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5828 GLENWOOD AVE CINGULAR WIRELESS ANTENNA Geotech Report 2022-10-25 (2)
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5828 GLENWOOD AVE CINGULAR WIRELESS ANTENNA Geotech Report 2022-10-25 (2)
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Last modified
10/25/2022 11:34:11 AM
Creation date
11/17/2021 3:02:51 PM
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Address Document
Street Name
GLENWOOD AVE
Street Number
5828
Tenant Name
CINGULAR WIRELESS ANTENNA
Address Document Type
Geotech Report
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Adapt Engineering <br /> Surface Conditions <br /> Our surface exploration consisted of a visual site reconnaissance. The existing wood telecommunication <br /> tower, proposed to be replaced by a new steel tower, currently resides in the southeast corner of the host <br /> parcel. In the vicinity of the proposed tower location,the surface of the gently north-sloped host parcel is <br /> primarily overlain by grass and landscaping shrubbery. The existing AT&T equipment facility and <br /> adjacent Verizon facility currently reside approximately 90 feet northwest of the tower location. A <br /> Snohomish County Public Utility Department(PUD)substation facility resides on the northern half of the <br /> host parcel,approximately 100 feet north of the proposed tower location. <br /> It should be noted that many public and private underground utilities were identified by public and private <br /> utility locating contractors. On-site utilities identified in the vicinity of the proposed tower location <br /> included gas, water, power and telecommunication lines. However, non-metallic utility lines may not <br /> have been identified. It is encouraged that the exact location of any underground utilities in the vicinity of <br /> the future construction footprint are located prior to commencing any subsurface excavation work, to <br /> avoid potential underground utility conflict or damage. <br /> Subsurface Conditions <br /> At the exploration location designated B-1, the near surface soil conditions consist of roughly 12 inches <br /> of sandy topsoil with silt and gravel mantling very loose, poorly graded sand with wood debris <br /> (interpreted to be possible fill). At approximately 5 feet bgs, the test boring encountered a loose, relic <br /> topsoil layer that was approximately 8 inches thick mantling native, medium stiff, sandy silt. The sandy <br /> silt graded into medium dense, poorly graded sand with silt and gravel. At an approximate depth of 15 <br /> feet bgs, the test boring encountered dense to very dense,poorly graded sand. Hard silt was encountered <br /> at approximately 30 feet bgs,which then extended to the full exploration depth of 41.5 feet bgs. <br /> It should be noted that heaving conditions were encountered at an approximate depth of 25 feet bgs, <br /> which may have influenced blow counts and the retrieved sample. <br /> Perched groundwater was encountered at approximately 8 feet bgs which appeared to extend to an <br /> approximate depth of 30 feet bgs. It should be noted that throughout the year, groundwater levels will <br /> likely fluctuate in response to changing precipitation patterns,off site construction activities, and changes <br /> in site utilization. <br /> Seismic Conditions <br /> Based on our analysis of subsurface exploration logs and a review of published geologic maps, we <br /> interpret the on-site soil conditions to correspond to Site Class D, as defined by Table 20.3-1 within <br /> Chapter 20 of ASCE 7 in accordance with the 2012 International Building Code (IBC). The soil profile <br /> type for this site classification is characterized by stiff soils with an average blowcount between 15 and 50 <br /> within the upper 100 feet bgs. Current (2003) National Seismic Hazard Maps prepared by the U.S. <br /> Geological Survey indicate that peak bedrock site acceleration coefficients of about 0.294 and 0.545 are <br /> appropriate for an earthquake having a 10 percent and 2 percent probability of exceedance in 50 years <br /> (corresponding to return intervals of 475 and 2,475 years, respectively). The IBC mapped spectral <br /> AT&T Mobility cio General Dynamics October 10,2016 <br /> Adapt Project No.WA16-20654-GEO <br /> LDt 2.0 <br />
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