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american samoa - University of Hawaii at Manoa Botany Department

american samoa - University of Hawaii at Manoa Botany Department

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LOCATIONChapter NineLEAFU STREAMLeafu Stream is generally situ<strong>at</strong>ed in Leone Village along the southwest coast <strong>of</strong> the Island <strong>of</strong>Tutuila (Figure 9-1). The stream is accessible via Route 1, which is situ<strong>at</strong>ed immedi<strong>at</strong>elysouthwest <strong>of</strong> Leone Pala (Figure 9-2).The study area included the downstream segment <strong>of</strong> Leafu Stream th<strong>at</strong> flows through theinhabited village area. In 1998, Pedersen Planning Consultants investig<strong>at</strong>ed this streamsegment in the context <strong>of</strong> potential stormw<strong>at</strong>er management opportunities. In November 1999,PPC focused its field investig<strong>at</strong>ions more upon the lower 300 feet <strong>of</strong> Leafu Stream, as well asunnamed stream parallel and immedi<strong>at</strong>ely west <strong>of</strong> Leafu Stream. ASG Land Grant Programand ASEPA represent<strong>at</strong>ives believed th<strong>at</strong> some wetland and stream enhancement opportunitieswere more feasible in this area.STREAM HYDROLOGYSources <strong>of</strong> Surface Run<strong>of</strong>fLeafu Stream and its four branches drain approxim<strong>at</strong>ely 875 acres <strong>of</strong> land area upslope <strong>of</strong>Leone Village. The main stem <strong>of</strong> Leafu Stream, which extends up to the southwest side <strong>of</strong>Aoloaufou Village, origin<strong>at</strong>es near the 1,135-foot elev<strong>at</strong>ion.General Stream CharacteristicsImmedi<strong>at</strong>ely upstream <strong>of</strong> Leone Pala, the Leafu Stream drainage becomes very different. Inthis area, Leafu Stream and an adjoining unnamed stream actually represent three to foursepar<strong>at</strong>e stream channels th<strong>at</strong> are interspersed with small transitory islands <strong>of</strong> land area. InNovember 1999, the vari<strong>at</strong>ions in the topography and stream hydrology <strong>of</strong> this area wereextremely difficult to identify in light <strong>of</strong> dense herbaceous veget<strong>at</strong>ion and standing w<strong>at</strong>er.Further upstream within the inhabited village area <strong>of</strong> Leone, the Leafu Stream channel isconsiderably more narrow. The stream represents a combin<strong>at</strong>ion <strong>of</strong> basaltic rock and earthlined channel. Smaller rock, cobble, sand, grass, muck, and decomposed organic m<strong>at</strong>erialcomprise the bottom <strong>of</strong> the stream channel.Cross-sections were documented by PPC in May 1998 <strong>at</strong> three stream loc<strong>at</strong>ions. Channeldepths ranged between two and nine feet below the top <strong>of</strong> the stream bank (Table 9-1). Thewidth <strong>of</strong> the stream segment (between east and west stream banks) ranges between 15 and 150feet. The gre<strong>at</strong>est stream width was recorded <strong>at</strong> cross section L6 just upstream from LeonePala.Onsite surveys along Leafu Stream in May 1998 and November 1999 discovered limited tomoder<strong>at</strong>e amounts <strong>of</strong> solid waste m<strong>at</strong>erial within the stream bed. In some cases, the type and/orvolume <strong>of</strong> wastes appeared to impede stream flow.American Samoa Wetlands/Streams Restor<strong>at</strong>ion and Enhancement PlanFebruary 2001, Leafu Stream, Page 9-1

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