HomeMy WebLinkAboutGeoTech Report Review for BLD2001-00764 - BLD Engineering / Geo-tech Reports - 10/5/2001 MASON COUNTY
PUBLIC WORKS DIRECTOR/COUNTY ROAD ENGINEER
Shelton,Washington 98584
DATE: October 5 h, 2001
INTER-DEPARTMENTAL COMMUNICATIONS
TO: Rick Mraz, DCD - Planner
FROM: Alan A. Tahja, P/W - Co. Hydr. Engr. DCD/Planniniz WO# 01-0174
SUBJ: Geo-Tech Report Review NAME: Bailor SFR at Lake Limerick
BLD2001-00764
Rick,
A geotechnical report prepared for the proposed Karen Bailor residence located on lot# 37,
Sleaford Road in the plat of Lake Limerick, has been received and reviewed by Public Works.
The report conforms to standards of engineering principles and practices for this time and place,
and appears to conform to the minimum requirements of DCD for geotechnical reporting.
Recommendations contained in the report should be made conditions for approval of proposed
construction.
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.
incerely,
4L
l
' Akan A. Tahj
File: H:\WP\GEO\REVIEWS\Bailor.doc
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GEOLOGICAL ASSESSMENT
FOR HOME CONSTRUCTION ON LOT 37,SLEAFORD RD.
MASON COUNTY, WASHINGTON
Prepared For: PLANNING
KAREN BAILOR
SHELTON, WA
Prepared By:
Geotechnical Testing Laboratory
Olympia, WA
With
Henry N. Alai, P.E.
September 26,2001
I. Objectives
The objectives of the Geotechnical Report are to:
A. Access the surface and subsurface conditions prevalent on the subject site, which
may have a bearing on its ultimate use as a site for residential development.
B. Recommend measures that may serve to mitigate any conditions of concern.
II. Site Conditions Assessment
A. General
The subject site, Lot 37, is located at Sleaford Road on Lake Limerick in Mason County,
Washington. The Parcel Number is 321275400037.
The lot is bounded by a moderate slope off Sleaford Road,by a steep wooded ravine on
the south and by a gentle slope toward the north and west. The lot is the highest point in
the surrounding area and runoff percolates into the ground and/or flows in a southerly
direction toward the natural drainage areas that were established when the subdivision
was approved.
In the general vicinity of the site is a well developed residential neighborhood.
B. Surface Conditions
The lot itself had been previously graded for a home. When the area was leveled, some
fill had been deposited and graded on the southern downhill side of the parcel to form a
building site that is almost level. This part of the fill shows very little settlement and
would have very little impact on the projected building. We assumed that no compaction
of the fill had been done and that differential settlement had already occurred. The
building area of the lot is completely clear of vegetation except for grasses. The wooded
part of the lot consists mostly of trees and shrubs. Natural slopes surrounding the home
site are less than 30%.
A topographic map of the parcel is found on Exhibit A. A typical slope profile is also
found in the Appendix.
The slopes in the vicinity are identified as stable with no evidence of deep seated
instability. Some evidence (i.e.,tree growth modification) of mass soil-creep movement
are found on the south slope below the leveled building area. However,the slopes show
no evidence of landslide activity.
C. Subsurface Conditions
The subsurface geotechnical investigation performed in September of 2001, consisted of
an examination of the cut slope on the east side of the proposed home site and the road
cuts entering the property. The resultant soil log produced from the site visit is included
in the Appendix. As shown in the boring log, about 32"of sandy gravel overlay the
semi-cemented gravely sandy soils at the site. The entire profile is well-consolidated.
The stiffness of the underlying soils indicates a low potential for liquefaction during
seismic activity.
The native soils encountered in our investigation were found to be of a quaternary
Vashon till.
D. Hydrologic Conditions
D.1 Surface Water
Lake Limerick is located on the western side of the East Mason Lake Road and north of
the subject property. Runoff from the general vicinity of the lot travels to the north and
to a low marshy area. No surface water was found on the site. Runoff from the roof will
become, in effect, surface water,and must be collected and conveyed down slope in such
a way as to protect downslope soil from erosion.
D.2 Groundwater
Groundwater was not observed or encountered. No instances of seeps of groundwater
were seen on the slopes on or adjacent to the parcel.
Normal footing drains for the dwelling will not be required for construction. The
groundwater conditions should be of little concern for the ultimate development of the
site.
III. Regulatory Requirements for Development
Development of the parcel is subject to requirements of the Mason County Building and
Planning Departments, which regulate slope stability. The Landslide Hazard Ordinance
includes criteria for erosion, landslide, and seismic hazard areas. If the criteria defining
these as hazard areas are not met by the characteristics of the site, then it can be argued
that the parcel is not within a geologically hazardous area. Otherwise,a permit for
development of the site can be issued by the County to mitigate the hazardous conditions
encountered.
The following narrative will address the relevant sections of the County's Ordinance:
Erosion Hazard Areas
The native soil found on the site, (Ac)Alderwood gravelly sandy loam415-30% slopes, is
described in the USDA-SCS Soil Survey of Mason County, WA (1960) as having little
erosion hazard. Very little construction activities are anticipated for the home so we do
not believe that an erosion hazard exists. No construction is expected to take place on
the slopes. The home will be placed on the level area of the lot. Otherwise, there is no
'evidence of soil erosion anywhere on the site to suggest that the site should be included in
the Erosion Hazard Area designation.
Landslide Hazard Areas
There is no evidence of soil mass movement in the vicinity of this parcel, and the site
generally does not match the criteria set forth in the Critical Areas Ordinance for
designation as a Landslide Hazard Area. The US SCS maps the area of the home as
having 15-30% slopes. The ordinance#88-00 Classification for landslide hazards
regarding hillsides and springs(A. 1. e.)are not applicable.
Seismic Hazard Areas
The well-consolidated site soils exclude the site from inclusion in this category. This
project is located within a"Zone 3 Area"as per the 1997 edition of the Uniform Building
Code.
IV. Slope Stability Analysis
Based on the geotechnical investigation,a model of site slope stability was prepared to
assess the instability of the slope under static and dynamic loading. Native soils were
modeled based on a unit weight of 133.21bs/ft3 and an internal angle of friction(0)of
35.50. The resultant model, in spreadsheet form, is included in the Appendix.
There is no evidence of deep seated instability in the site slope that would prevent
development of the site for residential-construction.
V. Cut& Fill slopes and Site Grading Requirements
No cutting or filling is required or anticipated for the project.
VI. Foundation Design Recommendations
On the basis of the data obtained from the site and the test results from the various
laboratory tests performed, GEOTECHNICAL TESTING LAB recommends that the
III following guidelines be used for the net allowable soils bearing capacity.
Net Allowable
Footing ASTM D 1557 Soils Bearing
Depth Sub grade Compaction Capacity
surface 90% 2,000 lbs./ft2
Any excessively loose or soft spots or areas that do not meet the compaction
requirements that are encountered in the footing sub-grade will require over-excavation
and backfilling with at least 2 ft. of structural fill. In order to minimize the effects of any
slight differential movement that may occur due to variations in the character of the
supporting soils and any variations in seasonal moisture contents, it is recommended that
all footings be suitably reinforced to make them as rigid as possible.
VII. Soil Compaction
All soil beneath the footings shall be placed in the firm native soil.
VIU. Proposed surface drainage
The only hard surface area that will collect water will be the roof of the proposed home.
We recommend that all downspouts be tight lined to a discharge area such as a seepage
pit. Subsurface drainage will not pose a problem to the home.
IX. Lateral earth pressures
The following data was determined for the on-site soils:
Lateral Pressure
Active coefficient 0.30
Passive (lbs/sq. ft.) 250
Friction (coefficient) 0.40
X. Erosion and Sedimentation Control
Best management practices for construction site erosion control must be implemented
during and after site development to insure that down slope soil and water resources are
not impacted by construction activities. See Exhibit C for details for a silt fence that can
be constructed should the site need earthwork. However, extensive earthwork is not
anticipated.
XI. Structural fill
We do not anticipate that fill will be needed for the home but should it become necessary,
the on-site soils may be used for structural fill.
XL Laboratory Data
Along with the field investigation, a supplemental laboratory testing program was
conducted to determine additional pertinent engineering characteristics of the foundation
materials necessary in analyzing the behavior of the proposed structure. Selected
sar ples,were subjected to amain analysis and a shear test Nvas—Ufo:med on samples
taken from the site for the purpose of determining the internal angle of friction to confirm
the stability of the slope. The results are included in the appendix.
XIII. Foundation Setback
In compliance with 1997 UBC Section 1809, any building foundation must be placed in
observance of an H/3 foot setback from the existing crest of the slope on the site. As
shown on Exhibit a substantial building site remains for development if this setback
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requirement and others imposed by Mason County are met. Compaction tests must be
conducted on any fill soils under the proposed home to determine if these soils conform
to 90% of the maximum dry density as per ASTM D-1557 as recommended above.
Storm water Management
Evidence of storm water runoff on this site has been minimal because of the vegetation
on the sloping portions of the site. Except for the roof runoff, which will be collected as
mentioned above,we do not anticipate a problem.
XIV. Conclusion
The subject parcel does not meet the defining criteria for inclusion in any of the Hazard
Areas included in the Mason County Critical Areas Ordinance and may be safely
developed with the recommended mitigation measures described above.
XV. Limitations
We have prepared this report for Karen Bailor for use on the above referenced site for the
construction or placement of a home. The data used in preparing this report should be
provided to prospective contractors for their bidding or estimating purposes only. Our
report, conclusions and interpretations are based on data from others and limited site
reconnaissance, and should not be construed as a warranty of the subsurface conditions.
Variations in subsurface conditions are possible and may also occur with time.
A contingency for unanticipated conditions should be included in the budget and
schedule. Sufficient testing and consultation should be provided by our firm during
construction to confirm that the conditions encountered are consistent with those
indicated by the field review, to provide recommendations for changes should the
conditions revealed during the work differ from those anticipated, and to evaluate
whether earthwork and foundation installation activities comply with our
recommendations.
The scope of our services does not include services related to environmental remediation
and construction safety precautions. Our recommendations are not intended to direct the
contractor's methods, techniques, sequences or procedures, except as specifically
described in our report for consideration in design.
If there are any changes in the loads, grades, locations, configurations or type 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 submitted,
Harold Parks
Engineering geologist
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GEOTECHNICAL TESTING LAB
Date: Sept. ,2001 File#:
Boring Log#: I Client: Bailor
Boring Type: road cut Depth Drilled: 8 feet
Depth Field Change Percent Minus
(in) Description in Soils %M I N I Qu I Qp V LL Pl, PI 3/411 #4 #200 Comments
6 duff
--------------
12 silty sandy gravel
-- ------ ----------------
---------- ------- -
18
--------------------------- ------ -----------
24 ;
1 2500 non- ;plastic roots
30
.......... ............... ----------
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36 :
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42 :
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48
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54 :
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60 :
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66 :
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72 :
sandy gravel
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84
---:---------------------------
90 :
---------------------------
96
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--------------------------- -------- --
108
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126
132
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