Beginning as an overflow of Otsego Lake, near Cooperstown, New York, the
Susquehanna River travels south 444 miles before emptying into the Chesapeake
Bay in Maryland at a rate of 19 million gallons of water every minute.
In an average year, water from the Susquehanna accounts for over half
the fresh water flowing into the Chesapeake Bay.
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Rock Run
Grist Mill, erected in 1794, is a three story stone structure and is fully
operational. Inside are displays of 19th century farm and mill equipment.
The water powered mill is operated during the summer months.
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One rooom inside the mill.
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Abundant with
spring wildflowers including arrowhead, pussy toes, mayapple, trout lilies,
Virginia bluebells, and trillium species. Numerous ferns and several endangered
plant species live in this habitat.
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With
a 13million-acre drainage basin, the watershed of the Susquehanna River
is the second largest in the eastern United States, encompassing over
half the state of Pennsylvania as well as parts of Maryland and New York
. While the river is broad, it is not deep -- it is the longest non-commercially
navigable river in the country.
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Wooded ridges
and valleys flank the wide Susquehanna River. Trails visit hardwood forests
and rolling agricultural fields with opportunities to observe herds of
white-tailed deer, wild turkeys and other wildlife.
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