Dnieper Rapids in the context of "Ukrainian Shield"

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⭐ Core Definition: Dnieper Rapids

The Dnieper rapids (Ukrainian: Дніпрові пороги, romanizedDniprovi porohy) also known as cataracts of the Dnieper, were the historical rapids on the Dnieper river in Ukraine, caused by outcrops of granites, gneisses and other types of bedrock of the Ukrainian Shield. The rapids began below the present-day city of Dnipro (formerly Kodak Fortress, Yekaterinoslav), where the river turns to the south, and dropped 50 meters in 66 kilometers, ending before the present-day city of Zaporizhzhia (whose name literally means "beyond the rapids").

There were nine major rapids (some sources give a smaller number), about 30–40 smaller rapids and 60 islands and islets. The rapids almost totally obstructed the navigation of the river.

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Dnieper Rapids in the context of Zaporozhian Cossacks

The Zaporozhian Cossacks or Zaporizhian Cossacks, also known as the Zaporozhian Cossack Army or the Zaporozhian Host (Ukrainian: Військо Запорозьке, romanizedViisko Zaporozke), were Cossacks who lived beyond (that is, downstream from) the Dnieper Rapids. They were predominantly Ruthenians, but also included other ethnic groups (most notably their legendary Kosh Otaman Ivan Sirko was of Moldavian origin). Along with Registered Cossacks and Sloboda Cossacks, Zaporozhian Cossacks played an important role in the history of Ukraine and the ethnogenesis of Ukrainians.

The Zaporozhian Sich grew rapidly in the 15th century from serfs fleeing the more controlled parts of the Polish–Lithuanian Commonwealth. The least controlled region, that was located between the Dniester and mid-Volga was first known from the 15th century as the Wild Fields, which was subject to colonization by the Zaporozhian Cossacks. Zaporozhian Host became established as a well-respected political entity with a parliamentary system of government. During the course of the 16th, 17th and well into the 18th century, the Zaporozhian Cossacks were a strong political and military force that challenged the authority of the Polish–Lithuanian Commonwealth, the Tsardom of Russia, and the Crimean Khanate.

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Dnieper Rapids in the context of Ukrainian Cossacks

The Zaporozhian Cossacks or Zaporizhian Cossacks, also known as the Zaporozhian Cossack Army or the Zaporozhian Host (Ukrainian: Військо Запорозьке, romanizedViisko Zaporozke), were Cossacks who lived beyond (that is, downstream from) the Dnieper Rapids. They were predominantly Ruthenians, but also included other ethnic groups (most notably their legendary Kosh Otaman Ivan Sirko was of Moldavian origin). Scientific studies conducted on the Zaporozhian Cossack genetics show that their Y-chromosomal genetic makeup forms the southern fragment of East Slavic population, with minimal levels to absence of Caucasian and Asian component in their paternal gene pool. Along with Registered Cossacks and Sloboda Cossacks, Zaporozhian Cossacks played an important role in the history of Ukraine and the ethnogenesis of Ukrainians.

The Zaporozhian Sich grew rapidly in the 15th century from serfs fleeing the more controlled parts of the Polish–Lithuanian Commonwealth. The least controlled region, that was located between the Dniester and mid-Volga was first known from the 15th century as the Wild Fields, which was subject to colonization by the Zaporozhian Cossacks. Zaporozhian Host became established as a well-respected political entity with a parliamentary system of government. During the course of the 16th, 17th and well into the 18th century, the Zaporozhian Cossacks were a strong political and military force that challenged the authority of the Polish–Lithuanian Commonwealth, the Tsardom of Russia, and the Crimean Khanate.

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Dnieper Rapids in the context of Dnieper Reservoir

The Dnieper Reservoir (Ukrainian: Дніпровське водосховище, romanizedDniprovske vodoskhovyshche) is a reservoir on the Dnieper river in Ukrainian oblasts of Dnipropetrovsk and Zaporizhzhia. The reservoir's water level is maintained by the dam of the Dnieper Hydroelectric Station, built in Zaporizhzhia from 1927 to 1932. The filling of the reservoir inundated the Dnieper Rapids.

The Samara River flows from Samara Bay into the northern end of the reservoir near Dnipro. The reservoir stretches 129 kilometres (80 mi) from there to the dam in Zaporizhzhia, and has a width of 3.2 km, a maximum width of 7 km, an average depth of 8 meters, a maximum depth of 53 meters, and a volume of 3.3 km.

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