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Botany and Wetlands Study Report - McMillen, LLC

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<strong>Botany</strong> <strong>and</strong> Wetl<strong>and</strong>s <strong>Study</strong> <strong>Report</strong>Southeast Alaska Power Agency3 ENVIRONMENTAL SETTINGThe Tongass National Forest, including Revillagigedo Isl<strong>and</strong>, is dominated by temperaterainforest. The maritime climate is characterized by cool, wet summers <strong>and</strong> mild winters withsignificant precipitation as snow <strong>and</strong> rainfall. In Ketchikan, approximately 23 miles southwest ofthe study area, typical summer temperatures average 60‐65° F, while winter temperaturesaverage 39‐44°F. The year‐round average temperature is 51.6° F. Annual precipitation as rainfallaverages 117 inches, with the least precipitation (16 percent) occurring from May through July.The wettest month is October with an average of more than 22 inches accumulation. Snowfallaccumulation averages 37 inches per year, with the most snow accumulating in January (35percent) (Western Regional Climate Center 2012). The study area lies about 300 to 350 feethigher in elevation than Ketchikan.Southeast Alaska is geologically composed of linear belts of tectonic assemblages that liesub‐parallel to, <strong>and</strong> have been accreted to, the continental margin. This coastal group ofmountainous isl<strong>and</strong>s lies west of the mainl<strong>and</strong> coast range. This area has been subjected toisostatic <strong>and</strong> tectonic uplift, as well as glacial <strong>and</strong> other climatic weathering processes (ForestService 1996). Bedrock in the project area is made up of the Taku terrane <strong>and</strong> includes“metamorphosed marine shales <strong>and</strong> muddy s<strong>and</strong>stones, metamorphosed <strong>and</strong>esites, basalts, <strong>and</strong>rhyolite lavas, along with small amounts of limestone, marble, <strong>and</strong> conglomerate” (Connor <strong>and</strong>O’Haire 1988:10). Many of the lakes, valleys, <strong>and</strong> mountains in <strong>and</strong> around the project area arethe result of more recent glaciation.3.1 Vegetation ResourcesThe Swan Lake Expansion analysis area is located on the Ketchikan‐Misty Fiords Ranger Districton Revillagigedo Isl<strong>and</strong> in southeast Alaska, 22 miles northeast of Ketchikan. The TongassNational Forest, including Revillagigedo Isl<strong>and</strong>, is covered primarily by temperate rainforestconsisting of Sitka spruce (Picea sitchensis) <strong>and</strong> western hemlock (Tsuga heterophylla), withlesser amounts of mountain hemlock (Tsuga mertensiana), Alaska yellow cedar (Callitropsis[Chamaecyparis] nootkatensis), <strong>and</strong> lodgepole pine (Pinus contorta). Common understoryspecies include oval‐leaf blueberry (Vaccinium ovalifolium), Alaska blueberry, (Vacciniumalaskanse), Devil’s club (Oploplanax horridum), thimbleberry (Rubus parviflorus), salmonberry(Rubus spectabilis), twisted‐stalk (Streptopus spp.), queen’s cup (Clintonia uniflora), three‐leaffoamflower (Tiarella trifoliata), <strong>and</strong> lady fern (Athyrium filix‐femina).Red alder (Alnus rubra) <strong>and</strong> Sitka alder (Alnus viridis ssp. sinuata) occupy riparian areas <strong>and</strong>other sites, such as avalanche chutes, where bare mineral soils are exposed. On RevillagigedoIsl<strong>and</strong>, extensive forest areas have been logged. Plant communities in these areas have changedto early successional types that differ in character than old growth forests. Regeneration is rapid<strong>and</strong> most of the logged areas are covered by dense st<strong>and</strong>s of young growth.Swan Lake Hydroelectric Project January 2013FERC Project No. 2911 Page 8 Version: Agency Review

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