HomeMy WebLinkAboutM052703
District No. 1 Commissioner: Dan Titterness
District No.2 Commissioner: Glen Huntingford
District No.3 Commissioner: Wendi H. Wrinkle
County Administrator: David Goldsmith
Clerk of the Board: Lorna Delaney
MINUTES
Week of May 27,2003
Chairman Titterness called the meeting to order at the appointed time. Commissioner Glen
Huntingford was present. Commissioner Wendi H. Wrinkle was not present.
COUNTY ADMINISTRATOR BRIEFING SESSION: County Administrator David
Goldsmith reported on the following:
. The Remote Access Policy which covers employee access to the County computer system from
remote sites, and the Complaint Review and Enforcement Policy are both ready and will be sent to
each department for employee review and, after any suggested changes are made, these policies will
be brought forward for adoption by the Board.
. The Board and several other Elected Officials attended a 2 day workshop last week on the "Price and
Priorities of Government." The workshop focused on how to view the budget to determine what the
County wants to accomplish and then go through a process to redirect the budget to address those
priorities. Performance parameters are addressed up front. The report card back to the citizens is
how well the County did on those items. There is a "bureaucracy buster" waiver request for
employees or citizens to submit.
· The Central Services Director candidates will be interviewed this week.
· The Memorial Rose Garden Ceremony to honor 6 past employees is scheduled on the Courthouse
lawn this week.
· Senate Bill 5028 deals with separating water quality issues (regulated by the State Department of
Health) and water quantity issues (regulated by the State Department of Ecology.) This bill is an
attempt to separate and clarify the two issues at the State level.
· He and the Board will attend the "State of the Mill" meeting that has been scheduled by the Port
Townsend Paper Corporation.
· The UFCW contract has not been forwarded from the Union for the Board's signatures and should
be coming to the County for final approval soon.
· The Commissioners' Chambers is not currently wired for video cameras. Information Services will
research the cost of equipment required to video tape the Commissioners' meetings and the process
for broadcasting on PTTV.
Page I
Commissioners Meeting Minutes: Week of May 27,2003
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. The Department of Community Development is preparing an ordinance to adopt the revised State
Building Code standards that include the International Building Code. These standards become
effective July I. Chairman Titterness asked that the County do a presentation for local builders
about the changes in these standards when they are adopted.
PUBLIC COMMENT PERIOD: A member of the Marine Resources Committee, speaking
as a private citizen, asked the Board to look at the MRC's report for what it does and doesn't say because the
report shows scientific data, but it doesn't show the concerns of people who are passionate about preserving
the marine environment and a scientific approach may be logical and direct, but may not work when it
comes to the nuances of the marine environment.
APPROVAL AND ADOPTION OF THE CONSENT AGENDA: Commissioner
Huntingford moved to delete Items #l and #4 and to approve and adopt the balance of the items as
presented. Chairman Titterness seconded the motion which carried.
I. DELETE Resolution: Establishing Objectives Related to Growth Management Act (RCW 36.70A.130) Required Plan Review
(See item later in minutes.)
2. AGREEMENT re: Professional Services for the Preparation ofTri Area Urban Growth Area
Development Regulations; Jefferson County Community Development; Mark Personius
3. AGREEMENT re: Designating the Official County Newspaper of Public Record for Printing of
Legal Publications Through June 30, 2004; Port Townsend & Jefferson County Leader
4. DELETE Agreement re: Coastal Zone Management (CZM31O) Grant No. G0300137 for Funding the Northwest Straits Project,
Marine Resources Committee Year 4 Project Task 3; Scope of Work for the Tarboo/Dabob Bay Fish Assessment; Washington State
University (WSU) - Cooperative Extension Jefferson County; Northwest Watershed Institute (See item later in minutes.)
5. AGREEMENT re: Irondale Beach Limited Site Cleanup & Improvements, County Project
#SPI429; Jefferson County Public Works; Pacific Environmental Services Company
6. AGREEMENT, Amendment No.1 re: Emergency Management Services; Amending Work
Elements, Tasks and Payment; Hamlin and Associates
7. AGREEMENT, Amendment No.1 re: Membership Composition and Possible Expansion;
Washington Counties Risk Pool
8. Jefferson County Public Works Construction Plans re: Upper Hoh Road, Log Jam Mitigation,
County Project No. X01313
9. Bid Award Recommendation re: Construction and improvements ofSheriff/DispatchlEOC facilities,
County Project #CCI543; Jefferson County Public Works; Primo Construction Inc.
] O. Final Short Plat Approval, #SUB02-00006; Heavy Metal Hill Short Plat, To Divide Approximately
40 Acres Into Two (2) Residential Lots; Located East ofSRl9 - Beaver Valley Road, Chimacum;
Richard Broders, Applicant
11. Letter of Assurance of Match for Larry Scott Memorial Trail, Segment 3 Grant Funding; L WCF
Grant #03-1054C; Washington State Interagency Committee on Outdoor Recreation
Page 2
Commissioners Meeting Minutes: Week of May 27,2003
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Marine Resource Committee re: Update on Committee Activities: Andy Palmer, Chair,
introduced Tom Cowan, Executive Director of the Northwest Straits Commission and the following
members of the Committee: Jeff Gallant, Bob Tilley, Ann Murphy, and Rex Price, as well as staff
Michelle O'Connell and Pat Pearson. He then reviewed a slide presentation of the activities of the Marine
Resources Committee.
AGREEMENT re: Coastal Zone Management (CZM310) Grant No. G0300137 for
Funding the Northwest Straits Project, Marine Resources Committee Year 4 Project Task 3; Scope of
Work for the TarboolDabob Bay Fish Assessment; Washington State University (WSU) - Cooperative
Extension Jefferson County; Northwest Watershed Institute: (Item #4 on the Consent Agenda)
Commissioner Huntingford asked if the Northwest Watershed Institute has done work for the Marine
Resources Committee in the past? An MRC member advised that the Institute's lead person is Peter Bahls
who has done a lot of research in Jefferson County and he recently made a presentation about the
importance of the Tarboo/Dabob watershed which is a main focus for the MRC. Pat Pearson explained
that he has been working with them under a signing statement and he is doing research in the area for
another project. The MRC wants to contract with him to train their volunteers and he has agreed to share
all of the information from his research. There was a brief discussion regarding some of Peter Bahls' past
work in Jefferson County.
Commissioner Huntingford moved to approve the agreement. Chairman Titterness seconded the motion
which carried.
Establishing Objectives Related to Growth Management Act (RCW 36, 70A,130)
Required Plan Review: (Item #l on the Consent Agenda) Commissioner Huntingford moved to approve
RESOLUTION NO, 21-03 establishing objectives related to Growth Management Act (RCW
36. 70A.130) required plan review with a change to the last paragraph to say". . . that Jefferson County
intends to comply with the requirements. . ." by deleting the word "fully" from that portion of the sentence.
Chairman Titterness seconded the motion which carried.
Bob Wilson, Fire Protection District No, 2 re: Annexation: Bob Wilson and Fire District
No.2 Commissioner Julie McClanahan advised the Board that there are 17 sections ofland in the County
that are not protected by a Fire Protection District. These sections were identified with the help of the staff
from the Auditor, Central Services, and Assessor's Offices. A petition has been submitted to Fire District
No.2 that represents 100% of the landowners in the sections adjacent to the Fire District asking that they
be annexed into the Fire District. The Auditor has certified the sufficiency of the signatures on the petition.
Assessor Jack Westerman explained the process for annexation as detailed in RCW 52.04 and reported
that Fire Districts No.1 and No.3 may also be coming in to ask for the same type of annexation approval.
Page 3
Commissioners Meeting Minutes: Week of May 27,2003
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Commissioner Huntingford moved to have the Clerk draft a resolution for Board that concurs with the
annexation of these identified properties into Fire District No.2 as requested. Chairman Titterness
seconded the motion which carried.
HEARING re: Seawater Intrusion Compliance: Commissioner Tittemess opened the
public hearing on the proposed changes to the UDC as recommended by the Planning Commission.
Associate Planner Josh Peters stated that this hearing is associated with Master Land Use Application 03-
202 which consists of several UDC amendment proposals and associated policy statements in the Planning
Commission recommendation, dated May 7, 2003. A supplement to the recommendation, dated May 21,
2003, is also included. The Planning Commission's recommendation is an effort to comply with a
Western Washington Growth Management Hearings Board Compliance Order issued on December 5,
2002.
Al Scalf, Director of Community Development, submitted 2 hydrogeologic assessment reports that DCD
received in May, one for a parcel on Marrowstone Island, and one for a property off Hastings Avenue. He
also submitted a single family building permit that was received in May that is located just outside of a
High Risk SIPZ (Seawater Intrusion Protection Zone.) The well for this property was dug in 1995, but the
proof of potable water test was just submitted and shows that the analysis for chlorides is at 249 which will
require a hydrogeologic assessment and means it will have to be included in the High Risk SIPZ area.
Charles Stirling, Coyle, the proponent for the building permit that needs a hydrogeological assessment,
submitted and read his testimony. (See permanent record.)
Curt Meyer, Bridgehaven Community Club, stated that they have concerns about the wording about
limiting each well to 400 gallons per day. Their community has 2 wells and services 186 connections. It
needs to be clarified that community well systems are exempt from this requirement.
Beau Bricklemeyer, Aquatic Resources, stated that they have submitted written comments. In 1993-94
Marrowstone Island was designated a sole source aquifer by the EP A. Developing a water system on
Marrowstone Island will not solve the seawater intrusion problem, because there is no requirement for
capping a well if there is another potable water source available. People will use their own well water,
rather than pay for public water and degradation can still occur with overuse.
Janet Welch, representing the petitioners to the Hearings Board, noted that it has been 18 months since the
Hearings Board order on this case and a lot of work has been done. However, there is a lot missing in the
final draft between what was adopted by the Board in the interim ordinance and the Planning Commission
recommendation. This is a countywide issue. The burden shouldn't just be placed on people who are
putting in new wells. There are other ways that the County could have dealt with this issue that would
have produced a more thorough end result. The County needs a monitoring program that will give a
baseline for the data. Groundwater withdrawal is not regulated by the County so it should not even be part
Page 4
Commissioners Meeting Minutes: Week of May 27, 2003
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of the discussion. The County needs to encourage alternative water systems. There are a number of things
that the residents on the island can do, and are willing to do, to conserve the groundwater.
Charles Stirling, stated that when he called DCD, the Permit Technician said that the County has tried to
discourage rainwater catchment as a water source.
Beau Bricklemeyer, pointed out that he called the State Department of Ecology and asked how they view
rainwater catchment? In the enabling legislation for DOE, it says that they control the water "above the
earth, on the earth, and under the earth in the State of Washington." This would include rainwater and
what happens to it. DOE has a policy that requires a rainwater catchment system to have a water right
permit, but they are not actively enforcing it and if you send an application for a water right, they will
process it under most circumstances.
Chairman Titterness replied that the County has run into problems regarding catchment systems with the
State Department of Health and their regulations, and not the Department of Ecology.
Hearing no further comment for or against the UDC amendments, the Chair closed the public testimony
portion of the hearing. The Board agreed that they will review the testimony before they make a final
decision.
Advisory Board Appointment; Community Investment Fund Board: Commissioner
Huntingford moved to appoint Kathleen Emmerson to represent Commissioner District 3 on the
Community Investment Fund Board. Chairman Titterness seconded the motion which carried. There is no
term limit set for this Board.
~~
Lorna Delaney, CMC
Clerk of the Board
JEFFERSON COUNTY
BOARD OF COMMISSIONERS
=~
Dan Titterness, Chair
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Glen Hun n for ,
(Excused Absence)
Wendi H. Wrinkle, Member
Page 5
Page lof2
Julie Matthes
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From: Josh Peters
Sent: Friday, May 30, 2003 11 :39 AM
To: Julie Matthes
Subject: FW: Marrowstone Island
-----Original Message-----
From: Victor C. Rupert [mailto:V-Man7@attbi.com]
Sent: Tuesday, May 27,200310:20 AM
To: Carol Wise; #Planning Department; BOCC
Subject: Marrowstone Island
TO: Whom it may Concern
FM: Victor C. Rupert
4304 Belvedere Drive
PIano, Texas 75093
Owner: 701 Fort Gate
Nordland, Washington
I have been made aware that there is a meeting Tuesday the May 27th at 2:00 p.m. to
discuss water and development on Marrowstone Island.
Since I live in Dallas, Texas I am unable to attend but would like to voice my view.
I understand that there is a movement to block all future growth on Marrowstone Island
by imposing a ban on development and subdivision until such point as public water can be
run to the Island,
I also understand that there are some on the Island that oppose city water and other
services,
I am NOT one of these persons, I strongly desire public water and services on the Island.
The Issue for me is property value, I have seen the value of my property plummet with
each new restriction imposed by the county, Yet I have seen NO improvement in
conditions on the Island, What I HA VE seen is ever increasing taxes,
My view is that you allow continued development and provide the necessary services to
support life on Marrowstone.
Furthermore, if this ban on growth is allowed to remain in force I would demand a
reduction in taxes commensurate with the loss of value to my property.
5/30/2003
Page 2 of2
Sincerely,
Victor C. Rupert
214-893-0440
5/3012003
cC. !X.D 6 -.¿o'Q3
May 27, 2003
"
Comments to the Jefferson Countv Board of Countv Commlssioners:
J J
In the spirÜ oftrymg to assist the county In complymg WJth the Hearmgs Board order,
Petitioners otTer the tòllowing comments on the Planning Commission recommendation to
the Board. By making these comments, PetÜJOners are not committmg themselves to a
position or restricting themselves to these issues when we submit our Compliance Brief
The Planning Commission's diligent work on the Issue is apparent in their proposals to
the BoCC. Nevertheless, issues of saltwater intrusion and groundwater protection are
complex Issues rooted in many fleJds of sc1ence. For this reason, the application of
methodologies used to detïne, identitY, track, prevent, and remedy groundwater
degradation do not appropriately fàJI to the lay public.
U isn't that the Planning Commission ignored best available science in their work, rather it
was largely absent fŸom the dJscussJOns. Peu1Ìoners are aware of no instance since receipt
of the FDO (dated January 200'2) that the perspectives of a protessional hydrogeologist
were brought into the discussion. This omission became dear at the BoCC meetmg of
May 19 when the Chairman of the Planning Commission and the Chairman of the BoCC
bantered whether to use one sample or an average of the first fÒUT for the baseline.
Clearly neither of these well intentìoned men have the qualtfícatìons for making that kind
of decision, yet the PJanning Commission recommendation before you was drafted ITom
exactly these kinds ofdiscussions! The science is absent from the methodology, and no
amount of money spent on a hydrogeologist at the cuJmination ofa samphng period can
establish legitimacy from an off-the-cuff monitoring design. Petitioners have the same
reservations about the sampJing objectives, techniques, anaJyticaJ methodology, and
application of the monitoring data as we presented at the Compliance Hearing.
The HoCC intends to inquire about the county's authority to limit water use from private
wells. If the authority does not exist, the BoCC 1000 gallon limit is moot. lfthe
authority does exist, the PC standard of 400 gaHons peI day is far more reasonable than
the original BoCC.
The following comments address the UDC "emergency ordinance" changes by the BoCC
and proposed changes by the Pc. For more detail we suggest that you refer to our
Compliance Hrief~ since many ofthe failings identifíed at that líme remain in the latest
proposals.
3.6.5a (4) What constitutes a "history of chloride analyses..." for the purposes of having
a well become a SIPZ, or alternately being removed from designation? How many
samples constltute a "history"?
The Administrator and the County Health Department do not have the expertise to
(ietermine "the status of an area'" suspected of experiencmg connate seawater. All high
chloride results must be considered non-connate until proven otherwise using BAS.
The BoCC's proposed long-term solution to aquifer degradatwn on Marrowstone Island
IS the expansion of the public water system currently serving the recently designated Tri-
Area UGA. Capital iàcíhtJes planningf()r the UOA has not yet begun, and their water
needs have not been evaluated. It seems premature to assume that the PUD has the
capacity to serve Marrowstone Island jnl1ddj/ion to an undefined UGA.
Many other issues anse when considering public water as a remedy for seawater
intrusIOn, not the least of which is that the extension ofpuhllc water mto rural areas
approaches the fuzzy line of promoting sprawl. When densities are too high for private
water systems, perhaps the problem is with the density and nol with waler availability.
From a technical standpoint, public water may not be feasible in many parts of the
county. The BoCC must have more to offer to areas around the county susepUble to
seawater intrusion.
It is also a questionable assumption that public water necessarily protects aquifers.
Groundwater withdrawJs on Marrowslone Island., and anywhere else 1 hat public water
has or may be provided, could actually increase as people increase outdoor watering with
"free'" groundwaler which they no longer may drink. 'fhe Planning Commission revised
document makes the assumption that high chloride wells fall into disuse when public
waler 1S provided. However, Petitioners are aware of no provisions which require
abandonment of wells when public water is provided. '[his assumption is of doubtful
validity.
3.65D( I) Standards shall apply "when specified" in SfPZ, but are not specified. fs this
an oversight or a deliberate attempt to minimize lhe ef1èctJveness of the controls?
3.6.5d(2) Infiltration is a vital aspect of groundwater recharge and the Administrator
must not have lhe authority to waive the requirements.
3.6.5D(4) Golf courses, turf cultivation, and any other water consumptive uses (where
waler is lost from the system through extensive evaporation) should be prohibited m
SIPZ, not simply managed for pesticide use.
3.65D(9)ii This sec1ion applies to subc\1visions with nel density less than five acres.
Since RR1:5 is the highest density land use allowed, is this an oversight or a deliberate
attemp1lo minimize the eHècÜveness of the controls?
3.65D(9)iii Only building permits which require proof of potable water are su~jecl to
the pohcy. Your staff assured you that permitting of Auxiliary Dwelhng Units (ADUs)
not not be subject to the policy. Since this is not an oversight, is it a deliberate attempt to
minimize the effectiveness of1he controls?
36.5D(9)iv Ongoing monitoring needs to be mandatory in this and all SIPZ.
36.50(9)ivC3 Is the only 1Ìme a sample over 250 mg/I triggers a notice to title when the
sample is taken the first time. What about subsequent sampling?
3.6.50(9)ivdH Only the "use of a new well shall be conditioned through the associated
building permit" triggers enrollment in the sampling program. What about the many
existing wells that are associated with building proposals? Is this an oversight or a
deliberate attempt to minimize the effectiveness of the controls?
The focus oflhese sketchy attempts at "more protective standards" targets groundwater
withdrawl and overlooks the real potential both rainwater collection and enhancing aquifer
recharge so that a higher volume ofJreshwa1er infil1rates into the drinking water aquitèrs.
There are many, many techniques to enhance recharge that can be used by both the
private and pubJic sector Public sector examples include the following: policies thai
require Public Works to infiltTate all road runoff rather than discharging ìt directly to
marine water Your slonnwater requirements could include shading of all stonnwater
ponds to reduce evaporation. Your clearing and grading ordinances could be more strict
with regard 10 runoff and impermeable surfaces. Private sector actions need to be
included as voluntary BMPs and included in educational opportunities.
While focusing on the: quagmire ofJimiting water withdrawls from wells, you have missed
the opportunity to impose legitimate standards that would have that effect. Two
examples: 1) on new construction prohibit outdoor hose bibs drawing from groundwater
sources, and 2) change the plumbing code to allow dual plumbing for potable and non-
potable uses (making catchment that much easier by not having 10 conform to potabJe
standards). You have not made the use of catchment any easier through any of the
proposed changes< In Jàct, by the definition of alternative system you added to the uoe
in July, an alternative system (catchment as an example) "is any system....over 400
gallons per day" Does Ihis, and the catchment policy 97-01, require catchment systems
to provide this outrageous (and functional1y unfeasible) amount?
No attention has been directed al upgrading oJd wells, BefiJre 1990, field test kits were
rarely used and wells were drì1led deeper for more volume without awareness of chloride
levels. Now with very low now pumps,jt is possible to "shorten up" wells with high
counts and reduce the chloride levels dramatically. Older wells associated with new
penn its (any expansion of water usage) need to be evaluated 1()T upgrades that. can
improve their performance.
No attention has been given to well starts in S[PZ. When the driller contacts the Hea[th
Department., wouldn '¡this be an excellent time for drj]Jer education? What about
standards requiring that the distance from the well to marine water be maximized?
And finally, you have ignored the need for education and the possibilities of using
innovative programs (including educational programs) to fund and carry out the
monitoring programs and upgrade incentive programs.
I f Jefferson County applied only a small percentage of the efforts and expense of fighting
land use controls in actually implementing wise policy that is protective of groundwater,
the people you represent could now have been secure in the knowledge that their water
supplies are protected now and forever,
[n groundwater protection, like any other complex problem, there are technical aspects of
the solution, there are non-technical aspects., and there are aspects that draw from
collaborative, creative efforts by involved citizens. Like a good soup, an must be present
for a satisfactory outcome, but it seems like Jefferson County is content to make its stone
soup with little more than boiled stone.
~
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Janet Welch
Representative for Petitioners
Box 1221
Hadlock, W A 98339
360-385-5910
LC Ul..U !:> -~ - U?
To: Tom McNerney, Planning Commission Chair
Jefferson County Department of Community Development
621 Sheridan Street
Port Townsend Washington 98368
Re: Application for County-Initiated UDCX Amendment MLA # 03-00202
Dear Sir,
. I am writ.ing in. regard to proposed policies related to securing building permits
ID seawater mtruslOn zones located in Jefferson County. My husband and I are in
the midst of trying to get a building permit for a two bedroom home located on
approximately eleven acres of land on Toandos Peninsula. We have owned this land
for o~er 13 years and have had a mobile home on the property and a functioning
well smce 1995. Our nearest neighbor with a functioning well is approximately 1200
feet north of our property. We have had a dream of building a home on our land
once we were both retired from full time employment. Since a building permit
requires evidence of potable water, we submitted the original well log and a recent
water analysis with our building permit proposal. The water analysis indicated a
chloride level of 249 which is high but still below the EP A's MCL of 250. Peter
Bonyun, a permit technician for the department of community development,
accepted all of our building permit papers and said that we just made it in terms of
both the chloride limit and the location of our well, as it is outside of any high risk
SIPZ. Assuming that there would be no problem, we went ahead with the permit
process and paid the county the required money which amounted to $2234.19.
About a week later we were notified that the county would require us to have our
well assessed by a hydrogeologist since the chloride level was above 200, It seems
that the county planning commission had agreed to lower the acceptable chloride
level to 200 instead of 250. However, after reading over the application for county
initiated UDCX Amendment MLA #03-00202, it seems that this requirement is not
yet law. So the main purpose of my letter is to ask that the county reconsider this
requirement of having all persons requesting a building permit in a SIPZ hire a
hydrogeologist to assess their wells if their wells have a chloride reading of 200 or
more.
My husband and I certainly understand the necessity to learn as much as
possible about our local aquifers and to educate all well users about the causes of
seawater intrusion and what needs to be done to mitigate the problem. All of us that
depend upon groundwater have a stake in maintaining as much quality as we can,
given the local situation, No one has the luxury of using water carelessly. No one
should be grandfathered in this regard as the water that needs to be protected is not
old water but new water! However, requiring only new home builders with high
chloride to hire a hydrogeologist in many situations would make no sense at all. It
seems as if the burden of collecting data about aquifers is landing on the backs of
the new homebuilder. Any hydro geologist would know that one needs data on
chloride levels from as many wells as possible throughout the year; one needs data
on water usage; one needs to know the local geology in terms of water permeablility
and recharge capacity, Any home owner can take his(her) own water samples in to
be tested for any type of cations and anions. Flow meters could be attached to all
wells to monitor usage. Information about the local geology, strata, can be obtained
from well logs which, I believe, are on record at the health department or from
internet sites, universities etc. All of these data could then be used by
hydrogeologists later on to help the county understand more about the severity of
the local seawater intrusion. Hydrogeologists could then suggest monitoring and
conservation programs that the county could set up to protect our groundwater.
Drilling a well is a very costly undertaking. Our well cost approximately $20,000.
All homeowners that have a well have also provided a window into an aquifer. The
county needs to assume their leadership role on educating their citizens regarding
the necessity of allowing all wells in SIPZ to be tested periodically. That, along with
water usage monitoring, are all good ideas and reasonable things to do by well
owners in at risk regions of our county, Well monitoring and water quality testing
will cost the homeowner and new homebuilder more money but at least concrete
information will be collected about the seawater intrusion problem. Spending an
unknown amount of money, perhaps thousands of dollars, on hiring a
hydrogeologist for every at risk well is just going to enrage the citizens asked to do
this. I feel that the county should at least require that all well users in SIPZ collect
the above data for a few years and then the county planning commission along with
state hydrogeologists could make some rational decisions about the severity of our
local seawater intrusion problem and come up with sound policies that the Jefferson
county citizens would respect.
Cf4 ~/ f?~~~~~~!:~ (
May 25-2003
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TWISS ANALYTICAL LABORATORIES, INC.
26280 Twelve Trees Lane, Suite C Poulsbo, W A 98370 Telephone (360) 779-5141 FAX (360) 779-5150
INORGANIC CHEMICALS (IOCS) REPORT
Private System Name: Stirling
01088246 Date Collected: 4/30/03 DOH Source N
----------
Sample Type: D Sample Purpose
__n___.____.._.__ -
4/30/03 Date Reported: 5/5/03 Supe~isor:_,,_
~-_._-----
Date Analyzed: 5/5/03 Analyst:
" ---.-.---
Jefferson Group:
·-_____n___.___-.-.____ ..___...._..__
[~yste~!D No:
I !-a~/~~,,~!~ N()~
MultiP!~ ~()~~~:
Date Received:
~ .- .-.... -_..__.._-~--_.-
Date ~~eJ>~~~_
. County:
I·-·"'·~~~~_~_n.
¡ Sample Location:
Send Report To:
I
--.-.-'----'--'---.-.---.....-
0:
: B ··~--·:T·--"-·-·-·~"
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- -Mr ---~--,,~.--.
-"--~------"'------'
Outside Faucet-267 Sierra Trail
Charles Stirling
267 Sierra Trail
Quilcene, W A 98376
--___________.h...__.__ ..._....
Bill To:
--.-----.-..------ .-.-,--.-
"~----'----
Trigger?
MCL?
Exceeds
Trigger? MCL?
---
Notes:
SRL:
Trigger Level:
(State Reporting Level), indicates the minimum reporting level required by the Washington Department of Health (DOH).
DOH Drinking Water response level. Systems with compounds detected at concentrations in excess of this level are required to take additional samples.
Contact your regional DOH office for further infonnation.
(Maximum Contaminant Level), If the contaminant amount exceeds the MCL, immediately contact your regional DOH office.
(Not Analyzed), in the results column indicates this compound was not included in the current analysis.
(Not Detected), in the results column indicates this compound was analyzed and not detected at a level greater than or equal to the SRL
indicates the compound was not detected in the sample at or above the concentration indicated.
MCL:
NA:
ND:
< (0.001):
Comments:
f~Ö~l~~~ll~~ \r\
\ \ '
MAY - 6 ØJ3 L~'
JEFFERSON COUNTY I,'
OEPT OF COMMUNITY DEV£lO~:~.L:
COpy
Twiss Laboratory Number: 41551
Page 1
Start card No. ('iO 44;J 4 0
,1S1 Copy wllh
, ..logy
. Ot ner's Copy
Driller's Copy
WATER WELL REPORT
UNIQUE WELL I.D. #
z\!?::?3ù::-:¡
.NER: Name l":.~.
,:I~::irL::3 3ì:irlin:;;
STATE OF WASHINGTON
Address ~J 0 3 S
Waler Right Permit No.
37th ~\-~e.:"~.E·.,
~';¡l1
331-15
SC2.1 t.:l:~,
. ,\j':; 1/4 .);:' 1/4Sec 32 T. 26 N. R hJ W.M.
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LOCATION OF WELL: County .J 8ff!êrson
.a) STREET ADDRESS OF WELL (or nearest address) off ThO:l3i:lnd Tr;ii.ls Roa(~,
(3) PROPOSED USE:
(10) WELL LOG or ABANDONMENT PROCEDURE DESCRIPTION
d Domestic
D Irrigation
D DeWater
Industrial D
Tesl Well D
Municipal D
Other D
(4) TYPE OF WORK:
Owner's number of well
(If more than one)
New well cI.
Deepened D
Reconditioned D
Bored D
DrtvenD
Jetted D
Abandoned D
Method: Dug D
Cable D
Rotary ¡j{
(5) DIMENSIONS:
Drilled 436
"
Diameter of well 'Q
feel Depth of completed wen
43B
Inches.
It.
(6) CONSTRUCTION DE"!AILS: 438
h 0
Casing InstsJrl: 'J · Dlam. from ft. to It.
Welded · DIam. from ft. 10 It.
Uner installed D
Threaded D · DIam. from ft. to It.
Perforations: Yes 0 No IA
Type of perforator used
SIZE of perforatfons
perforations from
perforations from
perforations from
Screens: Yes 0 No O!
Manufacturer's Name
Type
Diam. _ Slot size
Diam. Slot size
Gravel packed: Yes 0
Gravel placed from
In. by
It. to
ft. to
ft. 10
from
from
Model No.
It. to
ft. to
No tKI
Size of gravel
It. to
Surface seal: Yes 12§ . ~ No 0 . To what dep~?': 1 ¿,
Material used in seal i:~n tCl.'ll. t(~
Did any strata contain unusable water? Yes 0 No I){
Type of water? Depth of strata
Method of sealing strata off
(7) PUMP: Manufacturer's t-,lame COuJ.f15
Type: 3UD.æ-r3~b1.? J~.lO
(8) WATER LEVELS:
Static level )50
H.P.
J..
Land-surface elevation
above mean sea level
It. below top of well
lis. per square inch
Date
Date
I I It.
310f;;/~!!i
Artesian pressure
Artesian water is controlled by
(Cap. valve. etc.)
(9) WELL TESTS: Drawdown Is amount water level is lowered below static level
Was a pumJl ~st made? Yes ŒI N$. P If yes, by whom? Gre$l.1aM
Yield: , 1 gal.lmin. with ~~ T It. drawdown after I hrs.
..
..
..
..
..
..
Recovery data (time taken as zero when pump turned off) (water level measured from well
top to water level)
1im9r:<: _1 twater Level . ]im~ . Water Level 1ime Water Level
r-I.\ r~. ~1:;j "(JUn.
Date of test :3 iðG¡ ~ ~
Bailer test gal.lmin. with It.dra'!1tØown alter
Airtest ~ gal.lmin. with stem set at 4§~ ft. for
Artesian flow 5D g.p.m. Date
Temperature of water _ Was a chemical analysis made? Yes 00
,
No 0
ECY 050-'-20 (9/93) . . f ~
Formation: Describe by color, character, size of material and structure, and show thickness ot aquHers
and the kind and nature of the material in each stratum penetrated, with at least one entJy for each
change of information.
MATERIAL
FROM TO
-. 49
ij
Ü B6
'11 .-~ 1 ~,?
00 u_
102 145
145 189
189 309
309 330
330 342
342 349
34S· 390
3JC .JC2
402 417
;117 1~::2
42~:' ~12~)
4'·::6 ~3ò
in.
ft.
It.
ft.
Br~~/."n cla'lt:cun:I.:rr:1v31
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Br~¡n clav:X)u~j qr~v~l
Brown silty sand Z. '.:11:3.v21 .
LJOse b"cc-v.'l1 sand. Pt. ;1 rave 1
Gray tlarÒ:¡..:l;."1
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3t'c;m ht~rd~1\l
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,
WorllStarled ::/.IÆ~/'#¡ 19. Completed i.lIV~ D 19
WELL CONSTRUCTOR CERTIFICATION:
I constructed and/or accept responsibility 'for construction of this well, and its
compliance with all Washington well construction standards. Materials used and
the information reported above are true to my best knowledge and belief.
NAME
'~:n~sha¡lI .!",ell L.1;illi:¡lj, l.o.c..
(PERSON. FIRM. OR CORPORATION) (lYPE OR PRIN'!]
.~:1 OS~·~;>¡ ~~iH:..3rle~:'3 R(5. ,.¿jOul:,:;-00,~:~;Þ..
~//-. /1~J'1--_
.' .,. (WEll DRILLER)
0161
)dJï-J
..
Address
..
(Signed)
Ucense No.
Contractor's -: ':': r' '7::" :(.\'\'~ t.:; ~:'
~~istration¿;;à¡:i;;~f:<'iá;i:i~j:~ -
3/14 /1(;"
.19_
Date
hrs.
hrs.
(U~O~~S~ETSIFNECESSAR~
Ecology C.. rtunity ~ Affirmative Action employer. For spe-
cial accommodation needs. contact the Water Resources Program at (206)
407-6600. The TOO number is (206) 407-6006.
o
, Aspectconsulting
, IN-DEPTH PERSPECTIVE
May 14, 2003
COpy
Mr. Anthony Pellecchia
WPA
911 Western Avenue, Suite 380
Seattle, Washington 98104
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I JEFFERSON COUNTY
LE.~..:'T. OF COWi1111JITY DEVElOÞMENT .
--.._-~- . _..J
Re: Porter Lane Property Well
Hydrogeologic Assessment
Project No. 021067-003-01
~,¡. 5\ß\O~
Dear Anthony:
This letter-report presents a hydrogeologic assessment pertaining to local grourid water
conditions near your property located at 513 Porter Lane, Port Townsend, Washington. It is
our understanding that a drinking water supply well located on your property is within a
1,000-foot radius ofa High Risk Seawater Intrusion Protection Zone (SIPZ), as classified by
Jefferson County. Jefferson County Department of Community Development has required that
a hydrogeologic assessment be submitted as part of your building permit application process
since your well is within the High Risk SIPZ. This letter-report is intended to meet the
requirement of a hydrogeologic assessment per the Jefferson County Unified Building Code
Section 3 - Land Use Districts, Section 3.6.5 Critical Aquifer Recharge Areas, (9) Well
Drilling, Land Division, and Building Permits in Seawater Intrusion Protection Zones, iv. C 3.
High Risk SIPZ Mandatory Actions.
In preparing this hydrogeologic assessment, we have reviewed the following material to base
our findings and conclusions:
·
Water Well Reports on file with the Washington Department of Ecology (Ecology).
On-site well yield test data. .
On-site well water quality data.
Jefferson County Unified Building Code.
Property Location Maps, Topography Maps.
Jefferson County Coastal Seawater Intrusion Policy and Ordinance.
Map of Seawater Intrusion Protection Zones, Eastern Jefferson County.
Ecology report on the Geology, water resources, and seawater intrusion assessment of
Marrowstone Island, Jefferson County, Washington.
WRIA 17 report on Groundwater Quality Data Summary for Water Resources Inventory
Area 17.
·
·
·
·
·
·
·
·
. 179 Mac/rone Lane North Bainbridge Island, WA 98110 Tel: (206) 780-9370 Fax' (206) 780~9438 www.aspectconsultin(J.r;orn
-----------
.'0' .-..-'1:1 .... .......:..... ',- II!.. ¡~
Mr. Anthony Pellecchia - WP A
May 14,2003
Project No. 020167-003-01
Project Description
The project is located on the north end of the Quimper Peninsula, approximately 4 to .š miles
west of downtown Port Townsend, Washington (Attachment 1). The Pellecchia Property
(Parcel Number 001063007) is located at 513 Porter Lane and is a high-bank rectangular lot of
approximately 6 acres which abuts the Strait of Juan De Fuca to the north. The southern end of
the Pellecchia Property borders the McLaughlin Property (Parcel Number 001063003).
Attachment 2 is a parcel map that shows the layout of the Pellecchia Property to the
McLaughlin Property. Review ofthe United States Geological Survey 1 :24000 Port Townsend
South topographic map indicates that both the Pellecchia and McLaughlin property are at an
approximate elevation of 160 feet.
A water supply well located on the McLaughlin Property has had a chloride reading greater
than 200 parts per million (ppm). A water quality data report obtained :ITom Jefferson County
for a water sample collected on November 2, 2000 from the McLaughlin well indicates a
chloride level of326 ppm (Attachment 3). As a result ofthe elevated chloride reading, a High
Risk SIPZ surrounding the McLaughlin well has been established by Jefferson County. A
High Risk SIPZ extends in a 1,000-foot radius from any individual well that exhibits a chloride
reading of200 ppm or greater. The McLaughlin well is the only well on the northern portion
of the Quimper Peninsula that is classified as a High Risk SIPZ, which indicates a very
localized condition.
The Pellecchia Property water supply well was installed on November 8, 2001 (prior to Mr.
Pellecchia's purchase of property) and is located near the western property boundary over 400
feet :ITom the shoreline. The well is approximately situated between 835 to 840 feet from the
McLaughlin well (Attachment 4). As a result, the Pellecchia well lies within the High Risk
SIPZ and requires the development of a hydrogeologic assessment as per the mandatory
actions identified in the Jefferson County Unified Development Code.
Hydrogeologic Assessment
Well Log Information
Water Well Reports on file with Ecology were obtained and reviewed for both the Pellecchia
well and the McLaughlin well. The Pellecchia well and McLaughlin well were originally
recorded with Ecology as Kalalin Degroot and John Cahill, as the respective well owners at the
time of well completion. Copies of the well logs are presented as Attachment 5. A summary
of well completion data contained in the well logs is presented in Table 1. The well logs
indicate that the Pellecchia well is completed in a shallow water-bearing sand horizon
(aquifer), which was encountered between 154 feet and 159 feet below ground surface and is 5
feet thick. The McLaughlin well is screened between a depth of251 and 256 feet below
ground surface in a deep water-bearing sand horizon, which is about 97 feet deeper than the
Pellecchia well. A thick sequence of clay encountered at the McLaughlin well between 135
feet and 247 feet appears to develop a confined aquifer condition at this well location. The
confined aquifer condition is further supported by the fact that the static ground water surface
is at a higher elevation than the top of the water-bearing sand horizon. A cross section
completed between the McLaughlin well and the Pellecchia well projected out to sea level is
presented as Attachment 6. The cross section indicates that the Pellecchia well and the
McLaughlin well are completed in distinct, shallow and deeper water-bearing sand zones,
Page 2
Mr. Anthony Pellecchia - WP A
May 14,2003
Project No. 020167-003-01
respectively, that appears to be separated by a low penneability clay horizon. Ground water
elevation and water quality data further support the two separate ground water zones.
Ground Water Elevation
Ground water flows from areas of high head (elevation) to areas oflow head. Ground water in
the project area is thought to be flowing in a northerly direction and discharging into the Strait
of Juan De Fuca. Static ground water level data collected at the time of well completion
indicate a ground water level elevation of22 feet and 5 feet, relative to mean sea level, for the
Pellecchia and McLaughlin wells, respectively. The data indicate that the Pellecchia water
level is about 17 feet higher in elevation than at the McLaughlin well. This water level data
indicate that the wells are completed in two different zones. If the wells were completed in the
same water-bearing horizon, the McLaughlin well, which is located south or upgradient of the
Pellecchia well, would have a higher ground water elevation.
Water Quality Data
Seawater intrusion can be evaluated by collecting water quality data at a well and perfonning
measurements for chloride. Ground water aquifers in direct hydraulic continuity to the sea will
typically contain both freshwater and saltwater. The freshwater, which is a lower density than
the saltwater, will float on top ofthe denser saltwater. A mixing zone between the freshwater
and saltwater occurs as a result of hydrodynamic dispersion. This mixing zone typically
separates natural background freshwater (chloride levels typically <50 parts per million or
mg/l) from saltwater (chloride levels on the order of 19,000 mg/l) (Pacific Groundwater Group
& Parametrix, 2000).
Conductivity is a measure of the ability of water to conduct electricity and is measured in units
ofmicromohs per centimeter (µmohs/cm) at 25 degrees Centigrade. Conductivity can be
easily measured with field monitoring equipment and provides a good field tool for evaluating
the relative level of dissolved compounds, such as chloride, in ground water.
Chloride and conductivity has been analyzed at both the Pellecchia well and McLaughlin well
and are summarized in the following table.
Well Sample Date Conductivity Chloride (mg/l)
(µ.mhos/cm)
Pellecchia 11/5/2002 705 47.1
McLaughlin 11/2/2000 1870 326
The Pellecchia chloride sample was collected on 11/5/2002, upon completion of a well yield
pump test after approximately 2.4 hours of pumping after a total withdrawal of307 gallons of
water pumped from the well. Conductivity was measured in the field throughout the well yield
test and stabilized after 100 minutes of pumping at a level around 700 µmhos/cm. The
chloride level of 47.1 mg/l is within the range of concentrations for natural freshwater
background and does not indicate seawater intrusion.
The sample collected at the McLaughlin well on 11/2/2000 contained chloride at 326 mg/l and
conductivity at 1870 µmhos/cm. This level of chloride would indicate that saltwater intrusion
Page 3
Mr. Anthony Pellecchia - WP A
May 14,2003
Project No. 020167-003-01
is at an advanced stage in the deeper water-bearing sand zone that this well is completed in.
However, it is unclear, based on information reviewed for this report, as to how much water
was pumped or purged from the McLaughlin well prior to sample collection. Additional
ground water samples analyzed for chloride are necessary to evaluate any trend in water
quality data and confirm with certainty that seawater intrusion is occurring at this well
location. In our opinion, one single water quality sample does not form enough of a historical
data set to establish a High Risk SIPZ and its implications regarding surrounding land use.
The chloride data is another line of evidence that supports the fact that the Pellecchia well and
the McLaughlin well are completed in different water-bearing zones. If the wells were
completed in the same groundwater system the Pellecchia well should exhibit an equal or
higher chloride concentration since the well is completed closer to·the sea than the McLaughlin
well. It appears that the upper sand horizon that the Pellecchia well is completed in contains a
much greater amount of freshwater. Chloride concentrations in ground water in the upper sand
horizon is within the range of naturally occurring background levels for freshwater.
Well Water Flow Test Data
A well water flow test on the Pellecchia well was conducted on 11/512002 by Peterson Pump
and Water Treatment (Peterson) of Port Hadlock, Washington. The well is outfitted with a
variable speed Grundfos pump with an above ground flow controller. The well was pumped at
variable flow rates ranging between 1.75 and 3.5 gallons per minute (gpm) for a total period of
pumping of 145 minutes or 2.4 hours. Ground water level drawdown measurements, flow
measurements and conductivity measurements were recorded throughout the test. Attachment
7 contains the flow test data collected by Peterson. A graphical plot of the flow test data
showing drawdown at different pumping rates and conductivity reading for the duration of
pumping is shown in Attachment 8.
The flow test indicates that the well is capable of producing about 3 gpm with a stabilized
drawdown at about 21 feet. As mentioned above, the conductivity readings also stabilized
during the 3 gpm pumping interval at about 700 µmhos/cm. The conductivity reading
collected throughout pumping do not show an increasing trend as would be expected if
saltwater intrusion was occurring.
Based on information obtained during well testing, a distance to the seaward or downgradient
stagnation point (area in the ground water flow field at which ground water is not moving
towards the well) can be calculated from the following equation (EPA, 1993):
- Q
X --
L 27rKbi
Where: XL = Downgradient distance to stagnation point
Q = Pumping rate (gpm) = 3 gpm
Kb = Hydraulic Conductivity x Aquifer Thickness = Transmissivity (gpdlft)
Estimate T based on specific capacity (obtained by dividing pumping rate, Q
by drawdown, s (Q/s = 3 gpm/21 feet = 0.14 gpm/ft)
Page 4
Mr. Anthony Pellecchia - WP A
May 14, 2003
Project No. 020167-003-01
T = 1500x Q/s (unconfined aquifer) (Driscoll, 1986) = 210 gpdlft
i = Ground water gradient (unitless) = Ground water height above sea level/distance to
shoreline from well = 25 ft / 420 ft = 0.06
XL=
(3 gpm)(1440 minlday) 55
~ feet
2(3.1416) (210 gpd/ft) (0.06)
The results of this analysis suggests that the Pellecchia well pumping at a rate of 3 gpm will
draw ground water from the. down gradient or seaward side at a distance of 55 feet from the
well. This indicates that the well will not draw in seawater and leaves about a 365-foot buffer
between the sea and the downgradient area of influence of the well.
Conclusions
The following conclusions are developed based on a review of the available hydrogeologic
data:
1. The Pellecchia well is completed in a shallow water-bearing sand horizon which does not
appear to be connected to the zone that contributes ground water to the McLaughlin well.
A thick sequence of clay appears to provide a natural barrier that separates the shallow and
deep sand horizons.
2. Chloride and conductivity measurements collected from the Pellecchia well indicate a fresh
ground water source that is within the range of naturally occurring background.
3. The Pellecchia well appears to be able to sustain a pumping rate of 3 gpm and at that rate
the downgradient radius of influence would not extend to the sea.
4. An approximate 365-foot buffer exists between the downgradient radius of influence ofthe
Pellecchia well and the sea.
5. A variable speed pump is installed in the Pellecchia well and could be adjusted to a lower
flow rate if future water quality readings warrant an adjustment.
6. A 1,000-gallon storage tank will be installed in the Pellecchia water system which will
allow for adequate storage and limit the overall pumping of the well.
7. The Pellecchia development plan intends to infiltrate stonn water in an area between the
well and the sea which will further protect the shallow water-bearing horizon from
seawater intrusion.
Based on the data available for review, it appears that there is reasonable probability that
pumping at the Pellecchia well will not cause further degradation to the deeper zone supplying
water to the McLaughlin well.
Page 5
Mr. Anthony Pellecchia - WP A
May 14,2003
Project No. 020167-003-01
References
Driscoll, Fletcher G., 1986, Groundwater and Wells, Johnson Division.
Environmental Protection Agency, February 1993, Wellhead Protection: A Guide for Small
Communities, EP A/625/R-93/002.
Pacific Groundwater Group and Parametrix, Inc., June 2000, Groundwater Quality Data
Summary for Water Resources Inventory Area 17, prepared for Water Resources Inventory
Area 17 Planning Unit.
Limitations
Work for this project was performed and this report prepared in accordance with generally
accepted professional practices for the nature and conditions of work completed in the same or
similar localities, at the time the work was performed. It is intended for the exclusive use of
Anthony Pellecchia for specific application to the referenced property. This report does not
represent a legal opinion. Within the limitations of scope, schedule and budg~t, our services
have been performed in accordance with generally accepted hydrogeology practices in effect in
this area at the time our report was prepared. No other warranty, expressed or implied, is
made. The statements presented in this letter-report were developed based on data readily
available or provided by Anthony Pellecchia for my review.
Page 6
Mr. Anthony Pellecchia - WP A
May 14,2003
I
Project No. 020167-003-01
If you have any questions regarding information contained in this report, please do not hesitate
to call me at (206) 780-9370.
Sincerely,
Aspect consulting, LLC
~~LHG
Associate Geologist
jstrunk@aspectconsulting.com
Attachments: Table 1- Well Records
Attachment 1 - Location Map
Attachment 2 - Parcel Map
Attachment 3 - Water Quality Reports
Attachment 4 - Distance from Pellecchia Well to McLaughlin Well Map
Attachment 5- Well Logs
Attachment 6 - Cross Section
Attachment 7 - Flow Test Data
Attachment 8 - Pump Test and Conductivity Measurement Graph
W:\020167 Porter Lane Well\020167-003-01 Hydrogeo Letter.doc
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WATER 'WELL REPORT
STATE OF 'WASDJNG'fON
Pennit No. .... ..... __.._.._._.__
(1) OWNER: Narne.
(Z) LOCATION OF WELL:
Bearing and distance from sectJon or subdivwon corner
(3) PROPOSED USE: Domestic I;Y1"ndustrlal 0 ' Mwùcl¡)aI 0
Irrigation 0 Test WeU 0 other 0
(4) TYPE OF WORK: a~e~;~"Îh~~e)~ ~~_..__.____.
New weD flY' Method: Dug 0 Bored 0
Det!pened 0 ' Cable 8'" Driven 0
Reconditioned. 0 Rotary 0 Je"ed 0
(5) DIMENSIQ~S. Diameter of weD __...fP-..~1nr:hes.
Drilled.._a::L~~_.J:L Depth of completed wen_~_ _ _-ft.
,
(6) CONSTRUCTION I1ETAILS:
Casing installed: _W:..... Diam. from ..CL. 1t. to ~.S1 ft.
Tbreaded 0 .---!' Dlam. from ____ tt. to __ ft.
Welded V"' __" Diam. from .._._' ft. to __ ft. '
Perforations: Yes 0 No,~
Type of perforator used-.___.~___.._._,
SIZE of perforations tn. by _____ tn.
____.__ perfOrlltlOtlS from ._..___. ft. to ___ ft.
_.____ perforations from __.___ ft. to _._ ft.
____ __. perfOrlltlons from _____ ft. to ___ ft.
Screens: Yes e--No 0 ~ I ~.. . '"\
J.fanufJl.!'t~~~amr-~·.~.()~r.:¿__
Type_~_b...Le:;;_.S-_ Model No__
, Dlam.. --¡-,~- Slot size -__. from ~. ft. to -<-r.. 1t.
Dlarn. ~_ Slot size -.LL\=.,1romøí~~. ft. to~....:L\p:tt.
Gravel packed: Yes 0 No ¡;v"'" Size of gravel: _..____
Gavel placed :trom ______.._ It. to .....___..._._ fl..
Surface seal: Yes VNqO_ To what d,\~? .._.lY___ ft.
Material used in Sea1_...~~h-\.3;...~...._._.____
Did any strata contain unusable water? Yes 0 No
Type of water?________.___ ne¡)Ih-,of strata.......__..__
Method of sealtn¡¡ strata oft._.___.....__.._._._._._.._.~_
(7) PUMP: ManuIactu...r's Name___.....:.-......-____..__._._...
Type: ..._.._.________.___.._.___ K.P_._.._..
(8) W' "'TER LEVELS" Land-surface elevation
n. , above mean sea level... '-'4-
StaUc level _.l..s:..s:"__--ft. below top ol!'Bi1 Dat~~.~.L.-
Artesian pressure _____.._.__.lbs. per square Inch Date_._.__.____...
Artesian water is controUed by_.._...__.__._.._.._.___...____
(Cap, valve, etc.)
(9) WELL TESTS: Z:~~~l~~~~~tl:a';ler level is
Was a pump test made? Yes "NO ¡¡v'"U yes, by whom?_..._...._._.....__....
YJeld: gal./mJn. with ft. drawtlown after hts.
Recovery data (time taken as zero when pump turned off) (water level
measured trom weD top to water level)
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Ball~:~es:~jß;=:.~~~:ï;;;;n. with_{;l5-~~;. dra~own a!teroI..,.,...-._hrs.
Artesian fiow_.____.______g.P.m. Date..L.~Q.~. ._.I.___~_
Temperature ot water_.__ WØß a chemlcnl ana1ysls made? Yes 0 No
(10) WELL LOG:
Formation: Describe by colen'. charucter. me 01 matfl1'ia! IZItd $tTUcture, one!
shOw Chickne,,:r of aqutlen <me! the /ci1ld and nature of tbe ma&eriøl i3 each
ðtratum pB7U!Þ'a&ec!, ,.,{th at least one rntr¡¡ for each c/lcmge of fonnation.
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Work started...~~g,X... 19.9~g comPleted~g....r::t 1s83
WELL DRILLER'S STATEMENT:
This well was drilled under my jurisdiction and this report is
true to the best of my knowledge and belief.
_ I I. ~. A ~ "
NAME.MQ.t......Wl..t\l~A (S..._~....:o;..LLI.~.
. (Pet'SOn. firm.LJ~"~oration) (Type or print)
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. License No......5..~_~_..._.........:.. DatdLd.m€....~.., 19f.3
ECY 050-'-20
(USE ADDrrIONAL SBEE'l'S IF NEC1i:SSARY)
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, ~ PETERSON PUMP & WATiR TREATMENT.INC
PO BOX 1110, t0712 RHODY DRIVE
PORT HAOLO<:K. WA N339-1110
360..315.:1.&37 Ix: 385-'1T4
c;_ LI~!JUlTMtkIl
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;1 NAME; ..J"O~~ ~~ANAt+AN UNIQUE WELL IDJI AGe. ~17
~ LOC~TION: ~E;t ~ PoRt TðLù~SS').JD WA. G\ß%8 ¡ ':Jy . - I S9'
WELL DEPTH; 110 .STATIC: 1~5'-~" . SCREEN': YEo:;;
ORlLLER: W1t.1.IAI'W)S
¡ RE: WILL WATER flOW TEST
'I
TIME STATIC DRAWDOWN GPM COMMENTS
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Pump Test
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Pump Test conducted on 11/5/02 by Marty Peterson of Peterson Pump & Water Treatment, Inc.
Well Depth 170 feet
Static Ground Water Level 135.25 feet
Well Screen 154 - 159 feet
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Jefferson County Deoartment of CommunitY DeveloDment
621 Sheridan St. Port Townsend WA 98368. (360) 379-4450
APPLICATION FOR
DETERMINATION OF ADEQUATE POTABLE WATER SUPPLY
Resolution #99-90 requires building penolt applicants to provide evidence of an adequate potable water supply,
Name AW,-KC»M '( Pe.c..c...~"UA Phone ~O(Ö · ~ 1& ~ ·O~-O
Mailing
Address~t.t. F-e.ÞE£A~ A,V'J!.,/e.:¡c¡,EA1TLE wa.. ZipCode-9 e (Ø~
Parcel
1D#J2.e.J D~!» CO"7 Subdiv. Block Lot(s)
Site
Address 6"1~ PO.e:re.e l-A"-1E I PÐ~ T<D\AI~'s;.N1> I W.A. ZipCode~B~<óa
Type of Structure OtIJE. ~TcølLl ~I~L..I!. F-AMtL.'f ~E.c¡.., ØaNC,e.
TVDØ of Evidence (check one)
Type of Structure
Valid Water RIght Pennlt (attach copy) . , . ... .. h_ _
Approved Public Wa~r (Submit the attached Water Availability Notification'fç)~ c9m~teq..,by;~õu,~.r;'purvpyor
stating the system is capable of and will supply water.) , ;.;' . ::..~; ~,' _.'¿ ~-,~Y- : 2 It·,
~ Individual Well-attach copy of: .' ! . ~.~ -¡ ;; :'
1) Well logs (~f no well log re~rt is on file, a 2 hr pump test result may; ~ ~bstituted) - 8 ; : :
2) Lab analySIS for water quality parameters: ! ~ -MAT 2003,
-Total coliform ' ,
-Nitrate-N -''''- J
-Chloride and/or Sodium '. '¡' .
3) Plot plan showing location of well with respect to proposed sewage system, buildings.'drtveways and
surrounding properties. --
Two-party Well-items above AND recorded Operation & Maintenance agreement and recorded Easement
By signing the application form, the applicant/owner attests that the Information provided herein is true and correct to the best of their knowledge. Any
material falsehood or any omission of a material fact made by the applicant/owner with respect to this application packet may result in this permit being
null and void.
I further agree to save. indemnify and hold harmless Jefferson County against all I~bllities, judgments, court costs, reasonable attomey's fees and
expenses which may In any way accrue against Jefferson County as a result of or in consequence of the granting of this permit.
I further agree to provide access and right of entry to Jefferson County and it's employees, representatives or agents for the purpose of application
review and any required later inspections. Access and right of entry to the applicanfs property or strudure shall be requested and shan occur during
regular business hours. . ~' ,
Signature Å- -;-1 __~,GC,~ Date ~ · 1· t9 'Þ
H:\HOME\PLN~\NATERREV1102
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'lh'CoroPl~hôe Yè$ 'NÄ
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Individual Well . .' ,
=~ .. · . ... '.. ........ .. , ',. =~ ,.1':;~"¿<f¡~:t£~~4
M~tsWàterQualitýstÆindøfds' v. -NQ .····;:{:\:l~~
BaSeduponJÒfo,(I11.qtjØn\wovjde(fþYthèapPlica.nÌ;jtapP¢ars.thatthe,pot$blew~i~~:~Þ~: . \.,' ,
~m~Þ . ~', ,../~ndi.tjQn~'lymeets ..;.....-.d~~ot.tnt~l, x . ~.'
ÖlØ'GO~itiQJ1$of RCW1,a.27 .0.91 and the, G.i.ii(:JÈJliiiøs for Determining WaterAvªilªbilityfQrl?Ii~J~JJÌ!ÎIçf!PiJ$.
D¡te ~7í~iJ~'R;:rs.~~CDRéCe.¡PÙ#6~/7 Check # '1993 5 Ca~ #~L()Ì;'~'- ¿J9b
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1\, (..t,r øKI
REQUIRED) 1..0.'11I8 Dcg Lon. MinlSoc _
TD Partel No. CD' ()I; 3~?
DI&III. f,ulII :åE. t\ b. IsL CONSTItUCTlON Ok DECOMMJISION ~IbUU
, ! 10 J!:!:l;;' ,~ l>«cribe by co!«. cUrac1cr. lbe 0( matcNI ad SCNCOII"C. M4
..... ... ,', ....... ......r........ """"".. "'_...... _..0......_
DiaIIL f'olll . It 10 ~. aay for Itcb cb.t.Dte -.>f iAt'ormatiocI. IIIdicuc .n waltf ncOlllllteted.
US!! ADDITIONAL SHŒrs IP NECI!SSARY.)
MA TaRIA.L PROM
.WATER WELL REPqR~
('~·'i·t,;.rï'l on..... lat copy. I!cðIOSy. 2c4 "'pr - o*act. ~rd .., . driller
~"'~"","(·Jt·ÍII('VtW
0""'CaosIrucd<:ll
o ÐeconImission ORJGlN.4L CONSTRUÇTfON NtHÌC'~
InIUIl NIIIftber
K '''ac.¡ Lpçaåon
, "~r
MockISo, '
Slot $i.u from -rs; ¿./, ft. a<> J S 'I n.
_SIoI Si2e tJo:a ft. 10 ft.
ç""df1IUttt peclwcl: 0 Yes . 0 0 Siu of 1f'a>'Clltand ¡
MAIeNb aced from ft. 10 --L--__ _._n.
s.rr.œ SaI: t& 0 No To wIw. ~Ih? ft
Malf:fUlJ II&ed Íft IUI l!!., ,., fnn" '1-<-
Did any IWata c:ontai~ U'-blc waler? OYel ~
Typr or watet? _De¡Ø or.nta
...~ 0( seali. ,1UUI off
PUMP, M-.factwu'J NII1Ie
Typr: ftP~
W 4TER UVJ:t$"~':llUÍa<:e devalÌ01l abovc _ s.¡ue~ n
SIR.: Itvd L-£~ n. below lop of ~II Date~...l21-
An.eØc prCUIØC Ibs. per JqIllß iach Dale
AItesiaD waa ia COAlroUcd by
WELL TESTS: Drawdo"'n i, "'*'" level illowaed belJw IWic IeIlCI.
W.. a P\IIIIP teJll1\&de? 0 V CI Nt> If yes. b)' wbom?
VielcI:---flJJlNa. wid\ ft. cbwdwa eftcr IllS,
YlC'lcI:----.aIl.llDia. ...~ ft. cIra".fbooa after !Irs.
Yield: ---,IIJmia. willi ft. dnI..........ftet 1In.
If,{'.~" IÚItI fd_ laè,.. G" tC'1'O ....vII ptInIp """.J n/TX"'Øk, U'~l_."",,¿ 1_
_,U tIØp iii _, II.,,}
Ti_ Watu Lc"C1 Tillie WIIU Level Time WICet La-el
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tJniquC £cotolY Wdl ft>Taa No.
WtItCt Right hnuit No.
ProsIcrty Owner Name k~ /~ I ;11 ~h:Øf
Well SInXt AddIas tor~Pðl"'''~~' ~ .>
CiI7·/.brfT~t:J.~ CouDty: ~,
~~lll.114. 1'4 I/~ ~ 1'-!2.. ,jJJ~ r;:'-
WWM
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PETERSON PUM~ & WATER TREATMENT,INC
PO BOX 111~, 10712 RHODY DRIVE
PORT HAO:L()ÇK, WI.. H339-U10
360.315+~37 tx: 315-8114
Co"" LI~E'fIAPTMlKa
[1edI COfttr ~e w." LIef NT!IU'T"7A1
DATIE: -1' - 5 ·02-
NAME: .:rO~~SmANAHAN UNIQUEWELLID' AGe. '517
LOCATION: 4tTER. L.N' PORT -nWNSENþ WA. q~~s
WELL DEPTH: '70 STATIC: I 35'-f>" . SCREEN: Y£S .,:)'i'-'S<-i'
DRILLER: W'(.L,AMS
RE: WELL WATER FLOW TEST
TIME STATIC DRAWDOWN GP .1 COMMENTS
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TWISS AltlAL'VTICAl LABOItA TORIES, INC,
lfllW TwtlV\I Tree. &....t. s..-C IPou",.. WA 91)71) TdqIIIa.c (3IiO) m.sl.' .AX UOO) 7~~.~
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INOR.GA~.C CHEMICALS (lacs) RrPORT
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1'011 Hadlock. W A 98339
'n\-:at.
01011270
1 1/6102
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~ 26280 Twetve TI!8es,LAne. Suite C
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: (søO)-7i~51.41 \
:. ' WATER'BACTE':=IÇAL'ANALYSlS""
'. SAMPlE COI.1.EC11()N¡ RE.6D , œaACK OF GOL.DENFœf;OPY
, If 1mJIruc:tIons'...nvt ~ wtn be
,- DATEOOl1.ECTED l1ME~, ~ NAME
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r: .1YPE OF SYSTEM ,IF PU8UC.SYSTE~..COMPI..&TE "..~~,., , ' ' .
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~~:,~;"'t_ :. '''T~,8':'' ,
"NAME OF SYSTEM
ftG<: 571
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EVENING ( )
SVSTEM OWNEAJMGR.: (NIIme) :."
;...~!~.
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o REPEAT SAMPLE
PI'8VÌOII$ coIiIDrm presence
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o Fec:\II CoIIfonn
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RESUlTS . w.
,I .Eo COU ---:..- 1100 mI
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TWISS ~ALYTICAL LABORATORIES, INC.
26280TwdveTResLane.SuiIeC PouIsbo,WA 98370 Tdcphone(3fíO)719-~141 FAX(36O)779-SI5Q
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INORGAJiIC CHEMICALS (lOCS) REPORT
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I County: Jefferson :
1·~~~f~~f¿~9-'-~::-=rmTO:~----
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DOH Source No:
-----.... ... . .
Salq>lcPwposc: '~iL'- . ..'
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--......-....
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MCLT
Exceeds
TrløerT MCLT
NOles:
SRL:
Trigger Level:
I ~
(State Reporting Level). indicates the mÙlimllßl 1Porting Im:l required by Ihc Wuhillßlon Department ofHeattb (OOH).
DOH DrInking Water response level. S)'&Ums~" ~unds deIected al c:oncentøtions in excess of this level are required 10 lake additional samples.
Contact)'Otlr tqioIIa1 DOH off'lCe for rurther ~tion.
(Maximum Conlalllinanl Uvel), lf1he contamlnatlamount exceeds the MCL, Immediately tÐRtact your regional D()H office.
(Not Analyzed), in the results column indicates Ibjs compound was not in<:ludcd in the CIIImIt analysis.
(Not Detected). in lite rcsuks c:oIumn indicates ~ compound was analyzed and not ckto;:tcd at a level greater than or equal to the SRL
indicates the compound was not dctcçtecl ÙI the sample at or above te concenlration indicated.
MCL:
NA:
ND:
< (0.001):
Co_als:
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MAY - 8 2003
Twiss Laboratory Number: 38071
Page ]
Map Output
Page lofl
001063007
0 legend
SøladGd FøaliUNs
0 Parœl!l-H
Oly of PT WSA
· ClIRRØT
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Water SølNloe AMes
· CU'n!ôI
· FlU';!
00100f'
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FOR INFORMATIONAL PURPOSES ONl -
efferson County does not attest to the a uracy of the data contained herein and makes no warranty with
espect to its correctness or validity. Data ntained in this map is limited by the method and accuracy of its
lIection. Fri Ma 16 16:27:25 2003
http:// gisserver/servletlcom.esri.esrima*.Esrimap?ServiceN ame=eh&ClientV ersion=3.1 &... 05/16/2003
Map Output
Page 1 of 1
Legend
SeIeded Features
Pi\KCØISrH
2000 Shorelne Photo8-H
SIPZ
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. Hi(#IRiIk SI'Z
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.
FOR INFORMATIONAL PURPOSES ONL y-
efferson County does not attest to the accuracy of the data contained herein and makes no warranty with
espect to its correctness or validity. Data contained in this map is limited by the method and accuracy of its
lIection. Thu Ma 08 15:07:43 2003
http://gisserver/servletlcom.esri.esrimap.Esrimap ?ServiceName=Critical_ Areas&ClientV... 05/08/2003
JEFFERSON COUNTY
DEPARTMENT OF COMMUNITY DEVELOPMENT
621 Sheridan Street
Port Townsend, WA 98368
AI Scalf, Director
FAXTRANSMIITAL
DATE:
Mt)3
TO: ~..... Þ~t
PHONE: (ZÐto) 2.~~... cS"ra
FAX: (~~ 7~'t~ - O(OCo~
NUMBER OF PAGES including cover: 4>
FROM: ~~ Ito~N~
JEFFERSON COUNTY COMMUNITI DEVELOPMENT
-
PHONE: (360) 379-4450
FAX: (360) 379-4473
"
SUBJECT: ~~'\' PM-c...a...~ ~ IN~,
COMMENTS:
Building Permits/ Inspections
(360) 379-4450
Development Review Division
Long Range Planning
FAX: (360) 379-4451
~ liYi~~
26280 Twelve Trees Lane, Suite C
Poulsbo, Washington 98370
WATER BACTERIOLOGICAL ANALYSIS
SAMPLE COlLECTION: READ INSTRUCTIONS ON BACK OF GOLDENROD COpy
If Instructions are not followed, sample wIll be rejected.
DATE COLLECTED TIME COLLECTED COUNTY NAME
MONTH DAY YEAR -E-: $ð
/1 / tJ Z- ¡hØ~ J ef,.ø~IL$oc/
FlAM OPM
TYPE OF SYSTEM IF PUBLIC SYSTEM, COMPLETE
o PUBLIC II.D.NO·'lliJIIJ
~ INDIVIDUAL CIRCLE GROUP
(serves only 1 residence) A B
NAME OF SYSTEM
.-If ( ¿ ). " (: " ¿, , ,.J
....
SPECIFIC LOCATION WHERE SAMPLE COLLECTED
z..1 er-, II /I$'-,/ 1,",6-$ .o"¡,f' tV
fø ^-'C '1 þi.U ¡V Sðt Nt? , .....Þ/'r
tfðJt.€ f/¡'1!7 S.S'I'J:
SAMPLE COLLECTED BY: (Name)
TELEPHONE NO.
DAY (Zttl,)Q5z.. - 51:.4(f
A A.1 ,Aj (,.l/;!fL. e /-I
EVENING (2"'-)"1 ~ z. - <r;: {. 4f
SYSTEM OWNERlMGR.: (Name)
ðAlA-ø.J U,t"LAq<.-.. t-ltJ
-j
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SOURCE TYPE 0 GROUND WATER UNDER SURFACE INFLUENCE j
o SURFACE gt WELL or 0 SPRING 0 PURCHASED or 0 COt;1BINATION
WElL FIELD INTERTlE ~ OTHER .....'
SEND REPORT TO: (Print Full Name. Address and Zip Code) ~
j
:~
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o REPEAT SAMPLE
Previous coliform presence
o RAW SOURCE WATER Source #
o NEW CONSTRUCTION or REPAIRS
o OTHER (Specify)
REMARKS:
(LAB USE ONLY) DRINKING WATER RESULTS
o UNSATISFACTORY, Coliforms present ~A~ISFACTORY.
Cohforms absent
: ~'
:'"
REPEAT
SAMPLES
REQUIRED
o E. Coli present
o E. Coli absent
REMARKS
:1
'~
SAMPLE NOT TESTE" BECAUSE. TEST UNSUITABLE BECAUSE..!...·.'..'..
o Samples too old 0 Confluent growth
o Wrong container 0 TNTC
o Incomplete form 0 Turbid culture j
o 0 Excess debris i
SEE REVERSE SIDE OF GREEN COPY FOR EXPLANATION OF RESULTS ~,J
LAB NO. (7 DIGITS) DAT'T T!Þ'1E RECEIVED RECEIVED BY].
010 (;2ð'(l lill/po /1:~¡1 #.6]
1
I
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1
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TOTAL COLIFORM
FECAL COLIFORM
o Fecal present 0 Fecal absent
OTHER LABORATORY RESULTS
/100 ml E. COLI
/100 ml PLATE COUNT
ANOTHER SAMPLE REQUIRED
1100 ml
Iml
DATE REP9RTED
II ':J ({fill
WATFR !=:IIPPI IFR r,()PV
JA~-23-2001 04:32 PM
. I. ~. .,¡ '" ! : 1: .. ..... .
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BROTHERS PLUMBING. INC.
360 683 7719
P.02
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Phone a85-2OOI
JJ(Q)~ o~(Q)a~~
22090
"7-2.o,,- DA':rJ_ z,oø~
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BROIHER'S PLUMBING, INC.
~ In PlumbIng a. PumPs
ROo Box 1048
PORTTONNSEND. WA 983S8
TO
RAJA>
339Coi
.:PC'^, ..,-
t,JtLc.h
J..I.A-I:. T~ :;( £J£S"'"
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o DAYW'ORK
o OONI'RACT
LJ EXTÅA
JOINtl.lElllI~
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--
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. TERMS: ~ _ .... .. III wItH. 10 ..,. fill J!! .1tll11It. ,...... lilt .... ..
... ...,. fill ~ ...... lie ~ at 1.1" .... ...... ...........
- ¡::-lo6lAJ 7;$T" ðN Wf, t..I- ~
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T~i- ¡,M-1U- t.....u...e- 1#' "" /'
to:øo 13~ 2.0 V Ir ~ ~~ ~ \VI rF Q
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1-
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,. : 60 ?-;.O 13
II~'$ p.;.o 13
11:30 ~o 13
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AG;fi ' \
Wt-LI., AJ_ 12 I~ wI' ^'~ \
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-
TOTAL 011iER .
> S~-o'1..rÎ - L/ï <;, --") ,^, IL ~
Ð&f 1 þ~ . I ,
f
\
\ t\( ,
~ ~ '. fJJ'
~ } IV ",'
(~ b\1' 1 v- ¡tV
\ I ~. _ to''J \' TOTAL LABOR /9'1 ~t:?
00\11: .,- I TOTAL MATERIALS
\\ TOTAL MATERJALS
TOTAL OTHER
Work 0fdeNd by ~9Jsw
SIgnature TAX If. K
.. . . . . --- ---"- -. -'-Io:.._...........a..-~ Io&MIIIr 010. ,,'
TOTAL
JA~~23-2001 04:31 PM BROTHERS PLUMBING. INC.
360 683 7719
P.01
!1m! W" Levef ~MInute
//):00 la" ;)0
10: IS I '() ¡;>o
/0: 30 ól.:l.Ø 13
t D: 'IS ~:lO "
" : ÞO :A:J..ø /3
fl : , S· 22.0 13
J ,: (So .;). -0 I 3
*Needs ID be done for one ~Iized hour (at . GOnStant waœr level)
*Can be taken in 15 or 30 minute incæments
If you have any question 8nd 8Ie In JefI'enson County call (');M, Christianson 385-9418.
fõ) [E ~ [E ~ \Yl [E fñ\
Uìl JAN 2 4 2001 lW
JEFFERSON COUNTY
DEPT. OF COMMUNITY DEVELOPMENT
TWISS ANALYTICAL LABORATORIES, INC.
26280 Twelve Trees Lane, Suite C PouJsbo. W A 98370 Telcphooc (360) 779-5141 FAX (360) 779-5150
INORGANIC CHEMICALS (IOCS) REPORT FOR NITRATES
System ID No: Private
LablSample No: 010S4864
Multiple Sources:
Date Received: In,S/01
System Name:
Date Collected:
Sample 1)rpe:
Date Reported:
Date Analyzed:
Ann Welch
In,S/01
D
1n,9/0 1
1n,6/01
DOH Source No:
Sample Purpose:
Supervisor: ,
Analyst:
Group:
C
ST
MP
>.~.~:,,'~' .~~. ~~~;~~·~::;:::j.~::~~.:~q~Ii:;'~··~ ~;~~~~~.:. ~~~~"~~1~
County: Jefferson
Sample Location: Outside Faucet
Send Report To: Ann Welch
" 2108 42nd Ave SW
Seattle. WA 98116
Bill To:
Notes:
SRL:
Trigger Level:
(State Reporting Level). indicates the minimum reporting level required by the Washington Department ofHea1th (DOH).
DOH Drinking Water response level Systems with compounds detec:ted at concentrations in excess of this level are required to take additiooa1 samples. Contact
your regiooal DOH office for further information.
(Maximum Contaminant Level), If the contaminant amount exceeds the MCL, immediately contact your regional DOH office.
(Not Ana1yzed). in the resu1ts column indicates this compound was not included in the cwrent analysis.
(Not Detected), in the results column indicates this compound was analyzed and not detected at a level greater than or equal to the SRL
indicates the compound was not detected in die sample at or above the ,concentration indicated.
MCL:
NA:
ND:
< (0.001):
CoJllßlellts:
lfõ) lE (C IE ø WI lê ~
II11 JAN 3 t.. /!!J
DEPT. OFJEFFERSON COUNTY
. COMMUNITY~NT
Twiss Laboratory Number: 27689
Page 1
TWISS ANAL YTIÇAL LABORATORIES, INC,
26280 Twelve Trees Lane, Suite C Poulsbo, W A 98370 Telephone (360) 779-5 141 FAX (360) 779-5150
INORGANIC CHEMICALS (IOCS) REPORT
System ID No: Private System Name: McLaugblin
Lab/Sample No: 01052042 Date Collected: 11/2/00 DOH Source No:
Multiple Sources: Sample Type: D Sample Purpose: C
Date Received: 11/2/00 Date Reported: 11/16/00 SupeIVisor: ST XA-
Date Prepared: I Date Analyzed: 11n/OO Analyst: MP \.....J
County: Jefferson Group:
Sample Location: 3394 Hastings Ave
Send Report To: Ann Welch Bill To:
21084200 Ave SW
Seattle, WA 98116
Exceeds
Trfuer7 MCL7
21 Chloride 326 mgIL 20 250 250 Yes Yes SM 4500-CI B MP
8 Iron 0.2 mgIL 0.1 0.3 0.3 SM3500-FeB NP
10 Manganese 0.04 mgIL 0.01 0.05 0.05 SM3500-Mn B NP
22 Sulfate 32 mgIL 10 250 250 SM4500-S04 E JCS
Tricler7 MCL7
Yes Yes
Yes Yes
Trfuer7 MCL7
Notes:
SRL:
Trigger Level:
MCL:
NA:
ND:
< (0.001):
(State RcportiDg Level). indicates the minimum reporting level required by the Washington Departmeot ofHeaI1h (DOH).
DOH DrinIcing Waf« response leveL Systems with compounds detected at coocenuatioos in excess of this level arc required to take additional samples. Contact
your regiooal DOH office for further infonnation.
(Maximum CoIÞmi""nt Level). If the contaminant amount exceeds the MCL, immediately contact your regional DOH office.
(Not Analyzed), in the results column indicates this compound was not included in the CWTeIlt ana1ys~.
(Not Detected). in the results column indicates this compound was analyzed and not detected at a level greater than or equal to the SRL
indicates the compound was not detected in the sample at or above the concentration indicated.
Comments:
J.N3Wd013l\30 AJ.INOWWO~ :10 1d30
AlNnO:> NOS~3:U3r
~~;:;;~~
Twiss Laboratory Number: 26524
Page 1
--..
JEFFERSON COUNTY
DEPARTMENT OF COMMUNITY DEVELOPMENT
621 Sheridan Street
Port Townsend, WA 98368
AI Scalf, Director
FAXTRANSMITfAL
DATE:
5 },z..}03
TO: ~"þ~,
PHONE: Cl-0lq 2.'3'g- ðS"~
FAX: (?~) 2.~~ - OCOfo~
NUM:BER OF PAGES including cover: 3
FROM: ð1'f\c..t~ ~þ-t~ .~
JEFFERSON COUNTY COMMUNI1Y DEVELOPMENT
-
PHONE: (360) 379-4450
FAX: (360) 379-4473
SUBJECT: M~~ ~.-.A.c..£I. ~'t'£ ~\.M..\.
COMMENTS: ~ 8\1); 'lA.,\ Ibn.IT1f\a- "TIi-£' ~ A-'\ lbg f\:..~
~ ~ ~~ .p~C£L ~~~ .
Building Permits/ Inspections
(360) 379-4450
Development Review Division
Long Range Planning
FAX: (360) 379-4451
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- Parcel Print
Parcel Number: 001063003
Owner Mailing Address:
BRIAN D MC LAUGHUN
3394 HASTINGS AVE W
PORT TOWNSEND WA 983689200
Site Address:
3398 HASTINGS AVE W
PORT TOWNSEND 98368
Page 1 of 1
Section:
Qtr Section:
Township:
Range:
Mapped
Acreage:
Sub Division:
land Use Code: 1100 - HOUSES (single units, non-farm)
6 School District: Port Townsend (50)
SW1/4 Rre Dist: Cape George (6)
30N Tax Status: Taxable
1W Tax Code: 161
5.16 Planning area: Quimper (2)
Property Description:
56 T30 R1W
Nl/2 NE SE SW
http://www.co.jefferson.wa.us/assessors/parcellparcelprint.asp ?P ARCEL_NO=OO 1 063003
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JEFFERSON COUNTY
DEPT. OF COMMUNITY DEVELOPMENT
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o u-;d~~round Utility Connection
Elevation 95'
Brian Mclaughlin
3394- HastlngsA~. W.
Port Townsend,
WA98368
Parcel No.
001 063 003
Gross: acreaae:
Contact:
Ann Welch
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PACIFIC g 1'0 U 11 d \^/a te r GROUP
COpy
April 21, 2003
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Mr. Paul Marks
P.O. Box 63
Nordland, W A 98358
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Dear Mr. Marks,
This letter report presents our analysis of hydrogeologic conditions at the property listed
above on Marrowstone Island, Washington. Our anttlysis addresses "relevant
components of an Aquifer Recharge Area Report per UDC 3.6.lOe" as required by UDC
Groundwater Protection/Seawater Intrusion Amendments, March 3, 2003. Our
discussion with Jefferson County indicated that the "relevant components" were those
pertinent to exacerbating or causing seawater intrusion effects on neighboring wells
(personal communication, David Christensen, Jefferson County Division of Natural
Resources, 2003). Other components are not addressed in this report.
Our proposal of March 4, 2003 was authorized by Paul Marks on March 19, 2003. Our
work was performed, and this report prepared, in accordance with generally accepted
hydrogeologic practices at this time and place, for the exclusive use of Paul Marks, and
for exclusive application to the two primary wells on the subject property. This is in lieu
of other warranties, express or implied.
PropéÎty and Project Description
The Marks' property consists of about 8 acres on two parcels in the community of
Nordland on Marrowstone Island (Figure I). The property currently has the following
dwellings and water-use attributes:
· A two bedroom, one bath house (Johnson house) that is supplied off the dug well
· A one bedroom, one bath "cabin" that is supplied off the dug well
· A front parcel of about 3 acres (976200402), some of which is irrigated with
water from the dug well
· A back parcel of about 5 acres (976200501) that is grazed and not irrigated. Two
unused wells are located on this back parcel (wells ACC057 and ACC059).
P 206,329,0141 F 206,329,6968 I 2377 Easdake Avenue Easr I Searrle, Washingron 98102 I www.pgwg.com
\\';Hcr & environl11c:nral consul ring
The property is for sale and the prospective new owner proposes to make changes to the
dwellings that will require a building permit. Changes to the structures proposed by the
buyer are:
· Building a new two bedroom, 1.5-bath house on the front parcel that would be
supplied by the better of the two wells on the back parcel (well ACC059)
· Possibly moving the cabin to the back parcel and also supplying it off well
ACC059
· Maintaining the Johnson house as an "accessory dwelling", and maintaining the
water supply off of the dug well
If the cabin is moved, the total increase in bedrooms and baths on the combined parcels
will be 2 and 1.5, respectively (Table I). If the cabin is not retained, the total increase in
bedrooms and baths will be I and 0.5, respectively. '
As implied above, three wells exist on the two parcels. These wells, and other wells
located within about 1000 feet, are shown on Figure I. The Marks' wells are:
The dug well, which is located about 35 feet east of the Johnson house, is about 5 feet in
diameter and extends to 38 feet below land surface. It probably produces water from the
Qva aquifer with a water level about 10.6 feet below ground surface on April 3, 2003.
Access to the well is through a 5ft x 5ft x 605ft deep concrete vault which rises 2.5 feet
above ground surface. The concrete vault serves as' an (unconventional) surface seal
which penetrates into glacial till. The till extends to below water level. Elevation of the
top of the concrete vault is 2.5 feet above local ground surface. Ground surface elevation
was estimated to be between 20 and 25 feet above mean sea level based on LIDAR data
provided by the County. Based on that elevation, the bottom of the well is between 13
and 18 fe~t below mean sea level, and the water level elevation is between 8 and 14 feet
above mean sea level. That water level is unusually high for Marrowstone Island and
indicates unusually high groundwater storage near the well.
Well ACC059 was drilled in 1995 near the center of the back parcel. Its well log
(attached) indicates it is 54 feet deep, has a surface seal to 18 feet depth, and penetrates
30 feet of surface soil and glacial till. Water bearing sand and gravel of the Qva aquifer
was logged at 30 to 35 feet depth, and 44 to 50 feet depth. Bedrock was not encountered
within the drilled depth. The driller reported a water level 27 feet below ground in
Octoberl995. Water level in the well was 24.4 feet below the top of the steel casing
(2~.6 feet below ground) on April 3, 2003. The 6-inch casing rises 1.8 feet above ground
surface and is capped with a pitless adaptor, although no pump is in the weU. Elevation
of the top of the steel casing was estimated at 39 feet above mean sea level based on
LIDAR data provided by Jefferson County. Based on that elevation, the bottom of the
well is at about 17 feet below mean sea level, and the water level is 15 feet above mean
sea level. The water level elevation in ACC059 is ,similar tothaJ (}t'~tþe c¡lllg; well
suggesting hydraulic continuity, and unusually high g,roundW¡;tterstþtage \gc¿ÿ}y. t ': i
Page 2
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Well ACC059 was pump-tested in September 2000 by Bayview Pumps (see attachment).
A pumping rate of between 3.18 and 4.47 gallons per minute (gpm) was maintained tor 2
hours. Water level in the well declined from a static level of 23.5 feet below the
measuring point to stabilize near the bottom of the well at 54 feet below measuring point
after about 70 minutes of pumping. Although the well experienced complete drawdown,
a pumping rate of over 3 gpm was maintained for the last hour of the test. The test was
not analyzed further for this report. '
Well ACC057 was drilled in 1995 near the north end of the back parcel. Its well log
indicates it is 58 feet deep, has a surface seal to 18 feet depth, and penetrates 37 feet of
surface soil and glacial till. Water bearing sand and gravel of the Qva aquifer was logged
at 37 to 42 feet depth. Bedrock (gray sandstone) was logged from 45 to 58 feet depth.
The driller reported a water level at 25 feet below ground in October 1995. The well is
welded closed and no water level was measured in April 2003. The 6-inch casing rises
2.2 feet above ground surface. Elevation of the top of the stdel casing was estimated at
about 35 feet above sea level based on LIDAR data provided by the County. Based on
that elevation, bedrock in the well was encountered about 10 feet below mean sea level at
this location. The well log reports a well yield of 0.3 gpm.
Hydrogeology
The hydrogeology of Marrowstone Island has been extensively studied, most recently as
a result of seawater intrusion concerns. The following description of the hydrogeology in
the vicinity of the project is derived from tbe well logs discussed above, a recent
reconnaissance, and Geology, Water Resources, and Seawater Intrusion Assessment of
Marrowstone Island, Jefferson County, Washington, Washington State Department of
Ecology Water Supply Bulletin No. 59, by Kirk Sinclair and Robert Garrigues, 1994.
Marrowstone Island rises gently to the east of Mystery Bay in the vicinity of the site.
The lower parcel occupies much of that west-facing gentle slope. The upper parcel is
relatively flat, and occupies part of the central portion of the island, although lands
further east are of higher elevation. The eastern shore of Marrowstone at that location is
a cliff, with nearby land surface elevations as high as 150 feet above sea level. The
distance between Mystery Bay and the eastern shore of the island is about 1600 to 1800
feet. The Marks' parcels span the western 600 to 700 feet of that distance.
Groundwater on Marrowstone is derived from infiltration of precipitation on the island.
Sinclair and Garrigues (1994) estimated that in an average year 2.2 inches of water
infiltrate to recharge the aquifer. The volume of recharge water for the entire island was
estimated to be 730 acre-feet per year. Parametrix and Pacific Groundwater Group
(2000) estimated that recharge was about 5 inches in the average year near the site.
Although the percent difference between those recharge estimates is large, the absolute
difference is only about 3 inches of water per year, which is within a typical range of
precision for such calculations. The reason for the differé(nt r~h~ge,estimates w~ not
researched. The high groundwater head in the vicimtyof ~~ Maiks' )¥~lls may· hid,icate
MAY 1 9 2003
Page 3
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unusually high recharge rates for the island. Infiltration through the relatively flat upper
parcel, and similar lands to the north and south, may contribute to this effect.
Once groundwater reaches the aquifer, it moves mostly laterally toward the island's
shorelines. In island environments, the fresh groundwater typically floats as a lens on top
of deeper groundwater that is saline. The fresh groundwater discharges to the sea along
the shorelines or is withdrawn by wells. Water that is extracted by wells and used inside
houses is mostly discharged back into the ground through septic systems, thus resuming
its path toward the shorelines. Water used to irrigate lawns and other maintained
vegetation is added to the water that is transpired into the atmosphere from natural
vegetation and does not discharge to the sea.
Four geologic layers are involved with water movement and storage near the site.
Starting at land surface, they are as follows:
,
Surface soils are derived from the underlying glacial till and were observed to be
moderately to poorly drained, organic rich, and relatively fine grained. Surface water
was observed in shallow depressions during April 2003, following a very wet March.
The upper parcel and nearby lands comprising the central island terrace had extensive
areas of shallow groundwater and standing surface water. Detention of water within and
upon the surface soils of flat upland areas likely plays an important role in maintaining
groundwater recharge in this vicinity. '
Vashon till lies below the surface soils within a few feet of land surface. It is a very
dense, unsorted mixture of gravel and sand in a silt and clay matrix. Till is sometimes
called "hardpan" or "glacial concrete". Based on observations of shallpw water and the
till penetrated by the dug well, the till has low permeability and causes retention of water
in surface soils during the wet season. The two on-site well logs indicate that the till
extends to at least 30 feet below land surface.
;.;~
Vashon Advance Outwash (Qva) deposits constitute an aquifer that underlies the ~ill at
depths of 30 to 40 feet at this location. The deposit appears to be a stratified mixture of
sand and gravel, with occasional ~ clay lenses. The sand and gravel strata constitute the
primary aquifer east of Mystery Bay, although the aquifer may have different zones,
separated by horizontal aquitards (low permeability layers) and b,ygeologic
discontinuities of various orientations. ~ Groundwater in the aquifer at t11êiM~'(is' , .'.
confined below the till. In parts of the aquifer east of the Marks', the grÖùn'dwatei>í:s." ;. C ¡ "",'[ \¡'
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The Qva is absent on Griffith Point across Mystery Bay from the Mark's pr1pertl. _', _ -. ' ¡
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movement - although wells develop small quantities of groundwater from fractures
within the bedrock when no alternative exists. On Griffith Point west of Mystery Bay,
bedrock is within a few feet of land surface, and directly underlies glacial till. Because of
Page 4
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the absence of the Qva aquifer at that location, wells develop water from fractures in the
bedrock. Bedrock was logged below 45 feet depth (estimated elevation of 10 feet below
sea level) in on-site well ACC057 where it underlies the Qva aquifer. Sinclair and
Garrigues (1994) report a well log (AAB083) that shows bedrock at an elevation of 20
above sea level near the Marks' property. That bedrock elevation is above the
potentiometric surface in any well in the vicinity - thus establishing the potential for
physical separation of the Qva aquifer zones by a buried bedrock ridge. The bedrock
ridge is generally depicted in Plate 5 of Sinclair and Garrigues (1994).
Groundwater Quality
The primary water quality concern that is related to water use is the possible increase in
dissolved constituents because of seawater intrusion. The discùssion below focuses on
chloride concentration as an indicator of seawater intrusion. ' ,
Jefferson County recently classified all of Marrowstone Island as a high risk salt water
intrusion zone (SIPZ). The basis for the classification is the proximity of the shoreline to
almost all of the land on the island, and the presence of many wells on the island that
produce water that· contains more than 100 mg/L chloride. --
The Marks' dug well was sampled on April 3, 2003. Field analyses indicated that the
water was 54 degrees Fahrenheit, had a specific conductance of 465 uS, a pH of 7.8, and
a chloride concentration of 45 mg/L (low). Although well ACC057 was not sampled, the
well log reports a chloride concentration of30 to 45 mgIL. Well ACC059 was tested and
sampled in September 2000 and had a chloride concentration of29.6 mgIL (see attached
Twiss Analytical report).
Groundwßter chloride concentrations in Marrowstol1e Island are reported in a map on the
Jefferson County websiteI. The Marks' wells are not reported on that map; however,
many surrounding wells are. The data are shown on Figure 1 and indicate that the two
wells closest to the Marks' parcels are low in chloride «100 mgIL) but that many wells
in the vicinity have chloride concentrations greater than 100 mgIL. That data set,
combined with recent data from the on-site wells, indicates that the Marks' property is
underlain by a portion of the Qva aquifer that is not degraded by seawater intrusion.
A high risk of seawater intrusion is indicated by the County's data on Griffith Point along
the western shore of Mystery Bay. - The Qva aquifer is absent -in that area, and wells
produce water from the bedrock. Mystery Bay lies between Griffith Point and the Marks'
property. Because of the geographical and stratigraphic separation between the Griffith
Point bedrock aquifer and the Marks' property Qva aquifer, chadges-·irf:Jau({·tt~ê ¡ane!:
groundwater use at one location will have little to no affect on the otWrQbc'ãud1:~.~.l(.:,.:~ ',:.' [,. ,
W¡']~~~_~J~ j
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A high risk of seawater intrusion is also indicated by the County's data for the eastern
shore of the island and for areas along East Marrowstone Road, all east of the Marks'
property. Wells in that area produce from a portion of the Qva aquifer that appears to be
in poor hydraulic continuity with the portion of the Qva aquifer under the Marks
property. The separation may be related to a ridge of bedrock that rises near-to or above
the potentiometric surface of the aquifer and thus splits the Qva aquifer into eastern and
western portions. Sinclair and Garrigues (1994) report that the bedrock elevation in well
AAB083 begins at an elevation of 20 feet above sea level. That elevation is above the
potentiometric surface, in any well in the vicinity - thus establishing the potential for
physical separation of the Qva aquifer zones by the buried bedrock ridge. The bedrock
ridge is generally depicted in Plate 5 of Sinclair and Garrigues (1994). Other evidence
for the isolated nature of the portion of the Qva aquifer near the Marks' residence
consists of high groundwater heads (8 to 15 feet above seà level) and low chloride
concentrations compared to the surrounding aquifer zones.
Seawater Intrusion
The thickness of the fresh groundwater lens is directly related to the amount of fresh
groundwater that floats on the saline groundwater below. As groundwater is extracted by
wells, the fresh water lens thins, and the saline water interface moves laterally inward and
upward toward pumping wells. Effects of pumping are usually limited to establishment
of a new equilibrium position of the groundwater/sea water interface without actual
pumping of seawater by wells; however, under conditions where pumping water levels
are maintained below sea level for long periods of time, wells may begin to pump highly
saline water and become non-potable. At intermediate levels of effect, chloride
concentrations increase, particularly in wells near the shoreline, or in the deepest wells.
In the UQC Groundwater Protection/Seawater Intrusion Amendments of March 3, 2003,
Jefferson County has identified that many locations on Marrowstone IslaI?-dare at:rj~k,of. ,,_
seawater intrusion. It is the purpose of the amendments to prevent de#¥q4ti~~ ~~ ~ :; " f
potable water resource. ¡ i L/ r-"-h -'-, '., "1 ¡ I
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, ,¡ " MAY 1 9 2003 ¡I!'
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Water Use Analysis l! -~
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This section presents estimates of water use on the Marks' property un~fhiis1~~'~:fuid'~¡:i.'.;.'¡:.,C£:0EI>r~.
proposed future conditions. The conditions are sUmmarized in Table 1. Sinée all the
Marks'wells produce from the same aquifer and have similar bottom elevations, the
analysis does not differentiate between wells.
The analysis assumes that historical water use is near the high end of the per-capita range
cited by Sinclair and Garrigues (1994): 150 gallons per day (gpd) per person is the
assumed total water use. A high value was used because the Marks' property has old,
high-water-use fixtures and one of the largest lawns observed during our reconnaissance
on the island. For calculation purposes, we assume that the water supply for the property
Page 6
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includes irrigation of D.I acres of shrubs and lawn, with an annual irrigation depth of 6'
inches per year. We also assume that the average bedroom houses 1.5 people. Under
those conditions, we expect that the Qva aquifer supplied a total of 675 gpd of water to
the property, of which an average of 45 gpd was for irrigation (Table 2).
Under the proposed conditions, it is assumed that fixtures in all dwellings will be
changed to low-flow varieties, which is assumed to result in a 25% reduction of in-house
water use. Conditions where irrigation remains unchanged, or reduces to zero are
analyzed. Total water use under the proposed conditions is estimated to reduce to 113
gpd per person. Given the increased number of bedrooms under the proposed condition,
slightly more to slightly less water will be used under the proposed conditions compared
to the historic conditions (Table 2), depending on whether the cabin is retained or not,
and whether groundwater continues to be used for irrigation or not.
Although these calculations are approximate and contain several assumptions that may
not perfectly reflect historic or future conditions, they demonstrate that the proposed
change in land use can be approved without an increase in groundwater use. Key to
avoiding an increase in groundwater use is implementing water conservation measures
stipulated in the UDC and listed below in this report.
Impact Analysis
Based on the hydrogeologic conditions at the property, potential impacts are limited to
wells in the local Qva aquifer zone. Impacts to wells currently experiencing high
chloride concentrations (wells on Griffith's Point and along East Marrowstone Road) are
not likely because those wells draw water from aquifers that apparently have a low
permeability connection with the portion of the Qva aquifer from which the Marks' wells
draw wat~r.
Impairment of the local wells will not occur if water use does not increase· and
groundwater recharge is preserved. The water use analysis indicates that water use
increase can be avoided or limited to a small increase. Groundwater recharge potential
can be protected through land and water use regulations (this is particularly important on
the nearly flat terrace near the center of the island, of which the Marks' upper parcel is a
part. Under these conditions, impacts to the local wells will be avoided. '
Impacts' were not further quantified because the concepts discusse~. åbÞ~i_~rl?vÚie ,
reasonable probability that the aquifer will not be degraded by the proposF¡fITF'
¡U.·: MAY 1 9 2003
t""
Recommendations I L_,_.. ......__.......'._._... ".~_.....'_.___¡
f¡rf·rrr;(r··~·' (í\ítNT\J
We recommend that the Mandatory Actions listed for development in ~ih:-M~~i.:· fZ~:.~.~F¡/ENl
and Marrowstone Island SIPZ (OOC 3.6.5 - Groundwater Protection/Seawater Intrusion
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Amendments) be required for approval of the proposed construction. These actions are
listed below along with other recommendations specific to these parcels and wells:
1. Water meters should be installed on the dug well and well ACC059. Meter
readings should be made in accordance with any coordinated effort for the island,
or at least quarterly.
2. Samples of water should be collected from each well and analyzed for chloride, in
coordination with any program coordinated by the County.
3. A minimum 1000 gallon storage tank is required along with a pump for well
ACC059 that is designed to provide the required flow at reduced drawdown in the
well (by increasing pumping time duration, and reducing pumping rate). The
maximum allowed pumping rate for each property is 3 gpm (Jefferson County
Water Conservation List, October 25, 2002). In addition, the volume pumped
from each well is limited to 1000 gpd. Retrofitting the dug well with a new pump
and storage tank will not achieve much because the large diameter of the well
bore already provides a large in-ground storage capacity. The large well bore and
storage capacity naturally reduce drawdown spikes in the dug well.
4. Well ACC057 should be properly decommissioned, or converted to a monitoring
location incoordination with a County program, if desired.
5. All current water fixtures should be replaced with low-flow fixtures, and low-flow
fixtures should be used in all new construction.
6. Intercepted precipitation (roof drains, road runoff, etc) should be detained, and
infiltrated to the extent possible, by approved means. (See the paragraph below
regarding use of catchment water for irrigation.)
7. The Water Conservation Measures List stipulates that well water cannot be used
to irrigate lawns or gardens, but that roof and other run off can be retained in a
catchment and used for irrigation. Depending on whether the cabin is retained or
not, this measure may be urtnecessary to achieve a zero-net-impact based on the
water use analysis in this report. Because of the limited volume of typical
catchments, implementing this measure could result in a reduction in total water
use on the Marks' parcels if implemented for new and existing water supplies.
The owner may therefore wish to limit this restriction to the new construction, and
maintain limited irrigation capacity from the· dug well, if 'allowed by the County
through this permitting process. An increase in irrigation could increase future
water use compared to historical uses and should be avoided.
8. Current conditions wherein shallow groundwater and standing surface water on
the upper parcel accumulate and infiltrate should be maintained. That parcel
should therefore not be artificially drained. Also, any east-west elongate
excavation that connects the upper and 10~t?r pjl[qeJ.s...sh~u!d;;~~ Jnlc~ll<¡:d in a
manner that limits shallow groundwater mo!V'~r((w(fþi~1h~ ~þ.c1i;~~1Œ.\l. .
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Page 8
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Closing
We trust this report meets your needs. Please call if you have questions or concerns.
Respectfully,
~~nz;rGroup
Charles T, ~n
Principal
Attachments
I. Table 1. Project Desctiption
2. Table 2. Water Use Estimates
3. Figure 1. Project LocatioQ. and Wells
4. Well logs for ACC057 and ACC059
5. Well test record for ACC059
6. Twiss Analytical Report for well ACC059
7. Water Conservation Measures List
8. UDC 3.6.5 as amended
9. ' References
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Parcel with County Groundwater Chloride Concentration
H = Greater than 100 mg/L
L = Less than 100 mg/L
County reports data where no wells appear to exist.
o Confirmed Well (many are unused)
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MAY 1 9 æœ
FIGURE 1 :
Marks' Parcels and Local Wells
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File Original and Ani Copy with
Depørtmenlof Ecology
Seœnd Copy -Owner's Copy
ThIrd Copy - Drlfter's Copy
WATER WELL REPORT
STATE OF WASHINGTON
Start Card No. ú/-CJ6?/ 709
UNIQUE WELll.D.. ¡jé'C. () S-7
Water RIghi Pennlt No.
('I) OWNER: Nama~t.Æ'..tð::r -.R~ £u./S AdcRss $tJ,Ib.,x~:S ~Jn/U4. 98j',S~
(2) LOCATION OF well: CamIy œ~JtI . 5ItJ 114~1I4Seç~T. ~ N.,R /Fw».
(28) STREET ADDRESSOFWELl'ornearesla:kRss)~ði""'~~~~ Aà I/~.o,/d,. PEß~
(3) PROPOSeD USE:
11\ Dom8Slk:
o krlgQlion
o DsWaler
Municipal 0
Other 0
Induslrial 0
Tesl We. 0
(4) 1YPE OF WORK' Oovner'snumbørofwall /
. (If more than onB) _
AbBndoned 0 New weD 'g, MeUlod: Dug 0
Deepened 0 Cable 0
Reconãfoned 0 hie Rotary 18.
(5) DIMENSIONS: Dlømetør of wen tP II
Drilled L".r:J'
vO !eeL DspthofcomplBledweU
Bored 0
tJJ1venO
. Jetted 0
Inches.
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(8) CONSTRUCTION DETAILS:
Ces/ng Installed: 6"·· Dfam. from ..,. P-
n'::'~1aI1ed1 ~. Clarn. from 3 S-.
Threaded 0 ~. DIam. from q~
11.10 37
ft. to .37
ft. to 6:2.
Type 0/ pørforaIor used
SIZE 01 pødoraVons
perfcr¡¡tions from
perforaliDns from
perforations from
In. by
11.10
11..10
ft.1o
Screens: Yes ~ No 0
ManuIac:uer's Name í7ºt11t(·~
Type ~.><:2J¡P/c lfu-åt;&:rJ'
Dram,ew/~size , Ol~ from 87
Diam. Slot size from
Gravel pecked: Yes 0 No 0 Size of grayer
Gravel p/IIced Iran It. \0
Surface see!: Yes ~. No 0 To what depVt? /8..'
ModIIñeI used In seal ~ ~;?:>Q/nF
Did any straIa conIa/n LI1Usab/e wa\IIr? Yes 0 No J&. '
Type 0/ waI8r?;'; Depth of strata
Møthcd of sealn slrala 01
Model No.
ILIo 9..2-
ft.1o
(7) PUMP: Maourachnr's Name
Type:
-
H.P.
(8) WATER lEVELS: I.Jn..surface .levalÏCll I
-,;:-.;.:/ above Illßan SM level _ 11.-
SIalic"""" ~ t.be1owlDpolwell Dele /V-I'¥-Yr
Maslan p¡es$aM Ibs. per square inch Dele
Ar1esIan wahrla a:>I1IIoIIed by
(CIII. YIIMI, 011:.)
(9) WELL TESTS: Drawdown IUl110unt water level is lowered be1aw static level
Was a pump test made? Yes 0 . No ~ If yes, by whom? '
YI&Id: gølJrnin. with ft. ckawdown after hrs.
..
..
..
..
..
..
~ data (Iime'1aken as zero when pump turned 01) (water level ~red from well
lop 10 WIlier Ievit1)
l1me Wa1ur Level Trne Water LewI 1Irne Waler Level
,
.:'~- ...... ""Po '...&1t.~~ .., ,-
Date 0/ tøst
Ballertøst~QIIIJrnh.with I"
AIrtesI ga/JrnIrI. with stem set øt
AI\esIan 11IM g.p.m. ()Q\8
Tempera1ure ofW3ter _ Was a chemical ønelys19 made? Yes 0 No I]f
:J Ð -l{S:"' PPll1 (¡Ji.Cr~ ì:>cr
It. drawdovm after :::.
ILIor
ECY 050·1-20 (9/93) .., ......
(10) WELL LOG or ABANDONMENT PROCEDURE DESCRIPTION
Formallon: Describe by color. chÐIacIer, glza of rnale~aI and sIruc1uIe. and shol¥ Ihlè1cness 01 BqJIh!rs
and 110 Willi and MIUra orb ma1erlal1n eac:h l!r.11um penetrated, wtth III leas! one ontty lor each
change Dr Informallon.
n.
ft.
ft.
MATERIAL FROM TO
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I~A~-:W S. ,_ A v.-~..4Va I ~
ß¡t¿~,-W -. 'I!:~ J<.C~4'lt5 3 2..s.-'
C'l:tll'fJ ~ I ~-.-.. ),-~dT ZS- 33:
, w¿'l10?_ ~~R4trR.. . S"þ?~~" 33 3r
~ JhtJ.Rð CtAY ~r- 37
~1.JAlI~rJ~.tf!~V J,e;AfG"S'~O '% H ~2...
ßa:x.'" ,..._- ~Muk-~ 9~ 9'5
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WELL CONSTRUCTOR CERTIFICATION:
I constructed and/or accept responslbllily tor construction of \tis we.. and lis
co/1¥lllance wIIh an YehIngIon well conslnJcllon standards. Malerlals used and
the information repot1ed sboYe are true 10 my beslllnowledge and belief.
NAME S;"'Z>~ ~~LÛl-6 a~ d1~,
tl'l:RSON,FIRM,OR~ (lYPEORPR1N1)
Address ?a k~/6=-?d/å..I?è- 9~J'S2-
(SIgned) ~ _"~ ~ _ Uceose No. /P.?~
(WaL DfII
"
ConIracIor's
~/~~/S'7~ Date Pð~ /.s-
(USE ADDITIONAL SHEETS IF NECESSARY)
.19~
1Ys.
In.
Ecology Is an Equal OpportunIty and Affirmative Action employer. For spe-
cial accommodation needs, contact the Water Resources Program at (206)
407-6600. The TDD number is (206) 407-6006.
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Ale Original and Anlt Copy 1MI\h
Department of Ecology
Second Copy - OWner's Copy
ThIrd Copy - Driller's Copy
WATER WELL REPORT
STATE OF WASHINGTON
SlIlIt Card No. /t.J -ot::./7/0
UNIQUE WELL I.D.' /iee os-?
"
Water RIght Perm" No.
(1) OWNER: Naroo~£";.d.t'.r -/l~£Zd.5.
(2) LOCATION OF WElL: CoœIy J~t:W
(28) STREET ADDRESS OF WEll(orI>ellœS\a:ti1!ss) éfIk r e~ ?bB2.. ~ Æo
Aàtess 8Jr~V lG.s .u~~. Æt3~-¡j
- .:i'øL..114-.AIiJL 114 See !f3 '[ .sb No. R /ê w.u.
~øRÞ~¿¡!<J.?B~
(3) PROPOSED USE: ~ DomesIi: Industrial 0 Municipal 0 (10) WELL LOG or ABANDONMENT PROCEDURE DESCRIPTION
o lnigll/lon TeS1 Well 0 Other 0 Formetlon: DlISCrIbo by color. dwaclør. size of II1<IlalIal and 51rucIunI. and ~ thickness DIIlqlJIfeB
0 DeWa1ør srxl t.e Idnd and !l81urD Df !he malllrlelln each s1raIurn pen&lraled, wfth slleasl Dß8 entry fat each
(4) TYPE OF WORK: ON/Ier's number of we' :2- ch~ of InIDnnaIlon.
(~ mol8lhan 0l1Il) IImAlA!. FROM TO
Abandoned 0 New well II Uø1hod: DUll 0 Bored 0 J ~¿''''N ~,,'.'=L
Deepened 0 Cable 0 DrlvenD &Þ I
ReconrJIIoned 0 ð'Î'- AoIaIy Q Jelled 0 ~1ÌÛ.W ~!~... &Av re.. / 2-
(5) DIMENSIONS: DIameter of W9I 6" Inc;hes. ',O_ W bd.,_.F__. . ;,,~ P.r :L 2.D
Drilled ~ feet. Depth of completed we' ~ ft. ~_~-!"'" ó:~~ 20 go
(W fi~ SdN..o w/~ :5& 3.£-
(6) CONSTRUCßON DETAILS: S/'-(," ..s:øsI'.t'V aw ""~~ 3s- i:/l/
Casing Instilled: 611 · DIam. from -r,:J. ilia n. '-!tNc~/Š/l- ~...v ¡VA ' -1'7' $'7:1
Welded B ~n · DJam'~~1a 3/ It. .- ~b~ . WY ....~ot-f... $'Y
Uner k1sIaJ!ad¥} 5' · Dlam.1rom 11.10 .~z¡¡;,~ S-ò
Threaded ft. . ..
~.. ~u
Perforations: Yes 0 No J8{
1YPe of pedoralor used
S1Zëofpetforatlons In. by In.
perforations from IlIO 11.
perforations from 11.10 I\. .,~ ,,' '., - ,,"
perforaIons from /L1o I\. ¡ ',\ ¡;" '~!.i ;i ,; :
" ....,J
Sçreens: Yes þil]' NoD '" ' î" - .....p...~"~
Manufac1urer-s N8II1II \ ¡'.;:', : -
lÿpe Model No. ~ \ i '_ ~ UAY 1 ~ LWJ : !C:.-. : èf:
D1am.5'~sIze , ð/,r 3~ 3'- ....":\.
Clam. ,,",'àlot size from 1\.10 I\. ! ~ ' ( ;"""-::: ; r.~ ,
,008 S"I , .; r
from 111 1\.10 II. l \ -- .................... .."'............£.......>......,.,.~......,.....~~..:~ 1 -~.;..... . \ t::: r-....
Gravel packed: Yes D No 12\ Size Df gravel jtFFi'\,::',U,;\.\A'~.',t., "'''iZ:r~~' ; . . ~;
Gravel pieced lrom /LID n. i OFt! \)r ..' ..: )i";;~ ... : , _~,"'V __. . .-.........- -.¡ -. .
.-..... .",.~......,...._.. '>
Surface seal: Yes9.. No 0 TowhatdepCh? 18' II. --.. -,
Material usedlnaal ;?O~ .Bê1V?MfI;;:J-- .. , -. -'"
- ,~ . -.
Did any sIraIa COIIIaIn ~ v.aIÐr? Yes D No Ia. '~ - tJ 1..-
. .
~ ~
Type of water? ..,. DepCh of slrata -
Llelhod of sealing strata 011
{7} PUMP: MllflUlactulÐf's Name -
1)'pe: H.p.
(8) WATER LEVB.S: UnckurIace ø.vaØon Work Stalled 11J-/9 .19. CompIeIed lo~17 .19 9-:
, ab<we /Men ...1eveI II.
SIalic level :2..7 It. below lop 0/ WIll DaIII ¿D -/7 -9r- WELL CONSTRUCTOR CERllFlCATlON:
Ar1eslan lflSSUQI bs.persquantlnch Date
Ar1esIan oraIsr Is conIrolled by (Cap. VIIIYe. et:.) I constructed and/or accept responsibility for cons'rucIlOn of this weD, end its
compliance willi al WIshIngton weD construclion sIandIwds. Materials used and
(9) WELL TESTS: ÐrõIWdown is illllount wawleYells lowered below stat1c I8wI the infonna1Jon reported above arlt true to my best knowledge and beRet.
Was a pilmp lest mede? Yes 0 Nag. If yes. by'lrdIom? NAME ~/~~ø;i~ c;~"
ytekl: IIal.lmin. will! Il drawdown alt8r In. 1f'ERSOIf, 011 CORi'OIWJCJNI E OR PAINT)
" " .. .. -"'~£~~;.@_~2
.. .. " ..
Recovery data (lime taken as;uNO when pump IUmed ~ (WiI1eT level meesured 110m MI (SIgnad)' license No. /0 ? $
lop \0 wider hwiII) ~ ~ORIU.ER ,
TIme Water level T_ WalerLeveI 1lrne Walerløve/ Contraclor's
~~/C.oc::--/.K7A..S~ Dale .19_
Dale of test (USE ADDITIONAL SHEETS IF NECESSARY)
Bailer IÐSI ~galJlI1In. willi 5- ft. drawdown alter ~ hIS.
Alr\GS\ - gal./mIn. willi SI8m set at - It. for - hIS. Ecology Is an Equal Opportunity and Affimlatlve Action employer. For spa-
ArIesIan !low g.p.m. Dole cia! accom~atlon needs. contact the Water Resources Program at (206)
Temperalul1l of water_Was a chemical analysis made? Yes 0 NoD 407-6600. The TDD number is (206) 407-6006.
~
ECY 050-1-20 (9/93) .. I .....
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. 'Htrß ~ONN L- SCÐ1] ~M [£1A-jE
trHtJ ð L- f) D fZTO N &,. -- ~1
13503854:.95
P: 1/3
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w~m W!U OIILLIHO , P1JM, SALE.$ AND SUVICE , IUIGATION, COMMUNITY AND DOMunc lY,ua. sYSTf.MS
TEST D~IWNG ( WII.L "W'NS
SWÎCan Drilling C.m,any I In.. ~
"O«T~. WASH.
It'-, 3.1<>.115 -116.2057
St'QOlM. WASH.
".0.10. 161 - 6n.SSIO
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09/14/2000 14:14 3503853440
GRACE
PAGE 03
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"~H ~" " ~ _t,.,. $S,ti:. R. ec-l /?St:4..;. '" H. __ . ~ 'i5~-=_':1 1'1'-':: __.E")I:.__
Bayview Pumps
P. 0, Box 370
Port Hadlock, WA 98339
(360) 379-8000
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. ANALYTICAL, INC
26280 Twelve Trees Lane, SuJte C
Poulsbo, Washinoton 98370
WATER BACTERIOLOGICAL ANALYSIS
SAMPLE COllECTION: READ INSTRUCTIONS ON BACK OF GOlDENROD COPY
If 'nstructlont ate not followed, sample will be ,.¡.ct~.
DATE COlLECTED TIME COLLECTEO
~/ 1)1.1 / YUoII ~:~
-£ l 00 AM PM
TYPe OF SYSTEM IF PUBLIC SYSTEM, COMPLETE
o PU91.IC lliTIJJ
~IVIOUAL .II.D, No, . CIRCLE GROUP
(-...,,~ . . A 8
NAME OF SYSTEM
A«-.. oS'"
COUNTY NAME
~VSo""
SPECIflClOCATION WlfEAE SAMPI.E cou.eCTEO TEU,PHONE NO~Î ~ c;.o~
DAY (3Cpo ? \ g-.c:;¡
f.,.J e.U \a¿~~
eVENING ( )
SYSTeM OWNEFllMGR.: (Name)
SAMPLe COLLEcreD BY: (Name)
¡'!.ttJ(; ~
SOURCE TYPE;. _ DGAOUND WATER UNDER SUA FACE INFLU£NCE
o SURfACE tk"ièLL or 0 SPRING (J PURCHASED or Q COMelNATION
. WEll FIELD ~RTIE or OTHER
SEND REPORT TO: (PrkIIFIIIINIITIt, Addte.und ZIp CodeJ
~.
o ~EJEAT SAMPLe
PrOViOUC COliform pr."nçe Lab .
Date_'_I_
Q RAW SOIJACE WATER $QUIÇO .{~J CD 0 Total ColUotm
R'mw CONSTRUCTION or REPAIRS 0 Ftca! Colifo~
D OTHER (Specify,
REMARKS:
(lAB USE 0Nt.V) DNNI(INQ WAteR RESUI.TS
D UN~ATlSFÂCTORY. COIi1ormt ørt~"t ø.g~TSFACTOAV,
oIiIormt absenl
AEPEAT o E. COli present o E. Coli absent
SAMPLES
REQUIRED Qrtcal pr..en1 o Focal abstnl
OTHER LA8ORATOKr RESIA.TS
TOTAL COLIFORM _/100 mI e.COlI_f100ml
FECAL COUFORM-,--/100 mI PLA'TE COUNT ~ ImI
ANOTHER SAMPLE REOUIRED
~AMPLE NOT TESTED 8eCAUSE: TEST UNSUITABLE BECAUSE:
o Silmpln lOa old o Confllltnt OrOwth
[J Wrong ÇO1t1lner !:J TNTC
o Inccmø/ele form o TIKbIØ Cl,J/ture
Q o ExcGcs doÞric
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TWISS ANALYTICAL LABORATORIES, INC.
2\S280 Twdv~ Trees une. SuìteC Poultbo, WA 98)70 Tclcphonr(360)779-H41 FAX ()GO) 719.~lSO
INORGANIC CHEMICALS (IOC5) REPORT
..,
Systcm lD No: Private Syslem ~~:nc: ACe 059
LablSample No: 01049502 DJ[c Collected: 9/1/00
'--
!-Multiple Sourcc$: Sample Typ\:: R
.-. ._- . . .
Dale Received: 9/ t/OO OHio Reporlcd: 918/{I()
1--- -.,.. I' - .. -...---.. . ----..-
Date Prepared: Dale An<tI~:7.cd: 9/6/00
County: Jefferson ....--.
- -------------.. .-. .--.-..-..
Sample Loca1ion: Welt Head ..---.-
. ........ .- .. .. .. ... .. ..-
Send Report To: Ðayvicw Pumps, Inc. Bill'
PO Bo~ 370
}JOrt Hadlocl<. W A 9&339
- _. .- .._-
DOH Source No:
-.----.--
,~;lInpJc Purpose: B
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flIC!.?
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SRL:
Triuer Level:
MCL:
(lJJ\:
ND:
< {O.OOl};
(State RC(IOI\in& Levd). indi~t~5Ihc minimum TCJ'Ol1inS le\'~1 m¡UiTtd hy IIw Willihin&\OoI l)..'f'öIrlntcnt orli<CÕlhh (f)Of t).
DoH Orinkin, WAter T~ level. S~\!II; whit Ç()II1J',,(tnœ.dct,-.:tcd~t ~nll-:\li')"i in ,:;o¡"" orlli~ Jçvcl nn: rc'tllir.:d to IÐk~ /ltklitiollll un1rlCl. Con
your regional 00« olIiée for funJlCf inronnUlion.
(M~m ConliminJII\lI..c:...~I). If Ih~ COn!;lmill~nlllmouul ,))«:~.ro.-lh~ MCI" 'mm.:dì:lt~Jy CQlllõl~1 )I<)\lf r~gÍQnMII)oJ I am~;:,
(lI/ol Analyzed). in the T~lt~ ,'nlmUII ilUtjC;¡1~ Ihi~ \,\)II1P"1I11\I ";¡. nUl ill...",Ik,! IIIlh~ "'''IT~II :1II:tI~'J(I~
(Not Ik\tC\tII). in the r..'qIt~ c:olunul ;m"IIIII.'1' lI,i~ '''II1If'UUoo \\.1.. ¡maly,':d ;¡nd IIQ dct":l.'led;t1 it k-wl tr'''''''r than or ~""I;¡IIO Ihe Sit I.
ûtctkalq \he GOmI<)\tnd _ lIot d..'1<:çl.:d in tho! \:&11'rk :11 I)' :l1"hC 111':- ~")I~\.'1Ilr;¡tlOn ",..ic;.t......
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P ¡ ¡ ¡ MAY 1 9 2003' ! I t,jl ¡
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¡ jEHERS·ON COUNTY . .. I
LS~~ Fì:;!;::_~O r~~jr.\_!22~.~~E LOP'~~.!.J
Twiss LabQralory Number: 25551
Page