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The percentage of black-owned firms is 5.7%, and the percentage of women-owned firms is 30.2%.Ĭlick on the resources below to search Los Angeles County free public records. The total number of firms, at last estimate, was 1,046,940. The per capita income is $27,749, the median household income is $55,909, and 17.8% of the persons in Los Angeles County are considered below poverty level. The median home value is $420,200, there are 3,230,383 households, an average of 3.01 persons per household. 76.6% have a high school degree or higher, and 29.7% have a Bachelor degree or higher. The land area is 4,057.88 square miles and there are 2419.6 persons per square mile.ħ1.5% of the population is White, 9.2% is Black or African American, 48.3% is Hispanic or Latino, 14.6% is Asian, 1.5% is American Indian or Alaska Native, 0.4% is Native Hawaiian or Pacific Islander, and 2.9% is two or more races.
The County Seat is Los Angeles and the largest city is Los Angeles.
This eclogitic keel may have foundered in the Late Cenozoic, triggering uplift.Los Angeles County is located in southern California. Reduction of elevation and relief following pre‐Eocene uplift may have coincided with eclogitic recrystallization of the mafic root of Sierran batholith.
Minimal Eocene‐Miocene stream incision suggests that paleorelief and paleoelevations are relics of pre‐Eocene uplift. Elevations at ∼5 Ma (before Late Cenozoic uplift) may have been 2500 m in the southern Sierra. The elevation of pre‐Cenozoic basement rocks above the base of Tertiary paleochannels ranges from 1000 m in the south, and shows that significant relief predates Late Cenozoic incision. Tertiary stream gradients were lower than modern ones, suggesting that the bottoms of the canyons have been uplifted in the Late Cenozoic and that the mean elevation of the Sierra Nevada has increased. Low summit erosion rates suggest that the rock uplift approximates the surface uplift of crestal summits. Estimates of Late Cenozoic crestal rock uplift for different areas in the Sierra Nevada range from 1440 to 2150 m. Uplift of the Sierra Nevada, westward tilting, stream incision, and east‐down normal and dextral faulting along the present eastern escarpment of the range began at ∼5 Ma. Maximum Eocene‐Miocene incision was 150 m. Stream incision of up to 1 km has occurred since ∼5 Ma. Stream incision, faulting, thermochronologic, and geobarometric data suggest that Sierra Nevada topography is a consequence of two periods of uplift.
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