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I <br />� <br />Proposed Modification to the Residence of Joel 8 Kathy Larsen <br />Everett, Washington <br />4.2 Subsurtace Soil and Groundwater <br />February 12, 2004 <br />ORA Project Number: 04-065-Report 1 <br />The subsurface soil and groundwater conditions at this site are described in the <br />following paragraphs and are presented graphically on the boring logs in the Appendix <br />of this report. The stratification lines indicated on the boring logs represent the <br />approximate boundaries between soil types. Actual boundaries may be gradual and the <br />transitions may not be easily discernible during site excavation. <br />The surface of the site has been reworked somewhat due to the recent demolition and <br />grading activity. Therefore, topsoil was present to d depth of about one-foot in Boring 1 <br />and not present in Boring 2. In general, the soils extending to a depth of about 10 feet <br />are brown to gray, very loose to loose, Silty SAND (SM) or very soft to soft SILT (ML). <br />The Standard Penetration Resistance ("N-Value") of these soils ranges from 2 to 6 <br />blows per foot (averaging 4 blows per foot) at natural moisture contents ranging from <br />16.5 to 55.3 percent. Underlying these weak, compressible soils; gray-brown to gray, <br />stiff to hard, SILT (ML) to Clayey SILT (MH) was, in general, encountered to the <br />termi�ation depth of the borings — 25.5 feet. A three-foot thick layer of brown, medium- <br />derse Silty SAND (SM) was encountered at a depth of 15 feet in Boring 2. The "N- <br />�alue" of these soils ranges from 11 to 85 blows per foot at natural moisture contents <br />ranging from 10.6 to 32.4 percent. <br />Groundwater was encountered in both borings at completion. Boring 1 was left open for <br />90 minutes before backfilling for the purpose of obtaining a more accurate groundwater <br />elevation. Groundwater readings in granular soils, such as those encountered at this <br />site, are generally accurate even after short periods of observation. Whereas, the <br />groundwater level in fine-grained (silt and clay) soils, may require several days of <br />observation before it becomes stable and accurate. <br />5. DISCUSSION <br />IThe recommendations presented in this report are based on our understanding of the <br />project as presented in the Project Description Section and on the assumption that the <br />� subsurface conditions encountered in the borings adequately represent conditions near <br />and between the exploratory borings. Because project conditions regarding type and <br />Otto Rosenau 8 Associat�s, Inc. Page 4 of 13 <br />