HomeMy WebLinkAboutGeo-Tech Assessment Review for BLD2005-00562 and 00469 - BLD Engineering / Geo-tech Reports - 5/19/2005 STgTF MASON COUNTY
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° = PUBLIC WORKS DIRECTOR/COUNTY ROAD ENGINEER
S N Shelton,Washington 98594
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DATE: Mgy 19'h 2005
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INTER-DEPARTMENTAL COMMUNICATIONS
TO: Chuck McCoy, DCD -Planner
FROM: Alan A. Tahja, P/W - Co. Hydr. Engr. WO#PLG-05
SUBJ: Geo-Tech Assessment Review NAME: Gordon SFR 6D Jolly Roger Lane
BLD2005-00562 & 00469
Chuck,
The geotechnical assessment prepared for the proposed Gary Gordon Single Family Residence
(SFR)to be constructed at 181 & 191 Jolly Roger Lane, Belfair, (Parcel No. 12330-54-00019 &
12331-51-00066), in the plat of Beard's Cove, Belfair),has been received and reviewed by
Public Works.
The report appears to satisfactorily fulfill County requirements for geotechnical assessment
reporting. From the contents of the assessment, I recommend accepting the report as satisfying
the Count 's requirement(s)for stability investigation and geotechnical reporting.
Recommendations contained in the assessment should be incorporated into the site's
development and made conditions for permit issuance.
Adequate Erosion and Sediment(E&S) control features need to be implemented during land
disturbing activities to protect neighboring properties and State waters from adverse stormwater
runoff impacts. The migration or release of silty water or mud from the applicant's property will
be considered a violation of County and State water quality protection regulations.
In summary,the geotechnical assessment prepared for the proposed Single Family Residence
appears acceptable, and stability issues may be considered to have been adequately investigated
and addressed.
Please feel free to contact me at County extension 461 if you have any questions regarding these
comments, or if you feel any features need further discussion or attention.
Sin erely,
Ian A. Tahja
File: H: \WP\GEO\Assessments\Gordon.doc
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Geotechnical Assessment
181 & 191 JoyRogerJolly Ro Lane
Belfair, WA
Prepared for
Gary Gordon
Olympia, WA
by
Geotechnical Testing Laboratory
Olympia, Washington
May 9, 2005
GEOTECHNICAL TESTING LABORATORY
GARY GORDON
P.O. Box 3282
BELFAIR, WA 98528-3282
RE: GEOLOGICAL ASSESSMENT
181 & 191 JOLLY ROGER LANE
BELFAIR, WA 98548
PARCEL 12330-54-00019 & 12331-51-00066
N47026.848' W122051.354'
PURPOSE
The objective of the geological assessment is to assess the surface and subsurface conditions prevalent at the subject
site according to Mason County Ordinance 17.01.100.E4. The parcel is to be developed with a single-family
modular residence. Currently, an approved septic system has been constructed on site.
SITE CONDITIONS
The subject site is approximately 0.46-acre parcel located north of Lynch Cove on the Hood Canal. The site is
accessed from NE Larson Lake Road. The subject site is located in an area of moderate residential development.
Two mobile homes are on the site. The mobile homes are placed on fill material that is assumed to be native
material, which was graded to a level surface prior to the placing of the mobile homes. The steepest portion of the
site, with slopes approaching 25 percent, is situated downhill and to the east of the mobile home pads. The slopes
are vegetated with native plant species. Rapid stream incision was not identified at the site. Slope instability was
not discerned onsite or on adjoining parcels.
10011 Blomberg Street SW, Olympia,WA 98512 1
Phone#: (360) 754-4612 Fax#: (360) 7544848
GEOTECHNICAL TESTING LABORATORY
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GEOLOGIC CONDITIONS
The Geologic Map of Washington-Northwest Quadrant(2002)has mapped the site geology as glacial till deposits
(Qgt)of continental glacial origin. The report reads:
7-111- Unsorted, unstratified, highly compacted mixture of clay, silt, sand, gravel, and boulders
deposited by glacial ice; may contain interbedded stratified sand, silt, and gravel. Includes part
of the Vashon Drift undivided.
The Soil Survey of Mason County, USDA Soil Conservation Service (1960) has mapped the site soils as Everett
gravelly loamy sand, 15 to 30 percent slopes (Ef). The survey describes the soil .•��--f,.
as follows:
The Everett series consists of somewhat excessively drained, pale- '
brown gravelly soils. They occur as inextensive gravel ridges on the %- 4.
glacial moraines, or, more commonly, as continuous outwash
channels between ridges of Alderwood soils. They have developed " fi
upon assorted glacial till and outwash material. The rainfall is 45 to
60 inches a year. The vegetation is mainly drought-resistant
madrone, manzanita, and kinnikinnick.
Everett soils are droughty because the loose gravel and sand subsoil and substratum offer little
resistance to downward movement of water. The capacity of the
surface soil to hold available moisture is low.
Everett soils are in the eastern half of the country, in association
with Alderwood soils. They also occur in intricate patterns with the
oEti � Kitsap and Indianola soils. Compared to the Grove soils, the
Everett soils have a paler surface soil and subsoil and, in
development, were dominated more by acid igneous parent rock.
10011 Blomberg Street SW, Olympia,WA 98512 2
Phone#: (360) 754-4612 Fax#: (360)7544848
GEOTECHNICAL TESTING LABORATORY
Everett gravelly loamy sand, 15 to 30 percent slopes (Ej). Except for slopes, this soil is similar
to Everett gravelly loamy sand, 5 to 15 percent slopes. Profile characteristics vary greatly from
place to place, especially on the steeper slopes.
GROUNDWATER CONDITIONS
Groundwater seepage was not observed at the building location or near the pads of the trailers. No wetland
vegetation was observed at or near the proposed building location. Depth to static groundwater is unknown, but
neighboring wells list the depth to static groundwater at 29 feet below ground surface.
DEPTH TO COMPETENT SOIL
Typically, dense gravelly loamy sand is found throughout the site. Competent
soil can be expected approximately 12 inches below the ground surface. k
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PAST SLOPE INSTABILITY
Near the proposed building location, trees were found straight and vertical.
No indication of past instability was discerned at the proposed building
1 la similar signs o f
Adjoining parcels display
location r throu out the site.0
J 1n1� P P Y 1�
stability as the subject site.
HISTORY OF LANDSLIDE ACTIVITY
No historical landsliding was observed during our site investigation onsite or
near the subject parcel. At the proposed building location, the low angle slope
is compact and dense. Onsite trees are straight and vertical.
The Relative Slope Stability of the Southern Hood Canal Area, Washington, (1977)describes the site area as Class
1. Class 1 is expressed as:
Areas believed to be stable. Slopes generally less
than 15 percent, but may be greater locally in
areas too small to be shown at the map scale. = ="" 1��—
Largely comprises rolling uplands underlain by
very stable material such as young glacial till,
mantled in places by a thin layer of sandy gravel 1 w •
or other permeable material; also includes flood -
plains, deltas, alluvial fans, and some beach
deposits. Class 1 areas immediately adjacent to
steepslopes o class 3 areas be threatened b
P .f �' y
potential landsliding. Normal, proper engineering
practices generally are adequate to insure stability
s,
in these areas. r,
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10011 Blomberg Street SW, Olympia, WA 98512 3
Phone#: (360)754-4612 Fax#: (360)754-4848
GEOTECHNICAL TESTING LABORATORY
POTENTIAL FOR LANDSLIDE ACTMTY
This site has very little potential for landslide activity. The pads the trailers are placed upon are relatively flat. To
the east of the trailers is a retaining wall constructed of logs. This
retaining wall is not vertical and does not appear to have a drain in the
wall to relieve water pressure. To the east of the trailer pads, the slope
approaches 25 percent. The steeper slopes are highly vegetated.
The Liquefaction Susceptibility Map of Mason County, Washington by
Palmer, Magsino, Poelstra, Bilderback, Folger, and Niggemann
(September 2004) maps the site area as having a very low to low
liquefaction potential.
The Site Class Map of Mason County, Washington by Palmer, Magsino, Bilderback, Poelstra, Folger, and
Niggemann (September 2004) maps the site area as site class C to D. Site class C is a very stiff soil or soft rock
and site class D is a stiff soil.
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RECOMMENDATIONS
There is no evidence of soil erosion or deposition onsite to suggest that the site should be included in the Erosion
Hazard Area designation. Site conditions for the proposed development do not warrant a more comprehensive
Geotechnical Report. We recommend no further action is needed unless areas of concern are unearthed during
construction or damage ensues from vegetation clearing. To minimize erosion and sedimentation, we recommend
that underbrush remain for areas outside the building location.
10011 Blomberg Street SW, Olympia,WA 98512 4
Phone#: (360) 754-4612 Fax#: (360) 754-4848
GEOTECHNICAL TESTING LABORATORY
If there are any changes in the loads, grades, locations, configurations or types of facilities to be constructed, the
conclusions and recommendations presented in this report may not be fully applicable. If such changes are made,
we should be given the opportunity to review our recommendations and provide written modifications or
verifications, as appropriate.
Respectfully,
GEOTECHNICAL TESTING LABORATORY
Wash�n
Harold Parks, L.G., L.E.G.
Senior Engineering Geologist
HAROLD PARKS
X�- -_ 3l_QS',
10011 Blomberg Street SW, Olympia,WA 98512 5
Phone#: (360) 754-4612 Fax#: (360) 7544848
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