Along the Delaware River
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About this ebook
Richard C. Albert
Richard C. Albert has studied the Delaware River for more than twenty-five years and is currently the Delaware Riverkeeper Network scientist. He has written extensively on the Delaware River and river management. Carrie E. Albert holds a master's degree in history with certification in museum studies from the University of Delaware. She has interned at the Historical Society of Delaware and Frank Lloyd Wright's Fallingwater.
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Along the Delaware River - Richard C. Albert
Harlan.
INTRODUCTION
In the spring of 1764, Dan Skinner pushed a lumber raft off the banks of the upper Delaware River and headed to Philadelphia, Pennsylvania. For the next 150 years, men like Skinner made lumber rafting big business on the river. Each year, hundreds of rafts headed downriver. Like all the chapters in the Delaware River story, lumber rafting reflects the interactions of people and their natural landscape along a river corridor.
The Delaware River begins as two tiny trickles of water flowing from springs high in the Catskill Mountains of New York. The northern trickle becomes the West Branch of the Delaware River, and the southern one, the East Branch. In the town of Hancock, New York, the two tributaries merge, forming the Delaware River. From there, the river flows 331 miles to the Atlantic Ocean. At Trenton, New Jersey, 200 miles from Hancock and 134 miles from the Atlantic Ocean, the river becomes tidal. The last 48 miles of the tidal reach is Delaware Bay. Almost 60 rivers in the United States are longer than the Delaware River, and 32 of these carry more water in a typical year.
People have been working and playing along the Delaware River for thousands of years. It was the home of the Lenni Lenape (or Delaware Indians) prior to the arrival of European settlers. In 1610, Henry Hudson and the Dutch ship Half Moon wandered into Delaware Bay. Hudson named the river the South River. In the following year, Samuel Argall discovered it for England. Argall named what is now Cape Henlopen after Virginia’s governor, Lord De La Warre. After the English gained control of the region from the Dutch in 1664, the name De La Warre was applied to the whole river.
The Delaware River region is the birthplace of the American Revolution. On July 4, 1776, the Declaration of Independence was signed in Independence Hall, several blocks from the river in Philadelphia. Six months later, General Washington and his ragtag army made their daring nighttime crossing of the Delaware and saved the Revolution. In 1787, the Constitutional Convention met in Philadelphia and drafted the U.S. Constitution.
It can be argued that the industrial revolution began in the United States with the first shipment of coal to Philadelphia, via the Lehigh Canal and the Delaware River. Beginning in the mid-18th century, industrial development along the tidal Delaware made the region one of the largest urban-industrial complexes in the world. It remains the second largest concentration of petro-chemical plants in the United States. Seventy percent of oil delivered to the east coast goes to Delaware River refineries.
A boundary is created by the Delaware River between four states: Delaware, New Jersey, New York, and Pennsylvania. Eight million people live in its 13,539-square-mile watershed. Although the watershed is only two fifths percent of the land area in the United States, almost eight percent of the population gets water from it, including New York City and Philadelphia.
The Delaware is one of the last undammed major rivers in the United States. It is not, however, completely free flowing. During times of low flow, reservoirs owned by New York City and various power companies release much of the water seen farther south in the river. These flows are mandated by a 1931 U.S. Supreme Court decree, amended in 1954, that allowed large water-supply reservoirs to build on the West Branch, East Branch, and Neversink Rivers in New York. In spite of the reservoir releases, it is still very much a natural river.
Recreation is also an important part of the history of the Delaware River. Certainly one of the first resort hotels in the United States, the Kittatinny House was opened in 1833 in the Delaware Water Gap. The Delaware has been a source of good times for over two centuries, and millions still enjoy the river each year, making it one of the premier recreational rivers in the country. More than 175 miles of the 200-mile nontidal Delaware have been placed in the National Wild and Scenic Rivers System; the crown jewels of American rivers.
Heading downriver—whether by raft, canoe, or boat—is a Delaware River tradition. Although nothing can replace the real experience, this book offers a vicarious journey down the river as it appeared in the early 20th century.
Lumber rafting lasted longer on the Delaware than on many other rivers. In 1783, New Jersey and Pennsylvania restricted dams on the Delaware to avoid impeding rafts traveling downriver. The existence of this treaty, many years later, helped keep the Delaware River mainstream free of dams. In this view, two rafts are heading downstream. The location is unidentified.
One
HEADWATERS TO PORT JERVIS, NEW YORK
The first section of our trip is the upper Delaware River that flows between Pennsylvania and New York. The West Branch and East Branch of the river flow west from the Catskill Mountains and join in Hancock, New York, to form the Delaware River. The upper Delaware travels 77 miles to Port Jervis, New York. It is the steepest section of the river, with an average drop of more than six feet per mile. The river actually steps down