HomeMy WebLinkAboutGeoTech Assessment Review for BLD2004-00726 - BLD Engineering / Geo-tech Reports - 10/29/2004 1
ST
N,OATFo MASON COUNTY
o AS
t N_ PUBLIC WORKS DIRECTOR/COUNTY ROAD ENGINEER
y ` Shelton,Washington 98584
°° 1864 \° DATE: October 29 h, 2004
INTER-DEPARTMENTAL COMMUNICATIONS
TO: Rick Mraz, DCD -Planner
FROM: Alan A. Tahja, P/W - Co. Hydr. Engr. WO#PLG-04
SUBJ: Geo-Tech Assessment Review NAME: Barber SFR @ Tahna River Road
BLD2004-00726
Rick,
The geotechnical assessment prepared for the proposed Larry Barber Single Family Residence
(SFR)to be constructed at 811 NE Tahuya River Road, Tahuya,has been received and reviewed
by Public Works.
The report appears to satisfactorily fulfill County requirements for geotechnical assessment
reporting. The assessment's author indicates that, in his opinion,the completed development of
the property will not cause stability problems for either the subject property or neighboring
properties, and that a more detailed investigation(report) is not warranted. From the contents of
the assessment, I recommend accepting the report as satisfying the County'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 (Ecology Stormwater Best Management
Practices(BMPs)) 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 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.
S, cerely,
Alan A. Tahja
File: H: \WP\GEO\Assessments\Barber.doc
WORK ORDER - PUBLIC WORKS DEPT.
(A) Date: -� o
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RECEIVED
OCT: 2 6 2004
426 W- CEDAR ST!
Geotechnical Assessment
811 NE Tahuya River Road
Tahuya, WA
Parcel #322127500070
Prepared for
Larry Barber
Tahuya, WA
bkA 200H CEO -7 Z CQ
by
Geotechnical Testing Laboratory
Olympia, Washington
Oct. 18, 2004
GEOTECHNICAL TESTING LABORATORY
LARRY BARBER
811 NE TAHUYA RIvER ROAD
TAHUYA,WA 98588
RE: GEOLOGICAL ASSESSMENT
811 NE TAHUYA RIVER ROAD
TAHUYA, WASHINGTON
PARCEL 322127500070
N47024.892' W 123°00.503'
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. A single-family residence with a
daylight basement is proposed on the cleared parcel. The septic system and a groundwater well exists on
the developed site.
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SITE CONDITIONS
The subject site is a parcel located approximately 3.5 miles northeast of Tahuya, Washington. The lot is
located east of Tahuya River Road, see attached vicinity map. The site is accessed from the Belfair
Tahuya Road and then the Tahuya River Road. The subject site (5.15 acres) is located in an area of
sparse residential development. The site slopes to the east from the proposed building location. The
steepest portion of the site has a slope approaching 31 percent. Minimal grading is expected at the
proposed building location except for the proposed daylight basement. The lot is vegetated with mixed
vegetation but mostly grasses. 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)754-4848
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GEOTECHNICAL TESTING LABORATORY
GEOLOGIC CONDITIONS
The Soil Survey of Mason County, USDA Soil Conservation Service (1960) has mapped the western site
soils as Alderwood gravelly sandy loam, 5-15 percent slopes (Ab). The report reads:
The Alderwood soils typically formed from glacial advance outwash. They are described
as having good natural drainage. Typically, there is no occurrence of a high water table.
Internal drainage is described as medium. An erosion hazard may exist if the vegetation
is removed, otherwise, the soil has a low erosion hazard in its present condition.
Cementation is usually present. The soils are not considered hydric.
The Soil Survey of Mason County, USDA Soil Conservation Service (1960) has mapped the eastern site
soils as an Everett very gravelly sandy loam, 15 to 30 percent slopes (Ek). The Everett soils are described
as:
Very deep, somewhat excessively drained soil on terraces and outwash plains formed in
the glacial outwash stage of the most recent Fraser glaciation. Permeability is rapid(up
to 20 inches per hour) with a high rate of water transmission. These soils are typically
classified as a "Group A"relative to surficial runoff. The soils are further characterized
as having medium runoff potential and moderate water erosion potential. Shrink-swell
potential is described as low due to the low organic content. We observed no active
erosion or slope disturbance in the site area during our reconnaissance.
`i
10011 Blomberg Street SW, Olympia,WA 98512
Phone#: (360)754-4612 Fax#: (360) 754-4848
GEOTECHNICAL TESTING LABORATORY
The Geologic Map of Washington — Northwest Quadrant (2002)
has mapped the site geology as advance outwash deposits (Qga)
of continental glacial origin. The report reads:
Advance outwash — Glaciofluvial sand and gravel and
lacustrine clay, silt, and sand deposited during the
advance of glaciers; sandy units commonly thick, well
sorted, and fine grained, with interlayered coarser sand,
gravel, and cobbles; locally contains nonglacial
sediments and deposits mapped as transitional between
glacial and nonglacial. Includes the Colvos and
Esperance Sand Members of the Vashon Drift and part of
the Vashon Drift undivided.
The Geologic Map of the Shelton 1:100,000 Quadrangle, Washington, by Logan (2003) describes the
western site as Advance outwash, late Wisconsinan (Pleistocene). The Advance outwash (Qga) is
described as:
Glaciof luvial sand and gravel and lacustrine clay, silt, and sand deposited during the
advance of glaciers; sandy units commonly thick, well sorted, and fine grained with
interlayered coarser sand, gravel, and cobbles and silt rip-up lag deposits at their base;
may contain nonglacial sediments;generally overlain by till.
GROUNDWATER CONDITIONS
Groundwater seepage was not observed at or near the proposed building location. No wetland vegetation
was observed at or near the proposed building location. Depth to static groundwater is unknown.
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 location or throughout the site. Adjoining parcels
display similar signs of stability as the subject site.
.y
X
10011 Blomberg Street SW, Olympia,WA 98512 3
Phone#: (360)754-4612 Fax#: (360) 754-4848
IL
GEOTECHNICAL TESTING LABORATORY
DEPTH TO COMPETENT SOIL
Typically, dense gravelly sandy loam is found throughout the site. Competent soil can be expected
approximately zero to 20 inches below the ground surface. Glacial till is exposed at the proposed building
location.
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 slopes are dense, compact, and moderate in slope angle. Onsite and
neighboring 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 IS percent, but may be greater
locally in areas too small to be shown at the map scale. Largely comprises rolling
uplands underlain by very stable material such as young glacial till, mantled in places by
a thin layer of sandy gravel or other permeable material, also includes flood plains,
deltas, alluvial fans, and some beach deposits. Class 1 areas immediately adjacent to
steep slopes of class 3 areas may be threatened by potential landsliding. Normal,proper
engineering practices generally are adequate to insure stability in these areasAw
010
POTENTIAL FOR LANDSLIDE ACTIVITY
This site has very little potential for landslide activity. Even though slopes approach 31 percent, the
potential for landslide activity is not a concern. Surficial creep and sloughing at the proposed building
location is not a concern.
10011 Blomberg Street SW,Olympia,WA 98512 4
Phone#: (360) 754-4612 Fax#: (360) 7544848
GEOTECHNICAL TESTING LABORATORY
RECOM MNDATIONS
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.
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,
of W$8h!' GEOTECHNICAL TESTING LABORATORY
e
G..
a Harold Parks, L.G., L.E.G.
`g � Senior Engineering Geologist
827 0
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HAROLD PARKS
10011 Blomberg Street SW, Olympia,WA 98512 5
Phone#: (360) 754-4612 Fax#: (360)754-4848
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