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8.A. - Page 371 <br />8.A. - Page 129 <br />a Hummocky topography In numerous areas; <br />Areas of seeps p not mapped in geologic reports, <br />r A tilted telephone pole not noted In geologic report; <br />: Arcuate cracks In laurel Way, not noted In reports, with evidence for <br />seepage; and <br />* An actively Incising stream, which reduces resisting Forces that would <br />buttress the hillslope. <br />In my opinion, these features together indicate a deep -mated landslide complex roughly <br />coincident with serpentinite bedrock south of Laurel way in the eastern area of the <br />development, extending across Laurel Way to the north. <br />Gera '% <br />rearprel�f to be <br />I��V . r R :a •! <br />i. <br />s. <br />r <br />le <br />ris .r• <br />'t `� ' <br />M.n :: <br />fF� f <br />�"i':�a 11 <br />� <br />4 <br />� �'•` <br />•� �.%f •i � <br />44jj <br />T +r�,�•� <br />..4 <br />'P <br />1 , <br />fir <br />t!',r�,r��r •�1 <br />JAMM& cracks A r <br />rocs <br />The mitigation measures proposed In the DEIR are inadequate for preventing structural <br />damage to property from deep-seated slope movement. The DEIR needs to be revised <br />