Watercourse

VN Nová Bystrica

Váh basinSalmonid (trout)
fishing districts
2
fishing district length
16.0km
region
Žilina Region
Aerial image of watercourse VN Nová Bystrica 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 Nová Bystrica 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 2 fishing districts

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.
  • Very high0
  • High0
  • Average0
  • Low2

Best window today

15:00–17:00

VN Nová Bystrica – prítoky, window score 37.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 01:04.

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: 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.

    5006007008009001,0000 km2 km4 km6 kmVN Nová Bystrica – prítoky
    Terrain elevation profile (Reservoir): from 938 to 593 m a.s.l. over 6.5 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    642 m a.s.l.
    Lowest point of the profile
    593 m a.s.l.
    Highest point of the profile
    938 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 Nová Bystrica from 2018
    2018imaged 21 May 2018
    Aerial image of watercourse VN Nová Bystrica from 2021
    2021imaged 10 Sep 2021
    Aerial image of watercourse VN Nová Bystrica 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 Nová Bystrica 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 2 fishing districts with measurements have 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 Nová Bystrica 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 (16 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 alluvium40% of the water line

    40% flysch, 20% other rocks

    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 8.1modelled estimate

    water type Ca–HCO₃

    Mineralisation 245 mg/l, soft water (8.0 °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: Cobalt 10.8 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 79. 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

    39nGy/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

    0objects within 3 km

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

    Gold in river sediment

    0samples with gold

    11 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

    3 from 9indicators in the top 5 %

    highest: Lead 9.00 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 98 (Bystrica, potok).

    Boreholes and groundwater analyses

    10boreholes within 3 km

    458 water analyses nearby

    Of these, 10 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

    1sites within 3 km

    1 landfill

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

    Deposits and ore occurrences

    8records within 5 km

    8 ore occurrences

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

    Landslides and slope deformations

    213areas within 3 km

    12 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 alluvium40%SR 72 %
    • Flysch40%SR 4.7 %
    • Other rocks20%SR 4.1 %

    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

    • Quaternary40%
    • flysch40%
    • water20%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains2×
    flyschEoceneZlín Formation2×

    Quaternary cover

    • Typical thickness of the Quaternary cover2.7m
    • 2 – 567%SR 48 %
    • 0 – 233%SR 16 %

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

    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

    Neotectonic units

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

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

    Direction of neotectonic movements

    • medium uplift100%SR 32 %

    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 flyschoid rocks60%SR 5.4 %
    • water body20%SR 4.8 %
    • region of mountain-stream deposits20%SR 21 %

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

    Engineering-geological formations

    • flysch formation75%SR 13 %
    • formation of Quaternary sediments25%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 areas80%SR 95 %
    • Region of potentially unstable areas20%SR 4.4 %

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

    The map covers 5 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)

    • Sandstones86%SR 15 %
    • Gravel14%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 (Sandstones)86%SR 15 %
    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Gravel)14%SR 22 %

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

    Main hydrogeological region

    • Paleogene and Quaternary of the Kysuce Basin86%SR 2.7 %
    • Paleogene of the White Orava and Neogene of the Orava Basin14%SR 1.9 %

    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 8.11typical 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

    8.0°dH, soft

    Sum of calcium and magnesium (1.43 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    245mg/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

    • BicarbonatesHCO3161 mg/lpercentile 34
    • SodiumNa5.99 mg/lpercentile 34
    • CalciumCa46.7 mg/lpercentile 33
    • MagnesiumMg6.57 mg/lpercentile 18
    • FluoridesF0.0583 mg/lpercentile 15
    • SulphatesSO419.6 mg/lpercentile 15
    • PotassiumK1.11 mg/lpercentile 12
    • ChloridesCl2.27 mg/lpercentile 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)

    Nutrients and organic pollution

    • AmmoniumNH40.113 mg/lpercentile 51
    • Chemical oxygen demandChSK2.37 mg/lpercentile 29
    • PhosphatesPO40.0264 mg/lpercentile 15
    • NitratesNO31.33 mg/lpercentile 3

    Metals

    • ZincZn12.3 μg/lpercentile 72
    • AluminiumAl29.4 μg/lpercentile 28
    • IronFe0.0519 mg/lpercentile 23
    • ManganeseMn7.08 μg/lpercentile 13

    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

    • CobaltCo10.8 mg/kgpercentile 79
    • BismuthBi0.325 mg/kgpercentile 77
    • ChromiumCr93.8 mg/kgpercentile 77
    • NickelNi32.6 mg/kgpercentile 77
    • CopperCu28.1 mg/kgpercentile 66
    • VanadiumV69.7 mg/kgpercentile 54
    • SeleniumSe0.222 mg/kgpercentile 44
    • MolybdenumMo0.333 mg/kgpercentile 41
    • TinSn2.43 mg/kgpercentile 40
    • LeadPb14.0 mg/kgpercentile 40
    • ZincZn87.1 mg/kgpercentile 39
    • MercuryHg0.0585 mg/kgpercentile 20
    • ArsenicAs4.49 mg/kgpercentile 18
    • CadmiumCd0.0738 mg/kgpercentile 16
    • AntimonySb0.191 mg/kgpercentile 3

    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)
    • SodiumNa0.997 %percentile 71
    • IronFe2.59 %percentile 44
    • AluminiumAl5.45 %percentile 44
    • CalciumCa1.75 %percentile 41
    • TitaniumTi4,010 mg/kgpercentile 32
    • ManganeseMn690 mg/kgpercentile 31
    • MagnesiumMg0.724 %percentile 29
    • PotassiumK1.37 %percentile 28
    • PhosphorusP446 mg/kgpercentile 5
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • GalliumGa19.5 mg/kgpercentile 89
    • BoronB71.0 mg/kgpercentile 77
    • LithiumLi32.8 mg/kgpercentile 67
    • BerylliumBe1.25 mg/kgpercentile 41
    • StrontiumSr126 mg/kgpercentile 41
    • ZirconiumZr369 mg/kgpercentile 38
    • RubidiumRb83.5 mg/kgpercentile 36
    • BariumBa371 mg/kgpercentile 24
    • YttriumY21.5 mg/kgpercentile 20
    • CeriumCe49.4 mg/kgpercentile 17

    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

    39nGy/h in air

    range 39 to 42 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.

    • Equivalent thorium (eTh)eTh6.28 ppm15th percentile
    • Potassium (K)K1.01 %percentile 6
    • Equivalent uranium (eU)eU1.79 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 137CsCS1372,491 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

    +72nT

    range 64 to 84 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

    -62mGal

    residual −14.4 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.

    • Elevation of geomorphological units (from–to)355–1 325m a.s.l.
    • Average elevation of the units708m a.s.l.
    • Average slope14.7°
    • Average January temperature-5.5°C
    • Average July temperature15.3°C
    • Annual precipitation917mm

    Geomorphological units

    • Kysuce Highlands86%SR 0.0 %
    • Oravská Magura14%SR 0.0 %

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

    Geomorphological regions

    • Stredné Beskydy100%SR 3.0 %

    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

    Susceptibility of soils to acidification

    • soils moderately susceptible to acidification60%SR 25 %
    • soils susceptible to acidification40%SR 31 %

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

    Soil contamination (map 1:500,000)

    • relatively clean soil86%SR 53 %
    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A14%SR 45 %

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

    Lithogeochemical types

    • Cretaceous and Paleogene of the Outer Carpathians100%SR 9.5 %

    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.

    Zázrivá – Manganese ores (4.7 km from the water)pri ihrisku – Nová Bystrica – none (1.3 km from the water)Nová Bystrica – building stone – sandstone (30 m from the water)Riečnica – building stone – conglomerate, sandstone (40 m from the water)Riečnica – building stone – sandstone (70 m from the water)Nová Bystrica – building stone – sandstone (190 m from the water)Nová Bystrica – ceramic clays (450 m from the water)Nová Bystrica – Rajnohovia – building stone – sandstone (4.2 km from the water)Zázrivá – manganese ores (4.7 km from the water)Kozinská – general geology (4.6 km from the water)BUKOVA – Landslides (60 m from the water)Podhradie – Landslides (80 m from the water)– Landslides (100 m from the water)RIECNICA – Slope flows (110 m from the water)– Landslides (110 m from the water)– Landslides (110 m from the water)– Landslides (130 m from the water)– Landslides (130 m from the water)RIECNICA-BUCHOV – Landslides (130 m from the water)RIECNICA – Landslides (140 m from the water)– Landslides (150 m from the water)– Landslides (150 m from the water)– Landslides (150 m from the water)– Landslides (160 m from the water)HARVELKA – Landslides (160 m from the water)RIECNICA – Landslides (160 m from the water)RIECNICA-VANGOR. – Landslides (170 m from the water)– Landslides (170 m from the water)HARVELKA – Landslides (170 m from the water)RIECNICA – Slope flows (190 m from the water)– Landslides (200 m from the water)RIECNICA-CHOVANAD – Landslides (200 m from the water)– Landslides (200 m from the water)RIECNICA – Landslides (210 m from the water)RIECNICA – Landslides (210 m from the water)HARVELKA – Landslides (220 m from the water)Nolčovo – Landslides (220 m from the water)– Landslides (240 m from the water)BUKOVA – Landslides (240 m from the water)– Landslides (240 m from the water)– Landslides (240 m from the water)– Landslides (250 m from the water)RIECNICA-BUCHOV – Landslides (260 m from the water)– Landslides (260 m from the water)LAZY – Landslides (260 m from the water)RIECNICA – Landslides (280 m from the water)– Landslides (290 m from the water)RIECNICA – Landslides (290 m from the water)– Landslides (310 m from the water)– Landslides (310 m from the water)– Landslides (370 m from the water)RIECNICA – Landslides (390 m from the water)RIECNICA – Landslides (400 m from the water)– Landslides (420 m from the water)HARVELKA – Landslides (440 m from the water)RIECNICA – Landslides (440 m from the water)– Landslides (450 m from the water)RIECNICA-LESKOVO – Slope flows (460 m from the water)– Landslides (470 m from the water)– Landslides (490 m from the water)RIECNICA – Landslides (530 m from the water)– Landslides (540 m from the water)HARVELKA – Landslides (540 m from the water)– Landslides (570 m from the water)NOVA BYSTRICA – Landslides (570 m from the water)RIECNICA – Landslides (580 m from the water)RIECNICA – Landslides (580 m from the water)RIECNICA – Landslides (580 m from the water)– Landslides (590 m from the water)– Landslides (600 m from the water)HARVELKA – Landslides (600 m from the water)RIECNICA – Landslides (600 m from the water)– Landslides (630 m from the water)NOVA BYSTRICA – Landslides (640 m from the water)– Landslides (650 m from the water)– Landslides (660 m from the water)– Landslides (660 m from the water)NOVA BYSTRICA – Landslides (680 m from the water)RIECNICA – Landslides (740 m from the water)– Landslides (770 m from the water)– Landslides (780 m from the water)– Landslides (790 m from the water)– Landslides (790 m from the water)HARVELKA – Landslides (800 m from the water)RIECNICA – Landslides (810 m from the water)RIECNICA – Landslides (820 m from the water)– Landslides (830 m from the water)HARVELKA – Landslides (860 m from the water)– Landslides (860 m from the water)RIECNICA – Landslides (870 m from the water)Nová Bystrica – úzkoprofilový vrt s obyčajnou pitnou a ú (120 m from the water)Nová Bystrica – úzkoprofilový vrt s obyčajnou pitnou a ú (960 m from the water)Nová Bystrica – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Nová Bystrica – širokoprofilový vrt (Ø vŕtania nad 600 m (2.8 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.

    • LeadPbhigh (top 5 %)
      highest 9.00 μg/lmedian 4.00 μg/l9 samples22 % below the limit of quantification

      Highest value: Bystrica, potok1997, 130 m from the water. Comparison: percentile 98 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 8.20 μg/lmedian 0.500 μg/l8 samples88 % below the limit of quantification

      Highest value: vtok do nádrže od obce Harvelky1997, 60 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 0.800 μg/lmedian 0.250 μg/l9 samples11 % below the limit of quantification

      Highest value: Harvelka, potok, 50 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • CopperCuelevated (top 10 %)
      highest 7.20 μg/lmedian 1.40 μg/l9 samples22 % below the limit of quantification

      Highest value: Harvelka, potok1997, 50 m from the water. Comparison: percentile 94 of all samples in Slovakia.

    • SeleniumSeelevated (top 10 %)
      highest 0.800 μg/lmedian 0.500 μg/l9 samples78 % below the limit of quantification

      Highest value: prítok do Harvelky1997, 350 m from the water. Comparison: percentile 94 of all samples in Slovakia.

    • ChromiumCrelevated (top 10 %)
      highest 5.50 μg/lmedian 3.60 μg/l9 samples11 % below the limit of quantification

      Highest value: Bystrica, potok1997, 130 m from the water. Comparison: percentile 93 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 2.60 μg/lmedian 1.70 μg/l9 samples11 % below the limit of quantification

      Highest value: Bystrica, potok1997, 130 m from the water. Comparison: percentile 80 of all samples in Slovakia.

    • BariumBatypical value
      highest 43.0 μg/lmedian 43.0 μg/l1 sample

      Highest value: Biela Orava2009, 910 m from the water. Comparison: percentile 53 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l1 sample100 % below the limit of quantification

      Highest value: Biela Orava2009, 910 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    Major ions, mineralisation and pH

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

    • Silicon dioxideSiO2below half of Slovakia
      highest 4.07 mg/lmedian 4.07 mg/l1 sample

      Highest value: Biela Orava2009, 910 m from the water. Comparison: percentile 9 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)25 samples, at most 1815 grains
    • Pyrite (FeS₂)25 samples, at most 555 grains
    • Rutil (TiO₂)25 samples, at most 1115 grains
    • Limonite (FeO(OH)·nH₂O)24 samples, at most 815 grains
    • Magnetite (Fe₃O₄)24 samples, at most 815 grains
    • Anatas (TiO₂)22 samples, at most 315 grains
    • Ilmenit (FeTiO₃)19 samples, at most 315 grains
    • Monazit ((Ce,La,Nd)PO₄)17 samples, at most 55 grains
    • Hematite (Fe₂O₃)4 samples, at most 5 grains
    • Scheelit (CaWO₄)2 samples, at most 5 grains
    • Kasiterit (SnO₂)1 sample, at most 1 grains

    Rock-forming and accessory minerals

    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)25 samples, at most 4115 grains
    • Tourmalines (complex borosilicate)25 samples, at most 315 grains
    • Zirconium (ZrSiO₄)25 samples, at most 1815 grains
    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)22 samples, at most 315 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)16 samples, at most 55 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))6 samples, at most 5 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))5 samples, at most 5 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))4 samples, at most 5 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)3 samples, at most 5 grains
    • Korund (Al₂O₃)2 samples, 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

    • LithiumLihigh (top 5 %)
      highest 89.0 μg/lmedian 6.00 μg/l35 samples

      Highest value: vrt1992, 200 m from the water. Comparison: percentile 97 of all samples in Slovakia.

    • CopperCuhigh (top 5 %)
      highest 9.10 μg/lmedian 0.800 μg/l35 samples

      Highest value: prameň1992, 380 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 4.00 μg/lmedian 0.500 μg/l35 samples66 % below the limit of quantification

      Highest value: studňa1992, 2.0 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • AntimonySbelevated (top 10 %)
      highest 0.600 μg/lmedian 0.100 μg/l35 samples80 % below the limit of quantification

      Highest value: prameň1992, 420 m from the water. Comparison: percentile 93 of all samples in Slovakia.

    • ZincZnelevated (top 10 %)
      highest 720 μg/lmedian 0.500 μg/l35 samples74 % below the limit of quantification

      Highest value: studňa1992, 2.0 km from the water. Comparison: percentile 92 of all samples in Slovakia.

    • SeleniumSeslightly elevated
      highest 1.00 μg/lmedian 0.500 μg/l35 samples91 % below the limit of quantification

      Highest value: vrt1992, 2.8 km from the water. Comparison: percentile 83 of all samples in Slovakia.

    • AluminiumAlslightly elevated
      highest 0.0200 mg/lmedian 0.00500 mg/l35 samples97 % below the limit of quantification

      Highest value: studňa1992, 1.3 km from the water. Comparison: percentile 80 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l27 samples100 % below the limit of quantification

      Highest value: prameň1992, 2.9 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l35 samples100 % below the limit of quantification

      Highest value: prameň1992, 2.9 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l35 samples100 % below the limit of quantification

      Highest value: prameň1992, 2.9 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l35 samples100 % below the limit of quantification

      Highest value: prameň1992, 2.9 km from the water. Comparison: percentile 38 of all samples in Slovakia.

    • ChromiumCrbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l35 samples100 % below the limit of quantification

      Highest value: prameň1992, 2.9 km from the water. Comparison: percentile 29 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    source55,38 Bq/l1.94 Bq/l
    developed spring46,06 Bq/l4.90 Bq/l
    stream, river10,940 Bq/l0.940 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.

    Ore occurrences in the metallogenic map

    OccurrenceOre typeMetalsTypeFrom the water
    ZázriváManganese oresMnmineralogical occurrence4.7 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.

    10 boreholes in the 3 km zone, of which 4 hydrogeological and 6 other; with an archive report number 10.

    Borehole depths

    • up to 10 m6×
    • 10–30 m3×
    • 30–100 m1×
    • 100–300 m0×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Nová Bystricanarrow-diameter borehole with ordinary drinking and process water30.0 m74915 87Cc5.pdf120 m
    N-11engineering-geological6.0 m83779620 m
    Nová Bystricanarrow-diameter borehole with ordinary drinking and process water7.5 m38276 87Cc3.pdf960 m
    N-10engineering-geological6.0 m837791.5 km
    N-9engineering-geological10.0 m837791.8 km
    Nová Bystricanarrow-diameter borehole with ordinary drinking and process water9.0 m12273 87Cc1.pdf1.9 km
    N-4engineering-geological8.0 m837792.0 km
    N-8engineering-geological8.0 m837792.1 km
    N-5engineering-geological18.0 m837792.2 km
    Nová Bystricawide-diameter borehole10.0 m34662 87Cc2.pdf2.8 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
    pri ihrisku – Nová Bystrica300 m²1991–1.3 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

    • Landslides208×
    • Slope flows4×
    • Block fields1×

    Degree of activity

    • Potenciálny136×
    • Stabilizovaný65×
    • Aktívny10×
    • With potential and active forms2×

    Current state

    • SD taken from archival materials, ktorá bola konfrontova42×
    • Processed only in the scope of registration on a scale of 1:25,00036×
    • SD prebraná z archívnych materiálov (existuje inž. geologick15×

    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. OZ Piešťany2 fishing districts · 16 km30VN Nová Bystrica – prítoky30

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