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Glaciers remain year-round on some Cascade peaks higher than 7,000 feet (2,100 m) above sea level. [3] Annual snowfall along the coastal plain averages 1 to 3 inches (2.5 to 7.6 cm) a year, including years with none. Further inland, between the Coast Range and the Cascades, snowfall generally averages from 5 to 10 inches (13 to 25 cm) a year.
Climate data for Eugene Airport, Oregon (1991–2020 normals, [a] snow & sun 1981–2010, ... just north of Eugene. The event has been played every year since 1998, ...
Precipitation varies considerably across the valley and is closely correlated with elevation. Annual totals range from 36 inches (910 mm) at the lowest elevations to more than 80 inches (2,000 mm) in the foothills. Eugene, at the southern end of the valley, is 425 feet (130 m) above sea level and receives 46 inches (1,200 mm) per year.
The Willamette National Forest is a National Forest located in the central portion of the Cascade Range of the U.S. state of Oregon. [4] It comprises 1,678,031 acres (6,790.75 km 2). Over 380,000 acres (694 mi 2, 1,540 km 2) are designated wilderness which include seven major mountain peaks.
The Oregon High Desert is a region of the U.S. state of Oregon located east of the Cascade Range and south of the Blue Mountains, in the central and eastern parts of the state. Divided into a southern region and a northern region, the desert covers most of five Oregon counties and averages 4,000 feet (1,200 m) above sea level.
The McKenzie River is a 90-mile (145 km) tributary of the Willamette River in western Oregon in the United States. It drains part of the Cascade Range east of Eugene and flows westward into the southernmost end of the Willamette Valley. It is named for Donald McKenzie, a Scottish Canadian fur trader who explored parts of the Pacific Northwest ...
The Willamette Valley ecoregion is a Level III ecoregion designated by the United States Environmental Protection Agency in the U.S. states of Oregon and Washington.Slightly larger than the Willamette Valley for which it is named, the ecoregion contains fluvial terraces and floodplains of the Willamette River system, scattered hills, buttes, and adjacent foothills.
The climate in the Calapooya Mountains follows a pattern of wet winters and dry summers. Precipitation generally increases with elevation, ranging from an average of 40 to 50 inches (1,000 to 1,300 mm) per year in the valleys to 70 to 80 inches (1,800 to 2,000 mm) on the mountain peaks.
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