Tualatin Mountains
| Tualatin Mountains | |
|---|---|
West slope of the mountains from Beaverton looking north
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| Highest point | |
| Peak | Cornell Mountain |
| Elevation | Lua error in Module:Convert at line 1851: attempt to index local 'en_value' (a nil value). |
| Coordinates | Lua error in package.lua at line 80: module 'strict' not found. |
| Geography | |
| Country | United States |
| State | Oregon |
| District | Multnomah County |
| Range coordinates | Lua error in package.lua at line 80: module 'strict' not found. |
| Topo map | USGS Linnton |
The Tualatin Mountains (also known as the West Hills or Southwest Hills of Portland) are a range of hills on the western border of Multnomah County, Oregon, United States.[1] A spur of the Northern Oregon Coast Range, they separate the Tualatin Basin of Washington County, Oregon, from the Portland Basin of western Multnomah County and Clark County, Washington.
The highest peak in the range is Cornell Mountain at 1,270 feet (390 m).[2] Other notable peaks include Council Crest at 1,073 feet (327 m), the highest point in the city of Portland, and Pittock Hill, location of the Pittock Mansion.[2][3]
The hills date from the late Cenozoic era, and range up to over 1,000 feet (300 m). Composed mainly of basalt, the mountains were formed by several flows of the Grande Ronde basalt flows that were part of the larger Columbia River basalts.[4] Human settlement goes back 10,000 years[citation needed] to the area's earliest known residents, the Chinook people.[citation needed]
Despite steep slopes, periodic landslides, and multiple earthquake faults, many residences have been built in the Tualatin Mountains, though much of the northern portion is undeveloped land within the 5,000-acre (20 km2) Forest Park. The landscape, inside and outside the park, is predominantly forested.
U.S. Route 26 (the Sunset Highway) is the principal transportation link across the hills, traveling through the Tanner Creek Canyon and over the pass at Sylvan. This route through the hills connecting the agricultural Tualatin Basin to the navigable Willamette River was developed as a plank road in the 19th century. The Great Plank Road (Canyon/Jefferson Road) was a major factor in the early growth of the city of Portland.
Since 1998, the west side MAX Light Rail has run roughly parallel to US 26 through the hills, including a section tunneled deep underground.
See also
References
- ↑ 1.0 1.1 Lua error in package.lua at line 80: module 'strict' not found.
- ↑ 2.0 2.1 Lua error in package.lua at line 80: module 'strict' not found.
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
- ↑ Bishop, Ellen Morris. In Search of Ancient Oregon: A Geological and Natural History. Timber Press, 2003.
Further reading
- Southwest Hills Resource Protection Plan (Portland Bureau of Planning, 1992)
- A gravity study through the Tualatin Mountains, Oregon: Understanding crustal structure and earthquake hazards in the Portland urban area (R. Blakely, K. Cruikshank, A. Johnson, M. Beeson, K. Walsh, & R. Wells, 2001)
- Landslides in the Portland, Oregon Metropolitan Area Resulting from the Storm of February 1996: Inventory Map, Database and Evaluation (S.F. Burns, W.J. Burns, D.H. James, & J.C. Hinkle, 1998)
