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Gco�cchnicnl �nginccring Lcttcr NGA Pilc No. 865712 <br />5732 Sound Avenuc Slopc I:ealuatiun DrcentUcr 19, 2012 <br />I:ccrctt, \Vashington Pagc 3 <br />groundwatcr "lablc" �vi�hin thc upper soil horizons. Pcrchcd wa�cr tends to vary spatially nnd is <br />depcndent upon thc nmount of prccipitation. If perchecl watcr candi�ions cxis�, wc w�ald cxpcct ihc <br />amount of perched wa�er to decrcase during dricr times of the ycar and incrensc during wctter periods. <br />L:mdslidc Ilazard/Slopc Stability <br />'fhc critcria uscd for cvalualion of landslidc liarards includc soil t�Tc, slope gradicnt, and groundwa�cr <br />conJitions. '1'hc si�c is situa�cd on a stccp norlh-facing slopc tvith indinations of approsimatcly U l0 40 <br />degrees (31 �0 34 perccuQ. \Vc did not obsen�c any indications ol' rceent dcep-scatcd movemcnt of the <br />slopc during our during our sitc visii; hu�acvcr, ��•c did obscn•c somc minor slou�_hing and slumping of <br />�lic surficial fill and loosc surf'acc soils near thc tap of thc slopc. <br />I3ascd on our obscrva�ions and thc mappcd gcology of thc arca, thc corc of �hc slopc is infcrccd to consist <br />primarily of mcdium dcnsc or bcttcr nativc soil. Rclalivcly shallo�e sloughiug failures as �vell as surficial <br />crosion are nntunl proccsses mid should be expectcd on thc slope. It is our opiniou that while there is <br />potential for crosion, soil crccp, and sliallow failures ��•ithin thc loose surficial soils and undocumented fill <br />on the slcep slope, there is not a signiticant potcntial for deep-scated slope f.�ilure under current si�e <br />conditions. Proper sitc drainage and maintenance of Ihe slope, as �ecll as proper vegetation management <br />on the slope, should hclp mainlain current s�ability conditions. 1Vc ha��e provided prelitninary <br />rccomntendations for maintaining slopc s�ability in Ihc scction hclo�v. <br />CONCLUSIONS AND RECODI�IENDATIONS <br />It is our opinion �hal front a gwlechitical s�andpoint �hc sleep cast-f:uing slope bclow the residence and <br />,;arage is considcred stable o�ith respect �o decp-seated f.�ilures. It is also our opinion, based on our <br />obscrvations and perfonnancc of thc esisting garagc founda�ion, that Q�c gangc sc�back front ihc stccp <br />slapc is adcquate pro��ided �liat the more recent garage addition is removcd and viy espused soils after <br />addition ,emoval are properly protected. R'c recommend that the garage addition be removed as plannccl <br />and cxposed suils be covemcl �eith crosion control mattinS such as hcavy jute ne�ting and dcep-roo�ing <br />vegctation be establisl�ed. "fhe stom� drain pipe associated �vitli �he gange should also bc extended down <br />to thc toc of thc siccp slopc ncar thc crcck. A rock spall dissipatcr pad consisting oC 2- to 4-inch rock <br />spalls should bc placed bclo��� the owlct of thc pipe to adequatcly dissipate the runoff from thc pipe. Ne <br />�hould bc rctaincd to obscn-c tinal conditiuns and providc addilional rccommendations as ncedcd. <br />NELSON GEOTECHNICAL ASSOC/ATES, /NC. ' :, �� \I <br />;� <br />