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Quito vs. Valley - Comparison of sizes
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Quito
Valley

Quito vs Valley

Quito
Valley
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Quito

State

Country

Capital
Population 1873458

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Quito (; Spanish pronunciation: [ˈkito] (listen); Quechua: Kitu; formally Saint Francis of Quito) is the capital of Ecuador, the country's most populous city and at an elevation of 2,850 metres (9,350 ft) above sea level, it is the second highest official capital city in the world, and the closest to the equator. It is located in the Guayllabamba river basin, on the eastern slopes of Pichincha, an active stratovolcano in the Andes Mountains. In 2008, the city was designated as the headquarters of the Union of South American Nations.The historic centre of Quito is one of the largest, least-altered and best-preserved in the Americas.



Quito and Kraków, Poland, were the first World Cultural Heritage Sites declared by UNESCO, in 1978. The central square of Quito is located about 25 kilometres (16 mi) south of the equator; the city itself extends to within about 1 kilometre (0.62 mi) of zero latitude. A monument and museum marking the general location of the equator is known locally as la mitad del mundo (the middle of the world), to avoid confusion, as the word Ecuador is Spanish for equator.

Source: Wikipedia
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Valley

State

Country

Capital
Population 0

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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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