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Austin Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map , accessed March 9, 2011 southward-flowing in the mountains of western Sonoma County, California which empties into the Russian River about from the .


Course
The creek originates in an isolated area known as The Cedars, about west of Healdsburg, California. It flows south past Layton Mine into a wooded canyon, where it joins King Ridge Road just above its confluence with Bearpen Creek. It parallels King Ridge Road to the town of Cazadero and continues south through confluences with East Austin Creek and Kidd Creek. It flows under State Route 116 at milepost 4.93 and enters the Russian River about north of the town of Duncans Mills.


History
In the 1885–1886, the North Pacific Coast Railroad (NWP) extended its narrow-gauge line up Austin Creek to transport lumber from Cazadero to points south.
(1990). 9780804717311, Stanford University Press.
The railroad grade was later converted to road, becoming Cazadero Highway.


Sonoma Magnesite Company
The Cedars is a distinctive woodland of trees able to grow on a formation of intrusive .Koenig, James B. Geologic Map of California:Santa Rosa Sheet (1976) State of California Resources Agency Sonoma Magnesite Company was formed in 1912 to mine the Red Slide Deposit of in The Cedars. The mineral is important for steel-making and manufacture of bricks for high-temperature applications; but cost of transportation made mining in The Cedars infeasible until World War I interrupted availability of less expensive sources. The Sonoma Magnesite Tramway, an eleven-mile-long, narrow gauge industrial railway was built in 1914 along the bank of East Austin Creek to connect the mine with Magnesia station on the NWP railroad south of Cazadero. Thirty tons of ore were calcined daily in an oil-fired rotary kiln and packed into sacks for shipping. Production ended in 1920 when magnesite again became available from less expensive sources.


Sonoma Magnesite Tramway
The railway shipped sacks of magnesite on 4-wheel . Each of the ten flatcars was four feet wide by seven feet long and could be loaded with 5 tons of magnesite. Oil for the kiln was shipped in six 500-gallon eight feet long. Trains were pulled by an unusual variety of locomotives:
The HippoJoshua Hendy Iron Works of Sunnyvale, California purchased new; powered by an internal combustion engine
BetsyDavenport Locomotive Works purchased used from Washington
highway truck with flanged wheels on the powered rear axle and a 4-wheel supporting the front end
High water in East Austin Creek washed out significant portions of the tramway in 1921; and Betsy was washed downstream and partially buried in the gravel channel. Most of the rails had been salvaged by 1925; and the kiln was scrapped in 1937. About of track was left in place for children's amusement on the Baldwin estate near Austin Creek and the old road to Cazadero. That track was destroyed by the Christmas Week flood of 1955, and Betsy was converted to scrap metal in 1961.


Habitat and pollution
As of 2000, Austin Creek and all its major tributaries all supported . Austin Creek and East Austin Creek also harbored California freshwater shrimp.

In 2016, scientists found evidence of in water coming from underground at The Cedars, the first time that have been discovered beyond the ocean floor.


Bridges
Many bridges span Austin Creek. The longest of these is the State Route 116 bridge, which is long and was built in 1962.


See also
  • Armstrong Redwoods State Reserve
  • Austin Creek State Recreation Area
  • List of watercourses in the San Francisco Bay Area

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