Damascus vs Aurora

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Damascus ( də-MASS-kəs; Arabic: دِمَشْق, romanized: Dimašq [diˈmaʃq], Syrian Arabic: [dɪˈmaʃʔ] is the capital of Syria; it became the country's largest city in the early 2010s, after the decrease in population of Aleppo during the struggle for the city. It's colloquially known in Syria as aš-Šām (الشَّام) and titled the"City of Jasmine" (مَدِينَة الْيَاسْمِين Madīnat al-Yāsmīn). Damascus is a major cultural centre of the Levant and the Arab world. The town had an estimated population of 2,079,000 as of 2019. In south-western Syria, Damascus is the center of a large metropolitan area of 2.7 million people (2004). Embedded on the eastern foothills of the Anti-Lebanon mountain range 80 kilometres (50 mi) inland from the eastern shore of the Mediterranean on a plateau 680 metres (2,230 feet ) above sea level, Damascus encounters a dry climate because of the rain shadow effect.

The Barada River flows through Damascus. Damascus is one of the oldest continuously inhabited cities in the world. First settled in the 2nd millennium BC, it was selected as the capital of the Umayyad Caliphate from 661 to 750. Following the success of the Abbasid dynasty, the chair of Islamic power was transferred to Baghdad. Damascus saw its importance decline throughout the Abbasid era, only to regain substantial value from the Ayyubid and Mamluk periods. Today, it's the seat of the central government and each the government ministries. As of September 2019, eight years to the continuing Syrian Civil War, Damascus was appointed the least livable city in the worldwide Liveability Ranking.

Source: Wikipedia

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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