Watercourse

VN Kadurka

fishing district
1
fishing district length
0.3km
region
Žilina Region
Aerial image of watercourse VN Kadurka 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 VN Kadurka 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

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.

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
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    Elevation profile: reservoir

    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.

    3043053063073083093100.0 km0.1 km0.2 km0.3 km
    Terrain elevation profile (Reservoir): from 309 to 305 m a.s.l. over 0.3 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    307 m a.s.l.

    Source: Open Topo Data (eudem25m), 4 Nov 2026. The height is approximate (error of a few metres).

    Terrain in 3D

    Loading the 3D terrain model…

    Historical images

    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.

    Aerial image of watercourse VN Kadurka from 2018
    2018imaged 13 Sep 2018
    Aerial image of watercourse VN Kadurka from 2021
    2021imaged 10 Sep 2021
    Aerial image of watercourse VN Kadurka from 2024
    2024imaged 24 Aug 2024

    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 VN Kadurka watercourse

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

    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.

    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 VN Kadurka 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 (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.

    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 8.2modelled 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.

    Elements in river sediment

    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.

    1 km2 km35 °C55 °C

    Heat underfoot

    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.

    20200

    Natural gamma radiation

    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.

    Old mine workings

    1object within 3 km

    Nearest: Kutacie práce (other type of object), 2.6 km from the water.

    Gold in river sediment

    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.

    Trace elements in the stream water

    –

    There is no measurement in the surface water atlas samples within 1 km of the water.

    Boreholes and groundwater analyses

    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.

    Geothermal energy

    –

    2 geothermal and mineral water springs within 10 km.

    Environmental burdens and landfills

    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.

    Deposits and ore occurrences

    8records within 5 km

    4 deposits, 4 ore occurrences

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

    Landslides and slope deformations

    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.

    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
    QuaternaryPleistocene – Holoceneproluvial sediments: clays, sandy loams and clay gravels with debris in the higher floodplain cones1×

    Tectonic units

    • MAGURSKÝ PRÍKROV100%SR 34 %

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

    Tectonic division

    • NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

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

    Regional geological division

    • flysch belt100%SR 9.6 %

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

    Regional geological division (subunits)

    • Magura flysch100%SR 5.9 %

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

    Engineering-geological districts

    • region of proluvial cones and mantles100%SR 2.7 %

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

    Engineering-geological formations

    • formation of Quaternary sediments100%SR 71 %

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

    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 1 of 1 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)

    • Gravel100%SR 52 %

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

    Aquifer type

    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Gravel)100%SR 22 %

    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 8.19typical 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.

    Water hardness

    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.

    Dissolved substances

    361mg/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

    • CalciumCa69.0 mg/lpercentile 57
    • BicarbonatesHCO3221 mg/lpercentile 53
    • SulphatesSO439.6 mg/lpercentile 49
    • SodiumNa8.02 mg/lpercentile 45
    • ChloridesCl5.97 mg/lpercentile 40
    • FluoridesF0.0827 mg/lpercentile 31
    • MagnesiumMg9.29 mg/lpercentile 29
    • PotassiumK1.70 mg/lpercentile 25

    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

    • AmmoniumNH40.175 mg/lpercentile 65
    • PhosphatesPO40.0905 mg/lpercentile 41
    • NitratesNO33.94 mg/lpercentile 26
    • Chemical oxygen demandChSK2.20 mg/lpercentile 25

    Metals

    • IronFe0.249 mg/lpercentile 80
    • ManganeseMn73.4 μg/lpercentile 73
    • AluminiumAl129 μg/lpercentile 67
    • ZincZn8.15 μg/lpercentile 58

    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

    • ChromiumCr80.9 mg/kgpercentile 63
    • NickelNi27.0 mg/kgpercentile 61
    • SeleniumSe0.292 mg/kgpercentile 60
    • CopperCu25.1 mg/kgpercentile 56
    • MercuryHg0.109 mg/kgpercentile 53
    • ZincZn88.3 mg/kgpercentile 41
    • CobaltCo7.57 mg/kgpercentile 35
    • LeadPb13.0 mg/kgpercentile 34
    • BismuthBi0.172 mg/kgpercentile 31
    • VanadiumV59.4 mg/kgpercentile 28
    • MolybdenumMo0.243 mg/kgpercentile 23
    • TinSn1.99 mg/kgpercentile 20
    • AntimonySb0.360 mg/kgpercentile 18
    • ArsenicAs4.03 mg/kgpercentile 12
    • CadmiumCd0.0635 mg/kgpercentile 10

    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)
    • CalciumCa3.61 %percentile 71
    • PhosphorusP668 mg/kgpercentile 26
    • ManganeseMn635 mg/kgpercentile 23
    • TitaniumTi3,679 mg/kgpercentile 20
    • IronFe2.16 %percentile 18
    • MagnesiumMg0.632 %percentile 17
    • PotassiumK1.21 %percentile 11
    • AluminiumAl4.15 %percentile 7
    • SodiumNa0.481 %percentile 4
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • ZirconiumZr484 mg/kgpercentile 75
    • StrontiumSr139 mg/kgpercentile 52
    • LithiumLi28.5 mg/kgpercentile 45
    • BoronB58.7 mg/kgpercentile 44
    • BerylliumBe1.05 mg/kgpercentile 30
    • BariumBa381 mg/kgpercentile 29
    • GalliumGa10.5 mg/kgpercentile 23
    • YttriumY21.0 mg/kgpercentile 18
    • CeriumCe48.9 mg/kgpercentile 16
    • RubidiumRb72.6 mg/kgpercentile 15

    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

    43nGy/h in air

    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.

    • Equivalent uranium (eU)eU2.34 ppm24th percentile
    • Equivalent thorium (eTh)eTh6.18 ppm13th percentile
    • Potassium (K)K1.05 %percentile 8

    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 137CsCS1372,547 Bq/m²percentile 81

    Radon risk by isopleths

    • medium100%SR 64 %

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

    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

    +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.

    Bouguer gravity anomaly

    -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.

    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 55 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.

    • Average January temperature-3.8°C
    • Average July temperature17.8°C
    • Annual precipitation700mm

    Climatic-geographical types

    • basin climate100%SR 29 %

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

    Susceptibility of soils to acidification

    • soils not susceptible to acidification100%SR 27 %

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

    Soil contamination (map 1:500,000)

    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A100%SR 45 %

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

    Map of the corridor

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

    Kutacie práce – 6 – other type of object (2.6 km from the water)Kotešová – skládka PO a KO – SK1000500P (990 m from the water)Hlboké nad Váhom – skládka KO (pod brezami) V – SK2001800F (1.8 km from the water)Hlboké nad Váhom – skládka KO II – SK2001800F (2.0 km from the water)Bytča – bývalý areál SAD – SK1000500P (2.6 km from the water)Kotešová štrkovisko – Kotešová – permanent (900 m from the water)Hlboké nad Váhom – none (1.3 km from the water)Hlboké nad Váhom – skládka KO (pod brezami) – Hl – none (1.9 km from the water)Hlboké nad Váhom – skládka KO II – Hlboké nad Vá – none (2.0 km from the water)Dolný Hričov 1 – Dolný Hričov – none (2.1 km from the water)Dolný Hríčov – Dolný Hričov – none (2.3 km from the water)Hričovské Podhradie 1 – Hričovské Podhradie – none (2.3 km from the water)Bytča – Hlboké nad Váhom – none (2.5 km from the water)Bytča – Hliník nad Váhom – none (2.5 km from the water)Dolný Hričov – none (2.5 km from the water)Paština Závada 1 – Paština Závada – none (2.5 km from the water)Kotešová – occasional (2.9 km from the water)Bytča – pri križovatke – Veľká Bytča – none (3.0 km from the water)a1 (4.2 km from the water)a5 (5.4 km from the water)Kotešová – gravelly sands and sands (600 m from the water)Kotešová – Sihoť – Oblazov – gravelly sands and sands (2.6 km from the water)Veľká Bytča – gravelly sands and sands (4.3 km from the water)Veľká Bytča – gravelly sands and sands (4.3 km from the water)Štrkopiesky v koryte Váhu, úsek Zlatné – Žilina – gravelly sands (60 m from the water)Hričovské Podhradie – brown coal (1.8 km from the water)Ovčiarsko – building stone – conglomerate (4.0 km from the water)Horný Hričov – brick raw materials (5.0 km from the water)Hričovské Podhradie – general geology (2.0 km from the water)PSURNOVICE – Slope flows (820 m from the water)Hriźov.Podhradie – Landslides (940 m from the water)Doln‚ HLBOKE – Landslides (1.2 km from the water)KOTESOVA – Landslides (1.5 km from the water) (1.5 km from the water)HLBOKE – Landslides (1.7 km from the water)KOTESOVA – Landslides (1.7 km from the water)KOTESOVA – Slope flows (1.8 km from the water)KOTESOVA – Landslides (1.9 km from the water)KOTESOVA – Slope flows (1.9 km from the water)– Landslides (1.9 km from the water)HLBOKE – Landslides (2.0 km from the water)Kotešová – Landslides (2.0 km from the water)– Landslides (2.0 km from the water)KOTESOVA – Landslides (2.1 km from the water)– Landslides (2.1 km from the water)KOTESOVA – Slope flows (2.1 km from the water)HLBOKE – Landslides (2.2 km from the water)KOTESOVA – Landslides (2.2 km from the water)KOTESOVA – Landslides (2.2 km from the water)KOTESOVA – Landslides (2.2 km from the water)HLINIK NAD VAHOM – Landslides (2.3 km from the water)KOTESOVA – Landslides (2.3 km from the water)Doln‚ HLBOKE – Landslides (2.3 km from the water)DOLNY HRICOV – Landslides (2.3 km from the water)KOTESOVA – Landslides (2.3 km from the water)Hliník nad Váhom – Landslides (2.4 km from the water)KOTESOVA – Landslides (2.4 km from the water)– Landslides (2.4 km from the water)KOTESOVA – Landslides (2.5 km from the water)HLINIK NAD VAHOM – Landslides (2.5 km from the water)Oblazov – Landslides (2.5 km from the water)KOTESOVA – Landslides (2.5 km from the water)KOTESOVA – Landslides (2.6 km from the water)– Landslides (2.6 km from the water)– Landslides (2.6 km from the water)– Landslides (2.6 km from the water)HLINIK NAD VAHOM – Landslides (2.6 km from the water)Oblazov – Landslides (2.7 km from the water)PASTINA ZAVADA – Landslides (2.7 km from the water)HLINíK – Landslides (2.7 km from the water)DOLNY HRICOV – Landslides (2.7 km from the water)HLINIK NADVAHOM – Landslides (2.7 km from the water)KOTESOVA – Landslides (2.7 km from the water)KOTESOVA – Slope flows (2.8 km from the water)KOTESOVA – Landslides (2.8 km from the water)OBLAZOV – Landslides (2.8 km from the water)Oblazov – Landslides (2.9 km from the water)– Landslides (2.9 km from the water)– Landslides (2.9 km from the water)KOTESOVA – Landslides (2.9 km from the water)HLINIK NAD VAHOM – Landslides (2.9 km from the water)KOTESOVA – Landslides (2.9 km from the water)– Landslides (2.9 km from the water)HLBOKE – Landslides (3.0 km from the water)Kotešová – úzkoprofilový vrt s obyčajnou pitnou a ú (480 m from the water)Kotešová – SHMÚ observation borehole (890 m from the water)– úzkoprofilový vrt s obyčajnou pitnou a ú (1.1 km from the water)– úzkoprofilový vrt s obyčajnou pitnou a ú (1.3 km from the water)Bytča-Hlboké – negative borehole (1.4 km from the water)Dolné Hlboké – SHMÚ observation borehole (1.7 km from the water)Dolný Hričov – úzkoprofilový vrt s obyčajnou pitnou a ú (1.7 km from the water)Kotešová – úzkoprofilový vrt s obyčajnou pitnou a ú (1.7 km from the water)Dolný Hričov – úzkoprofilový vrt s obyčajnou pitnou a ú (1.7 km from the water)Hliník nad Váhom – SHMÚ observation borehole (1.8 km from the water)Bytča-Kotešová – negative borehole (1.8 km from the water)Bytča-Hlboké – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Hliník – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Bytča-Kotešová – negative borehole (1.9 km from the water)Bytča-Hlboké – negative borehole (2.0 km from the water)Dolný Hričov (2.0 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)Hliník nad Váhom – SHMÚ observation borehole (2.3 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.3 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.3 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.6 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.7 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.7 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.7 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.9 km from the water)Bytča-Makyta – širokoprofilový vrt (Ø vŕtania nad 600 m (2.9 km from the water)Bytča – úzkoprofilový vrt s obyčajnou pitnou a ú (2.9 km from the water)vodárensky využívaný prameň – Groundwater springs (2.1 km from the water)vodárensky využívaný prameň – Groundwater springs (2.2 km from the water)vodárensky využívaný prameň – Groundwater springs (2.3 km from the water)vodárensky využívaný prameň – Groundwater springs (2.3 km from the water)vodárensky využívaný prameň – Groundwater springs (2.4 km from the water)prameň – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (2.6 km from the water)vodárensky využívaný prameň – Groundwater springs (2.7 km from the water)vodárensky využívaný prameň – Groundwater springs (2.9 km from the water)Kotešová – borehole (740 m from the water)Hlboké n/Váhom, 300m od K548 – source (1.8 km from the water)Hrič.Podhradie, 600m Z od K530 – source (2.0 km from the water)Hlboké – prameň v obci – source (2.0 km from the water)Dolný Hričov – Materská škola – borehole (2.1 km from the water)Hlboké n/Váhom, 700m JJZ od K408 – drainage (2.1 km from the water)Dolný Hričov, 1300m S od K530 – borehole (2.2 km from the water)Hlboké – prameň na JZ okraji obce – source (2.3 km from the water)Hlboké n/Váhom, 850m SZ od K714 – source (2.5 km from the water)Dolný Hričov – Benzinol – borehole (2.7 km from the water)Paština-Závada – source (2.9 km from the water)dolina Hlboké – source (2.9 km from the water)2 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.

    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.

    Chemical water types nearby

    • Ca-Mg-HCO38×
    • Ca-HCO33×
    • Na-Mg-Ca-HCO31×

    Water quality class according to the hydrogeochemical map

    • class A9×
    • class G1×
    • class B1×
    • class F1×

    Metals in groundwater

    • MercuryHghigh (top 5 %)
      highest 0.400 μg/lmedian 0.100 μg/l11 samples91 % below the limit of quantification

      Highest value: vrt1992, 760 m from the water. Comparison: percentile 98 of all samples in Slovakia.

    • ZincZnhigh (top 5 %)
      highest 1,988 μg/lmedian 14.0 μg/l11 samples18 % below the limit of quantification

      Highest value: vrt1992, 760 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 0.900 μg/lmedian 0.250 μg/l11 samples91 % below the limit of quantification

      Highest value: vrt1992, 760 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ChromiumCrhigh (top 5 %)
      highest 4.10 μg/lmedian 0.250 μg/l11 samples82 % below the limit of quantification

      Highest value: prameň1992, 2.5 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 3.00 μg/lmedian 0.500 μg/l11 samples73 % below the limit of quantification

      Highest value: vrt1992, 2.6 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • AluminiumAlelevated (top 10 %)
      highest 0.0500 mg/lmedian 0.00500 mg/l11 samples91 % below the limit of quantification

      Highest value: vrt1992, 760 m from the water. Comparison: percentile 91 of all samples in Slovakia.

    • ArsenicAselevated (top 10 %)
      highest 2.30 μg/lmedian 0.500 μg/l11 samples91 % below the limit of quantification

      Highest value: drenáž1992, 2.1 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • AntimonySbelevated (top 10 %)
      highest 0.400 μg/lmedian 0.100 μg/l11 samples64 % below the limit of quantification

      Highest value: prameň1992, 1.8 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 23.0 μg/lmedian 7.00 μg/l11 samples

      Highest value: prameň1992, 2.1 km from the water. Comparison: percentile 81 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 2.40 μg/lmedian 0.800 μg/l11 samples

      Highest value: vrt1992, 1.6 km from the water. Comparison: percentile 79 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l6 samples100 % below the limit of quantification

      Highest value: prameň1992, 2.5 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l11 samples100 % below the limit of quantification

      Highest value: prameň1992, 2.5 km from the water. Comparison: percentile 39 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    source13,28 Bq/l3.28 Bq/l
    water source for individual supply121,5 Bq/l21.5 Bq/l
    well18,87 Bq/l8.87 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

    • other type of object1×

    Nearest old mine workings

    NameTypeMinedEndedFrom the water
    Kutacie práceother type of objectcoal19292.6 km

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    Kotešovágravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – VÁHOSTAV, a.s.600 m
    Kotešová – Sihoť – Oblazovgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – OBCHOD S PALIVAMI, s.r.o.2.6 km
    Veľká Bytčagravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – SDP, spol. s r.o.4.3 km
    Veľká Bytčagravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – Ján Korbáš VANDO4.3 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.

    96 boreholes in the 3 km zone, of which 36 hydrogeological and 60 other; with an archive report number 95.

    Borehole depths

    • up to 10 m43×
    • 10–30 m38×
    • 30–100 m0×
    • 100–300 m0×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    HV-10engineering-geological10.0 m100480350 m
    VN98-4environment–96444390 m
    VZ-3-1engineering-geological8.0 m86882400 m
    HV-9engineering-geological10.0 m100480420 m
    VN98-3environment–96444430 m
    Kotešovánarrow-diameter borehole with ordinary drinking and process water11.0 m53726 98Ac62.pdf480 m
    VN98-2environment–96444490 m
    VZ-3-2engineering-geological8.0 m86882550 m
    VS-01hydrogeological3.0 m102120590 m
    DPS-02engineering-geological6.8 m102120610 m
    DPS-01engineering-geological8.0 m102120630 m
    IG-01engineering-geological8.0 m102120630 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.

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 514.2 km
    category a5mineral water< 15> 5015.4 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.

    Environmental burdens

    SiteActivitySubstanceClassificationFrom the water
    Kotešová – landfill PO a KOSK1000500P990 m
    Hlboké nad Váh – landfill KO (pod brezami) VSK2001800F1.8 km
    Hlboké nad Váh – landfill KO IISK2001800F2.0 km
    Bytča – bývalý areál SADSK1000500P2.6 km

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom 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 Váh40 m²––2.0 km
    Dolný Hričov 1 – Dolný Hričov––monitored2.1 km
    Dolný Hríčov – Dolný Hričov–––2.3 km
    Hričovské Podhradie 1 – Hričovské Podhradie–––2.3 km
    Bytča – Hlboké nad Váh60 m²––2.5 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

    • Landslides49×
    • Slope flows5×

    Degree of activity

    • Potenciálny41×
    • Aktívny7×
    • Stabilizovaný6×

    Current state

    • Processed only in the scope of registration on a scale of 1:25,00032×
    • SD prebraná z archívnych materiálov (existuje inž. geologick11×
    • SD taken from archival materials, ktorá bola konfrontova1×

    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.
    • Panning concentrates. 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. Bytča1 fishing district · 0.3 km20VN Kadurka20

    More watercourses nearby

    Váh basin