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Red Clover Creek

Red Clover Creek
stream
Country United States
State California
Region Plumas County
Tributaries
 - left Crocker Creek, Dixon Lane-Meadow Creek, California
 - right Dixie Creek
Source Horton Ridge, Sierra Nevada
 - elevation 6,610 ft (2,015 m)
 - coordinates 39°52′45″N 120°20′17″W / 39.87917°N 120.33806°W / 39.87917; -120.33806 
Mouth Last Chance Creek
 - elevation 3,743 ft (1,141 m)
 - coordinates 40°03′28″N 120°40′08″W / 40.05778°N 120.66889°W / 40.05778; -120.66889Coordinates: 40°03′28″N 120°40′08″W / 40.05778°N 120.66889°W / 40.05778; -120.66889 

Red Clover Creek is a northwestward-flowing stream originating on Horton Ridge east of the Sierra Nevada crest in Plumas County, California, United States. It courses 27 miles (43 km) through Dotta Canyon and the Red Clover Valley, culminating in Last Chance Creek, which flows in turn, into Indian Creek in the Genesee Valley, and from there to the East Branch North Fork Feather River. The Red Clover Valley sits at an elevation of about 5,400 feet (1,600 m) and is located on the east side of the Sierra Nevada crest, approximately 60 miles (97 km) north of Truckee and 30 miles (48 km) southeast of Quincy. This region of the northern Sierra Nevada is known as the Diamond Mountains.

Most of the Red Clover Creek Basin is uninhabited, although a few residences and vacation homes exist near the mouth in Genesee Valley. Most of the mountain and foothill lands are owned and managed by the U. S. Forest Service for timber production, wildlife management, grazing, recreation, and watershed management. There are no developed campgrounds along Red Clover Creek, however, there are several areas that offer suitable camping, and are frequented by campers, hunters, and fishermen. County Route 111, a dirt and gravel road, follows the creek from Red Clover Valley to Genesee Valley, and is referred to as the Genesee-Beckworth road.

The largest tributary watersheds are those of Crocker and Dixie Creeks. The upper and middle reaches are low gradient, alluvial valleys while the lower reach runs through a bouldered canyon.

Prior to 1880, the upper portion of Red Clover Creek, was as a low gradient, narrow channel with a well-developed riparian zone comprising hardwoods, sedges, and willows that protected the streambanks. It had a reputation as a good trout fishery. Heavy sheep and cattle grazing, eliminated riparian vegetation, leading to erosion of the creek. By 1985, the actively eroding channel was 50 to 60 feet wide and had vertical incised to a depth of ten feet. The erosion contributed large amounts of sediment to the North Fork Feather River system via Indian Creek.


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