Pechora River in the context of "Manpupuner"

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⭐ Core Definition: Pechora River

The Pechora (Russian: Печо́ра; Komi: Печӧра; Nenets: Санэроˮ яха) is the sixth-longest river in Europe. Flowing from Northwest Russia and into the Arctic Ocean, it lies mostly in the Komi Republic but the northernmost part crosses the Nenets Autonomous Okrug.

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👉 Pechora River in the context of Manpupuner

The Manpupuner rock formations (Man-Pupu-Nyor; Mansi: Мань-Пупыг-Нёр [manʲ.pupiɣ noːr], literally ’Small Idol Mountain’; Komi: Болвано-Из [bolvano iz], literally ’Idol Stone’) are a set of 7 stone pillars located west of the Ural Mountains in the Troitsko-Pechorsky District of the Komi Republic. They are located on the territory of the Pechoro-Ilychski Reserve on the mountain Man-Pupu-nyor, between the Ilych and Pechora rivers. They are also known as the Seven Strong Men Rock Formations and the Poles of the Komi Republic. Deemed one of the Seven Wonders of Russia, the Manpupuner rock formations are a popular attraction in Russia, though relatively unspoiled by tourism.

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Pechora River in the context of Mount Narodnaya

Mount Narodnaya (also known as Naroda and Poenurr; Russian: гора Народная, Komi: Народа-Из ("People's Mountain"), Mansi: Поэӈ-ур, Поэн-урр) is the highest peak of the Urals in Russia. Its elevation is 1,894 metres (6,214 ft). It is located on the border between Khanty–Mansi Autonomous Okrug in Tyumen Oblast and Komi Republic, the highest point being 0.5 km to the east from the border. The name may refer to Naroda River, which originates from the mount, located in the Research Range.

It is the highest point in European Russia outside the Caucasus. This leads to its large topographic prominence of 1,772 metres (5,814 ft). Narodnaya is located in the Ural mountains water divide, and therefore on the border between Europe and Asia: the Naroda river flows south-east from the summit into the Ob river in Siberia, and the Kos'yu river flows north-west from the summit into the Pechora river in Europe.

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Pechora River in the context of Pustozersk

67°32′N 52°35′E / 67.533°N 52.583°E / 67.533; 52.583

Pustozersk or Pustozyorsk (Russian: Пустозёрск) was the first town built by Russians north of the Arctic Circle. It was the administrative center of Yugra and Pechora regions of the Russian Empire. It was situated in what is today Nenets Autonomous Okrug, about 20 km south-west of Naryan-Mar.

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Pechora River in the context of Northern Dvina

The Northern Dvina is a river in northern Russia flowing through Vologda Oblast and Arkhangelsk Oblast into the Dvina Bay of the White Sea. Along with the Pechora River to the east, it drains most of Northwest Russia into the Arctic Ocean. It should not be confused with the Western Dvina (Daugava), to which it is not connected.

The principal tributaries of the Northern Dvina are the Vychegda (right), the Vaga (left), and the Pinega (right).

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Pechora River in the context of Naryan-Mar

Naryan-Mar (Russian: Нарья́н-Мар; Nenets: Няръяна мар, romanized: Njarjana mar, lit.'red town') is a sea and river port town and the administrative center of the Nenets Autonomous Okrug, Russia. The town is situated on the right bank of the Pechora River, 110 kilometers (68 mi) upstream from the river's mouth, on the Barents Sea. Naryan-Mar lies north of the Arctic Circle. Population: 21,658 (2010 census); 18,611 (2002 census); 20,182 (1989 Soviet census); 17,000 (1973). About half of the population of Nenetsia lives in the city.

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Pechora River in the context of Komi peoples

The Komi (Komi: комияс, romanized: komijas also коми-войтыр, komi-vojtyr) are a Permian ethnic group who are indigenous to, and primarily inhabit a region around the basins of the Vychegda, Pechora and Kama rivers in northeastern European Russia. They mostly reside in the Komi Republic, Perm Krai, Murmansk Oblast, Khanty–Mansi Autonomous Okrug, and Nenets Autonomous Okrug in the Russian Federation.

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Pechora River in the context of Barents–Kara Ice Sheet

The Barents–Kara Ice Sheet was an ice sheet which existed during the Weichselian Glaciation. It is named after the seas it was centred upon: Barents Sea and Kara Sea. The ice sheet covered the Pechora Sea, the southeastern part of the Barents Sea, Novaya Zemlya and the Kara Sea, likely reaching up to Svalbard and Franz Joseph Land in the north. In the continent, it covered from the North Russian Plain to the North Siberian Lowland.During the periods 90–80 ka and 60–50 ka, the produced ice-damming resulted in the creation of lakes and a significant rerouting of drainage in northern Eurasia, including the major rivers Yenisei, Ob, Pechora and Mezen that now flow northwards.

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