UNITED STATES DEPARTMENT OF THE INTERIOR
GEOLOGICAL SURVEY National Center for Earthquake Research
CATALOG OF EARTHQUAKES ALONGTHE SAN ANDREAS FAULT SYSTEM IN CENTRAL CALIFORNIA
FOR THE YEAR
OPEN-FILE REPORT 78-1010
The report is preliminary and has not been edited or reviewed for conformity with Geological Survey standards and nomenclature.
Any use of trade names and trademarks in this publication is for descriptive purposes only and does not constitute endoresment by the U.S. Geological Survey.
Menlo Park, California
1978
CATALOG OF EARTHQUAKES ALONG THE SAN ANDREAS FAULT SYSTEM IN CENTRAL CALIFORNIA, FOR THE YEAR 1974
by F. W. Lester and K. L. Meagher
CONTENTS
PageIntroduc tion........................................................ 2Instrumentation..................................................... 2Data Processing and Analysis........................................ 3Discussion of Catalog............................................... 13Acknowledgments..................................................... 16References.......................................................... 17
ILLUSTRATIONS
Figure 1 Block diagram of the NCERtelemetered seismograph system........................ 4
2 System response of a typicalNCER telemetered seismograph station.................. 5
3 Map showing principal seismographstations used in locating earthquakes................. 11
4 Map showing earthquake epicenters reportedin the Appendix....................................... 15
TABLES
Table 1 Station data.............................................. 6
APPENDIX
Central California Earthquakes, 1974................................ 19
INTRODUCTION
Numerous small earthquakes occur each day in the Coast Ranges of central California. The detailed study of these earthquakes provides a tool for gaining insight into the tectonic and physical processes responsible for the generation of damaging earthquakes. This catalog contains the fundamental parameters for earthquakes located within and adjacent to the seismograph network operated by the National Center for Earthquake Research (NCER), U.S. Geological Survey, for the year 1974.
The motivation for these detailed studies has been described by Pakiser and others (1969) and by Eaton and others (1970). Similar catalogs of earthquakes for the years 1969, 1970, and 1971 have been prepared by Lee and others (1972b, c and d). Catalogs for the first, second, third, and fourth quarters of 1972 and the first, second, third, and fourth quarters of 1973 have been prepared by Wesson and others (1972a, b, 1973b, and 1974a and b), by Bufe and others U975J, and by Lester and others (1976a and b). The basic data contained in these catalogs provide a foundation for further studies.
This catalog contains data on 3073 earthquakes in central California. Arrival times at 152 seismograph stations were used to locate the earthquakes listed in this catalog. Of these 136 were telemetered stations operated by NCER. Readings from the remaining 16 stations were obtained through the courtesy of the Seismographic Station, University of California, Berkeley (UCB), and the California Department of Water Resources, Sacramento.
The Seismographic Station of the University of California, Berkeley, has for many years published a bulletin that both describes earthquakes in northern California and the surrounding area and lists readings at UCB stations from more distant events. The purpose of the present catalog is not to replace the UCB Bulletin, but rather to supplement it, by decribing the seismicity of a portion of central California in much greater detail.
INSTRUMENTATION
The telemetered seismograph system used is illustrated by the block diagram in Figure 1. The equipment at each station includes a vertical component, 1 Hz seismometer (usually Mark Products, Model L-4C), a package containing a preamplifier and voltage-controlled oscillator (usually Develco, Model 6202), and batteries. The frequency-modulated tone produced at each station is carried by wire (occasionally by radio) to a terminal where it is combined with tones from up to 7 other stations The resulting multiplexed signal is then transmitted by voice-grade telephone circuits or radio to the NCER office in Menlo Park, California.
The eight channels of data on each line are separated and demodulated by discriminators (usually Develco, Model 6203), and recorded on 16 mm film using a Develocorder (Teledyne, Geotech, Model FR-400). Each Develo- corder records seismic signals from up to 17 stations. In addition, 2 timing signals (WWVB on 2 traces, and a chronometer on 1 trace) are recorded simultaneously with the seismic signals.
Figure 2 illustrates the overall response of the seismic system for a typical station. Magnification for individual stations is adjusted according to the background noise level in steps of 6 decibels. As a result, the response for an individual station may differ from that of the typical station by a factor of 2, 4, 8, or 16. Precise calibrations indicate that most stations are operated at magnifications of 25,000 to 100,000 at 1 Hz.
All stations used in the present study are listed in Table 1. Station locations are plotted on Figure 3, except for 13 stations which are located outside the map boundaries.
DATA PROCESSING AND ANALYSIS
The telemetered seismic data recorded on 16 mm film were processed manually to yield information on first P-arrivals, directions of first motions, maximum amplitudes, and signal durations. These data were then processed by computer, using the HYP071 computer program (Lee and Lahr, 1972), to give origin time, hypocenter location, magnitude, and pattern of first motions of the earthquakes. Each roll of film contains about 24 hours recording and was processed in the following steps" (1) scanning, (2) timing, (3) preparing punched cards, (4) batch processing by computer program HYP071, (5) correcting errors, (6) adding data from other sources, (7) rerunning HYP071, (8) analyzing poor solutions, and (9) eliminating explosions.
In March of 1973 an automatic real-time earthquake detection system was introduced. It resembles but was different in many respects to that described by Stewart and others (1971). During the period reported here, this new system was only experimental and was not used to replace the technique of manually scanning films to detect earthquakes.
In the routine data processing, local events with signal duration of 10 seconds or more were always timed (see p. 12 for an explanation of signal duration). This corresponds to a cutoff at about magnitude 1 for events within the NCER network. Some smaller events for which 6 clear first arrivals could be obtained were also timed. The magnitude cutoff for events outside, but near the NCER network, was somewhat larger than 1. The catalog of earthquakes reported here contains all hypocenter solutions obtained, based on the above criteria. Because the station coverage was not uniform and because some events outside the network were reported, the cutoff for small magnitudes was not uniform over the entire area reported.
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FREQUENCY
100
Figure 2 System response of a typical NCER telemetered seismograph station. This magnification curve is obtained for a typi cal system (L-4C seismometer, Develco VCO/Amplifier, Develco Discriminator, and Geotech Develocorder) with electronic gains adjusted to produce a 10 mm peak-to-peak record ampli tude when a 10 v rms, 5 Hz, calibration signal is intro duced in place of the seismometer (attenution set at 42 db).
CODE
TABLE 1. STATION DATA
OES TELEMETERED STATIONS
LAT N LONG W ELV DCE) 0(W> NOTE**
ABPACHALMALXANDAN6
ANZARNBBRBCRBENB6H
BGMBOLBROBRPBTWBVL
BWRCALCANCARCASCBC
CBOCCRCDRCHRCNRCNS
COECOPCRNCRKCSHCYH
DILDIRDOODSRDURE6R
37-56.3537-58.5737- 9,5038-42.6537- 9.7737-51.68
36-53,0837-20'.9638-15.6537- 9.6236-30.6037-20.52
36-35.4837-48.9738- 0,4838-40.0736-18.9036-34.51
37-55.4537-27.0737- 1,5238-19.2835-55,9036-55.88
37- 6.7137-47.3038-22.1936-57.4636-42.5537-56.33
37-15,4637-58^3638- 1.1237-14.5037-38,8837-33154
f -36-50.1236-20.1837-43,8037-57,9838- 1.7837- 2.11
122-45.53121-45.62121-50,82122-45.30121-37.45122-25.77
121-35.45121-3T.96122-32.99122- 1.57121- 4.53122-20.34
121- 1.52122- 3.72120-24,92122-11.60120-55.75121-11 .34
122- 6.40121-47,95121-29.02122-47.73120-20.22121-39163
121-41.33121-57.00122-27 ? 70121r35'.01121-20.60120-31.76
121-40,35120-37.02120-30.57122- 7.82122-02,57122- V.62
_ T121-38.64120-22,58121-50,12122-15,17122- 0,05122- 6.25
14074
244379244223
122628137660448158
1216610387867381510
22126533298
1189219
192185620241305373
36633647560717038
204496198109168442
211111
211222
111122
111112
111121
111211
211112
(3.5)7.01.60.83.02.2
4 p 43,92.23,73,43.8
3.04.6(3,5)3.92.13.1
5.14.93.62.2
V4.4
2.27.12.22.14.8(3.5)
5 9(3^5)(3.5)4.0(3.5)21 5
3.25.16.8(3,5)5.4ii?
(3.5) 01/01 TO 10/316.21.8(3.5)3.22.2
1.44^22.24.73.03.8
(3.5)5.0
(3.5)(3.5) 05/10 TO 12/312.10.6
5.14.35.0.2.25.23.2
2.77.12.23.60.7(3.5)
6,8(3.5)(3.5)4.44.03.2
,.2,24<66.8 .
(3', 5)5.41.7
6
CODE
TABLE 1. STATION DATA (CONTINUED)
OES TELEMETERED STATIONS
LAT N LONG W ELV D(E) D(W)
EKHEMMEUCFELFRPFWL
GDHGHSGVRHCCHECHER
HMRJHCJOLJONLCHLNS
LORLRVLTRLTWLWRMCM
MDCMGAMHRMILMIXMNR
MOBMONMOPMORMRSMSJ
MUSOBFOCROLCPALPCL
36-39^8836-39.6837- 3.0436-59,0036-4512238- 1.17
35-49.8637- 5.7538-16.8436-58.8835-40.9336-22.38
38- 9.2836-32.8236- 5.0236-36.6537-44.2838- 9.15
36-14.7936-25.4636-53.0737-21.2236-39.9637-53.17
37-52'.9037-38.2237-21.5737-46,8838-24.6837-35.68
37-27,0136-36.0336-12.9137-48.6836-39.4837-31.25
38-33^0337-54.0036-55.0338- 2.3837-37.8837- 3.13
121-10145121- 5.76121-48.56121-24.09121-29.43120-35.00
120-21.17121-26.83122-12^89121-43.35121-09.15120-49.13
121-48.02121-23.53121-10.15121-18.81122- 3.83122-42.75
121- 2.55121- 1.08121-18.49122-12.25121-16.36120-30.40
121-54.85122-28.43121-45.38122-10 f 55122- 3.44121-38.22
122-11.00121-55,06120-47.69121-48.15120-^7.62121-52.23
122-43.37120-34.04121-30.46122-47.55121757,37121-17.40
342488438323705880
433778257159514750
65207336
1052312120
308555183270232362
117320151890
177500
21192784792769498
1341769830
463152
112121
111221
122211
221221
121111
122111
111211
1.60.83.03.22.2
(3.5)
3.32,35,24.04,34.3
6*. 30.92.11.54.31.9
0.15.53.03.85.1
(3.5)
4.82.45.33.15.74.6
3.81.11.86.63.94.3
3.3(3.5)3.02,64.32.2
4*.0
2.23.84.30.8(3.5)
3.44.45.24.24.30.8
6.30.91.10.74.61.9
0.12.14.53.42.4
(3.5)
4.82.46.2(3.5)5.74.6
2.61.11.96.63.84.3
3.3(3.5)4.42*64^13.6
NOTE
01/31 TO 12/31
01/01 TO 06/01
CODE
TABLE 1. STATION DATA (CONTINUED)
OES TELEMETERED STATIONS
LAT N LONG W ELV DCE) 0(W) NOTE
PESPFPPKFPKHPLVPMR
PNCPNMPNPPTVQSRRBM
RUSSACSAW
SBAISBCCSBCD
SBLCSBLGSBLPSBSCSBSMSBSN
SFRSFTSGMSHCSHGSHR
SJGSL1SL2SL3SL4SL5
SL6SL7SL8SPTSRSSTC
37-11,9436-13.8235-52.9136-51.3836-58.6236-57.19
36-33.7338-50.8536-10,1236- 6*. 5036-50.0236-50.70
37-54 r 7537-34.9537-12.7434-00.8034-56".4834-22.12
34-29.7934- 6.5734-33 f 6233-59.6834- 2.2533-14.70
37-47.2837-24.3138-52.0338-40.2236-24.8338-31.20
36-47^8837-04.87377 01 f 9037-06.8837-00.2637-04.26
^37-01.7037-01.7837-04.8138-10.9636T 40.1136-38;iO
122-20.90121-46.32120-24.81121-24.37121-49.93121-41.70
121-38.18122-56.78121-22.68120-43.27121-12.76120-49.40
121-54.33122-25.03122-10.06119-26.23120-10.32119-20.63
119-42.81119- 3.85120-24.03119-37.99120-20.99119-30.40
122-23.37122-10.55122-42.58122-38.03121-15.22122-36.43
121-34U3121-03.67121-03 ? 32121r08.29121-06.90121-d9".36
^121-05.52121-08.41121-05.65122-27 ? 20121-31.13121-14.38
8434946912215894
305783
1591506536372
331207262113610213
1190415134457172259
8143
10801200192328
171116293189219180
30221912288
399259
211122
212211
122222
222222
111121
211111
111122
V2.24.34.64.93.7
lU1 i?2.11,9V5?7
4.82.24.6(3.5)(3.5)(3.5)
(3.5)(3.5)(3.5)(3.5)(3.5)(3.5)
1.94104.11.30.52.0
3.02.32.32.32.32.3
2.32.32. 32.3VIf - £
2,52.45.36.54.03.5
1.61.61.31.9
; 4.0- 5^4
4.82.24.0(3.5)(3.5)(3.5)
(3.5)(3.5)(3.5)(3.5)(3.5)(3.5)
1.94.04.0 07/021.60.12.0
1.55.2 02/285.2 02/285.2 02/285.2 02/285.2 02/28
* 5.2 02/28* 5.2 02/28
5.2 02/282.20,5 ~1.9
TO 12/31
TO 12/31TO 12/31TO 12/31TO 12/31TO 12/31
TO 12/31TO 12/31TO 12/31
8
TABLE 1. STATION DATA (CONTINUED)
OES TELEMETERED STATIONS
ODE
STJSTNSTVSVCTAYTMN
TWNWDSWHWWKR
t LAT N
37-20.0337-54 p 2737-17.0737-17.113*-56.7338-23.15
36-03^1637-25.*0838-27,4235-48.87
LONG W
122- 5.48120-24,29122- 7.42121-46.35120-28.45122-40.83
121-30U5122-16.33122-53.26120-30.67
ELV
122366357128552105
147628050
503
K
112111
2212
D(E)
6.1(3,5)3.05.44.32.7
2*43,3r.64.2
DCW)
Ail(3 f 5)3.04.85.62.7
oU2.51.64.4
NOTE**
THIS COLUMN INDICATES THE OPERATION PERIOD. IF IT IS 9LANK THEN THIS STATION HAS BEEN OPERATED CONTINUOUSLY DURING 1974
UNIVERSITY OF CALIFORNIA STATIONS
CODE LAT N LONG W ELV DCE) DCW)
BKSBRKFHCFRIGCCJAS
LLAMHCMINPCCPRIPRS
SAOWDC
37-52.6037-52.4040-48,1036-59,5037- 1.8037-56.80
36-37,0037T 20,5040-20,7037-30,00
-367 *s 50. 36-19190
36-45^9040-34.80
122-14.10122-15.60123-59.10119-42,50121-59.80120-26.30
120-56.60121^38,50121-36.30122-22.90120-39.90121-22.20
121-26",70122-*2.40
27681
610119122457
47512821495
911187363
350300
111121
111212
21
2.42.4
(3,5)C3'.5>1.7
(3.5)
V4.5
(3.5)3.74.01.1
2>(3'. 5)
2.42.4
(3.5)(3.5)1.7
(3.5)
2.15.0
(3.5)3.74.01.1
1.0(3.5)
TABLE ll STATION DATA (CONTINUED)
CALIFORNIA DEPARTMENT OF WATER RESOURCES STATIONS
CODE LAT N LONG W ELV K D(E) D(W)
ORV 39-33 v.33 121-30^.00 362 1 (3.5) (3U) SLD 37-04.48 121-13.33 443 1 2.3 5.2
*LAT AND LONG ARE LATITUDE AND LONGITUDE IN DEGREES AND MINUTES. ELV IS ELEVATION IN METERS. D(E) AND D(W) ARE GIVEN IN KILOMETERS. SEE TEXT (P. 12 ) FOR EXPLANATION OF K, D(E), AND D(U).
10
40.00*
lSAN FRANCISCO\\
A NCER TELEMETERED STATION
O STATION OPERATED BY UCB
STATION OPERATED BY COWR
0 SOKM
35.50*'
Figure 3. Map showing principal seismograph stations used in locating earthquakes.
11
Location of earthquakes was based mainly on first P-arrivals. When an adequate location could not be obtained using P-arrivals alone, S-arrivals were used to supplement the P-arrivals whenever possible. The HYP071 computer program uses Geiger's method (Geiger, 1912) to determine hypocenters by minimizing the residuals between observed and calculated arrivals in a least-squares sense. Traveltimes from a trial hypocenter to the stations and their partial derivatives are computed on the assumptions of a horizontal multilayer velocity model by a technique introduced by Eaton (1969).
The crustal velocity model used was derived mostly from analysis of explosion data by Wesson and others (1973a). It is specified by:
Layer Depth (km) P-velocity (tap/sec) S-velocity (km/sec)
1 0 to D 4.0 2.22 D to 15 5.9 3.33 15 to 25 6.8 3.84 below 25 8.05 4.5
The variable boundary between the first and second layer (depth D) is determined for each station from time-term analysis of explosion data. The variable first layer in the crustal model is an approximation of the sedimentary layer above the Pg refractor. To allow for sharp changes in sediment thickness across the San Andreas fault, two D values for each station were determined: one for sources east of the fault, and the other for sources west of the fault. The set of D values to be used in the program is determined by the location, relative to the fault, of the station with the earliest P-arrival time. For example, if the earliest P-arrival occurs at a station west of the fault, then the set of D values appropriate to the sources on the west side, D(W), of the fault is selected. Table 1 shows values of D, in kilometers, at each station for sources east (D(E)) and west (D(W)) of the San Andreas fault, as well as the location of the stations relative to the fault (K = 1 for east, and K = 2 for west). An assumed value for D of 3.5 km (about the median of the calculated values) is given in parentheses if a value could not be determined from the explosion data.
The method used for estimating the Richter magnitude of the earth quakes has been described by Lee and others (1972a). In brief, the magnitude of an earthquake is based on the average of magnitudes estimated at various stations. Station magnitude (M) is derived from its recorded signal duration (T) according to:
M = -0.87 + 2.00 log (T) + 0.0035A
where A is the epicentral distance in kilometers. The signal duration is defined as the duration time in seconds from the onset of the first P-arrival to the point where the trace amplitude (peak-to-peak) falls below 1 cm as it appears on the Geotech film viewer.
12
For earthquakes with Richter magnitudes of 3.5 and below, equation (1) gives a good estimate of the magnitude: however, for Richter magni tudes above 3.5, the relationship between signal duration and magnitude is still under investigation. Therefore, for earthquakes with signal duration magnitudes of 3.5 or greater, Richter magnitudes have been calculated (Richter, 1942) using records obtained from the UCB Wood- Anderson seismographs at Berkeley and Mount Hamilton, and the Stanford- USGS Wood-Anderson at Palo Alto. The earthquakes for which the Richter magnitude has been determined from Wood-Anderson records are indicated in the Appendix by an R next to the magnitude.
A substantial effort has been made to identify man-made explosions so as to eliminate them from the catalog* Explosions can be identified on the basis of one or more of the following criteria: location of a known quarry or blasting site, shallow focal depth, time of day, focal mechanism, and/or through correspondence with quarry operators. During 1974, 138 blasts were identified and eliminated from the catalog.
DISCUSSION OF CATALOG
The parameters for the earthquakes listed in the Appendix include the origin time, location of hypocenter (epicenter and focal depth), and magnitude. In addition, six other parameters are listed so that an evaluation of the quality of the hypocenter solution may be made. These parameters are (1) the largest azimuthal separation between stations, GAP, (2) epicentral distance to the nearest station, DMIN, (3) root-mean-square error of the time residuals, RMS, (4) standard error of the epicenter, ERH, (5) standard error of the focal depth, ERZ, and (6) number of P- and S-arrivals used in locating the event, NO. Based on these parameters, the general reliability of each earthquake solution is graded as either excellent (A), good (B), fair (C), or poor (D). Exact rules of quality classification are given in the Appendix.
A brief discussion on the accuracy of hypocenter determinations has been given by Lee and others (1971). To obtain a reliable epicenter, GAP should be less than 180*: to obtain a reliable focal depth, DMIN should be less than the focal depth. In addition, systematic errors arise from uncertainties in the crustal velocity model. These errors cannot be determined except through controlled experiments, e.g., known explosions in the focal region. Because we present all hypocenter solutions of earthquakes in the region we studied, their quality varies. Although standard errors of epicenter and focal depth (ERH and ERZ) are given, they must be interpreted with caution, especially for quality C and D solutions. Hypocenter solutions for known blasts distributed throughout the San Francisco Bay region indicate that the true positions are often within the standard error limits of the solutions, provided that the conditions GAP < 180° and DMIN is within a few kilometers are met. For example, comparison of locations determined for well-recorded quarry blasts (solution quality A) with the known coordinates indicate a typical
13
error of about 1 km. Based on comparisons between calculated and true quarry blast locations, a general statement on the accuracy of our hypocenter solutions is as follows:
Solution Quality Approximate accuracy inEpicenter Focal Depth
A (excellent)B (good)C (fair)D (poor)
12.555
kmkmkmkm
2 km5 km5 km5 km
Epicenters listed in the Appendix are plotted according to magnitude in Figure 4.
The dashed lines in Figure 4 indicate the boundaries of the NCER seis mograph network as it existed during 1974. We feel that the hypocenters listed in the the Appendix represent a nearly complete set of earthquakes above magnitude 1 within these boundaries and that these earthquakes are generally well located. Earthquakes outside the dashed boundaries in Figure 4 tend to have less reliable locations, depending on their distance from the network and their relationship to its geometry. Further, the minimum magnitude event that we can detect and locate increases with increasing distance from the network. For earthquakes outside the network, which yielded unsatisfactory locations on the basis of first P-arrivals alone, S-arrivals were included whenever possible.
We believe that the precision of the earthquake locations (or the relative locations) is better than the absolute accuracy of the earthquake locations. Despite our attempts to model the laterally inhomogeneous nature of the velocity structure within the earth's crust using a variable surface layer, we suspect that the locations within certain parts of the area included in the boundaries of the network may be systematically biased by as much as 2-3 km (Mayer-Rosa, 1973).
Some of the earthquakes listed in this catalog represent multiple events, that is, earthquakes from a given source region which occur in such rapid succession that the seismographs are still recording arrivals from one earthquake when the first arrivals from a following earthquake begin to appear. Depending on the size of the individual events and their separation in time, it may not be possible to accurately time and locate the later event(s), and therefore only the location of the first event in the multiple sequence is listed in the Appendix.
The contents of the Appendix, along with similar location information for central California earthquakes since 1969, may be obtained (at modest cost) in forms amenable to computer input (magnetic tape) by contacting:
National Geophysical Data Center Environmental Data Service
NOAA Boulder, CO 80302
14
40C O.CO
SYMBOL MAGNITUDE
M < I 5
15 < M < 25
x 25 < M < 35
X 35 < M <X M > 45
Figure 4. Map showing earthquake epicenters reported in the Appendix, Earthquakes in the region enclosed by the dashed line are generally well recorded and located.
15
ACKNOWLEDGEMENTS
Some of the arrival times used in this study were obtained through the courtesy of the Seismographic Station, University of California, Berkeley, and the California Department of Water Resources, Sacramento. We thank Dr. B. A. Bolt, Director of the first institution, and Mr. Paul Morrison of the last institution, for their cooperation. Roy Miller of UCB and his staff offered generous help with their data and records. We are indebted to many quarry operators for helping us to eliminate blasts from the earthquake catalog.
We are grateful to Wayne Jackson, John Van Schaack, Ron Radarabek, Wes Hall and their associates for operating the NCER seismograph stations and telemetry network. We thank Shirley Marks, Carol McHugh, Sharon Kirkman, and Sue Conens for their help in various phases of data processing and for comments on the manuscript.
We are most deeply indebted to J. P. Eaton, W. H. K. Lee, J. C. Lahr, and J. H. Pfluke of NCER for their development of the techniques and computer programs which have made the preparation of this catalog a routine production.
16
REFERENCES
Bufe, C. G., F. W. Lester, K. L. Meagher, and R. L. Wesson, Catalog of earthquakes along the San Andreas fault system in central California, April-June, 1973, U.S. Geological Survey Open-File Report 75-125, 44 p., 1975.
Eaton, J. P., HYPOLAYR - a computer program for determining hypocenters of local earthquakes in an earth consisting of uniform flat layers over a half space. U.S. Geological Survey Open-File Report, 155 p., 1969.
Eaton, J. P., W. H. K. Lee, and L. C. Pakiser, Use of mi cr ©earthquakes in the study of the mechanics of earthquake generation along the San Andreas fault in central California, Tectonophysics , v. 9, p. 259-282, 1970.
Geiger, L. , Probability method for the determination of earthquake epi centers from the arrival time only (translated from Geiger 's 1910 German article) Bulletin of St. Louis University, v. 8, p. 56-71,
Lee, W. H. K. , and J. C. Lahr, HYP071: a computer program for determining hypocenter, magnitude, and first motion pattern of local earthquakes, U.S. Geological Survey Open-File Report, 100 p., 1972.
Lee, W. H., K. , J. P. Eaton, and E. E. Brabb, The earthquake sequence near Danville, California, 1970, Bulletin Seismological Society of America, v. 61^, p. 1771-1794, 1971.
Lee, W. H. K. , R. E. Bennett, and K. L. Meagher, A method of estimating magnitude of local earthquakes from signal duration, U.S. Geological Survey Open-File Report, 18 p., 1972a.
Lee, W. H. K. , J. C. Roller, P. G. Bauer, and J. D. Johnson, Catalog of earthquakes along the San Andreas fault system in central California for the year 1969, U.S. Geological Survey Open-File Report, 49 p., 1972b.
Lee, W. H. K. , J. C. Roller, K. L. Meagher, and R. E. Bennett, Catalog of earthquakes along the San Andreas fault system in central California for the year 1970, U.S. Geological Survey Open-File Report, 73 p., 1972c.
Lee, W. H. K. , K. L. Meagher, R. E. Bennett, and E. E. Matamoros, Catalog of earthquakes along the San Andreas fault system in central California for the year 1971, U.S. Geological Survey Open-File Report, 62 p., 1972d.
17
Lester, F. W., K. L. Meagher, and R. L. Wesson, Catalog of earthquakes along the San Andreas fault system in central California, July-September, 1973, U.S. Geological Survey Open-File Report 76-169, 38 p., 1976a.
Lester, F. W., S. L. Kirkman, and K. L. Meagher, Catalog of earthquakes along the San Andreas fault system in central California, October - December 1973, U.S. Geological Survey Open-File Report 76-732, 37 p., 1976b.
Mayer-Rosa, Dieter, Traveltime anomalies and distribution of earthquakes along the Calaveras fault zone, California, Bulletin Seismological Society of America, v. 63, p. 713-729, 1973.
Pakiser, L. C., J. P. Eaton, J. H. Healy, and C. B. Raleigh, Earthquake prediction and control, Science, v. 166, p. 1467-1474, 1969.
Richter, C. F., An instrumental earthquake magnitude scale, Bulletin Seismological Society of America, v. 25, p. 1-32, 1942.
Stewart, S. W., W. H. K. Lee, and J. P. Eaton, Location and real-time detection of microearthquakes along the San Andreas fault system in central California, Recent Crustal Movements, Royal Society of New Zealand Bulletin, v. 9, p. 205-209, 1971.
Wesson, R. L., R. E. Bennett, and K. L. Meagher, Catalog of earthquakes along the San Andreas fault system in central California, January-March, 1972, U.S. Geological Survey Open-File Report, 60 p., 1972a.
Wesson, R. L., R. E. Bennett, and F. W. Lester, Catalog of earthquakes along the San Andreas fault system in central California, April- June, 1972, U.S. Geological Survey Open-File Report, 42 p., 1972b.
Wesson, R. L., J. C. Roller, and W. H. K. Lee, Time-term analysis and geologic interpretation of seismic traveltime data from the Coast Ranges of central California, Bulletin Seismological Society of America, v. 63, p. 1447-1471, 1973a.
Wesson, R. L., K. L. Meagher, and F. W. Lester, Catalog of earthquakes along the San Andreas fault system in central California, July- September, 1972, U.S. Geological Survey Open-File Report, 49 p., 1973b.
Wesson, R. L., F. W. Lester, and K. L. Meagher, Catalog of earthquakes along the San Andreas fault system in central California, October- December, 1972, U.S. Geological Survey Open-File Report, 46 p., 1974a
Wesson, R. L., F. W. Lester, and K. L. Meagher, Catalog of earthquakes along the San Andreas fault system in central California, January- March, 1973, U.S. Geological Survey Open-File Report, 46 p., 1974b.
18
APPENDIX; CATALOG OF EARTHQUAKES FOR THE YEAR 1974
Earthquakes along the San Andreas fault system in central California for 1974, are listed chronologically in this Appendix.
The following data are given for each event:
1. Origin time in Coordinated Universal Time (UTC): date, hour (HR), minute (MN), and second (SEC). To convert to Pacific Standard Time (PST), subtract eight hours, to Pacific Daylight Time (PDT), subtract seven hours.
2. Epicenter in degrees and minutes of north latitutde (LAT N) and west longitude (LONG W).
3. DEPTH, depth of focus in kilometers. If "*" follows the DEPTH, it means that the focal depth is constrained by the location program.
4. MAG, local magnitude of the earthquake. If "R" follows the magnitude, it indicates the Richter magnitude calculated from Wood-Anderson seismograph records.
5. NO, number of P- and S-arrivals used in locating earthquake.
6. GAP, largest azimuthal separation in degrees between stations.
7. DMIN, epicentral distance in kilometers to the nearest station.
8. RMS, root-mean-square error of the time residuals:
RMS = / I R i
where R^ £ s the observed seismic-wave arrival time minus the computed time at the ith station.
9. ERH, standard error of the epicenter in kilometers:
ERH » / SDXZ + SDYZ
where SDK and SDY are the standard errors in latitude and longitude, respectively, of the epicenter.
10. ERZ, standard error of the depth in kilometers.
11. Q, solution quality of the hypocenter. This measure is intended to indicate the general reliability of each solution.
19
Epicenter Focal Depth
A B C D
excellent good fair poor
good fair poor poor
Q is based on both the nature of the station distribution with respect to the earthquake and the statistical measure of the solution. These two factors are each rated independently according to the following schemes.
Station Distribution
NO
A B C D Others
GAP
±9°I135 <180
DMIN
< DEPTH or 5 kmT 2 x DEPTH or 10 km< 50 km
Statistical Measures
A B C D
RMS (sec)
< 0.15 < 0.30 < 0.50 Others
ERH (km)
-? 1.0< 2.5< 5.0
ERZ (km)
2.0 5.0
Q is taken as the average of the ratings from the two schemes, i.e., an A and a C yield a B, and two B's yield a B. When the two ratings are only one level apart the lower one is used, i.e., an A and a B yield a B.
12. QUADRANGLE, for earthquakes between 35o QO.O 1 and 40° 00.0* N latitude and 119o 45.0' and 123° 45.0' W. longitude, QUADRANGLE indicates the name of the U.S. Geological Survey 7.5 quadrangle (or quadrant of 15* quadrangle), on which the epicenter is located. For earthquakes offshore or outside the designated area, the entry is starred and indicates the general geographic area in which the epicenter is located, for example, "***MONTEREY BAY***".
20
CE
NT
RA
L
CA
LIF
OR
NIA
F
AP
TH
fiU
A<
FS
--1
l?7
4
19
74
JA
N
1 1 1 1 1 1 1 2 2 2 2 2 2 3 3 3 3 3 3 4 4 4 5 5 5 5 5 5 5 6 6 6 6 6 6 6 6 7 7 7 7 7 7 7 7
HR
M
N
6 12
7 9
7 58
9 35
15
0
17
47
23
39
1 1
52
318
6
18
41
9
25
21
61
32
3 3
2
8 55
11
28
1315
21
38
0 1
5
10
50
17
2
53
56
4 0
4 1
2
10
4
617
2
722
5
22
3
61
12
2 35
2 41
3 6
4 55
5 6
21
52
22
43
1 3
75
53
10
38
1 1
91
5 4
516
30
17
0
18
14
sec
14
.010.9
53
.635.6
46.9
4.0
54,9
47.0
20*.
99
*8
19,7
23
?1
8,4
45^3
34.6
16,2
40*
79.8
13.6
58.0
5 6*
. 8
38.5
47
.151.0
4*.
6
59
.51
9.0
58.3
53
,01711
17
.43
5*8
59
.154.1
27.8
39.0
u'.o
17
.41
2.0
39
1 7
29
.35?.
43
9.4
47.0
43
.4
LA
T
N
38-4
412
36-2
7.
337-3
8.
33
6-5
0.6
35
-48
.0
36-5
7.7
36
-31
, 5
36
-54
,637-3
7,9
36
-46
.9
37-1
2^0
36-4
4t5
36
-30
*8
36
-1 6
, 0
36
-41
.2
36
-56
17
37-1
7,3
36
-27
.236-3
0.3
36-5
6*.
8
37
-45
', 6
36
-36
.73
7-2
6.9
37
-15
. 3
36-2
4*.
1
36
-56
. 8
36-3
8.8
36-4
5.2
37-4
9'.8
36-3
8'. 3
36-5
7.2
36
-57
,13
6-4
4'. 0
36-3
9.8
36
-28
.4
37
-25
,037-2
5'. 5
37
-50
.736-3
2.
337-
0.9
36-4
5.
83
7-5
H.3
35-5
7.7
37
-51
.8
36-3
*.
2
LON
G
W
1 22-4
4.0
12
1-
4.3
1?
2-
1 .9
121-3
4.5
12
1-
9.6
121
-39.
01
21
- 7.0
121-4
7f
91
21-4
3.9
12
1-3
1 .
3
% 2
1-4
31
51
1*1
-27
.31
21
- 7t9
;i2
0-4
3R
7,;<
121 -
20.1
' 121-3
6f
51
21
-38
16
12
1-
4.7
12
1-
7.1
121-2
5.9
121-5
6.7
121-1
5.0
1 2
1-3
2.1
121-5
7,8
1 20-5
8*.
1
121-3
6.9
121-1
7.6
121-2
0,8
12
1-5
61
1121-1
6.9
121-3
8.0
. 121-3
7,5
121-2
5.6
121-1
9.4
12
1-
2.8
121-4
9.2
1 2
1 -
4 1
1 6
122-1
7,5
12
1-
8.6
121-4
3.1
121-2
8.0
121-5
9.0
120-5
6.7
1 21
-57.
P121-1
6.9
DF
PT
H
?.8
5]2
2.P
5.
S8
.1
2.5
8.4
11.2 slo
7.5
9.0
6.8
1 0
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10,3
3.1
9,6
3.0
5.7
7.5
415
5.8
5.5
7.8
5.3
8.1
1 .7
1 3
.17.4
1.0
5.2
3.5
5l4
5.4
1 5
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3.2 Us
5.0
9.4
9.9
5.8
11.8
1 3.S
5.^
1.4
MA
G
1,8
n . *
1 .0
1 .5
11
*
O.R
1 .
11
.1nl
*2
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0.9
2,0
0.9
1 .7
0.4
V n.9
1 ?R
1.3
1 .4 r
31 !
i1 ,3 1t
71.7
0.5
1 .1
n.7
1 .6
1 .5
1 .7
n.9
1 1 1
2.1
n.p
n.7
n 1 °
1 .3
n.9
1 .7
Ol9
1 .2
1.?
1 .0
nil
NO 9 7
1 3
1 6 9
10
1 1
1 3 7
27 16
25 9 7 7 8 9
20 8
16
1 3
1 4 9
1 6
11 10 1 2
1 0
16
10
23 m 1 5
21 7 9 9
1 1 7
24 R
1 3 6
1 1 8
GA
P
1*7
12
858 72
??
3
60 84
178
15
78
8 80
73
91 111
11
6 79
86
63
'
95 75 55
60
20
85
81
25 84 52
90 57
57
45 63 69
59
161
11
81
06
98
154 48
90
611
69
7S S7
DM
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55
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31
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3j5
4S,0 8(
n
4!?
8,'0
5*1 V 2:6
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6,2
3.8
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2?
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14
4
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«»
10
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3*0
2,8
5»
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53
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3*4
& 456
17
10
4 2
9 ,
21
2.4
51 7
3.7
213
4,0
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4,R
3,3
RM
S
o.m
0.1
20.1
50.1
5O
lU
0.0
50.1
30
,11
O',
08
0.1
4
0.1
10^16
0,1
20
,06
0:06
0.1
00
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0,1
10
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0.1
4
otn
0,0
70^20
0.0
70112
0.0
60
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Of
09
01
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0.0
6
0,1
30.0
90
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0.1
00
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0.1
20
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0.1
10
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0.1
0
0",
13
0.0
90
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0,1
70
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3
FR
H
1 '
1
1.2
n'1'
6
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72.2
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2
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0,3
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0,6
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*9 °i? 0*3
1.4
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0.6
1*
4
014
1*6
°0j7
0'8
1^8
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1^6
ni
92
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VOf,2
Q C 8 9 B D A A 9 B A A 8 B B B A A"
9 B B A A D B B A A
.'' "
B A B B a B 3 A 8 A C B A
QU
AD
RA
NG
LE
MO
UN
T
ST
H
ELE
NA
TO
PO
V
AL
LE
YH
AY
WA
RD
SA
N
JUA
N
BA
UT
IST
AR
UR
NE
TT
P
EA
K
WA
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ON
VIL
LE
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AS
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AN
P
EN
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WA
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ON
VIL
LE
W
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TA
LT
AM
ON
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AN
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AN
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AU
TIS
TA
MO
RG
AN
H
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MT
HA
RLA
NB
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MO
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C
AN
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NS
AN
B
EN
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M
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AIN
PA
ICIN
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CH
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NL
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VA
TO
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TO
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AL
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YS
AN
B
EN
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SA
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LIP
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:
DIA
BL
OB
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MO
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C
AN
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NH
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LA
R
MT
NS
AN
JO
SE
W
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TR
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SP
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CH
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PIN
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RV
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MT
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AM
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V
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PL
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S
21
CENTRAL CALIFORNIA FAR THOUAKFS--1974 (CONTINUFD)
1974
HR MM
SEC
LAT
NLONG W
OFPTH
MAG
NO GAP
DM IN
RMS
FRH
FRZ Q
QUADRANGLE
JAN
7 7 8 8 8 8 8 8 8 9 9 9 9
10
10
10
10
10
10
10
10
10
10
10
10
10
10
10
10
10
10 10
10
10
10
10
10
10
10 10 11 11 11 11 11
?1
422
22
n 57
3 56
4 4
9
11
12
13
6
16
38
20
30
5 3
2
6 0
20
17
21
8
7 3
79
27
9 35
10
5
511
8
11
18
11
19
11
22
11
33
11
37
11
38
11
44
12
21
12
26
12
53
13
01
3
5
13
2114
26
14
29
15
17
17
7
18
5
819
14
21
21
23
12
23
47
0 50
n 56
1 47
5 2
911
2
6
8.6
13
.55
?.
420.8
is; 6 9.3
58.3
32'.
11
4.4
17.9
42.7
39
.638.4
16.2
31:6
27".
64
1.4
30.0
1 .7
2 9*
. 9
24
.739.6
10
,55
.810.4
25.1
52
^3
57
.859.2
36
,11
19,4
22*.
747.0
23
.027.1
2U
22
9^2
53
.642.4
29'.9
19.2
45.5
9.4
42.2
24.2
37
-51
.9
36
-V3
.63
6-3
3.9
36-3
5.7
38
-2?
. 8
37-2
5.2
37-2
1.8
37
-29
^0
37-2
2.9
36-2
7.7
37
- 3y6
36-3
6f
43
6-4
5.8
36-3
3.7
36-3
7*7
36-3
7^8
36
-37
.63
7-3
2.
33
7-3
2*
0
37-3
2.2
36-5
7.1
37-3
2.3
36-3
7.8
36-3
3.5
36
-57
. 1
36
-56
.836-5
7.1
36
-37
*.4
36
-57
.03
6-5
7;
1
37
- 2
.636-5
7,0
36
-57
.236-5
6.9
36-5
6;9
36
-5l'.7
36-4
9.1
36
-57
, 2
38-4
2".
836-5
8*.
8
37-4
7.9
37-4
7.8
37
-47
. 7
37
-10
*. 4
36-2
7.8
1 2
1-5
8.
5121-1
?.
11
21
-11
. 5
121-1
1 .
4122-3
6.0
121-4
5.3
12?-
8i9
12
1-3
6.2
1 21-4
2.6
121-
4.3
12
1-1
2.6
f21
- 7
lO121-2
8.3
42
1-1
1.6
1;2
1-
8.7
12
1-
8*5
12
1-
8.5
121-5
4.3
12
1-5
4.3
121-5
4^4
121-3
5.7
121-5
4.5
12
1-
8.7
1 2
1 -
1 T
. 5
121-3
5.4
121-3
5.0
121
-34', 7
12
1-
8*. 6
121-
37:1
12
1-3
4.9
121-A
4r
81
21
-35
.31
21
-35
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21
-35
.1121-3
5;0
121-3
0*.
11
21
-28
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21
-35
.31
22
-44
;9121-2
7'.0
12
1-5
7.6
12
1-5
7.6
12
1-5
7.4
122-
6'.9
12
1-
4.9
5.?
6.1
V 9.1
4.4
4 .4
6,
80
.66
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6,4
5.6
6.9
6?
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1 2*
. 7
15,5
5.5
5.1
5*5
7.7
5.'4
1 2
t 5
P.1
5.8
5.9
7.1
1 4
.61
2.7
5.8
12,8
5.4
6.8
6.3
5.6
7.8
5.?
6.5
1.2
5to
5.0
6.7
6.3
3,8
6.0
1 .9
P.
61
.30*
. P
2.2
0.4
1.0
O'.R n.6
1 .1
1 .1
n',8
1 .8
0.6
1.5
1*,
1
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01
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4.3
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1 .7
1 .2
0.8
1,6
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0.8
1 .3
1,0
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n.3
0.6
0.5
0,6
0.8
1 .
71
.?
1 .9
0.7
1 .0
1 .2
1 .9
?0 6
1 1 9
10 6
1 1 6 8 8 6 7
1 9
1 1
19
1 5
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74
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1974
JAN
21 ?2 22
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1974
HR MN
CENTRAL CALIFORNIA F4RTHOUA<FS--197 4 (CONTTNUFO)
SFC
LAIN
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OFPTH
MAG
NO GAP
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JAN 26
26 27 27 27 27 27 27 27 27 27 28 28 28 28 28 28 28 28 28 28 28 29 29 29 29 29 29 30 30 30 30 30 30 30 30 30 30 30 31 31 31 31 31 31
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PAICINES
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MT JOHNSON
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MT DAY
BICKMORE CANYON
STOCKDALE MTN
BICKMORE CANYON
TOPO VALLEY
BICKMORE CANYON
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MT CARMEL
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20
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21 21 21 21 21 21 21 21 21 21 22 22
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22 22 22 22 23 23 23
23
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24 24 24 24 24 24 24 24 25
25 25 25
HR 22
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31
CENTRAL CALIFORNIA
F A R THOU AK
E S--1 9 7 4 (CONTINUED)
1974
HR MN
SEC
LAT N
LONG W
DEPTH
MAG
NO GAP
OMIN
PMS
ERH
EPZ
Q QUADRANGLE
FE
8
25
25
25 26
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MO
RC
C
AN
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ON
AR
CH
P
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TH
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BIC
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N
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32
CENTRAL CALIFORNIA EARTHGUAKFS 1974 (CONTINUED)
1974
MA
R
3 3 3 3 3 3 3 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 5 5 5 5 6 6 6 6 6 6 6 6 7 7 7 7 7 7 7 7 7 8 8
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M
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0 2
00
27
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09
19
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46
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20
23
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81
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56
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9 3
69
39
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2
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37
17
511
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27
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30
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2
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QUADRANGLE
SAN RENITO
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MENDENHALL SPRINGS
HOLLISTER
LONOAK
CALAVERAS RESERVOIR
WUNPOST
OAKLAND EAST
PAICINES
BICKMORE CANYON
TOPO VALLEY
CHITTENDEN
WATSONVILLE EAST
BICKMORE CANYON
BICKMORE CANYON
QUIEN SABE VALLEY
PAICINES
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TOPO VALLEY
PAICINES
>,;MT SIZER
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CHITTENDEN
HERNANDEZ RESERVOIR
LICK OBSERVATORY
CHITTENDEN
HFPSEDAM PEAK
BICKMORE CANYON
SAN BENITO
33
CENTRAL CALIFORNIA FARTHQUA*
FS--197 A (CONTINUED)
1974
MR MN
SFC
LAT
NLOMC
WDFPTH
MAG
NO GAP
D *l
I N
RMS
FRH
ERZ
Q QUADRANGLE
MA
R
8 8 8 8 9 9 9 9 9 9
10
10
10
10 10 10 10
10 10
10
10
10 11 11 11 11 11 11 11 11 1 1 11 11 12
12
1 2
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12 12 12 12 12 12
16
1
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81
91
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1 1
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16
20
23 5 9 9
12 13 13 15 17
20 21 23
23 3
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11 11 12 12
15 16 17
2? 4 6 7
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21 21
27
55
56
10 15 25 30
21 36 9
226
26
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36 11 32 524
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28 3
41 29 16 8
47
56
1 5
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20 3 5 5
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50
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15.0
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PAICINES
PAICINES
PAICINES
SAN BENITO
WATSONVIILE EAST
MINDFGO HILL
MINDFGO HILL
TOPO VALLEY
TOPO VALLEY
6ICKMORE CANYON
SAN SIMEON
HAYWARD
8ICKMORE CANYON
STOCKOALE MTN
STOCKOALE MTN
iMT SI2ER
PAICINES
GILROY HOT SPRIN6S
TRgS PINOS
LICK OBSERVATORY
CAYUCOS
SAN JUAN BAUTISTA
TOPO VALLEY
TOPO VALLEY
TOPO VALLEY
- TOPO VALLEY
MT MADONNA
THREE SISTERS
SAN SIMFON
***6ULF OF THE FARALLONES***
CALAVERAS RESERVOIR
BICKMORE CANYON
CORDELIA
7
MT SIZER
HUNTERS POINT
THRFF SISTERS
CALAVERAS RESERVOIR
LA HONDA
LA HONDA
LA HONDA
MT MADONNA
GILROY HOT SPRINGS
SLACK CANYON
SAN BENITO
34
CE
NT
RA
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LIF
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13
13
13
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16
16
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8
QUADRANGLE
BICKMORE CANYON
MT DAY
CHITTENDEN
CALAVERAS RESERVOIR
LICK OBSERVATORY
BICKMORE CANYON
BICKMORE CANYON
FRANKLIN POINT
PAICINES
TOPO VALLEY
LA COSTA VALLEY
LA COSTA VALLEY
LA COSTA VALLEY
LA COSTA VALLEY
LA COSTA VALLEY
LA COSTA VALLEY
'LA
COSTA VALLEY
LA COSTA VALLEY
LA COSTA VALLEY
LA COSTA VALLEY
[
ST HELENA
LA COSTA VALLEY
SAN
LEANDRO
BICKMORE CANYON
LA COSTA VALLEY
SAN BENITO
LA COSTA VALLEY
STOCKDALE MTN
THREE SISTERS
HOLtlSTER
CALAVERAS RESERVOIR
SAN BENITO
SAN PENITO
MONARCH PEAK
PARKFIELD
PARKFIELD
ROCK SPRING PEAK
WINTFRS
BICKMORE CANYON
MT DAY
CALAVERAS RESERVOIR
CALAVERAS RESERVOIR
SAN PENITO
PAICINES
PAICINES
CE
NT
RA
L
CA
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OR
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RT
HG
U0
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19
74
(C
ON
TIN
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1 9 7 A
H R
M N
SEC
LAT N
LONG W
DEPTH
MAG
NO GAP
DMIN
RMS
ERH
FRZ
Q QUAOPANPLE
MA
R
28
28
28
28 28
28 29
29 29
29
29
29
29
29
29
29 29
29
30
30
30
30
30
30
30
31 31 31 31 31 31A
PR
1 1 1 1 1 1 1 1 2 2 2 3 3 3
5 7 1
112 14 19 1 2 3 3 5 6 8
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17
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37 38 53 25
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49
16
21 26 7
15
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19
26 19 51 32 19
10
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812.6
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N
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MT
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NY
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TH
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CA
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OR
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E
AR
TH
QU
AK
ES
--1974
(CO
NT
INU
ED
)
1 974
APR
3 3 3 3 4 4 4 5 5 5 5 5 5 5 5 5 5 6 6 6 6 6 6 6 6 6 6 6 6 6 6 6 7 7 7 7 7 7 7 8 a 8 8 8 8
HR MN
5 4?
10 43
14
111716
7 28
8 21
19 36
1 1
2 47
7 37
10 24
11 57
13 40
18 30
20 53
21 43
23 56
3 8
10 47
10 47
11 22
11 36
1215
15
81511
15 41
16 37
16 51
23
223
39
23 39
23 59
3 37
8 55
10 47
13 30
18 10
19 30
22
70
46
1 26
2 35
6 49
7 12
9 20
SEC
9'.0
11 .7
6.9
51 .1
35.4 5.4
"«:
3S3
59.1
45.6
46.7
19.1
56,9
28.3
21 '
.3
25'.4
8f'6
7.1
50.9
5310
55.7
38.9
51,7
36.8
29.2
44.8
25.8
53^3
54.2
56.5
57.9
38.9
19;?9.4
40.8
2'. 3
4.8
1 .9
3 2: 4
44". 3
31.3
1.1
10.4
54*8
48.7
LAT N
37-21.1
37- 6,6
36-13.3
36-52'.2
36-27.5
36-27.7
36-56.7
36-34.2
35-59*6
37- 1:0
36-32J8
36-57*5
36-13.2
35-59j3
35-5910
35-58',
736-56,6
36-52.7
36-37.2
36-37*3
35-58.7
36-35.7
36-49*9
36-15.2
37-
4.5
35-58.0
36-51.6
35-5
9*.7
37-
8.7
36-51.7
36-51.5
37-
2.3
37-
8.6
36-31.9
36-33.4
36-3
5'.6
37-
5.4
37-
8.7
36-3?
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36-56.9
37-55.1
36-32.6
36-29. 1
38-4?".
336-58.8
LONG W
122-10.0
121-30.6
120-49.4
121-19.1
121- 4.3
121- 4.3
121-35:3
121-1 2
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120-33.1
121-12.5
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1974
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1974
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CENTRAL CALIFORNIA E«RTHQUAKES--1974 (CONTINUED)
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CFNTRAL CALIFORNIA FARTHPUAKES--1974 (CONTINUED)
1974
MA
Y
25 25 25 25
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197 4
(C
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1 9
74
JUN
5 5 5 6 6 6 6 6 6 6 6 6 6 7 7 7 7 7 8 8 8 8 9 9 9 9 9 9
10 10
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10
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1 974
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CENTRAL CALIFORNIA EARTHGUAKFS--1 974 (CONTINUED)
1974
HR MN
SEC
LAT
NLONG W
DEPTH
MAR
NO GAP
DM IN
RMS
ERH
FRZ
Q QUADRANGLE
JUN
1
5 15
15 15 15
15 15 15 16
16
16
16
16
16
16
16 16
16 16
16
16
16 16 16
17
17 17 17 17 17
17 17 17
17 17 17 17
17 17 17 17 17 17 18 18
19
53
21
4
22
242
2
30
22
3
2
23
82
3
27
23
5
30
59
1 0
3 9
3 42
5 12
5 17
5 38
5 39
6 14
8 11
8 29
8 35
9 4
15
54
17
3
722
1 4
1 3
6
1 5
2?
36
? 56
445
446
4 46
4 59
6 4
07
32
10
5
9
11
38
12
13
13
39
1 3
47
14
4
15
11
1 7
442
3
16
4 11
10
34
16
. P
52.0
2
0.7
34
,21
6.1
59
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02
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47
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659,0
16
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13
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25
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8
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55
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47,6
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10
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41
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52
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22
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8.6
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30
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52
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1 .2
22
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11.8
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53
CENTRAL CALIFORNIA FARTHQUAK'E
C;--1974 (CONTINUED)
1 9
74
JUN
18
18 18 18 19 19
19 19
19
19 19 19 19 19
19 19
19
20
20 20
20 20
20
20
20
20
21 21 21 21 21 21 21 21 21 21 22 22
22 22 ?2
22 22 22 22
HR
M
N
18
9
18
51
20
3R
21
37
1 32
9 4
01
21
514
14
15
3115
52
15
5
21
6
81
7
52
17
58
21
5
21
142
2
25
2 4
3 4
94
26
4 44
5 16
6 1
69
41
7
31
22
2
51
47
3 42
6 2
47
23
8 1
913
17
13
57
15
18
18
5
5
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0 19
0 58
3 1
57
17
9 3
29
48
9 5?
10
48
15
17
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C
24.6
16
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10.3
32.9
44'
91.7
34.3
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QUADRANGLE
SAN FELIPE
PANOCHF. PASS
PANOCHE PASS
PANOCHE PASS
WATSONVILLE EAST
BICKMORE CANYON
8ICKPORE CANYON
PAICTNFS
***OFFSHORE -
MORO BAY***
ROCK SPRING PEAK
ROCK SPRING PEAK
ROCK SPRING PEAK
PANOCHE PASS
BICKMORE CANYON
NIT HARLAN
MT HARLAN
'PAICINES
NORTH CHALONE PEAK
PAICINES
PANOCHE PASS
MT HARLAN
PANOCHE PASS
LA COSTA VALLEY
SAN FELIPE
MT HARLAN
SAIf
BfNITO
PAICINCS
MT HARLAN
BICKMORE CANYON
MT HARLAN
MT HARLAN
TOPO VALLEY
BICKMORE CANYON
CUPERTINO
BICKMORE CANYON
LICK OBSERVATORY
LICK OBSERVATORY
LICK OBSERVATORY
PAICINES
GILROY HOT SPRINGS
54
CENTRAL CALIFORNIA F.ARTHQUAKES--197 4 (CONTINHFD)
1 974
JUN
2
3 23
23
23
24 24 24 24
24
24 24 24 25 25 25 25 25
26 26
26
26
26 26
26
26
26
26
26
26
27 27
27
27
27
27
27 27
27 27 27 28
28 28
28
28
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CENTRAL CALIFORNIA E*
R T HO U A<
F «? --1 9 74 (CONTINUED)
1974
JUN
29 29
29
29 30 30 30
30 30
JUL
1 1 1 1 2 2 2 2 2 2 3 3 3 3 3 3 3 3 4 4 4 4 4 4 4 4 4 4 5 5 5 5 5 5 5 5
HR
M
N
0 9
2 24
9 4
214
47
12
13
14
13
14
18
18
45
22
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0
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11
26
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13
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0
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11
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14
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19
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70
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15
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33
20
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40
23
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C
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CENTRAL CALIFORNIA EARTHrUAKES--1974 (CONTINUED)
1974
JUL
6 6 6 6 6 6 6 6 6 6 6 6 6 7 7 8 8 8 9 9 9 9 91
010
10 10
10 10
10 10
10 10
10
11 11 11 11 11 11 11 11 11 11 12
HR
M
N
4 3
4 5
5 21
5 2
21
0
41
10
57
12
33
15
31
18
50
19
48
21
55
22
34
23
318
33
18
5
2
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16
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3
76
911
4
13
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13
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23
522
24
3 5
5
10
3
511
3
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11
14
12
15
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42
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44
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19
38
13
35
19
20
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C
56
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CENTRAL CALIFORNIA FAR T HQU Ate E S--1 9 74 (CONTINUED)
1974
JUL
12 12 12 12 13
13
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14 14 14 14 14 14 14
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58
CENTRAL CALIFORNIA EARTHOUAKFS--1974 (CONTINUED)
1974
HR MN
SEC
LAT
NLONG W
DEPTH
MAG
NO GAP
OMIN
ERH
ERZ
Q QUADRANGLE
JU
L
17
17
17
18
18
18
19
i 1
9 19
19
19
19
19
19
20
20
20
20
20
20
20
20
21 21 21 21 21 21 21 21 21 22
22
22
22
23
23
23
23
23
23
24
24
24
24
1 3
45
14
13
21
31
7
32
7
55
1 1
42
3 1
13
313
34
6 13
8 4
811
3
914
35
21
24
5 7
5 5
36
51
7 4
22
0
22
11
22
16
22
19
7 3
77
52
8 1
8
10
3
311
5
01
2
53
16
2
11
8
22
21
26
2 1
64
87
41
6
42
3 19
3 36
6 2
51
7
210
35
?3
93
48
9 4
010
82
0
48
6.0
30.9
2
3*.
51
3.8
12.3
21 5
47
.211.5
19l6
T.2
23
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48.4
5V 29I3
28'. 6
2l5
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28.8
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45
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17
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2.7
44.7
42.7
15.2
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20.0
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21.4
0,8
17.5
58.9
60
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8.4
2.0
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12
0.1
28.3
19.7
36
-50
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36-3
9,8
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2.9
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2.4
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-28
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3.5
36
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CENTRAL CALIFORNIA
fAPTHQUA<FS--19?4 (CONTINUED)
1 9
74
JUL
24 25
25
25 25
25 26
26
26 26
26
26
26 27
27
27 27 27 28 28
28 28
28
28
28 29
29
29
29 29
29
30 30 30
30
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UG
1 1 1 1 1 1 1 2
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22
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217
27
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11
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10
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18
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61
CENTRAL CALIFORNIA EARTHOUAKES--1974 (CONTINUED)
1 974
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1974
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1974
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70
CENTRAL CALIFORNIA EARTHQUAKES--1974 (CONTINUFD)
1974
HR MN
SFC
L AT N
LONG W
DFPTH
MAG
WO GAP
DMIN
RMS
ERH
FRZ Q
QUADRANGLE
SE
P
27 27 27
27 28 28
28 28
28 28 28 28
28 28 28 28 29
29
29 29 29
29
29
29
29
29
29 29
29 29 30 30 30
30 33 30 30 30
OC
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18
57
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2
920
5
92
3
310
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26
32
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4
9
14
16
15
43
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26
18
19
19
56
23
10
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4 24
8 59
10
56
13
57
20
22
21
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24
21
24
21
252
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20
22
22
22
25
11
10
11
18
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56
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5
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41
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37
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71
CENTRAL CALIFORNIA EARTHOUAKES--197 4 (CONTINUED)
1974
HR
OC
T 1
222
12
42
72
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CENTRAL CALIFORNIA EARTHOUAKES--1974 (CONTINUFD)
1974
OC
T
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10
10
10
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1974
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314 1
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74
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(CO
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1974
HR
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25 25 25 25 25 26 26
26
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CENTRAL CALIFORNIA FARTHOUAKFS--1974 (CONTINUFD)
1 974
OC
T 26
26 26 26 26
26 26
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28 28
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1 9
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CENTRAL CALIFORNIA EARTHOUAKES--1974 (CONTINUED)
1974
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SEC
LAT N
LONG W
DEPTH
MAG
NO GAP
DMIN
RMS
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FRZ
Q QUADRANGLE
DE
C
10
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12
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13 13
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13 14 14 14
14 14 14 14 14 14 15 15 15
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CALAVERAS RESERVOIR
RICKMORE CANYON
SAN FELIPE
SAN JUAN BAUTISTA
SAN FELIPE
MT MADONNA
LOS GATOS
{ TOPO VALLEY
^ BICKMORE CANYON
i SAN BENITO
CHERRY PEAK
CERRO COLORADO
CALAVERAS RESERVOIR
LICK OBSERVATORY
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THE GEYSERS
86
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