REVIEWED nelson geo 10.16.20_MEMO_11584B20__Florez_Additional_ExplorationsNELSON GEOTECHNICAL
ASSOCIATES. INC.
17311-135"' Ave. N.E. Suite A-500
Woodinville, WA 98072
(425)486-1669
www.nelsongeotech.com
MEMORANDUM
DATE: October 15, 2020
TO: Mr. Jorge Florez
Mrs. Tatiana Giraldo
FROM: Khaled M. Shawish, PE
Katelyn Brower, GIT
RE: Comment Response for Additional Structures
Florez Property Additional Explorations
16000 — 75th Place West
Edmonds, Washington
NGA File No. 115841320
This memorandum documents our opinions and recommendations regarding the additional existing
structures at your residence located at 16000 — 75th Place West in Edmonds, Washington.
INTRODUCTION
We previously performed work on the site for the demolition of a partially constructed retaining wall
system, with our opinions and recommendations outlined in a letter issued to you on February 27, 2020.
The subject property is a trapezoidal -shaped parcel approximately 0.46 acres in area. The property is
currently occupied by a gated single-family residence with associated paved driveway areas, a grass yard
area and landscaping throughout the site. It is bordered to the east by 75th Place West, to the north and
south by existing residential development, and to the western lower property line by the BNSF railroad.
Localized steep slope hazards are mapped on the property by the City of Edmonds. The entire property
steps down moderately westward toward the railroad tracks, with the subject pond, shed, and stairs
structures situated above and to the east of the western property line. We understand that work
related to these projects was not permitted according to the City of Edmonds code, and we have been
requested to provide this evaluation of the current conditions of these structures to satisfy the City's
requirements.
Memorandum — Comment Response
Florez Property Additional Explorations
Edmonds, Washington
SCOPE
NGA File No. 11584620
October 15, 2020
Page 2
Based on our understanding of the planned development and site conditions, the services to be
provided by NGA were to:
1. Review available soil and geologic maps of the area.
2. Explore the subsurface soil and groundwater conditions within the vicinity of the
existing structures of the shed, pool, and stairs with hand auger explorations.
3. Qualitatively map the conditions of the site slopes in the vicinity of the structures.
4. Perform grain -size sieve analyses on soil samples, as necessary.
5. Provide opinions and conclusions on the construction of the present structures.
6. Provide recommendations for improving/replacing the structures, as needed or
warranted.
7. Provide recommendations for site drainage and erosion control.
8. Document the results of our findings, conclusions, and recommendations in a written
geotechnical letter.
9. Provide consultation and construction monitoring services throughout the duration of
the project.
SITE CONDITIONS
Surface Conditions
The property is generally a trapezoid -shaped parcel covering approximately 0.46 acres in area. The
property is currently occupied by a gated single-family residence with associated paved driveway areas,
a grass yard area, and landscaping throughout the site. The property is bordered to the east by 75tn
Place West, to the north and south by existing residential development, and to the western lower
property line by the BNSF railroad. Localized steep slope hazards are mapped on the property by the
City of Edmonds, and the site itself is located within the Meadowdale Landslide Complex, as designated
by the City of Edmonds. The entire property steps down moderately westward toward the railroad
tracks, with the subject rockery, pond, shed, and stairs situated above the partially constructed retaining
wall. The shed, pool and associated hardscape are situated immediately above an approximately 4 foot
tall rockery and the stairs are situated between the partially constructed retaining wall and pathway
along the bottom of the rockery. Based on discussions with the property owner, the unpermitted
structures are 3 years old.
NELSON GEOTECHNICAL ASSOCIATES, INC.
Memorandum — Comment Response
Florez Property Additional Explorations
Edmonds, Washington
NGA File No. 11584620
October 15, 2020
Page 3
The subject structures exist along the terraced slope that steps down below the residence, as shown in
the representative cross-section of the slope, Cross -Section A -A' in Figures 3. We did not observe
surface water ponding during our site visit on September 21, 2020.
ADDITIONAL EXPLORATIONS
Geology: The Geologic Map of the Edmonds East and Part of the Edmonds West Quadrangles,
Washington (MF-1541), by James P. Minard, (USGS, 1983) was reviewed for this site. The site is mapped
as Quaternary glacial deposits of Whidbey Formation (Qw), but is also located within the Meadowdale
Landslide Complex, which can contain old landslide debris. The Whidbey Formation is described as
medium bedded, brown to gray sand, silt, and clay. From our explorations, it appears that the onsite
soils fit the description of the mapped Whidbey Formation glacial deposits.
Explorations: The subsurface conditions within the site were explored with three additional hand auger
explorations located in the general vicinity of the structures west of the existing residence, and east of
the partially constructed retaining wall. The approximate locations of our explorations are shown on the
Schematic Site Plan in Figure 2. A geologist from Nelson Geotechnical Associates, Inc. (NGA) was
present during the explorations, examined the soils and geologic conditions encountered, obtained
samples of the different soil types, and maintained logs of the explorations. The soils were visually
classified in general accordance with the Unified Soil Classification System presented in Figure 4. The
logs of our explorations are attached to this letter and presented as Figure 5. We present a brief
summary of the subsurface conditions in the following paragraphs. For a detailed description of the
subsurface conditions, the exploration logs should be reviewed.
At the surface of the hand augers above the rockery, Hand Augers 101 and 103, near the pool and shed,
we encountered 2.0 feet of dry dark brown silty fine to medium sand with organics, which we
interpreted as undocumented fill. At 2.0 feet, we encountered brown to dark gray silty fine to medium
sand with gravel in a medium dense or better condition that we interpreted as native glacial soils. In
Hand Auger 102 below the rockery, we encountered 2.0 feet of undocumented fill before encountering
dark gray silty fine to medium sand in a loose to medium dense condition at depth. In the hand augers
done above the rockery, Hand Augers 101 and 103, the soils were dry to moist. In Hand Auger 102
below the rockery, soils were moist to wet. Hand augers were terminated between 2.2 and 3.5 feet of
depth below the existing ground surface.
NELSON GEOTECHNICAL ASSOCIATES, INC.
Memorandum — Comment Response
Florez Property Additional Explorations
Edmonds, Washington
NGA File No. 11584620
October 15, 2020
Page 4
Hydrogeologic Conditions
Heavy groundwater seepage was encountered within Hand Auger 102 below the rockery and pool. We
interpreted this water to be perched water. Perched water occurs when surface water infiltrates
through less dense, more permeable soils, and accumulates on top of a relatively low permeability
material. Perched water does not represent a regional groundwater "table" within the upper soil
horizons. Perched water tends to vary spatially and is dependent upon the amount of rainfall. We
would expect the amount of perched groundwater to decrease during drier times of the year and
increase during wetter periods.
CONCLUSIONS AND RECOMMENDATIONS
Based on our observations and general explorations of the site, as well as the previous explorations of
the site, we believe the additional unpermitted structures, consisting of the stairs, pool and associated
hardscape, and pumphouse/shed, are stable in their current state and should not pose a significant
danger or significant impact to the current slope conditions. According to discussions with the property
owner, these structures are approximately 3 years old. In our opinion, from a global stability standpoint,
we do not believe the minor grading associated with the construction of these structures has
significantly changed the loading of the slope or the drainage picture. The hardscape around the pool
does not show visible cracking or settling, but the rockery below the shed, hardscape, and pool does
show some minor soil erosion through the rocks. A rockery is generally not considered a retaining
structure and acts more as an erosion control feature. Therefore, some soil movement and/or
settlement is to be expected to require some maintenance and should be expected with time. Provided
the pond/pool is lined with a flexible membrane, this should not be a concern. Even if minor seepage
from the pond/pool exists or has a potential to exist, it should not pose a significant issue for the current
site and slope conditions, provided that drainage systems are maintained on the site. We recommend
the existing subject structures remain in place so as to avoid further unnecessary disturbance of the site
slopes.
Significant seepage was encountered below the rockery, which is below the pond and shed. The soils
above the pond on the slope were dry to moist, with no perched water. As a result, we recommend that
the drainage practices around the pond be investigated and improved. This could entail installing a level
spreader to help disperse runoff over a larger area. Under no circumstances should water be allowed to
flow freely over and concentrate on the site slopes.
NELSON GEOTECHNICAL ASSOCIATES, INC.
Memorandum — Comment Response
Florez Property Additional Explorations
Edmonds, Washington
NGA File No. 115841320
October 15, 2020
Page 5
As noted in our previous letter, the soils on the site are extremely moisture sensitive and disturb easily
when wet. Although no grading should be required to retain the current structures on the site, if
grading is to occur for previously evaluated projects, it is our recommendation that no grading or
earthwork be performed during the wet season between October 1st and April 30th. If grading is to
take place during this time period, additional expenses are to be expected and could include, but are not
limited to, the placement of rock spalls to protect native soils, installation of temporary drainage, and
covering bare soils with erosion resistant materials.
CONSTRUCTION MONITORING
We should be retained to provide construction monitoring services during the earthwork phase of the
project and during any wet season work, to evaluate slope conditions, any excavations, and drainage
system installation.
CLOSURE
We trust that this memorandum should satisfy your needs at this time. Please do not hesitate to
contact us should you require anything further.
Five Figures Attached
• • •
NELSON GEOTECHNICAL ASSOCIATES, INC.
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No.
Date
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Florez Additional
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NGA
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Original
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Number and approximate location
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GROUP
MAJOR DIVISIONS
GROUP NAME
SYMBOL
CLEAN
GW
WELL -GRADED, FINE TO COARSE GRAVEL
COARSE-
GRAVEL
GRAVEL
GP
POORLY -GRADED GRAVEL
GRAINED
MORE THAN 50 %
GRAVEL
GM
SILTY GRAVEL
OF COARSE FRACTION
RETAINED ON
SOILS
NO.4 SIEVE
WITH FINES
GC
CLAYEY GRAVEL
SAND
CLEAN
SW
WELL -GRADED SAND, FINE TO COARSE SAND
SAND
SP
POORLY GRADED SAND
MORE THAN 50 %
RETAINED ON
MORE THAN 50 %
NO. 200 SIEVE
OF COARSE FRACTION
SAND
SM
SILTY SAND
PASSES NO. 4 SIEVE
WITH FINES
SC
CLAYEY SAND
FINE -
SILT AND CLAY
ML
SILT
INORGANIC
GRAINED
LIQUID LIMIT
CL
CLAY
LESS THAN 50 %
SOILS
ORGANIC
OL
ORGANIC SILT, ORGANIC CLAY
SILT AND CLAY
MH
SILT OF HIGH PLASTICITY, ELASTIC SILT
INORGANIC
MORE THAN 50 %
PASSES
LIQUID LIMIT
CH
CLAY OF HIGH PLASTICITY, FAT CLAY
NO. 200 SIEVE
50 % OR MORE
ORGANIC
OH
ORGANIC CLAY, ORGANIC SILT
HIGHLY ORGANIC SOILS
PT
PEAT
NOTES:
1) Field classification is based on visual SOIL MOISTURE MODIFIERS:
examination of soil in general
accordance with ASTM D 2488-93. Dry - Absence of moisture, dusty, dry to
the touch
2) Soil classification using laboratory tests
is based on ASTM D 2488-93. Moist - Damp, but no visible water.
3) Descriptions of soil density or Wet - Visible free water or saturated,
consistency are based on usually soil is obtained from
interpretation of blowcount data, below water table
visual appearance of soils, and/or
test data.
Project Number
NELSON GEOTECHNICAL
No.
Date
Revision
By
CK
11584B20
Florez Additional
ASSOCIATES, INC.
NGA
Explorations
GEOTECHNICAL ENGINEERS & GEOLOGISTS
1
9/28/20
Original
DPN
KSB
Figure 4
Soil Classification Chart
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811-1%[h Ave.NE,A-500 Industry Lane,88
Woodinville, WA 98072 East Wenatchee, WA 98802
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(425) 486-1669 / F_ 481-2510 www. nelsongeotech.con, (509) 665-7696 1 Fax: 665-7692
LOG OF EXPLORATION
DEPTH (FEET) USC SOIL DESCRIPTION
HAND AUGER 101
0.0 - 2.0 GRASS, UNDERLAIN BY DARK BROWN SILTY FINE TO MEDIUM SAND WITH ORGANICS AND
GRAVEL (LOOSE, DRY) (FILL)
2.0 - 2.2 BROWN GRAY SILTY FINE TO MEDIUM SAND WITH ROCK SPALLS
(MEDIUM DENSE TO DENSE, MOIST)
NO SAMPLES WERE COLLECTED
NO GROUNDWATER SEEPAGE WAS ENCOUNTERED
NO HAND AUGER CAVING WAS ENCOUNTERE
HAND AUGER WAS COMPLETED AT 2.2 FEET ON 9/21/2020
HAND AUGER 102
0.0 - 2.0 GRASS, UNDERLAIN BY DARK BROWN SILTY FINE TO MEDIUM SAND WITH GRAVEL, ROOTS,
ORGANICS, (LOOSE, MOIST TO WET) (FILL)
2.0 - 3.5 SM-ML DARK GRAY SILTY FINE TO MEDIUM SAND WITH SILT LENSES (MEDIUM DENSE, WET)
NO SAMPLES WERE COLLECTED
SLIGHT TO HEAVY GROUNDWATER SEEPAGE WAS ENCOUNTERED AT 2.0 FEET
NO HAND AUGER CAVING WAS ENCOUNTERED
HAND AUGER WAS COMPLETED AT 3.5 FEET ON 9/21/2020
HAND AUGER 103
0.0-2.0 BROWN SILTY FINE TO MEDIUM SAND WITH GRAVEL, ORGANICS, AND WOOD DEBRIS
(LOOSE, DRY) (FILL)
2.0 - 3.0 SM BROWN GRAY SILTY FINE TO MEDIUM SAND WITH GRAVEL
(MEDIUM DENSE TO DENSE, DRY -MOIST)
NO SAMPLES WERE COLLECTED
NO GROUNDWATER SEEPAGE WAS ENCOUNTERED
NO HAND AUGER CAVING WAS ENCOUNTERED
HAND AUGER WAS COMPLETED AT 3.0 FEET ON 9/21/2020
KSB: NELSON GEOTECHNICAL ASSOCIATES, INC.
FILE NO 115841320
FIGURE 5