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SU0003901_SSNL
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2600 - Land Use Program
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PA-0300602
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SU0003901_SSNL
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Entry Properties
Last modified
11/19/2024 3:59:59 PM
Creation date
9/8/2019 12:34:36 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0003901
PE
2622
FACILITY_NAME
PA-0300602
STREET_NUMBER
28567
Direction
E
STREET_NAME
STATE ROUTE 120
City
ESCALON
ENTERED_DATE
5/11/2004 12:00:00 AM
SITE_LOCATION
28567 E HWY 120
RECEIVED_DATE
11/21/2003 12:00:00 AM
QC Status
Approved
Scanner
SJGOV\sballwahn
Supplemental fields
FilePath
\MIGRATIONS\O\HWY 120\28567\PA-0300602\SU0003901\SS STDY.PDF
Tags
EHD - Public
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Geologic Map <br /> Van de Fol f roperty <br /> 28567 State Poute 120 <br /> Escalon, CA 95320 <br /> . �.C'f <br /> olteg+tt tte cI`h, } ` <br /> � PI <br /> s_.J AC PI PI 1' <br /> ' YAplisetdrn <br /> Weil .c f <br /> ii• A �, i t.? r <br /> kd <br /> 1 <br /> - <br /> `� l c a <br /> Itu - <br /> '" f t.Folin <br /> �. a <br /> Explanation <br /> Holocene Alluvium- poorly sorted stream and basin <br /> deposits;clay to boulder size <br /> Map Base: California Geological Survey <br /> QM Quaternary Modesto Formation - (formerly California Division of Mines&Geology), <br /> Arkosic alluvium forming Mokelumne River terraces and alluvial 1991, Geologic Map of the <br /> fan;chiefly sand with minor gravel and silt:probably glacial outwash San Francisco- San Jose Quadrangle; <br /> CDMG Map 5A,Scale 1 : 250,000. <br /> Qmr Quaternary iZiverbank-Modesto Formations (undifferentiated) <br /> Or Quaternary Riverbank Formation-weathered reddish gravel, Scale <br /> sand,and silt forming clearly recognizable alluvial terraces and fans 0 2 4 <br /> C25 Quaternary Dune Sand Miles <br /> 1 in = 5.95 miles <br /> Qtl Quaternary Turlock Lake Formation-deeply weathered 1:250,000 <br /> arkosic gravels with minor resistant metamorphic rock fragments <br /> and quartz pebbles <br /> FI Pliocene Laguna Formation- interbedded alluvial gravel,sand <br /> and silt. Pebbles and cobbles of quartz and sedimenta are <br /> invariably arkosic. <br /> _ NEIL O. ANDERSON <br /> Tm Tertiary Mehrtern Formation- sandstone,laminated siltstone, A N D A S S O C I A T E S <br /> conglomerate,and tuff breccia composed almost entirely of <br /> andesitic material with only smallamounts of amountof igneous and rrtetamorphic rock fragments late 7 <br /> E:1 Location of 5ubiect Site <br />
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