Bishkek | |
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State | |
Country | Kyrgyzstan |
Capital | |
Population | 1012500 |
Bishkek (Kyrgyz: Бишкек, Bişkek, بىشکەک, IPA: [biʃˈkek], Kazakh: Бішкек), formerly Pishpek and Frunze (Russian: Фрунзе), is the capital and largest city of Kyrgyzstan (Kyrgyz Republic). Bishkek is also the administrative centre of the Chuy Region. The state surrounds the city, even though the city itself is not part of the state, but instead a province-level unit of Kyrgyzstan. It's also near the Kazakhstan-Kyrgyzstan border.
In 1825, the Khanate of Kokand established the fortress of"Pishpek" to restrain local caravan routes and also to collect tribute from Kyrgyz tribes. On 4 September 1860, with the approval of the Kyrgyz, Russian forces led by Colonel Apollon Zimmermann destroyed the fortress. In 1868, a Russian settlement was established on the website of the fortress under its original title,"Pishpek". It lay within the General Governorship of Russian Turkestan and its Semirechye Oblast.
In 1925, the Kara-Kirghiz Autonomous Oblast was established in Russian Turkestan, encouraging Pishpek to its own capital. In 1926, the Communist Party of the Soviet Union renamed the city as Frunze, after the Bolshevik military leader Mikhail Frunze (1885--1925), who was born there.
Earth | |
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Population | 0 |
Earth is the third planet from the Sun and the only astronomical object known to harbor life. About 29% of Earth's surface is land consisting of continents and islands. The remaining 71% is covered with water, mostly by oceans but also lakes, rivers and other fresh water, which together constitute the hydrosphere. Much of Earth's polar regions are covered in ice. Earth's outer layer is divided into several rigid tectonic plates that migrate across the surface over many millions of years. Earth's interior remains active with a solid iron inner core, a liquid outer core that generates Earth's magnetic field, and a convecting mantle that drives plate tectonics.
According to radiometric dating estimation and other evidence, Earth formed over 4.5 billion years ago. Within the first billion years of Earth's history, life appeared in the oceans and began to affect Earth's atmosphere and surface, leading to the proliferation of anaerobic and, later, aerobic organisms. Some geological evidence indicates that life may have arisen as early as 4.1 billion years ago. Since then, the combination of Earth's distance from the Sun, physical properties and geological history have allowed life to evolve and thrive. In the history of life on Earth, biodiversity has gone through long periods of expansion, occasionally punctuated by mass extinctions.