Orange County, NY

Orange County is a county located in the U.S. state of New York. It is part of the Poughkeepsie–Newburgh–Middletown, NY Metropolitan Statistical Area and is located at the northern reaches of the New York metropolitan area. The county is in the state’s Mid-Hudson Region of the Hudson Valley.

Orange County is in southeastern New York State, directly north of the New Jersey-New York border, west of the Hudson River, east of the Delaware River and northwest of New York City. It borders the New York counties of Dutchess, Putnam, Rockland, Sullivan, Ulster, and Westchester, as well as Passaic and Sussex counties in New Jersey and Pike County in Pennsylvania.

Orange County is the only county in New York State which borders both the Hudson and Delaware Rivers.

Orange County is where the Great Valley of the Appalachians finally opens up and ends. The western corner is set off by the Shawangunk Ridge. The area along the Rockland County border (within Harriman and Bear Mountain state parks) and south of Newburgh is part of the Hudson Highlands. The land in between is the valley of the Wallkill River. In the southern portion of the county the Wallkill valley expands into a wide glacial lake bed known as the Black Dirt Region for its fertility.

The highest point is Schunemunk Mountain, at 1,664 feet (507 m) above sea level. The lowest is sea level along the Hudson.

http://en.wikipedia.org/wiki/Orange_County,_New_York

Newburgh – Beacon 1947

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A series of topographic maps shows the twin cities before the superhighways and the Newburgh-Beacon bridge.

Orange County – National Land Cover Dataset

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Orange County is one of the farthest north counties in the Metropolitan Region, serviced by the MTA Trains. They pay a special tax for that privilege. Orange County has many large forested areas, along with sprawling cities and towns, pasture land and the rich farm black dirt farm county.

Newburgh (1969 Urban Renewal Proposal vs. Today)

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[nychistory id=”19391″]

In the late 1960s and early 1970s, the city's response to the economic decline was an ambitious urban renewal plan. The city's historic waterfront area, an area composed of several square blocks which included numerous historically significant buildings, was completely demolished between 1970 and 1973. Residents were relocated, or were supposed to be relocated, to newer housing projects around Muchattoes Lake in the city's interior.

A grand complex that was planned for the urban renewal area was never built when state and federal spending began to dry up after the 1973 oil crisis. To this day, the blocks which slope down to the river remain open, grassy slopes, offering sweeping views of the Hudson but generating no property taxes for the city. Public sentiment is mixed on whether they should be built on again at all, and the city's view-protection ordinances make it less likely. Below, the waterfront was developed in the late 1990s after the city was once again able to secure grants from the state's Environmental Protection fund for riprap (a type of stone) to stabilize the shoreline.

https://en.wikipedia.org/wiki/Newburgh,_New_York