Fishing conditions score, the best window of the day and fishing districts from the best conditions Low activity · average of one fishing district 15:00–17:00 VN Kadurka, window score 25. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 12:04. The course of the watercourse and its fishing districts. You can switch the line color to today's conditions, quality or any other parameter. Detailed filtersregion, district, riverbed, depth, shading, satellites, water chemistry and pollution, fish, geology Move the map with two fingers. In full-screen mode one finger is enough. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. For each fishing district you can see what it is made of, how well it is supported by data and where the data comes from. Terrain height along the fishing district and the approximate water level. Reservoir This is a reservoir, so the watercourse is not assessed here: the water has no current, fall or gradient. The chart shows the terrain height along the fishing district. Source: Open Topo Data (eudem25m), 4 Nov 2026. The height is approximate (error of a few metres). Loading the 3D terrain model… Changes in the surroundings and nature from 2018 to 2024: how the banks, vegetation and landscape around the water change. The images switch automatically; you can also browse them by hand. Orthophoto mosaic of Slovakia © GKÚ Bratislava, NLC Zvolen. The year and day of imaging depend on the location, so individual years may differ in season and weather. Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby 0 of 1 fishing district with measurements has groundwater nearby with a value above the limit for at least one indicator. Source: SHMÚ (yearbooks on surface and groundwater quality), the register of wastewater treatment plants from VÚVH and the EEA. A SHMÚ site is assigned to a fishing district by the same watercourse name and by distance; the yearbook lists the sites that failed the standard, so a missing site is not proof of clean water. Metals and gold in river sediments and water, old mine workings and deposits, boreholes with archive reports, geothermal energy, environmental burdens and landslides around the stream The overview is based on public registers and atlases of the State Geological Institute of Dionýz Štúr. The search covers a zone around the water of all fishing districts of the stream (0 km of line in total): stream samples within 1 km, boreholes, mine workings and burdens within 3 km, ore occurrences within 5 km, geothermal sources within 10 km. River alluvium100% of the water line Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000. pH 8.2modelled estimate water type Ca–HCO₃ Mineralisation 361 mg/l, moderately hard water (11.8 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Chromium 80.9 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 63. Interpolation of the Geochemical Atlas of river sediments. 35°C at 1,000 m depth heat flow 55 mW/m² At a depth of 2,000 m about 55 °C (increase of 20 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 43nGy/h dose rate percentile 10 in Slovakia Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ. 1object within 3 km Nearest: Kutacie práce (other type of object), 2.6 km from the water. 0samples with gold No gold was found in river sediment samples within 1 km of the water. The samples do not cover every stream, so this does not mean there is no gold here. – There is no measurement in the surface water atlas samples within 1 km of the water. 96boreholes within 3 km 153 water analyses nearby Of these, 95 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 2 geothermal and mineral water springs within 10 km. 17sites within 3 km 4 environmental burdens, 13 landfills Nearest burden: Kotešová – skládka PO a KO, 990 m from the water. Proximity does not mean that substances leak from the site into the water. 8records within 5 km 4 deposits, 4 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 55areas within 3 km 7 active Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed. Which rock lies beneath the water line (Geological Map of Slovakia 1:50,000), how old it is, how thick the Quaternary cover is and in which tectonic unit the water flows. The bedrock decides the hardness of the water, the bottom, the turbidity after rain and the abundance of springs. The points follow the water line (for a stream and a basin, fishing district after fishing district). The strip is a cross-section by distance, not a map; the width of a section corresponds to the number of points. marker on the bar: share among all sample points on streams in Slovakia River alluvium: Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia The map covers 1 of 1 points on the water line. Streams and rivers are fed by groundwater. Hydrogeological maps show in which rocks the water is stored, how permeable they are and what the water in them is like. The data come from ŠGÚDŠ maps, not from measurements at a particular water. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia Modelled composition of the water in the area the fishing district line runs through. The rasters of the Geochemical Atlas of Slovakia (surface waters) are an interpolation of measurements in sampled streams, so they show the typical background of the area, not a measurement in a particular stream. pH 8.19typical range Most rivers and streams in Slovakia have a pH of 6.5 to 8.5. More acidic water is found in streams on acidic rocks (granites, quartzites), more alkaline water near limestones. 11.8°dH, moderately hard Sum of calcium and magnesium (2.11 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 361mg/l mineralisation Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds. Water type by dominant ions: Ca–HCO₃ Shares are in equivalents, the usual way of comparing the composition of waters. dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile) The Geochemical Atlas of Slovakia (river sediments) describes what the river carries in the fine material on its bed. Sediment collects metals from rocks, ore occurrences and past mining and industry. It is not a legal limit or a health risk assessment: it shows how an element on this stream ranks among streams in Slovakia. dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile) Airborne gamma-ray spectrometry by ŠGÚDŠ measures radiation from potassium, uranium and thorium in rocks and soil. Granites and some acidic volcanic rocks have the highest values, limestones and floodplains the lowest. Caesium-137 is a remnant of fallout from the Chernobyl accident and nuclear weapons tests. 43nGy/h in air Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains. medium Radon is a natural gas from rocks. The risk concerns buildings and cellars, not the water in the stream; it shows what the bedrock is like. dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile) marker on the bar: share among all sample points on streams in Slovakia Maps of the magnetic field and gravity (ŠGÚDŠ) reveal what lies beneath the sediments and the surface: volcanic bodies, faults and crustal thickness. For an angler they are interesting indirectly: they show where the bedrock changes, and with it the water. +37nT range 37 to 37 nT Deviation of the Earth's magnetic field from its surroundings. Positive and negative anomalies reveal rocks with magnetite (basalts, basic volcanic rocks) and boundaries in the bedrock. -59mGal residual −16.4 mGal Negative values lie over thick sediments and under mountains (light crust), positive over dense rocks and thinner crust. It shows the structure of the Earth's crust, not the water. The Atlas of Geothermal Energy of Slovakia records rock temperature and heat flow from the Earth's interior. It is the potential of the area, not the actual warmth of the water in the stream. Specific geothermal boreholes and springs near this water are in the geothermal energy section below. 35 / 55 °Cat depths of 1,000 and 2,000 m increase of 20 °C per km The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 55 mW/m². A basin is not just water: slope and elevation determine the speed of runoff, climate the temperature and amount of water, and soils what is washed into the stream. The data come from the geomorphological division, climatic-geographical types and soil maps of ŠGÚDŠ. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off. The line is the water of the fishing district, the light band is the 3 km zone in which boreholes, mine workings and burdens were searched for. The map shows the nearest objects (at most a few dozen from each register), not all of them. The points correspond to the position in the register; area objects are marked by their centre. Hydrogeochemical objects (analyses of springs and boreholes), the geochemical atlas of groundwater (1996) and radiohydrochemical sampling. Groundwater feeds streams, so its composition also affects the water in the stream. Highest value: vrt1992, 760 m from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: vrt1992, 760 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: vrt1992, 760 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1992, 2.5 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: vrt1992, 2.6 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: vrt1992, 760 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: drenáž1992, 2.1 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: prameň1992, 1.8 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: prameň1992, 2.1 km from the water. Comparison: percentile 81 of all samples in Slovakia. Highest value: vrt1992, 1.6 km from the water. Comparison: percentile 79 of all samples in Slovakia. Highest value: prameň1992, 2.5 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1992, 2.5 km from the water. Comparison: percentile 39 of all samples in Slovakia. Old mine workings outside mining areas (Geofond register), deposits and mining areas, and the metallogenetic map. Gold, silver and other metals near streams can get into sediments and water. Register of hydrogeological boreholes, other boreholes and geothermal boreholes. Each borehole has a report in the Geofond archive (geological profiles, pumping tests, chemical analyses of the water); the report number is in the table. 96 boreholes in the 3 km zone, of which 36 hydrogeological and 60 other; with an archive report number 95. Geothermal boreholes (wellhead water temperature, yield, chemical type) and sources of geothermal and mineral waters within 10 km. Data on the use and existence of a borehole come from the Geofond register. Recorded environmental burdens (industrial sites, landfills, mining), the register of waste landfills and monitoring of anthropogenic sediments (industrial sludge). It is a list of places, not a measurement of water pollution. Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. Who manages the fishing districts and where they are Váh basin
By the water now
Today on the VN Kadurka watercourse
Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the watercourse
Elevation profile: reservoir
Terrain in 3D
Historical images



Water pollution on the VN Kadurka watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VN Kadurka stream
Rock under the water
Water according to the atlas
Elements in river sediment
Heat underfoot
Natural gamma radiation
Old mine workings
Gold in river sediment
Trace elements in the stream water
Boreholes and groundwater analyses
Geothermal energy
Environmental burdens and landfills
Deposits and ore occurrences
Landslides and slope deformations
Geological structure beneath the water
Geological age of the rocks
Most common rock units
System Age Unit Points Quaternary Pleistocene – Holocene proluvial sediments: clays, sandy loams and clay gravels with debris in the higher floodplain cones 1× Tectonic units
Tectonic division
Regional geological division
Regional geological division (subunits)
Engineering-geological districts
Engineering-geological formations
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Aquifer rocks (hydrogeological map 1:200,000)
Aquifer type
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
69.0 mg/lpercentile 57221 mg/lpercentile 5339.6 mg/lpercentile 498.02 mg/lpercentile 455.97 mg/lpercentile 400.0827 mg/lpercentile 319.29 mg/lpercentile 291.70 mg/lpercentile 25Nutrients and organic pollution
0.175 mg/lpercentile 650.0905 mg/lpercentile 413.94 mg/lpercentile 262.20 mg/lpercentile 25Metals
0.249 mg/lpercentile 8073.4 μg/lpercentile 73129 μg/lpercentile 678.15 μg/lpercentile 58Elements in river sediments
Potentially toxic and trace elements
80.9 mg/kgpercentile 6327.0 mg/kgpercentile 610.292 mg/kgpercentile 6025.1 mg/kgpercentile 560.109 mg/kgpercentile 5388.3 mg/kgpercentile 417.57 mg/kgpercentile 3513.0 mg/kgpercentile 340.172 mg/kgpercentile 3159.4 mg/kgpercentile 280.243 mg/kgpercentile 231.99 mg/kgpercentile 200.360 mg/kgpercentile 184.03 mg/kgpercentile 120.0635 mg/kgpercentile 10Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
3.61 %percentile 71668 mg/kgpercentile 26635 mg/kgpercentile 233,679 mg/kgpercentile 202.16 %percentile 180.632 %percentile 171.21 %percentile 114.15 %percentile 70.481 %percentile 4Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
484 mg/kgpercentile 75139 mg/kgpercentile 5228.5 mg/kgpercentile 4558.7 mg/kgpercentile 441.05 mg/kgpercentile 30381 mg/kgpercentile 2910.5 mg/kgpercentile 2321.0 mg/kgpercentile 1848.9 mg/kgpercentile 1672.6 mg/kgpercentile 15Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
2.34 ppm24th percentile6.18 ppm13th percentile1.05 %percentile 82,547 Bq/m²percentile 81Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Rock temperature with depth
Relief, climate and soils
Climatic-geographical types
Susceptibility of soils to acidification
Soil contamination (map 1:500,000)
Map of the corridor
Groundwater: chemistry, water types and radioactivity
Chemical water types nearby
Water quality class according to the hydrogeochemical map
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median source 1 3,28 Bq/l 3.28 Bq/l water source for individual supply 1 21,5 Bq/l 21.5 Bq/l well 1 8,87 Bq/l 8.87 Bq/l Mine workings, deposits and ore occurrences
Types of mining objects
Nearest old mine workings
Name Type Mined Ended From the water Kutacie práce other type of object coal 1929 2.6 km Deposits and mining areas
Deposit Mineral Status and organisation From the water Kotešová gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – VÁHOSTAV, a.s. 600 m Kotešová – Sihoť – Oblazov gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – OBCHOD S PALIVAMI, s.r.o. 2.6 km Veľká Bytča gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – SDP, spol. s r.o. 4.3 km Veľká Bytča gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – Ján Korbáš VANDO 4.3 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water HV-10 engineering-geological 10.0 m 100480350 m VN98-4 environment – 96444390 m VZ-3-1 engineering-geological 8.0 m 86882400 m HV-9 engineering-geological 10.0 m 100480420 m VN98-3 environment – 96444430 m Kotešová narrow-diameter borehole with ordinary drinking and process water 11.0 m 53726 98Ac62.pdf480 m VN98-2 environment – 96444490 m VZ-3-2 engineering-geological 8.0 m 86882550 m VS-01 hydrogeological 3.0 m 102120590 m DPS-02 engineering-geological 6.8 m 102120610 m DPS-01 engineering-geological 8.0 m 102120630 m IG-01 engineering-geological 8.0 m 102120630 m Geothermal energy and mineral waters
Sources of geothermal and mineral waters
Source Type Water temperature (°C) Yield (l/s) Count Nearest from water category a1 mineral water < 15 < 5 1 4.2 km category a5 mineral water < 15 > 50 1 5.4 km Environmental burdens, landfills and anthropogenic sediments
Environmental burdens
Site Activity Substance Classification From the water Kotešová – landfill PO a KO SK1000500P 990 m Hlboké nad Váh – landfill KO (pod brezami) V SK2001800F 1.8 km Hlboké nad Váh – landfill KO II SK2001800F 2.0 km Bytča – bývalý areál SAD SK1000500P 2.6 km Waste landfills
Landfill Area Year established Monitoring From the water Kotešová štrkovisko – Kotešová – – – 900 m Hlboké nad Váh – – – 1.3 km Hlboké nad Váh – landfill KO (pod brezami) – Hlboké nad Váh – – – 1.9 km Hlboké nad Váh – landfill KO II – Hlboké nad Váh 40 m² – – 2.0 km Dolný Hričov 1 – Dolný Hričov – – monitored 2.1 km Dolný Hríčov – Dolný Hričov – – – 2.3 km Hričovské Podhradie 1 – Hričovské Podhradie – – – 2.3 km Bytča – Hlboké nad Váh 60 m² – – 2.5 km Landslides and slope deformations
Types of deformations
Degree of activity
Current state
How to read these data
Organizations and location
Organizations on the watercoursewho manages the fishing districts and what the conditions are there today
More watercourses nearby
20from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
MercuryHghigh (top 5 %)
highest 0.400 μg/lmedian 0.100 μg/l11 samples91 % below the limit of quantification
ZincZnhigh (top 5 %)
highest 1,988 μg/lmedian 14.0 μg/l11 samples18 % below the limit of quantification
CadmiumCdhigh (top 5 %)
highest 0.900 μg/lmedian 0.250 μg/l11 samples91 % below the limit of quantification
ChromiumCrhigh (top 5 %)
highest 4.10 μg/lmedian 0.250 μg/l11 samples82 % below the limit of quantification
LeadPbhigh (top 5 %)
highest 3.00 μg/lmedian 0.500 μg/l11 samples73 % below the limit of quantification
AluminiumAlelevated (top 10 %)
highest 0.0500 mg/lmedian 0.00500 mg/l11 samples91 % below the limit of quantification
ArsenicAselevated (top 10 %)
highest 2.30 μg/lmedian 0.500 μg/l11 samples91 % below the limit of quantification
AntimonySbelevated (top 10 %)
highest 0.400 μg/lmedian 0.100 μg/l11 samples64 % below the limit of quantification
LithiumLislightly elevated
highest 23.0 μg/lmedian 7.00 μg/l11 samples
CopperCuslightly elevated
highest 2.40 μg/lmedian 0.800 μg/l11 samples
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l6 samples100 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l11 samples100 % below the limit of quantification



