HUDSON HIGHLANDS PLACES TO SEE

The Hudson Fjord !

In the book "Roadside Geology of New York" by Bradford B. Van Diver, the author documents:
"The Hudson River has cut a narrow, 15-mile long gorge through the range between Peekskill and Newburgh that served as a channelway for ice erosion during Pleistocene glaciation. The gorge is a true fjord, like those of the Norwegian coast, a glacially-gouged valley now invaded by the sea, and through which daily tides reach 160 miles inland to Troy!"
The tides rise and fall an average of six feet daily through the Highlands as fresh water flows above the salt water on its way to the Atlantic Ocean.

Faults across the Hudson Gorge.


The Ramapo Canopus fault, known in the Tri-State area due to its occasional but benign activity, lies at the southernmost part of the Highlands crossing the Hudson River from Sufferen to Peekskill. Eight faults cross the Hudson Gorge in the Highlands, with many smaller secondary faults on each side of the river.

View of the Hudson Gorge from West Point showing the Fjord. Elevation of 1410 feet and 1368 feet on the left of the gorge anchor the western side of the fjord while Mount Tauris (Bull Hill) and Breakneck Mountain anchor the right or east side of the fjord.

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