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Roebling's Delaware Aqueduct, also known as the Roebling Bridge, is the oldest existing wire suspension bridge in the United States. [1] It runs 535 feet (163 meters) over the Delaware River , from Minisink Ford, New York , to Lackawaxen, Pennsylvania .
Compared to the flood of 16–17 July 1865, the 1833 flood was exceeded by 6 feet (1.8 m), rupturing the Turk Dam and destroying almost all of the bridges downstream. As the waters reached the Delaware River, the flow was so great as to reach the New Jersey shoreline leaving a large pile of debris and preventing shipping from traversing the ...
The Delaware–New Jersey border is actually at the easternmost river shoreline within the Twelve-Mile Circle of New Castle, rather than at mid-river, mid-channel or thalweg, so small portions of land lying west of the shoreline, but on the New Jersey side of the river, are pene-exclaves under the jurisdiction of Delaware. The rest of the ...
As of Wednesday morning, the water level of the Delaware River at Trenton stood at 12.49 feet, and is expected to reach 16.85 feet early Friday before receding. The flood stage is 20 feet.
The Delaware River looking north above Walpack Bend near Walpack, New Jersey, where the river leaves the historic Minisink region, a buried valley eroded from the Marcellus Formation The watershed of the Delaware River drains an area of 14,119 square miles (36,570 km 2 ) and encompasses 42 counties and 838 municipalities in five U.S. states ...
The United States Geological Survey (USGS) maintains many stream gauges along the West Branch Delaware River. The station by the Village of Delhi , in operation since 1937, but making daily measurements since November 1996, is located .6 miles (0.97 km) upstream from the bridge on Route 28 , and 1.9 miles (3.1 km) upstream from the confluence ...
This is a list of bridges, ferries, and other crossings of the Delaware River and Delaware Bay from the Atlantic Ocean upstream to the confluence of the East Branch and West Branch at Hancock, New York. There are no tunnels under the Delaware (excepting utilities), and no dams crossing the full width of its main stem.
Ice caused a massive flood along the Delaware River on the night of March 27, 1904. During that flood, the river reached 6–8 feet (1.8–2.4 m) higher than normal and flooded much of the valley around the town of Cochecton. Flooding and ice blocks caused damage to houses, barns and other structrues in the area.