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\lil! thrtltcr to the south, Ihr start ot'^ slide teas <br />Il~~frll [n slOprs nl ~Q°, i(!°ir, Jf 1 Vl'nll'211 tU i.l{ <br />h~~riiontal. This area i. ahmr Mond 1'_, and terttct <br />c.:nrrials near the for and under the hacklill <br />nucht tx- contrihutors to the I~ilutro. <br />I nun ntrasurcntrnts olt u1' f{shihit b-I (mupl. the <br />«hrst ul~ natural slopes in this area appear hl hr <br />l irtiral h! ±.? horinmtul (i0°.'o nr 17"1. <br />In ,ummar<, rcrlainud slopes o(otrr 3 <br />L,n iiuntal to I trrtiral I??"~~ ur 18"1 appear to he <br />sll hl<. '. ~~ .'~ .il~_~.~ `I~~".thllltt ~,!-LUIUIi. 1lll'?l'. ,i! icrn Ilsslr slaprs nllr',hl hl iUhJCCt lU lallUR' II <br />N;1I <'i' 1~ Ilfi \i i:i \I~~I~~ ~ I111 L'lli Iii ~li.'I~i llr,l 1~ ~I<',ICnld and constructed as stnlcuuul lilts <br />Icunu•ollyd nwisnur cuntrnu ;utd compartiun, :old ^s dctemtined by suthilit~ analysesl. Rock <br />drains should hr considered lire anr' seeps ur springs Gum li,nnatiun exposures ur other uxtrccs <br />that are to he cotcrcd up. <br />