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10008 25TH AVE SE 2016-01-01 MF Import
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10008 25TH AVE SE 2016-01-01 MF Import
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Last modified
4/1/2017 11:59:08 AM
Creation date
4/1/2017 11:58:52 AM
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Address Document
Street Name
25TH AVE SE
Street Number
10008
Imported From Microfiche
Yes
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_ . . � <br /> � <br />�'� �: �� � � <br /> -� <br /> � 2.Q EXISTING SITE CONDITIONS <br /> � <br /> I <br /> The following sections summarize existing surface and subsurface conditions observed during <br /> �, our May l5, 2002 site visit,and subsudace conditions observed during the 1989 explorations. ,' <br /> I <br /> l 2.1 SURFACE CONDITIONS . ! <br /> � The subject property is generally level with a slight slope from the northwest to the southeast. <br /> � The propeRy is approximately rectangular and extends 105 ft along IOOth Street SE to the north,and 125 <br /> R along 25th Avenue SE to the east. Site vegetation includes coniferous and deciduous trees, with dense <br /> landscape vegetation around the perimeter. The center of the site is occupied by the existing building and il <br /> asphalt-paved parking areas. The property has a 6-ft high chaiu-link fence around the perimeter. Access � <br /> i to the property is by a driveway off of 25th Avenue SE. The area of the proposed additions aze generally I <br /> within asphalt-paved areas. <br /> � 2.2 SUBSURFACE CONDITIONS <br /> , The test pits completed in 1989 indicated a soil profile of fill overlying unconso(idated post- <br /> lacia(de sds overl ❑ lacial ti1L Soil conditions at the site are enerall consistent with the ma d � <br /> B P� � , Y� S S 8 Y PPe I <br /> geology (Minnard 19851. Fill soils were typically 1 to 2 ft thick, and described as loose, brown to red- <br /> brown, sandy, gravelly silt. Underlying the fill was an unconsolidated post-glacial deposit described zs <br /> i brown to reddish brown, loose, sandy,gravelly silt. The unconsolidated post-glacial deposit was l to 3 ft <br /> � thick and was reportedly observed in test pits TP-I and TP-3. The lowest soil unit observed in the test <br /> pits was glacial till. The till unit was described as light gray, dense to very dense, sandy silt, silty sand, <br /> and sandy gravel, and extended to the bottom of the excavations. Grounflwater seepage was not � <br /> � <br /> encountered during excavation of the 1989 test pits. Copies of the summary logs of the test pits from the <br /> � previous explorations are provided in Appendix A. <br /> On May 15, 2002 a represenlative of Landau Associates eacavated two borings(HA-I and HA-2) <br /> ; slightly outside of the footprint of the proposed building additions. The borings were completed to depths <br /> of 3'/z and 1'/. ft below the existing site grad�s using a hand-auger. Representative soil samples from the <br /> ; explorations were taken to Landau Associates soil labo�atory for further classification and moisture <br /> content detertnination. The approximate locations of borings HA-I and HA-2 are shown on Figure 2. <br /> Soil encountered in the borings was classified in accordance with the classification system presented on <br /> Figure 3. Summary logs of the conditions encountered are presented on Figure 4. <br /> ; 5/78/021WROJECTtO1W050101EASTMONT flPT.pp� Z-� LANpAUASSOCIATES � <br />
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