandro.  In certain places there was an uplift of 4-6 feet.  Hayward, San Leandro, Oakland and San Francisco had major damage.  Fremont’s Mission San Jose crumpled. The Hayward Fault has created the scenic hills and valleys in the East Bay.  Much of the length of the Hayward Fault outlines the hills of the Diablo Range.  However in Fremont, the Hayward Fault's trace is through the flatland.

The Hayward fault, running through the East Bay from the North Bay to Santa Clara County, is one of a handful of faults in the world that ‘creeps’ at the surface. Fault creep, where a fault moves steadily at the surface (instead of staying locked by friction, like most faults), has many observable effects in the East Bay – it separates curbs and paving slabs, cracks asphalt and walls, and damages buildings, most notably the Berkeley football stadium. The rate of movement, around 5 mm per year in Fremont, is enough to visibly move objects within a year or two.

Geophysicists are interested in this unusual behavior for a couple of reasons. First, we want to explain why some faults creep and others do not – why it happens on the Hayward fault in Fremont, and not (for example) on the San Andreas fault in Palo Alto. Second, and more importantly, knowing where and how fast the Hayward fault creeps allows us to make estimates of where it is not creeping. These ‘locked’ areas are accumulating strain for a future earthquake. We know that there was a large earthquake on the Hayward fault in 1868, and our best estimates suggest that there is a high probability of a repeat earthquake in the next few decades. Understanding in advance where this earthquake will happen will allow citizens, the public utilities and city governments to prepare for the worst.
 

Come see the "Faulted Floor" Exhibit.  See a map of the East Bay and where the Hayward Fault is ripping it apart.  For more information on the Faulted Floor Exhibit which is a permanent exhibit click here.

(left - San Leandro City Hall devastated in 1868)

 
MATH SCIENCE NUCLEUS since 1982 has served the education and public by offering quality science and math lessons that take our children learn critical thinking skills. We manage the Children's Natural History Museum and Tule Ponds at Tyson Lagoon Wetland Center. http://msnucleus.org.

  

Math/Science Nucleus
 4074 Eggers Drive, Fremont, California, U.S.A., 94536
 (510) 790-6284
msn@msnucleus.org