Izhma River
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The Izhma () is a river in the
Komi Republic The Komi Republic (; ), sometimes simply referred to as Komi, is a republics of Russia, republic of Russia situated in the northeast of European Russia. Its capital city, capital is the types of inhabited localities in Russia, city of Syktyvka ...
of
Russia Russia, or the Russian Federation, is a country spanning Eastern Europe and North Asia. It is the list of countries and dependencies by area, largest country in the world, and extends across Time in Russia, eleven time zones, sharing Borders ...
. It is a left
tributary A tributary, or an ''affluent'', is a stream or river that flows into a larger stream (''main stem'' or ''"parent"''), river, or a lake. A tributary does not flow directly into a sea or ocean. Tributaries, and the main stem river into which they ...
of the
Pechora Pechora (; ) is a types of inhabited localities in Russia, town in the Komi Republic, Russia, located on the Pechora (river), Pechora River, west of and near the northern Ural Mountains. The area of the town is . Population: History Pechor ...
. It is long, with a
drainage basin A drainage basin is an area of land in which all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, ...
of . At a point from its mouth, it has an average discharge of . The river freezes over in November, and stays icebound until the spring thaw starts in May. Main tributaries are the Ukhta, Ayuva and Sebys. The Izhma has its sources in the Timan Ridge. In its upper course the banks are wooded, while its lower parts is characterized by meadows and bogs. The river is twisting, and in its upper reaches it forms rapids and rocky stretches. At its confluence with the Ukhta lies the town of Sosnogorsk. The Izhma is navigable to its confluence with the Ukhta. In its lower parts the river widens, its flow slows down and it starts forming
meander A meander is one of a series of regular sinuous curves in the Channel (geography), channel of a river or other watercourse. It is produced as a watercourse erosion, erodes the sediments of an outer, concave bank (cut bank, cut bank or river cl ...
s and small islands. It flows into the Pechora at Ust-Izhma.


References

{{Authority control Rivers of the Komi Republic