Hudson Valley
The Hudson Valley is a valley of the Hudson River. It runs from about Westchester County to Albany.
The Hudson River valley runs in a north-south direction across eastern New York State. There are many rock types in the valley. This includes Triassic sandstones and redbeds in the south, and the Palisades Sill. Older Precambrian gneiss is in the north (and east).
In the Hudson Highlands, the river enters a fjord. This fjord was cut during previous ice ages. To the west are the very long Appalachian highlands. Near Tappan Zee Bridge, the west side of the river has high cliffs. They are about 400–800 feet high.[1]
Most of the Hudson Valley is part of the Appalachian Mountains.[2] The northern part of the Hudson Valley is part of the Great Lakes area.
During the last ice age, the valley was filled by a large glacier. The glacier went down as far as Long Island. Near the end of the last ice age, the Great Lakes drained south down the Hudson River. The drained water is called Lake Iroquois.[3] Lake Ontario is the remnant of that lake.
Hudson Valley Media
Map of Washington's retreat through New York and New Jersey
Robert Havell, Jr., View of the Hudson River from Tarrytown, c. 1866
The Stone Barns Center for Food & Agriculture is a leading nonprofit farm and educational center in the region.
The main laboratory building of the IBM Watson Research Center is located in Yorktown Heights.
The Mid-Hudson Bridge, connecting Poughkeepsie and Highland
The Yonkers station serves Amtrak intercity trains and Metro-North commuter trains.
References
- ↑ Van Diver, B.B. 1985. Roadside Geology of New York. Mountain Press, Missoula. p. 59-63.
- ↑ "Physiographic divisions of the conterminous U. S." U.S. Geological Survey. Retrieved 2007-12-06.
- ↑ Eyles, N. Ontario Rocks: Three Billion Years of Environmental Change. Fitzhenry & Whiteside, Markham, Ontario. 339 p.
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