Fast
Facts
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Here are some facts about the
Upper Connecticut River and its watershed.
For more, explore our web site and its
extensive links.
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length ~ depth
~ watershed
~elevation~ towns
~ state boundary ~
flow ~ dams
~ tributaries ~
water quality ~
shoreland
protection ~ special
designations
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Length
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The
Connecticut River is the largest river in New
England. It flows 410 miles from its source at
Fourth Connecticut Lake, a tiny beaver pond 300
yards from the Canadian border, to Long Island
Sound. New Hampshire and Vermont share some two
thirds of the river's length, or 275
miles.
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Depth
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The river's
depth varies from a few inches to 130' deep just
below the French King Bridge in Gill,
Massachusetts. The depth of the river in most
places is constantly changing as the river
transports and rearranges its load of
sediment.
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Watershed
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The
Connecticut River drains 4.5 million acres, or
7,000 square miles, of New Hampshire and Vermont.
This amounts to 63% of the whole four-state
watershed (which is 11,250 square miles, or 7.2
million acres). The watershed is a long basin lying
between the spines of the Green Mountains of
Vermont and the White Mountains of New
Hampshire.
The
river's
watershed
includes 41% of Vermont's total land area, 33% of
New Hampshire's, and also a very small part of
Quebec, in the Hall Stream basin.
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Elevation
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The
Connecticut River rises a few hundred yards south
of the Canadian border at Fourth Connecticut Lake,
at an elevation of 2,670 feet above sea level. It
drops half of that elevation before it ever leaves
the town of Pittsburg. By the time the river
reaches the Massachusetts line, it has fallen to
approximately 190 feet above sea level.
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Towns
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Lying within the upper Connecticut
River's watershed are 114 Vermont towns and 93 New
Hampshire towns. Fifty-three towns border the
river, 27 in Vermont and 26 in New
Hampshire.
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State boundary
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The border
between New Hampshire and Vermont was set by King
George II in 1764 as the western bank of the
Connecticut River. The U.S. Supreme Court
re-affirmed this boundary in 1934 as the ordinary
low-water mark on the Vermont shore, and markers
were set. In some places, the state line is now
inundated by the impoundments of dams built after
this time.
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Flow
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In the
Connecticut River, flows vary widely according to
location, time of year, snow melt, precipitation,
and management of dams. For more information, and
links to US Geological Survey gages that give real
time flow data, click here.
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Dams
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There are 13
existing dams
on the mainstem of the
upper Connecticut River, and two more that the
river has breached. There are hundreds of smaller
dams on tributaries throughout the
watershed.
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Tributaries
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The
Connecticut River is the sum of hundreds of
tributaries, large and small. For more information
about the major VT and NH tributaries, click
here.
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Water quality
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The
quality of the river's waters has greatly improved
in the last 40 years. To learn more about the
safety of the river for swimming, click
here.
For the State of New Hampshire's assessment of each
hydrologic unit in the watershed, click
here.
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Shoreland
protection
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Shoreland
on the NH side of the Connecticut River is
protected by state
law, which requires a 50
foot building setback and a 150 foot natural
shoreland buffer, and in many towns by local zoning
which is often more protective. While some VT towns
have local zoning that protects their Connecticut
River shoreland, there is no state protection for
shorelands in Vermont.
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Special
designations
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Congress
created the Silvio
O. Conte National Fish & Wildlife
Refuge in 1991,
encompassing the entire four-state watershed, with
the Connecticut River as its centerpiece. The
following year, NH General Court designated
the Connecticut River into the New
Hampshire Rivers Management and Protection
Program. In 1998, the
White House designated the Connecticut as an
American
Heritage
River.
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