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Lake Oswego Odd Fellows Hall

1890 establishments in OregonBuildings and structures in Clackamas County, OregonBuildings and structures in Lake Oswego, OregonNational Register of Historic Places in Clackamas County, OregonOdd Fellows buildings in Oregon
Oregon Registered Historic Place stubs
Lake Oswego Odd Fellows Hall
Lake Oswego Odd Fellows Hall

The Lake Oswego Odd Fellows Hall, in Lake Oswego, Oregon, was built in 1890. It was listed on the National Register of Historic Places in 1979. It served historically as a meeting hall of the local Independent Order of Odd Fellows chapter, which formed in 1888. It also has served as a specialty store and in other uses.The 31 feet (9.4 m) by 60 feet (18 m) building is one of the oldest in Lake Oswego.

Excerpt from the Wikipedia article Lake Oswego Odd Fellows Hall (License: CC BY-SA 3.0, Authors, Images).

Lake Oswego Odd Fellows Hall
Furnace Street,

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Geographical coordinates (GPS)

Latitude Longitude
N 45.413888888889 ° E -122.66083333333 °
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Address

Furnace Street

Furnace Street
97036
Oregon, United States
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Lake Oswego Odd Fellows Hall
Lake Oswego Odd Fellows Hall
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Nearby Places

Tryon Creek
Tryon Creek

Tryon Creek is a 4.85-mile (7.81 km) tributary of the Willamette River in the U.S. state of Oregon. Part of the drainage basin of the Columbia River, its watershed covers about 6.5 square miles (16.8 km2) in Multnomah and Clackamas counties. The stream flows southeast from the Tualatin Mountains (West Hills) through the Multnomah Village neighborhood of Portland and the Tryon Creek State Natural Area to the Willamette in the city of Lake Oswego. Parks and open spaces cover about 21 percent of the watershed, while single-family homes dominate most of the remainder. The largest of the parks is the state natural area, which straddles the border between the two cities and counties. The bedrock under the watershed includes part of the last exotic terrane, a chain of seamounts, acquired by the North American Plate as it moved west during the Eocene. Known as the Waverly Hills Formation, it lies buried under ash and lava from later volcanic eruptions, sediments from flooding and erosion, and layers of wind-blown silt. Two dormant volcanoes from the Boring Lava Field are in the Tryon Creek watershed. Named for mid-19th century settler, Socrates Hotchkiss Tryon, Sr., the creek ran through forests of cedar and fir that were later logged by the Oregon Iron Company and others through the mid-20th century. Efforts to establish a large park in the watershed began in the 1950s and succeeded in 1975 when the state park was formally established. As of 2005, about 37 percent of the watershed was wooded and supported more than 60 species of birds as well as small mammals, amphibians, and fish. At the same time, the human population was about 18,000.