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Lateral Spreading <br /> In addition to liquefaction induced settlements, there is the possibility that lateral spreading of the soils <br /> could occur as a result of liquefaction. Lateral spreading involves lateral displacement of large, surficial <br /> blocks of non-liquefied soil, as well as the liquefied soil, as the underlying soil layer liquefies and loses <br /> strength. Lateral spreading generally develops in areas where sloping ground is present or near a free face, <br /> such as in this instance adjacent to the river channel. If liquefaction were to occur within the sands at the <br /> site, we anticipate that there would be a moderate potential for lateral spreading to occur, characterized <br /> by movement of the soils towards the Snohomish River. In general, the magnitude of lateral spread will <br /> decrease with increasing distance between the point of interest and the Snohomish River. During a design <br /> earthquake, lateral spread displacements across the site are estimated to be on the order of 5 to 12 feet. <br /> The design recommendations for the structural foundations presented in subsequent sections of this report <br /> do not take into the account the effects of liquefaction and lateral spreading. Measures to mitigate theses <br /> effects include densifying/reinforcing the liquefiable soils or constructing a foundation system that will <br /> resist differential settlement or limit lateral movement of the foundation. Remediation would most likely <br /> consist of densifying the sand deposits with methods such vibro-compaction or installing stone columns. <br /> These mitigation measures are typically very costly and not commonly accomplished for projects of <br /> this type. <br /> We recommend that Cadman Materials, Inc. (Cadman) be made aware of the risks associated with <br /> liquefaction and lateral spreading at this site. We can provide additional recommendations for mitigating <br /> the seismic hazards at the site upon request. <br /> Fault Rupture <br /> The site is located approximately 7 miles northeast of the northern trace of the Southern Whidbey Island <br /> fault zone. Based on our knowledge of regional geology in the vicinity of the site,the substantial thickness <br /> of glacial and postglacial sediments beneath the site, and the distance to the nearest known fault, we <br /> conclude the potential for surface fault rupture is remote. <br /> Preload and Surcharge Fill <br /> We recommend placing a preload and surcharge fill in the area of the planned soil remediation shed <br /> structures and the recycled asphalt building and other settlement-sensitive structures.The purpose of the <br /> preload and surcharge fill is to pre-induce a major portion of the settlement that would otherwise occur <br /> when the planned stockpiles and structure loads are applied. <br /> Preload and Surcharge Height <br /> For planning purposes, we suggest a preloading program with heights matching planned stockpiles of <br /> 25 feet for the recycled asphalt product pile and soil remediation plant and storage shed buildings. <br /> An additional 5-foot-high surcharge is also recommended. Areas surcharged to 30 feet will pre-induce <br /> settlement caused by the planned stockpiles.The preload and surcharge height(30 feet) is the thickness <br /> of the preload and surcharge fill that is placed above the planned finished grade elevation.The crest of the <br /> surcharge should extend laterally at least 5 feet beyond the footprint of the structures in each direction. <br /> The preload and surcharge fill should consist of structural fill quality material such as the existing recycled <br /> asphalt compacted only to the extent necessary to support construction equipment.Side slopes should be <br /> planned no steeper that 1H:1V(horizontal to vertical).The surcharge surface should be crowned slightly to <br /> GEOENGINEERS/ AuguSt3,2018 Page8 <br /> file No.0643-015 00 <br />