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i <br /> IIndkect indkk�ton d hydrolopy k�dude weter Ikbs on tree tnmke end metted leaves. Prkn�ry water <br /> eouroes k�dude proclpketlon erd runoff. A smeN cMnrbl lesde towarda Wetlend V to ths wuM bul b <br /> ( docked an ths wrlace by e mound d eerth. tt le undesr whether a rat the lwo wstlends �ro <br /> hydroloplally cor�nected. <br /> I Wetlend hx�ctiond valuea are slmAer to thoee deecribed above fa Wetlerd T. A mkar emamt <br /> d watx�tonps capecNy Is p►ovlded and wNdlMe berbHts aewcleted wlth etendlnp weter prob�dy occur <br /> for sort�e poRion d the q►owirp aeaeo�. <br /> IWedand V ie In an Isdated depreseion. The vepetatlon cortxMmlty le eNnler to Wetlend T bekp <br /> dominated by red elder,Paclf�wNlow,and Skke wAlc�w. Few herbs ware obaerved In tMe wetland. The <br /> I eoNa heve a low cMort�e,end ere qleyed and motded. Evlder�ce d hydrdopy k�duded water�epoeked <br /> aedlmerMe,water IM�ee on trees,e�d metted leaves. Ae with the dher wetlende,ths prknery sou►Cee d <br /> I weter ere preclpksllon and rumH hom the eurroundkq foreat. In eddNbn.weter hom Wedand U mey <br /> drain Nito Wedend V. <br /> ' Wetlard hxidlond valuea ere eseemislly the eeme se deecrlbed ebove fa Wetlend T and k�dude <br /> water etoreqe end wkNlfe benellta aseocieted wlth standkq water durinp the eerly portlon d the p►awirp <br /> eeaeon. Addklond wAdlNs hebkat velues are eMder to thae evaAede In the ed�K uplend taert, <br /> IIndudM►p cover, neetin0, end a mkior emaxrt d foregs vMues. <br /> WeGe�d X le domN�eted by red alder uP to eipht kal�ee dbh� eelmon berty. wlvet pnu� end <br /> I Art�e�lcen epeedweN. The ert�erqent area had recentlY been deered d ehn�bt erd troea: herbaceoue <br /> epeciee are bepk�nkq to revepetate the eree. Sdmon berty a�d red dder wMl INcNy revepMete the <br /> deered eree over tkne.recreetinp ecnib ehrub wetlend hebkat which mey succesd lo faeeted wetland <br /> � M nd disturbed. <br /> SoNs ere orpeMc M eome ereas, with low chrome end mottlee at sipht N�chsa. SoNa were <br /> I mturoted to the w�face end elendinp weter occurred in the eol pRs wkMn Mrs k�cfbs d the wrfece In <br /> Noverriber 1990. Olher kdk;atbne of hydrolopy Indude e�Mace weter obeervsd In draNieye cMnnels, <br /> water�epoaNed eNt. and bere eoNe below the ehnba. WMx sourcee k�duds predpltalbn end runoM <br /> ( es well ae d�alnepe aseocieted with the smetl krtermNtent etreem observed In Novernber t980. <br /> Wedend fundlo�d veluea ere IlmRed by the ertbll elze o'the wetlend and ke eimAerMy in vepetatlon <br /> I structure to the aunounding upland foreat end shrub communNles, whba deo caNaM red alder and <br /> ealmon beny. The surface weter obaerved in November 1990 appeero to be eeesonel and b rat <br /> expected to provide waterfa wNdlHe use lorthe erHire growirp eeason. <br /> I4.2 MITIGATION AREA <br /> I The mltipetlon sMe M Powder MNI Gulch weat d the creelc hee been the eke d verloue dbturbunce <br /> activltles over the yeere. Sand has been eMreaed M leset two dMlererR tNnee, once before Boekp <br /> purchased k,and or�ce eRer. The north edpe was dlaturbed by the conetn�ctlon d Se�wsy Boulevard, <br /> � and the south edpe wee dlaturbed by the constructlon d the a1pMd detention beein md the ax►erM <br /> Ir.rrwi��r.�.w� �0 <br /> ( DAME9 4 MOORB <br />