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| source_length_imperial = | source_lat_d = 42 | source_lat_m = 03 | source_lat_s = 06 | source_lat_NS = N | source_long_d = 122 | source_long_m = 48 | source_long_s = 15 | source_long_EW = W | source_coordinates_note = 〔 | mouth_name = Applegate River | mouth_location = about northwest of Buncom | mouth_location_note = | mouth_district = Jackson County | mouth_region = | mouth_state = Oregon | mouth_country = | mouth_note = | mouth_lat_d = 42 | mouth_lat_m = 11 | mouth_lat_s = 55 | mouth_lat_NS = N | mouth_long_d = 123 | mouth_long_m = 02 | mouth_long_s = 43 | mouth_long_EW = W | mouth_coordinates_note = 〔 | mouth_elevation_imperial = 1440 | mouth_elevation_round = 1 | mouth_elevation_note = 〔 | length_imperial = 21 | length_round = 0 | length_note = | watershed_imperial = 113 | watershed_round = 0 | watershed_note = | discharge_location = Mouth | discharge_imperial = 226 | discharge_round = 2 | discharge_note = 〔 | discharge_max_imperial = | discharge_min_imperial = | discharge1_location = | discharge1_note = | map = Oregon Locator Map.PNG | map_size = 300 | map_caption = Location of the mouth of the Little Applegate River in Oregon | map_locator = Oregon | map_alt = A map of Oregon with a red dot in the southwest | map1 = Little Applegate River Watershed.png | map1_size = 300 | map1_caption = The Little Applegate River watershed | map1_alt = | commons = }} The Little Applegate River is a tributary of the Applegate River located in the U.S. state of Oregon. It is part of the Rogue River watershed, draining approximately of Jackson County. Rising in the Siskiyou Mountains, the river flows generally northwest to meet the Applegate about northwest of Buncom and south of Ruch. The Little Applegate River's watershed was originally settled about 11,000 years ago by the Latgawa, Shasta, and Dakubetede Native American tribes. The first non-indigenous settlers arrived in the early 19th century. Two boomtowns—Sterlingville and Buncom—were founded in the 1850s and grew rapidly as gold and other precious metals were discovered. They slowly declined in population as the supply of gold was exhausted; only three buildings remain in Buncom, while Sterlingville was abandoned and later destroyed. Despite low water quality, the Little Applegate watershed supports populations of coho and Chinook salmon, along with 138 known and 134 suspected species of other vertebrates. Sixty-four percent of the watershed is forested, although its health is slowly declining due to fire suppression. ==Course== The Little Applegate River arises at several springs near Siskiyou Peak, in the Siskiyou Mountains.〔 It flows north, receiving McDonald Creek on the right, and Glade Creek on the left.〔 Water is diverted into Sterling Ditch near the Little Applegate's confluence with Glade Creek. Sterling Ditch is an approximately aqueduct, built in 1877 to provide water for hydraulic mining in the now destroyed town of Sterlingville. About one mile past Sterling Ditch, the river turns west. It receives another major tributary, Yale Creek, on the left.〔 Yale Creek drains nearly , making it the largest of the Little Applegate's tributaries by watershed area.〔 From Yale Creek, the Little Applegate flows northwest, receiving water from Sterling Creek on the right.〔〔 The town of Buncom is located at the mouth of Sterling Creek.〔 The stream empties into the Applegate River about northwest of Buncom and south of Ruch, above the Applegate's confluence with the Rogue River.〔 For fish swimming upstream, the Little Applegate is the last major tributary of the Applegate before the unpassable Applegate Dam.〔 The Little Applegate River's average discharge is , but can range anywhere from depending on the season and the amount of precipitation.〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Little Applegate River」の詳細全文を読む スポンサード リンク
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