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AET #22-00173- Page 3 of 10 <br /> SITE CONDITIONS <br /> Soi1s <br /> The log test borings and location diagram (Figure l) are included in the Appendix. The logs <br /> contain information concerning soil stratification, soil classification, geologic descriptions and <br /> relative moisture; the density or consistency are also noted, based on the Standard Penetration <br /> resistance (N-value, "blows per foot"). <br /> The boring logs only indicate the subsurface conditions at the sampled locations and variations <br /> often occur beyond the borings. <br /> Boring No. 1 was located in the footprint of the proposed garage addition. In this boring, we <br /> found about 5'/2 feet of fill; the fill consisted of a mixture of clayey sand, and sandy silt. Below <br /> the fill we found interbedded strata of naturally-occurring non-organic coarse alluvium and till to <br /> the boring termination depth of 21 feet. The granular soils consisted of silty sand and sand with <br /> silt and were of loose to medium dense consistency, with N-values ranging from 5 to 20. The <br /> cohesive soils consisted of sandy lean clay and clayey sand and were of a stiff to ve�y stiff <br /> consisiency, with N-values ranging from 13 to 20. <br /> Boring No. 2 was located off the northeast corner of the existing foundation. In this boring. we <br /> found approximately 10 feet of fill; the fill consisted of a mixture of sand, silty sand, clayey <br /> sand, and sandy silt. Trace roots were noted in the recovered samples. Below the fill, we found <br /> a layer of organic clay with sand to a depth of about ]2'/2 feet below grade. These organic soils <br /> were very soft to soft in consistency, with N-values ranging from weight of hammer to 4. Below <br /> the fill and organic soils, we found till to the boring termination depth of 31 feet. The cohesive <br /> soils consisted of clayey sand, sandy lean clay, and lean clay with sand and were of a soft to stiff <br /> consistency, with N-values ranging from 4 to ]0. <br />