HomeMy WebLinkAboutHartstene Island Bluffs Tree Removal Site Eval - GEO General - 6/10/2009 ��Obacauoncc*a
June 10, 2009
Judith M. Greene
4301 Fairwood Blvd NE
Tacoma, WA 98422-4636
RECEIVEDSummary of Site Reconnaissance
Nov 2 $ 2Q12 179 Nantucket Road
426 W. CEDAR ST- Mason County, Washington
File No. GRE5-01
This letter report summarizes our observations and conclusions relative to geotech-nical
conditions in the vicinity of your property located at 179 Nantucket Road, based on our
reconnaissance of that property and adjacent areas with you on April 11, 2009. Our services
have been provided at your request and in accordance with our services agreement dated
April 10, 2009.
The subj ect property is located near the north end of Harstene Island in Mason County,
Washington, in the southeast portion of the Hartstene Pointe development. The existing
duplex within the property is located approximately 40 feet from the top of a steep bluff
overlooking Case Inlet. The adjacent bluff is approximately 30 feet high and consists
primarily of dense,glacially consolidated sand that predates the most recent glacier to occupy
this area, some 15,000 years ago. Along the base of the bluff, very stiff to hard glacial silts
are exposed within the lower portion of the bluff face. Near the top of the bluff, there exist
patches of the glacial till and recessional outwash from the most recent glaciation.
This segment of the shoreline faces toward the east, and has a relatively long eastward
"fetch" (the expanse of water across which wind blows toward the shore) and it is therefore
subject to active wave erosion. Based on typical erosion rates along Puget Sound shorelines,
it is our opinion that the bluff segment adjacent to your property is likely to have a long term
bluff retreat rate (averaged over a period of many decades) of between 0.1 and 0.25 foot per
year. However, shoreline retreat does not occur at a slow and stead), rate but is episodic.
Decades may go by with little or no or no observable changes, followed by one or more
landslide events that result in several feet of bluff retreat. The amount of retreat along the
top of the bluff that occurs during a single landslide event depends on the style and size of
the landslide, but is typically in the range of about 3 to 10 feet.
7030 NE 134th Street Kirkland, Washington 98034 425-821-2015 www.tubbs.com
Judith M. Greene
June 10, 2009
Page 2
So as not to increase the rate of erosion along the bluff, it is important that uncontrolled
surface water not be allowed to drain across the top of the bluff. A corrugated plastic pipe
presently conveys stormwater from within your property to the base of the bluff. We
recommend that the pipe be replaced with HDPE(High Density Polyethylene) pipe, which
is much more resistant to breakage.
During our site reconnaissance,you expressed concerns regarding a group of evergreen
trees located along the top of the bluff northeast of your residence. The southern three of
these trees have not yet been undermined by bluff retreat, but the northern two have been
partly undermined, In addition,the northern two trees have intertwined roots such that if one
were to fail, it would likely take the other with it. Your concerns were that the trees may take
a portion of the adjacent upland area with them if they were to fall or slide down the bluff,
or that the trees may fall toward the duplex during a storm blowing from the east, since their
eastern roots are partially undermined.
As we indicated to you at the time of our site visit,we believe those are both reasonable
concerns,though we don't believe either of those issues represent a probable and immediate
danger to your property. The tree roots presently provide some reinforcement to the soils
near the top of the bluff,but that reinforcement is progressively diminishing as the top of the
bluff erodes, and when they fall or slide they will indeed disturb a much larger area of soil
than if they were preemptively removed. From the standpoint of slope stability we have no
objection to their removal, so long as the root systems are left intact and care is taken to
minimize disturbance of areas on and adjacent to the top of the slope. We are not as well
qualified to comment on the hazard that the trees represent to the adjacent structures,except
to note that it appears to be a reasonable concern, and therefore recommend that the HPMA
have their forestry consultant look at the trees and provide and opinion regarding that
concern.
If the trees are removed, it is our opinion that planting of replacement trees is not
necessary from the standpoint of erosion and slope stability, because other large trees
presently exist a few yard back from the slope. However, where vegetative gaps exists or
will exist along the top of the slope,we suggest that you consider planting brushy vegetation
as a barrier to discourage people from too closely approaching the top of the bluff. Native
vegetation in that area presently includes evergreen huckleberry,salal and Oregon grape,and
these and other brushy vegetation would be suitable. The evergreen huckleberry would
probably provide the best barrier, but according to a botanist who reviewed our photographs,
7030 NE 134th Street Kirkland, Washington 98034 425-821-2015 www.tubbs.com
Date: July 13, 2009
Subj: Bluff Erosion Adjacent to Island Homes on Nantucket
To: Hartstene Point Maintenance Association (HPMA)
Board of Directors
202E Pointes Drive East
Shelton, WA 98584 p��+ f (t
From: Island Homeowners at 177 Nantucket
179 Nantucket
181 Nantucket
183 Nantucket
We are enclosing bluff inspection letters recently written by Dr. Tubbs for Judith Greene
(179 Nantucket) and William and Mary Ann Andersen (183 Nantucket). As you will see,
Dr. Tubbs expresses concerns about possible damage to our homes and to the bluff
should identified trees be toppled by wind or further erosion--events he believes are
reasonable concerns.
We are requesting the Hartstene Point Maintenance Association (HPMA) Board of
' Directors consider removal of the problematic trees on both properties as described by
Dr. Tubbs. Please advise.
hank you,
1
u ith M. Greene, 179 Nantucket
GENERAL CONDITIONS
This agreement describes the terms and conditions under which'fubbs Geosciences provides professional services to our clients.and the rights
and responsibilities that we and the Client have under this agreemment.
COMPENSATION
Our compensation will be a lump sum amount if so indicated in the proposal or services agreement.or wil I be determined on the basis of brie
and expenses in accordance with the following schedule:
Labor
Principals $150/hour
Senior Scientists and Engineers $120/hour
Staff Scientists and Engineers $80/hour
Secretaries,Drafters and Technicians $50/hour
Contracted professional and technical services will be charged at the applicable hourly rates listed above or at cost plus 10 percent.
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charged in accordance with the foregoing schedule.
Equipment
Field and laboratory equipment,per day Ranges from$20.00-250.00
Mileage for vehicle travel,per mile $0.50
Other
Charges for services,equipment and facilities not fumished directly by us,and any unusual items of expenses not customarily
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We strive to perform our professional services with the standard of care and skill of qualified geoscience professionals currently providing
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CLIENT FURNISHED INFORMATION
The Client is responsible to provide us with a description of the property,its location.and the locations of any underground utilities.facilities
or structures on or adjacent to the property that are relevant to our work.The C lient also must advise us ofthc location and nature of any known
or suspected hazardous materials that may exist on the property. The Client is responsible for advising us of any requirements for entry or work
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Client agrees to defend,indemnity and hold harmless Tubbs Geosciences from any claims,damages and expenses arising from such reuse.
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HARTSTENE POINTE e.a DAIE:YAA.3UD9
q p MAINTANANCE ASSOCIATION ,T "
//�9.. SCAIE: NOTED
Y:AN CpINtt 9A91NCfON - �•� !� 7
W N DRAINAGE IMPROVEMENTS Z AQ' DDA+" A" Cn—Y OYbo�'..,I.
MIS CFILAXEWO DETAIL! a<r ALA orcdEO: "S CONSULTING ENGINEERS
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Na. AEM90N OAR AA9D APPROVED:N.S 9GTDL�N.9�ND10x Mom'(1AE)>••-ALEA
Bill &Mary Ann Anderson MID J U NI 3 0 2009
183 Nantucket Road
Shelton, WA 98585
SERVICES AGREEMENT
File AND4-01
This confirms the agreement between Bill & Mary Ann Anderson (Client) and
Tubbs Geosciences for geotechnical services relative to slope stability conditions at your
property located at 183 Nantucket Road in the Hartstene Pointe area of Hartstene Island,
Washington.
The services provided by Tubbs Geosciences will consist of:
1. Review of published geologic information regarding the subject property and nearby
areas, and any information that you may provide regarding drainage issues or slope
instability at and near the property.
2. Surface reconnaissance together with you of the subject site and adjacent areas.
3. Discussions with you regarding geologic, hydrologic and other influences that
contribute to slope stability within your property,possible impacts of slope stability and
bluff retreat on the existing house, and possible means of mitigating those impacts.
4. Additional services that may be requested by you and agreed to by Tubbs Geosciences.
The professional services listed above will be provided in accordance with the terms
described in the attached General Conditions,which is a part of this agreement. The fee for
items 1 through 3 listed above will be a lump sum fee of$150,payable at the time of our site
reconnaissance. The fee for additional services including a written report if requested will
be determined on a time-and-expense basis using the rates indicated in the General
Conditions.
Tubbs Geosciences The services described above are
authorized by:
Donald W.Tubbs 'Authorizing Signature
Typed or Printed Name
April 10, 2009 ji/' 1 �
Date Date
;Individual with contracting authority and responsible for payment of Tubbs Geosciences services.
Please Return One Signed Copy of This Agreement For Our Files
Attachment
7030 NE 134th Street Kirkland, Washington 98034 425-821-2015 www.tubbs.corn