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NORTHWESTERN TERRITORIES, INC.
A JLS GROUP COMPANY
717 SOUTH PEABODY STREET, PORT ANGELES, WA 98382
Engineers Land Surveyors Geologists
/VTR (360) 452-849D1n FAX 452-8498 ewww nti4u. matE-Mas n~otQ ~i4u com
JLS GROUP,
INC.
Geotechnical Report
Tax # 921191019
May 8,-2006
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SeaHome Services, Inc.
Attn: Greg Barron
7425 Thorndyke Rd.
Quilcene, WA 98376
Subject: Geotechnical Report for Tax # 921191019 located in Section "19, Township 29
North, Range 1 East, W.M., Jefferson County, WA
Dear Mr. Barron:
Background
At your request, Bill Payton, Engineering Geologist with NTI .Engineering. and Surveying (NTI)
conducted a bluff stability inspection at the above referenced location on April 19,2006. The
purpose of this inspection was to examine the marine bluff at the subject site by visual means
and provide an opinion regarding the relative impact that a proposed beach access stairway
would have on the stability of the bluff.
It is our understanding that you desire to construct a stair tower on the beach with a bridge
leading from. the top of the bluff to the tower as approximately shown in the preliminary drawing
(Figure 1). We further understand that the stair system will be founded on piers and that the toe
of the bluff will not be excavated out in order to construct the stairs. And further, that bluff
disturbance will be limited to the immediate vicinity of the stair location and will not encroach
onto adjacent properties, and that disturbed areas on the bluff will be restored upon completion
of the stairs.
Site Description
The subject waterfront property is located at 3133 Oak Bay Road, south of Port HadlocK. The
property overlooks Puget Sound to the east and is bounded on the north and south by
residential property (Figures 2, 3 and 4).
Existing improvements to the property include a gravel driveway, garage and log home which
sits approximately 85' (75' for the deck) back from the top of the bluff (Photo 1). Drainage for the
existing homesite arrears to be controlled with catch basins in the driveway and roef~~uf~rs--with - . ~._-
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downspouts conveyed to tightline drains over the bluff.
The upland portion of the property slopes gradually to the east and is mixed wooded and open.
A ditch cuts across the middle of the property in a north-south direction and directs water from
the south .through the property and eventually to the beach via tightline drain on the property
north of the subject property. Water was flowing in the ditch at the time of the site visit.
The bluff at the property is approximately 60 feet high. Slope angles are variable but generally
range from about 40° to 55°, with the lower third of the bluff at about 70°. The upper and mid
bluff areas are predominantly vegetated with young alders and brush, with a few larger trees
(Photo 2). Some of the trees on the bluff have curved trunks, indicating that shallow down slope
creep of the surface soils is occurring. The steeper lower sections of the bluff are predominantly
void of vegetation due to wave erosion during the recent winter storms (Photo 3). Some areas of
the bluff were moist from groundwater seeps.
Site Geology
The Washington State Department of Ecology's Coastal Zone Atlas maps the upland and upper
bluff soils as Vashon lodgment till (Qvt1), and the lower bluff as Tertiary shale and mudstone
(Tg) (See Appendix). The till is described as consisting mostly a compact mixture of boulder to
sand size particles with some silt and clay. The Atlas lists this soil as excellent for foundation
stability, good for seismic stability, and says that that it stands in steep natural and/or cut slopes
for long periods. The Tertiary shale and mudstone is described as interbedded siltstone and
sandstone. The Atlas maps the stability of the upland as Stable and the bluff as Intermediate.
The Department of Ecology's "Geology and Ground-Water Resources of Eastern Jefferson
County, Washington" maps the soils in the area of the subject property essentially the same as
the Coastal Zone Atlas. This publication further states that these units are impermeable.
According to the Soil Survey of Jefferson County Area, Washington (United States Department
of Agriculture, 1975), the subject property is in an area mapped as Alderwood gravelly loam
(AmD) and Cassolary sandy loam (CfD). The Alderwood soil formed in glacial till and is
composed of silty sand or silty gravel. The Cassolary soil formed in reworked glacial and marine
sediments and is composed of stratified silty sand with a layer of clay:
Visual. observations of surface soils on the bluff face are generally- consistent with the above
descriptions, including siltstone and sandstone (Photo 4) and very compact silt. and glacial till
(Photo 5).
The bluff soil and rock at the site is very dense. As the bluff surface is weathered and softened,
vegetation can begin to take root and grow, except in areas where waves frequently contact the
toe of the bluff. As the vegetation grows, its roots further loosen the surface layer of soil,
typically a foot or so thick depending on the size of vegetation. When a slide occurs, triggered
by winter storm waves eroding the lower bluff in this case, and compounded by the saturation of
the soil from winter rains, this thin surface layer of soil that has been loosened by roots is
typically what slides down taking the vegetation with it. The resulting bare slope has a visually
dramatic appearance but the now exposed underlying soil is usually left relatively undisturbed
and the process begins all over again, resulting in a typically slow landward retreat of the bluff.
2
Conclusions and Recommendations
Based upon our understanding of the project and our site investigation, we conclude that the
beach access stairs will have minimal impact on the stability of the bluff. However, the natural
processes of bluff retreat are occurring at the subject property and periodic sloughing of the bluff
should be expected to continue which may necessitate future maintenance/repair of the stair
system. As mentioned earlier, it appears that drainage for the existing homesite has been
addressed previously.
The following recommendations should be considered with regards to the proposal:
1. It will be necessary to maintain ground cover in order to reduce erosion from surface
runoff. Any bare areas that develop, on the bluff or on the upland, should be
revegetated if possible. Native deep-rooted low growing vegetation that requires little
or no irrigation would be the most beneficial. Please consult the enclosed publications
for further information. It should be noted however that vegetation establishment in the
very compact soil and rock on the bluff may not be possible.
2. Vegetation on the bluff face provides stabilization to the bluff face soils and helps
remove water from the soil. Existing established vegetation should be left in as natural
state as possible. Once construction of the stair system is completed, any areas that
were disturbed should be revegetated as needed. As far as pruning for a better view,
minor thinning and pruning should be done in such a way that minimizes disturbance
to the soil and root zone and that insures the. continued health of the vegetation.
3. Tree limbs, lawn clippings, etc. should not be thrown over the bluff because these piles
have a tendency to damage/kill the underlying vegetation which in turn increases the
erosion potential of the bluff soils.
4. Heavy irrigation or other activities that would contribute large quantities of water to the
soil should be avoided.
5. Surface runoff from hard surfaces such as roofs, driveways, walkways and patios
appears to have been controlled already. The existing, and any future drainage control
devices need to function such that surface water discharge to adjacent properties does
not significantly exceed predevelopment conditions. We recommend that on site
infiltration of this water not be considered for this site due to the impervious nature of
the soil
6. Silt fences or other sediment control devices may be needed on the top of the bluff
during construction such that sedimentation to adjacent properties does not
significantly exceed predevelopment conditions.
7. Existing, and any new drainage control devices should be maintained in good working
order and inspected at least once a year.
For further information please review the three publications (included with the original of this
report) published by the Washington State Department of Ecology (DOE) entitled: °'~lope
Stabilization and Erosion Control Using Vegetation", "Vegetation Management:, A`Guide for
Puget Sound Bluff Property Owners" and "Surface Water and Groundwater on Coasfat Bluffs".
3
These publications can also be viewed on the DOE website at:
http://www.ecY.wa.gov/biblio/sea.html under the 1993 and 1994 year heading. The DOE website
also contains additional useful information regarding slope stability and site development; this
reference is highly recommended.
Limitations
This report has been prepared for your exclusive use in conjunction with. the above referenced
project. The report has not been prepared for use by others or for other locations. It may be
used for other purposes only with the. expressed written permission of the Engineer.
Within the limits of scope, schedule and budget, this report was prepared in general accordance
with accepted professional engineering and geological principles and practices in this or similar
localities at the time the report was prepared. No other warranty, expressed or implied, is made
as to the conclusions and professional advice included in this report.
The observations, conclusions and recommendations presented in this report were based on
our visual observations of the subject property at the time of our site visit; no laboratory tests
were performed. Soil. and geologic conditions can vary significantly between test holes and/or
surface outcrops. If there is a substantial lapse of time, conditions at the site have changed or
appear different than. those described in this report, we should be contacted and retained to
evaluate the changed conditions and make modifications to our report if necessary.
Sincerely,
NORTHWESTERN TERRITORIES, INC.
Robert A. Leach, P.E., MBA
Principal Engineer
t,
Bill Payton, L.E.G.
Engineering Geologist
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GEOTECHNICAL REPORT
Prepared For SeaHome Services, Inc.
May 8, 2006
For the Property Described as
3133 Oak Bay Road
Tax # 921191019
Section 19, Township 29 North, Range 1 East, W.M.
Jefferson County, Washington
Prepared by
NTI Engineering and Surveying
717 S. Peabody Street
Port Angeles, Washington 98362
Phone 360-452-8491 Fax 360-452-8498
Web Site www.nti4u.com
E-mail info@nti4u.com