Watercourse

Šibská voda

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
14.3km
region
Prešov Region
Aerial image of watercourse Šibská voda 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 Šibská voda watercourse

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

Average of the watercourse's fishing districts

Low activity · average of one fishing district

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

Best window today

06:00–08:00

Šibská voda, window score 40.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 07:04.

Map and fishing districts of the watercourse

The course of the watercourse and its fishing districts. You can switch the line color to today's conditions, quality or any other parameter.

Detailed filtersregion, district, riverbed, depth, shading, satellites, water chemistry and pollution, fish, geology

1445fishing districts
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    Water state on the watercourse

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

    Water levels on the watercourse

    StationStatusChangeTemperature
    Kľušovská Zábava55 cm–
    Source: SHMÚUpdated 9 Nov 2026 06:57

    Elevation profile of the watercourse

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

    Bystrina A mountain stream with a steep gradient, cascades and a rocky bottom. The water is clear and cold; fishing requires a careful approach.

    2004006008001,0000 km5 km10 km
    Elevation profile of the watercourse: from 783 to 269 m a.s.l. over 14.3 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
    783 m a.s.l.
    Lowest point
    235 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.
    548 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.
    38 ‰
    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.
    1.13

    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 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 Šibská voda from 2019
    2019imaged 24 Aug 2019
    Aerial image of watercourse Šibská voda from 2022
    2022imaged 5 Aug 2022
    Aerial image of watercourse Šibská voda from 2025
    2025imaged 12 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.

    Water pollution on the Šibská voda watercourse

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

    Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025

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

    • 3 or more indicators1

    Most polluted fishing districtsall with an unmet standard

    • Šibská vodaŠibská voda · standard not met in 1 of 4 years4 indicators

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

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

    Source: SHMÚ (yearbooks on surface and groundwater quality), the register of wastewater treatment plants from VÚVH and the EEA. A SHMÚ site is assigned to a fishing district by the same watercourse name and by distance; the yearbook lists the sites that failed the standard, so a missing site is not proof of clean water.

    Geology and geochemistry of the Šibská voda 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 (14 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 alluvium50% of the water line

    25% sandstones and conglomerates, 25% flysch

    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 406 mg/l, moderately hard water (12.9 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    0 from 15elements in the top 10 %

    highest: Chromium 91.4 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 75. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km45 °C75 °C

    Heat underfoot

    45°C at 1,000 m depth

    heat flow 75 mW/m²

    At a depth of 2,000 m about 75 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    45nGy/h dose rate

    percentile 15 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

    12samples with gold

    17 ore minerals in the sediment

    Up to 2 grains in one sample (80 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.

    Trace elements in the stream water

    0 from 8indicators in the top 5 %

    highest: Barium 62.0 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 73 (bez mena).

    Boreholes and groundwater analyses

    2,618boreholes within 3 km

    492 water analyses nearby

    Of these, 2618 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    13 geothermal and mineral water springs within 10 km.

    Environmental burdens and landfills

    26sites within 3 km

    4 environmental burdens, 22 landfills

    Nearest burden: Bardejov – areál SNAHA v.d., 490 m from the water. Proximity does not mean that substances leak from the site into the water.

    Deposits and ore occurrences

    14records within 5 km

    14 ore occurrences

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

    Landslides and slope deformations

    33areas within 3 km

    11 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 alluvium50%SR 72 %
    • Sandstones and conglomerates25%SR 1.8 %
    • Flysch25%SR 4.7 %

    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

    • Quaternary50%
    • flysch50%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains2×
    flyschEocene – OligoceneMalcov Formation1×
    flyschEoceneStrihovce and older Malcov Formations1×

    Quaternary cover

    • fluvial sediments of floodplains67%SR 68 %
    • deluvial sediments33%SR 16 %

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

    • 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

    Neotectonic units

    • positive unit (mountain range)50%SR 60 %
    • negative unit (intermountain basins)50%SR 14 %

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

    Direction of neotectonic movements

    • medium uplift50%SR 32 %
    • very small subsidence50%SR 7.3 %

    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)

    • Čergov–Beskydy flysch100%SR 1.7 %

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

    Engineering-geological districts

    • region of sandstone-conglomerate rocks67%SR 3.4 %
    • region of flyschoid rocks33%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 areas100%SR 95 %

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

    The map covers 4 of 6 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)

    • Gravel67%SR 52 %
    • Sandstones33%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 (Gravel)67%SR 22 %
    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Sandstones)33%SR 15 %

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

    Type of permeability (basic hydrogeological map 1:50,000)

    • fissure100%SR 12 %

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

    Hydrogeological function

    • aquifer100%SR 95 %

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

    Main hydrogeological region

    • Paleogene of Čergov67%SR 1.4 %
    • Paleogene of the Low Beskydy Mountains in the Tople Basin33%SR 1.5 %

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

    Genetic type of groundwater

    • carbonate-silicatogenic groundwater100%SR 3.5 %

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

    Chemical type of groundwater

    • Ca-Mg-HCO3 typ100%SR 5.5 %

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

    Groundwater quality class

    • A100%SR 36 %

    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

    12.9°dH, moderately hard

    Sum of calcium and magnesium (2.31 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    406mg/l mineralisation

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

    Ionic composition of the water

    Water type by dominant ions: Ca–HCO₃

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

    Major ions

    • CalciumCa69.3 mg/lpercentile 58
    • SodiumNa10.1 mg/lpercentile 54
    • BicarbonatesHCO3225 mg/lpercentile 54
    • PotassiumK3.12 mg/lpercentile 52
    • ChloridesCl9.58 mg/lpercentile 52
    • MagnesiumMg14.1 mg/lpercentile 46
    • SulphatesSO436.2 mg/lpercentile 44
    • FluoridesF0.0781 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

    • NitratesNO330.0 mg/lpercentile 95
    • PhosphatesPO40.0939 mg/lpercentile 42
    • AmmoniumNH40.0516 mg/lpercentile 26
    • Chemical oxygen demandChSK2.08 mg/lpercentile 22

    Metals

    • ManganeseMn21.8 μg/lpercentile 41
    • IronFe0.0578 mg/lpercentile 27
    • ZincZn1.13 μg/lpercentile 3
    • AluminiumAl10.3 μg/lpercentile 1

    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

    • ChromiumCr91.4 mg/kgpercentile 75
    • CadmiumCd0.269 mg/kgpercentile 67
    • NickelNi22.0 mg/kgpercentile 37
    • BismuthBi0.181 mg/kgpercentile 35
    • TinSn2.08 mg/kgpercentile 25
    • SeleniumSe0.145 mg/kgpercentile 22
    • LeadPb10.6 mg/kgpercentile 17
    • CopperCu16.4 mg/kgpercentile 16
    • MolybdenumMo0.185 mg/kgpercentile 13
    • ZincZn64.0 mg/kgpercentile 12
    • VanadiumV51.1 mg/kgpercentile 11
    • AntimonySb0.292 mg/kgpercentile 10
    • CobaltCo5.06 mg/kgpercentile 8
    • MercuryHg0.0384 mg/kgpercentile 6
    • ArsenicAs2.99 mg/kgpercentile 4

    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)
    • SodiumNa1.16 %percentile 84
    • TitaniumTi4,663 mg/kgpercentile 57
    • PotassiumK1.51 %percentile 49
    • AluminiumAl5.08 %percentile 30
    • CalciumCa1.18 %percentile 20
    • ManganeseMn536 mg/kgpercentile 10
    • MagnesiumMg0.575 %percentile 10
    • IronFe1.97 %percentile 9
    • PhosphorusP496 mg/kgpercentile 8
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • ZirconiumZr465 mg/kgpercentile 70
    • BerylliumBe1.51 mg/kgpercentile 56
    • BoronB58.7 mg/kgpercentile 44
    • YttriumY26.1 mg/kgpercentile 41
    • RubidiumRb80.8 mg/kgpercentile 30
    • BariumBa367 mg/kgpercentile 23
    • CeriumCe50.6 mg/kgpercentile 20
    • LithiumLi23.9 mg/kgpercentile 18
    • GalliumGa8.00 mg/kgpercentile 10
    • StrontiumSr90.4 mg/kgpercentile 6

    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

    45nGy/h in air

    range 42 to 49 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

    low

    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)K1.26 %percentile 33
    • Equivalent thorium (eTh)eTh6.36 ppm16th percentile
    • Equivalent uranium (eU)eU2.17 ppm13th 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 137CsCS1371,069 Bq/m²percentile 22

    Radon risk by isopleths

    • low75%SR 36 %
    • medium25%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

    -39nT

    range -48 to -35 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

    -29mGal

    residual +7.2 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 km45 °C75 °C

    Rock temperature with depth

    45 / 75 °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 75 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)130–749m a.s.l.
    • Average elevation of the units336m a.s.l.
    • Average slope7.9°
    • Average January temperature-4.3°C
    • Average July temperature17.0°C
    • Annual precipitation783mm

    Geomorphological units

    • Ondava Highlands100%SR 4.4 %

    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 climate67%SR 33 %
    • basin climate33%SR 29 %

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

    Susceptibility of soils to acidification

    • soils moderately susceptible to acidification100%SR 25 %

    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

    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.

    Kľušov – Mercury ores (2.3 km from the water)Bardejov – Arsenic ores (3.7 km from the water)Bardejov – areál SNAHA v.d. – SK1001300P (490 m from the water)Bardejov – areál podniku JAS – SK1001300P (940 m from the water)Bardejov – areál Bardejovských strojární (ZŤS) – SK1001300P (1.8 km from the water)Bardejov – elektrická stanica (ES) – SK1001300P (2.2 km from the water)Bardejov – cannot be estimated (60 m from the water)Bardejovská Zábava – Bardejov – none (60 m from the water)Bardejovská Zábava – Bardejov – none (60 m from the water)Bardejovská Zábava – Bardejov – none (70 m from the water)Šiba – cannot be estimated (80 m from the water)Bardejov – cannot be estimated (120 m from the water)Bardejov – none (150 m from the water)Bardejov – none (160 m from the water)Kľušovská Zábava – Kľušov – none (630 m from the water)Kľušov – none (780 m from the water)Miháľov – Bardejov – none (1.6 km from the water)Kľušov – cannot be estimated (1.9 km from the water)Bardejov – none (1.9 km from the water)Bardejovská Nová Ves – none (2.2 km from the water)Hervartov – none (2.3 km from the water)Bardejov – none (2.3 km from the water)Hertník – none (2.5 km from the water)Richvald – none (2.6 km from the water)Bardejovská Nová Ves – none (2.6 km from the water)Bardejovské Kúpele – Bardejov – cannot be estimated (2.8 km from the water)Bardejovská Dlhá Lúka – Dlhá Lúka – cannot be estimated (2.8 km from the water)Bardejovská Nová Ves – none (3.0 km from the water)a1 (820 m from the water)a1 (1.5 km from the water)b1 (2.4 km from the water)a1 (2.5 km from the water)a1 (2.7 km from the water)a1 (2.9 km from the water)a1 (5.3 km from the water)a1 (7.2 km from the water)a1 (7.7 km from the water)a1 (7.9 km from the water)a1 (8.1 km from the water)a1 (9.2 km from the water)a1 (9.9 km from the water)Kľušov – Kľušovská Zábava – brick raw materials (190 m from the water)povodie rieky Topľa (Bardejov – Hrabovec) – Au – placers (490 m from the water)povodie rieky Topľa (Bardejov – Hrabovec) – Au – placers (1.4 km from the water)povodie rieky Topľa (Bardejov – Hrabovec) – Au – placers (2.2 km from the water)Kľušov – Hg ores (2.3 km from the water)Lukavica – brick raw materials (2.3 km from the water)povodie rieky Topľa (Bardejov – Hrabovec) – Au – placers (2.5 km from the water)Bardejovská Nová Ves – brick raw materials (2.6 km from the water)Kríže – building stone – sandstone (2.8 km from the water)povodie rieky Topľa (Bardejov – Hrabovec) – Au – placers (3.5 km from the water)povodie rieky Topľa (Bardejov – Hrabovec) – Au – placers (3.8 km from the water)Lukavica – brick raw materials (5.0 km from the water)Bardejovské Kúpele – hydrogeology (3.2 km from the water)Bardejovská Zábava, č.domu 55,56 – Landslides (30 m from the water)Bardejovská Zábava, č.domu 55,56 – Landslides (40 m from the water)Bardejovská zábava – Landslides (50 m from the water)Bardejovská zábava – Landslides (50 m from the water)Bardejovská Zábava, Mičkova ul. č.domu 12 – Landslides (60 m from the water)BARDEJOV – Landslides (60 m from the water)Bardejovská Zábava, č.domu 55,56 – Landslides (80 m from the water)Kľušovská Zábava, č. domu 228,227,225 – Landslides (90 m from the water)Bardejovská zábava – Landslides (100 m from the water)Kľušovská Zábava, č. domu 228,227,225 – Landslides (120 m from the water)Bardejovská Zábava, č.domu 31,34 – Landslides (120 m from the water)Kľušovská Zábava, č. domu 228,227,225 – Landslides (170 m from the water)– Landslides (220 m from the water)Kľušovská Zábava, č. domu 260 – Landslides (300 m from the water)Kľušovská Zábava, č. domu 260 – Landslides (300 m from the water)Kľušovská Zábava, č. domu 260 – Landslides (320 m from the water)Kľušovská Zábava, č. domu 260 – Landslides (340 m from the water)BARDEJOV – Landslides (380 m from the water)Kľušovská Zábava, č. domu 260 – Landslides (400 m from the water)Kľušovská Zábava, č. domu 260 – Landslides (450 m from the water)– Landslides (450 m from the water)Kľušovská Zábava, č. domu 260 – Landslides (470 m from the water)BARDEJOV – Landslides (580 m from the water)KLUSOVSKA ZABAVA – Landslides (620 m from the water)BARDEJOV – Landslides (810 m from the water)– Landslides (850 m from the water)– Landslides (880 m from the water)– Landslides (910 m from the water)– Landslides (1.1 km from the water)– Landslides (2.2 km from the water)– Landslides (2.3 km from the water)BARDEJOVSKA NOVA VES – Landslides (2.5 km from the water)– Landslides (2.6 km from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (10 m from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (30 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (30 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (40 m from the water)Kľušov – širokoprofilový vrt (Ø vŕtania nad 600 m (40 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (40 m from the water)Šiba – štruktúrny vrt s obyčajnou vodou (nad 20 (50 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (50 m from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (50 m from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (60 m from the water)Kľušov – širokoprofilový vrt (Ø vŕtania nad 600 m (60 m from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (80 m from the water)Kľušov – širokoprofilový vrt (Ø vŕtania nad 600 m (80 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (100 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (100 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (100 m from the water)– monitoring borehole (170 m from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (230 m from the water)Bardejov – SHMÚ observation borehole (260 m from the water)– monitoring borehole (300 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (330 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (370 m from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (430 m from the water)Bardejov – monitoring borehole (480 m from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (490 m from the water)Bardejov – monitoring borehole (510 m from the water)Bardejov – monitoring borehole (550 m from the water)Bardejov – monitoring borehole (570 m from the water)Bardejov – negative borehole (580 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (600 m from the water)Bardejov – monitoring borehole (650 m from the water)Bardejov – úzkoprofilový vrt s obyčajnou pitnou a ú (660 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (670 m from the water)Bardejov – širokoprofilový vrt (Ø vŕtania nad 600 m (670 m from the water)Bardejov – monitoring borehole (680 m from the water)Bardejov – monitoring borehole (750 m from the water)Bardejov – monitoring borehole (850 m from the water)Bardejov – monitoring borehole (860 m from the water)Bardejov – monitoring borehole (890 m from the water)Bardejov – monitoring borehole (920 m from the water)prameň – Groundwater springs (30 m from the water)prameň – Groundwater springs (50 m from the water)vodárensky využívaný vrt – Hydrogeological boreholes (50 m from the water)prameň – Groundwater springs (50 m from the water)prameň – Groundwater springs (50 m from the water)prameň – Groundwater springs (50 m from the water)prameň – Groundwater springs (60 m from the water)prameň – Groundwater springs (60 m from the water)prameň – Groundwater springs (70 m from the water)prameň – Groundwater springs (70 m from the water)prameň – Groundwater springs (70 m from the water)prameň – Groundwater springs (90 m from the water)prameň – Groundwater springs (90 m from the water)prameň – Groundwater springs (110 m from the water)prameň – Groundwater springs (110 m from the water)prameň – Groundwater springs (120 m from the water)prameň – Groundwater springs (130 m from the water)prameň – Groundwater springs (140 m from the water)prameň – Groundwater springs (140 m from the water)prameň – Groundwater springs (170 m from the water)prameň – Groundwater springs (200 m from the water)prameň – Groundwater springs (240 m from the water)prameň – Groundwater springs (320 m from the water)prameň – Groundwater springs (370 m from the water)prameň – Groundwater springs (670 m from the water)prameň – Groundwater springs (700 m from the water)prameň – Groundwater springs (770 m from the water)prameň – Groundwater springs (790 m from the water)prameň – Groundwater springs (890 m from the water)prameň – Groundwater springs (900 m from the water)prameň – Groundwater springs (900 m from the water)prameň – Groundwater springs (940 m from the water)prameň – Groundwater springs (1.0 km from the water)prameň – Groundwater springs (1.1 km from the water)prameň – Groundwater springs (1.1 km from the water)prameň – Groundwater springs (1.1 km from the water)prameň – Groundwater springs (1.1 km from the water)prameň – Groundwater springs (1.2 km from the water)prameň – Groundwater springs (1.2 km from the water)prameň – Groundwater springs (1.3 km from the water)Siba, 1500 m Z – source (180 m from the water)SIBA, dolina Lipského potoka, 1200m SV od K841 – source (210 m from the water)SIBA, dolina Lipského potoka, 400m S od K841 – source (370 m from the water)Kríže, 500m Z od K1019 – source (890 m from the water)Kríže, 3200 m JJV – source (960 m from the water)Siba – borehole (1.2 km from the water)Kríže, 700m JJV od K662 – source (1.2 km from the water)Hertník, dolina potoka Sekčov – source (1.4 km from the water)Hertník – borehole (1.7 km from the water)Hertnik, 4900 m JZ – source (1.7 km from the water)Hertník, 1300m J od K1019 – source (1.8 km from the water)Hertník, dolina potoka Veska, 2300m nad obcou – source (1.9 km from the water)Hervartov, 300m nad obcou – source (1.9 km from the water)Hertnik, 3 km JJZ – source (2.0 km from the water)Kríže, dolina Chotárneho potoka, 700m VJV odK879 – source (2.2 km from the water)Hertník, 1500m S od K593 – source (2.3 km from the water)Hervete, 800m V od K814 – source (2.5 km from the water)Kríže, dolina Chotárnerho potoka – source (2.6 km from the water)Kríže, 1900m ZSZ od K912 – source (2.8 km from the water)zlato 2 ks – gold (20 m from the water)zlato 2 ks – gold (40 m from the water)zlato 1 ks – gold (50 m from the water)zlato 1 ks – gold (60 m from the water)zlato 1 ks – gold (70 m from the water)zlato 1 ks – gold (70 m from the water)zlato 2 ks – gold (80 m from the water)zlato 1 ks – gold (80 m from the water)zlato 1 ks – gold (120 m from the water)zlato 1 ks – gold (170 m from the water)zlato 1 ks – gold (220 m from the water)zlato 1 ks – gold (760 m 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.

    • BariumBatypical value
      highest 62.0 μg/lmedian 56.0 μg/l3 samples

      Highest value: bez mena2008, 60 m from the water. Comparison: percentile 73 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l3 samples100 % below the limit of quantification

      Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l3 samples100 % below the limit of quantification

      Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l3 samples100 % below the limit of quantification

      Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • ChromiumCrbelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l3 samples100 % below the limit of quantification

      Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 32 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l3 samples100 % below the limit of quantification

      Highest value: Šibská voda, 100 m from the water. Comparison: percentile 26 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l3 samples100 % below the limit of quantification

      Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 22 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l3 samples100 % below the limit of quantification

      Highest value: Šibská voda2008, 100 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 9.97 mg/lmedian 9.72 mg/l3 samples

      Highest value: Richvaldský potok2008, 790 m from the water. Comparison: percentile 46 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.

    • Ilmenit (FeTiO₃)64 samples, at most 815 grains
    • Magnetite (Fe₃O₄)63 samples, at most 4115 grains
    • Rutil (TiO₂)57 samples, at most 815 grains
    • Monazit ((Ce,La,Nd)PO₄)51 samples, at most 55 grains
    • Hematite (Fe₂O₃)39 samples, at most 815 grains
    • Pyrite (FeS₂)33 samples, at most 55 grains
    • Sphalerite (ZnS)25 samples, at most 50 grains
    • Limonite (FeO(OH)·nH₂O)19 samples, at most 315 grains
    • Anatas (TiO₂)12 samples, at most 55 grains
    • Gold (Au)12 samples, at most 2 grains
    • Barite (BaSO₄)8 samples, at most 55 grains
    • Markazit (FeS₂)3 samples, at most 5 grains
    • Cinabarit (HgS)2 samples, at most 5 grains
    • Realgár (AsS)1 sample, at most 1 grains
    • Auripigment (As₂S₃)1 sample, at most 1 grains
    • Malachit (Cu₂CO₃(OH)₂)1 sample, at most 5 grains
    • Scheelit (CaWO₄)1 sample, at most 5 grains

    Nearest samples with gold

    SampleGold in sampleFrom the water
    20042 grains20 m
    20132 grains40 m
    19991 grain50 m
    18171 grain60 m
    20011 grain70 m
    18231 grain70 m
    20002 grains80 m
    18251 grain80 m

    Rock-forming and accessory minerals

    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)65 samples, at most 4115 grains
    • Zirconium (ZrSiO₄)64 samples, at most 315 grains
    • Tourmalines (complex borosilicate)52 samples, at most 55 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)47 samples, at most 815 grains
    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)13 samples, at most 815 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))7 samples, at most 5 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))6 samples, at most 315 grains
    • Korund (Al₂O₃)2 samples, at most 5 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)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.

    Chemical water types nearby

    • Ca-Mg-HCO310×
    • Ca-HCO38×
    • Na-HCO31×

    Water quality class according to the hydrogeochemical map

    • class A13×
    • class C2×
    • class E1×
    • class F1×
    • class B1×
    • class D1×

    Metals in groundwater

    • ZincZnextreme (top 1 %)
      highest 6,275 μg/lmedian 14.0 μg/l38 samples5 % below the limit of quantification

      Highest value: studňa1993, 1.9 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • ChromiumCrhigh (top 5 %)
      highest 9.20 μg/lmedian 0.250 μg/l38 samples79 % below the limit of quantification

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • CopperCuhigh (top 5 %)
      highest 9.60 μg/lmedian 0.250 μg/l38 samples

      Highest value: studňa1993, 2.0 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • ArsenicAshigh (top 5 %)
      highest 6.30 μg/lmedian 0.500 μg/l38 samples97 % below the limit of quantification

      Highest value: studňa1993, 1.5 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • SeleniumSeelevated (top 10 %)
      highest 1.80 μg/lmedian 0.500 μg/l38 samples66 % below the limit of quantification

      Highest value: prameň1993, 760 m from the water. Comparison: percentile 91 of all samples in Slovakia.

    • AluminiumAlelevated (top 10 %)
      highest 0.0400 mg/lmedian 0.0100 mg/l38 samples47 % below the limit of quantification

      Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • LithiumLielevated (top 10 %)
      highest 33.0 μg/lmedian 9.50 μg/l38 samples5 % below the limit of quantification

      Highest value: studňa1993, 1.5 km from the water. Comparison: percentile 90 of all samples in Slovakia.

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

      Highest value: prameň1993, 2.2 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.200 μg/lmedian 0.100 μg/l38 samples97 % below the limit of quantification

      Highest value: studňa1993, 40 m from the water. Comparison: percentile 83 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l25 samples100 % below the limit of quantification

      Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l38 samples100 % below the limit of quantification

      Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l38 samples100 % below the limit of quantification

      Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    stream, river10,500 Bq/l0.500 Bq/l
    developed spring218,8 Bq/l10.8 Bq/l
    source612,5 Bq/l9.17 Bq/l
    water source for public supply13,82 Bq/l3.82 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
    KľušovMercury oresHgmineralogical occurrence?2.3 km
    BardejovArsenic oresAsmineralogical occurrence3.7 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.

    2,618 boreholes in the 3 km zone, of which 126 hydrogeological and 2492 other; with an archive report number 2618.

    Borehole depths

    • up to 10 m2146×
    • 10–30 m397×
    • 30–100 m3×
    • 100–300 m6×
    • over 300 m1×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Bardejovnarrow-diameter borehole with ordinary drinking and process water7.3 m25039 103Ba62.pdf10 m
    S-2engineering-geological7.0 m2489410 m
    V-5engineering-geological6.0 m1744320 m
    S-5engineering-geological5.0 m2489420 m
    V-1engineering-geological8.8 m6151320 m
    Bardejovnarrow-diameter borehole with ordinary drinking and process water5.8 m21066 103Ba21.pdf30 m
    Bardejovwide-diameter borehole8.0 m64502 103Ba95.pdf30 m
    S-4engineering-geological3.0 m2489430 m
    S-1engineering-geological2.4 m196330 m
    JV-5engineering-geological3.2 m7200930 m
    JV-4engineering-geological7.0 m7202230 m
    JV-3engineering-geological9.0 m7202230 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< 512820 m
    category b1mineral water15-22< 512.4 km

    Environmental burdens, landfills and anthropogenic sediments

    Recorded environmental burdens (industrial sites, landfills, mining), the register of waste landfills and monitoring of anthropogenic sediments (industrial sludge). It is a list of places, not a measurement of water pollution.

    Environmental burdens

    SiteActivitySubstanceClassificationFrom the water
    Bardejov – areál SNAHA v.d.SK1001300P490 m
    Bardejov – areál podniku JASSK1001300P940 m
    Bardejov – areál Bardejovských strojární (ZŤS)SK1001300P1.8 km
    Bardejov – elektrická stanica (ES)SK1001300P2.2 km

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom the water
    Bardejov200 m²1980–60 m
    Bardejovská Zábava – Bardejov80 m²1980–60 m
    Bardejovská Zábava – Bardejov60 m²1985–60 m
    Bardejovská Zábava – Bardejov–1985–70 m
    Šiba–1980–80 m
    Bardejov500 m²1980–120 m
    Bardejov300 m²1975–150 m
    Bardejov100 m²1980–160 m

    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

    • Landslides33×

    Degree of activity

    • Potenciálny20×
    • Aktívny11×
    • Stabilizovaný2×

    Current state

    • SD prebraná z archívnych materiálov (existuje inž. geologick18×
    • SD taken from archival materials, ktorá bola konfrontova9×
    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S6×

    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. Bardejov1 fishing district · 14 km34Šibská voda34

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