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• <br /> Geotechnical Engineering Report lierracon <br /> Merrill Creek Operations Base Expansion x• Everett, Washington <br /> December 14, 2020 r Terracon Project No. 81205012 GeoReport <br /> Item Description <br /> The project site consists of existing rigid pavement at the west end of the <br /> existing operations and maintenance building —this building occupies a <br /> footprint of approximately 57,500 square feet and comprises the largest <br /> building on the greater Community Transit campus (other CT buildings are <br /> Site Information and situated to the east and south). The proposed building expansion will <br /> Existing increase the existing operations and maintenance building by about 16,550 <br /> Improvements feet, add several bays for coach maintenance, painting, equipment and <br /> materials storage, and related coach fleet activities. Renovation and <br /> reprogramming of these activities within the western portion of the existing <br /> building footprint will also occur. <br /> See Site Location <br /> Project site is flat and paved with concrete pavement. This topography is a <br /> result of previous site filling, which occurred in the mid-1980s to early-1990s, <br /> following aggregate mining and processing activities in the 1960s and 1970s. <br /> Fill is presumed to have been derived largely from flattening of the slope <br /> above the site to the west. <br /> Existing Topography <br /> Prior to construction of the existing building in 1996/1997, re-working and re- <br /> and Site History <br /> compaction of upper portions of the fill — plus placement of additional fill <br /> occurred, resulting in the dense to very dense upper layer of fill encountered <br /> (as discussed below). <br /> A greater discussion of site history, previous explorations, and fill placement <br /> is presented later in this section. <br /> • Dense to very dense silty sand fill with gravel to depth of about 12 feet <br /> (below existing grade)was observed at both exploration locations. <br /> • Below 12 feet, additional fill consisting of silty sand was encountered; <br /> soil density is variable below 12 feet and ranges from loose to very <br /> Geology dense. <br /> ✓ Native advance outwash was encountered near the bottom of the deeper <br /> boring, below a depth of 40 feet. <br /> • Groundwater was encountered at a depth of 27 feet below the ground <br /> surface. <br /> Site History <br /> Based on Washington Geologic Information portal, the site geology is mapped as Vashon <br /> Advance Outwash, although this native soil was encountered only at considerable depth <br /> in our deeper exploration. The sand and gravel of this outwash soil unit were historically <br /> mined for concrete and asphalt aggregate and other building materials; mining of <br /> aggregates occurred on-site from at least as early as the early 1960s through the early <br /> 1970s. Between about 1986 and 1990, excavations were filled in by flattening of <br /> surrounding high banks around the pit and by "borrowing" of soil from the slope to the <br /> Responsive • Resourceful z Reliable <br />