HomeMy WebLinkAbout2000.06.08 - Happy Valley Wetland Determination:t '1. ''. " r.
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P,\GIFIC Rtirt Son. & \\'rrpn, I xc
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203 FounmrAvizNus E^sr, SrnrB 521
OLtrrpre' Wesmrcrortg8s0l
VoI@: (360)534{346
. nrx.(seolrir-roiz
' jlnde Grahn ' . l
Madiona Piarrning and Dwelopment Sves
1256 Lawrence Street
Port Towiisen{ WA98368
Report FileNumber:
Report Subject:
J,ocation:
tdgl\trrtL, ? ,71 June 8,'2000
'.'t
M00-0041 . -' : : -. i :
itnpt Valley Wetland Delineation Report
The parcels evaluated are located in Happy Valley in Port
Townsend; southaast of the intersection of Sa4 Jiian Avenue and , .
Tr.emont Street, parcel numbers 001022003 Q..O4ac), 001022009 :
(3,98 ac) and001022010 (4.13 ac).
BACKGROI.]ND
Site.wetlands assesSment and delineation were canied out by Lisa Palazzi (certified professional
soil:and wetland scientist) onMay 23,2000. The purpose ofttiis report is to describe rezults of
that work.
Wntmno Rrcur,lrrons'
A standard overview ofr-egulbtions @ctingimpacts towetlands areprovided below foryour'
information..
Lopal Regulations: Port Townsend
To qualigas a regulated wetland in Port Townsentl (as per thb reoently e.nr{cted W4shington ,. .
State Wetlands Delineation Manual adopted lvlarch 1997),an area must meet sriteria:defined in .. .
.the 1987 afmy Corp3 ofEngineers trAanuat lCorps ofEngineers Wetlands Delineation Manual, '
Technicat Reporf y-87-l) with all recent regulatory unendmerts and qtarif,cations- fhory critgria
require that an areamust predominautly nippo.rt wetland vegetatiorg must hav.e hydric goils, and ,
rrrust bave wetlandhydrolgry characteristics defined foi,the on site soil Qp9 - iothiq 4"t", ::
evidence or obseriratipn of a long-duration water table at 12 inches or less depth during tlie.grori'ingseason . .,. .,.:.:
The iliigimum regulatgry watland piPin port fqwn$eNd is as follows: .: :r No ruinimum sizdfol Class t (hiehe$ quality) wetlands !. 5000 square ea lSotSO) for Category n and U (high qualrty) wetlands
Page l.
.. .l 101000 qquare feet 000k100) forCa and rv-'(smail' isohtd, bw qi4lty) wetlmds'
,: thui nd.os that.an area that meets the tbrgg-paranreter cnt€dq lild abole must also be larger -
. .
:. than the minimuni sizeto be regul"t d ; ; dtland by the city The wetland edgg illocated by
- ;r;r.dfihr;;il;;*r&* oithe ttuee.parart"te"s, then flagged tn the field for a :
" zubsequent surveY: '
once identified as jurisdictional wetlan4 the waland is nrated' usins $9 l99l edition ofthe
uf,J.*w"rrriogtl"wetlandsRating sy{* The.rling system combinss a-series of questions
and a point system to determing the specific vahrg olthginalividual wetland: Dependiag on site
;*iri";;;it"*ld;;;Ailveeetation" r"oo.ry"qosf anfjlscharasteristics; tt'e
wetlaod n , gr*to * lesser vfilue arJd.so is afotaeA varyiqgiwiit o{qrorytion in the fgim of '
, ;;;;d Uofr"rr, rft f,igho the rating and the higher the intensity of development, the gr- eaGt .
i;;trr,;dru tor
"'urioitn
rrn of 25 feet followqqalityr srnall yetlands adjaced to losr
il";riry i*"rip.*t af,easupto amarirnumof 150 rtetOittt"hftlrpst gualitr' orrarewetl€nds
"Ji"*rt to trigtr intensity dwelopment areas rtrg area wittrin the wetland and bufFers is generalty
considered unuuuituilrot o*rtopreot, unless there is lro reasonable alternative tothe proposed
activity.
'.F'ediralRegulations:AmyCorpsofEpgr4gels- ^L..''--- "'
; rerffia-rythe Army cgrps_of*ry:ers (CoE). The
coEregulates*Jma, of any sizg i.e.,-tnereisno minimum sizefor afderal*Tqoti9""l
'","uu"a] Furtlrermore th" coE must be notified of impacts to wetlands, evgll if_the iryraqt-s.Te
il il ;;;;in size. The coE ro.ai..r chooses lot to regulate impaots ofless than la
;: o'rel but prefer tb make.that decisioq themselveg (i.e.; if they arenot notified, thevSav, chog:: to
. check tn" p-i.rt ior potrttfiJ oiotutiorrr once oonstructioi tt{t Iftlgy do regulate impacts of
i*S it * fil u.r", it is uzually under one ofthe manyNationwide Pennits - pre-defined pennits
that describe certain allowed-pctions and their related mitigations. ,. ' ':'
, ",'. rmpacts of t/3 to 2 acnes gqust be reviewed bv the coe anl 1e_tryi${.::*g flT""l" oq. .
.rhpNationwidePeninits, l*p."tsgrJ;td?-"q"tiequireani"^SYd"ttlry*gTlt:-1,*tis:' ' ''-
no piedefined allowed impaot. uffJan inoivlluar pe#ii a iletailed assessmelil.gf,h"-t-i€ctis '; ':
:, ,require4inoludingbutnotliritrdi;;afternativesinatrslianodaailedjustificationofthe: ,' j
propoied inPacts:
take from one to sweral'Years'
' Tri", on the varioiis fg\refb of notification and permiaing.described abore is. varied- But as .a
g€,nerat rute, watiJn#Je p.*titr can take fronoire to sw.rat months; individual'p€|!its ilar
. ., I
Otnernegulatory.'A,gencies . . .
otlrer potentially ioffi:**.6i include the \Mashingoq St"te oepatt ."t dfrish and Ttlildliip ' '
(wDFm for endanger6d animal speci.r ir*.r, tne.WalEobioo st"tiouputtutett orubol9.g S ' '' . '
;of;#itdrgir*.r, andtheTtresbington stat"o.pattmeot ofNrituralResourcel@llR) .: . -';'
' Natural HeritageProgram for endangered plantiszues.
MntEoos & Mlrnnrus
,Eveluatirin of F'ieH eonditions ,
As required io port6omr*{E" wetland was delineated using methods:described tnlhe 1982' I :
, .. Army Corps ofEngineers Manual (Corps ofEnefnpers Wetlqods Delineation M*q4 Technical. Rgport Y-87:l). The project site was traversed to det€finine whethe,r norrtnal environnrental
bonditions exist and to ide,ntify plant community types inoluding wetland habitattlpes. The
. routino determination method was used because the wetland areas af,e relatively homogeneorrs in'. regalds to vegetation, soils,. and the hydrology regime.
-!.:
" In areasthat appeared to havdwetland characteristics, a rgpresentative observation point for each:
plant community was selected and data onvegetation, soils,'and hydrology.were collected. At: ,each location, awetland/nonwetland determbation was made. If an areawas determined ts be
trtd4 tn"Uo*toywasil4gged with d pink fla& assigned aletter, th'e,tr numbered sequentially.:
: .Wetland Iletineafion end Classitipation ," . :.
The 1987 nianualrequires examinatifficharacteristics'and indicators ofhydrophytiovegetation"
..hydrio soils, and wetland hydrology, Positive wetlar.rd indicatorg of all three ctraracteristics must
be normally present to make a positivewetland determindtion. Each characteristic is summariz6d
in the sections below. Data were recorded on the Ro.utine Wetland Determination Data Form I,
. which is provided in Apperdix II, The plot ID number for each data point taken appears in.the' upper right corner ofthe data sheet. firis plot nurnbgr corresponds to the plot sho.wn on the
surveyed wetlands map as the area where the data was collected. .
Vegetation
Hydroptrytic vegetation is defined as "the zum total of macrophytic plantlife growing in water
or on a substrate that is at least periodicalty deficient in oxygen'a.s a result of excessive water
content'(WashingtonDepartrrent of Ecology 1997). Several indioators may be used to
det€rminewhetlier hydrophyric.vegetation is present on a site. The most reliable indicatoi is
when:more than 50lo of tnJ Oominant plant qpecies'bre classified as wetland plants on a, .' 'oAain list of spgcies that ocqr in wettands; tne fist is qaintaioed bf the U.S. Fish A Wildlife
1 Qervice GeeO tgg8, wirth a 1993 update povided forthe northwestffnitea States). r
Tbe spegies list separates vasanlar plant's.pecies into five basic groups basef bn their dredand
indicatorstatus - Obligate (OBL), Faculiative Wetland.(FACW), Facultative (FAC),
Faqrh4ive Udand CfeCffl, and Uplirnd (LIPL): fire plant species intliqator statusiC birsed
oo *ustersmeot of-tnsinAviauat specier; frbqu*.y otoc"rrrren"" in.awcland. Table I
.b,elow srmmari2es theindicator status ratings, , t
Otherindicators of hydrophytic vegetafioi include visuJ observation ofplant species growing
, : .. :. :- '
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in areas ofprolongd inundafon and/or soil saturation'inorphological adaptations,.tichnical
literatre, botanical jotunals, tec_hnical reports, waland plartt database, physiological .
' adaptations, and re,productive adaptations. Plailt sp.ecies re identified psing Flora.ofthe. , ,: Pacifio"Northwest (tiltchcock and Cronquist 1973). Plant comnrunitieswere classified using a
system developed by the United States Fish and Wildfife Seidce (Cowardin et'al 19?9). .This
sy$emlq hierarchical and structured around biological hydrologiqal apd:zubstrate' characteristics. .,
Table 1.Status
DetinitionIndicator Category/trndicator
SYmbol
Plants that occur almost.always inwetlands: .
esdftrated probabilitv in wetlands greater than 9994
under nahral conditions. .
Obligate Wetland Plants (OBL)
Plairts that have in estiniated probability of 67Yo -
99o/olo be found inwalands
Facultative Wetland Plants
(FACW)
Facultative Plants (FAC)Plants that are equally likely to occur inwetlands
or nonwetlands: ixtirnated probability of 34Ta' -
66%tobefoundinv,'etlands., :
Plants that uzually occrr in nonwetlands,
estimated probability of lYo - 33yoto be found in
nBtlands. '
Facultative Upland Plants (fACII)
Plants that occur almost alwayt in nonwetlands
irnder nahral conditions, estimated probability
ereat€rthat 99/o.
sbits . ,.' ,. -
.
A soil piofle.was sr(dminbd,at eachplot using a Ginch soil atrger and tile spade. Soils were, sampld to a depth of * leaqt Z:hohes. When usiirg the 1987 methodolggy, fu *.1 ry' , :
observed forhydrio soil indicators iinniediately below the A-hpdzm or l0 inclies'fhich e\rcr
js shaltower. Hydrii indicators for nonsandy soils iriplude at a miniruum, one or more oftho
,: following generally witttin 12 inches ofthe soil sdrftice: ..
organio soils (ttrstosoG), .
ni{d eOineaois,
zulfidicmateriat - : . -' , . ..,, :' '. ..' -' .: . '' .'' .:
aquic or peraquio..noisture regimes (i.e. two weekq of contitiuous inundetion or
sattration), . .jreducing soil conditions, and
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soil colqrs; gteyed soils or nongleyed soits with a matrix chroma of 2 or fess in mottleil
soils or a ;tri- chroma of ! oi less in uinmottlea ioitsl Soil chroma, oi co.lor, was
determined using aMunsell color'char.t (Kollmorgeri Corporation 1975). . .
ln aiditio& we used the most recent vdrsion ofField Indicators ofHydric Soil$ wtrtch = - '
provides tletailed descriptions of specific soil morphologio featurbs thet i'ndicate lpng-duration ,
sahrration. :
Cinsite soil characteristics were compared to Natuial Resource Conservation Service CNRCS)
desuiptions ofthe mapped soils to either coirfirnt the mSpping or deelmne if an inglusro4 of
anothir soil type is present. Whe,n usingthe 1987 Routine Methodolory, hydrio soils are
aszumed to be present in any plant comairnity ilwhich all dominant spet1 !T-an ldic{or
status of OBL or, all dominarrt species ha.ve an indicator status of OBL or FACW, and
;rtf*O hydrology is present.
Hydrologr: - '.' .' ':.
Wetland hydrology is,defined as areas that are periodically inundated or have soils that are . .. '
saturated io the qlrface for a zufficient duration during the growing seqson to create auaerobii
conditions. Indicators ofwetland hydrology are difficulJ tointerpret inthe field duringthe dry
s"ason'ot the rainy wintei season as ? watertable may be non-existeni during the dry seasorL
or higher than average for some periods during the rainy season. The 1987 COE manual lists
field indicators ofwetland hydrotogy that may provide evidence ofrece,nt and/or long-term
hydrology events. The indicators are listed in oilter of decreasing reliability. They indude
recorded-data and field data" zuch as visual observation of inundation.or saturatiorL . '
watermarks, drift lines, sediment deposits, and drainagc patt€rns.
'Duration of io.rndution and/ot soil saturation for the COE 1987 method is based on the
numb'er of days at 32 degrees Fahrenheit or above d*iog the growing season.. For the Paoific .
Northwest, inundrition or .saturation'to the surface for at le*rsf l2.5yo or greate.r ofthe
growing season in'most years is required. The Seattle District of the COE requires two weeks:
If *ntiltro"s soil inurdation oi sahrptionwithin'the gro,iog seasonto safsfy wetlild . ,
,ihydrology. tttg latter criterion was uged for this dete{.foinatiorl ..
. , ,,
.,
t ' ...''
Forthis projecq we hatl to makg,awetland.determination during dry-timeofyearwhen ''' ' .
hydrolqgywasnotpresedt. ,- . , ..:
. i.\' .: r Motle" or'redoiiinrirtlhio featur* re spots or blotches of oonliisdng
Gleyed'soils are predaminantly neunal gny in colm. :
oolm occuning *i&in &e soil mitht
Page 5
. , : ,R$Strtrs Ar{D DrscussroN
Site description '-'
@ed study siteis located southeast of the intersdction df San luan Avenuo
and Tremont stregt, dir;ctly eai of oxisting seoiol houping complexes, and south of a row of,', existing single O-iiy homes. The site is covcred with I ttof ry$ed.and o9p€-gr- srys forpS. .
: . rrost paa 6ut includes occasio.nal.fiees and small shrubs. There is a depressional kettle wetland
located in the rrortn*i half of th;e sitg. WeAana recoirnaiSsance work tstti"d out by gFqtartig
in years past indicated that there could be wetlands in the portion as well. City of
p"* i".i,rr*a topography maps indicate that the depressional kettle wetlttod tf .t !*tt-y: feet
to** in eievationin* foi other area onsitg and ttr,at elwition !s approximately 6 @ highqr
than the rlater zurface expressed at the golf course ponA fc'aed about l?00 feet tothe south- It
, is proposed to build somi tlpe o'f senior care facility in the southern portions of the.si1e. '
Vegetation
A"--*ti*.C abovg vegetation across the rnajority of the study site parcels is a mixture of '
-seeded'and native gr*r"r with ogcasionat surall shnrbs and one or two trees. The dominant
grasses are fescues, pos, and bentgrass species. The shrubs are wild rose, native crabapp,le, and
hawthorne
The wetland vegetation is quite different from the zurrounding up!and9, Soft rush ("Iuncus
efusus)covers-about SOTobf the wetland with reed cinarygOss (Plnlais mwdittoceae)
*"oiog about 407o, and butterorp (Rmrncutus ryfns) and a potenfilla species covering $e.
' balancel These plants are all classified as Facultative or wetter (i.e., they are all wetland plants),
There is some buttercup, teea canarygrass and soft rush in a transitional areljust outside the
jurisdistional wetland
"Oge
but for the most paft, fhey are notrfound more than l0 feet from the
wetland edge.'.:
Soils
lfirdiog to the Jefferson:Co"trty soil survey; the San Jtian ioil series is mrrpped on and -near th9,
wetland. -The San luan gravelly saoOy,toatu-ObZ;-stopes is classified as.'coarse-loany gveJsandl
"t r."ey skeletal mixexfmesic Paohic X€tudbreed. it is not a hydric,soif but can lrave hj'&ic, '
' . soil inolusions.
. . Becarfse the Siur Juan soils have very dark-colored; deep surfacs soils, it can be difficult to '
' . il.rp16tr f"; hydti" ;it rtr.ort"rirtiO-q iothr abs€nc€ ofwet+trason hydrolory. How,ever, at this
, . , siter'the difterences were relatively apparent. The spils within th9 wetland had a sandy $rfaco
. . 2 Co*rrfo*V .over sody or carty skda4 nii€4 tri€sio po*ii, XennOn+, 8to"{ry ryrydb rs hls licil€d hnim dcr diDtn€d : .
teptlfigqdr**fia""A"in f*-*n".fowt"*soriinim(unbrlfrg.OeweqadOercfimiriooOniduofwdwhienad'droudtry;ffi;46;n;-"-d..p(!rederrho50.-f ar*.oLd-qEcgiqir-q.Ftb-"dd"rentelerbtesbe(ryimualteopiafc :.'
r-eE"fi;3rto fS;C6f - SFg,ioryeCqgfrerat"gcsonocfdpOf ns tS-S09e sp4lcssria 18?6dty,.odpostrygre4erdi'at5%
"otr-oibgn ds lcoorsetomy over sandy or sody *da'D.
Page,6
... ,horizon,with unuzuatly high organic matter content. ThiS characteristic rneets tfre reqrirei,nents of
' nd".tor Sl .; Sandy-Mriky tffneral (F eld Indicators ofHydric Soils, USDA). .So the soils with
these characteristicg u/ere classified as hy&ic. . . . :. -
: For your informatiorg stan{ard characteristics of the mappd soil series are desdribed in Appendix
I, Please notqthat tlie SCS soil series rnaps and descriptions clarasterize expested characteristics
in only the top OOIOO inches of soil.r Furtlreimore, the m3p rmits cim havg extensive inglusieins of
- other soil t1pes, and in some rare Gases, gan be entirely in error. firis particular Soil Survey is a . '
lower level survey,'so should always be verified with field;work.
Hyirology ' i .
As.described above, because this field work was undertaken during 6 iime of fear.when ttte .
.hydrology is absent we had to look for indicator3 oihydrology , ' .
Hydrolory sgurces at tliewetlandinclude zurface precipitation'and seasonal stormwater .
uo*rrrrtuft"g above thq groundwater surfticeibelow, There is no apparelrt direct inlet oi otrtlet, .
So seasonal and annual flustuations o{the underlying groundwater stirfa0e will control.what is
considered tobe the long-tBrmwetland edge. :
..
In lower parts of the wetland ther.e were some small areas that appeared to havebpen covered
with surface water for extended periods during this past winter- In additio.rU thesoils had oxitlizcd
rhizoqpheres (rusty halos around living plant roots) wittrin 12 inches of the soil nirface, indicating
long-duration saturation during the growing season.
Wetland Ratins :
This Palushine Emergerit wetland sygem is rated as a CategoryfVwetland (25 foot buffer '
setbac$because it is dominated by soft nrsh and reed canarygrass and is less than 2 acres in.size
(see Appendix,t[). :
OtherPotentialWetlandAreas :. .,. j i
. , ft"t wm or.less in the southeast corner of parcel numbe,q O0 rc22003 that
was ideritified prwiously as being possible wetland. ,Howwer, we waluated both soils antt . ,
.vegetation in that area and did not find any places where there.were indicators of a lo4gduration
w.ater table within 12 inches of the surface. .The soils were not hydrie having po mottling gfeying
ff high qlgaoic.matter co,ntents within 12 inches of the zurface: 'The plam community did not
change significantly aside frorn a small increase in buttercup in the low.gst elwation areas along
the eastern felrce line similartq what we observed in trimsitional areas around the.wetland. '..
.
That is not to say that there is no shallow groundvater in these treas; just ihat it is zufficiently far
from the strfface to not meet the hydrology:requirg.ment - i.t, a:long duration watq table witHn
12 inches ofthe surf,ace. . :. t t " : .' "
PageT
Sunimary
This is q small, Palusring Emerge,m wedand that has formed in a kettlein the northwest portion .
ofwhat appears to have beena ieeded pa:sture inthe pa*., fire wetland is dominated by soft nrsh . i
. and reed ganarygrass. Ornentty the upland pashre is a mii< of seeded andnative gras!€.s - ii,hat .
appeql to b-e mostly upland qpecies. Invasio.n by and gron'th of small n$ive agd iintroduced ihnrbs. la the zunounding uplands indicate that the pasture has piob,ably not bee,n mowed in at least a. coupleofyears.
The wgtland liydrology source is a seasonally fluctuating grciundwate,r tablg that is aszumed to
underlie the e,ntire parcet ; It Slould bq noted that the surface water expressed at the golf course
poird about 1200 feet to the south.is about_ E feet lower in elwatioa tlr"" the study site water -
qurfrce, according to City ofPort Townsend topography maps. This indicates either that the '.
gfoundwater surFace slopep (i,e. drains) to the south in this area at about O.5.o/o,or that thd.two'
grorrndwatei surfaces are independent of eaehother. Ifttrat information is critical to project
dwelopme,nf it i3 zuggested that the groundwater zurface elevation below the site be det€nnined'
either by digging soil pits at the northern and southern ends ofthe site and interpreting soil
indications oflong-duration seasonal sahration" or by monitoring groundwaterthis comingwinter
with dataloggers or gpen test holes.
The soils are mapped as San Juan grav,ety sandy loanU but inwetland areas havg a shalloirv water
table and nouoh higher organic matter cor$e,nt in the zu@ce soils. The wetland soils met the Sl -
Sandy Mucky Mneral indicator requirements, so wer.e considered hydric.
. Based on the above datg the kettle area in the northwest portion ofthe sitg was determined to be
a three par.ametbr, jurisdictional Category fV wetland. ttJ functions and values in terrrs of habitat
have been greatly reduced by past practices, but it offers s-ome minimal flood control'and water
quality improv.erre,nt functions. j
-ar."s to the southeast portion of the site that were previously identified * U"lng potentially wet'tlid riot have hydric soils oi a hydrophytic yegetation community. However, a shallo-w .
gtroundwater grrface is ocpected qr the iolvest glwation areas It'shoutd be'aszumed tha! the
groundwater sur'face exryessed inthewetlands ocsurs across the e,ntire parcel. ': '
,i
,: Ifyou haiie any Ere*ions, please feel free to call and disctiss.
(
'SWS certified Brofessional Wetlands Scientist (PTS)
ARCPACS Certified Professional Soil Scientist (C"SS)
Certification t&3l3:
Page',E'
("Befsregcet
,Cbwardi4 L.M., V, Carter, F.C...Golet, and.B.T. Lb Roe,, 1979:,.Classification ofWetlands and'
Deepwater Habitatq oftheUnited States. Office of Biological Seryrce9, Fibh and WilOite-
,1 '. Seryioe, U.S. De,partnent ofttre Interior, {'WS;1035-79/8!. 103 pp, ' . . ,
-:.
' Bqyironmental Lab-oratory. t987. :Corps ofEnginecfs "W.AuoAt Delineation Manuaf Tphnical
. Report Y-87,1, U.S. Arniy EngneeiWaterwaysExperiment Station, Vicksburg Mss.
: -''::-
Ilitchcock, C.L. and A. Cronqui st. ' 1973 , Flora of the Pacifio Northwest. Univers$ of
WashingonPrpss: ?30 PP. ' - ,
Kolhnorgen Colporation: 1975. Munsell Soil Color ifrai+. Macbeth Division of Kollmorgbn '
Corporation.Baltimore,MAl-d.'.,.'. . .
w.:
Reed, P.B., Ir. 1988. National List ofPlant Spebies That Occur in'Wetlands: Northwest
'(Rggon 9). U-S. Fish and Wildlife Swice Biologicat Report.r 38 (26.9). 89 pp.
Washington Department pfEcology . lgg7. Washington State Wetlands Identification an{ '
Delineation Manual, publication *eO-. W*nhgtoo State Departm€nt ofEcoloily. Olympia,
Washington.
t
.\
Page 9
:
{t^'
:
I APPENDD(I',
.. .. : ,. , t . : '' -: .:
:, sAll JUAN SEnrES . , ,'
The San luan gravelly sandy loarfis ar.g very deep, somewhat excessively drained soils formed in.
gUrlA uut*"r[. Td r,nfa; gorls are ge"&ailfdark-cblored grave[y sandy loams, Soil tsxtur-e
, 5*nro coar.serwittr deptb, grading to Cfaeily lolmy coarse sagd and gravelly coarqg'sand,
i'. Avetug" soilpermeabilityisexpected to'be rapiri (6-20inches perhour) tlro,rghou!.
-,The.San'Juan soils are is used for farrrland, hayland pa*ure, woodland or homesites with feur
limitritions. Thepriinary tlmitationfor septic drainfiplds or stormwbter facilities are related to '
'poor fiftaing "npirtty due to rapld perc,o-lation rates and relatively low surface area in'sandy soils.
,iihousing dinsity-is mpdeiate to nigb conununity se\ilqge W{efns ot alternative septic designs
ar" r"comto"nded to redUce potential ofwdter zupp$contarninationby seepage,
.i
Page'I
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The pubticworks Technical conference is desisned to provide the Prospq$Y"m"k**;
D3S-
x:ffi{s ?ifiHr;*'H:xfl";$1;;Hiftrli:ffili#$$fi#ffii' \,f p
departnrents of the crty, a?
"pproprir,t".
A fd of $25O.0O ii .rtatgei- Fees paid may be applie
toi,ard a street ano utiitv oev'eiopine"i;;;it f* irt:d: in Tier iif a comptete street developme"t0p'
apprication is received within on" v""iJr-0"i" oi fieiechnicar conference, unless changes to
proiect plans o,,u*unding development require further review-
lf you only wish to rcceive the location of the utilities along the proper$ frontage' call the util'tty
locate sewice at 1-g0G424-5555. Water and sewer mapi mqv be purchased from the Public
works Departmentoiievieweo atrhe?-ih/s permit cenier, gr Rooi, waterman & Katz Building,
181 QuincY Street'
Purchaser/APPlicant:
Purchasefs Address:tfl ,
Olvnet's Name:
Orvner's Mailing Address:
Site Legal DescriPtion:Addition:
Zoning District
G
Tier No.4-
*toPr14
'Pane lYle
W:-)
38 9o
Phone:?8tt€'
Block . Lo(s)
Parcel No:. oQ!0.22@ 3
po lo +rca 7
outbuildings
outbuildings
L8
st
Proposed Project '/ Single'Family residence(s) with
Multi-FamilY dwelling with
Mixed use, @mmercial or manufacturing
Subdivision or PUD
The principle means of access to the s'tte is proposed to be from
fie area of the entire site is A.trO, 6f ,, sq, fL, ot vthich iLrXAS sq' ft is
with buildings, deckg etc'
ls any part of the subiect property UIin 20O feet of a fresh or saltwater shoreline?
flYes E No
:
short ptail, varianca, conditiond us" p"ilit, street Y99?tion ol nblned unil de
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T"x 'lt', su
rn
be
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