(2) China Creek is a year-round creek that flows about three miles. It joins Redwood Creek one- quarter mile south of the community of Brice land. Reference: Turner 1993: 49; United States Geological Survey 1969.
(5) China Gulch has a one and one-half mile-long stream that flows in an east-to-west direction where it joins North Russian Creek. It is just north of Little China Gulch in the Klamath National Forest. There has been considerable tunnel and shaft mining in the area. See Little China Gulch, Siskiyou County. Reference: United States Geological Survey 1977.
(2) China Creek is a perennial stream five miles long and travels in an east-to-west direction within the Trinity National Forest. It merges with New River near the community of Dailey. There has been wide spread mining activity throughout the area. Reference: United States Geological Survey 1982c.
Trinity National Forest. It joins the North Fork of the Trinity River. There is extensive evidence of mining along the creek. Reference: United States Geological Survey 1982i.
It joins Little Browns Creek four and one-half miles northeast of Weaverville. Considerable placer mining has occurred in the area. Reference: United States Geological Survey 1982d.
considered a Chinese placer mining area. This resulted from it being registered as a mining claim by the She Lim Company in 1860. It was worked primarily by the Chinese until at least 1885. The claim covered 1250 feet of river bank. Reference: Kelly and McAleer 1986: 5, 23-24.
See Weaverville Elementary School, Trinity County.
Recommendation for the Ohio Flat Mining District, Trinity County. Sacramento: