The 'Delaware River' is a river on the
Atlantic coast of the
United States.
The Delaware was explored by
Adriaen Block as part of the
New Netherlands Colony, and was named the ''South River'' to mark the southernmost reach of that colony.
The river meets tide-water at
Trenton, New Jersey. Its total length, from the head of the longest branch to the capes, is 410 miles (660 km), and above the head of the bay its length is 360 miles (579 km). The mean freshwater discharge of the Delaware River into the estuary is 11,550 cubic feet (330 m³) per second.
The Delaware River constitutes in part the boundary between
Pennsylvania and
New York, the entire boundary between
New Jersey and Pennsylvania, and most of the boundary between
Delaware and New Jersey. A historical oddity, the Delaware-New Jersey Border is actually at the eastern-most river shoreline within the
Twelve-Mile Circle of New Castle, rather than the usual mid river or mid channel borders, causing small portions of the New Jersey peninsula falling west of the shoreline to fall under the jurisdiction of Delaware. The rest of the borders follow a mid-channel approach.
Commerce was once important on the upper river, primarily prior to railway competition (
1857).
★ The
Delaware Division of the Pennsylvania Canal, running parallel with the river from Easton to Bristol, opened in 1830.
★ The
Delaware and Raritan Canal, which runs along the New Jersey side of the Delaware River from
Milford to
Trenton, unites the waters of the Delaware and
Raritan rivers as it empties the waters of the Delaware River via the canal outlet in
New Brunswick. This canal water conduit is still used as a water supply source by the State of
New Jersey.
★ The
Morris Canal (now abandoned and almost completely filled in) and the
Delaware and Hudson Canal connected the Delaware and
Hudson rivers.
★ The
Chesapeake and Delaware Canal joins the waters of the Delaware with those of the
Chesapeake Bay.
The mean tides below
Philadelphia are about 6 feet. The magnitude of the commerce of Philadelphia has made the improvements of the river below that port of great importance. Small improvements were attempted by
Pennsylvania as early as
1771.
In the "project of 1885" the United States government undertook systematically the formation of a 26 ft (8 m) channel 600 ft (180 m) wide from Philadelphia to deep water in
Delaware Bay. The River and Harbor Act of
1899 provided for a 30 foot (9 m) channel 600 feet (180 m) wide from Philadelphia to the deep water of the bay.
Course
The main,
west or Mohawk branch rises in
Schoharie County, New York, about 1886 feet (575 m) above the sea, near
Mount Jefferson, and flows tortuously through the plateau in a deep trough, impounded at one point to create the
Cannonsville Reservoir, and then becoming the state boundary at the
42nd parallel, until it emerges from the
Catskills. Similarly, the
East Branch begins from a small pond south of
Grand Gorge in the
town of
Roxbury in
Delaware County, flowing southward toward its impoundment by New York City to create the
Pepacton Reservoir, the largest reservoir in the
New York City water supply system. The
confluence is just south of
Hancock.

The lower Delaware as viewed from
New Castle in 2006
After leaving the mountains and plateau, the river flows down broad
Appalachian valleys, skirts the
Kittatinny range, which it crosses at the
Delaware Water Gap, between nearly vertical walls of limestone, and passes through a quiet and charming country of farm and forest, diversified with plateaus and escarpments, until it crosses the Appalachian plain and enters the hills again at
Easton, Pennsylvania. From this point it is flanked at intervals by fine hills, and in places by cliffs, of which the finest are the Nockamixon Rocks, 3 miles (5 km) long and above 200 feet (60 m) high.
At Trenton there is a fall of 8 feet (2.4 m). Below Trenton the river flows between
Philadelphia and
New Jersey before becoming a broad, sluggish inlet of the sea, with many marshes along its side, widening steadily into its great estuary, Delaware Bay.
Tributaries
Its main
tributaries in New York are the
Mongaup and
Neversink rivers and
Callicoon Creek; from Pennsylvania, the
Lackawaxen,
Lehigh, and
Schuylkill rivers; and from New Jersey,
Rancocas Creek and the
Musconetcong and
Maurice rivers.
Oldmans and
Raccoon creeks are tributaries in New Jersey.

A 1655 nautical chart showing part of the Delaware River
★
Appoquinimink River
★
Alloway Creek
★
Assiscunk Creek
★
Assunpink Creek
★
Big Timber Creek
★
Brodhead Creek
★
Bushkill
★
Chester Creek
★
Christina River
★
Cooper River (New Jersey)
★
Crafts Creek
★
Crosswicks Creek
★
Equinunk Creek
★
Flat Brook
★
Frankford Creek
★
Lehigh River
★
Lockatong Creek
★
Maurice River
★
Musconetcong River
★
Neshaminy Creek
★
Oldmans Creek
★
Paulins Kill
★
Pennypack Creek
★
Pequest River
★
Pomoeston creek
★
Pohatcong Creek
★
Poquessing Creek
★
Raccoon Creek (New Jersey)
★
Rancocas Creek
★
Ridley Creek
★
Salem River
★
Schuylkill River
★
Shohola Creek
★
Tohickon Creek
★
Wickecheoke Creek
Flooding
The Delaware has experienced a number of serious flooding events as the result of snow melt and/or rain run-off from heavy rainstorms. Record flooding occurred in August 1955, in the aftermath of the passing of the remnants of two separate hurricanes over the area within less than a week: first
Hurricane Connie and then
Hurricane Diane, which was, and still is, the wettest tropical cyclone to have hit the northeastern United States. The river gauge at Riegelsville, PA recorded an all time record crest of 38.85 feet on 8/19/1955.
More recently, moderate to severe flooding has occurred along the river. The same gauge at Riegelsville recorded a peak of 30.95 feet on 9/23/2004, 34.07 feet on 4/4/2005, and 33.62 feet on 6/28/2006, all considerably higher than the flood stage of 22 feet. Source:
USGS
See Also:
(State of New Jersey: RECENT FLOODING EVENTS IN THE DELAWARE RIVER BASIN)
Since the upper Delaware basin has few population centers along its banks, flooding in this area mainly affects natural unpopulated flood plains. Residents in the middle part of the Delaware basin experience flooding, including three major floods in the past three years that have severely damaged their homes and land. The lower part of the Delaware basin from Philadelphia southward to the Delaware Bay is tidal and much wider than portions further north, and is not prone to river related flooding (although tidal surges can cause minor flooding in this area).
The Delaware River Basin Commission, along with local governments, is working to try to address the issue of flooding along the river. As the past few years have seen a rise in catastrophic floods, most residents of the river basin feel that something must be done. However, due to insufficient federal funds, progress is slow.
[1]
New York City Water Supply
After
New York City had made 15 reservoirs (with more to come) for their water supply, and with a growing population, the city tried to gain permission to make five reservoirs along the Delaware River's tributaries. However, they were denied the permission to impound the Delaware's tributaries to make new reservoirs. So in
1928, New York City decided to draw water from the Delaware River to feed the population boom that had started during the beginning of the
Great Depression. There were, however, villages and towns across the river in
Pennsylvania that were already using the Delaware for their water supply. The two sides eventually took their case to the
U.S. Supreme Court, and in
1931, New York City was finally allowed to draw 440 million gallons of water a day from the Delaware and its upstream tributaries.
Crossings
Main articles: List of crossings of the Delaware River
The Delaware River is a major barrier to travel between
New Jersey and
Pennsylvania. Most of the larger bridges are tolled only westbound, and are owned by the
Delaware River and Bay Authority,
Delaware River Port Authority,
Burlington County Bridge Commission or
Delaware River Joint Toll Bridge Commission.
Washington's crossing of the Delaware
Main articles: Washington's crossing of the Delaware
Perhaps the most famous “Delaware Crossing” involved the improvised boat crossing undertaken by
George Washington’s army during the
American Revolution on
Christmas Day, 1776. This led to a successful surprise attack on the
Hessian troops occupying
Trenton, New Jersey.
Major oil spills
A number of
oil spills have taken place in the Delaware over the years.
[1][2][3]
★ 01-31-1975 — 11,000,000 gallions of crude oil spilled from the ''Corinthos'' tanker
★ 09-28-1985 — 435,000 gallons of crude oil spilled from the ''Grand Eagle'' tanker after running aground on
Marcus Hook Bar
★ 06-24-1989 — 306,000 gallons of crude oil spilled from the ''Presidente Rivera'' tanker after running aground on
Claymont Shoal
★ 11-26-2004 — 265,000 gallons of crude oil spilled from the ''Athos 1'' tanker; the tanker's hull had been punctured by a submerged, discarded anchor
See also
★
Burlington County Bridge Commission
★
Delaware River Joint Toll Bridge Commission
★
Delaware River Port Authority
★
List of Delaware rivers
★
List of New Jersey rivers
★
List of New York rivers
★
List of Pennsylvania rivers
★
Tocks Island Dam Project
★
Upper Delaware Scenic and Recreational River
★
Washington Crossing
Notes
1. Athos 1 Oil Spill
2. 1985 Grand Eagle Oil Spill
3. Presidente Rivera Spill – June 24, 1989
References
★
★
DEVASTATION ON THE DELAWARE: Stories and Images of the Deadly Flood of 1955 (2005,
Word Forge Books, Ferndale, PA) The only comprehensive documentary of this weather disaster in the Delaware River Valley.
External links
★
Delaware River Basin Commission
★
Delaware Riverkeeper Network
★
National Park Service: Delaware Water Gap National Recreation Area
★
National Park Service: Upper Delaware Scenic & Recreational River
★
National Park Service: Lower Delaware Wild & Scenic River
★
U.S. Geological Survey: NJ stream gaging stations
★
U.S. Geological Survey: NY stream gaging stations
★
U.S. Geological Survey: PA stream gaging stations