Homes, condos and land for sale and rent in Oroville, CA
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Brief information about Oroville
The town was originally called Ophir City, but the name was changed to Oroville when the first post office opened in 1854 (“oro” is “gold” in Spanish). The City Of Oroville was incorporated on January 3, 1906.
Gold was found at Bidwell Bar, one of the first gold mining sites in California, bringing thousands of prospectors to the Oroville area seeking riches. Now inundated by the waters of enormous Lake Oroville, which was filled in 1968, Bidwell Bar is memorialized by the Bidwell Bar Bridge, an original remnant from the area and the first suspension bridge in California (California Historical Landmark #314). In the early 20th century the Western Pacific Railroad completed construction of the all-weather Feather River Canyon route through the Sierra Nevadas giving it the nickname of “The Feather River Route”. Oroville would serve as an important stop for the famous California Zephyr during its 20-year run. In 1983, this became a part of the Union Pacific Railroad as their Feather River Canyon Subdivision. A major highway, State Route 70, roughly parallels the railroad line winding through the canyon.
Oroville sits on the eastern rim of the Great Valley, defined today by the floodplains of the Sacramento River and its tributaries. Around Oroville these sediments are dominated by thick fans of Feather River sediments, but just east of this there is a thin, N-S band of late Cretaceous sediments. These sit on top of the Sierran basement, which beneath eastern Oroville comprise greenschist-facies metavolcanic rocks of Jurassic age, giving way to granites of the Sierra batholith to the east. These are manifestations of a vigorous island arc sequence, built out over an east-dipping subduction zone of mid-to-late Mesozoic age. The gold veins lace this ancient arc, remobilized by Mesozoic shearing and intrusions of igneous rock. The crystalline foothills are locally overlain by a Cenozoic sequence of Eocene clean beach sands overlain by Neogene volcanics, including the Diamond Head-like profile of Table Mountain.
The Census reported that 14,662 people (94.3% of the population) lived in households, 72 (0.5%) lived in non-institutionalized group quarters, and 812 (5.2%) were institutionalized.
There were 5,646 households, out of which 2,126 (37.7%) had children under the age of 18 living in them, 1,893 (33.5%) were opposite-sex married couples living together, 1,174 (20.8%) had a female householder with no husband present, 430 (7.6%) had a male householder with no wife present. There were 615 (10.9%) unmarried opposite-sex partnerships, and 33 (0.6%) same-sex married couples or partnerships. 1,699 households (30.1%) were made up of individuals and 718 (12.7%) had someone living alone who was 65 years of age or older. The average household size was 2.60. There were 3,497 families (61.9% of all households); the average family size was 3.22.
The population was spread out with 4,267 people (27.4%) under the age of 18, 1,969 people (12.7%) aged 18 to 24, 3,940 people (25.3%) aged 25 to 44, 3,417 people (22.0%) aged 45 to 64, and 1,953 people (12.6%) who were 65 years of age or older. The median age was 31.5 years. For every 100 females there were 93.7 males. For every 100 females age 18 and over, there were 91.8 males.
There were 6,194 housing units at an average density of 476.0 per square mile (183.8/km²), of which 2,423 (42.9%) were owner-occupied, and 3,223 (57.1%) were occupied by renters. The homeowner vacancy rate was 3.6%; the rental vacancy rate was 8.4%. 6,293 people (40.5% of the population) lived in owner-occupied housing units and 8,369 people (53.8%) lived in rental housing units.