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Ashgabat vs. Aurora - Comparison of sizes
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Ashgabat
Aurora

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Ashgabat vs Aurora

Ashgabat
Aurora
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Ashgabat

State

Country

Turkmenistan
Capital
Population 909,000

Informations

Ashgabat (Turkmen: Aşgabat; Ашгабат, pronounced [ɑʃʁɑˈbɑt], Persian: عشق آباد‎; Russian: Ашхабад), formerly named Poltoratsk (Russian: Полтора́цк, IPA: [pəltɐˈratsk]) between 1919 and 1927, is the capital and the largest city of Turkmenistan. It is situated between the Karakum Desert and the Kopet Dag mountain range in Central Asia. It is also near the Iran-Turkmenistan border. The city was founded in 1881 on the basis of an Ahal Teke tribal village, and made the capital of the Turkmen Soviet Socialist Republic in 1924.



Much of the city was destroyed by the 1948 Ashgabat earthquake but has since been extensively rebuilt under the rule of Saparmurat Niyazov’s "White City" urban renewal project, resulting in monumental projects sheathed in costly white marble. The Soviet-era Karakum Canal runs through the city, carrying waters from the Amu Darya from east to west. Since 2019, the city has been recognized as having one of the highest costs of living in the world largely due to Turkmenistan's inflation and import issues.

Source: Wikipedia
Change

Aurora

StateMissouri

Country

United States
Capital
Population 7,377
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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