We use them to give you the best experience. If you continue using our website, we'll assume that you are happy to receive all cookies on this website.
Summary of controlling seismic events: seismic stability evaluation of Anderson Dam, Santa Clara County, Caliornia
Fault
Fault parameters
Distance (km)
Average PGA1
Average SA at 0.2 sec1
Average SA at 1.0 sec1
Arias intensity (m/sec)
Type
Mmax
HW
rmap
rjb
rrup
PGAmed
PGA84th
0.2med
0.284th
1.0med
1.084th
Travasarou et al 2003
Watson-Lamprey 2007
AImed
AI84th
AImed
AI84th
Coyote Creek2
RV
6.6
Yes
0.0
0.0
0.0
0.66
1.14
1.49
2.74
0.49
0.94
2.49
7.24
2.29
3.22
Calaveras
SS
7.25
No
2.0
2.0
2.0
0.50
0.85
1.15
2.07
0.44
0.84
2.95
8.45
2.66
3.73
San Andreas
SS
7.9
No
20.6
20.6
20.6
0.22
0.37
0.47
0.85
0.21
0.40
1.09
3.08
0.91
1.28
Notes 1 PGA (peak ground acceleration at bedrock) and spectral accelerations (SA) were computed using all five NGA attenuation relationships. 2 The Range Front fault (i.e. the southern continuation of the Coyote Creek fault) is considered non-seismogenic. Fault Type: RV = Reverse, SS = Strike slip HW: Yes = on hanging wall. No = on foot wall Rmap = map distance Rjb = Joyner-Boore Distance Rrup = fault rupture distance