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September 10,2017 <br /> Infiltration Tests <br /> L&A Job No. 17-095 <br /> Page 3 <br /> The deposits of the Vashon till soil unit were plowed directly under glacial ice during the <br /> most recent glacial period as the glacier advanced over an eroded, irregular surface of <br /> older formations and sediments. This soil unit is composed of a mixture of unsorted clay, <br /> silt, sand, gravel, and scattered cobbles and boulders. The Vashon till soil over the top <br /> two to four feet is normally weathered to a medium-dense state, and is moderately <br /> permeable and. compressible. The underlying fresh till soil, commonly referred to as <br /> "hard pan", is very-dense and weakly-cemented. The fresh till soil possesses a <br /> compressive strength comparable to that of low-grade concrete and can remain stable on <br /> steep natural slopes or man-make cuts for a long period. The fresh till deposits can <br /> provide excellent foundation support with little or no settlement, but are of extremely low <br /> permeability and would hardly allow stormwater to seep through. <br /> Soil Condition <br /> Subsurface conditions of the proposed access road were explored with three backhoe test <br /> pits excavated on August 23, 2017. The approximate locations of the test pits are shown <br /> on Plate 2 - Site and Exploration Location Plan. The test pits were located with either a <br /> tape measure or by visual reference to existing topographic features in the field and on the <br /> topographic survey map, and their locations should be considered as only accurate to the <br /> measuring method used. <br /> A geotechnical engineer from our office was present during subsurface exploration to <br /> monitor test pit excavation, examine soil and geologic conditions encountered, and <br /> complete logs of the test pits. Soil samples obtained from each soil layer in the test pits <br /> were visually classified in general accordance with United Soil Classification System, a <br /> LIU & ASSOCIATES, INC. <br />