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15000 cfs. The Pee Dee River, also known as the Great Pee Dee River, is a river in the Carolinas of the United States. It originates in the Appalachian Mountains in North Carolina, where its upper course, above the mouth of the Uwharrie River, is known as the Yadkin River. The river empties into Winyah Bay, and then into the Atlantic Ocean near ...
The Mississippi River[ b ] is the primary river and second-longest river of the largest drainage basin in the United States. [ c ][ 15 ][ 16 ] From its traditional source of Lake Itasca in northern Minnesota, it flows generally south for 2,340 miles (3,766 km) [ 16 ] to the Mississippi River Delta in the Gulf of Mexico.
Lake Taneycomo originated when the White River was confined by the completion of the Powersite Dam, near Forsyth, Missouri, in 1913. [2] From 1913 until 1958 it was a warm water lake. [3] In the 1920s and 1930s, tourists began to be drawn to the lake and its nearby communities, Branson and Rockaway Beach. Water skiing, boating, fishing, sunning ...
Depth of channel: 9 ft (2.7 m) or more. Width of channel: mostly 250 ft (76 m) to 300 ft (91 m). Bridge clearance: 300 ft (91 m) horizontal; 52 ft (16 m) vertical. Although Congress originally authorized USACE to dredge the channel to a depth of 12 ft (3.7 m) in 2005, it did not provide the funds to do so.
Big Sandy Lake. 1 Shore length is not a well-defined measure. Big Sandy Lake is a lake in Aitkin County, Minnesota, approximately nine miles north of McGregor. The lake is considered fertile walleye ground with several habitat types, including the open main basin, the deep, cold eastern basin, and a shallow, more isolated south basin.
The Washington Bridge is a 2,375-foot (724 m)-long arch bridge over the Harlem River in New York City between the boroughs of Manhattan and the Bronx. The crossing, opened in 1888, connects 181st Street and Amsterdam Avenue in Washington Heights, Manhattan, with University Avenue in Morris Heights, Bronx. It carries six lanes of traffic, as ...
The water began overflowing at approximately 10 a.m. [4] As the water overtopped the isthmus, it flowed downhill to the Wisconsin River approximately 800 feet (240 m) away, quickly eroding and creating a 400-foot-wide (120 m) channel that rapidly drained the lake in an out-of-control torrent into the river, 40 feet (12 m) below the lake's level ...
The lower Wisconsin River flows through glacial drift until it enters the Driftless Area and eventually reaches the Mississippi River. [1] It extends about 116 river miles (187 river kilometers) from Portage to its confluence with the Mississippi River, falling 171 feet (52 m) from about elevation 782 feet (238 m) above sea level (msl) at Portage to 611 feet (186 m), msl at the Mississippi.