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Voth Brothers Construction, Inc. E-1201-1 <br /> , _ October 20, 1980 Page 4 <br /> Subsurface <br /> !» Ouc test borings indicate the site is immediately underlain <br /> by a surficial layer of loose to medium dense silty sand and <br /> ,� sandy silt with some gravel and organics. This surficial layer <br /> is about 2.5 to 4 feet thick. Beneath this surficial soil layer <br /> the borings encountered a very dense gray glacial till to the <br /> full depth of our exploration. <br /> Glacial till is a heterogeneous mixture of gravel, sand, <br /> silt and some clay, deposited 12,000 to 14,000 years ago during <br /> � the advance of the Vashon Glacier over the Puget Sound Basin. <br /> The ice was a lobe of a larger continental ice sheet which cov- <br /> ered the majority of Western Canada. During the greatest �axtent <br /> „ of the Vashon Stade, a glacier covered most of the Strait of <br /> Juan de Fuca and the entire Puget lowland. The maximum ice <br /> � � thickness has been estimated at 3,000 to 4,000 feet. This con- <br /> siderable weight of the ice consolidated all the underlying sedi- <br /> " ments. <br /> � . <br /> Near surface groundwater was encountered as perched water <br /> , above the impervious glacial till in the test pits from our pre- <br /> � , vious study. During drilling of the borings for this study, <br /> water was encountered at a depth of about 17 to 18 feet. On Sep- <br /> tember 21� 2980 groundwater was measured at a depth of about <br /> � 17.5 feet and 15.4 feet in Borings B-2 and B-4, respectively. <br /> , <br /> DISCUSSION AND RECOMMENDATIONS <br /> I • <br /> ,., General <br /> � . As described earlier in th� previous section, the site is <br /> basically underlain by glacial till at relatively shallow <br /> " depths. These dense overconsolidated stratam should provide ade- <br /> quate bearing for the proposed structures supported on conven- <br /> tional footings bearing on undisturbed dense glacial till at the <br /> •- basement level. The single-story section of the proposed facil- <br /> ity may be supported on the undisturbed medium dense silty sand <br /> to sandy silt below the topsoil layer. The surficial loose <br /> _ soils are not suitable for support of building loads. Building <br /> loads must, therefore, be extended beneath these materials. <br /> The following sections of this report present more detailed <br /> - recommendations for various geotechnical engineering aspects of <br /> the project which should be incorporated into the project design <br /> and construction. This report has been prepared for specific <br /> - application to this project in accordance with generally accept- <br /> ed geotechnical engineering practices for the exclusive use of <br /> Voth 8rothers Construction, Inc. and their representatives. No <br /> _ other warranty, expressed or implied, is made. <br /> Earth Consultants, Inc <br /> � _. <br />