The Susquehanna River is a river in the northeastern United States. At approximately 410 mi (715 km) long, it is the longest river on the American East Coast. The Susquehanna forms from two main branches, with the North Branch, which rises in upstate New York often regarded as an extension of the main branch. The shorter West Branch, which rises in western Pennsylvania, is sometimes regarded as the principal tributary, joining the North Branch near Sunbury in central Pennsylvania. The river drains a large watershed within the Allegheny Plateau of the Appalachian Mountains, cutting through water gaps in the lateral mountain ridges in a broad zigzag course to flow across the rural heartland of southeastern Pennsylvania, emptying in the north end of the Chesapeake Bay.
Downstream from the confluence of its branches it flows south past Selinsgrove, where it is joined by its Penns Creek tributary, and cuts through a water gap at the western end of Mahantongo Mountain. It receives the Juniata River from the northwest at Duncannon, then passes through its last water gap, through Blue Mountain Pennsylvania, just northwest of Harrisburg. It passes downtown Harrisburg (where it is nearly a mile wide), the largest city on the lower river, and flows southeast across south-central Pennsylvania, forming the border between York and Lancaster counties, as well as receiving Swatara Creek from the northeast. It crosses into northern Maryland approximately 30 miles (50 km) northeast of Baltimore and enters the northern end of the Chesapeake Bay at Havre de Grace.
Before the end of the last ice age, the Susquehanna was a much longer river. The Chesapeake Bay constituted its lower valley before it was flooded by rising waters at the conclusion of the Pleistocene.
In the late colonial times, the river became an increasingly important transportation corridor with the discovery of anthracite coal by Necho Allen in its upper reaches in the mountains. In 1792, the Union Canal was proposed linking the Susquehanna and the Delaware along Swatara Creek and Tulpehocken Creek. In the 19th century the river became the scene of the growth of industrial centers.
Conflicting land claims by Pennsylvania and Connecticut to the Wyoming Valley along the Susquehanna led to the founding of Westmoreland County, Connecticut and the Pennamite Wars, which eventually led to the territory being ceded to Pennsylvania.
During the American Civil War's 1863 Gettysburg Campaign, the commander of the Department of the Susquehanna, Union Major General Darius N. Couch resolved that Robert E. Lee's Confederate Army of Northern Virginia would not cross the Susquehanna. He positioned militia units under Maj. Granville Haller to protect key bridges in Harrisburg and Wrightsville, as well as nearby fords. Confederate forces approached the river at several locations in Cumberland and York counties, but were recalled on June 29 when Lee chose to concentrate his army to the west.
In 1972, the remnants of Hurricane Agnes stalled over the New York-Pennsylvania border, dropping as much as 20 inches of rain on the hilly lands. Much of that precipitation was received into the Susquehanna from its western tributaries, and the valley suffered disastrous flooding. Wilkes-Barre, Pennsylvania, was among the hardest hit communities. The Chesapeake Bay received so much fresh water that it killed much of the marine life.
In 1979 the river was the scene of the most serious nuclear power accident in U.S. history at Three Mile Island southeast of Harrisburg.
Susquehanna River | American Heritage Rivers
Susquehanna River | Susquehanna (fleuve) | Susquehanna (fiume) | Rio Susquehanna | 薩斯奎哈納河
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