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Proposed McGbe Residence Remodel <br />Everett, Washington <br />Projcct No. 6G-9701022 <br />Page 5 <br />�� �l \ � �p.-1\C.,� � � i� � ,� i� .� i� r � <br />During the site reconc►aissence, xveral ceoent "tlow" W�dslides w�a�e obxrved on slopes adjacent <br />to the developed pert of t6e siu. The flows generslly involved movement of shsllow tayers of s�uface <br />soils a� a r�ult of satucation by surface and subsurfece wata. T6e largest of the raxnt sGda appeared <br />to have ban triB6� P���Y bY a�uation of surfice soila, hovreva Poor drainaBe mw4eaKnt aed <br />slope maeagement practioes weie probably coMributory ca�na. 7Le tvro largest alide aars hsd piles of <br />yard wavte or other debcia nar their up-slope limib, which probsbly held �anificant surfsce water and <br />enhanced suface weta in6ltration at the tops of the siidw. Additionelly, the lerger siide to the east of <br />the house had occu�red where a drainage pipe from tLe developed pert of the site was draped over the <br />siope and pafo� to allow disct�arge direcdy oato the alope. <br />Sius such ag this one are espxially prone to flow feilures as a rault of reladvely looae gcanular <br />soils located above more denx, siltier soils, in a sloping environnxnt. The body of stcuctural RU beneath <br />the deck en�a and extax�ing to tLe south on the east side of the Iwuse (B-3) is petticularly suspxt becaus�e <br />of the very low densiry, abundac�ce of perched water within the 611, exposiue of � soil conditions W <br />slopes ranging from approximately 30 W 40 degras, and the surcharge caused by the fill geometry. <br />Several soil, groundwater, and topogrephic condi6ons are present on titis aite thet create the <br />potential for slope movement, and numerous mxnt 8ow failuns were noted. It does not �ppear thet any <br />of the previous slope movert�n►ts have raulted in significaat dart�ege W the site improvements, however <br />some slope debris &om the site may have been depositai on the reilroed grade to the noKh or in the crak <br />bed to the east. In Gtles' opinion, the potential for future �tope movema�b aimiler to those tlut are <br />already known must be considered high. [t would not be feasible, within a reasonable cost �nd effoK, to <br />nmove all risks of future slope movement and all potendal for dart�ege w sioe improvea�enb. 'tikre are, <br />however, numerous measures that can be readily ac:complished that would redua risks aignificandy. <br />Ultimately, only the hommwner can dccide what level of risk is Wlerable, and wttere the belance betw�cee <br />costs and benefits for risk reduction measures lies. This is a particulerly good time to conaida risk <br />reduction measures, as a pact of planning for the remodeling of the residenee which eould inerease the <br />potential risk exposure. <br />The following improvements would reduce the potentiel for slope movemenb, and therefore risk <br />of damage to site irnprovements as a rosult of slope movement. The rawmmmdadons are presented <br />generally in order of decreasing effectiveness, though it sheuld be realiud that the admation of <br />effectiveness of these measures is subjective and based on our experience with similer projxts: <br />• Begin a rcgular program of inspcction, maintenance, end cepair of site drainage systems. <br />Any drainage component that collects surface water could potendally leek, clog, or <br />overflow, resulting in uncontrulled discharge in undesirable locadons. Inspecdon� should <br />be pedormed et least once each fall beforc the winter raii►y season. <br />