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Smith River (California)

River in California, United States

Smith River (California)

Summary

River in California, United States

FieldValue
nameSmith River (California)
imageMouthSmithRiver.jpg
image_captionThe mouth of the Smith River as it enters the Pacific Ocean
image_size300
mapSmith_River_map.png
map_size300
map_captionMap of the Smith River watershed
subdivision_type1Country
subdivision_name1United States
subdivision_type2State
subdivision_name2California
length25.1 mi
discharge1_locationabout 7 mi east of Crescent City
discharge1_min160 cuft/s
discharge1_avg3748 cuft/s
discharge1_max228000 cuft/s
source1Confluence of North and Middle Forks
source1_locationGasquet, Klamath Mountains,
Six Rivers National Forest,
Del Norte County
source1_coordinates
source1_elevation315 ft
mouthPacific Ocean
mouth_locationnear community of Smith River, Del Norte County
mouth_coordinates
mouth_elevation0 ft
basin_size719 sqmi
tributaries_leftMiddle Fork Smith River, South Fork Smith River
tributaries_rightNorth Fork Smith River
extra{{Designation list
embedyes
designation1nwsr
designation1_typeWild 78.0 mi
Scenic 31.0 mi
Recreational 216.4 mi
designation1_dateJanuary 19, 1981

Six Rivers National Forest, Del Norte County Scenic 31.0 mi Recreational 216.4 mi

The Smith River (Tolowa: xaa-wvn’-taa-ghii~-li~’, nii~-li~’ {{Cite web

Course

The [[confluence]] of the South Fork with the main Smith River near [[Crescent City, California

The Smith River is formed by the confluence of its Middle Fork and North Fork, near the community of Gasquet. The Middle Fork, 27.8 mi long, The South Fork Smith River enters the Smith River near the community of Hiouchi. The 43.3 mi fork rises on the eastern edge of the Smith River National Recreation Area, approximately 30 mi east-northeast of Crescent City, flowing southwest and then northwest.

From the confluence with the South Fork, the Smith River flows generally northwest, entering the Pacific Ocean near the community of Smith River, approximately 10 mi north of Crescent City. Smith River estuary is recognized for protection by the California Bays and Estuaries Policy.

Watershed

The river's watershed catchment area is 719 sqmi. It drains a rugged area of the western Klamath Mountains and Northern Outer California Coast Ranges, west of the Siskiyou Mountains, barely across the Oregon border, and north of the watershed of the Klamath River.

By average discharge, the Smith is the largest river system in California that flows freely along its entire course. The highly variable annual flow is approximately 3746 cuft/s, with an average monthly high of 8432 cuft/s in January, and an average low of 336 cuft/s in September. The all-time highest flow was 228000 cuft/s on December 22, 1964, during the Christmas flood of 1964.

The river was named for the explorer Jedediah Smith.

Conservation

The free-flowing nature of the river—without a single dam along its entire length—makes it especially prized among conservationists and is considered one of the crown jewels of the National Wild and Scenic River program. It is the only major California river never to have been dammed.

Former Smith River Bridge crossing the Lower Smith River.
truss]] of Smith River Bridge.

Crossings

The 1929 Smith River Bridge, also known as the Hiouchi Bridge or Bridge Wo. 1-06, was a rare example of a cantilever highway truss bridge within California, until it was demolished in 1989. The two-lane road bridge carried U.S. Highway 199 across the Smith River. The structural steel components were fabricated by Virginia Bridge & Iron Co. in Roanoke, shipped via the Panama Canal to San Francisco, then reloaded to a smaller coastal vessel and shipped to Crescent City. The suspended center span was a Parker truss.

It was the first cantilever truss type designed by the California Division of Highways Bridge Department engineers in 1928. The bridge type was briefly popular during the late 1920s to the late 1930s in the United States, but because it was best suited to specialized applications only limited numbers were built in the state. Its design was influenced by the first Carquinez Bridge, designed by David B. Steinman and completed in 1927 (demolished 2007).

Studies for the replacement of the Smith River Bridge began in 1987. U. S. Highway 199 provides a link between Highway 101 at Crescent City on the northern California coast, and Interstate Highway 5 inland at Grants Pass, Oregon. The proposal to replace the bridge was based on its functionally obsolete structural condition. Because of the high percentage of heavy truck traffic using the route, the bridge had sustained damage from high loads over the years, causing concern that the bridge was susceptible to collapsing.

Since it had been determined eligible for inclusion on the National Register of Historic Places, it was required to be documented to Historic American Engineering Record−HAER standards prior to its removal in 1989.

References

References

  1. (1932–2013). "USGS Gage #11532500 on the Smith River near Crescent City, CA". U.S. Geological Survey.
  2. {{cite gnis
  3. "National Wild and Scenic Rivers System". National Wild and Scenic Rivers System.
  4. U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. [http://viewer.nationalmap.gov/viewer/ The National Map], accessed March 9, 2011
  5. rises in Del Norte County, approximately {{convert. 60. mi. North Fork Smith River]], {{convert. 28.1. 264212
  6. State Water Resources Control Board ''Water Quality Control Policy for the Enclosed Bays and Estuaries of California'' (1974) State of California
  7. "Smith River Scenic Byway Overview". [[National Scenic Byway.
  8. "Smith River, California". National Wild and Scenic Rivers.
  9. Johnson, Julie. (November 16, 2025). "Major state highway crumbling into ocean". The San Francisco Chronicle.
  10. (May 1989). "Smith River Bridge (Hiouchi Bridge)". Library of Congress.
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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