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1 <br /> , � , / "ti.� ) t Al 1 "r •s''^r , �'-. -'�K,� <br /> L <br /> ( {IIS <br /> 1 r <br /> j <br /> SRO Y <br /> Irr <br /> I 'E <br /> Yl� <br /> IN .-k <br /> r ' f <br /> rye <br /> t <br /> le-1 <br /> _71\ <br /> `--�` .�} .�`f rf"�`,r / 1, .<'``'•�"`- - Pj " �._. � if � <br /> Floodplain deposits (Holocene)--Nleditunt to dark gray. dense. sandy to <br /> Qh f P silty- clay. Lenses of coarser inateriai (silt. sand, and pebbles) may be <br /> locally present. Flood plain deposits tistially occtu between levee <br /> deposits ( Qh 1) and basun deposits ( Qh b) <br /> Source: Geology of the Onshore part of San Mateo County,California:derived from the <br /> digital database open-file 98-137. E.E..Brabb, R.W.Graymer, and D.L.Jones(1998) <br /> GEOFORENSICS, INC. <br /> 303 Vintage Park Dr.,Suite 2211,Faster City,CA 94404 Figure 3-Geologic Map <br /> Tel:(6.50)349-3369 Fax:(650)571-1878 <br />