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The Delaware River is a major river in the Mid-Atlantic region of the United States and is the longest free-flowing (undammed) river in the Eastern United States. From the meeting of its branches in Hancock, New York, the river flows for 282 miles (454 km) [1] along the borders of New York, Pennsylvania, New Jersey, and Delaware, before ...
Following is a list of dams and reservoirs in West Virginia.. All major dams are linked below. The National Inventory of Dams defines any "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 river forms part of the borders between Maryland and Washington, D.C., on the left descending bank, and West Virginia and Virginia on the right descending bank. Except for a small portion of its headwaters in West Virginia, the North Branch Potomac River is considered part of Maryland to the low-water mark on the opposite bank.
This is a list of locks and dams of the Ohio River, which begins at the confluence of the Allegheny and Monongahela rivers at The Point in Pittsburgh, Pennsylvania and ends at the confluence of the Ohio River and the Mississippi River, in Cairo, Illinois . A map and diagram of U.S. Army Corps of Engineers operated locks and dams on the Ohio River.
Clip from John Senex map c. 1710 showing the people Captain Vielle passed by to arrive in Chaouenon's country as the French Jesuit called the Shawnee.. For nearly 15 years, missionaries and "coureurs de bois" confused ideas of a "beautiful River, large, wide, deep, and worthy of comparison . . . with our great river St. Lawrence" that in 1660 and 1662 they were able to describe a river below ...
Elkhead Reservoir. Englewood Dam. Green Mountain Reservoir. Gross Dam – Gross Reservoir. Horsetooth Dam – Horsetooth Reservoir, built as part of the Colorado-Big Thompson project. John Martin Reservoir. McNulty Reservoir Dam. McPhee Dam – McPhee Reservoir. Morrow Point Dam – Morrow Point Reservoir.
The Delaware Water Gap with the Pennsylvania town of the same name visible in the lower left next to the I-80 crossing. A water gap is a geological feature where a river cuts through a mountain ridge. The Delaware Water Gap formed 500 million years ago [4] when quartz pebbles from mountains in the area were deposited in a shallow sea.
The river, the longest free-flowing river east of the Mississippi, is 113 feet deep at River Mile 290, counting from Delaware Bay, and visible from the bridge connecting Pennsylvania and New York.