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Ciudad del Este vs. Valley - Comparison of sizes
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Ciudad del Este
Valley

Ciudad del Este vs Valley

Ciudad del Este
Valley
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Ciudad del Este

StateAlto Paraná

Country

Paraguay
Capital
Population 0

Informations

Ciudad del Este (Spanish pronunciation: [sjuˈðað ðel ˈeste], Spanish for Eastern City; often shortered as CDE) is the second-largest city in Paraguay and capital of the Alto Paraná Department, situated on the Paraná River. It is located 327 km from Asunción, the capital, and is adjacent to the border with Brazil, to which it is connected by the Friendship Bridge on the Paraná River. It is the largest city within the Triple Frontier region, which borders Foz do Iguaçu, Brazil and Puerto Iguazú, Argentina. The Itaipú Dam, one of the largest hydroelectric power plants in the world, is near Ciudad del Este, as is the Iguazu Falls.



Ciudad del Este is a commercial city, and is one of the largest free-trade zones in the world. Its tax-free status attracts many Brazilians and Argentines to the city.Ciudad del Este has consulates for Argentina, Brazil, Mexico, Peru, Uruguay, Spain, France, Germany, Italy, Slovakia, Syria, Turkey, and Taiwan.The city is home to Club Atlético 3 de Febrero, whose home ground Estadio Antonio Aranda was used for the 1999 Copa América and is Paraguay's third biggest football stadium.The city is the seat of the Roman Catholic Diocese of Ciudad del Este.

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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