Seismograms
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Credit: Richard Allen/UC Berkeley
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The Berkeley Earthquake
The "Berkeley Earthquake" occurred on the Hayward Fault at 1:24 am on June 26 1994 and was a magnitude 4.2 event. The figures show the three components (BHZ (bottom) is vertical; BHN (middle) is north-south horizontal; and BHE (top) is east-wast horizontal) recorded at station BKS which is in the Byerly Vault (photos below) on the UC Berkeley campus. The P-wave arrives first at about 187 sec and is relatively low amplitude but clearly distinguishable from the background noise seen before 187 sec. The S-wave starts with the big pulse arriving at about 189 sec and contains most of the energy. There is only 2 sec between the P and S because the station is so close to the earthquake.
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Earthquake animation: M8.0 on the San Andreas Fault
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Right-Click to download the movie as a 14Mb MP4 file
Right-Click to download the movie as a 321Mb AVI file
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This animation shows a magnitude 8.0 earthquake on the San Andreas Fault.
This earthquake is about the same magnitude as the 1906 event and runs in realtime.
As the rupture propagates from the north to the south, radiating P-wave energy is represented as red circles and S-wave energy as yellow.
The total rupture takes 2 to 3 minutes to complete, and it is not until the rupture reaches the San Francisco Bay Area that most of the damage occurs in the Bay Area.
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Earthquake early warning
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Credit: Richard Allen
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Active and developing earthquakes early warning systems around the world superimposed on a map of seismic hazard.
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Credit: Richard Allen
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Comparison of the seismic stations in Japan used for earthquake early warning to those in California that could be used for earthquakes early warning. The maps are shown at the same scale.
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Seismic stations in California and Japan
There are about 300 seismic stations in California today that be used at the basis of an earthquake early warning system. All of these stations would benefit from upgrades to their equipment allowing data to stream more rapidly to the network control centers providing a few additional seconds of warning. Japan, shown at the same scale, uses over 1000 instruments for its early warning system. California's warning system would benefit from an additional 300 stations to fill in the gaps in the current network.
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Credit: Richard Allen
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Seismic stations in California that could potentially be used for earthquakes early warning.
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Credit: Richard Allen
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Alum Rock AlertMap
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Alum Rock AlertMap (left)
On October 30, 2007 the magnitude 5.4 Alum Rock earthquake rippled across the San Francisco Bay Area. The largest earthquake in the region since the 1989 Loma Prieta earthquake, it was felt by most people but caused little damage. The CISN early warning test system named ElarmS caught the earthquake. This map shows the distribution of ground intensity predicted using the first few seconds of data recorded by seismometers near the epicenter in San Jose. The epicenter is shown as a star and the estimated magnitude is 5.2. The warmer colors show stronger shaking near the epicenter and the cooler colors show weaker shaking at greater distances. The predicted ground shaking is very accurate. The data used to generate this map was available a few seconds before the shaking was felt in San Francisco.
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Earthquakes, faults and seismic station maps
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Bay Area
earthquakes: red; faults: black lines; seismic stations: blue
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Credit: Richard Allen
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California and Nevada
earthquakes: red dots and black circles (mag > 5); faults: black lines
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Credit: Richard Allen
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Seismic station/seismometers - Byerly vault
In Strawberry Canyon above the UC Berkeley campus and home to the Berkeley Digital Seismic Network Station BKS.
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Entrance to the Byerly vault
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The pier inside the vault
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STS-1 seismometers on the pier
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Seismic station/seismometers - PASSCAL deployments
Seismic stations deployed in various regions. These are "temporary" stations meaning that they are deployed for 2-4 years as part of regional seismic network.
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Credit: Richard Allen
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One of 84 seismic stations installed in northern California in 2007 as part of the Mendocino Experiment.
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Credit: Richard Allen
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The installtion team as work installing one of 84 seismic stations in northern California in 2007 as part of the Mendocino Experiment.
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Memorial Stadium
Built in 1923, the stadium straddles the Hayward Fault which runs goalpost to goalpost. Continuous creep on the fault has caused the building to deform over time.
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Memorial Stadium
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Credit: Richard Allen
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Exterior expansion joint in section KK
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Credit: Richard Allen
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Expansion joint in section KK
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Credit: Richard Allen
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The columns on either side of the expansion joint are offset by the creep
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Credit: Richard Allen
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This offset causes cracks in the columns
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Credit: Richard Allen
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Diagonal cracks are also a result of the deformation
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Credit: Richard Allen
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Japan
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Credit: Richard Allen
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The control room at the Japanese Meterological Agency for the earthquake early warning system.
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Credit: Richard Allen
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The Bullet Trains were one of the first users of earthquakes early warning in Japan.
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Turkey
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Credit: Richard Allen
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The antennas on the roof of the Kandilli Observatory and Earthquake Research Institute of Bogazici University in Istanbul. These receive the seismic data from the stations across the city used for earthquke early warning.
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