Watercourse

Podkylavka – Prašník

Váh basinSalmonid (trout)
fishing district
1
fishing district length
5.4km
region
Trnava Region
Aerial image of watercourse Podkylavka - Prašník 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 Podkylavka – Prašník 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

Podkylavka – Prašník, window score 43.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 00:04.

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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    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.

    1502002503003500 km2 km4 km
    Elevation profile of the watercourse: from 322 to 200 m a.s.l. over 5.4 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
    322 m a.s.l.
    Lowest point
    188 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.
    134 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.
    25 ‰
    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.
    1.15

    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 Podkylavka - Prašník from 2017
    2017imaged 22 May 2017
    Aerial image of watercourse Podkylavka - Prašník from 2020
    2020imaged 22 Aug 2020
    Aerial image of watercourse Podkylavka - Prašník from 2023
    2023imaged 14 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 Podkylavka – Prašník 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

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

    • ammonium or nitrites above the standard at at least one station1

    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 Podkylavka – Prašník 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 (5 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

    Young sediments100% of the water line

    Young unconsolidated sediments; fine material easily washes into the stream during rain. Geological Map of Slovakia 1:50,000.

    510

    Water according to the atlas

    pH 8.2modelled estimate

    water type Ca–Mg–HCO₃

    Mineralisation 633 mg/l, very hard water (22.2 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    1 from 15elements in the top 10 %

    highest: Antimony 6.19 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 91. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km35 °C65 °C

    Heat underfoot

    35°C at 1,000 m depth

    At a depth of 2,000 m about 65 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    61nGy/h dose rate

    percentile 88 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

    0objects within 3 km

    No old mine working is recorded within 3 km of the water.

    Gold in river sediment

    0samples with gold

    6 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

    2 from 10indicators in the top 5 %

    highest: Selenium 2.67 μg/l

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

    Boreholes and groundwater analyses

    22boreholes within 3 km

    273 water analyses nearby

    Of these, 22 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    No geothermal borehole or spring is recorded within 10 km.

    Environmental burdens and landfills

    14sites within 3 km

    14 landfills

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

    Deposits and ore occurrences

    30records within 5 km

    8 deposits, 22 ore occurrences

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

    Landslides and slope deformations

    5areas within 3 km

    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.

    • Young sediments100%SR 8.6 %

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

    Young sediments: Young unconsolidated sediments; fine material easily washes into the stream during rain.

    Geological age of the rocks

    • Quaternary100%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryPleistocene – Holocenedeluvial sediments: predominantly loamy-stoney (subordinate sandy-stone) slopes and rubble1×

    Quaternary cover

    • deluvial sediments100%SR 16 %

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

    • Typical thickness of the Quaternary cover1.0m
    • 0 – 2100%SR 16 %

    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

    Neotectonic units

    • negative unit (intermountain basins)67%SR 14 %
    • positive unit (mountain range)33%SR 60 %

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

    Direction of neotectonic movements

    • very small subsidence67%SR 7.3 %
    • medium uplift33%SR 32 %

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

    Regional geological division

    • intramontane basins50%SR 44 %
    • Klippen Belt and the adjacent peri-Klippen zone50%SR 2.2 %

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

    Regional geological division (subunits)

    • Danube Basin50%SR 23 %
    • Myjava Hills50%SR 0.0 %

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

    Engineering-geological districts

    • region of flyschoid rocks100%SR 5.4 %

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

    Engineering-geological formations

    • flysch formation100%SR 13 %

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

    Susceptibility of the area to slope deformations

    • Region of stable areas67%SR 95 %
    • Region of potentially unstable areas33%SR 4.4 %

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

    The map covers 1 of 3 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.

    Main hydrogeological region

    • Neogene to the Cretaceous of the Myjava hills southwest of the Bradl zone100%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 8.18typical 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

    22.2°dH, very hard

    Sum of calcium and magnesium (3.96 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    633mg/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–Mg–HCO₃

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

    Major ions

    • BicarbonatesHCO3381 mg/lpercentile 90
    • CalciumCa105 mg/lpercentile 90
    • MagnesiumMg32.5 mg/lpercentile 87
    • SulphatesSO467.5 mg/lpercentile 74
    • ChloridesCl19.9 mg/lpercentile 69
    • SodiumNa7.76 mg/lpercentile 44
    • FluoridesF0.0799 mg/lpercentile 30
    • PotassiumK1.88 mg/lpercentile 29

    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

    • NitratesNO317.0 mg/lpercentile 89
    • PhosphatesPO40.0810 mg/lpercentile 39
    • AmmoniumNH40.0794 mg/lpercentile 39
    • Chemical oxygen demandChSK2.45 mg/lpercentile 31

    Metals

    • IronFe0.219 mg/lpercentile 77
    • AluminiumAl79.9 μg/lpercentile 55
    • ManganeseMn36.5 μg/lpercentile 54
    • ZincZn6.31 μg/lpercentile 47

    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

    • AntimonySb6.19 mg/kgpercentile 91
    • ChromiumCr106 mg/kgpercentile 84
    • NickelNi36.3 mg/kgpercentile 84
    • BismuthBi0.263 mg/kgpercentile 65
    • MolybdenumMo0.446 mg/kgpercentile 62
    • CobaltCo8.67 mg/kgpercentile 53
    • ArsenicAs6.65 mg/kgpercentile 50
    • SeleniumSe0.233 mg/kgpercentile 47
    • VanadiumV64.0 mg/kgpercentile 40
    • TinSn2.36 mg/kgpercentile 38
    • ZincZn83.5 mg/kgpercentile 35
    • MercuryHg0.0763 mg/kgpercentile 34
    • LeadPb12.0 mg/kgpercentile 27
    • CopperCu18.6 mg/kgpercentile 26
    • CadmiumCd0.0663 mg/kgpercentile 12

    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)
    • PotassiumK1.80 %percentile 85
    • CalciumCa3.18 %percentile 68
    • PhosphorusP883 mg/kgpercentile 55
    • MagnesiumMg0.891 %percentile 50
    • TitaniumTi4,334 mg/kgpercentile 45
    • AluminiumAl4.98 %percentile 26
    • IronFe2.24 %percentile 22
    • SodiumNa0.714 %percentile 20
    • ManganeseMn578 mg/kgpercentile 15
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • BoronB82.4 mg/kgpercentile 90
    • RubidiumRb93.5 mg/kgpercentile 63
    • GalliumGa15.3 mg/kgpercentile 61
    • CeriumCe59.2 mg/kgpercentile 50
    • ZirconiumZr376 mg/kgpercentile 40
    • LithiumLi27.5 mg/kgpercentile 38
    • StrontiumSr123 mg/kgpercentile 38
    • YttriumY22.7 mg/kgpercentile 24
    • BerylliumBe0.919 mg/kgpercentile 23
    • BariumBa363 mg/kgpercentile 22

    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

    61nGy/h in air

    range 60 to 63 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)K1.65 %percentile 90
    • Equivalent thorium (eTh)eTh9.29 ppm88th percentile
    • Equivalent uranium (eU)eU2.80 ppm73th 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 137CsCS1371,349 Bq/m²percentile 41

    Radon risk by isopleths

    • medium50%SR 64 %
    • low50%SR 36 %

    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

    +14nT

    range 11 to 15 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

    -6mGal

    residual +22.6 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 °C65 °C

    Rock temperature with depth

    35 / 65 °Cat depths of 1,000 and 2,000 m

    increase of 30 °C per km

    The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow –.

    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)195–543m a.s.l.
    • Average elevation of the units327m a.s.l.
    • Average slope7.3°
    • Average January temperature-3.5°C
    • Average July temperature18.5°C
    • Annual precipitation700mm

    Geomorphological units

    • Myjava Hills100%SR 0.0 %

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

    Geomorphological regions

    • Slovak-Moravian Carpathians100%SR 5.4 %

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

    Climatic-geographical types

    • mountain climate100%SR 33 %

    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 A67%SR 45 %
    • relatively clean soil33%SR 53 %

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

    Lithogeochemical types

    • Clayey-sandy sediments of the Cretaceous and Paleogene of the Klippen Belt, Tatricum and Hronicum100%SR 2.9 %

    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.

    Prašník – occasional (80 m from the water)Prašník – occasional (630 m from the water)Podkylava – Krížne cesty – Krajné – none (740 m from the water)Prašník – occasional (860 m from the water)Prašník – none (1.1 km from the water)Prašník – occasional (1.1 km from the water)Prašník – none (1.1 km from the water)Dobrovodský Mlyn – Prašník – none (1.2 km from the water)Krajné – Kahúnova dolina – Krajné – none (1.8 km from the water)Prašník – occasional (1.9 km from the water)Prašník – none (2.0 km from the water)Šípkové – none (2.6 km from the water)Šípkové – none (2.6 km from the water)Šípkové – none (2.9 km from the water)Prašník – building stone (3.7 km from the water)Vrbové – building stone (3.8 km from the water)Prašník – building stone (3.7 km from the water)Vrbové – building stone (3.8 km from the water)Košariská – dolomite (4.4 km from the water)Košariská – dolomite (4.4 km from the water)Košariská – dolomite (4.3 km from the water)Košariská – dolomite (4.3 km from the water)Prašník – stavebný piesok – sandstone (400 m from the water)Prehôrka – Krajné – building stone – sandstone (740 m from the water)Šípkové – stavebný piesok – sandstone (1.6 km from the water)Šípkové – stavebný piesok – sandstone (1.8 km from the water)U Marušíkov pri Prašníku – building stone – limestone (1.9 km from the water)Krajné – 2 – brick raw materials (2.1 km from the water)Mošnáci pri Prašníku – building stone – dolomite (2.1 km from the water)U Bajciarov pri Prašníku – building stone – dolomite (2.2 km from the water)Mošnáci pri Prašníku – building stone – dolomite (2.2 km from the water)Krajné – 3 – building stone – sandstone (2.2 km from the water)Vrbové – stavebný piesok – sandstone (2.4 km from the water)Krajné – Drieňovica 2 – building stone – crinoidal limestone (2.7 km from the water)Krajné – brown coal (2.8 km from the water)Krajné – Podrienie – building stone – calcareous sandstone (2.8 km from the water)Šterusy – building stone – dolomite (3.0 km from the water)Šterusy – building stone – dolomite (3.1 km from the water)Šterusy – building stone – dolomite (3.3 km from the water)Krajné – Luskovica – building stone – piesčitý dolomitický vá (3.9 km from the water)Prašník – U Fajnorov – building stone – limestone (4.1 km from the water)Krajné – Luskovica – building stone – calcareous conglomerate (4.5 km from the water)U Hrotkov pri Prašníku – building stone – dolomite (4.7 km from the water)Korytné – Obuchovci – building stone – calcareous sandstone (4.7 km from the water)Košariská – general geology (4.7 km from the water)– Landslides (130 m from the water)– Landslides (930 m from the water)– Landslides (1.1 km from the water)KRAJNE – Landslides (1.5 km from the water)KRAJNE – Landslides (1.6 km from the water)Prašník – monitoring borehole (170 m from the water)Prašník – monitoring borehole (250 m from the water)Podkulava – úzkoprofilový vrt s obyčajnou pitnou a ú (260 m from the water)Prašník – Pustá Ves – úzkoprofilový vrt s obyčajnou pitnou a ú (280 m from the water)Prašník – monitoring borehole (480 m from the water)Prašník – monitoring borehole (480 m from the water)Prašník – monitoring borehole (500 m from the water)Prašník – monitoring borehole (620 m from the water)Krajné-Podkylava – úzkoprofilový vrt s obyčajnou pitnou a ú (860 m from the water)Trenčín-Krajné – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Šípkové – širokoprofilový vrt (Ø vŕtania nad 600 m (2.0 km from the water)OZS Krajné – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Pustá Ves (Prašník) – monitoring borehole (2.9 km from the water)Pustá Ves (Prašník) – monitoring borehole (2.9 km from the water)Pustá Ves (Prašník) – monitoring borehole (3.0 km from the water)Vrbové – úzkoprofilový vrt s obyčajnou pitnou a ú (3.0 km from the water)Pustá Ves (Prašník) – monitoring borehole (3.0 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.

    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.

    • SeleniumSeextreme (top 1 %)
      highest 2.67 μg/lmedian 0.500 μg/l6 samples83 % below the limit of quantification

      Highest value: Holeška, potok2002, 660 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • CopperCuhigh (top 5 %)
      highest 8.60 μg/lmedian 6.50 μg/l6 samples17 % below the limit of quantification

      Highest value: potok – ľavostranný prítok Pokylavského p.1999, 340 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • StrontiumSrelevated (top 10 %)
      highest 597 μg/lmedian 594 μg/l2 samples

      Highest value: Prašník – Boorovci, potok 1800 m SZ od k-2472004, 60 m from the water. Comparison: percentile 94 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 23.0 μg/lmedian 5.00 μg/l6 samples67 % below the limit of quantification

      Highest value: potok – ľavostranný prítok Pokylavského p.1999, 340 m from the water. Comparison: percentile 86 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 3.40 μg/lmedian 1.00 μg/l6 samples83 % below the limit of quantification

      Highest value: Holeška, potok2002, 660 m from the water. Comparison: percentile 83 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 1.00 μg/lmedian 0.500 μg/l6 samples83 % below the limit of quantification

      Highest value: Podkylavský, potok1999, 30 m from the water. Comparison: percentile 82 of all samples in Slovakia.

    • CadmiumCdslightly elevated
      highest 0.250 μg/lmedian 0.150 μg/l6 samples83 % below the limit of quantification

      Highest value: Holeška, potok, 660 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • BariumBatypical value
      highest 60.0 μg/lmedian 54.5 μg/l4 samples

      Highest value: potok – ľavostranný prítok Pokylavského p.1999, 340 m from the water. Comparison: percentile 71 of all samples in Slovakia.

    • ArsenicAstypical value
      highest 1.53 μg/lmedian 0.855 μg/l6 samples33 % below the limit of quantification

      Highest value: Prašník – Boorovci, potok 1800 m SZ od k-2472004, 60 m from the water. Comparison: percentile 63 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l6 samples100 % below the limit of quantification

      Highest value: Holeška, potok1999, 360 m from the water. Comparison: percentile 43 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 19.1 mg/lmedian 11.5 mg/l6 samples

      Highest value: potok – ľavostranný prítok Pokylavského p.1999, 340 m from the water. Comparison: percentile 76 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)1 sample, at most 5 grains
    • Rutil (TiO₂)1 sample, at most 55 grains
    • Scheelit (CaWO₄)1 sample, at most 1 grains
    • Monazit ((Ce,La,Nd)PO₄)1 sample, at most 5 grains
    • Pyrite (FeS₂)1 sample, at most 55 grains
    • Anatas (TiO₂)1 sample, at most 5 grains

    Rock-forming and accessory minerals

    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))3 samples, at most 55 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))3 samples, at most 55 grains
    • Tourmalines (complex borosilicate)3 samples, at most 55 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)2 samples, at most 55 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))2 samples, at most 55 grains
    • Kyanit (Al₂SiO₅)1 sample, at most 5 grains
    • Sillimanit (Al₂SiO₅)1 sample, at most 5 grains
    • Zirconium (ZrSiO₄)1 sample, at most 55 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 70.0 μg/lmedian 0.750 μg/l22 samples

      Highest value: studňa1993, 2.8 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • ZincZnhigh (top 5 %)
      highest 2,210 μg/lmedian 115 μg/l22 samples

      Highest value: studňa1992, 1.1 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • LithiumLihigh (top 5 %)
      highest 69.0 μg/lmedian 15.5 μg/l22 samples

      Highest value: studňa1993, 2.7 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • SeleniumSehigh (top 5 %)
      highest 2.90 μg/lmedian 0.500 μg/l22 samples77 % below the limit of quantification

      Highest value: studňa1992, 1.1 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 0.600 μg/lmedian 0.250 μg/l22 samples86 % below the limit of quantification

      Highest value: prameň1992, 720 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LeadPbelevated (top 10 %)
      highest 2.00 μg/lmedian 0.500 μg/l22 samples64 % below the limit of quantification

      Highest value: studňa1993, 1.6 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 1.90 μg/lmedian 0.250 μg/l22 samples55 % below the limit of quantification

      Highest value: studňa1993, 2.4 km from the water. Comparison: percentile 89 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.300 μg/lmedian 0.100 μg/l22 samples91 % below the limit of quantification

      Highest value: prameň1992, 720 m from the water. Comparison: percentile 87 of all samples in Slovakia.

    • AluminiumAlslightly elevated
      highest 0.0300 mg/lmedian 0.00500 mg/l22 samples59 % below the limit of quantification

      Highest value: studňa1993, 2.0 km from the water. Comparison: percentile 85 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l8 samples100 % below the limit of quantification

      Highest value: studňa1993, 3.0 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l22 samples100 % below the limit of quantification

      Highest value: vrt1993, 2.7 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l22 samples100 % below the limit of quantification

      Highest value: vrt1993, 2.7 km from the water. Comparison: percentile 38 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    well725,2 Bq/l11.7 Bq/l
    source330,5 Bq/l28.1 Bq/l
    developed spring244,2 Bq/l28.0 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.

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    Prašníkbuilding stoneDeposit with halted mining or where use of reserves is not expected – LOMtrans, s.r.o.3.7 km
    Prašníkbuilding stoneDeposit with halted mining or where use of reserves is not expected – LOMtrans, s.r.o.3.7 km
    Vrbovébuilding stoneDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená3.8 km
    Vrbovébuilding stoneDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená3.8 km
    KošariskádolomiteDeposit with expected use of reserves – Organizácia neurčená4.3 km
    KošariskádolomiteDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.3 km
    KošariskádolomiteDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.4 km
    KošariskádolomiteDeposit with expected use of reserves – Organizácia neurčená4.4 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.

    22 boreholes in the 3 km zone, of which 17 hydrogeological and 5 other; with an archive report number 22.

    Borehole depths

    • up to 10 m18×
    • 10–30 m2×
    • 30–100 m2×
    • 100–300 m0×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Prašníkmonitoring borehole8.0 m74931 132Ab30.pdf170 m
    Prašníkmonitoring borehole7.5 m74931 132Ab31.pdf250 m
    Podkulavanarrow-diameter borehole with ordinary drinking and process water22.0 m82456 120Cd13.pdf260 m
    Prašník – Pustá Vesnarrow-diameter borehole with ordinary drinking and process water9.0 m55362 132Ab20.pdf280 m
    Prašníkmonitoring borehole7.5 m74931 132Ab34.pdf480 m
    Prašníkmonitoring borehole7.5 m74931 132Ab33.pdf480 m
    Prašníkmonitoring borehole7.5 m74931 132Ab32.pdf500 m
    Prašníkmonitoring borehole8.0 m74931 132Ab35.pdf620 m
    Krajné-Podkylavanarrow-diameter borehole with ordinary drinking and process water9.2 m74054 120Cd10.pdf860 m
    V-1engineering-geological9.0 m844851.2 km
    Trenčín-Krajnénarrow-diameter borehole with ordinary drinking and process water8.0 m64740 120Cd8.pdf1.2 km
    KV-2engineering-geological5.0 m868191.9 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
    Prašník1 000 m²1980–80 m
    Prašník5 000 m²1970–630 m
    Podkylava – Krížne cesty – Krajné5 685 m²1972monitored740 m
    Prašník1 500 m²1970–860 m
    Prašník1 500 m²1980–1.1 km
    Prašník12 000 m²1992–1.1 km
    Prašník250 m²1990–1.1 km
    Dobrovodský Mlyn – Prašník2 000 m²1970–1.2 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

    • Landslides5×

    Degree of activity

    • Potenciálny5×

    Current state

    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S3×
    • SD taken from archival materials, ktorá bola konfrontova2×

    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. Vrbové1 fishing district · 5.4 km33Podkylavka – Prašník33

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