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500 LAUREL DR 2016-01-01 MF Import
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500 LAUREL DR 2016-01-01 MF Import
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Last modified
5/8/2017 12:48:45 PM
Creation date
2/19/2017 1:37:04 PM
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Address Document
Street Name
LAUREL DR
Street Number
500
Imported From Microfiche
Yes
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Geotechnical Engineering Study Page 7.6 <br />00-2267 Three Story Addition - 500 Laurel Street, Everett <br />January 31, 2001 <br />Based on the er.ploratory data it is also our professional opinion that the soil <br />beneath this site generally fall into what the UBC describes as a"stiff soil" profile. <br />This is a material where the Standard Penetration Test N-values typically range <br />betwees� 15 and 50 per foot. Thus, according to Table 16-J of the 1997 UBC the <br />�ite is considered to have the foll�wing profile designation: <br />■ 1997 UBC "stiff' soil profile = S� <br />According to Tables 16-Q and 16-R the following seismic design coefficients should <br />also be used: <br />e 1997 UBC Seismic coefficient Ce = 0.33 <br />■ 1997 UBC Seismic coefficient C� = 0.45 <br />�iquefaction <br />Based on the observed soil conditions, given the generally increasing density <br />observed with depth, the small cohesive clay content of the bulk of the in-situ soils, <br />and the lack of an established shallow water level ttiat might be capable of surging <br />and saturating the shallow soi�, these soil do not ap�ear to us to be susceptible to, <br />or at any significant degree of risk of, liquefaction during an earthquake. In our <br />opinion the risk of liquefaction, and liquefaction related settlement, may be <br />considered very low to negligible and does not in our professional opinion pose a <br />threat to the construction process or the completed :�tructure. <br />Slone Stability <br />Generai: As part af our work on this project we also evaluated the g�nsral <br />stability of the sites' wEstern bluff sl�,�e. From the subsurface data acquired from <br />ourexploratory boring and data review, ourvisual axamination ofthe seils exposed <br />across the f2ce of the site slope and on the surrounding properties, and our <br />geological review, it is believed likely that the bulk of the materials beneatn the site <br />�� <br />
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