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ARCHIVED REPORTS_1989
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ARCHIVED REPORTS_1989
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Last modified
7/17/2020 3:52:44 PM
Creation date
7/3/2020 11:00:53 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1989
RECORD_ID
PR0440058
PE
4433
FACILITY_ID
FA0004518
FACILITY_NAME
NORTH COUNTY LANDFILL
STREET_NUMBER
17720
Direction
E
STREET_NAME
HARNEY
STREET_TYPE
LN
City
LODI
Zip
95240
APN
06512004
CURRENT_STATUS
01
SITE_LOCATION
17720 E HARNEY LN
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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SJGOV\rtan
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FilePath
\MIGRATIONS\SW\SW_4433_PR0440058_17720 E HARNEY_1989.tif
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EHD - Public
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Appendix C <br />SEISMICITY STUDY <br />The maximum probable earthquake (MPE) evaluation for the San Joaquin <br />County Landfill Development site was conducted to develop estimates of <br />design ground accelerations that may occur at the site due to earth- <br />quakes occurring on potential seismic sources (i.e., faults) within <br />100 kilometers (km) of the site. Because the San Joaquin County <br />Landfill Development site is a proposed Class III landfill, the study <br />included a determination of peak ground accelerations expected in <br />association with MPEs, as required by Subchapter 15 regulations. The <br />MPE is defined in Subchapter 15 as the maximum earthquake that is <br />likely to occur during a 100 -year interval. <br />Identifying faults capable of generating earthquakes that may affect <br />the site in a 100 -year period was the initial step in developing MPE <br />estimates. To accomplish this, faults which are considered to have <br />been active in Late Quaternary time (i.e., the last 300,000 to <br />500,000 years) and are within 100 km of the site were evaluated based <br />on a review of publications pertaining to the geology and tectonics of <br />the region (Jennings, 1975; Woodward -Clyde Consultants, 1977 and 1986; <br />and Clark, et al., 1984). The geographic relationships between the <br />site and significant Late Quaternary faults are depicted on the <br />Regional Fault Map (see Plate C-1). Relevant characteristics, and the <br />spatial relationship between faults nearest the site are summarized in <br />Table C-1. <br />Pertinent seismic sources include faults of both the Sierra Nevada and <br />Northern Coast Ranges geomorphic provinces (see Plate C-1). The <br />nearest known faults are the Bear Mountains fault zone and the Melones <br />fault zone, located 28 and 38 km east of the site, respectively. Both <br />of these faults are considered part of the Sierran Foothills fault <br />system. All other significant faults are located at least 57 km from <br />U <br />
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