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Revision as of 08:19, 10 January 2025 editFromCzech (talk | contribs)Extended confirmed users, Page movers121,333 edits page created  Latest revision as of 09:02, 10 January 2025 edit undoFromCzech (talk | contribs)Extended confirmed users, Page movers121,333 edits Characteristic 
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==Characteristic== ==Characteristic==
The Trkmanka originates in the territory of ] in the ] range at an elevation of {{cvt|249|m}} and flows to ], where it enters the Thaya River at an elevation of {{cvt|152|m}}. It is {{convert|41.7|km|abbr=on}} long. Its ] has an area of {{convert|363.3|km2|abbr=on}}.<ref name=dibavod>{{cite web |title=Základní charakteristiky toku Trkmanka a jeho povodí|url=https://www.dibavod.cz/download.php?id_souboru=2420|publisher=T. G. Masaryk Water Research Institute|language=cs|access-date=2025-01-10}}</ref> The Trkmanka originates in the territory of ] in the ] range at an elevation of {{cvt|249|m}} and flows to ], where it enters the Thaya River at an elevation of {{cvt|152|m}}. It is {{convert|41.7|km|abbr=on}} long. Its ] has an area of {{convert|363.3|km2|abbr=on}}.<ref name=dibavod>{{cite web |title=Základní charakteristiky toku Trkmanka a jeho povodí|url=https://www.dibavod.cz/download.php?id_souboru=2420|publisher=T. G. Masaryk Water Research Institute|language=cs|access-date=2025-01-10}}</ref> The average discharge at 11.2 river km in ] is {{convert|0.33|m3/s|abbr=on}}.<ref>{{cite web |title=Evidenční list hlásného profilu č.400a|url=https://hydro.chmi.cz/hppsevlist/download?seq=2505256|publisher=]|language=cs|access-date=2025-01-10}}</ref>


The longest tributaries of the Trkmanka are:<ref>{{cite web |title=Vodní toky|url=https://mapy.chmi.cz/ords/chmi_app/r/fewshlprf/stream-list?|work=Evidence hlásných profilů|publisher=]|language=cs|access-date=2025-01-10}}</ref> The longest tributaries of the Trkmanka are:<ref>{{cite web |title=Vodní toky|url=https://mapy.chmi.cz/ords/chmi_app/r/fewshlprf/stream-list?|work=Evidence hlásných profilů|publisher=]|language=cs|access-date=2025-01-10}}</ref>

Latest revision as of 09:02, 10 January 2025

River in South Moravian Region, Czech Republic
Trkmanka
The Trkmanka in Velké Pavlovice
Location
CountryCzech Republic
RegionSouth Moravian Region
Physical characteristics
Source 
 • locationŽdánice, Ždánice Forest
 • elevation249 m (817 ft)
Mouth 
 • locationThaya
 • coordinates48°48′51″N 16°50′1″E / 48.81417°N 16.83361°E / 48.81417; 16.83361
 • elevation152 m (499 ft)
Length41.7 km (25.9 mi)
Basin size363.3 km (140.3 sq mi)
Discharge 
 • average0.33 m/s (12 cu ft/s) in Velké Pavlovice
Basin features
ProgressionThayaMoravaDanubeBlack Sea

The Trkmanka is a river in the Czech Republic, a left tributary of the Thaya River. It flows through the South Moravian Region. It is 41.7 km (25.9 mi) long.

Characteristic

The Trkmanka originates in the territory of Ždánice in the Ždánice Forest range at an elevation of 249 m (817 ft) and flows to Podivín, where it enters the Thaya River at an elevation of 152 m (499 ft). It is 41.7 km (25.9 mi) long. Its drainage basin has an area of 363.3 km (140.3 sq mi). The average discharge at 11.2 river km in Velké Pavlovice is 0.33 m/s (12 cu ft/s).

The longest tributaries of the Trkmanka are:

Tributary Length (km) Side
Spálený potok 19.0 right
Lovčický potok 10.1 left
Trníček 8.8 right
Čejčský potok 7.4 left

Course

The river flows through the municipal territories of Ždánice, Dražůvky, Želetice, Násedlovice, Terezín, Krumvíř, Kobylí, Bořetice, Velké Pavlovice, Rakvice and Podivín.

Bodies of water

There are 89 bodies of water in the basin area. The largest of them are the fishponds Balaton and Jezero, both with an area of 4.5 ha (11 acres).

See also

References

  1. ^ "Základní charakteristiky toku Trkmanka a jeho povodí" (in Czech). T. G. Masaryk Water Research Institute. Retrieved 2025-01-10.
  2. "Evidenční list hlásného profilu č.400a" (in Czech). Czech Hydrometeorological Institute. Retrieved 2025-01-10.
  3. "Vodní toky". Evidence hlásných profilů (in Czech). Czech Hydrometeorological Institute. Retrieved 2025-01-10.

External links

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