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Volos vs. Valley - Comparison of sizes
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Volos
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Volos vs Valley

Volos
Valley
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Volos

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Volos (Greek: Βόλος, [ˈvolos]) is a coastal port city in Thessaly situated midway on the Greek mainland, about 330 kilometres (205 miles) north of Athens and 220 kilometres (137 miles) south of Thessaloniki. It is the sixth most populous city of Greece. It is the capital of the Magnesia regional unit of Thessaly Region. Volos is the only outlet to the sea from Thessaly, the country's largest agricultural region. With a population of 144,449 (2011), it is an important industrial centre, while its port provides a bridge between Europe and Asia. Volos is the newest of the Greek port cities, with a large proportion of modern buildings erected following the catastrophic earthquakes of 1955.



It includes the municipal units of Volos, Nea Ionia and Iolkos, as well as smaller suburban communities. The economy of the city is based on manufacturing, trade, services and tourism. Home to the University of Thessaly, the city also offers facilities for conferences, exhibitions and major sporting, cultural and scientific events. Volos participated in the 2004 Olympic Games, and the city has since played host to other athletic events, such as the European Athletic Championships. Volos hosted the 7th International Olympiad on Astronomy and Astrophysics from 27 July to 5 August 2013.

Source: Wikipedia
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Valley

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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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