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1 - The Hudson River Estuary: Executive Summary

Published online by Cambridge University Press:  06 January 2010

Jeffrey S. Levinton
Affiliation:
Department of Ecology and Evolution, Stony Brook University
John R. Waldman
Affiliation:
Hudson River Foundation
Jeffrey S. Levinton
Affiliation:
State University of New York, Stony Brook
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Summary

From the Tear of the Clouds to the Verrazano

The ecological and cultural importance of the Hudson is surely not revealed by its size. Its drainage basin is about 34,000 square kilometers (km) (13,000 square miles), which is less than one percent of the United States. In contrast, the Mississippi drains about half of the area of the lower 48 states. Compared to the mighty Mississippi's length of 3,700 km, the Hudson, originating in the Adirondacks and pulsing to the sea through the Verrazano Narrows, flows over a main course of only 500 km (ca. 300 miles).

Henry Hudson and his crew first saw the mouth of the Hudson in 1609, but it wasn't until the 1870s that its origin was declared, at tiny Lake Tear of the Clouds, near Mt. Marcy in the Adirondacks. The small rivers and streams flowing from Adirondack peaks over 1000 meters (m) in elevation descend to a lowland drainage usually less than 100 m above sea level. Below Troy the river is navigable to the Narrows entrance to the ocean.

The Terrane

The Hudson River drains New York, and parts of Vermont, Massachusetts, Connecticut, and New Jersey. The basin contains three subareas: the upper Hudson from Mt. Marcy to Troy, the Mohawk from Rome to Troy, and the lower Hudson from Troy to New York Bay (we try to stick to this terminology throughout the book, but some authors have failed us).

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Publisher: Cambridge University Press
Print publication year: 2006

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