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1329 MADRONA AVE Geotech Report 2022-10-25
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1329 MADRONA AVE Geotech Report 2022-10-25
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10/25/2022 2:03:11 PM
Creation date
4/1/2022 4:04:40 PM
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Address Document
Street Name
MADRONA AVE
Street Number
1329
Address Document Type
Geotech Report
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Subsurface Exploration,Geologic Hazard,and <br /> Janowicz Property Geotechnical Engineering Report <br /> Everett,Washington Geologic Hazards and Mitigations <br /> II. GEOLOGIC HAZARDS AND MITIGATIONS <br /> • <br /> The following discussion of potential geologic hazards is based on the geologic, slope, and <br /> shallow groundwater conditions,as observed and discussed herein. <br /> 5.0 LANDSLIDE HAZARDS AND MITIGATION <br /> The City of Everett identifies landslide hazard areas based on certain geologic, topographic, <br /> hydrologic, and historic conditions. The sloping terrain and landslide deposits (Qls) found on <br /> the subject project meet the criteria for a very high/severe landslide hazard area as defined in <br /> Everett Municipal Code (EMC) 19.37.080.1. The definition is stated as "Very high/severe: <br /> slopes greater than fifteen percent in the Qtb, Qw, and Qls geologic units; and slopes greater <br /> than fifteen percent with uncontrolled fill." <br /> It should be noted that the steep slope to the northwest of the site is located on adjacent <br /> private property (the railroad right-of-way) and therefore our ability to comment on the slope <br /> hazard here is limited to review of existing geologic mapping,our visual observations from the <br /> project site, and our nearby borings. However, it is likely that the steep slope was created • <br /> during the development of the railway corridor. The condition of the slope along the northwest <br /> side of the property is typical of slopes in the Puget Sound. There is evidence of small-scale <br /> erosion and surface slope movement in the area. Due to weathering and/or groundwater <br /> seepage, the lower slopes are inherently unstable and commonly exhibit surface failures. <br /> Comparing the existing lower slope with the surrounding property may indicate that the top of <br /> the slope could migrate back to an inclination similar to the slopes on the adjacent properties <br /> to the north and south. <br /> In order to mitigate landslide hazards and improve slope stability to allow construction on the <br /> subject lot within the landslide hazard area,we offer the following recommendations: <br /> • Deep foundations should be used to carry building loads through landslide deposits to <br /> competent bearing stratum below as determined by a geotechnical engineer. <br /> • All site development should be set back a minimum distance from the top of steep slope <br /> not less than twice the height of the steep slope, about 50 feet. This setback area <br /> should not be loaded with such loads as material stockpiles and heavy equipment. <br /> • All excavations deeper than 4 feet made in colluvium or landslide deposits should be <br /> shored during construction. Permanent cuts should be retained by retaining walls or <br /> basement walls founded on suitable bearing stratum and designed to withstand lateral <br /> pressures imposed by colluvium and landslide deposits. <br /> May10,2018 ASSOCIATED EARTH SCIENCES,INC. <br /> NS/1d-170649E002-2-ProJects120170649lKE1WP Page 6 <br />
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