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2610 VIEWCREST AVE 2022-04-13
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2610 VIEWCREST AVE 2022-04-13
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4/13/2022 10:13:52 AM
Creation date
4/6/2022 9:08:08 AM
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Address Document
Street Name
VIEWCREST AVE
Street Number
2610
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McCann Property Geotechnical Services Report <br /> 2610 Viewcrest Avenue,Everett, Washington <br /> Subsurface Exploration <br /> In order to confirm subsurface conditions on the property a series of 4 exploration pits were <br /> excavated on the property on March 23,2019. Logs of the exploration pits are attached with this <br /> letter. The location of the pits is shown on the attached site plan. All of the explorations <br /> encountered sand with silt to silty sand. Most of the sand was fine to medium grained but medium <br /> to coarse sand was observed in EP-1 and EP-2. The soils ranged from loose to medium dense to <br /> dense. Much of the loose soil may be related to past clearing and minor grading of the property. <br /> Mappings <br /> According to the Preliminary Surficial Geologic Map of the Mukilteo and Everett Quadrangles, <br /> Snohomish County, Washington, by Mackey Smith, 1976, Washington Department of Natural <br /> Resources,Division of Geology and Earth Resources,the site is mapped near the contact between <br /> as Vashon age advance outwash deposits, (Espersance Sand(Qe)and Vashon age glacial till(Qt). <br /> Our explorations are in agreement with the published geology map of the area as we did not <br /> encounter any glacial till but the underlying dense, sand and silty sand would be identified as <br /> Esperance sand. <br /> Seismic Hazards <br /> Generally,there are four types of potential geologic hazards associated with large seismic events: <br /> 1) surficial ground rupture; 2) seismically induced landslides; 3) liquefaction; and 4) ground <br /> motion. <br /> The site is located approximately 2 miles north of the northern splay of the South Whidbey Island <br /> Fault Zone. No surficial faulting has been noted anywhere near this area and the potential for <br /> surficial ground rupture during the lifespan of the residences is considered to be low. <br /> The building area slopes are gentle (8 percent slope gradient), are underlain by glacially <br /> consolidated sediments and do not present a risk of seismically induced slope movement. <br /> The underlying dense Esperance sand sediments especially in the absence of a ground water table, <br /> are not subject to liquefaction. <br /> Based on the encountered site conditions,seismic design criteria should follow 2015 International <br /> Building Code recommendations for Site Class D soils. <br /> CONCLUSIONS AND RECOMMENDATIONS <br /> Based on the results of our site reconnaissance, subsurface investigation and literature review it is <br /> our opinion that the subject site is suitable for the planned new construction. <br /> Gary A.Flowers,PLLC. <br /> 5205 23'd Avenue W Everett,Washington 98203 206-819-4304 <br /> 2 <br />
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