HomeMy WebLinkAboutGEO2018-00059 BLD2018-00724 - GEO Geological Review - 7/10/2018 �iED 2-0 (2) - X0,59
Geological Assessment
for
Blaisdell Single Family Residential Property
630 Rauschert Road
Parcel No. 12118-50-00014
Mason County, Washington
September 10, 2018
Project#18177
Prepared For:
TN Miller Remodeling
1670 E Benson Lake Road
Grapeview, Washington 98546
Prepared By:
—777
Envirotech Engineering, PLLC i)-'111� 4 9/10/ 8
PO Box 984 tE.El
Belfair, Washington 98528
Phone: 360-275-9374
MASON COUNTY
COMMUNITY SERVICES
Geological Assessment
Instructions:
This checklist must be submitted with a Geological Assessment and completed, signed, and stamped by the licensed
professional(s)who prepared the Geological Assessment for review by Mason County pursuant to the Mason County
Resource Ordinance. If an item is found not applicable, the report should explain the basis for the conclusion.
Note: Unless specifically documented, this report does not provide compliance to the International Residential Code Sections
R403.1.7 for foundations on or adjacent to slopes, Section R403.1.8 for expansive soils or section 1808.7.1 of the International
Building Code Section for Foundations on or adjacent to slopes.
Applicant/Owner TN Miller Remodeling Parcel# 12118-50-00014
Site Address 630 Rauschert Road, Grapeview
(1) A discussion of geologic conditions in the general vicinity of the proposed development, with geologic unit
designation based on referenced maps.
Located on page(s) 6
(2) (a)A discussion of the ground water conditions at the site,
Located on page(s) 7
(b) A discussion of the estimated depth to water,
Located on page(s) 7
(c) A discussion of the quantity of surface seepage.
Located on pages) 7
(d) A discussion of the upslope geomorphology,
Located on page(s) 3
(e) A discussion of location of upland waterbodies and wetlands.
Located on page(s) 3
(3) The approximate depth to hard or dense competent soil. e.g. glacial till or outwash sand.
Located on page(s) 6
(4) A discussion of any geomorphic expression of past slope instability(presence of hummocky ground or ground
cracks,terraced topography indicative of landslide block movement, bowed or arched trees indicating
downslope movement etc.).
Located on page(s) 4
(5) A discussion of the history of landslide activity in the vicinity; as available in the referenced maps and records.
Located on page(s) 8
(6) An opinion on whether the proposed development is within the landslide hazard area or its associated buffer or
setback and the potential for landslide activity at the site in light of the proposed development.
Located on page(s) 8
(7) A recommendation by the preparer whether a Geotechnical Report should be required to further evaluate site
conditions and the proposed development of the subject property.
Rev.February 201E
Located on page(s) 12
(8) If the presence of a hazard is determined within 300 feet of the proposed development, then the following are
delineated on a geologic map/site map:
(a) the area of the proposed development,
Located on Map(s) n/a
(b) the boundaries of the landslide hazard area(top, both sides, and toe),
Located on Map(s) nla
(c) the associated buffers(top, both sides, and toe),
Located on Map(s) n/a
(d) building or other setbacks(top,both sides, and toe).
Located on Map(s) n/a
(9) A site map drawn to scale showing the property boundaries, scale, north arrow. and the location and nature of
existing and proposed development on the site.
Located on Map(s) Site Plan (appendix A)
1, Michael C. Staten hereby certify under penalty of perjury that I am a
civil engineer licensed in the State of Washington with specialized knowledge of geotechnical/geological engineering
or a geologist or engineering geologist licensed in the State of Washington with special knowledge of the local
conditions. I also certify that the Geological Assessment, dated September 10, 2018 and entitled
Blaisdell Single Family Residential Property meets all the
requirements of the Mason County Resource Ordinance, Geologically Hazardous Areas Section, is complete and true,
that the assessment demonstrates conclusively that the risks posed by the landslide hazard can be mitigated through
the included geotechnical design recommendations, and that all hazards are mitigated in such a manner as to prevent
harm to property and public health and safety.
3045
f,
(Signature and Stamp)
Page 2 of 2
Disclaimer. Mason County does not certify the quality of the work done in this Geological Assessment.
TABLE OF CONTENTS
1.0 INTRODUCTION..................................»»............»...».»........».............»....,.................»......»...........1
1.1 PROJECT INFORMATION.............................................. ..................................................................... 1
1.2 PURPOSE OF INVESTIGATION AND SCOPE OF WORK........................................................................ 1
2.0 SURFACE CONDITIONS....____............-—-------------------------------------------_--------3
2.1 GENERAL OBSERVATIONS..................................................................................................................3
2.2 TOPOGRAPHY......................................................................................................................................3
2.2.1 Upslope Geomorphology............................................................................................................3
2.3 SLRFACE DRAINAGE..........................................................................................................................3
2.3.1 Upland Water Bodies....................... ..............._......................................................................3
2.4 SLOPE AND EROSION OBSERVATIONS................................................................................................4
3.0 SUBSURFACE INVESTIGATION....».................»........».........»..»»»,....».,,...».»»..»».....................
3.1 FIELD METHODS,SAMPLING.4ND FIELD TESTING...........................................................................5
3.2 GEOLOGIC CONDITIONS.....................................................................................................................5
3.3 SPECIFIC SUBSURFACE CONDITIONS.............................................................._.................................6
3.3.1 Groundwater............................................................................................................................... 7
4.0 ENGINEERING CONCLUSIONS...........».......................................................»...............................8
4.1 LANDSLIDE HAZARDS.......................................................................................................................8
4.1.1 Landslides and Slope Stablltty Analysis......................................................................................9
4.1.2 Surface and Subsurface Drainage...........................................................................................10
4.2 EROSION HAZARDS................................................................................».........................................10
4.3 SEISMICH:AZARDs...........................................................................................................................10
4.4 OTHER CONSIDERATIONS................................................................................................ 11
5.0 CLOSURE......................................»»............................»...........................................................»12
Appendix A-Site Plan
Appendix B-Soil Information
1.0 INTRODUCTION
Envirotech Engineering, PLLC. (Envirotech) has completed this geological assessment for a
residential property located at 630 Rauschert Road, identified as parcel number 121 18-50-000I4
in Mason County, Washington. As presented herein, this assessment includes information
pertaining to the Project in this Introduction Section; observations of the property and
surrounding terrain in the Surface Conditions Section; field methods and soils descriptions in the
Subsurface Investigation Section; and, assessments for landslides, erosion, seismic hazards, and
other considerations in the Conclusions Section.
An initial geological/ geotechnical evaluation of the project was conducted by Envirotech on
September 8, 2018. It was determined that natural slopes between 15% and 40a/a were present
within 300 feet of the project. Due to these slope grades, a geological assessment is required
pursuant to landslide hazard areas of the Mason County Resource Ordinance(MCRO).
During the evaluation and site visit by Envirotech, surface and subsurface conditions were
assessed in order to determine if further geotechnical studies are required.After completion of the
field work and applicable Project research,Envirotech prepared this geological assessment.
1.1 Project Information
Information pertaining to the project was provided by the proponent of the property, and
observations from a field visit by Envirotech.The proposed development is expected to consist of
a new 2 story garage with living quarters, and other ancillary features typical of this type of
development. Approximate site development with relation to existing site features are illustrated
in the Site Plan in Appendix A of this report.
1.2 Purpose of Investigation and Scope of Work
The purpose of this geological assessment was to evaluate the project in order to confirm that the
proposed development is outside of any landslide hazard area and its associated buffers and
setbacks as determined in the MCRO. The investigation included characterizing the general
project surface and subsurface conditions,and evaluating the suitability of the soils to support the
planned site development. In order to fulfill the purpose of investigation, the geologicalf
geotechnical program completed for the proposed improvements of the Project include:
• Review project information provided by the proponent of the project;
• Conduct a site visit to document the site conditions that may influence the construction
and performance of the proposed improvements;
• Define general subsurface conditions of the site by observing soils within test pit
excavations, review well logs from existing wells new the Project, and evaluate
geological and hazard maps depicting the site geology for the vicinity of the project;
• Perform soils testing,such as visual classifications,to determine selected index properties
of the soils;
• Complete an engineering assessment supported by planned site alterations and the surface
and subsurface conditions that were identified by the field investigation, soil testing, and
applicable project research;and,
• Establish engineering conclusions based on findings and anticipated development.
Envirotech Engineering,PLLC Blaisdell Geological Assessment
PO Box 984 page 1 Parcel 12 1 1 8-50-000 14
Belfair,Washington 98528 Mason County, Washington
(360)275-9374 September 10,2018
EE.
..... ts
a y .
}
Project
1
s
}
-- - -- -XI
S aari<r section
Vicinity Map from Mason County Website
Envirotech Engineering.PLLC Blaisdell Geological Assessment
PO Box 984 page 2 Parcel 121 18-50-00014
Belfair,Washington 98528 Mason Count. Washington
(360)275-9374 September 10,2018
2.0 SURFACE CONDITIONS
Information pertaining to the existing surface conditions for the project was gathered on
September 8, 2018 by a representative with Envirotech. During the site visit, site features were
documented that may influence construction or reveal potential geological hazards. This Surface
Conditions Section provides information on general observations, vegetation. topography,
drainage and slope/erosion conditions for the project and surrounding areas.
2.1 General Observations
The property is currently vacant land and surrounded by residential development. Rauschert Road
dead ends near the south of the property, and Pickering Passage is over 300 feet beyond.
Vegetation on and new the property consists primarily of firs, and other trees and shrubbery
common to this area of the Pacific Northwest. An aerial photo of the Project and immediate
vicinity is provided on the following page.
21 Topography
The topographic information provided in this section was extrapolated from a public lidar source,
and incorporated observations and field measurements. Where necessary, slope verification
included measuring slope lengths and inclinations with a cloth tape and inclinometer. See the Site
Plan in Appendix A for an illustration of the general slope indicators with respect to the planned
development.
Slopes exceeding 15% are located on and beyond the property. Maximum slope grades are
approximately 20%with a vertical relief of approximately 30 feet.
2.2.1 Upslope Geomorphology
The upland area of the property is situated on a gentle to moderate sloping hillside.
Landforms are primarily of glacial origin with centuries of weathering overburden.
Additional geomorphology that is pertinent to both upslope and downslope areas are
provided in the Subsurface Investigation Section of this report.
2.3 Surface Drainage
The majority of the stormwater runoff originating upslope from the anticipated development is
expected to be minimal to moderate. Significant scour, erosion and sediment transport was not
apparent near the project.
2.3.1 Upland Water Bodies
There are no apparent water bodies or wetlands located upslope from the planned
development that would significantly influence the Project.
Envirotech Engineering.PLLC Blaisdell Geological Assessment
PO Box 984 page 3 Parcel 12 1 1 8-50-000 14
Belfair.Washington 98528 Mason County. Washington
(360)275-9374 September 10.2018
2.4 Slope and Erasion Observations
The existing moderate slopes near the Project signal a potential landslide or erosion hazard area.
Some indicators that may suggest past slope movements include:
• Outwash of sediments near the bottom of the slope,
• Fissures,tension cracks or naturally stepped land masses on the face or top of the slope,
and parallel to the slope,
• Fine,saturated subsurface soils,
• Old landslide debris,
• Significant bowing or leaning trees,or,
• Slope sloughing or calving.
The above mentioned indicators, or other signs of significant mass wasting on the property or
,within the general vicinity of the Project were not observed or discovered during research.
Indications of past landslides, current unstable slopes, deep-seated slope problems, or surficial
slope failures were not observed during the site visit.
91E MOUNTAIN
126'E MOUNTAIN DR
r sg A!54R E R
}
iQi E MOUNTAIN DR
121iE MOUNTAIN DR • -_
250 E CREST EN
111iE'MOUNTAIN DR
580 ERAUSCHERT F
S echm
1L
640 E RAUSCHERT RD
320 E CREST LN '6U1 EIRAUSCHERT Rt
591 E RAUSCHERT RD
611 E,RAUSCHERTRD
€i 631 E RAUSCHERT RD
291 E CREST,LN ^' ,
fi E RAUSCHERT RD, r
3Q1 E CRESTLN� �r
'.27 E''CREST LN
Aerial Photo front-Vason County We site
Envirotech Engineering.PLLC Blaisdell Geolo_ical Assessment
PO Box 984 page 4 Parcel 1 2 1 1 8-50-00014
Belfair,Washington 98528 Mason County,Washington
(360)275-9374 September 10.2018
3.0 SUBSURFACE NVESTIGATION
Information on subsurface conditions pertaining to the project was gathered during research and a
site reconnaissance. The site visit was accomplished on September 8, 2018 by a representative
with Envirotech. Specific information on field methods, sampling, field testing, subsurface
conditions,and results from soil testing are presented in this section of the report.Appendix B has
pertinent information on subsurface conditions for the Project, including test pit log(s)
representative of the site soils,and water well report(s)originating from the subject property and/
or nearby properties.
3.1 Field Methods,Sampling and Field Testing
Information on subsurface conditions for the Project was accomplished by probing anticipated
foundation areas with hand tools, and observing soils within test pit excavations and/ or earth
cuts. Information on subsurface conditions also included reviewing geological maps within the
Project vicinity, and water well reports originating from nearby properties.No soil samples were
collected for this Project. Envirotech measured the relative density of the in-situ soils by gauging
the resistance of hand tools.
3.2 Geologic Conditions
In general, soils at the project are composed of materials from glacial advances. The geologic
conditions as presented in the "Geologic Map of Washington," compiled by J. Eric Schuster,
2002 indicates Quaternary sediments, Qg. Quaternary sediments are generally unconsolidated
deposits, and dominantly deposited from glacial drift, including alluvium deposits. This project is
located within the Puget Lowland. Typically, "lower tertiary sedimentary rocks unconformably
overlie the Crescent Formation."as revealed in the Geologic Map. Initial sedimentary rocks were
formed from shales, sandstones and coal deposits from rivers. During the Quaternary period,the
Puget Lowland was covered by numerous ice sheets,with the most recent being the Fraser glacier
with a peak of approximately 14,000 years ago. Upon the glacial retreat, the landscape was
formed by glacial erosion glacial drift deposits.
The "Geologic Map of the Vaughn 7.5-minute Quadrangle, Pierce and Mason Counties,
Washington"by Robert L. Logan and Timothy J. Walsh, December 2007,provides the following
caption(s)for the project area:
4gt Vashan till—LTnstratified to moderately stabbed..compact.unsoiled nux-riue of clad'.silt. sand.
and gavel deposited 3irectly by glacial ice:gm ta t!to n:nearly even- here in sharp contact x%ith
underlying units:does not drain well as permeability-and poro-a\ are lox-sand and finer grams
in matrix are very angular pebble-to boulder-size clasts are couunwtly striated and faceted.
having angu lar and(or)rounded edges:boulden are zmertlly disseminated mid relatively-rare:
may contain interbeds of sand and grazvel.The surface of this unit is characterized by strearnitnec
drumlins.striations_and flutes that are generally htmdreds to thousands of feet lon_s.Angular to
subrounded ahicial erratic boulders. consisting mostly of plutonic or metamorphic rock are
common but dissemunated on the surface of this unit.Unit niav be capped by a fen-feet of
unsorted and stained ablation sand and gr2vel or by unit Qgos.Vashon till locaRv crosscuts older
sediments_forming angular unconfornuties.Drag folding and horizontal shearing rnav occur at
the base of the till or internally,between layers of till,especially-in duck deposits.Unit Qgt
1 anges in thickness from 0 to at least 50 fr.
Envirotech Engineering.PLLC Blaisdell Geological Assessment
PO Box 984 page 5 Parcel 12 1 1 8-50-00014
Belfair.Washington 98528 Mason County.Washington
{;60)275-9374 September 10.2018
a
- - Ols',
Ob
,i
3.3 Specific Subsurface Conditions
The following subsurface conditions are estimated descriptions of the project subgrade utilizing
information from the depth of penetration at all testing, sampling, observed and investigated
locations. Soils for this project were described utilizing the Unified Soil Classification System
(USCS). Using the USCS in conjunction with estimated relative densities and other anticipated
engineering properties of the soil, susceptibility for potential landslides, erosion and seismic
hazards may be assessed.
The project is primarily composed of undisturbed, native soils, without indications of substantial
fill. Competent bearing soils were encountered at 12 inches below the existing native ground
surface in locations where the ground was probed. For engineering purposes, these native soils
consist of distinguishable layers,as presented below.
Soils within the upper 2.5 feet of natural ground were observed to be primarily moist, brown silty
sand with gravel (SM). Soils below the upper SM layer were observed to be an SM hardpan. The
hardpan is believed to extend to depths of at least 50 feet. This is based on nearby well reports,
site geology, and/ or knowledge of the general area. Expanded and specific subsurface
descriptions, other than what is provided in this section, are provided in the soil logs located in
Appendix B of this report.
According to the "Soil Survey of Mason County," by the United States Department of
Agriculture, Soil Conservation Service (SCS), the site soils are described as Indianola sandy
loam, It, with 5% - I S% slopes. See the soil map below, and the applicable SCS soil profile(s) in
Appendix B of this report.
Envirotech Engineering. PLLC Blaisdell Geological Assessment
PO Box 984 page b Parcel 12 1 1 8-50-000 14
Belfair,Vdashingt on 98528 Mason County, Washington
(360)275-9374 September 10.2018
i 13 •J
ti.
Y" Y
is
�94
may,
Soil Survey From USDA Natural Resources Conservation Service
3.3.1 Groundwater
From the water well report(s)and knowledge of the general area,permanent groundwater
is at least 50 feet below the current ground surface. Surface seepage or perched
groundwater at shallow depths was not observed on-site, nor indicated on the well
reports. However, some seasonal groundwater is expected to flow directly above the
hardpan on occasion.
Ens'imtzch Engineering, PLLC Blaisdell Geolosical:assessment
PO Sox 984 page 7 Parcel 121 18-50-00014
Belfair.Washington 98528 Mason County, Washington
(360)275-93 74 September 10.2018
4.0 ENGINEERING CONCLUSIONS
The following sections present engineering assessments and conclusions concerning the project,
These conclusions have been made available based on the planned construction activities as
outlined in the Introduction Section of this report; general observations of drainage and
topography as summarized in the Surface Conditions Section; and, soil conditions that were
identified by the field investigation and soils testing as outlined in the Subsurface Investigation
Section. Conclusions for the Project that is provided herein, includes pertinent information for
landslide, erosion and seismic hazards.
4.1 Landslide Hazards
For the planned development, as provided in the Introduction Section of this report, it is
Envirotech's opinion that the proposed development is not subjected to or cause adverse impacts
to a landslide hazard area or its associated buffer or setback as defined in the MCRO. This
conclusion is based on the contents provided in this report.
Landslides are natural geologic processes, and structures near slopes possess an inherent risk of
adverse settlement, sliding or structural damage due to these processes.Geotechnical engineering
cannot eliminate these risks for any site with sloping grades because gravity is constantly
inducing strain on the sloping soil mass. Excessive wet weather and/ or earthquakes will
exacerbate these strains. Geotechnieal engineering considers excessive wet weather and `design'
earthquakes in order to provide an acceptable factor of safety for developing on or near sloping
terrain. These factors of safeties are based on engineering standards such as defining engineering
properties of the soil,topography,water conditions, seismic acceleration and surcharges.
Surface sloughing or other types of surficial slope movements usually do not affect the deep-
seated structural capability of the slope. However, excessive and/or repeated surficial slope
movements, if not repaired, may represent a threat to the structural integrity of the slope.
Maintenance of the slope should be completed if the situation does arise in order to prevent the
possibility of further surficial or deep seated slope movements that may be damaging to Iife or
property.
According to the Department of Natural Resources (DNR) "LHZ — Final A-I Map — Landslide
Inventory—Mason Watershed,by Sarikhan, et. al.,May 2007,"previous landslide activity is not
recorded new the project. Per the Resource Map from DNR, the Project is not within terrain
labeled `highly unstable' or `highly erodible' relating to soils. DNR labeled portions of this
project as medium to high slope instability with relation to slopes. This delineation is primarily
dependent upon slopes and convergence. Secondly, lithology and precipitation are modeled
within this delineation. In summary, this designation is based on mapping without field
observations or knowledge of the specific site geology or soils. A resource map from DNR is
provided below:
Envirotech Engineering.PLLC Blaisdell Geological Assessment
PO Box 984 page 8 Parcel 12118-50-00014
Belfair,Washington 98528 Mason County, Washington
(360)275-9374 September 10,2018
Ar
/ir-
!! i
Mo�i
5 fff ip
r !t f
�� J�•
/ all
r li
,�
r� �a
' �,• a
to
E Project
.= -
Map from Washington State Department of Natural Resources YYebsite
4.1.1 Landslides and Slope Stability Analysis
Past landslide activity or high slope instability indicators near the proposed development
was not revealed during the project research. In addition,detrimental landslide activity or
potential high landslide indicators were not observed during the site visit as outlined in
the Surface and Subsurface Conditions Sections of this report. Due to these factors, and
existing/proposed conditions, a slope stability analysis was not deemed necessary for this
project. Considering the planned construction as summarized in the Introduction Section
of this report; the aforementioned surface and subsurface conditions for the project; the
slope stability assessment provided herein; and the Engineering Conclusions provided
later in this report, it is our opinion that the project is not within a landslide hazard area,
and that the proposed site alterations will not encourage a landslide hazard.
Envirotech Engineering.PLLC Blaisdell Geological Assessment
PO Box 984 page 9 Parcel 12 1 1 8-50-000 14
Belfair, Washington 98528 Mason County-, \Vashin-on
(360)275-9374 September 10,2018
4.1.2 Surface and Subsurface Drainage
This project does not appear to experience significant subsurface drainage or surface
runoff. It is our opinion that groundwater or surface drainage is not a limiting factor for
this Project.
4.2 Erosion Hazards
Based on the USCS description of the Project soils, the surface soils are considered moderately
erodible. According to the Resource Map from the Washington State DNR, as provided above,
the Project is not within terrain labeled `highly erodible.' This Project is not within an erosion
hazard area as defined by the MCRO. Erosion hazard areas are those with USDA SCS
designations of River Wash (Ra), Coastal Beaches (Cg), Alderwood Gravelly Sandy Loam on
slopes 15% or greater (Ac and Ad), Cloquallum Silt Loam on slopes 15% or greater (Cd),
Harstine Gravelly Sandy Loam on slopes 15% or greater(Hb), and Kitsap Silt Loam on slopes
15%or greater(Kc).
Temporary and/ or permanent erosion control measures may be required for any site when land.
disturbance is involved. Erosion control will mostly depend on the timeliness of construction,
moisture content of the soil,and amount of rainfall during construction. Soil erosion typical to the
existing conditions and planned disturbance of this Project include wind-borne silts during dry
weather, and sediment transport during prolonged wet weather. Sediment transport of disturbed
soils could be from stormwater runoff or tracking off-site with construction equipment. Although
an engineered erosion control plan is not warranted for this project, Best Management Practices
(BMP's) should be employed during and after construction. Ordinary BMP's includes silt
fencing,protection of drainage outlets and vegetating denuded areas.
Erosion control information and specifications may be found in the applicable "Stormwater
Management Manual for Western Washington,"prepared by the Washington State Department of
Ecology Water Quality Program.
4.3 Seismic Hazards
Soils immediately below the expected foundation depth for this Project are generally Type D,
corresponding to the International Building Code(IBC) soil profiles. According to the IBC, the
regional seismic zone is 3 for this Project. The estimated peak ground acceleration ranges from
0.50g to 0.60g.This estimation is based on the United States Geological Survey(USGS)National
Seismic Hazard Project in which there is an estimated 2% probability of exceedance within the
next 50 years.
There are no known faults beneath this project. The nearest Class `A' or'B' fault to this property
is the Tacoma Fault Zone. This fault is a Class `A,` and is located approximately 4 miles to the
north of the Project. This information is supported by the USGS Quaternary Fault and Fold
Database for the United States.
The potential for liquefaction and other earthquake induced hazards are believed to be low for
this project. This is based on subsurface conditions such as soil characteristics and the lack of a
permanent and substantial shallow water table. Subgrade characteristics that particularly
contribute to problems caused by seismic events include submerged and confined, poorly-graded
Envirotech Engineering, PLLC Blaisdell Geological Assessment
PO Box 984 pale 10 Parcel 12118-50-00014
Belfair,Washington 98528 Mason County,Washington
(360)275-9374 September 10.2018
granular soils. Although gravel- and silt-sized soil particles could be problematic, fine and
medium grained sands are typically subjected to these types of seismic hazards.
4.4 Other Considerations
Conclusions in this report are based on the type and location of the anticipated development, and
existing on-site and off-site conditions. Site development that significantly deviates from the
anticipated improvements presented in this report, or nearby development that influences this
Project may require geotechnical design recommendations.
Envirotech En_ineering.PLLC Blaisdell Geological Assessment
PO Box 984 page I I Parcel 121 18-50-00014
Belfair,Washington 98528 Mason County,Washington
(360)275-9374v September 10.2018
5.4 CLOSURE
Based on the project information and site conditions as presented in this report, it is Envirotech's
opinion that additional geotechnical studies are not required to further evaluate this project.
Due to the inherent natural variations of the soil stratification and the nature of the geotechnical
subsurface exploration, there is always a possibility that soil conditions encountered during
construction are different than those described in this report. Therefore, it is recommended that
Envirotech is promptly notified if project and subsurface conditions found on-site are not as
presented in this report so that we can re-evaluate our recommendations.
This report presents a geological/geotechnical assessment, and is intended only for the owner,or
owners' representative. Furthermore, this report is only valid for the project information and
location described herein.
The services described in this report were prepared under the responsible charge of Michael
Staten, a professional engineer with Envirotech. Michael Staten has appropriate education and
experience in the field of geotechnical engineering in order to assess landslide hazards,
earthquake hazards,and general soil mechanics.
Please contact Michael Staten at 360-275-9374 if you have any questions, comments, or require
additional information.
Sincerely,
Envirotech Engineering
Michael Staten,P.E.
Geotechnical Engineer
Envirotech Engineering. PLLC Blaisdell Geological Assessment
PO Box 984 page 12 Parcel)21 18-50-00014
Belfair, Washington 98528 Mason County. Washington
(360)275-9374 September 10,2018
APPENDIX A
SITE PLAN
SCALE- 1 INCH 30 FEET
0 15 30
300'
PROPOSED
DRAINFIELD
.10
\
TPle
Ica
�o� c
PO
PROPOSED
BUILDING
PO
RP�SGN�R� R�A�
PROJECT/ OWNER/ LOCATION,
SINGLE FAMILY PROPERTY
GEOLOGICAL ASSESSMENT
NOTES BLAISDELL
630 RAUSCHERT ROAD
L SLOPE INDICATORS WERE FIELD MEASURED BY ENVIROTECH, AND/ OR PARCEL 12118-50-00014
EXTRAPOLATED FROM A PUBLIC LIDAR SOURCE WHERE APPROPRIATE. MASON COUNTY WASHINGTON
2. BOUNDARIES ON THIS SITE PLAN WERE NOT PREPARED BY A LICENSED LEGEND ENGINEER
SURVEYOR, LOCATIONS OF SITE FEATURES AND GEOLOGICAL/ SUBSURFACE ENVINEER, ENGINEERING
DESIGNATIONS AS SHOWN HERE, WITH RELATION TO THE PROPERTY LINES PO BOX 984
MUST BE VERIFIED BY THE OWNER. THE CONCLUSIONS AND SLOPE INDICATOR BELFAIR, WASHINGTON 98528
RECOMMENDATIONS PROVIDED IN THE GEOTECHNICAL/ GEOLOGICAL REPORT
ARE BASED ON GEOLOGIC AND SPECIFIC SUBSURFACE FEATURES THAT MAY PO PROBE 360-275-9374
BE LOCATED ON AND OFF THE PROPERTY, AND ARE NOT NECESSARILY
BASED OFF OF PROPERTY LINES SHOWN ON THIS SITE PLAN. TPJo TEST PIT SITE PLAN
APPENDIX B
SOIL INFORMATION
TEST PIT LOG
TEST PIT NUMBER TP-1
PROJECT: Blaisdell Geological Assessment DATE OF LOG: 0 9/812 0 1 8
PROJECT NO: 18177 LOGGED BY: MCS
CLIENT: TN Miller EXCAVATOR: N/A
LOCATION: Parcel 12118-50-00014 DRILL RIG: None
Mason County, Washington ELEVATION: N/A
INITIAL DEPTH OF WATER: N/A FINAL DEPTH OF WATER: N/A
SOIL STRATA, STANDARD PENETRATION TEST
DEPTH SAMPLERS USCS DESCRIPTION LL PI CURVE
AND TEST DATA DEPTH N 10 30 50
0 - — . .. .... ................. ......... ... ..... ... .. .. .. .
_ SM Brown, moist, medium dense SILTY
SAND with GRAVEL.Gravel is course
and subrounded. Sand is primarily
medium and coarse. Non plastic.
2
Light brown, low moisture,very dense
Excavation terminated at approximately
3 2.5 feet
4
5
6
7
8
I
9
10
No Groundwater Encountered ENVIROTECH ENGINEERING
This information pertains onty to this boring and should not be Geotechnical Engineering
interpreted as being indicative of the entire sde.
Map Unit Description:Indianola sandy loam,5 to 15 percent slopes—tvlason County..
Washington
Mason County, Washington
le Indianola sandy foam, 5 to 15 percent slopes
Map Unit Setting
National map unit symbol: 2hlg
Elevation: 0 to 300 feet
Mean annual precipitation: 30 to 55 inches
Mean annual air temperature. 48 degrees F
Frost-free period: 190 days
Farmland classification: Farmland of statewide importance
Map Unit Composition
Indianola and similar soils: 100 percent
Estimates are based on observations; descriptions. and transects of
the mapunit.
Description of Indianola
Setting
Landform: Terraces
Parent material: Glacial sandy outwash
Typical profile
H1 - 0 to 5 inches: sandy loam
H2-5 to 28 inches: loamy sand
H3-28 to 60 inches: sand
Properties and qualities
Slope: 5 to 15 percent
Depth to restrictive feature: More than 80 inches
Natural drainage class: Somewhat excessively drained
Capacity of the most limiting layer to transmit water(Ksat). High
(1.98 to 5.95 in/hr)
Depth to water table: More than 80 inches
Frequency of,flooding: None
Frequency of ponding: None
Available water storage in profile. Low(about 5.0 inches)
Interpretive groups
Land capability classification (irrigated): None specified
Land capability classification (nonirrigated): 3e
Hydrologic Soil Group: A
Forage suitability group: Droughty Soils (G002XN402WA)
Hydric soil rating. No
Data Source Information
Soil Survey Area: Mason County, Washington
Survey Area Data: Version 13 Sep 7. 2017
Natural Resources Web Soil Survey 9/8/2018
Conservation Service National Cooperative Soil Survey Paoe 1 of 1