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Messina vs. Valley - Comparison of sizes
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Messina
Valley

Messina vs Valley

Messina
Valley
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Messina

State

Country

Capital
Population 236962

Informations

Messina (, also US: , Italian: [mesˈsiːna] (listen); Sicilian: Missina [mɪsˈsiːna]; Latin: Messana; Ancient Greek: Μεσσήνη, romanized: Messḗnē) is the capital of the Italian Metropolitan City of Messina. It is the third largest city on the island of Sicily, and the 13th largest city in Italy, with a population of more than 231,000 inhabitants in the city proper and about 650,000 in the Metropolitan City. It is located near the northeast corner of Sicily, at the Strait of Messina, opposite Villa San Giovanni on the mainland, and has close ties with Reggio Calabria. According to Eurostat the FUA of the metropolitan area of Messina has, in 2014, 277,584 inhabitants.



The city's main resources are its seaports (commercial and military shipyards), cruise tourism, commerce, and agriculture (wine production and cultivating lemons, oranges, mandarin oranges, and olives). The city has been a Roman Catholic Archdiocese and Archimandrite seat since 1548 and is home to a locally important international fair. The city has the University of Messina, founded in 1548 by Ignatius of Loyola. Messina has a light rail system, Tranvia di Messina, opened on 3 April 2003. This line is 7.7 kilometres (4.8 mi) and links the city's central railway station with the city centre and harbour.

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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