551.22
St29
V.9
pt.1
cop. 2
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to
MISCELLANEOUS PAPER S-73-1
STATE-OF-THE-ART FOR ASSESSING
i EARTHQUAKE HAZARDS IN THE
UNITED STATES
Report 9
CATALOGUE OF STRONG MOTION EARTHQUAKE RECORDS
VoJume I
WESTERN UNITED STATES, 1933-197!
by
Frank K. Chang
Soils and Pavements Laboratory
U. S. Army Engineer Waterways Experiment Station
P. O. Box 631, Vicksburg, Miss. 39180
April 1978
Report 9 of a Series
Approved For Public Release; Distribution Unlimited
W^
J Mill
Prepared for Office, Chief of Engineers, U. S. Army
Washington, D. C. 20314
Destroy this report when no longer needed. Do not return
it to the originator.
Unclassified
SECURITV CLASSIFICATION OF THIS PAGE (When Data Entered)
St ^9
REPORT DOCUMENTATION PAGE
READ INSTRUCTIONS
BEFORE COMPLETING FORM
1. REPORT NUMBER
Miscellaneous Paper S-T3-1
2. GOVT ACCESSION NO
3. RECIPIENT'S CATALOG NUMBER
4. TITLE (and Subtitle)
STATE-OF-THE-AET FOR ASSESSING EARTHQUAKE
HAZARDS IN THE UNITED STATES; Report 9, Cata-
logues of Strong Motion Earthquake Records;
Volume I, Western United States, 1933-1971
5. TYPE OF REPORT & PERIOD COVERED
Report 9» Volume I
6. PERFORMING ORG. REPORT NUMBER
7. AUTHORfa;
Frank K. Chang
8. CONTRACT OR GRANT NUMBERfs;
9. PERFORMING ORGANIZATION NAME AND ADDRESS
U. S. Army Engineer Waterways Experiment Station
Soils and Pavements Laboratory
P. 0. Box 631, Vicksburg, Miss. 39l80
10. PROGRAM ELEMENT, PROJECT, TASK
AREA a WORK UNIT NUMBERS
11. CONTROLLING OFFICE NAME AND ADDRESS
Office, Chief of Engineers, U. S. Army
Washington, D. C. 2031^
12. REPORT DATE
April 1978
13. NUMBER OF PAGES
53
14. MONITORING AGENCY NAME & ADDRESS(ll dlHerent from Conlrolllne Olllce)
IS. SECURITY CLASS, (oi thla report)
Unclassified
15a. DECLASSIFI CATION/ DOWN GRADING
SCHEDULE
16. DISTRIBUTION ST ATEMENT fof tfi/« ReporO
Approved for public release; distribution unlimited.
17. DISTRIBUTION STATEMENT (ot the abstract entered in Block 20, II different from Report)
18. SUPPLEMENTARY NOTES
19. KEY WORDS (Continue on reverse aide If neceeaary and Identify by block number)
Earthquake engineering
Earthquake hazards
Earthquakes
Ground motion
State-of-the-art studies
20v ABSTHACT (Caat£aum aa rmvermm •fdfl* f/ n m ^ e e a a ry ami Identify by block number)
A working catalogue was prepared to facilitate the selection of strong
motion earthquake records for design purposes. The records are those pro-
cessed by the California Institute of Technology from western United States
during the period 1933-1971. They are presented graphically in terms of
magnitude, type of fault, focal depth, site classification, peak acceleration,
velocity, displacement, dirration, and distance from epicenter.
DD/,
FORM
AN 73
1473
EDITION OF I NOV 6S IS OBSOLETE
Unclassified
SECURITY CLASSIFICATION OF THIS PAGE (When Data Entered)
SECURITY CLASSIFICATION OF THIS PAGE(TW»«n Data Bntend)
SECURITY CLASSIFICATION OF THIS P ACECWhen Data Entered)
Preface
This report is part of ongoing work at the U. S. Army Engineer
Waterways Experiment Station (WES) in Civil Works Investigation Study:
"Methodologies for Selecting Design Earthquakes," sponsored by the
Office, Chief of Engineers.
This study is directed by Dr. E. L. Krinitzsky, Engineering Geol-
ogy and Rock Mechanics Division (EG&IMD), Soils and Pavements Laboratory
(S&PL). General direction was by Mr. J. P. Sale, Chief, S&PL, and
Mr. D. C. Banks, Chief, EG&RMD. The report was prepared by Mr. F. K.
Chang, Earthquake Engineering and Vibrations Division.
COL J. L. Cannon, CE, and Mr. F. R. Brown were Director and Tech-
nical Director, respectively, of WES during the period of this study.
STATE-OF-THE-ART FOR ASSESSING EARTHQUAKE HAZARDS IN
THE UNITED STATES
CATALOGUE OF STRONG MOTION EARTHQUAKE RECORDS
Volume I
WESTERN UNITED STATES, 1933-1971
This report was prepared to facilitate the selection of appropri-
ate strong motion earthquake records for design purposes. It is a work-
ing catalogue in which groupings of earthquakes were made according to
their magnitude, type of fault, focal depth, and site classification.
For each category, the records are shown by peak acceleration, velocity,
displacement, duration, and distance from epicenter. Figures 1-24 pre-
sent these data.
It is intended that peak values for design earthquakes will have
1 2
been determined earlier either by use of Report 7 and Report 8 of this
series, or by other means. Figures 1-2^1 then provide an easy-to-use
presentation of what strong motion records are available in each cate-
gory. The records would then be selected for either direct utilization
in dynamic analyses or rescaling as needed.
The presentation of peak values is by catalogue ninnbers of the
California Institute of Technology (CIT) uniformly processed data from
which the actual strong motion records were obtained.
The present report (Volume l) concerns the strong motion records
from western United States during the period 1933-1971- The other vol-
umes contemplated are: Voliome II, Western Hemisphere, 1972 to present;
and Volume III, Other World-Wide Data.
Appendix A lists in columns l-l6 the CIT file numbers, station
location, instrumental direction, site classification, peak ground mo-
tions, epicentral distance, Richter magnitude, MM intensity (epicentral
and local), focal depth, duration, predominant period, and type of
causative fault. The duration (column 12) is the "bracketed diiration"
or the time interval between the first and last acceleration peaks that
is equal to or greater than 0.05 g-
To compile the predominant periods (column 13), three different
soiorces were used, as designated by subcolumns 1-3. Subcolumn 1 was
calculated from the formula T = 2Tr(v/a) , where V and a are peak
velocity and acceleration, respectively. Subcolumn 2 was obtained from
the publications, "United States Earthquakes" by the U. S. Coast and
Geodetic Survey. Subcolumn 3 was determined from the maximum value of
2 5
the acceleration response spectra and its corresponding period. ' The
periods calculated by the formula T = 27r(v/a) do not agree with the
others. Of the three sources, the predominant period values in subcol-
umn 3, adopted from the response spectra, are recommended.
Appendix B simmarizes the site conditions as determined by
Trifunac and Brady.
References
1. Krinitzsky, E. L. and Chang, F. K. , "State-of-the-Art for Assessing
Earthquake Hazards in the United States; Specifying Peak Motions for
Design Earthquakes," Miscellaneous Paper S-73-1, Report 7, Jan 1978 »
U. S. Army Engineer Waterways Experiment Station, CE, Vicksburg,
Miss.
2. Chang, F. K. and Krinitzsky, E. L. "State-of-the-Art for Assessing
Earthquake Hazards in the United States; Duration, Spectral Content,
and Predominant Period of Strong Motion Earthquake Records from
Western United States," Miscellaneous Paper S-73-1, Report 8, Jan
1978, U. S. Army Engineer Waterways Experiment Station, CE, Vicks-
burg, Miss.
3. California Institute of Technology, Earthquake Engineering Research
Laboratory, "Strong Motion Earthquake Accelerograms; Corrected Ac-
celerograms and Integrated Ground Velocities and Displacements,"
Vol 2, Parts A-Y, 1971-1975, Pasadena, Calif.
h. United States Earthquakes. Annual publication of the U. S. Depart-
ment of Commerce, Coast and Geodetic Survey, 1933-1968; the NOAA
National Ocean Survey, I969; and the NOAA Environmental Data Service,
1970.
5. California Institute of Technology, Earthquake Engineering Research
Laboratory, "Analyses of Strong Motion Earthquake Accelerograms;
Response Spectra," Vol 3, Parts A-Y, 1973-1975, Pasadena, Calif.
6. Trifunac, M. D. and Brady, A. G., "On the Correlation of Seismic
Intensity Scales with the Peaks of Recorded Strong Ground Motion,"
Bulletin, Seismological Society of America, Vol 65, Feb 1975,
pp 139-162.
O 440
\ 400
2
°- zao
1
1
1
1
1
1
I
I
1
-
1 1 1
STRIKE SLIP FAULTS
WESTERN U. S. A.
-
MAG 5.0-6.0
LEGEND
TYPE OF FOCAL DEPTH.
STRATA KM
-
-
Q
ALLUVIUM 8 6
ALLUVIUM 10
■
•
A
ALLUVIUM 11
INTERMEDIATE 8 6
INTERMEDIATE 110
d
-
■
ROCK
86
-
-
"BO
33
-
-
°B0
34
'
-
-
,B03
7
-
-
□ b
)35
-
-
1
,A0I8
'U309
-
-
-
A0I6
B022
-
^AOI
°B036
4
013
-
°B023
1
1
1
4 8036
, 1 ,
1
1
1
1
1
1
1
80 100 120 140
EPICENTRAL DISTANCE, KM
Figure 1. Peak acceleration versus epicentral distance for
strike-slip faults , magnitudes 5 •0-6.0, in alluvial, inter-
mediate and rock sites
77 9 CM/SEC
DB033
1
1
1
1
1
"T
1
1
1
1
■ -1
-
STRIKE SLIP FAULTS
(ALLUVIUM)
WESTERN U. S. A.
-
-
MAG 5.0-6.0
-
-
D
•
- *
m
LEGEND
TYPE OF FOCAL DEPTH
STRATA KM
-
ALLUVIUM 8 6
ALLUVIUM 10
ALLUVIUM 110
-
-
-
IN
RC
TERMEDIAT
CK
E
11
86
-
-
-
-
-
-
-
-
-
-
-
-
-
-
qBo:
■b03
)4
7
-
-
,
^AOIS
-
-
-
-
B035"
I
B022o
B036q„
,U30»
-
"AOI6a^^
013
-
A0I4^
A0I7^ °
, 1 ,
3023
1
8038^
1
1
1
1
1
1
1
1
80 100 120 140
EPICENTRAL DISTANCE, KM
Figure 2. Peak velocity versus epicentral distance for strike-
slip fault , magnitudes 5-0-6.0, in alluvial, intermediate and
rock sites
B033
77.9 CM/SEC
36
^
1
1
1
1
1
1
1
STRIKE SLIP FAULTS
WESTERN U. S. A.
MAG 5.0-6.0
32
-
-
-
LEGEND
-
30
TYPE OF FOCAL DEPTH.
STRATA KM
28
D
ALLUVIUM 8 6
-
•
4
ALLUVIUM 110
INTERMEDIATE 8 6
-
26
f\
INTERMEDIATE 1 1
■
ROCK
86
24
22
2
o
Z
UJ
UJ
_i
a
-
-
-
-
-
-
-
-
X 16
<
UJ
a.
14
-
-
-
-
12
-
-
10
-
(
AOIS
-
8
6
-
B034a
-
3037" °B036
4
B°"0 Jb022
-
(
iU309
-
A0I4A
-A0I6^
aA0I7
B023o
B038A
-
1
1
1
1
)
1
1
1
1
1
1
1
80 100 120 140
EPICENTRAL DISTANCE, KM
Figure 3. Peak displacement versus epicentral distance
for strike-slip fault , magnitudes 5.0-6.0, in alluvial,
intermediate and rock sites
I
1
1
I
1
1
1
1
1
1
I
1
-
STRIKE SLIP PAUL
(ALLUVIUM)
WESTERN U. S. /
MAG 5.0-6.0
1 1
LEGEND
TYPE OF fOCfi
TS
V
-
-
a
•
4
' ■
1 nppTH
-
-
STRATA KM
-
ALLUVIUM 6 6
ALLUVIUM 10
ALLUVIUM 110
INTERMEDIATE 8 6
INTERMEDIATE 110
-
-
-
RO"
CK
86
-
-
-
-
-
-
-
-
-
-
-
-
-
-
'B033
,Anin
-
-
1
iU309
B022
-
1
8035°
S034°
-
-
-
-
B037
■
-
AOI6a
,
1
1
1
1
1
1
1
1
1
-
100 120 140
EPICENTRAL DISTANCE, KM
Figure h. Bracketed duration (a >_ 0.05 g) versus epicentral
distance for strike-slip faults , magnitudes 5* 0-6.0, in al-
luvial, intermediate and rock sites
\200
5
0- 140
nAOO
1
I
1
1
I
1
I
1
I
'
T
1 1 1
STRIKE SLIP FAULTS
(ALLUVIUM)
\«jr-f^-ri-r->M 1 1 f^ A
-
-
MAG 6.0-7.0
-
-
LEGEND
TYPE OF FOCAL DEPTH,
STRATA KM
-
a ALLUVIUM 12
ALLUVIUM 16
. • ALLUVIUM 20
-
-
■ INT
ERMEDIATE
20
-
-
U3I2
■
-
-
-
-
V3I5
□
(3BO24
-
-
-
-
B02I
□
-
-
A0I9
•
-
-
-
-
V3I4°
-
-
-
-
B040a
-
-
A020
•
•y370
Y379
-
1
1
1
1
1
1
1
V332
1
Y37I
•
1
Y376-^ ^Y378
>. i •Y380
Y372« «* •,
Y375-^ 'Ya^S
III 1
100 120 140
EPICENTRAL DISTANCE, KM
Figure '-> . Peak acceleration versus epicentral distance for
strike-slip faults , magnitudes 6.0-7-0, in alluvial and in-
termediate sites
O
1
1
1
1
1
I
1
1
1
1
I
I
-
ST
V
1
RIKE SLIP PAUL
(ALLUVIUM)
VESTERN U. S. ^
MAG 6.0-7.0
TS
-
-
-
-
1 1 1
LEGEND
TYPE OF FOCAL DEPTH,
STRATA KM
-
-
D ALLUVIUM 10
A ALLUVIUM 12
ALLUVIUM 16
-
-
• ALL
■ INT
UVIUM
ERMEDIATE
20
20
-
-
-
-
-
AOOl
-
-
-
-
V3I5
-
-
A0I9
•
-
-
V3I4°
}B024
-
-
B02I
-
-
-
-
■
V3I2
-
-
A020
•
B040g
Y37I,
f37«^
Y378
-
1
1
1
1
1
•Y370
A
V332
1
1
Y3
1
'3. \\
Y3764^,
1
•y380
75
*Y373
1
100 120 140
EPICENTRAL DISTANCE, KM
Figure 6. Peak velocity versus epicentral distance for
strike-slip faults , magnitudes 6.0-7-0, in alluvial and
intermediate sites
10
z
UJ
2
o
< le
1
1
1 1
- I
I
1
1
. ^... .
1 1
1
I
I
-
1 1
STRIKE SLIP FAULTS
(ALLUVIUM)
-
-
WESTERN U. S. A.
MAG 6 0-7.0
-
-
LEGEND
TYPE OF FOCAL DEPTH
STRATA KM
-
-
D ALLUVIUM 10
A ALLUVIUM 12
ALLUVIUM 16
-
-
" • ALL
■ INT
UVIUM
ERMEDIATE
20
20
-
-
V3I5
-
-
-
u
AOOl
-
-
B02I
V3I4q
-
-
-
-
A0I9
•
-
-
-
-
-
-
-
-
-jBOZA
A020
•
»Y370
0Y372
-
-
8040a
Y37I*
Y379
•
Y376- •
y378
1
U3I2"
1
1
1
1
1
V332
1
1
Y375*
1
^— •Y380-
,Y373 -
1
80 100 120 140
EPtCENTRAL DISTANCE, KM
Figiore ?• Peak displacement versus epicentral distance for
strike-slip faults , magnitudes 6.0-T.O, in alluvial and in-
termediate sites
11
1
I
I
1
I
1
1
1
1
I
I
1
-
STRIKE SLIP FAULTS
(ALLUVIUM AND INTERMEDIATE)
-
-
WESTERN U. S. A.
MAG 6.0-7.0
1 1
LEGEND
TYPE OF FOCAL DEP
STRATA KM
-
-
TH.
-
ALLUVIUM 10
ALLUVIUM 12
ALLUVIUM 16
-
-
AOOl
•
INTERME
DIATE
2U
10
-
-
-
-
-
-
B024
n
-
-
-
-
-
-
-
-
-
-
-
-
-
-
D
B02I
-
-
A0I9
•
-
1
U3I2
■
1
1
1
1
1
1
1
1
1
1
eO 100 120 140 160
EPICENTRAL DISTANCE, KM
200 220 240
Figure 8. Bracketed duration (a >_ 0.05 g) versus epicentral
distance for strike-slip faults , in alluvial and intermediate
sites
12
\ 200
2
1
1
1
1
1
1
I
r- ■
T
1
1
1
-
T
HRUST
(ALLU
/ESTERh
MAGe
CAL DE(
FAULTS
\/IUM)
>J U. S. A
.0-7
=TH 13 K
-
-
FO
CM
-
-
-
Foasf
-
-
«C048
Q^33
• R253
-
-
HMS
•0199
•F09e
-
-
GIIO, .1
1058
-
-
GIOSi
R24aM
1
•R25I
1 131
-
-
Q23(a
,E063
-
-
Q239*
S26eJ
0057%
D0S9^^
lOoes
• R244
•C054
-
1
cn4«
NI8S|
FIO^A
,E075
• 0082
,C05I
-
-
R24t.
J145* 1
P217-^
S26l"
GII2
-•HI2I
• Mi7e
lJI4S
kGI07
^ •F00<
J
-
-
Doee*^
FOS
R24S,
I>34 .^
«S25a
88
-
-
5287,
NI87«
-
-
P23I,
»020€
l«NI95
-
-
HII8«
MI8
0205% J
0204* "
124
0»,F087
S.*l07l
_ P222
•fioi
«NI97
-
1
1
1
1
1
1
I
1
1
1
1
so 100 120 140 160 ISO 200 220 240
EPICENTRAL DISTANCE, KM
Figure 9- Peak acceleration versus epicentral distance for
thrust faults, magnitudes 6.0-7-0, in alluvial sites
13
1
1
1
1
1
1
!
I
1
1
1
1
-
Tf
HRUST F
(ALLUV
ESTERN
MAG 6
:AL DEP
AULTS
lUM)
U. S. A.
0-7.0
TH 13 K
-
-
W
FOC
M
-
-
-
-
-
-
-
-
-
-
-
-
-
-
q
233« '^l"
, "Fosa
•C048 1
aHIIS
-
-
^E075
-
S2
E08:
1137
»8-^— J
1 D056*
'^^,--006
<^ — CO
t FO
^F089
5
51
98
9
-
0239
- S26H
R24e
F095H
"R24e^
D057r:3l
■-Ml/el
i ^R253
-
JI48-
1131-—
NI88-
1134
R249-I
GII4
,y\NS:rGii2
-
FI05,
HI18»^
Niae«
,02
0204 •»"
OS
196
,MI80
-
-
,FI03
P222,
HI24*
•f087
«NI95
-
1
1
1
NI87*
1
•e07I
1
• 0206
•fioi
1
1
1
,NI97
1
-
100 120 140
EPICENTRAL DISTANCE, KM
Figure 10. Peak velocity versus epicentral distance for
thrust faults, magnitudes 6.0-7-0, in alluvial sites
111
- t
1
I
— r
1
1
I- -■■
— 7 ■
1
1
-
-
r\
HRUST F
(ALLUV
ESTERN
MAG 6
;AL DEP
AULTS
lUM)
U. S. A.
0-7.0
TH 13 K
-
-
w
FOC
M
-
-
-
-
-
-
-
-
-
-
9233
-
-
JI45*
-
-
,0048
0058*
,F08i
1
-
h
1115,
D057*<
DOSS,
,MI76
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DOSS
-
-
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-COSI
-
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W;.
_J»^ruo«
jue-
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-•S258
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— R253
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-
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^ •P23
7
1 ,N
lOR
-
-
006
R248,
137, • 1
.0236«
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-
-
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86
t
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-
-
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GI08
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124
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-
1
1
1
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1
,E07I
1
,0206
•fioi
1
1
1
1
,NI97
1
1
1
100 120 140
EPICENTRAL DISTANCE, KM
Figure 11. Peak displacement versus epicentral distance
for thrust faults, magnitudes 6.0-7.0, in alluvial sites
15
1
1
1
1
1
1
1
I
... _,
1
1
1
-
T
HRUST
(ALLU
/ESTER^
MAG 6
CAL DEF
FAULTS
k/IUM)
J U. S. A
.0-7.0
^TH 13 K
-
-
\A
FO
M
-
-
-
-
-
-
-
-
-
-
-
•
1137
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-
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-
-
-
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-
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-
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r •nibs
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• D05I__M|76
-
-
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103
086
-
-
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86
7
-
-
D068**
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-
1
1
S267
I*
1
1
1
1
1
1
1
1
100 120 140
EPICENTRAL DISTANCE, KM
Figure 12. Bracketed duration (a >_ 0.05 g) versus epicentral
distance for thrust faults , magnitudes 6.0-7.0, in alluvial
sites
16
(J
1
1
«JI44
I
1
1
1
1
1
1
I
-
T
(
HRUST
NTERM
ESTERh
MAG 6
DAL DEF
-AULTS
EDIATE)
J U. S. A
.0-7.0
'TH 13 K
-
-
D056
•
FO(
M
-
-
-
-
-
-
-
-
-
-
-
-
-
«E07a
-
-
P2I4*
-
-
S25S,
•Q24I
S2«5
-
-
E072«
FI04
•
-
-
52624
^NI92
-
-
r*F092
NI85,
-
-
•mI8
•mI7
4
3
i
-
-
NI9I
P220*
-
1
1
1
1
1
1
LI7l'
1
1
1
1
1
1
80 100 120 140 160
EPICENTRAL DISTANCE, KM
200 220 240
Figure 13. Peak acceleration versus epicentral distance for thrust
faults , magnitudes 6.0-7.0, in alluvial intermediate sites
17
1
1
1 '
1
1
1
1
1
I
■1 —
1
-
-
T
(
HRUST
NTERM
ESTERh
MAG 6
3AL DEF
FAULTS
EDIATE)
J U. S. A
.0-7.0
'TH 13 K
-
-
FO
M
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
•
•
DOSS
-
-
P2I4,
szssa
E072«
*E078
-
-
NIB2
4
S26S
-
-
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«F0B2
-
-
FI04,
-
-
y
NISI
-(I84»«N
P220c
185
-
1
1
1
•Mia3
•m17'9
1 1
1
(
1
LI7I
1
1
1
1
20 40 60
80 100 120 140 160
EPICENTRAL DISTANCE, KM
180 200 220 240
Figure 1^4-. Peak velocity versus epicentral distance for thrust
faults , magnitudes 6.0-7.0, in intermediate sites
18
1
1
1
1
1
1
1
1
1
-
T
(
VA
HRUST
NTERM
^ESTERh
MAG 6
CAL DEF
FAULTS
EDIATE)
J U. S. A
.0-7.0
=TH 13 K
-
-
FO
.M
-
-
-
-
-
-
-
-
-
-
-
-
-
5262,
-
-
S235*
-
-
S2e5«
•E07a
-
-
E072'
,F092
-
-
aJI44
«005(
•0241
-
-
-P2I4*"
'NI92
P220,
-
-
-
-
FI04*
• NI9I
NieSf
LI7I,
-
1
1
1
I83#M'8
•mI7
4
9
1
I
1
1
1
1
1
1
80 100 120 140 160
EPICENTRAL DISTANCE, KM
Figtire 15. Peak displacement versus epicentral distance for
thrust faults ? magnitudes 6.0-7.0, in intermediate sites
19
1
1
1
1
I
1
1
1
I
I ■■-
1
-
1 1 1
THRUST FAULTS
(INTERMEDIATE)
yj/CCTCDM MCA
_
-
FO
MAGE
CAL DE
) .0-7.0
PTH 13 h
(M
-
-
-
-
-
-
-
-
-
-
-
-
-
0056
•
-
-
_»JI44_
-
-
-
-
S2S5,
-
-
szezf
S2S5*
-
E072'
P2l4a
•024l
,NI92
-FIf
>4
-
-
•e078
NI8S*
-
-
•f092
-
1
1
1
1
1
1
1
1
1
1
1
1
80 100 120 140 160 180 200 220 240
EPICENTRAL DISTANCE, KM
Figiire l6. Bracketed duration (a ^ 0.05 g) versus distance for
thrust faults , magnitudes 6.0-7.0, in intermediate sites
20
1 148.1 CM/SEC/SEC
Ic04l
O
2
1
1
1
1
1
1
1
1
1
1
-
\
THRUST
{RC
WESTER
MAG
)CAL DE
FAULT
)CK)
N U. S. >
6.0-7.0
PTH 13
S
\.
KM
-
FC
-
-
-
-
-
-
-
-
-
Eoaic
-
-
Gioe«
-
oi9a«
• JI42
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-
-
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-
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-
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-
-
P223,
-
-
-
-
FI02
•
-
1
,
1
1
1
1
1
1
1
1
1
378 3 KM
|02I3 1
40 80
80 100 120 140 160
EPICENTRAL DISTANCE, KM
ISO 200 220 240
Figure IT. Peak acceleration versus epicentral distance for
thrust faults , magnitudes 6.0-7.0, in rock sites
21
C04I
113.2 CM/SEC
5-
o
1
1
1
1
1
1
1
1
1
1
I
r- - ■■
-
1 1
THRUST FAULTS
(ROCK)
-
FO
/bSlhHr>
MAG 6
CAL DEF
J U. S. A
.0-7.0
^TH 13 K
.M
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
oita»
-
-
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•
-
-
•
LISA
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-
-
Jl
GI06*
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*2« ,02
81
37
-
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«JI43
«P22I
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-
1
1
1
FI02
•
1
1
1
1
1
1
1
1
378 3KM
0213
•— ^
20 40 60 80 100 120 140 160 180 200 220 240
EPICENTRAL DISTANCE, KM
Figure l8. Peak velocity versus epicentral distance for
tt;rust faults , magnitudes 6.0-T.O, in rock sites
22
37.7 CM/SEC
{c04l
<C 16
<
1
1
1
1
1
1
1
- -1 —
1
1
T
-
T
HRUST
(RO(
ESTER^
MAG 6
3AL DEF
FAULTS
1 U. S A
.0-7.0
'TH 13 K
-
-
FO(
M
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
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-
-
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-
Jl
1
42» •02
1
07
1
,FI02
1
1
1
1
1
1
1
378 3 KM
10213
20 40 60 80 100 120 140 160 180 200 220 240
EPICENTRAL DISTANCE, KM
Figure 19. Peak displacement versus epicentral distance for
thrust faults, magnitudes 6.0-T.O, in rock sites
23
z
o
< le
a
o
o
1
1
1
I
(
1
T
1
1
I
1
-
T
HRUST
(ROC
ESTER^
MAG 6
3AL DEF
FAULTS
J U. S. A
.0-7,0
'TH 13 K
-
-
FO(
M
-
-
-
-
-
-
-
-
-
-
-
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-
-
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-
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106
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-
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1
1
1
,P223
1
1
1
1
1
1
1
1
1
20 40 eo eo loo rzo i4o leo iso 200 220 240
EPICENTRAL DISTANCE, KM
Figure 20. Bracketed duration (a _^ 0.05 g) versus distance
for thrust faults, magnitudes 6.0-7-0, in rock sites
2k
u
z
o
p leo
H 160
0- 140
1
1
I
1
1
1
1
I
1
1
1
1
-
THRUST FAULTS
(ALLUVIUM)
-
WESTERN U. S. A
MAG 7.0-8
-
LEGEND
• FOCAL DEPTH 16
FOCAL DEPTH 70
-
B029o
-
-
-
-
-
-
-
-
-
-
•A004
-
-
-
-
A005
•
-
-
-
-
-
-
D028o
-
-
1
Aooet
•a003
-
-
-
1
1
1
1
1
1
1
1
1
1
1
1
80 100 120 140
EPICENTRAL DISTANCE, KM
200 220
Figure 21. Peak acceleration versus epicentral distance for
thrust faults, magnitudes 7- 0-8.0, in alluvial sites
25
o
1
1
r — 1
1
1
1
1
I
I
1
I
1
-
THRUST FAULTS
(ALLUVIUM)
-
-
WESTERN U. S. A.
MAG 7.0-8.0
1 1
-
-
•
LbUtNU
FOCAL DEP
FOCAL DEP
TH 16
TH 70
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
-
■ B028o
-
-
•a004
A005
-
-
-
-
0028o
A006|
A007'
«A003
-
-
-
-
1
1
1
1
1
1
1
1
1
1
-
40 60
100 raO 140 160 180 200 220 240
EPICENTRAL DISTANCE, KM
Figure 22. Peak velocity versus epicentral distance for
thrust faults, magnitudes 7.0-8.0, in alluvial sites
26
1
1
1
1
1
1
I
I
I I I 1
THRUST FAULTS
(ALLUVIUM)
32
-
WESTERN U. S A.
MAG 7.0-8
-
LEGEND
* prtr'Ai nCDTUI 1C
28
26
-
FOCA
L DEPTH 70
-
24
22
o
-
-
^'20
Z
UJ
:
u
-1
a
M
a
>C 16
<
UJ
Q.
14
12
10
e
-
-
-
-
-
-
-
B029o
-
-
• A004
-
6
A007,
-
A005
A00«*
-
-
D028o
«A003
-
2
-
-
1
1
1
1
1
1
1 1
,
1
1
> 20 40 80 80 100 120 140 160 ISO 200 220 240
EPICENTRAL DISTANCE, KH/I
Figure 23. Peak displacement versus epicentral distance
for thrust faults, magnitudes 7-0-8.0, in alluvial sites
27
34
1
1
1
1
1
I
1
1
1
1
-T
-
THRUST FAULTS
32
30
(ALLUVIUM)
VESTERN U. S. 1-
MAG 7.0-8.0
-
V
V
LEGEND
28
26
24
22
Al
"
• FOCAL DEPTH 16
FOCAL DEPTH 70
-
-
-
-
B02»o
-
-
-
.
•a004
_
O
u 18
U)
Z
O
o
-
-
_
.
14
12
10
8
00280
-
•
A009
-
4
2
1
1
1
1
1
1
1
1
1
1
1
1
20 40 60 80 100 ijo 140 160 180 200 220 240
EPICENTRAL DISTANCE, KM
Figure 2U. Bracketed dioration (a >_ 0.05 g) versus epicentral
distance for thrust faults , magnitudes 7.0-8.0, in alluvial
sites
28
Appendix A: Strong Motion Data, Earthquakes of
Western United States, 1933-19T1
(Columns 1 to 10: California Institute of Technology,
Earthquake Engineering Research Laboratory, "Strong
Motion Earthquake Accelerograms; Corrected Accelero-
grams and Integrated Ground Velocities and Displace-
ments," Vol 2, Parts A-Y, 1971-1975, Pasadena, Calif.
Colimms 11 to l6: Compilation prepared at WES.)
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Appendix B: Site Characteristics
(Coiirtesy of Trifimac, M. D. and Brady, A, G., "On
the Correlation of Seismic Intensity Scales with
the Peaks of Recorded Strong Ground Motion," Bulle-
tin, Seismological Society of America, Vol 65, 1975 »
pp 139-162. )
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B12
In accordance with letter from DAEN-RDC, DAEN-ASI dated
22 July 1977, Subject: Facsimile Catalog Cards for
Laboratory Technical Publications, a facsimile catalog
card in Library of Congress MARC format is reproduced
below.
Chang, Frank K
State-of-the-art for assessing earthquake hazards in the
United States; Report 9: Catalogue of strong motion earth-
quake records; Vol. I: Western United States, 1933-1971 /
by Frank K. Chang. Vicksburg, Miss. : U. S. Waterways Ex-
periment Station ; Springfield, Va. : available from National
Technical Information Service, 1978.
28, 13, 12 p. : ill. ; 27 cm. (Miscellaneous paper - U. S.
Army Engineer Waterways Experiment Station ; S-73-1, Report
9, v.l)
Prepared for Office, Chief of Engineers, U. S. Army, Wash-
ington, D. C.
References: p. 4.
1. Earthquake engineering. 2. Earthquake hazards. 3. Earth-
quakes. 4. Ground motion. 5. State-of-the-art studies.
I. United States. Army. Corps of Engineers. II. Series:
United States. Waterways Experiment Station, Vicksburg, Miss.
Miscellaneous paper ; S-73-1, Report 9, v.l.
TA7.W34m no. S-73-1 Report 9 v.l
"i 0112 084235305