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Binghamton vs. Valley - Comparison of sizes
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Binghamton
Valley

Binghamton vs Valley

Binghamton
Valley
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Binghamton

StateNew York

Country

United States of America
Capital
Population 47376

Informations

Binghamton is a city in, and the county seat of, Broome County, New York, United States. It lies in the state's Southern Tier region near the Pennsylvania border, in a bowl-shaped valley at the confluence of the Susquehanna and Chenango Rivers. Binghamton is the principal city and cultural center of the Binghamton metropolitan area (also known as Greater Binghamton, or historically the Triple Cities), home to a quarter million people. The population of the city itself, according to the 2010 census, is 47,376.From the days of the railroad, Binghamton was a transportation crossroads and a manufacturing center, and has been known at different times for the production of cigars, shoes, and computers.



IBM was founded nearby, and the flight simulator was invented in the city, leading to a notable concentration of electronics- and defense-oriented firms. This sustained economic prosperity earned Binghamton the moniker of the Valley of Opportunity. However, following cuts made by defense firms after the end of the Cold War, the region has lost a significant portion of its manufacturing industry.Today, while there is a continued concentration of high-tech firms, Binghamton is emerging as a healthcare- and education-focused city, with the presence of Binghamton University acting as much of the driving force behind this revitalization.

Source: Wikipedia
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Valley

State

Country

Capital
Population 0

Informations

A valley is an elongated low area often running between hills or mountains which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period of time. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountain or polar areas. At lower latitudes and latitudes, these glacially-formed valleys may have been created or enlarged during ice ages but now be ice-free and occupied by streams or rivers.



In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valley are described by geographers, using terms that may be global in use or else applied only locally.

Source: Wikipedia

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