Kosový potok explained

Kosový potok
Source1 Location:Stará Voda, Upper Palatine Forest
Mouth Location:Mže
Mouth Coordinates:49.7989°N 12.8314°W
Progression:Mže
Subdivision Type1:Country
Subdivision Name1:Czech Republic
Subdivision Type2:Regions
Length Km:46.4
Discharge1 Avg:1.29m3/s in Třebel
Basin Size Km2:226.1

The Kosový potok (also called Kosí potok) is a stream and a left tributary of the Mže in the Czech Republic. It flows through the Plzeň and Karlovy Vary regions. It is 46.4km (28.8miles) long.

Name

The name literally means 'blackbird stream'.

Characteristic

The Kosový potok originates in the territory of Stará Voda in the Upper Palatine Forest on the slope of Dyleň Mountain at an elevation of and flows to Planá, where it enters the Mže River at an elevation of . It is 46.4km (28.8miles) long. Its drainage basin has an area of 226.1km2.[1] The average discharge at the 4.8 river km is 1.29m3/s.[2]

The longest tributaries of the Kosový potok are:[3]

Tributary Length (km) Side
Úšovický potok 10.6 left
Senný potok 10.2 right
Jilmový potok 8.5 left
Bahnitý potok 8.1 left

Course

The stream flows through the municipal territories of Stará Voda, Tři Sekery, Valy, Velká Hleďsebe, Mariánské Lázně, Chodová Planá, Lestkov, Olbramov, Černošín and Planá.

Bodies of water

There are 265 bodies of water in the basin area. The largest of them is the fishpond Regent with an area of, built on the Senný potok. There are no fishponds or reservoirs built directly on the Kosový potok.[1]

Use

There used to be many water mills on the stream. The existence of 35 mills is documented. Today, only ruins remain of most.[4]

Nature

The middle course of the stream flows through the protected landscape area of Slavkov Forest.

Species of animals that are endangered within the Czech Republic and live in or near the stream include brook lamprey, European crayfish, Eurasian beaver, common kingfisher and white-throated dipper.[4] [5]

Bridges

In Dolní Kramolín (part of Chodová Planá), the stream is bridged by a valuable stone bridge, protected as a cultural monument. Originally built in the Baroque style in the first half of the 18th century, it was rebuilt into its present form in the 19th century.[6]

Tourism

The lower course of the stream flows through a valley with meanders, without human intervention. An long educational trail leads through the valley.[4]

The Kosový potok is suitable for river tourism, but it is navigable only in spring and after heavy rains.[7]

See also

External links

Notes and References

  1. Web site: Základní charakteristiky Kosového potoka a jeho povodí. T. G. Masaryk Water Research Institute. cs. 2024-11-28.
  2. Web site: Evidenční list hlásného profilu č.164. Czech Hydrometeorological Institute. cs. 2024-11-28.
  3. Web site: Vodní toky. Evidence hlásných profilů. Czech Hydrometeorological Institute. cs. 2024-11-28.
  4. Web site: Údolí Kosího potoka. CzechTourism. cs. 2024-11-28.
  5. Web site: Koncepce ochrany přírody a krajiny Karlovarského kraje na období 2016–2025. Karlovy Vary Region. 80. cs. 2024-11-28.
  6. Web site: Silniční most. National Heritage Institute. cs. 2024-11-28.
  7. Web site: Kosový potok (Kosák). Pádler. cs. 2024-11-28.