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BLD2006-01643 Wetland Delineation and Analysis Report - PLN General - 10/13/2006
-LV, 1J rw viJ iVi rnVri- 1'-'(1i t'10101/�410 r-'ly9 Pmfermd. Real- " g North Mason To: From: Fax Number: Fax Number: (360)275 - 1605 Number of Pages: Date/'rime:Notes: er-M �- n ng C)(& q� =23552NE State Route 3, PO B0X 3240 Belfair, W' A. 98528 Office Number: (360) 275 - 1600 au-ao- IUU wo.aw rrsuL,i— 1--l13 FOIOL/10410 r—Lyy ( i THE WETLAND CORPS, lfqC# Vatlar D elineatYan• Habimt Maraysmer t Plans • R4mrim Restoration• Misigatiosa• Biological Evaluations P-astside Division,(509)899-0355 'lestside Division (360)620.0618 IIARDINO IU LL WETLAND DELINEATION AND ANALYSIS REPORT Parcels: 12232239001.1 122322390012 122322330013 122322390014 Mason County,Washington Prepared for.- Paul and Linda Archambeau PO Box 646 Orapeview,WA 98646 Prepared by: ]Heather Lane and Lee Road February,2006 1%LJ 1J VU UjI-L0 rnvri- f--(1;i YIOId;i/14410 r-'Lyy TADLIE OF CONTENTS INTRODUCTION.............................................. .1 .......................................................................... METHODOLOGY ..........................................................................................•---•• ..... ........ .....2 BACKGROUND INFORMATION................................................................................ . .....3 WETLAND DELINEATION RESULTS....................................................................................4 WETLAND&STREAM EVALUATION....................................................... ... . ......4.............6 SUNMAIZY..... ......................................................... .7 REFERENCES..............................................................................................................................9 Fioures Figure 1. Site Vicinity Map Figure 2. 'Wetland Boundary Map Figure 3. National'Wetland Inventory Map Figure 4. Mason County Soil Survey Map Figure S. DNR Stream Map Appendices Appendix A. Routine Wetland Determination Data Forms Appendix B. Soil Survey Text lu-13- WU UZ1;10 rnuL,J- T-Yl1� P0104/040 r-'Lyy THE WETLAND CORPS, INC* Vedaiad D"eat6n% Habitat MatagementPlaces • ltivasianRestoration, Mitigation• Biola*alEvaluat6bs Eaetside Division-(509)899.0355 Weetdde Division-(36Q)620.0618 Marcie 2006 Project#TWC06W 155 Pagel of 9 WETLAND DELINEATION AND ANALYSIS REPORT Harding Mill Mason County,Washington INTRODUCTION The Wetland Corps has been authorized by Paul and Linda Archambeau to perform a wetland delineation at the four tracts located on Harding Hill Road, located off of Highway 3, near the city of Allyn in Mason County, Washington, (Tax Identification Numbers 122322390011, 1223223900122 122322390013, and I22322390014). The focus of the work was to identify any regulated wetland and/or stream buffers within each tract that would be applied to the anticipated land use (Single-family residence). The subject properties are located in the Northwest V4 of Section 32, Township 22 North, Range 01 West WM (Figure 1 'Vicinity Map). The entire ownership is comprised of four tracts which are each approximately 2.5-acres, and rectangular in shape. Harding Hill Road makes up the northern boundary of Tract 1. Tracts 2, 3 and 4 are south of Tract 1. For the purposes of federal, Washington State, and Mason County jurisdictional oversight, methodology used for the wetland delineation is consistent with the wetland definition provided in paragraph 25a of the Washington State Wetlands Identification and Delineation Manual (Washington State Department of Ecology, 1997). The sections below provide: (I) an introduction to the site; (2) a description of methods used in the field delineation;and,(3)technical results. GENERAL SITE CONDITIONS Collectively, the four tracts contain a mixtuiiv of forested/shrub, and herbaceous communities. Upland forested areas are dominated by Douglas fur, Western red cedar, and big leaf maple with a typical understory dominated by evergreen huckleberry, salal, salmonberry and sword fern with lesser amounts Himalayan blackberry. Wetland areas primarily consist of dense, herbaceous communities of slough sedge, skunk cabbage and creeping buttercup, with an overstory dominated by red alder, western red cedar,and big leaf maple. The shrub layer in wetland areas is mainly comprised of salmonbeny. 9465 Provost Road NW.Suite 202 ®Silverdale,Washington 98383 Phone: (360) 613-2407 Fax: (360) 613-2405 110-15- IUD IUD:110 rnu�•r 1-(1� Y101051�0410 r-Lyy ' Harding Hill Wetland TViWC 166 March 2006 Page No.2 The general topography throughout the area is sloping easterly at a low to moderate gradient,towards a large depressional/swale area, where an intermittent stream and headwater wetland run northerly along the eastern portion of all four tracts. Existing development surrounding the subject property is comprised of low-density single-family residential development, cleared areas, and undeveloped forested areas. METHODOLOGY Review of Existing Information Consistent with procedures detailed in the Washington State Wetlands Identification and Delineation Manual (Washington State Department of Ecology, 1997) (1997 Manual), preliminary information on the project site was gathered prior to the field review and delineation. General information sources included: United States Geological Service (USGS) topographic maps, 1974 United States Fish and Wildlife Service(USFWS)National Wetland Inventory(NWI)maps, the Soil Survey of Mason County Area, Washington(USDA, 1960),and Mason County's critical areas regulations. Field Delineation Methodology used for wetland delineation was consistent with the technical approaches articulated in the 1997 Manual. This document is the wetland delineation manual that is used in determining wetland areas when applying state and local government regulations under the Shoreline Management Act and the Growth Management Act in Washington State. The extent and location of project site wetlands were determined during field work performed on several days in March 2006. Field work was conducted under sunny skies with an ambient temperature ranging between 40 and 50 degrees Fahrenheit. The time of year and recent precipitation history were considered in assessing the type and extent of wetlands presumed to exist on site. Specific field methodology used in determining the extent and location of wetland areas include: a As part of the initial project site reconnaissance, the site was walked to determine the general extent and location of potential wetland areas; ■ Wetland and upland sample plots were established in the identified potential wetland areas and in the adjacent upland area; and ■ Wetland boundaries were delineated with flagging by noting localized topography and vegetation, patters and comparing parameters of hydrology, soil, and vegetation with data collected at the wetland and upland sample plots. The project areas were investigated and data was several sample plot locations. Data collected at each sample plot were entered onto a Routine Wetland Determination Data Form(Washington State Department of Ecology 1997). Copies of data forms for each sample plot are provided in Appendix A. PO Box 2854,Belfair, WA 98528 cell:360-620-0618,Office:360-372-2421 e-mail:boad40@peoplepe.com av-10- ou UZ);au rnurr- '1'-'t1.i P005/040 F-299 ' Harding Hill Wetland TWCl66 March 2006 Page No.3 WETLAND & STREAM EVALUATION Wetland Categorization The wetlands were classified and rated using the categories set forth in the Mason County Resource Ordinance, which defines wetland categories according to Washington State Wetland Rating,System, Western Washington, a"d Edition, or as amended hereafter (Department of Ecology 1993). This wetland evaluation used the new rating manual, Washington State Wetland Rating Sysrem for Western Washington (Hmby 2004). This system identifies various complexities within wetland structures, habitat attributes and various functions associated with wetlands. Stream Identification and Assessment The onsite stream was classified using the Department of Natural Resources stream typing system. Factors that influence stream typing such as channel width, possibility of intermittent dry periods, and obstructions downstream that would effect fish migration were analyzed to accurately classify the stream. BACKGROUND JNJ'OIRMATJON Mason County Soil Survey The soil survey of Mason County indicates two onsite soil types(USDA, 1960): Soil type one has been identified as: (Ac) — Alderwood gravelly loam, 15 to 30 percent slopes. Alderwood is a well-drained soil that usually occurs on uplands. Native vegetation is a dense forest consisting of Douglas-fir with an understory of salal, Oregon-grape,vine maple, and huckleberry. This soil has developed from mixed gravelly glacial till dominated by igneous rock. Surface drainage is more rapid than on the more gentle slopes. Runoff and erosion on the logged and semicleared areas are controlled by the dense growth of plants. Soil type two has been identified as: (Ab)—Alderwood gravelly sandy loam, 5 to 25 percent slopes. The characteristics of this soil are the same as the Alderwood found on slightly steeper slopes described above. A more detailed soil description can be found in Appendix B, Mason Soil Survey Text. The Mason County Soil Survey map is shown in Figure 4. National Wetlands Inventory The USFWS NWI map (online wetlands mapper) shows two identified wetland areas in the project vicinity (Figure 3). A freshwater forested wetland and a freshwater pond wetland are located east and northeast of the ownership. The NWI map shows no identified wetland areas within the subject parcels. PO Pox 2854,Belfair, WA 98528 cell:360-620-0619,Office: 360-372-2421 a-mail:boad4O@peoplepc.com au-1J- vu v o.iw rnun- Hardiag Till Wetland TWC166 March 2006 Page No.4 WETLAND DELINEATION RESULTS General Wetland Conditions The Wetland Corps identified one stream and four areas meeting the criteria for wetlands on the subject property. The wetlands are delineated in the field with pink flagging. Data was collected at representative sample plot locations in each wetland. Specific findings on wetland soils, hydrology, and vegetation for sample plots within each wetland are provided below Wetland A and haLmittent Stream Wetland A is the largest of the four wetlands. The wetland is located in the depressional area on the eastern portion of Tract 3 and 4, with its northern edge extending into Tract 2. The wetland tapers into a channel, and transitions to an intermittent stream at the boundary between Tracts 1 Mid 2, runs northerly through Tract 1, and exits the property at the northern boundary of Tract 1 through a culvert under Harding Hill Road. Two data plots were analyzed in Wetland A. Data Plot Al is located on Tract 2 at the northern end of the wetland near the transition to a stream, and Data Plot A2 is located on Tract 4, where the wetland continues south and offsite for several acres (as mapped by the National Wetlands Inventory,shown in Figure 3). Vegetation in Wetland A consists of a dense understory of slough sedge (Carex obnupta, OBL), creeping buttercup (Ranunculus repens, FACW), and piggy-back plant(Tolmiea menziesh, FAC). The shrub layer in the wetland is comprised of salmonberry (Rubes spectibilis, FAC+), which is mainly located along the perimeter of the wetland. The overstory within the wetland includes western red cedar (Thuja plicata, FAC), red alder (Alnus rubra, FAC) and big leaf maple (Ater macrophyllum, FAC). Hydrology indicators within the wetland include inundationlsoil saturation in the test pits, water marls on trees, sediment deposits on woody debris, drainage patterns, and presence of FAC neutral vegetation. Soil pits excavated within the wetland revealed a single layer profile of a mucky peat with matrix chroma 10'YR 3/1 to 12 inches with observation of sulfidic odor during excavation. photo L Wetland A;picture taken on Tract 4,facing east. PO Box 2854,Belfair, WA 98528 ce11:360-620-0618,Office:360-372-2421 e-mail: boad40Qpeoplepc.com -LV -Lo- ern Wj.10 rnurj- T-71i f'IOIO�i/�410 1~-'Lyy Harding Hill Wetland TWC166 March 2006 Page No.5 Wetland B Wetland B is a slope wetland, located parallel to Harding Hill Road on Tract 1 and continuing south,to approximately 50 feet into Tract 2. The wetland has several seeps which finger along the slope, and drains into the intermittent stream. Vegetation in this wetland is comprised of a deciduous overstory of red alder (Alnus rubra, FAC) and big leaf maple (Ater macrophyllum, FAC), with a shrub layer of salmonberry(Rubes speclibilis,FAC+),deer ferny(Blechnum spicant,FAC+), lady fern(Athyrium felix- femina, FAC), and Himalayan blackberry (Pubus discolor, FACU) with lesser amounts of sword fern (Polystichum munitum, FACU). The wetland contains a diverse herbaceous layer of skunk cabbage (Lysichiton americanum, OBI.), piggy-back plant (Tolmiea menziesil, ,FAC), creeping buttercup (Ranunculus repens, FACW), wild lily-of the-valley (Malantherneum dilatatum, FAC) and slough sedge (Carex obnupta, OBL). 'Wetland hydrology is indicated by inundation/soil saturation, drainage patterns, and sediment deposits. Hydric soil indicators were present in this wetland with a peaty muck with matrix chroma of 10YR 3/1,and presence of iron concretions at a 12-inch depth. ' J a . i! Phato Z. Wetland B;photo taken facing east, upslope from intermittent stream, The circled area is one of several seeps along the slope within this wetland Wetlands C and D Wetlands C and D are relatively smaller wetlands located on Tracts 2 and 3. Vegetation in Wetlands C and D are similar, comprised of salmonberry (Rubus spectibilis, FAC+), Himalayan blackberry (Rubus discolor, FACU), slough sedge (Carex obnupta, OBL) and swordfern (Polystichum munitum, FACU), with an overstory of western red cedar(Thuja plicata,FAC)and red alder(Alnus rubra, FAC). Hydric soil indicators are present within each wetland for an area less than 600 square feet, and are a sandy loam with low-chroma (=1) matrix to a 12-inch depth. These two wetlands appear to be water tables that have been unearthed by the use of heavy equipment. In addition, these areas have been influenced PO Box 2854,BelfzYir,WA 98528 cell:360-620-061 S,Office:360-372-2421 a-mail:boad40@peoplepe.com -Lv-1J- vu vo,ii rnvci- Cfarding Hill Wetland TWC166 March 2006 Page No.6 i by the recent large-scale vegetation removal that has occurred west and upslope of the ownership. The removal of vegetation has allowed a greater than normal amount of surface water runoff along the slope, and has caused water tables to elevate. These areas indicate hydrophytic vegetation and positive hydrology, but fail to indicate hydric soils for any area greater than 600 square feet, e% Photo I Patch of slough sedge(Caret obnupta, OBL) subsisting in soils exhibiting so hydric soil indicators. Suspected Wetland E A dense patch of soft rush (Juncos e,ffufus, FACW) interspersed with salmonberry (Rubus specitibilis, FAC+) and 14imalayan blackberry (Rubus discolor, FACU) located along the northern boundary of Tract 4 was inspected for wetland conditions. This area lacked hydric soil indicators. The soil exhibited a two-layer profile of gravelly sandy loam with matrix chroma IOYR 3/4 in the upper 5 inches, and matrix chroma 10YR 4/4 from 5 to 16 inches, with no redoximorphic features. This area does not meet criteria for a wetland because it fails to exhibit positive indicators in one of the three wetland parameters. Therefore, this area is not regulated. Similar to Wetland C and D, this area is likely to have recently been introduced to higher than normal surface runoff and raised water tables due to the upslope vegetation removal. Uplands Upland plant species include evergreen huckleberry(Vaccinium ovatum, FACU), sword fern (Polystichum munitum,FACU),mial (Gaultheria shallon,FACU),Oregon grape(Mahonia nervosa, FACU), with an overstory of big-leaf maple(Ater rnacrophyllum,)NACU)and western red cedar(Thuja plicata,PAC). Soils in upland areas were consistent with Aldercwood gravelly sandy loam,exhibiting a matrix chroma of 10YR 3/3 in the upper eight inches and 1 OYR 4/4 to 16 inches. WETLAND AND STREAM E'VALUA,TION Wetland Categorization The on-site wetlands were classified per Washington State Wetland Rating System for Western Washington (Hruby 2004). The wetlands have been rated based on water quality, hydrology, and habitat functional attributes associated with each wetland. PO Box 2854,Belfau-, WA 98529 oell:360-620-0618,Office:360-372-2421 a-mail:boad4O@peoplepe.com 110-16— 10b 0y;11 rHur7- T-713 P010/040 F-299 Hardbig Hill Wetland TWC 166 March 2006 Page No.7 Wetland A is classified as a slope wetland, because it is on a gradual slope, water flows through the wetland in one direction, and the water leaves the wetland without being impounded. Wetland A scored 46 points on the rating form, meeting criteria for a Category III wetland. Category III wetlands greater than 2500 square feet are regulated in Mason County, requiring a base buffer width of 50 feet, with an additional 15-Foot building setback. Wetland B is also classified as a slope wetland, scoring 31 points on the rating form. Wetland B meets criteria for a Category III wetland. Category III wetlands greater than 2500 square feet are regulated in Mason County,requiring a base buffer width of 50 feet,with an additional 15-foot building setback. Wetlands C and D are classified as depressional wetlands, because they are each in a topographical depression in which water ponds, or is saturated to the surface, at some time of the year and has no outlet. Each wetland scored 32 points on the rating form, meeting criteria for Category III wetlands. Category III wetlands less than 2500 square feet are not regulated in Mason County according to the Mason County Critical Areas Ordinance. Due to the fact that hydric soil indicators are present for areas significantly less than 2500 square feet in both wetlands, Wetland C and Wetland D are considered non jurisdicational. Special setbacks for the jurisdictional Category III wetlands include 100 feet for an onsite septic drainfield,and 200 feet for onsite livestock feedlots. Stream Evaluation The stream has been identified as a Type 5 Stream because it is an intermittent, nonfish habitat stream. The stream is draining northerly, towards several possible streams which eventually drain into North Bay of the South Puget Sound. (See Figure 5, Department of Natural Resources Water Resource Map, for nearby stream drainages). Type 5 streams require 75 feet of undisturbed buffer with an additional 15-foot building setback. SUNINLA RY This wetland report documents the presence of four wetlands, each meeting Mason County's classification criteria for Category III wetlands, and one seasonal stream meeting the Department of Natural Resource's classification criteria for a type 5, or type "Ns", stream on the property located off of Harding Hill Road. One Category III wetland(Wetland B) and the type 5 stream are located within Tract 1; two Category III wetlands, less than 2500 square feet in size, are located within Tracts 2 and 3 (Wetlands C and D); and one Category III wetland is located on the eastern sides of Tracts 2, 3 and 4 (Wetland A). Wetlands A and B require buffer widths of 50 feet with an additional 15-foot building setback. Wetlands C and D are each less than 2500 square feet and therefore, are not regulated in Mason County. The type 5 stream is regulated in Mason County and requires a base buffer width of 75 feet, with an additional 15-foot building setback. To avoid required mitigation, future site development must be sited outside of these protective buffers. PO Box 2854,Belfair,'WA 98528 ce11:360-620-0619,Office:360-372-2421 e-mail:boad4O@peoplepe.com 1YJ-1J- v1D ��;1c rtSlJCI- '1'-'/1�i YId11f�d410 1'-'Lyy Harding Hill Wetland 'l'WC166 March 2006 Page No.8 Thank you for choosing the Wetland Corps as your environmental consultant. We trust this information is sufficient for your needs at this time. If you have any questions,feel fi-ee to call. RespectfWly submitted, The Wetland Corps,Inc_ Lee Boad Senior Wetland Ecologist Heather S.L Staff Wetland Specialist Attached: Figures Figure 1. Site Vicinity Map Figure 2. Site/Wetland Map Figure 3. NWI Map Figure 4. Mason County Soil Survey Map Figure 5. DNR Stream Map Anoendices Appendix A. Routine Wetland Determination Data Forms Appendix B. Soil Survey Text PO Box 2854,Belfair,WA 98528 cell:360-620-0618,Office:360-372-2421 e-mail:boad40Qa peoplepc.com 1YJ-1J- YJO 10�:1L rrsur�- '1'M 1'02Z/1641d F-299 Harding Hill Wetland TWC166 March 2006 Page No.9 REFERENCES Bredberg&Associates,Inc., 1999. Kitsap County Critical Areas Study Wetland Report.Prepared for Ken Feigner,Gig Harbor,WA. Cowardin,L.M.,V.Carter,F.C.Golet and E.T.LaRoe, 1979. Classification of Wetlands and Deepwater Habitats of the United States.U.S.Fish and Wildlife Service document FWS/OBS-79/31. 84 pp. Washington,D.C. Hitchcock,L.C.and A.Cronquist, 1913. Flora of the Pacific Northwest. University of Washington Press. 730 pp. Hruby,T.,2004. Washington Stare Wetland Rating System for Western Washington--Revised. Washington State Department of Ecology Publication#04-06-025. Munsell Soil Color Charts, 1998. GretagMacbeth_ New Windsor,New York. Pojar,r. and A.MacKinnon, 1994.Plants of the Pacific Northwest Coast. Lone PinePublishing. 528 pp. Vancouver,British Columbia. Speare-Cooke, S., 1997. A Field Guide to the Common Wetland Plants of Western Washington and Northwestern Oregon. Seattle Audubon Society. 417 pp. US Department of Agriculture,Soil Conservation Service. Soil Survey of Khsap County Area, Washington. September, 1977. US Fish and Wildlife Service. National Wetlands Inventory. 1979. Washington State Department of Ecology,'1997. Washington State Wetland Identification and Delineation Manual. Ecology Publication#96-94, various pagination.Olympia,Washington. Washington State Department of Ecology, 1993. Washington State Wetlands Rating,System, Western Washington Second Edition.61 pp.Ecology Publication#93-74.Olympia,Washington. Washington State Department of Ecology, 1999. Methods for Assessing Wetland Functions for Reverine and Depressional Wetlands in the Lowlands of Western Washington. Ecology Publication#99-115,Olympia, Washington. United States Fish and Wildlife Service, 1993.National List ofPlant Species that Occur in Wetlands Region 9—Northwest. Resource Management Group 11U-1J- VJO ��;lc rrsuri— '1'—'(13 P013/040 F-299 Appendix A Routine'ViV 02nd Determination Data Foray _LV_.L0_ Vu Va.IL rrSUL'J- P014/040 F-299 U. :7 M.. _Wk .J K D;.- Approximate re- x A..j-e�f ownership Location e! AU. Ile F� Olt un" V) e PA" Rod*emai 5A. A'Y 'T a fe U 7 IM 7 Highway 3 A 7. 112 7 U-1 V N &ION JA F V • AIL, a: �: : > . ... ...... 4 nam,I YLCRM Mas Project Name:Harding Hill Location: Allyn,Washington Project: 'rWC06-WI5,5 THF. Wen.AND CORPS, INC. Client: Archambeau 'W*tlmbdDd6md— MAhqtM*MXM=tP" Uid=*m Wastside Division�(360)6200&8 Date: 3/06 lri 1J vu Uj.14 rrsuri— 1—f lb Y141�/Id4l� r—Lyy I IIe VVctiand C,E re Client: Paul a-W Unda Ardianbew HardN Hill, Maser+Ca*, WA fax ParrelSo122�22594O1l-!� �^_____�� Harding N111 Road 660' ��x��-�#122322�90011 I 1\ i .40' � � Wefland I3 164' j I Ga�ctor III Wetland I � fax Parcel#122322590012 a � t�WAand eo�lated) � � i 65' 13uddkm 164' f 5e / 1 fax Pend#12Z22W0013 j Weiland f7 //� i � I t novrequiated) 164 Tax Parcel#12232Z90014 50` Duffer /� Wetland A j CateMoN III WAND 194, I I ,� 1 t r I.• S. � � �� ;S �' r^y�'"h fir.: �4�i� Ae 7 � ��•� ��11�•'�,�. J �1E 2C�-f Y�J,{� "T•]"y� 'J�l!y i r r N r. Y� 4� t•� T c r ,MINI, I,x ". - 6 _ Iw 1YJ-13— YJO 10�;13 rrsurr 1'-71 i P017/040 F-299 . t '4• e Y I / t S � .1 1. Approximate location of parcels ; M arrabdwii�ArcINS-C�ni�,I C11ec�20Q2BBRit� y Onsite Soil Type: Mderwood Gravelly Sandy Loam Alderwood gravelly sandy loam(Ab&Ac)_-This is the most extensive,soil ofthe Alderwood series. Alderwood gravelly sandy loam occupies undulating to rolling moraines.In undisturbed areas a I-to 2-inch mat of very dark brown,acid organic matter is on the surface. This grades to a thin,dark grayish-brown,highly organic mineral soil.The surface soil consists of a friable,brown,medium acid gravelly sandy loam 8 to 13 inches deep.It has a weak granular structure and contains numerous rounded shot.Below the surface soil,to depths ranges from 18 to 24 inches,is a pale-brown gravelly sandy loam that is very friable,is single grained,and contains small to moderate amounts of shot.Between this layer and the cemented till is a 3-to 10- inch layer of very pale brown gravelly sandy loam.It contains no shot and is firmer but has the same texture as the layer above. However,it is faintly to distinctly spotted and horizontally streaked with brown and yellow.The cemented tiff consists of light- gray,gravelly sandy loam,and it normally occurs at depths ranging from 24 to 32 inches.It is impermeable to roots and very slowly permeable to water.The fust few inches is usually laminated and streaked with reddish brown and yellow.Below this,to a depth of many feet,the till is uniformly cemented,fairly uniform light gray,and medium to strongly acid.A thin mat of roots often lies over the till.The cemented substratum tends to restrict the rapid downward movement of moisture-. This soil is in capability subclass VIs and in site classes 4 and 5 for Douglas-fir. The Alderwood series consists of brown,well-drained,upland soils.They have developed from mined gravelly glacial till dominated by acid igneous rock.Rainfall is 45 to 60 inches a year. The native vegetation is a dense forest consisting almost entirely of Douglas-fir and a dense understory of salal,Oregon-grape, vine maple,and huckleberry.Alderwood soils occupy the extensive rolling glacial moraines,and they are the dominant soils in the eastern part of the county. For complete soil text for this Alderwood soils see Appendix R. FIGS 4 SOIL MAP Project Name:Harding Hill Location: Allyn,Washington 'p�y Project: TWC06-Wi55 Y�THE wa LAND CORPS, INC. Client: Archambeau OGtuudDdinWtiea•H.4at.tuyrysa�PLws•A;paetauRamnuon•Mmpt$on•n�,,;,.,pw...tor Date: 3/06 F.eraiidc faividon-(509)89aos5S �Vinaiidu bidwwon•t3ob)6d0A618 -LV-1J- IOU quo.io raUri- '1'-'I'l.i rldl�i/Id41d F-299 17 8 7 1T • 7T 24' "17• 28" $ �`` will Pond , 50{ 056 8 6' I)AT 17 ;�' Q8$04 ."170MOO O5ON 17057.0 r.ir tL Fs�* - F Catfish La, �� tL -r� + s j � oQ T 5s8 ApPioX111]ate 1711 " 817 to — -- 4- Site Location j '. ;. SS. f n 1� -- i $PYsat Sauaid• 7 17 17Q f 17 1?446B�A. 1 a 17tW$8817D4 �ifl� 1� , 41 . : : 70484 1 }1 A 170464 i1.704844 �17D4i34 t170"48 1704t 40 i.0 1. a• , ,� i f fi 303 '. -•, it r-•' � `' � '' s o t � SOILS Hy dric %oih HWy TOnstable Hilly erodible S'L©PF :Ifgait I-TWUN`_e.z Medium Slope Instab� rI£g'::Es EnsdiE•la No Data or Gm,el Pi.5 Nigh Slope InstabRity STRF AM TRAN&PORTATION , `'' Stream Water Type 1-5(East side) Paned Road Stream Type Unknown(FAst side) Unpaved Road � F Stream Water Type o^� Road(Surface Unknown) S,F.NO.Ns(West side) ,W'*/'r Abandoned Road � U Stream Type Unknown yA+° 4"* Orphaned Road (West side) el %� 'Trail Water Type Change ' Railroad FIGURE 5 D)NR STREA MAP Project Name:Harding RCe11 Iwation: Allya i l Wsisbin tsn T�IR_ ' "['L.AND CORPS. �1VC. Project: TWCO6-W'1s5 W&WDdin atba•linbIMMW—twaKhat7=Rvft-6-1 ubsube• CHent: Archamboln BasM1sid�Dioisian•($09)899A355 W�9de b�'v;rion.p01D)620A618 Date: "6 DATA FORM 9 �jRevisealq WA Stab V_�tfand 0etineadon Manual ot"iM Pp-Ms W'eSand Defineatson Manual) Bate: -b( I 610(.0 Applicant/owner: County: wloio-r ltwestlgator(s): \.�AjovA State: VJA WTIR- Db normal Circumstances exist on the site? Yes Community ID: is the ails 9101TIMntli dina 4l((44- left SlIEN tdit)? No i'iftsea a. V'VULr%-d Is the area a potential problem area? No Plot ID: jN,1 Pas anation of at ieai or problem,area: uF;CffA?IQN Ifor*strata,Indicate T=tree;S=ahrub;W= herb;V=dine) Donunaut PlantSpecies "Stratum gb cover lnd'mator Dominant Plant S soles "Stratum % cover Indicator 4,- XA T a zl, 6 ;t anA ¢ s, riaa�s< et,Fi.4 � • "" ze ,a in c 3 IHYDROPkIMC 1 EGETATIO NWICATOR& Check all indicators that apply and explain below: E� Visuat obsewatlen of plant species growing irt. physiologicayreprodudhm adaptations i areas of prolonged inundation/saturation X Weiland plant diftbase ❑ Morphological adaptations X Personal knowledge of regional plant communities D TWma4 utomr<' Qf a Fier(explaain} 3'ydrephytic Vagetanon prosent?tlko Rationale for decisfonlRemartcs: 44�:b"Jb OVA-, 10 Is it the am wing ssaaar? Watermarks: Sediment Deposits: �41 Based.on: mr � DfI t LOW. t4o Drainage Patterns: �o Depth of inundation:NO t,'ai.LaAd.A�14V-1 Oxidized Root(live roots): Local Soil Survey: Channels<12ht t,b Depth to free water in pit: `>!��� FAC Neutral, Kto Water-stained Leaven. 1�-1�- r�o ��;1� rnuri- '1'-'I1;� Y10'Lid/Id4ld 1+-Z99 Check all umt apply&explain beky'v: der fexpla n): La -stream,lake Or gage data X Aerial photographs Wetland hydrology presents Rationale for decisiotfemaritrs: SOILS Map U1111 Narab. Drainace Class: vS' lQ Field observations confirm mapped type? C@Pth MWOX caolof Mc�til�*ocr!of4 Motlte abuncJanae 7sxtufe,sorrorepohst DrewittQ of&aft profiio inches MUnseft tnbist) MUrj%efi tntil$t} stEs anti contrast shudwre etc. (match desetiou0n) ID- 43904a.q3o.� ydric Solt fndfcatore: (cheat all that apply) Q f- uQ'wl 131Makitctfiratfw:g Z with names — Histic EPlpedon Q Mg or Fa Concrollons Gsuliidfa•t?d or- Q l9 h 9 Q Agific lvlbistU(B Regli�a . MWO Cris"itt f€r".rbr L;Y#F 0` tidy �ft� Q Riduah,-2 COMMOK Q Organic Streaking in Sandy Soils Q l_�as N- 5NMAt1l.OaM hW;lg Q Gleyed or Low�ehroma(=1)matrix Hydac salts presohE? , ❑Other(explain in remarks) Rationale for decleion/Remarks: t lAly2snd t nn' _Jnaflan $ HYdTOPhYtic vegetation present? as N' ft v ' pr 3nv �t7 Wetland hydrology present? f•b RatiogalefRenrarics: r^ �' Jim 1�!y:, �!.v-�/:�1 �p `aa C,4,�. •ai ' Y, t;!7 G. K'� M072t�7� 1{0-15- 100 10y;15 rtsurr T-713 P021/040 F-299 DATAFORM9 (Revised) State 1rf ttanti i t ManbW ar ISp cb blPet#artct Delineation Marc rl) A � ;,�f'r of�-is +r- DatII� `�11WOO' Pplicantlowner .,• ,,.. •;.: tee._M County: O tllvesligater(s): StSf&: Do narmat circumstances exist on the site? Yes Community t0: $tea:r �iii ll;the Sb Wrop-Am dwilaw yout xiluxi ny? No Is the area a potential problem area? No Plot ID: ,,�,� F' •t� � A anatlon of of last or blem area: -429MILgW 4For*strata,Wioate T-two;6 H=herb;Y=vine) Dominant plant S ales *Stratum %cover Irrdi�eat+ar Damlrsanf Plant S ales "Siraturn % cover Fndicator �. %OM&WHOM D$L,FAOW,&FAM "' c>' Check all Indicators thai apply and explain below: EY'Virsual obseriation of plant-species growing irr 0 PEt'yslologicallreproductive,adeptations awas of prolonged inundation/saturation X VMnW plant database 0 M' oWcal adaptaWns X Personal knowledge of mgional plant communities 0- T-aOiteratp Other(e.*stnj Hydrophytic vegebtien pm; �S, Rationale for dec'rslonikernarks: =x ;> .S• g=a;�a• ,g, �;. ,t��,, �: �; WDROLO Is it 1119 arm"season? t.,Ao w81ai'1K&rfm: ^. : Sedimen-l posh : t. Qrlit Lines: DFaInage Patterns. . T Depth of inundation_ ear A Oxidized Root(five roots): Local Soil Survey- ; Channels<t2in Depth to free grater in pit: FAC Neutral: %4 Water-.5tained Loaves,- MOW,. r.• 10-16— IOb IOy;15 I EUrl- T-713 P022/040 F-299 CF�c all that apply&explain Wow: Ottw(e ka): L, Stfsam.-lake or-gags data X Aerial,photographs El iee�evf• Wetland hydrology present? Ps Raitoriale.for docisirlrr:rernarks. � ► n , , � < s ll,jyl,�liti'� Gt,:ti.(A S•.,,.r C1h.+�ti..R !„�et�.••h,�i'?S�i +�u^,s\v'^C�Z,tIWi^ J MAP Unit hiamb, )kUv/W i 2Ik ,� � � i raitta iasa: V "dL'✓ojuv-J i,,t,11,, 'f`► Field observations confirm mapped type? N(,;C3 Depth Matrix color Mottle v9101s Mettle abundanoo Texture concretions, Drawing of soil profile inoh®s Munsell moist} Nuns mofsf� size and cordrest structure, etc. frnatch descripti00 l `" A Aotivzst i w�titi Hydric fall indicators: (check all that apply) HistcsQl L�1 sttc�pipedon 0 M �"9 3 >nattdsa ©Mg Or Fa Concretions • •ao?€ •��. �t'dtl�lt�r�.�r�€�lt.9i'�•.ft•�ut>'°..�:��cT���dy�tl� 0 AgUic N ature Roglme Organic Streaking in Sandy Solis Rc` r3 C�7rdiL`8tt= 13 LWW cn ya ail i3i tdlydn3 Su-N LW 2'Gieyed or Low-Chroma(=1)matrix ❑Other ex fain in remarks) Hydric lofts present? 4,e3 Rationale for decision/Remarks: ._.__.�--_�—_ ._.__.._...._�.—. _.�.� �� '�L,�.�Ldw•G. a�+•wrr- � ��w_�v�'�•ca,. av+a�' x3c.. WedmW belerminadoa HYdruPhYtic vegetation present/ '-?.c l-;Y�solf* 5 Wetland hydrology present,? S la-tfta-8 —1y i �R zi"vt+ at�i`i '`I�C RationgleJRemarlts: ,S c:(��,c di.` c�civs' •t� - c c� �� �f'�.i..f.c..�. •a t �.� �y: �,�^.". eiLG 4 vVLA64,o..j 110-15-• 10b 10:15 11huri- T-713 P023/040 F-299 R-MM00 MOW UsUrs iinedw DATA FORM 1 (R®vftQ4 WA State Vhdand DagnwHon Manmil or 1627 Cons Wedand DOi-imt-ion Manual Applicant/owner: kvd&�vvAv-AAk County: yVlaLttn fnvestigator(e): )A . .vu. GjQtW. \*.)A 61TIR� � zk 1w Do normal exist on the site? Yes Community ID.- J;,44, ts- Ifta situ i'ivr.ioafy'ftfun—n— d(013000 sffimb I Na Tmngoat ID:4p, Is the area a potential problem area? No Plot ID: �,•��a-l�� Y:x fanation of al fcal or gMbfern area: . T.AT11 (Fgr*s#rata,iadii`�te�'=tree=S=shrub; 3 hertz;V=yt!t+�) Dominant Plant Species `stratum ' cover indicator Dominant plant u0scles *stratum 9b lover indicator ,PctaL a k• = i;, iit AJ7 - Ae of t3MitiaM OBL,FnCW,lei FAD 69b " 110 Check all indicators that apply and explain below: 0 Visual Observation of plant species gmwing in f� Physiologlea#freprodw%ve adaptations arcs of pwionged inundation/saturation X Welland plant datalbaw 0 Morphological attaptatlons X Personal knowledge of regional plant communities EJ T-6ohn t6al,Lftwatum 0 Mdc s r"afn" Hydrophylk vagawien pmsert? i,W Rationale for dedsion/Remarkw. C Saj, , 14YOR©LOOY Is it II'm growing stason? Nw Water Marks, KL a �e�#trnartt LQ-poslis: Owed on, Drib Line& Patters: t O Depth of inundation: JA4> �vti«v,Az1zct,, Oxidized Root(live roots): Local Soil Survey: Channels--12 , Depth to free water in pit: 1�p FAC Neutral: 1Ma Water-4talned Lzave¢: i cS 110-16-' Ub 0-4:1b eNUM- T-713 P024/040 F-299 Check all that app}y&eWmn L-eltw: OW-er (ettplaln): M Stream,.lake or Q"g data X Aerial.photographS- Q Ov Wetland hydrology present? ti RatiOraie,fOr decls%tsWretrtltitcs: AILS a� Map Unit Male: MA"Y'roWA suyt' E-f Dutimp Mass: wed c�a u.0 Field abseroations Confirm mapped type? Yc< Depth Matrix colot fl-OMO colors MoMe sbundanora Toxturs,concretions, Drawing of soil profile inehes -Munseff moist} Munsell mots size sees!COMMAstruc structure, sets; match des ri Bart}� . Hydtic$a[liume4ors: (check all that appiy) - - - - - — Higto�vl ©Meft chroma s 2 with mottles Li Hisft Eptpedon ❑Mg or Fe comretions �•�t+ititii=•t�dor• [Q Aquic Moistilre Regime Q-l'ilV}t.t p Organic Streaking in Sanely soils 0 Reducing Co+�dttttittet El l! on1i11it4erixefJLt;�'!Hydrit;R�ls`llsi! [] Gteyed or Low�Chroma(�1)matrix Other ®xpiain in remarks} Hydrio Balls ptmsontt? lad Rationale for decision/Remarks: V9f and adore HydmPhytic vagetation pre%ant?)-A-C> Hyddo sollo pwart v 1-L0 Weiland hydrology present? (Ucp 'ffi'fka a"�t'ri'pliEt ar�irt63�"t�'r�'SoatfBrri+� �.Q RatloreaiefRernarks: NOTM: T;k- 0'ak ��� 6� t-awdwa. � vu �G�u,�.vL e,��.�1 0 ►�. '�..� 110-15 IOb MI:1b rtiuCi- T-713 P025/040 F-299 DATA FORM 9 ulsad) VJA Bute Weiland DWinaa db n Manual al or 1987 o WoVand Delineation Manual) OEM Applicant/owner: , County: .amrmt, Do normal elreurnstanres exist on the sael Yes Community ID' l 5i; igit`c '�3 ty d �`csi d�� � uacaui No Tranna m; tva Is the area a potential problem area? No Plot ID: vv-At k ExplanOon of atypical or ptoWem area: (for"'etrate,indiMe T=tree;5=shrub;t•�I=herd 1�=bite) R minant Plant 5 ecles "S7natum %cover Indicator Dominant Plant Species "stiatum Na vover Indicator A. ,t�b r.. i Check all indicatois that apply and explain below: [� Visual observation of plW-species growing in 0 Physiologieai/reproductive adaptations areas of prolonged inundafion1s4*iratlon X VW'anU plant dafabase Morphological adaptations X Personal knowledge of regional plant.communities T-#F.4.—JO* ft- ralt �' i�t(axPi$id3 Hydras Motion� a `ttis Rationale for decision/Remarks: -2 Is it tft umwfna man? t�(,� VVMT A►lsfi{?:��c, Sediment i oW.Ra, Based on: QdR Lines: �� � Drainage Patterns Depth of inundation: w Lt-(.OcL Oxidized Root(live mots): loom Soil Survey: J\b Cttann8ls<121n. �a Depth to#tom wajer in pit Opt FAC Neutral,�t S Water-stained LeeveG: �t } Depth tQ*sturafe&.i.svif= © � J 0;1b MUM- T-713 P026/040 F-299 ChOCk all that a€pAy&eWzd-,l balav-r tither a Stream,lake osgaQs data X Aerial Photographs t 0 ctil 3 Wafland hydrology present? N6 Refidfiale for decialonlromrit.: SOILS Field observations confirm mapped type? Depth Mabix color Mottle ooiors Mottle abundance Texture,conoretians, Drawing of spil profile /.,�iriehes 'Adunseti moist Mun1041 rngi ' s12e ft"d eot*ast sttUCWFe,etc. (Match descrfgoott) V ✓✓ .bs• ..Yr �;• rr Hydria sails lndicaft : (chook all that apply) -- 9 HW"94 0 141NWX r-hMf M vyl�lt.s339 y� 0 Hilflc Epipedon 0 Mg or Fe Contradons 0 Aqulc Maisture Rsgime ❑Organic Streaking in Sandy Soils 0 RwBtclrtg a;owff LMM tin Ma-VUnhtrl o-i HYMa Uft U-9 0 Gieyed or Low-Chroma(-1)matrix ❑Other ex lain in remarks) Hytltic V*Ii s present'i N Ratio vale for decision/Rernarks: kdt�,r.••, a�i�:tttl� HYdrophypC vegetation present?WA rlydit soeq prod ?1,1.0, Wetland hydrology present? id 2i"la`"i;i"srriuifn ntf'a'v+iac�ar�.' RatlonahalRernarks: NOTES: -K, 1u GA- d �,�. T �� 4- IU-10- WO Uzi;10 rmui7- T-YIS r1d'L'(/1040 r-L`Jy t �:i9i �aj3'Deters ffir6 doff DATA FORM 1 (Revised# WA State t llanci DelineWon Manual er 1987 Corps Wetland l ellnead6n Manual) I3rcr a )tt: � DOW bI�W 01.. Applicant/owner: WOOcow County: V-1j #.50v Invesllgator(s): ,�- . LO-V'-f, state;vVA Do normal elrOUMSjaneas exist on the site?, Yes Community Is dYi0 946 9WIMOSY distuibed(a—Waal abg— rj)? Ne TWOU ID: Is the area a potential problem area? No Plot ID:` 4 irx )anatlon of leaf or prob6m area: A—GUATMU t,For*strata,indicate T tree; S=$i'rrub;H=hQrb;V=vine) Dominant Plant Species *Stratum cover Indicator Dominant Plant Sp *Stratum °,5 cover Indicator tf • 9 Sr• �' �l d 1 w t %3f dorriiftlit is OEL,FACW,&FAc-. `j 5j Check all indicators that apply and explain below: (d Visual observation.of plant speeies growing in ❑ PhyslologicallreprodueUve adaptations areas of prolonged inundation/saturation X Wattand lint dateban 0 Morphaioglcal adaptations X personal knowledge of regional plant communities Ef T430nift LWattti Q bier(explafn) Hydmphy.nc tilrtWort Rationale for decision/Remarks_ �s�° ( �f G ----- !s it the growing season? t\:o water mart- KL o aadimant Depoa ts: Based oo: 064 Lines: KO Drainage Patterns: Depth of inundation: L �1 I Oxidized Root(live roots): local soil Survey: 90 ti Ghanneis c12h Depth to free Meter in FAC Neutral, � � Water stsiniW Leaves: u 110-16- 100 10�j;1f VMurl- r-(13 Y10'L�i/Id410 r-'Lyy Check all the apply&explain below, Other(exphda); C- Strom,.lake or gage data k Aerial ghotogmphs Q Omer Wetland hydrology present? Rath t&Ee for d t lSiortlretptaft: su C'A-� — Map Unit NAF46: y�,-L�t W0,4AI �u��, 9-&4AL j Dram a Class: W&- �.wzti laa�.W� Field observations confirm mapped type? a Depth Matrix color Mottle colors Motile abundance Twduro,eoncredons, Drawing of soil profile lrtehes (Munsetl mo Evluhsett mW size and contrast: structure, etm ftgEt h Beset Ion) •o'�Z .lc�_� � •wul.e,� fly fie Soit Indicates: (cheek all that apply) 0 mistowl 0 mata x aroma s 2 VAft mottles E3 Ftistic Epipedon 13 Nag or So Concret{orm YSum ic•odar. Q High rOE1~ at.vanay SWE� (•Aqulc Moisture Regime Q Organic Streaking in Sandy Soils 0 Redualrtg Cant"07m [7 L6Ud an P+t�Yle�aiii,`l. l Hydrfg butt$tifif @"'Gleyed or low=Chroma(=1)matrix ❑other explain in remarks) ttydric wits-pre"fit? YLS Rationale for deeisionlRernarks: � kt ai.c �- Wetland nglermtt�;ion Hydrophylic vegetation present?'�GS Hydrly soil$pmotit? Wetland hydrology present? f:£•tfe•sdiftgm i RationaleiRmnarks• S i irc, L1nt�l.c r �.r;..c ri Ida?Tl^OS -PLD� �f�,% �y 10-13— 00 MI;16 rriuri- 1'-'I1� Y�iLy/ID410 r-'L59 ��e�6 �t� r.q �,i�ll.PslisEs� i�4 �f0 DATA FARM 7 (Rovised) WA;bye Wdlaud neiensa*m Manual or 1987 Cora Vbdand Delhwallion Manual Prt?peo :t-6,V14.1 ' ► .DWIME Applicant/owner. A-4Wo wS>�A County: lnvesilgator(s): state: wi-� SF1'/R: 3 �l C2.1'W Do normal efrouM$tanoes exist an the sita? yes Community lt�:fctrr��k�41wu.� a ft ift agnmawy dm ru`i1'itd Oi FAI&dAgors}? No rwwa ax Is the area a potential problem area? No Plot ID:t (�t,vu� Explanation of cal or problem area: NEGIETATIAN Tor*strata,indicate T=tree;$=shah;H=herb;V-vine) Dominant Plant Species *Stratum % cover lndloator Dominant Plant Specles "Sti"dWrn %cover Indicator r � T us At's ol w S HYMOPHYTIC VEGETAAON If WICATORS: gib of d0m-Mat%0 DBL,FACW,&FAC: Z oak Check all indicators that apply and explain below: Q Visual.Observation,of plant species growing(n. Physioldgical/reproductive adaptations areas of prolonged inundationisaturation ❑ l4Aorpito � 'We�end plant database adaptations X Personal knowledge of regional plant EJ T€chnl "eratu g t communities Q' Oftr(expt`sin) ttydrapbyus v t3o»prae�na �l�o Rationale for dedsion/Remart ; HYDRtit.E3G is it the growing season? N6 Water marm Sedirnam Vapoalts; �(,o Sgised on: ftk,-Aj1rt1n [MR Lines: ( Drainage PattoM- S: �(o Depth of inundaiton: o; 1�4ua Oxidized Root(five roots): Local soil Survey: o Channels<12NL Depth to free water in pit: 'S�b� FAC Neutral; �� W®tar stained leaves: �O 0 Depth-to Satitrhtt'_d_ elf:. 7 1U'-13- 100 ��;1t5 rn�r�- '1'-'I1�i 1'10�10/10410 l'-Ly9 Check ai1 that apply&explain below. Otl�:r te�lal�): 0 Stroam„lake or gags data X Aertal photographs Q OffW Wetland hydrology present? y-GS i Ratiertg#e for E0dsi0rlfrdmiAf'lf8: -�v1.�.v�t,� �� �GC�tts�t,�.j •U��.�1.t-t�Zs,�C �6',r+��-ir;,..u�E-.. $ l4iieP Urllt Name: Field observations confirm mapped type? NLO Depth Matrix coler Mottle Mors Mettle abundance inches Texture,concretions, Drawing of soil profile Munsell rmn Munsdil moist` size and contrast _ stvcture etc. (match descri ion) '.S`rL FCw i du tme �t t�e0 lcrhkVl Hydrfc gal lndicawm: Eahec-all that apply: -- El Hictowl EJ Histtc Epipsdon ��c uhrma-,5 2 with sables e'9Viflctc-0dor• �or pS Commons CJ Aquic Moisture Regline �fgft WORM#Contspt,lrt attf'1'#v*Layor of.: l"T ClOrganic Streaking in Sandy Soils��.oirf�Go�itiarr� Q LiiW oil hfj4Fdri$1�.�aJ Hjt'ait'IG lt�iia l_igt WGieyed or Low-Chroma(,1?matrix Hyr�rl�se##x prnt7`�t,s Other favftlain in remarks) Rationale for decision/Remarks: ,�V ilV C.ILVVIpt -{�- i tland�ert�" �l�.l.(, cfs6tty � �"tt•V+�'t,lAJtg .�._, ttrta'tiatt Hydrophyrfc vegetation present`- %j t-S 3 iydrle salts prosent?44-e Wettand hydrology present?`.C, Ratianaf�IRemarks: 110-1.5— Idb 10J:ly rtiurr T-713 P031/040 F-299 DATA FORM 9 vl WA State Wedand Delineation Manual or 9887 Corm Wetland Delineation Manual) Prc�actiSit�: �,cti�-S N�• ' s��z: Appiicantlowner: Avr)-W'+kgLkk County:*t.. -S6" lnvestigator(s): ,,.�,p State:%,wy� 1. sr IR; -�-attaars k\,V Da normal dreurnstances exist on the site? Yes Community ID:hwbkU6\A-5 is eno ske migam `f v awfiffud(ttwam a `maw)? NO rrr `4 W a 1,'0: li Is the area a potential problem area? No Plot ID; lays 0a of atypical or problem area: YAOETAT10N (For Vrraa.ladioats T-tree;6=abrub;H=herb;V=ding-) Dominant Aunt Species *stratum gb cover Indicator Dominant Plants Iles *Stratum oover Indicator bkA I L U U MROt°HYTIC VIEGETATIoN lN©ii ATOR$: %Of&rt-414 s f5$IL,PACOW,a FAC' 7'�')o Check ail Indicators that apply and explain below: [� Visual observation of plant species growing in Physiologlealtteproductive adaptatfons arras of prolonged inundation/saturation X vNiland cant data [� Morphological adaptations X Personal knowledge of regional plant communities Ej• T-30hrdM-Lt tur* �' der{oxpl in) Hydra"Yfi><VnetWon P nt? Rationale for decislonlRemarks: HYDROLOPaV IS it em omwing season? { tester"l-affrs: wv s :z art t3er.J03I`ts: Na Based on: " V► &l Ddit Lines: No Drainage Patterns_ 'YGS Depth of Inundation: Otddlted Root{five roots}: Local soil Survey: (�(„ Channels.c l2 h Wo Depth to free water in pit; U FAC NcWat �(o Wetamtalned Leave.*; 1\1 Clepth.te aa�rated.�i� t) 110-16— IOb Ioy:zo rHUrl- T-713 P032/040 F-299 ftwc all thig apply -axplatr b;, a Wtream.,lake or gar,data X Aerial photographs 0 Gmv J Wetland hydrolODY Present? 1`l Rationale for dacjsI,0nj mgfks:�U ��t��s+,,� �ir��••- sots map unit INk ia: p vv -6-A ,Avt,'lou S & L� � l o�.Mn t t�ral�,aaa Class: v�,t� Figfd obtcrvatisns cortfimn mapped type? ,� r . DVM _Matrix oCior nAc#ti4,Sorg M9rile abltndanoe There, 6�tktretkNts, Drawing et soil�ra#8� finches Mttns�eIt moist) (Mubsell insist) atze and rayyrdr8st stnsetui e,l aba. ( {��h descrf tibn) - r. 17 JG SaLn�°I Hydria$01 lntlicaOrs, check all that t -- Ftisiic Epipedon Mat*4uwm s� n�gttlraa summe ter• ❑leg or Fe Conct"ons 0 Agula MoIgUre Regime H 1.0h,0rov 0 C*n ant I-5Wfti���i ftr,-dY El RWttc'iitg wogfto?w �7 Organic Streaking in Sandy Solis 13 W(s vn hlatlonaifL ab;i4ye�1'ic'8aNej Lj 13 � Glayed or Love-Chroma(---I)matrix ❑Other Hydrio sails�osif� ��, f®xpiaih in remarks) �R�/a^tiionale for decision/Remarks: i\LO eftEMi[tatlon HydrophygcYegetatiart present'? NLJ "Wrto 0Mmv Nu Weiland hydrology present? M0 i '#fta-� rr f -Sint vvl` in a''vmbandT o RationalelRetnarks: a 10-ItS' Ob UJ:zl kHUM- T-713 P033/040 F-299 1n -4 am ant-D0 ffW a r&L;-(Y f.0 DATA FORM 9 (Reuikerf WA State We0and DeNneatlon liftival or'1887 Co Wetland Dellneanon Manu8i �_� •���: 3 lac�I vL. Applicantlowner: a��!�E1 ,oR. County: tnvestigator(s): q.La.k, slate: �-q:y Do normal grcurtrtstancas eylat oil the site? Yes Community lD:Fj'vts1j yVvvu l; t e sli ;ti9MMy fthrrcUd(AW&N man)7 t16 i imp ID! Is the area a potential problem area? No Plat ID: Ex ianafion of a "cal or Problem area: V +t MT-110M Wor vrata,indicate T=lgs;5 6hruln H a lei;V Dominant Plant Muler, erratum %cover indirotor Dominant.Plant cover lndioatoi Aao7G1 r- 1 �; Ctv L t A- t. WDROPH"c vEGETA't IOf-i IND(CAvoRs: - - - - - c�#cf rrsittasi1 OBL,FAt , &FAC; L b Check all indicators that apply and explain below: 0 Visual observation of plant species growing in Q Physlofogicallrepmduetive adaptations areas of prolonged inundation/s$turation X MOWd pfsf3#dZt9bM CI Marphoiopical adaptations X Personal knowledge of regional plant communities (� Omer(exptsI&I F ationale for decision/Remarks: Hyg oho Y - - -- -- - ' rt tlta a t meson? I\Lo � i Ot triter: ��,� 8 #3�ri8iPd S}SicS: Gs Sec#on: WWI Drift Lines: NO Drainage Patterns: '1 a Depth of inundation; � , Z;�Lia{'mod ` G<rt O4dized Root{live roots): Local soil Survey: R� �t Channels<'t�ct �j o laaptl3 to free water in pit; 7'�La FAC Neutr'sl_ Water.Oained fi �� ii•tr s�, retgdd•�il.. �� �.T. 110-15-' IOb fly:zz IIEUM- T-713 P034/040 F-299 Phook all that aWy&OWWn belOv: tt3er(sx ain): Q. S"treamdake or,ago data, X Aerial photographs 001 Wetland hydrology present? �ti5 Rationale for itedsionff ema SOILS map Wit Name: ��� Dfaii @ Claw:vveu c� � .du j 10 0.111/1 Field observations confirm mapped type? Depth Mat X color Motfie colors Mollie abund a TeMure,concretions, Drawing of sell prn�tz itches Munssil in0i ilUluhsetl cnolgt size and coi*ast struou",eta. fmatc�otlbtion) �O`$X2'-�l ► -SA, Y 16A.r0 ydrfn Goff M410ators: (checkoff that apply) - - — 0 idlsrAwi C3 Mahic uhronP3 s 2 vAh n10?as 0 H€stic lEp€pedon ❑Mg or Fe Concretions 1�' sulftdic Lzdor ;3 Migh 4rganfs CCr�l�t€n SuT�co t ayo€+of a id�clls C7 A4ufo lillelsWre Rsgifne Q Organic Streaking in Sandy Soils Wf ouaalii4 Condtions Q Li tYfr USOMMUL"91 HYW.e 34rfW Liar Gteyetl or Low-chroma(=1 j matrix j]Other(explain in remarks) Hydrio soft pt6sebt?".(-C S. Rationale for decision/Remarks:ILL ,y � CY )rwJva Y Wettand 13eter� gq&oft L vegetation prssent?fasesltt? � 5 ology present? Y•r5 ,.49"'31ft� S.-f iit,8"tii�tl46o.}'Fes- marks: ?p LUAAk "N�t1rGC jf 4rM,�Lt,�� OM: V[A- 1� .� W,,,n CA +a te t � C� u)O oTi 110-1a- or) MI:LS rhurr 1'-'�1i rld�5/1041d r-�yy R Uffe bumd Deter- DATA FORM 9 Otavism* WA Uate Weiland beli'neadon Manual or 19#7 Corps Watiand Defifineaftn Manual) Applicant/owner.- County:Wto-s 'n finvestigator{s): t Stato; VA SITlk3: fv-kw Do normal drournstances exist on the site? Yes Community 113:�rr Y the Opmair y dimmed lW061 81MANOW No Tfffflmd ID;.D is the area a potential problem area? No Plot ID:MdU` ,FA Ex f creation of at cat or Problem area: VEGUT TIM (For**ate,iredWte T;--heel S R slembi H a heth;V w viniv) Dominant Plant ft2gLes *Stratum Dover ineeator Dominant Plant S eves *Stratum %cover indicator ;YOROPHMO VEGETATION INDICATORS! - -- - %af dcrminartle 08L,l='1tM.a PAD: Check all indicators that apply and explain below: ❑ Visual observation of plant spebies growing in [I Physlofogleailreproductive adaptations areas of proloNed irumdationlsaturation X Watland plant dWabase 0 Morphological adaptations X Personal knowledge of regional plant communities E` -rwA Htt a1•t:Kr mw* �' der�expilxi'n) YIID'dr�f�5�3rsa�ta3lt�put8l�.c� Rationale for decisionXtemarks: FAG / IROLOGY - - - — — 1s€t me gang segsryr? "Amer Ma&-& JN6 Satilmetd Depostte; Q`�a Based on: `�n drift Lines: Drainw Flotems: 9-o � Depth of inundation; s`t VA S Oxidized Root give roots): Local Soil Survey: d Channels<12n o I Depth to free water in pit: FAG Neutral. Kv Water-stained LeaveN Deptks.to tratiia. �1 6,0 110-1�- 00 IOy:L4 rtiuri- T-713 P035/040 F-299 Check all that apg(y&explain babas: Other(explain): Q Straami.lake or gage data X Aedal Photographs EJ tip Wetland hydrology present? Rationale for deefsiottfrernarks: N,b L� pve eY SOILS Map unit tiine: ��ah TAB Drainaca tiles: jovl:iGY� Field observations confirm mapped type? e� • ?:vats it—'" ._ 00pth Matrix rotor Mete colors Muhle abunt(mve Texture,concretions; Drawing of soli proTils finches Munsell mot Munsell tnofs size and comrasE sbucture, sba install dese' lion) d- Lf 0 .............. ................................. Hydrib soil ladic m: (check a8 that apply) -- - 0 Histozol 0 P,4eh*uhranm S 2 roles 13 Hisfic Epipedon ©Mg or Fe Cuttarelians 0.141911 CNVaitiv�on�nt ir't•�ut•t�e•,�y�'oi•��uy-��1� ❑Aquic Mofi§ture Regime Q Organic Streaking in Sandy Solis ❑ Gleyed or Low-Chroma(=1)matrix C3 other(®xplain in remarks) HWHe soils omsent? I\Lo Rationale for decision/Remarks:14a �y - Wetland DetQrmins3'rtm Hydrophytic vegutation pressnt7 Welland hydrology pres®nt? PAD is tRa S�rri i�-'�61�f4b�itR't3'�i.�f�l{a7'�b RationaWlkemarks r #1wS: 6�1 �oG.,A c 4V\ -�MG a j S4, �� 'l �•t►- i ( V.VL2�(�' 1,4 C-�Y V) " . 110-16 1013 IMy:45 rnum- T-713 P037/040 F-299 Rif' eld V~Mwafta DATA)FORM 9 P?euiseq WA Oland DeBneat ion Manual Or 9881 Oops Welland bei;ineat ion Manual) VIMD&te: Applicant/owner: o�; County: VVW&N Investtgator(a): �, ,.� state; WA Do noMal draumstances exist on the site? Yes COMMUnily 1D: 5VWv Aa li#,fie M oaff ` dandy-"' (gr'yw.31tilikR rh)? Pja Tmasm tO: I> Is the area a potential problem area? No Plot ID- L Ex anatfon of aE pkal or problem sma: M9 9 ! (For*strata indic-Mg T o tree;S=shrub;H=herb,V=yir Dominant Plant speeles *stratum %diver Indicator Dominant Plant fteiojes *Stratum Flo cover indicator e �A du Ilan ILA r�_.�.- WORt7PHYM VEGF-T k'nO 4(NOICATORsi - - — ct#dori f'Afift OBL,FAO'dt?,&PA. Check all indicators that apply and explain below. a Visual obae►vatfon of plant species growing In El PhysWooleaftproduebve adaptations MOM of prolonged inundation/saturaflon X yM0114nd pl damf e Q M OM11ologlcal adaptations X Personal knowledge of regional plant communitles ' Oftr�encpfgsn)' Hydr-al*ya-veVctWm W c Rationale for decisioNRemaws. jq Is it the graMng saason-t B elf on: "I Drift E.lnm f\6 Drainage Paftrns;iAA Depth of inundation: N;A Oxidized Root plve roots): Local Boll Survey: tdo Channels-c i2 R - v DORM to#coo wat*r in pit: -7 l�a FAD Neutral: Nu Loaevs,%;. PAo 9avti}•Eo sat���tasi• il;. �7 r 110-13- 100 W1 J:4t) rnurl- T-'(13 F038/040 F-299 Check all that apply&explain below: ether(explain): 0 Stream;,lake or gage data X Aerial photograptig Q• Omer Wetland hydrology present? L Rationale for decisWrsmaf'tW OILS - ----- map Una-dame: AlhN►rm 1, sv41 Ow"Dot Oulu: !�. Field observations confUm mApped hype? umxv�, Dept Matrix color Mottle color* Motu*abunda rm .T"rq,concretions. Dra wing,ot soil profile inches munself moist munsaff moist size and contrast stntcture etc. (match deEariplion} Hyddc$Q insiedbm: (chebic all that aPOY) -- C)•Hiet�vi Q.11�4r�.d,►•vrr���,Hith•mottl� Q Histiv Epipeftn Q �� Q Me or Fe Concretsons Q HO C" C-OnnM to>°rti"*m Lw;w g gtm1y 1911i: El Musa M612hire Reglirio ❑Organic streaking in Sandy Soils QR� $•Cottt tf�srt� Q'k€3�va v�'idBg�Pl$ifL3�aiHyvPfcS�tsLia�t• Q tsleyed or Lomr-chroma(-M)matrix ❑Other sx lain in remarks) Hyddv Saito p m cant? 1",v Rationale for decision/Remarks: 00 WeI1294 Determingdon HYdrvPhybc vegetation present? `1 6 "rts soP-p N 0 Wetland hydrology present? j�p It the WAdilfil c�rltt W t if�r v�ttd7 a Rationale/Remarks:tj t &A tims-. TIC,+ C>C-k--Q AZY�CaJ CAvLVCL<+ "-C,("/ \mst �v�>,un.d.a�'i�r\ o�i c�•Yc��,v�.ce r� �. ��L�� ��,�-��mr► �i✓� �� G(M-t�.l.��,�1/W'',- �1.eli/C„ 1/'•�,-�" '1'•� ��;•C�;,j�►•c.r.�s ��r�tbd„p�,•�*�,.� � �•��,,VL-C. 1�-1,s— goo ��:co rrsuri— '1'-71;� Yld�iy/10410 r—'Gyy Appendix B Soil Survey Text ALDERWOOD SERIES The Alderwood series consists of brown,well-drained,upland soils. They have developed from mixed gravelly glacial till dominated by acid igneous rock. The imbedded gravel is mainly granite and quartzite.Rainfall is 45 to 60 inches a year. The native vegetation is a dense forest consisting almost entirely of Douglas-fir and a dense understory of salal,Oregon-grape,vine maple,and huckleberry.Northeast of the Hood Canal the understory is mainly rhododendron. Alderwood soils occupy the extensive rolling glacial moraines,and they are the dominant soils in the eastern part of the county. The Alderwood soils are associated with the somewhat excessively drained Everett and Indianola soils and with the moderately well drained Kitsap soils. Shelton and Hoodsport soils differ from the Alderwood soils in that they have developed under high rainfall and from glacial till having a much higher content of basic igneous rock.The Shelton and Hoodsport soils are more reddish throughout the profile. The Shelton soils are usually deeper to the cemented till than the Alderwood soils. Alderwood gravelly sandy loam,5 to 15 percent slopes(Ab).-This is the most extensive, soil of the Alderwood series. It occupies undulating to rolling moraines. In undisturbed areas a 1-to 2-inch mat of very dark brown,acid organic matter is on the surface.This grades to a thin,dark grayish-brown,highly organic mineral soil. The surface soil consists of a friable,brown,medium acid gravelly sandy loam 8 to 13 inches deep. It has a weak granular structure and contains numerous rounded shot. Below the surface soil,to depths ranging from 18 to 24 inches,is a pale-brown gravelly sandy loam that is very friable, is single grained;and contains small to moderate amounts of shot. Between this layer and the cemented till is a 3-to 10-inch layer of very pale brown gravelly sandy loam. It contains no shot and is firmer but has the same texture as the layer above. However,it is faintly to distinctly spotted and horizontally streaked with brown and yellow. The cemented till consists of light-gray,gravelly sandy loam,and it normally occurs at depths ranging fxom 24 to 32 inches. It is impermeable to roots and very slowly permeable to water.The first few inches is usually laminated and streaked with reddish brown and yellow. Below this,to a depth of many feet,the till is uniformly cemented,fairly uniform light gray,and medium to strongly acid.A thin mat of roots often lies over the till. The cemented substratum tends to restrict the rapid downward movement of moisture. Use and suitability.-Not more than about 5 percent of this soil has been cleared and is used for crops or pasture. Most of the cultivated acreage is near the inlets of Puget Sound in the vicinities of Arcadia and Allyn. In this area the Alderwood soils are associated with the better agricultural soils of the Cloquallum, Sinclair and Kitsap series. Hay, small grains,pasture, fruits,nuts,grapes,and berries are the principal crops grown on the Alderwood soils.The lack of subsoil moisture damages crops in summer. For this reason, early maturing,short-season crops are suited best to this soil. Yields of all crops are usually fairly low because of low fertility and the dry summers. Pastures produce good forage in spring and late in fall if proper plants are used and management is good. The deeper soils are suited best to fruits,nuts,and grapes. The uncleared and remote areas are lYJ-13- 00 wj:4r MUM- 1-fli YId410/la4�a r-Gyy better suited to forestry than to cultivated crops.Nearly all the uncleared acreage is in second-growth forest 70 to g0 years of age. Shallowness to the compact till often inhibits growth of the older trees. The soil,however,is well suited to production of Christmas trees. Douglas-fir readily restocks in thick stands containing trees of good form. Stands of small trees are often thinned and pruned to nuintain good form of growth.the growing Of Christmas trees has eXpanded rapidly in the past few years and is now one of the important industries in the county. It is one of the proper uses of the cutover lands that are not in a high site class.Alder-wood soils need barnyard manure, green manure,nitrogen, or Iegumes to maintain a fertility for crop production.Phosphate fertilizers and green manure or barnyard manure greatly improve fertility.Nitrogen fertilizer is often:applied with barnyard manure or when cover crops are plowed under. The fertilizer furnishes additional nitrogen needed to hasten decay of the organic matter. This soil is in capability subclass'Vis and in site classes 4 and 5 for Douglas-fir. Small areas along-the border, where the soil is more than 32 inches deep to compact till,are in site classes 3 and 4 for Douglas-fir.