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The Dalles Lock and Dam is a concrete-gravity run-of-the-river dam spanning the Columbia River, two miles (3.2 km) east of the city of The Dalles, Oregon, United States. [2] It joins Wasco County, Oregon , with Klickitat County, Washington , 192 miles (309 km) upriver from the mouth of the Columbia near Astoria, Oregon .
The canal remained in use until it was flooded by the Dalles Dam in 1957. ... (2.1 km 2), or 10.81%, are water ... On June 28, 2021, Dallesport's high temperature of ...
Water supply South Fork Tolt River Dam: King: South Fork Tolt River: South Fork Tolt Reservoir: Earthfill 6.55: 200 61 57,900 71,400 1964 Seattle Public Utilities: Water supply Swift Dam: Skamania: Lewis River: Swift Reservoir: Earthfill 240.0: 512 156 755,600 932,000 1958 PacifiCorp: Hydroelectric The Dalles Dam† Klickitat: Columbia River ...
The Dalles Dam: 191.5 ... Columbia River Water Management Report, Water Year 2001. US Army Corps of Engineers. Archived from the original (PDF) on January 10, 2009
The nearly 8100 major dams in the United States in 2006. The National Inventory of Dams defines a major dam as being 50 feet (15 m) tall with a storage capacity of at least 5,000 acre-feet (6,200,000 m 3), or of any height with a storage capacity of 25,000 acre-feet (31,000,000 m 3).
The Dalles (/ ˈ d æ l z / ⓘ) DALZ; formally the City of The Dalles and also called Dalles City, is an inland port and the largest city in Wasco County, Oregon, United States. The population was 16,010 at the 2020 census , and it is the largest city in Oregon along the Columbia River outside the Portland Metropolitan Area .
Celilo Falls itself was the first in a series of cascades and rapids known collectively as The Narrows or The Dalles, stretching for about 12 miles (19 km) downstream. [8] Over that length, the river dropped 82 feet (25 m) at high water and 63 feet (19 m) at low water. [4] The Dalles (photo from Horner, 1919)
The weather pattern changed a few weeks later, producing significant snowfall in lowland areas. Moscow, Idaho recorded 42 inches (110 cm) of snow in ten days during the second half of January. [ 5 ] Prolonged cold settled in following the heavy snow, causing the ground to freeze throughout much of the Columbia Basin and surrounding valleys.