Watercourse

Tovarský potok

Váh basinSalmonid (trout)
fishing district
1
fishing district length
19.8km
region
Trenčín Region
Aerial image of watercourse Tovarský potok with the line highlighted
Blue line: course of the watercourse (approximate). Orthophoto mosaic of Slovakia © GKÚ Bratislava, CC BY 4.0Google Maps

By the water now

Today on the Tovarský potok watercourse

Fishing conditions score, the best window of the day and fishing districts from the best conditions

Average of the watercourse's fishing districts

Low activity · average of one fishing district

The number in the header is an estimate for the middle of the watercourse based on weather and measurements. The average of the fishing districts also counts satellite data, shading and geology of each district.

Best window today

06:00–08:00

Tovarský potok, window score 27.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 05:04.

Map and fishing districts of the watercourse

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

1445fishing districts
Pick a category to narrow the selection. Next to each option you can see how many fishing districts remain.
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    Water state on the watercourse

    Measurement of water level, temperature and flow, weather by the watercourse and status from satellites

    Water levels on the watercourse

    StationStatusChangeTemperature
    Tuchyňa35 cm–
    Source: SHMÚUpdated 9 Nov 2026 04:57

    Elevation profile of the watercourse

    How the watercourse falls downstream: fall, gradient and water speed.

    Fast watercourse Podhorský potok: fast water, stony bottom, riffles and the pools below them. Typical trout waters.

    2003004005006007000 km5 km10 km15 km
    Elevation profile of the watercourse: from 634 to 246 m a.s.l. over 19.8 km.
    Fishing districts in order from the highest (left) to the lowest. There may be a section without a fishing district between districts; it is not displayed.
    Highest point
    634 m a.s.l.
    Lowest point
    222 m a.s.l.
    Fall of the fishing districtsFallThe difference in altitude between the upper and lower end of the fishing district in metres. The greater the fall over a shorter length, the faster the water.
    412 m
    Average slopeWatercourse gradientFall per kilometre in per mille (‰, metres per kilometre). Up to 2 ‰ is a slow lowland river, 5 to 10 ‰ a foothill river (grayling, trout), above 10 ‰ a fast stream.
    21 ‰
    SinuositySinuosityThe length of the watercourse divided by the straight-line distance between its ends. 1.0 is a straight watercourse; above 1.3 it meanders strongly. Meanders create pools under the banks and shallows in the reaches between.
    1.17

    Source: Open Topo Data (eudem25m), 4 Nov 2026. Gradient and fall are approximate and include only the sections of fishing districts.

    Terrain in 3D

    Loading the 3D terrain model…

    Historical images

    Changes in the surroundings and nature from 2017 to 2023: how the banks, vegetation and landscape around the water change. The images switch automatically; you can also browse them by hand.

    Aerial image of watercourse Tovarský potok from 2017
    2017imaged 24 Aug 2017
    Aerial image of watercourse Tovarský potok from 2020
    2020imaged 22 Aug 2020
    Aerial image of watercourse Tovarský potok from 2023
    2023imaged 13 Aug 2023

    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 pollution on the Tovarský potok watercourse

    Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby

    Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025

    0 of 1 fishing districts on the watercourse with SHMÚ data: the nearest site has an unmet standard in at least one indicator.

    • No unmet standard1

    Groundwater: measured valuestypical value from stations within 10 km, 2025

    0 of 1 fishing district with measurements has groundwater nearby with a value above the limit for at least one indicator.

    Watercourse profile from source to mouthnumber of unmet indicators in 2025 at SHMÚ sites

    01234Červený Kameň, above, river km 13.6: no failed standard (2024)Červený Kameň, below the WWTP, river km 7.2: no failed standard (2024)Tuchyňa, river km 2.6: 1 indicator (2022)river km 14 (upper course)river km 3 (towards the mouth)
    Show sites in the table (3)
    • Červený Kameň, aboveriver km 13.6no unmet standard
    • Červený Kameň, below the WWTPriver km 7.2no unmet standard
    • Tuchyňariver km 2.61 indicator
    • standard not met
    • no unmet standard
    • site not in the yearbook

    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.

    Geology and geochemistry of the Tovarský potok stream

    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 (20 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.

    Rock under the water

    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.

    510

    Water according to the atlas

    pH 8.3modelled estimate

    water type Ca–HCO₃

    Mineralisation 410 mg/l, moderately hard water (14.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    0 from 15elements in the top 10 %

    highest: Nickel 29.5 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 69. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km35 °C55 °C

    Heat underfoot

    35°C at 1,000 m depth

    heat flow 64 mW/m²

    At a depth of 2,000 m about 55 °C (increase of 20 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    40nGy/h dose rate

    percentile 5 in Slovakia

    Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ.

    Old mine workings

    1object within 3 km

    Nearest: Halda Tunežice (spoil heap), 2.9 km from the water.

    Gold in river sediment

    0samples with gold

    10 ore minerals in the sediment

    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.

    Trace elements in the stream water

    4 from 10indicators in the top 5 %

    highest: Lead 10.0 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (Zapotok, potok).

    Boreholes and groundwater analyses

    253boreholes within 3 km

    472 water analyses nearby

    Of these, 253 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    21°C at the wellhead

    4 geothermal boreholes within 10 km

    Warmest: Belušské Slatiny – BS-1, 6.6 km from the water.

    Environmental burdens and landfills

    13sites within 3 km

    13 landfills

    No environmental burden is registered within 3 km; landfills are only recorded.

    Deposits and ore occurrences

    22records within 5 km

    12 deposits, 10 ore occurrences

    Geofond registers, the metallogenetic map and the mineral resources map.

    Landslides and slope deformations

    130areas within 3 km

    10 active

    Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed.

    Geological structure beneath the water

    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.

    • River alluvium100%SR 72 %

    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.

    Geological age of the rocks

    • Quaternary100%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains3×

    Quaternary cover

    • fluvial sediments of floodplains50%SR 68 %
    • deluvial sediments50%SR 16 %

    marker on the bar: share among all sample points on streams in Slovakia

    • Typical thickness of the Quaternary cover3.5m
    • 2 – 5100%SR 48 %

    marker on the bar: share among all sample points on streams in Slovakia

    Tectonic units

    • BIELOKARPATSKÝ PRÍKROV100%SR 4.0 %

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    Tectonic division

    • NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

    marker on the bar: share among all sample points on streams in Slovakia

    Neotectonic units

    • positive unit (mountain range)100%SR 60 %

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    Direction of neotectonic movements

    • medium uplift75%SR 32 %
    • small uplift25%SR 7.7 %

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    Regional geological division

    • intramontane basins67%SR 44 %
    • flysch belt33%SR 9.6 %

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    Regional geological division (subunits)

    • inner basins67%SR 4.5 %
    • Magura flysch33%SR 5.9 %

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    Engineering-geological districts

    • region of lowland-stream deposits100%SR 20 %

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    Engineering-geological formations

    • formation of Quaternary sediments100%SR 71 %

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    Susceptibility of the area to slope deformations

    • Region of stable areas100%SR 95 %

    marker on the bar: share among all sample points on streams in Slovakia

    The map covers 3 of 7 points on the water line.

    Hydrogeology: aquifers and groundwater

    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.

    Aquifer rocks (hydrogeological map 1:200,000)

    • Gravel40%SR 52 %
    • Limestones20%SR 3.1 %
    • Sandstones20%SR 15 %
    • Ílovce20%SR 2.9 %

    marker on the bar: share among all sample points on streams in Slovakia

    Aquifer type

    • Zvodnence s prevažne medzizrnovým typom priepustnosti (prevažne nespevnené sedimenty) (Gravel; Fluviálne)40%SR 27 %
    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Limestones)20%SR 1.9 %
    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Sandstones)20%SR 15 %
    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Ílovce)20%SR 2.8 %

    marker on the bar: share among all sample points on streams in Slovakia

    Main hydrogeological region

    • Paleogene and Mesozoic of the Bradl zone of Javorník and the northeastern part of the White Carpathians71%SR 1.8 %
    • Quaternary and Neogene Ilava Basin29%SR 0.0 %

    marker on the bar: share among all sample points on streams in Slovakia

    Surface water chemistry according to the atlas

    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.

    510

    Water acidity

    pH 8.34typical 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.

    Water hardness

    14.0°dH, moderately hard

    Sum of calcium and magnesium (2.50 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    410mg/l mineralisation

    Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds.

    Ionic composition of the water

    Water type by dominant ions: Ca–HCO₃

    Shares are in equivalents, the usual way of comparing the composition of waters.

    Major ions

    • CalciumCa81.7 mg/lpercentile 71
    • BicarbonatesHCO3251 mg/lpercentile 63
    • FluoridesF0.112 mg/lpercentile 49
    • SulphatesSO438.1 mg/lpercentile 47
    • SodiumNa6.50 mg/lpercentile 37
    • MagnesiumMg11.2 mg/lpercentile 36
    • PotassiumK2.01 mg/lpercentile 32
    • ChloridesCl4.09 mg/lpercentile 28

    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)

    Nutrients and organic pollution

    • AmmoniumNH40.279 mg/lpercentile 76
    • PhosphatesPO40.0867 mg/lpercentile 40
    • NitratesNO34.86 mg/lpercentile 36
    • Chemical oxygen demandChSK2.09 mg/lpercentile 22

    Metals

    • ZincZn7.77 μg/lpercentile 56
    • AluminiumAl80.0 μg/lpercentile 55
    • ManganeseMn23.5 μg/lpercentile 43
    • IronFe0.0760 mg/lpercentile 37

    Elements in river sediments

    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.

    Potentially toxic and trace elements

    • NickelNi29.5 mg/kgpercentile 69
    • SeleniumSe0.330 mg/kgpercentile 68
    • CopperCu28.1 mg/kgpercentile 66
    • CobaltCo9.50 mg/kgpercentile 66
    • ZincZn105 mg/kgpercentile 58
    • VanadiumV67.7 mg/kgpercentile 49
    • ChromiumCr70.4 mg/kgpercentile 47
    • LeadPb14.9 mg/kgpercentile 46
    • TinSn2.44 mg/kgpercentile 41
    • BismuthBi0.188 mg/kgpercentile 38
    • MercuryHg0.0690 mg/kgpercentile 28
    • ArsenicAs5.05 mg/kgpercentile 26
    • CadmiumCd0.0989 mg/kgpercentile 25
    • AntimonySb0.343 mg/kgpercentile 16
    • MolybdenumMo0.136 mg/kgpercentile 7

    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)

    Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
    • CalciumCa5.12 %percentile 81
    • PhosphorusP817 mg/kgpercentile 46
    • IronFe2.52 %percentile 40
    • MagnesiumMg0.794 %percentile 40
    • AluminiumAl5.32 %percentile 39
    • ManganeseMn668 mg/kgpercentile 28
    • TitaniumTi3,796 mg/kgpercentile 24
    • SodiumNa0.686 %percentile 16
    • PotassiumK1.18 %percentile 9
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • BoronB74.3 mg/kgpercentile 82
    • StrontiumSr167 mg/kgpercentile 74
    • GalliumGa16.7 mg/kgpercentile 73
    • LithiumLi34.4 mg/kgpercentile 73
    • RubidiumRb89.8 mg/kgpercentile 54
    • BerylliumBe1.00 mg/kgpercentile 28
    • BariumBa360 mg/kgpercentile 21
    • ZirconiumZr283 mg/kgpercentile 18
    • YttriumY19.8 mg/kgpercentile 15
    • CeriumCe47.4 mg/kgpercentile 13

    Natural radioactivity and radon

    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.

    20200

    Gamma radiation dose rate

    40nGy/h in air

    range 27 to 46 nGy/h

    Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains.

    Radon risk of the bedrock

    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.

    • Potassium (K)K1.17 %percentile 18
    • Equivalent thorium (eTh)eTh5.92 ppm9th percentile
    • Equivalent uranium (eU)eU1.64 ppm4th percentile

    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)

    • Areal activity of 137CsCS1371,720 Bq/m²percentile 60

    Radon risk by isopleths

    • medium83%SR 64 %
    • low17%SR 36 %

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    Geophysical fields: magnetics and gravity

    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.

    SVJZ

    Magnetic anomaly

    -4nT

    range -11 to 5 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.

    Bouguer gravity anomaly

    -44mGal

    residual −5.9 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.

    Geothermal potential

    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.

    1 km2 km35 °C55 °C

    Rock temperature with depth

    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 64 mW/m².

    Relief, climate and soils

    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.

    • Elevation of geomorphological units (from–to)203–923m a.s.l.
    • Average elevation of the units452m a.s.l.
    • Average slope11.2°
    • Average January temperature-3.5°C
    • Average July temperature18.3°C
    • Annual precipitation683mm

    Geomorphological units

    • Biele Karpaty67%SR 1.4 %
    • Považie Valley33%SR 1.5 %

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    Geomorphological regions

    • Slovak-Moravian Carpathians100%SR 5.4 %

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    Climatic-geographical types

    • basin climate100%SR 29 %

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    Susceptibility of soils to acidification

    • soils moderately susceptible to acidification43%SR 25 %
    • soils not susceptible to acidification29%SR 27 %
    • soils susceptible to acidification29%SR 31 %

    marker on the bar: share among all sample points on streams in Slovakia

    Soil contamination (map 1:500,000)

    • relatively clean soil50%SR 53 %
    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A50%SR 45 %

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    Lithogeochemical types

    • Neogene50%SR 48 %
    • Cretaceous and Paleogene of the Outer Carpathians50%SR 9.5 %

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    Map of the corridor

    Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off.

    Halda Tunežice – 5 – spoil heap (2.9 km from the water)Lednické Rovne – Manganese ores (4.0 km from the water)Mikušovce – Nad obcou – Mikušovce pri Pruskom – permanent (60 m from the water)Červený Kameň – nad cintorínom. – Červený Kameň – none (330 m from the water)Tuchyňa – Šustínsky járok – Tuchyňa – none (340 m from the water)Mikušovce – osada Babinec – Mikušovce pri Prusko – none (380 m from the water)Dúlov – Nad obcou – Dulov – cannot be estimated (860 m from the water)Dulov – Pri Váhu – Dulov – permanent (1.2 km from the water)Pruské – Nad Kamenicami – Pruské – occasional (1.6 km from the water)Nad cintorínom – Kvašov – none (1.7 km from the water)Bohunice – Nad obcou – Bohunice – permanent (2.7 km from the water)Potok pri Chachuloch – Lednica – permanent (2.8 km from the water)Krivoklát – Pod obcou – Krivoklát – occasional (2.8 km from the water)Bohunice – Pri ceste medzi Bohunicami a Krivoklá – occasional (2.8 km from the water)Krivoklát – Pod obcou – Krivoklát – permanent (2.9 km from the water)Belušské Slatiny – BS-1 – non-spa (6.6 km from the water)Belušské Slatiny – BHS-2 – non-spa (6.7 km from the water)Belušské Slatiny – BHS-1 – non-spa (6.7 km from the water)Belušské Slatiny – BHS-3 – non-spa (6.9 km from the water)a1 (3.7 km from the water)a1 (6.4 km from the water)b1 (6.7 km from the water)b1 (6.8 km from the water)b2 (6.8 km from the water)a1 (7.6 km from the water)b1 (7.8 km from the water)a1 (8.0 km from the water)Belušské Slatiny (8.0 km from the water)Tunežice – building stone (3.0 km from the water)Ilava – brick raw materials (3.1 km from the water)Tunežice – building stone (3.0 km from the water)Ilava – brick raw materials (3.1 km from the water)Krivoklát – limestone, other (4.3 km from the water)Krivoklát – calcareous marl (4.3 km from the water)Dulov – Dolné Prúdy – gravelly sands and sands (1.7 km from the water)Horovce – gravelly sands and sands (2.2 km from the water)Pruské – Kúty – gravelly sands and sands (3.4 km from the water)Lednické Rovne – Sigoť – gravelly sands and sands (4.1 km from the water)Za Váhom II – gravelly sands and sands (4.7 km from the water)Za Váhom – gravelly sands and sands (4.8 km from the water)Tuchyňa – brick raw materials (280 m from the water)Červený Kameň – pyrite (650 m from the water)Mikušovce pri Pruskom – Skalice – building stone – limestone (750 m from the water)Štrkopiesky v koryte Váhu, úsek Púchov – Tunežic – gravelly sands (1.2 km from the water)Lednická Lehota – pyrite (3.7 km from the water)Krivoklát – drahé a ozdobné kamene – limestone (3.9 km from the water)Košeca – building stone – limestone (4.0 km from the water)Sedmerovec – Pominovec – gravelly sands (4.4 km from the water)Lednické Rovne – manganese ores (4.0 km from the water)Červenokamenské bradlo – general geology (160 m from the water)Vršatské bralá – general geology (2.8 km from the water)Košeca – general geology (3.3 km from the water)MIKUSOVCE – Landslides (20 m from the water)CERVENY KAMEN – Landslides (50 m from the water)Červený Kameň – Landslides (60 m from the water)– Landslides (100 m from the water)Červený Kameň – Landslides (100 m from the water)CERVENY KAMEN – Landslides (110 m from the water)– Landslides (110 m from the water)– Landslides (140 m from the water)– Landslides (160 m from the water)CERVENY KAMEN – Landslides (160 m from the water)CERVENY KAMEN – Landslides (180 m from the water)KVASOV – Landslides (180 m from the water)CERVENY KAMEN – Landslides (180 m from the water)MIKUSOVCE – Landslides (190 m from the water)MIKUSOVCE – Landslides (200 m from the water)Červený Kameň – Landslides (220 m from the water)Červený Kameň – Landslides (220 m from the water)– Landslides (240 m from the water)CERVENY KAMEN – Landslides (240 m from the water)– Landslides (250 m from the water)KVASOV ZOSUV – Landslides (250 m from the water)CERNY KAMEN – Landslides (260 m from the water)Červený Kameň – Landslides (280 m from the water)– Landslides (280 m from the water)CERVENY KAMEN – Landslides (280 m from the water)KVASOV – Landslides (290 m from the water)– Landslides (290 m from the water)KVASOV – Landslides (290 m from the water)CERVENY KAMEN – Landslides (320 m from the water)MIKUSOVCE – Landslides (340 m from the water)– Landslides (360 m from the water)– Landslides (360 m from the water)Cerveny Kamen – Landslides (360 m from the water)CERVENY KAMEN – Landslides (370 m from the water)– Landslides (380 m from the water)– Landslides (380 m from the water)KVASOV – Landslides (410 m from the water)KVASOV – Landslides (440 m from the water)KVASOV – Landslides (460 m from the water)– Landslides (460 m from the water)– Block fields (460 m from the water)KVASOV – Landslides (490 m from the water)– Landslides (530 m from the water)KVASOV – Landslides (540 m from the water)CERVENY KAMEN – Landslides (580 m from the water)KVASOV – Landslides (580 m from the water)KVASOV – Landslides (590 m from the water)CERVENY KAMEN – Landslides (640 m from the water)– Landslides (660 m from the water)KVASOV – Landslides (670 m from the water)CERVENY KAMEN – Landslides (690 m from the water)MIKUSOVCE – Landslides (690 m from the water)– Block fields (700 m from the water)NEDASOVA LHOTA – Landslides (730 m from the water)MIKUSOVCE – Landslides (750 m from the water)CERVENY KAMEN – Landslides (840 m from the water)KVASOV – Landslides (930 m from the water)KVASOV – Landslides (970 m from the water)VRSOLSKE PODHRAD – Landslides (980 m from the water)– Landslides (1.1 km from the water)KVASOV – Landslides (1.2 km from the water)KVASOV – Landslides (1.2 km from the water)KVASOV – Landslides (1.3 km from the water)– Landslides (1.3 km from the water)KVASOV – Landslides (1.3 km from the water)– Landslides (1.4 km from the water)– Landslides (1.4 km from the water)KVASOV ZOSUV – Landslides (1.5 km from the water)KVASOV – Landslides (1.5 km from the water)– Block fields (1.5 km from the water)KVASOV – Landslides (1.5 km from the water)– Landslides (1.5 km from the water)KVASOV – Landslides (1.5 km from the water)KVASOV – Landslides (1.5 km from the water)CERVENY KAMEN – Landslides (1.5 km from the water)– Landslides (1.5 km from the water)KVASOV – Landslides (1.6 km from the water)KVASOV – Landslides (1.6 km from the water)– Landslides (1.6 km from the water)KVASOV – Landslides (1.6 km from the water)Červený Kameň – úzkoprofilový vrt s obyčajnou pitnou a ú (20 m from the water)Tuchyňa II. – úzkoprofilový vrt s obyčajnou pitnou a ú (60 m from the water)Červený Kameň – úzkoprofilový vrt s obyčajnou pitnou a ú (60 m from the water)Mikušovce – úzkoprofilový vrt s obyčajnou pitnou a ú (60 m from the water)Mikušovce – širokoprofilový vrt (Ø vŕtania nad 600 m (70 m from the water)Červený Kameň – širokoprofilový vrt (Ø vŕtania nad 600 m (70 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (70 m from the water)Miklušovce – úzkoprofilový vrt s obyčajnou pitnou a ú (70 m from the water)Červený Kameň – úzkoprofilový vrt s obyčajnou pitnou a ú (80 m from the water)– úzkoprofilový vrt s obyčajnou pitnou a ú (90 m from the water)Mikušovce – úzkoprofilový vrt s obyčajnou pitnou a ú (90 m from the water)Červený Kameň – úzkoprofilový vrt s obyčajnou pitnou a ú (90 m from the water)Mikušovce – úzkoprofilový vrt s obyčajnou pitnou a ú (100 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (100 m from the water)Tuchyňa II. – úzkoprofilový vrt s obyčajnou pitnou a ú (100 m from the water)Tuchyňa-liehovar – úzkoprofilový vrt s obyčajnou pitnou a ú (110 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (110 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (120 m from the water)Mikušovce – úzkoprofilový vrt s obyčajnou pitnou a ú (130 m from the water)Mikušovce – úzkoprofilový vrt s obyčajnou pitnou a ú (130 m from the water)Tuchyňa – negative borehole (140 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (160 m from the water)Červený Kameň – úzkoprofilový vrt s obyčajnou pitnou a ú (170 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (170 m from the water)Miklušovce – úzkoprofilový vrt s obyčajnou pitnou a ú (180 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (190 m from the water)Pruské – úzkoprofilový vrt s obyčajnou pitnou a ú (190 m from the water)Mikušovce – úzkoprofilový vrt s obyčajnou pitnou a ú (190 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (290 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (340 m from the water)Tuchyňa – úzkoprofilový vrt s obyčajnou pitnou a ú (430 m from the water)Savčina – úzkoprofilový vrt s obyčajnou pitnou a ú (580 m from the water)Podvažie-Savčina (800 m from the water)Podvažie – úzkoprofilový vrt s obyčajnou pitnou a ú (830 m from the water)Pruské – úzkoprofilový vrt s obyčajnou pitnou a ú (850 m from the water)Pruské (1.1 km from the water)Dulov – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Dulov – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Pruské – úzkoprofilový vrt s obyčajnou pitnou a ú (1.3 km from the water)Košeca – úzkoprofilový vrt s obyčajnou pitnou a ú (1.3 km from the water)5 km

    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.

    Trace elements in surface waters

    Arsenic, antimony, cadmium, lead, copper, zinc and other elements in samples from rivers and streams (Geochemical Atlas of Slovakia, surface waters, 2015). The bar shows where the highest value lies among all samples in Slovakia; the light marker is the median of the samples at this water.

    • LeadPbhigh (top 5 %)
      highest 10.0 μg/lmedian 2.50 μg/l10 samples80 % below the limit of quantification

      Highest value: Zapotok, potok1995, 40 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • StrontiumSrhigh (top 5 %)
      highest 1,010 μg/lmedian 460 μg/l10 samples

      Highest value: Tovarský, potok, 110 m from the water. Comparison: percentile 98 of all samples in Slovakia.

    • ChromiumCrhigh (top 5 %)
      highest 6.50 μg/lmedian 1.85 μg/l10 samples20 % below the limit of quantification

      Highest value: Tovarský, potok1995, 80 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • BariumBahigh (top 5 %)
      highest 130 μg/lmedian 88.0 μg/l7 samples

      Highest value: Červený Kameň, 1450 m JZ od K635 Zavlacne1995, 540 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • CadmiumCdelevated (top 10 %)
      highest 0.600 μg/lmedian 0.150 μg/l10 samples80 % below the limit of quantification

      Highest value: Červený Kameň, 1450 m JZ od K635 Zavlacne, 540 m from the water. Comparison: percentile 93 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 17.0 μg/lmedian 5.00 μg/l10 samples90 % below the limit of quantification

      Highest value: Tovarský, potok, 110 m from the water. Comparison: percentile 81 of all samples in Slovakia.

    • CopperCutypical value
      highest 2.30 μg/lmedian 1.40 μg/l10 samples40 % below the limit of quantification

      Highest value: Mikušovce, 1200 m SV od K470 Kalvária1995, 70 m from the water. Comparison: percentile 73 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.760 μg/lmedian 0.500 μg/l10 samples80 % below the limit of quantification

      Highest value: Tovarský, potok, 110 m from the water. Comparison: percentile 47 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification

      Highest value: Dulov, 1500 m JJZ od K2651995, 110 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • AntimonySbbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification

      Highest value: Dulov, 1500 m JJZ od K2651995, 110 m from the water. Comparison: percentile 37 of all samples in Slovakia.

    Major ions, mineralisation and pH

    Basic water chemistry: which rocks the minerals in it come from.

    • Silicon dioxideSiO2slightly elevated
      highest 27.7 mg/lmedian 6.72 mg/l10 samples

      Highest value: Tovarský, potok, 110 m from the water. Comparison: percentile 86 of all samples in Slovakia.

    Gold and ore minerals in river sediments

    Regional panning prospecting: the heavy fraction was washed out of river gravel and the mineral grains in it were counted. The map of finds is positive: a sample without gold is not listed in the atlas, so the absence of a find is not proof that there is no gold.

    • Barite (BaSO₄)26 samples, at most 815 grains
    • Ilmenit (FeTiO₃)26 samples, at most 1815 grains
    • Limonite (FeO(OH)·nH₂O)26 samples, at most 815 grains
    • Magnetite (Fe₃O₄)26 samples, at most 1815 grains
    • Rutil (TiO₂)26 samples, at most 815 grains
    • Anatas (TiO₂)25 samples, at most 55 grains
    • Pyrite (FeS₂)20 samples, at most 815 grains
    • Monazit ((Ce,La,Nd)PO₄)15 samples, at most 55 grains
    • Hematite (Fe₂O₃)11 samples, at most 55 grains
    • Kasiterit (SnO₂)2 samples, at most 1 grains

    Rock-forming and accessory minerals

    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)26 samples, at most 1815 grains
    • Tourmalines (complex borosilicate)26 samples, at most 315 grains
    • Zirconium (ZrSiO₄)26 samples, at most 1815 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))21 samples, at most 55 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)19 samples, at most 1115 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))15 samples, at most 55 grains
    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)13 samples, at most 55 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))7 samples, at most 55 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)5 samples, at most 55 grains
    • Korund (Al₂O₃)2 samples, at most 5 grains
    • Andaluzit (Al₂SiO₅)1 sample, at most 5 grains
    • Sillimanit (Al₂SiO₅)1 sample, at most 5 grains

    Groundwater: chemistry, water types and radioactivity

    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.

    Metals in groundwater

    • CopperCuextreme (top 1 %)
      highest 24.5 μg/lmedian 0.850 μg/l38 samples

      Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • ZincZnextreme (top 1 %)
      highest 4,925 μg/lmedian 19.5 μg/l38 samples

      Highest value: studňa1993, 1.0 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • CadmiumCdextreme (top 1 %)
      highest 1.90 μg/lmedian 0.250 μg/l38 samples95 % below the limit of quantification

      Highest value: prameň1993, 780 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • LithiumLihigh (top 5 %)
      highest 112 μg/lmedian 12.0 μg/l38 samples

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 98 of all samples in Slovakia.

    • AluminiumAlhigh (top 5 %)
      highest 0.130 mg/lmedian 0.0100 mg/l38 samples39 % below the limit of quantification

      Highest value: prameň1993, 110 m from the water. Comparison: percentile 97 of all samples in Slovakia.

    • SeleniumSehigh (top 5 %)
      highest 3.00 μg/lmedian 0.500 μg/l38 samples89 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • MercuryHghigh (top 5 %)
      highest 0.200 μg/lmedian 0.100 μg/l38 samples97 % below the limit of quantification

      Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • ChromiumCrelevated (top 10 %)
      highest 3.10 μg/lmedian 0.250 μg/l38 samples79 % below the limit of quantification

      Highest value: studňa1993, 200 m from the water. Comparison: percentile 93 of all samples in Slovakia.

    • AntimonySbelevated (top 10 %)
      highest 0.500 μg/lmedian 0.100 μg/l38 samples97 % below the limit of quantification

      Highest value: studňa1993, 910 m from the water. Comparison: percentile 92 of all samples in Slovakia.

    • ArsenicAselevated (top 10 %)
      highest 2.60 μg/lmedian 0.500 μg/l38 samples92 % below the limit of quantification

      Highest value: vrt1993, 2.5 km from the water. Comparison: percentile 91 of all samples in Slovakia.

    • LeadPbelevated (top 10 %)
      highest 2.00 μg/lmedian 0.500 μg/l38 samples76 % below the limit of quantification

      Highest value: studňa1993, 1.0 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l17 samples100 % below the limit of quantification

      Highest value: vrt1993, 2.5 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    well822,1 Bq/l12.2 Bq/l
    source619,6 Bq/l12.0 Bq/l
    developed spring525,3 Bq/l16.3 Bq/l
    water source for public supply223,9 Bq/l13.4 Bq/l

    Mine workings, deposits and ore occurrences

    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.

    Types of mining objects

    • spoil heap1×

    Nearest old mine workings

    NameTypeMinedEndedFrom the water
    Halda Tunežicespoil heapbuilding stone2.9 km

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    Dulov – Dolné Prúdygravelly sands and sandsMined deposit – AGROFARMA, spol. s r.o. Červený Kameň1.7 km
    Horovcegravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – ZEMPRA, s.r.o.2.2 km
    Tunežicebuilding stoneMined deposit – PK Metrostav, a.s.3.0 km
    Tunežicebuilding stoneMined deposit – PK Metrostav, a.s.3.0 km
    Ilavabrick raw materialsDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená3.1 km
    Ilavabrick raw materialsDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená3.1 km
    Pruské – Kútygravelly sands and sandsMined deposit – INFINITY TRUST, s.r.o.3.4 km
    Lednické Rovne – Sigoťgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – SESTAV, s.r.o.4.1 km
    Krivoklátlimestone, otherDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.3 km
    Krivoklátcalcareous marlDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.3 km
    Za Váh IIgravelly sands and sandsMined deposit – SESTAV s.r.o.4.7 km
    Za Váhgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – SESTAV s.r.o.4.8 km

    Ore occurrences in the metallogenic map

    OccurrenceOre typeMetalsTypeFrom the water
    Lednické RovneManganese oresMnmineralogical occurrence4.0 km

    Boreholes and Geofond archive reports

    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.

    253 boreholes in the 3 km zone, of which 73 hydrogeological and 180 other; with an archive report number 253.

    Borehole depths

    • up to 10 m111×
    • 10–30 m129×
    • 30–100 m7×
    • 100–300 m2×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Červený Kameňnarrow-diameter borehole with ordinary drinking and process water8.0 m21014 97Cb2.pdf20 m
    S-9engineering-geological5.0 m1192020 m
    S-12engineering-geological2.5 m1192030 m
    T-6hydrogeological10.0 m6680640 m
    S-10engineering-geological5.0 m1192040 m
    Tuchyňa II.narrow-diameter borehole with ordinary drinking and process water11.0 m66806 97Cd30.pdf60 m
    Červený Kameňnarrow-diameter borehole with ordinary drinking and process water14.4 m88899 97Cd47.pdf60 m
    Mikušovcenarrow-diameter borehole with ordinary drinking and process water12.0 m74629 97Cd41.pdf60 m
    HVT-4hydrogeological11.0 m6680660 m
    T-5hydrogeological10.0 m6680660 m
    V-1engineering-geological6.0 m9943460 m
    S-1engineering-geological8.0 m1192060 m

    Geothermal energy and mineral waters

    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.

    BoreholeTemperatureYieldDepthChemical water typeUseFrom the water
    Belušské Slatiny – BS-121 °C–58.5 mCa-HCO3-(SO4)unused6.6 km
    Belušské Slatiny – BHS-220 °C–501 mCa-Na-HCO3-SO4unused6.7 km
    Belušské Slatiny – BHS-121 °C–226 mCa-Na-HCO3-SO4unused6.7 km
    Belušské Slatiny – BHS-321 °C0.0 l/s1671 mCa-Na-HCO3-SO4unused6.9 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 543.7 km
    category b1mineral water15-22< 536.7 km
    category b2mineral water15-225-1516.8 km
    category Belušské Slatinythermal baths––18.0 km

    Environmental burdens, landfills and anthropogenic sediments

    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.

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom the water
    Mikušovce – Nad obcou – Mikušovce pri Pruskom–1975–60 m
    Červený Kameň – nad cintorínom. – Červený Kameň–1975–330 m
    Tuchyňa – Šustínsky járok – Tuchyňa–1975–340 m
    Mikušovce – osada Babinec – Mikušovce pri Pruskom–1985–380 m
    Dúlov – Nad obcou – Dulov–1970–860 m
    Dulov – Pri Váh – Dulov–1970–1.2 km
    Pruské – Nad Kamenicami – Pruské–1975–1.6 km
    Nad cintorínom – Kvašov–1975–1.7 km

    Landslides and slope deformations

    Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel.

    Types of deformations

    • Landslides126×
    • Block fields4×

    Degree of activity

    • Potenciálny81×
    • Stabilizovaný39×
    • Aktívny9×
    • With potential and active forms1×

    Current state

    • SD taken from archival materials, ktorá bola konfrontova52×
    • Processed only in the scope of registration on a scale of 1:25,00042×
    • SD prebraná z archívnych materiálov (existuje inž. geologick7×
    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S5×

    How to read these data

    • Zone and distance. The distance is measured from the line of the water to the point in the register (to the centre for areas), with an accuracy of tens of metres. Counts apply only to the zone, not to the whole catchment.
    • Percentile. For chemistry, the highest value is compared with all atlas samples in Slovakia. It is not a legal limit or a health risk assessment; the atlases are historical (published: surface waters 2015, groundwater 1996, river sediments 1999).
    • Limit of quantification. Many samples have a value at the lowest level the laboratory can determine; such results mean "below the limit". For these, the position in the distribution is an estimate.
    • Šlichy. Only samples with a find are recorded. The number of grains in a concentrate is not the gold content in grams per tonne.
    • Relation to water. A mine working, landfill or burden nearby proves nothing about the quality of the water in the stream. It serves as a prompt for attention and a starting point for further investigation.
    • Sample points. The area and raster maps of ŠGÚDŠ cannot be downloaded as points, so along the line of each fishing district the value is looked up at points roughly every 3 km. It is a sample of the line, not a continuous record; a very short section may have a single point.
    • Atlas rasters. The chemistry of water and sediments is an interpolation of measurements in a sampling network (Geochemical Atlas of Slovakia). The value at a point is a modelled estimate for the surroundings, not a measurement in the water. The percentile compares the average of this stream with all sample points on streams in Slovakia.
    • Positions and scales. The maps have different scales (1:50,000 to 1:1,000,000), so the level of detail differs between sections. A map outside its coverage means there is no area at that point, not that there is nothing there.

    Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology.

    Organizations and location

    Who manages the fishing districts and where they are

    Organizations on the watercoursewho manages the fishing districts and what the conditions are there today

    1. Dubnica nad V1 fishing district · 20 km20Tovarský potok20

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    Váh basin