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Stoke-on-Trent vs. Aurora - Comparison of sizes
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Stoke-on-Trent
Aurora

Stoke-on-Trent vs Aurora

Stoke-on-Trent
Aurora
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Stoke-on-Trent

State

Country

Capital
Population 0

Informations

Stoke-on-Trent (often abbreviated to Stoke) is a city and unitary authority area in Staffordshire, England, with an area of 36 square miles (93 km2). Together with the neighbouring boroughs of Newcastle-under-Lyme and Staffordshire Moorlands, it is part of North Staffordshire. In 2016, the city had a population of 261,302. It is the largest settlement in Staffordshire. Stoke is polycentric, having been formed by the federation of six towns in 1910. It took its name from Stoke-upon-Trent where the main centre of government and the principal railway station in the district were located.



Hanley is the primary commercial centre. The other four towns are Burslem, Tunstall, Longton, and Fenton. Stoke-on-Trent is the home of the pottery industry in England and is commonly known as the Potteries, with the local residents known as Potters. Formerly a primarily industrial conurbation, it is now a centre for service industries and distribution centres.

Source: Wikipedia
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Aurora

StateMissouri

Country

United States
Capital
Population 7377
Postcode65605

Informations

An aurora (plural: auroras or aurorae), sometimes referred to as polar lights (aurora polaris), northern lights (aurora borealis), or southern lights (aurora australis), is a natural light display in the Earth's sky, predominantly seen in high-latitude regions (around the Arctic and Antarctic). Auroras are the result of disturbances in the magnetosphere caused by solar wind. These disturbances are sometimes strong enough to alter the trajectories of charged particles in both solar wind and magnetospheric plasma. These particles, mainly electrons and protons, precipitate into the upper atmosphere (thermosphere/exosphere).



The resulting ionization and excitation of atmospheric constituents emit light of varying color and complexity. The form of the aurora, occurring within bands around both polar regions, is also dependent on the amount of acceleration imparted to the precipitating particles. Precipitating protons generally produce optical emissions as incident hydrogen atoms after gaining electrons from the atmosphere. Proton auroras are usually observed at lower latitudes.

Source: Wikipedia

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