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3829 SHORE AVE 2018-01-02 MF Import
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3829 SHORE AVE 2018-01-02 MF Import
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Last modified
8/5/2021 2:52:44 PM
Creation date
3/9/2017 7:19:25 PM
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Address Document
Street Name
SHORE AVE
Street Number
3829
Imported From Microfiche
Yes
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water flows in the pipes. Thrust blocks and pipe anchorages <br /> ehould be incorporated 3n the design to resist these £orces. <br /> The drainage outfall east of 33rd Avenue West presently dis- <br /> charges in the vicinity of an 18" culvert under the railroad . <br /> This outfall may best be relocated to the natural drainage which <br /> generally occurs down the slope in the vicinity of the 42" culvert <br /> several hundre� Peet to the east. <br /> Surface and ground water intercept drains in the area appeaz' to <br /> be performing relatively well. Consideration should be given to <br /> upgrading the drainaga interception along the north side of the <br /> low area. This would lead to additional drain ;e along Shore <br /> Avenue from Sound Avenue to 33rd Avenue West. This drainage should <br /> be connected to the outfall located in the central part of this <br /> area. <br /> Ground water seepage from the slope generally occurs above low <br /> permeability strata substantially below the aurface of the upland. ii <br /> It is not considered feasible to intercept these relatively small � <br /> amount of ground water at depth. The piezometers installed in I <br /> the borings drilled for this stuny should be read periodically i <br /> to determine significant changes in the upper perched ground <br /> water level. <br /> S JMNIARY <br /> The observed slope conditions discussed in this report are gener- 1t <br /> ally similar to a number of other slopes within the areas which face <br /> Puget Sound. Geologically, the slope consists of a variety of � <br /> glacially compacted soils. Theae soils are generally very dense <br /> andposses fairly high strength properties resulting in a rela- <br /> tively stable slope . Prior to the railroad sea wall construction, <br /> the area was one of rapid sea cliff retreat due to toe erosion <br /> from wave activity. A slower rate of backwasting of the slope <br /> is now considered the primary condition affecting relative slope <br /> stability of the area. The rate of natural backwasting is ob- <br /> served to be accelerated pr.imarily by debris dumping on the slope. <br /> Suggested mitigating measures are predominately oriented at proper <br /> disposal af debris, presently being dumped on the slope, and im- <br /> provement of the upslope and residential surface water drainage <br /> systems.� <br /> — -12- <br />
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