253:, center of which was formerly inaccessible Jata marsh and nowadays it is a wildlife reserve of the same name. The Northern Krzna is shorter than the Southern Krzna. However, its watershed area is bigger. During the Pleistocene epoch, the valley of the Northern Krzna was one of the routes of draining meltwater to the East. Nowadays, it drains the northern area of Łuków Plain, particularly the remainings of a sandur. From the Jata reserve to the village of Gołaszyn, the Northern Krzna is on the terrain of Łuków Park of Protected Landscape.
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The Krzna is a naturally meandering river, partially unbended by hydrolological processes which constantly change her original character. In the lower current, the water levels of the Krzna are strictly dependent on the
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The average flow of the Krzna close to its estuary is 10.5 cubic metres per second (370.8 cu ft/s). The maximum range of water levels in the lower course is 3.3 metres (11 ft).
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213:. The river is 107 kilometres (66 mi) long and its watershed area is 3,273 square kilometres (1,263.7 sq mi). The Krzna flows through Poland's
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221:: Northern Krzna and Southern Krzna which is considered to be the beginning of the Krzna. The river empties into the Bug near the town of
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The
Northern Krzna is a short river which connects with the Southern Krzna in the town of
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Some sections of the Krzna valley are taken into protection, e.g. in the Bug River
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Harasimiuk, Marian; Szwajgier, Wojciech; Terpiłowski, Sławomir (2004).
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left tributaries: Krzymosza, Piszczanka, Złota
Krzywula, Klukówka
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249:. Similarly to the Southern Krzna, the river flows from
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Statistical
Yearbook of the Republic of Poland 2017
303:The most important tributaries of the Krzna are:
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229:, close to the Belarus border near, the city of
391:Michalczyk, Zdzisław; Wilgat, Tadeusz (1998).
319:The most important towns located by the Krzna
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205:is a river in eastern Poland, and a left
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156:11.4 m/s (400 cu ft/s)
134:3,273 km (1,264 sq mi)
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278:Gorge Landscape Park of Podlachia
395:. Wydawnictwo UMCS. p. 67.
393:Water relations of Lublin region
307:right tributaries: Dziegciarka,
295:(in the Southern Krzna valley).
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85: • coordinates
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420:. Lublin: UMCS. p. 164.
418:Glaciation of Warta in Poland
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233:. A canal connects it to the
57:Physical characteristics
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73: • location
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369:. Onet.pl. Archived from
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126:107 km (66 mi)
448:Tributaries of the Bug
257:Features of the Krzna
286:Kania Nature Reserve
328:Międzyrzec Podlaski
311:, Zielawa, Czapelka
247:Międzyrzec Podlaski
225:and the village of
165:Basin features
107:52.1328°N 23.5219°E
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35:Międzyrzec Podlaski
326:(Southern Krzna),
241:The Northern Krzna
215:Lublin Voivodeship
354:Statistics Poland
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453:Rivers of Poland
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202:[ˈkʂna]
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375:. Retrieved
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219:Łuków Forest
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367:"The Krzna"
299:Tributaries
289: [
282:Czapli Stóg
268:oxbow lakes
170:Progression
110: /
442:Categories
377:2011-05-22
356:, p. 85-86
337:References
198:pronounced
186:Baltic Sea
131:Basin size
98:23°31′19″E
95:52°07′58″N
264:Bug River
207:tributary
143:Discharge
33:Krzna in
223:Terespol
42:Location
209:of the
182:Vistula
47:Country
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235:Wieprz
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123:Length
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51:Poland
324:Łuków
309:Rutka
293:]
231:Brest
227:Neple
195:Krzna
178:Narew
63:Mouth
22:Krzna
422:ISBN
397:ISBN
284:and
193:The
211:Bug
174:Bug
78:Bug
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352:,
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291:pl
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184:→
180:→
176:→
430:.
405:.
380:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
