Misplaced Pages

#914085

27-589: The McKenzie River originates as the outflow of Clear Lake in the high Cascades of eastern Linn County in the Willamette National Forest . (Clear Lake is fed by Ikenick Creek and Fish Lake Creek, the latter of which flows from Fish Lake . Fish Lake's main tributary is Hackleman Creek, which drains the north side of Browder Ridge east of Tombstone Pass. U.S. Route 20 crosses the pass and follows Hackleman Creek.) The McKenzie River flows south from Clear Lake, paralleled by Oregon Route 126 , and goes over

54-571: A bottleneck. The lake is primarily fed by snow runoff from nearby Mount Washington and the surrounding areas. The runoff filters through caverns for more than 20 years before emptying into Clear Lake. The lake is also fed by two small creeks, which may dry up seasonally, along with Great Spring, the source of the McKenzie River. Clear Lake is the headwaters of the McKenzie River , which is the sole source of drinking water for Eugene. Clear Lake

81-448: A hike loop made up of Clear Lake Trail and McKenzie River Trail that is 5 miles (8.0 km) long. An accompanying trail guide prepared by Willamette National Forest tells visitors about Clear Lake and the neighboring lava field and forest. This Linn County , Oregon state location article is a stub . You can help Misplaced Pages by expanding it . Eugene Water %26 Electric Board The Eugene Water & Electric Board (EWEB)

108-617: A post in 1811 at Fort Astoria at the mouth of the Columbia River for the Astor Expedition . McKenzie, the following spring, formed a party to explore the Willamette River. The party found a large tributary of the Willamette River and named it after McKenzie. However, much of the McKenzie River remained largely unvisited by white settlers and explorers until October 1853, when a group of Oregon Trail settlers became lost trying to cross

135-651: A temperate climate with wet winters and dry summers. About 90 percent of precipitation in the watershed comes between October and May. Precipitation in the basin varies greatly with elevation; about 40 inches (1,000 mm) fall annually in the Willamette Valley, while the Three Sisters in the high Cascades can receive 125 inches (3,200 mm) in a year. Above 4,000 feet (1,200 m), about 35 percent of precipitation falls as snow, and at 7,000 feet (2,100 m) and higher, over 75 percent of precipitation

162-542: Is Oregon's largest customer-owned utility. Founded in 1911, it provides electricity and water to more than 86,000 customers in or around Eugene, Oregon . Chartered by the City of Eugene , a five-member Board of Commissioners is elected by the citizens of Eugene and governs the utility. Four commissioners are elected by their respective geographic wards; a fifth commissioner is at-large and elected by all of Eugene's voters. This board retains full control and sets policies for

189-466: Is reported to be one of the most exceptional freshwater dive spots in Oregon. Submerged 100 feet (30 m) deep in the lake is a stand of upright trees that were killed approximately 3,000 years ago when volcanic activity created the lake. The trees are remarkably preserved due to the cold year-round water temperatures of between 35–43 °F (1.6–6 °C). Clear Lake is circled by Clear Lake Loop Trail,

216-452: Is snowfall. At these elevations, melting snow beginning in the spring season brings more cold water out of springs under the permeable rock, increasing the McKenzie's flow and maintaining cold water temperatures in the river and its tributaries. Along the lower McKenzie, however, winter rain slides easily off the less permeable rock and erodes sediment into the river. There are six major dams in

243-589: Is the uppermost dam on the McKenzie, located less than 2 miles (3.2 km) south of Clear Lake, the McKenzie River's source. Water from Carmen Reservoir is diverted southwest through a tunnel to Smith Reservoir on the Smith River. Through both the Smith River and another tunnel, water in Smith Reservoir moves south to the Carmen Power Plant, then into Trail Bridge Reservoir—which the McKenzie joins—and through

270-705: The Pacific Crest Trail in the Three Sisters Wilderness and flows north-northwest for about 30 miles (48 km) through Cougar Reservoir and Cougar Dam .) After the South Fork confluence, the main stem of the McKenzie River continues west through a narrow valley in the mountains, receiving the Blue River from the north at the community of Blue River. The McKenzie then passes Vida and continues to Leaburg and Walterville . The McKenzie valley widens as

297-491: The Sahalie and Koosah waterfalls to Carmen Reservoir, a man-made lake from which the river is then diverted into a 2-mile (3.2 km) tunnel to Smith Reservoir. Between Carmen Reservoir and Tamolitch Falls , the riverbed is dry for 3 miles (4.8 km) because lava from Belknap Crater buried that stretch of the river about 1,600 years ago. The river flows under the lava for those three miles and re-surfaces at Tamolitch Pool at

SECTION 10

#1733093783915

324-552: The power-producing Trail Bridge Dam. The engineered system is called the Carmen–;Smith Hydroelectric Project, and it has been used by the Eugene Water & Electric Board since 1963 to generate electricity for EWEB customers. The system's generating capacity is 114 megawatts (MW). EWEB also owns and manages two power-producing canals farther downstream along the McKenzie River. The Walterville Canal, completed in 1910, and

351-686: The Cascades into the Willamette Valley via the Elliott Cutoff . In 1910, travelers completed the first automobile crossing over McKenzie Pass . However, crossing along the river was limited to summer because winter conditions closed the pass. Year-round travel was not possible until 1960, with the completion of a road over Santiam Pass. Fish in the McKenzie River and some of its tributaries include spring Chinook salmon , mountain whitefish , and bull , cutthroat and rainbow trout . Dippers , mergansers , bald eagles , ospreys , and various ducks feed on

378-468: The Cascades is known as the McKenzie Valley. The following communities, listed west to east, are in the valley: Cedar Flat , Walterville, Deerhorn , Leaburg, Vida, Nimrod , Finn Rock , Blue River, Rainbow , McKenzie Bridge, and Belknap Springs. For about 8,000 years, the McKenzie River has been home to Native Americans. In more recent history, Kalapuya and Molala tribes lived nomadically in

405-528: The Leaburg Canal, completed in 1930, each contain water diverted from the McKenzie to produce electricity. Most of the water is returned to the river after power production. The eastern portion of Oregon Route 126 passes through the valley of the McKenzie River, closely following the river for much of its route. The 60-mile (97 km) stretch of the river from the edge of the Springfield metro area eastward to

432-557: The McKenzie River watershed—three on the river and three each on a different tributary of the McKenzie. The three dams on the McKenzie's main stem form Carmen Reservoir, Trail Bridge Reservoir, and Leaburg Reservoir, respectively. The other dams in the watershed are the Smith River dam on the Smith River in the upper basin, Cougar Dam on the South Fork McKenzie River, and Blue River Dam on the Blue River. The Carmen Diversion Dam

459-697: The McKenzie basin include the Calapooia ; the South , Middle and North Santiam rivers to the north; the Middle Fork Willamette River to the south; and the Deschutes River to the east. Most of the watershed is lightly populated; about 70 percent of it is public land managed by the U.S. Government , of which about 39 percent is the Three Sisters Wilderness. Over 96 percent of

486-551: The base of Tamolitch Falls. It then flows south into Trail Bridge Reservoir, where the Smith River enters from the right . After passing through Trail Bridge Dam, the river enters Lane County . The McKenzie continues south to Belknap Springs , where it turns west and flows past the community of McKenzie Bridge . It receives the South Fork McKenzie River about three miles east of Blue River . (The South Fork rises near

513-568: The basin is forested, just under 4 percent is devoted to agricultural use—mainly farms and orchards on the lower floodplain—and the remainder is residential or industrial. Most of the public land is part of the Willamette National Forest and is important for logging and recreation. The river is the sole tap water source for the cities of Eugene and Springfield, fulfilling the water needs of about 200,000 people. The Eugene Water & Electric Board (EWEB) utility draws

540-483: The fish. The threatened northern spotted owl inhabits dense forest on the west side of the upper McKenzie basin in Linn County. Forests of Douglas fir , western hemlock , and western red cedar cover the vast majority of the watershed. The McKenzie River is popular for boating—especially fishing, kayaking, and whitewater rafting. The McKenzie River dory (or drift boat), specifically designed for use in whitewater,

567-524: The river continues west, receiving the Mohawk River from the northeast just north of Springfield . Emerging from the Cascade foothills, the McKenzie enters a broad floodplain. It joins the Willamette River from the east 5 miles (8 km) north of Eugene . The McKenzie River drains a region of about 1,300 square miles (3,400 km) and is one of the primary tributaries of the Willamette River. Elevations in

SECTION 20

#1733093783915

594-481: The summer and spent winters in the lower valley. This way of life continued until the mid-19th century, when many natives died of disease or were relocated to reservations. The first recorded exploration of the river occurred in the spring of 1812, when the Pacific Fur Company reached the McKenzie via the Willamette River, as part of a larger exploration led by Donald McKenzie . The company had established

621-570: The upper McKenzie. Most whitewater rafting takes place between Quartz Creek and Helfrich Boat launch. This segment is roughly nine miles long and has three rapids, Browns Hole, Mamma's Pies, and Marten's Rapid (Class III). There are also a couple of smaller surfer rapids that kayakers typically stop at. Clear Lake (Linn County, Oregon) Clear Lake is a mountain lake 86 mi (138 km) northeast of Eugene, Oregon , United States in Linn County . It has two main bodies connected by

648-412: The water and electric utilities. More than 95 percent of the electricity EWEB serves its customers comes from hydropower , wind and other sources that do not generate carbon-based emissions that are linked to global warming. Most of this electricity comes from the federal Bonneville Power Administration and from EWEB's own hydroelectric projects. EWEB was the first public utility in Oregon to own

675-455: The water at river mile (RM) 11 or river kilometer (RK) 18 in Springfield. Water quality in the river is rated good to excellent, with better quality upstream than downstream. Principal sources of contaminants in the McKenzie are agriculture and residential development, including septic systems. Small amounts of herbicides detected in the river and some of its tributaries may be from aerial spraying by timber companies for forestry. The region has

702-578: The watershed range from 10,358 feet (3,157 m) at the summit of the South Sister to 375 feet (114 m) at the McKenzie's mouth on the Willamette River north of Eugene. The upper basin, in the high Cascades, consists of granular , permeable igneous rocks that are geologically young, while most of the middle and lower McKenzie valley in the Western Cascades is made of the remnants of older, more weathered volcanic rocks. Major watersheds bordering

729-579: Was first developed on the Mckenzie in the 1940s; adaptations of this design quickly grew in popularity on other Western rivers such as the Rogue and the Colorado . Boating is also common on Blue River Reservoir and Cougar Reservoir. Hiking and mountain biking are popular activities on trails in the McKenzie watershed. Trails include the 26.5-mile (42.6 km) McKenzie River National Recreation Trail, which follows much of

#914085