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The California Department of Water Resources regularly posts the Oroville Dam's current water level on the California Data Exchange Center website. The dam's water level fluctuates throughout the year and is dependent on precipitation and melting snowpack.


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Satellite images show the increase of water levels at California's Oroville Dam in June 2016, left and February 2017, right, where the threat of overflowing has prompted a state of emergency.


Oroville Dam is an earthfill embankment dam on the Feather River east of the city of Oroville, California, in the Sierra Nevada foothills east of the Sacramento Valley. At 770 feet (235 m) high, it is the tallest dam in the U.S. [8] and serves mainly for water supply, hydroelectricity generation and flood control.


California's water agency says the Oroville Dam's water level continues to decrease. The reservoir's level had dropped 15 feet by Tuesday afternoon. Officials say it needs to drop another 37 feet ...


north america; Oroville Dam: Frantic fight to lower water levels ahead of new storms. CREWS are racing to repair America’s tallest dam ahead of new thunderstorms, as the governor came under fire ...


By Robert Mullin. Water levels behind the FERC-regulated Oroville Dam have continued to decline in recent days, falling to nearly 50 feet below the height of a severely damaged emergency spillway ...


Oroville Dam: Oroville Dam is the tallest dam in the United States, measuring 770 feet high and 6,920 feet across. Construction is occurring on the main and emergency spillways, not on Oroville Dam itself. Oroville Wildlife Area: The primarily riparian woodland habitat along the Feather River and grasslands around the Thermalito Afterbay. P


Lake Oroville is a reservoir in the U.S. state of California, formed by the Oroville Dam across the Feather River. The lake is situated in the foothills of the Sierra Nevada about 5 miles (8.0 km) northeast of Oroville. At over 3,500,000 acre feet (4.3 km3), it is one of the largest reservoirs in California, after Shasta Lake.


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