Marseille | |
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State | |
Country | |
Capital | |
Population | 863310 |
Marseille ( mar-SAY, also spelled in English as Marseilles; French: [maʁsɛj] (listen), locally [maχˈsɛjə] (listen); Occitan: Marselha [maʀˈsejɔ, -ˈsijɔ]) is the prefecture of the department of Bouches-du-Rhône and region of Provence-Alpes-Côte d'Azur in France. It is located on the coast of the Gulf of Lion, part of the Mediterranean Sea, near the mouth of the Rhône. Marseille is the second largest city in France, covering an area of 241 km2 (93 sq mi) and had a population of 870,018 in 2016. Its metropolitan area, which extends over 3,174 km2 (1,225 sq mi) is the third-largest in France after those of Paris and Lyon, with a population of 1,760,653 as of 2017, or 3,100,329 (2019) by the broader Eurostat definition of metropolitan region. Its inhabitants are called Marseillais.
One of Europe's oldest cities, founded around 600 BC and known to the ancient Greeks as Massalia (Greek: Μασσαλία, romanized: Massalía) and Romans as Massilia. Marseille has been a trading port since ancient times. In particular, it experienced a considerable commercial boom during the colonial period and especially during the 19th century, becoming a prosperous industrial and trading city. Nowadays the Old Port still lies at the heart of the city where the manufacturing of soap, its famous savon de Marseille, began some 6 centuries ago. Overlooking the port is the Basilica of Notre-Dame-de-la-Garde or "Bonne-mère" for the people of Marseille, a Romano-Byzantine church and the symbol of the city.
Aurora | |
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State | Missouri |
Country | United States |
Capital | |
Population | 7377 |
Postcode | 65605 |
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).