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* I <br />g^e, Sfnc, <br />Qray &iological Co/isultmts Qra\j ~ l^resident <br />DATA FORM-ROUTINE ONSITE DETERMINATION METHOD <br />netd lavcstiiator: Jerry Gray ]>ate(s)oflnres«igatioB: Jvne9,1999 <br />Projcct/Site: Located la SactfoB 30-T.118K-K23W.W,HaaaBplaCouoty,MN and within the Miaiuhaba Creak Watenhtd. <br />Appikaot: Mr. Chris DkicmllOOTowBUneRd.,MaptePlalB,KKSS3S9 <br />Plant CtMBiBttaity Area WcIlaadTypc <br /># Ctrc39 Cawardla <br />NWI Mapped SoOa Dominaiit Vegetation <br />Wat Meadow PEMA Band phaUrti anuuOtiacat <br />TIm area nadertaveatigattoa la mapped as PEMCdoa the MWl map aad borders a Urge narth. Thcadiaccnt <br />nplaiid ii MBnmuis-Poa asioclatton wttli clover and alfalfat a seeded putarc mixture. <br />Do normal envlronaieiital condidons exiit at the plant comnnaity? @ The area investigated has a history of being <br />hayed and ar mowed. <br />Has vegetadoo* soil, andfor hydr been aignilicandy distarbed? <br />VEGETATION <br />Percent of dominant spcdea that arc OBLt FACW, aad/or TAC <br />Basin Dominant Plant Species Indicator Stratum <br />Percent <br />OBL FACW FAC <br />FACW4-herb <100 <br />b the hydrophyde vegetation criterion met? (Vcj <br />Rationale: more that 50% of the composition of the domlBaat ipedes from lU strata an naked at hydrophytlc vegetatioa. & <br />shoold bo Botod that the domlaact vegetatioa. Phalaris, calits io the traniitioB zone tad la some instances ciists oa the upland as <br />It followi the southci^ fence li%e wcttorly. <br />SOILS <br />Pasta Serica/Phase Subgroup <br />Hydric <br />Sotb Lis* Hietoeol Mottled <br />Hemel TVne ARCUQUOLLS <br />Histic <br />Eoioedon Cleved <br />No Ifo <br />Other Hydric soil iadicaton: The upper 10 iacbea were dark oigank coatcat, below die 10 inch level nuall grains of <br />silica sand were present (less than 1% of the mQ) end continued witii incresKdcootcot ts a depth of Id inchei <br />Gray Jreshwater Cei^ter • Si^ite^S • 2500 Shadywooct • Excelsior.MN 55331 <br />Ton free 1-500-271 ‘2A50 • 61 2~^7U0^72