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".-000 NZ A �- <br />Main Office <br />17311 — 135' Avenue NE, A-50o <br />Woodinville, WA 98072 <br />(425) 486-1669 FAX (425) 481-2510 <br />(425) 337.1669 Snohomish County <br />DATE: October 28, 2009 <br />NELSON GEOTECHNICAL <br />ASSOCIATES, INC. <br />GEOTECHNICAL ENGINEERS & GEOLOGISTS <br />Enginoodng-Geology Branch <br />437 East Penny Road <br />Wenatchee, WA 98801 <br />(500) 665-7696 FAX (509) 665-7692 <br />MEMORANDUM <br />TO: I lolly and Rick Anderson <br />CC: John Dippold — Carney Badley Spellman <br />Eileen Mattes — Perko Insurance Company <br />FROM: Khala.i M. Shawish, PE <br />RE: Anderson Slide <br />Shoring Plan Coniments <br />Everett, Washington <br />NGA File No, 816909 <br />i6%�sjvy <br />This memorandum presents our responses to the concerns raised by Frank Pita, PE of Jacobs Associates, <br />Inc. In his letter dateA October 18, 2009 to Chris &'Todd Chase regarding geotechnical and structural <br />plans for stabilizing a slide that occurred on the Anderson property located at 4704 harbor Lane in <br />Everett, WA. The letter references the wall design prepared by CG Engineering, however; the letter <br />does not specifically reference our gcotechnical engineering report which was the basis for the shoring <br />wall design. Mr. Pita did not specifically state that he reviewed the geotcchrtical report. <br />Most of Mr. Pita's comments mist minor issues related to code referencing and typographical errors that <br />do not represent a fundamental disagreement with the provided design. The main exceptions would be <br />the statement made by Mr. Pita that the wall will only stabilize the upper few feet of the slope, and leave <br />the remainder of the slope prone to future slides. Ile also had concerts with, site drainage. <br />In regard to the ability of the wall to stabilize the slope, extensive stability analyses were perfonned and <br />included in the gcotechnical report. Our analyses clearly showed that the wall will indeed stabilize the <br />slope and prevent future slides (if our recommendations arc followed). This slope has a history of <br />landsliding activity. We found that the source of the sliding activity on the slope was the saturation of <br />TV Cry 146s �1,/,ed �s <br />m6,mo a ad i*e ire aw vs <br />F/I7W i/O SUhSf+cnJr(/2 I--eGSah !ar <br />glfo�i, 41C. <br />-fog- it✓aarocc:•. .YB //-4-D� <br />