Everything about The Sprague River totally explained
The
Sprague River is a tributary of the
Williamson River, approximately 75 mi (121 km) long, in southwestern
Oregon in the
United States. It drains an arid
volcanic plateau region east of the
Cascade Range in the watershed of the
Klamath River.
It is formed by the confluence of its North and South forks in eastern
Klamath County, approximately 35 mi (56 km) ENE of
Klamath Falls. The North Fork (30 mi/48 km) rises in southwestern
Lake County in the
Fremont National Forest near
Gearhart Mountain and flows southwest. The South Fork (30 mi/48 km) rises northeast of
Quartz Mountain Pass and flows WNW. The combined stream flows west through the broad Sprague Valley, past the small communities of
Bly,
Beatty and
Sprague River. It joins the Williamson from the east at
Chiloquin, approximately 10 mi north of the mouth of the Williamson on
Upper Klamath Lake.
It receives the
Sycan River from the north at Beatty. Superb trout fishing exists in the Sprague and its tributaries.
Further Information
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