Watercourse

VN Zbojné

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
0.5km
region
Prešov Region
Aerial image of watercourse VN Zbojné 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 Zbojné watercourse

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

Average of the watercourse's fishing districts

Average activity · average of one fishing district

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

Best window today

06:00–08:00

VN Zbojné, window score 51.

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: 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.

    2942952962972982993000.0 km0.1 km0.2 km0.3 km0.4 km
    Terrain elevation profile (Reservoir): from 299 to 295 m a.s.l. over 0.5 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    297 m a.s.l.
    Lowest point of the profile
    295 m a.s.l.
    Highest point of the profile
    298 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 2019 to 2025: 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 Zbojné from 2019
    2019imaged 23 Aug 2019
    Aerial image of watercourse VN Zbojné from 2022
    2022imaged 4 Aug 2022
    Aerial image of watercourse VN Zbojné from 2025
    2025imaged 13 Aug 2025

    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.

    Geology and geochemistry of the VN Zbojné 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 (1 km of line in total): stream samples within 1 km, boreholes, mine workings and burdens within 3 km, ore occurrences within 5 km, geothermal sources within 10 km.

    Rock under the water

    River alluvium100% of the water line

    Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000.

    510

    Water according to the atlas

    pH 8.3modelled estimate

    water type Ca–HCO₃

    Mineralisation 344 mg/l, moderately hard water (12.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    0 from 15elements in the top 10 %

    highest: Nickel 34.2 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 80. Interpolation of the Geochemical Atlas of river sediments.

    0 °C80

    Heat underfoot

    45°C at 1,000 m depth

    heat flow 75 mW/m²

    Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    53nGy/h dose rate

    percentile 66 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

    8 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

    0 from 8indicators in the top 5 %

    highest: Barium 64.0 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 75 (Výrava).

    Boreholes and groundwater analyses

    73boreholes within 3 km

    116 water analyses nearby

    Of these, 71 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    6 geothermal and mineral water springs within 10 km.

    Environmental burdens and landfills

    3sites within 3 km

    3 landfills

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

    Deposits and ore occurrences

    3records within 5 km

    3 ore occurrences

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

    Landslides and slope deformations

    27areas 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.

    • River alluvium100%SR 72 %

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

    River alluvium: Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium.

    Geological age of the rocks

    • Quaternary100%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains1×

    Quaternary cover

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

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

    Tectonic units

    • ŠUPINOVÁ ZÓNA MIKOVÁ – SNINA100%SR 1.4 %

    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)

    • Dukla–Bukovec flysch100%SR 1.8 %

    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)

    • Sandstones100%SR 15 %

    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)100%SR 15 %

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

    Main hydrogeological region

    • Paleogene and Quaternary of the Laborca Povodia to Brekov and the Mesozoic of the Humen Mountains100%SR 3.0 %

    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 8.33typical 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

    12.0°dH, moderately hard

    Sum of calcium and magnesium (2.15 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    344mg/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

    • CalciumCa67.7 mg/lpercentile 56
    • SodiumNa9.14 mg/lpercentile 50
    • BicarbonatesHCO3210 mg/lpercentile 49
    • FluoridesF0.108 mg/lpercentile 47
    • PotassiumK2.54 mg/lpercentile 42
    • MagnesiumMg11.1 mg/lpercentile 36
    • SulphatesSO430.6 mg/lpercentile 35
    • ChloridesCl4.31 mg/lpercentile 30

    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

    • AmmoniumNH40.0620 mg/lpercentile 31
    • PhosphatesPO40.0167 mg/lpercentile 5
    • NitratesNO31.72 mg/lpercentile 5
    • Chemical oxygen demandChSK0.506 mg/lpercentile 1

    Metals

    • IronFe0.0971 mg/lpercentile 48
    • ZincZn3.54 μg/lpercentile 25
    • AluminiumAl25.8 μg/lpercentile 25
    • ManganeseMn7.75 μg/lpercentile 15

    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

    • NickelNi34.2 mg/kgpercentile 80
    • SeleniumSe0.402 mg/kgpercentile 78
    • MolybdenumMo0.538 mg/kgpercentile 74
    • CopperCu26.9 mg/kgpercentile 63
    • ChromiumCr77.6 mg/kgpercentile 59
    • VanadiumV71.1 mg/kgpercentile 56
    • AntimonySb0.609 mg/kgpercentile 47
    • CadmiumCd0.170 mg/kgpercentile 46
    • CobaltCo8.00 mg/kgpercentile 43
    • ArsenicAs5.77 mg/kgpercentile 38
    • ZincZn85.8 mg/kgpercentile 38
    • LeadPb12.9 mg/kgpercentile 32
    • MercuryHg0.0627 mg/kgpercentile 23
    • TinSn1.96 mg/kgpercentile 19
    • BismuthBi0.0666 mg/kgpercentile 2

    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)
    • PotassiumK1.66 %percentile 72
    • AluminiumAl5.68 %percentile 52
    • TitaniumTi4,468 mg/kgpercentile 50
    • IronFe2.67 %percentile 49
    • SodiumNa0.793 %percentile 34
    • CalciumCa1.32 %percentile 25
    • ManganeseMn636 mg/kgpercentile 23
    • MagnesiumMg0.663 %percentile 21
    • PhosphorusP484 mg/kgpercentile 7
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • LithiumLi36.7 mg/kgpercentile 81
    • GalliumGa17.7 mg/kgpercentile 80
    • BerylliumBe1.89 mg/kgpercentile 78
    • BoronB69.8 mg/kgpercentile 75
    • RubidiumRb98.8 mg/kgpercentile 74
    • ZirconiumZr430 mg/kgpercentile 59
    • YttriumY28.6 mg/kgpercentile 55
    • CeriumCe57.6 mg/kgpercentile 45
    • StrontiumSr120 mg/kgpercentile 36
    • BariumBa380 mg/kgpercentile 28

    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

    53nGy/h in air

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

    • Potassium (K)K1.40 %percentile 72
    • Equivalent thorium (eTh)eTh8.10 ppm70th percentile
    • Equivalent uranium (eU)eU2.50 ppm40th 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 137CsCS1371,365 Bq/m²percentile 42

    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

    -41nT

    range -41 to -41 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

    -17mGal

    residual +7.5 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.

    • Rock temperature at 1,000 m depth45°C
    • Surface heat flow density75mW/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)166–902m a.s.l.
    • Average elevation of the units440m a.s.l.
    • Average slope12.8°
    • Average January temperature-3.5°C
    • Average July temperature18.5°C
    • Annual precipitation700mm

    Geomorphological units

    • Laborec Highlands100%SR 1.7 %

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

    Geomorphological regions

    • Nízke Beskydy100%SR 7.5 %

    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 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.

    Svetlice – occasional (1.5 km from the water)Svetlice – none (2.4 km from the water)Zbojné – occasional (2.4 km from the water)a1 (6.2 km from the water)a1 (7.5 km from the water)a1 (7.9 km from the water)a1 (8.2 km from the water)a1 (8.9 km from the water)a1 (9.8 km from the water)Výrava – brick raw materials (4.3 km from the water)Svetlice – building stone – sandstone (4.5 km from the water)Valentovce – coal, asphalt (4.9 km from the water)– Landslides (260 m from the water)– Landslides (260 m from the water)– Landslides (670 m from the water)– Landslides (840 m from the water)– Landslides (920 m from the water)– Landslides (1.0 km from the water)– Landslides (1.0 km from the water)– Landslides (1.1 km from the water)SVETLICE – Landslides (1.2 km from the water)VYSNA ZBUJNA – Landslides (1.5 km from the water)– Landslides (1.5 km from the water)NIZNE ZBOJNE – Landslides (1.6 km from the water)ZBOJNE – Landslides (1.6 km from the water)SVETLICE – Landslides (1.7 km from the water)SVETLICE – Landslides (1.7 km from the water)– Landslides (1.7 km from the water)ZBOJNE – Landslides (2.0 km from the water)SVETLICE – Landslides (2.2 km from the water)– Landslides (2.2 km from the water)VYPRAVA – Landslides (2.2 km from the water)ZBOJNE – Landslides (2.2 km from the water)– Landslides (2.5 km from the water)VYRAVA – Landslides (2.7 km from the water)– Landslides (2.7 km from the water)ZBOJNE – Landslides (2.8 km from the water)SVETLICE – Landslides (2.9 km from the water)ZBOJNE – Landslides (3.0 km from the water)Zbojné – úzkoprofilový vrt s obyčajnou pitnou a ú (940 m from the water)Zbojné – úzkoprofilový vrt s obyčajnou pitnou a ú (1.3 km from the water)5 km

    The line is the water of the fishing district, the light band is the 3 km zone in which boreholes, mine workings and burdens were searched for. The map shows the nearest objects (at most a few dozen from each register), not all of them. The points correspond to the position in the register; area objects are marked by their centre.

    Trace elements in surface waters

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

    • BariumBaslightly elevated
      highest 64.0 μg/lmedian 64.0 μg/l1 sample

      Highest value: Výrava2009, 80 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification

      Highest value: Výrava2009, 80 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l1 sample100 % below the limit of quantification

      Highest value: Výrava2009, 80 m from the water. Comparison: percentile 43 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: Výrava2009, 80 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • ChromiumCrbelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification

      Highest value: Výrava2009, 80 m from the water. Comparison: percentile 32 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l1 sample100 % below the limit of quantification

      Highest value: Výrava, 80 m from the water. Comparison: percentile 26 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification

      Highest value: Výrava2009, 80 m from the water. Comparison: percentile 22 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification

      Highest value: Výrava2009, 80 m from the water. Comparison: percentile 22 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 6.73 mg/lmedian 6.73 mg/l1 sample

      Highest value: Výrava2009, 80 m from the water. Comparison: percentile 24 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)9 samples, at most 815 grains
    • Rutil (TiO₂)6 samples, at most 815 grains
    • Anatas (TiO₂)5 samples, at most 5 grains
    • Limonite (FeO(OH)·nH₂O)5 samples, at most 815 grains
    • Pyrite (FeS₂)2 samples, at most 5 grains
    • Magnetite (Fe₃O₄)2 samples, at most 55 grains
    • Ilmenit (FeTiO₃)2 samples, at most 315 grains
    • Monazit ((Ce,La,Nd)PO₄)2 samples, at most 5 grains

    Rock-forming and accessory minerals

    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)7 samples, at most 55 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)5 samples, at most 4115 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)5 samples, at most 315 grains
    • Tourmalines (complex borosilicate)5 samples, at most 315 grains
    • Zirconium (ZrSiO₄)5 samples, at most 815 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

    • ChromiumCrextreme (top 1 %)
      highest 120 μg/lmedian 0.250 μg/l9 samples56 % below the limit of quantification

      Highest value: prameň1993, 1.6 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AluminiumAlextreme (top 1 %)
      highest 0.720 mg/lmedian 0.0100 mg/l9 samples33 % below the limit of quantification

      Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • CopperCuhigh (top 5 %)
      highest 8.20 μg/lmedian 0.900 μg/l9 samples

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • LithiumLielevated (top 10 %)
      highest 37.0 μg/lmedian 21.0 μg/l9 samples

      Highest value: prameň1993, 630 m from the water. Comparison: percentile 91 of all samples in Slovakia.

    • ZincZnslightly elevated
      highest 187 μg/lmedian 17.0 μg/l9 samples

      Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 78 of all samples in Slovakia.

    • LeadPbslightly elevated
      highest 1.00 μg/lmedian 0.500 μg/l9 samples89 % below the limit of quantification

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 75 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l3 samples100 % below the limit of quantification

      Highest value: prameň1993, 630 m from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l9 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l9 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    • AntimonySbbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l9 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 40 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l9 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 39 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l9 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 38 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    developed spring12,14 Bq/l2.14 Bq/l
    source213,6 Bq/l11.8 Bq/l

    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.

    73 boreholes in the 3 km zone, of which 2 hydrogeological and 71 other; with an archive report number 71.

    Borehole depths

    • up to 10 m60×
    • 10–30 m11×
    • 30–100 m1×
    • 100–300 m1×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    JV-4engineering-geological13.0 m7256540 m
    V-28engineering-geological5.8 m2078950 m
    JV-5engineering-geological8.0 m7256560 m
    JV-1engineering-geological10.6 m7256580 m
    JV-3engineering-geological8.0 m7256580 m
    V-6engineering-geological10.0 m7024780 m
    JV-2engineering-geological8.2 m7256590 m
    V-9engineering-geological10.0 m70247100 m
    V-8engineering-geological5.5 m70247150 m
    JV-4engineering-geological9.0 m71420150 m
    JV-2engineering-geological7.8 m71420160 m
    JV-3engineering-geological7.6 m71420170 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< 566.2 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
    Svetlice200 m²1984–1.5 km
    Svetlice2 000 m²1991–2.4 km
    Zbojné240 m²1984–2.4 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

    • Landslides27×

    Degree of activity

    • Potenciálny27×

    Current state

    • SD taken from archival materials, ktorá bola konfrontova22×
    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S5×

    How to read these data

    • Zone and distance. The distance is measured from the line of the water to the point in the register (to the centre for areas), with an accuracy of tens of metres. Counts apply only to the zone, not to the whole catchment.
    • Percentile. For chemistry, the highest value is compared with all atlas samples in Slovakia. It is not a legal limit or a health risk assessment; the atlases are historical (published: surface waters 2015, groundwater 1996, river sediments 1999).
    • Limit of quantification. Many samples have a value at the lowest level the laboratory can determine; such results mean "below the limit". For these, the position in the distribution is an estimate.
    • 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. Humenné1 fishing district · 0.5 km44VN Zbojné44

    More watercourses nearby

    Bodrog basin and Hornád