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ARCHIVED REPORTS LEC APPLICATION FOR CERTIFICATION
EnvironmentalHealth
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2900 - Site Mitigation Program
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PR0516806
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ARCHIVED REPORTS LEC APPLICATION FOR CERTIFICATION
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Last modified
9/26/2019 8:41:30 AM
Creation date
9/25/2019 4:52:39 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
LEC APPLICATION FOR CERTIFICATION
RECORD_ID
PR0516806
PE
2965
FACILITY_ID
FA0012817
FACILITY_NAME
WHITE SLOUGH WATER POLLUTION CONTRO
STREET_NUMBER
12751
Direction
N
STREET_NAME
THORNTON
STREET_TYPE
RD
City
LODI
Zip
95241
APN
05513016
CURRENT_STATUS
01
SITE_LOCATION
12751 N THORNTON RD
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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LODI ENERGY CENTER PROJECT(LEC);CULTURAL RESOURCES ASSESSMENT <br /> Railroad,on the eastern end of the project area and will connect to existing Pacific Gas and <br /> Electric pipeline,Line 108, on the east side of the rail line. The project site is located <br /> approximately 41/2 miles southwest of Lodi. <br /> The LEC site is located in the San Joaquin Valley in an area with recent sedimentary and <br /> metasedimentary fan deposits and basin deposits (Strand and Koenig 1965) and the site is <br /> relatively flat. Considerable disturbance exists within the STIG plant, the WPCF, and the <br /> LEC site. Excavation and grading occurred during the WPCF's initial construction in the late <br /> 1960's and excavations to a depth of six feet occurred during the construction of the STIG <br /> plant in the 1990's (Joe Bittner, 2008, email June 24, 2008). An underground Pacific Gas and <br /> Electric line runs to the STIG plant, through the LEC project area and two of the laydown <br /> and/or parking areas, through the WPCF, and continues east. Areas surrounding the STIG <br /> plant, the WPCF, and the LEC have been excavated to create reservoirs for the WPCF to the <br /> north and the San Joaquin mosquito abatement ponds to the south. Additionally, extensive <br /> earthmoving activities were observed within the proposed project area and the natural gas <br /> line is proposed along a corridor where a natural gas line is already extant. <br /> Prehistoric Period <br /> The general trend throughout California prehistory has been an increase in population <br /> density over time, coupled with greater sedentism and the use of a greater diversity of food <br /> resources. There is abundant evidence that humans were present in the New World for at <br /> least the past 11,500 years. There is also fragmentary, but growing, evidence that humans <br /> were present long before that date. Linguistic and genetic studies suggest that a date of <br /> 20,000 to 40,000 years ago for the human colonization of the New World may be possible. <br /> The evidence of this earlier occupation is not yet conclusive, but it is beginning to be <br /> accepted by archaeologists. The Meadowcroft Rockshelter in Pennsylvania and Monte <br /> Verde in Chile,for instance, are two early sites that have produced apparently reliable dates <br /> as early as 12,500 years before present. These earliest known remains indicate very small, <br /> mobile populations, apparently dependent on hunting of large game animals as the primary <br /> subsistence strategy. <br /> Several chronologies have been proposed for central California archaeology. Generally, <br /> these chronologies are variations based on the general California chronology,which consists <br /> of an Early Horizon, a Middle Horizon, and a Late Horizon (Fredrickson 1974, Elsasser <br /> 1978). However, wide regional differences in central California, as well as significant <br /> temporal overlap between site types classified into these three horizons, prevented clear <br /> distinctions between horizons. Eventually, a model was proposed for central California that <br /> primarily emphasized the patterns of cultural identity and deemphasized associated <br /> occupation dates (Moratto 1984). <br /> The earliest sites in the San Joaquin Valley are Fluted Point Tradition and Western Pluvial <br /> Lakes Tradition sites found at Tracy, Tulare, and Buena Vista lakes. These sites are few in <br /> number and remain undated by scientific means but the assemblage types indicate probable <br /> ages of 11,500 to 7,500 years old. Deposition in the San Joaquin Valley is quite active; many <br /> older sites are likely buried under rapidly building alluvial deposits (Moratto 1984). <br />
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