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2nd Open Record Period: Public Testimony (3-22-18 to 3-30-18)
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2nd Open Record Period: Public Testimony (3-22-18 to 3-30-18)
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Last modified
4/2/2018 2:41:50 PM
Creation date
4/2/2018 2:40:58 PM
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Template:
PDD_Planning_Development
File Type
PDT
File Year
17
File Sequence Number
1
Application Name
CAPITAL HILL PUD
Document Type
Public Comments
Document_Date
3/30/2018
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Yes
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Ms. Virginia Gustafson-Lucker <br />March 28, 2018 <br />Page 3 <br />If the ridge were indeed underlain by massive igneous rock, as stated in the Branch Engineering <br />Addendum of May 30, 2017, slope movements in this area would be unlikely. However, regardless <br />of the published geologic maps, the vast majority of the site is clearly underlain by sandstone, which <br />according to the maps is dipping to the NE at 11 E. Mydiagrammatic cross section conservatively <br />shows a dip of 10 degrees for the sandstone, which is very close to the mapped dip. Therefore, the <br />dip-slope-failure mechanism proposed in my previous submission is quite clearlya perfectly viable <br />explanation for the observed slope instability on the east side of the ridge. <br />The limited reliability <br />of published geologic literature is the reason that EC 9.6710 requires subsurface exploration <br />. <br />to determine actual site conditions <br />Biased Assessment <br />The bias in the distribution of the test pits, which are located only in the gently sloping area not <br />exhibiting evidence of slope movement is obvious even to the untrained eye. No further rebuttal <br />is necessary. <br />th <br />However, Mr. Derricks statements regarding the landslide at E. 30 Avenue are incorrect. The slide <br />I was referring to is located 0.36 miles from the S boundary of the proposed PUD and occurred in <br />1995. The report by Squier and Associates was written in 1996, as evidenced by the map of their <br />th <br />test pits, which is attached. Mr. Derrick may be confusing this slide with another one along E 30 <br />Avenue located about 0.6 miles to the SE, which occurred during the 1980s when the access road <br />to LCC was constructed. The reason for mentioning the 1996 slide at the W-bound exit ramp for <br />Spring Boulevard was the fact that this slide is located along the same E-facing and E-dipping slope <br />and likely resulted from placement of fill for the ramp embankment on a pre-existing failure deposit. <br />This is very similar to the setup which is likely to occur along the east edge of the development <br />portion of the proposed PUD, where fills will likelybe placed at the top of the slope to support <br />houses and driveways. <br />Placement of Level Spreaders <br />This is the most interesting part of Mr. Derricks rebuttal. At face value, Mr. Derricks statements <br />show that he is in complete agreement with mytestimonyregarding the placement of one of the <br />PUDs main storm drainage systems: <br /> <br />Little can I say on this topic, it is not the best idea in my opinion. Three claims I would like <br />(emphasis added) .... <br />to be able to make are: <br />Clearly, Mr. Derrick recognizes that he cannot make these statements, given the design of the PUD <br />which does not consider the geologic constraints of the site. And finally, Mr. Derrick states: <br />I am not sure where that more suitable point of disposal is but it would be nice to find one. <br /> <br />
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