Watercourse

Jakuboviansky potok

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
15.8km
region
Prešov Region
Aerial image of watercourse Jakuboviansky potok 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 Jakuboviansky potok 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

Jakuboviansky potok, window score 52.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 08:04.

Map and fishing districts of the watercourse

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

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

1445fishing districts
Pick a category to narrow the selection. Next to each option you can see how many fishing districts remain.
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    Elevation profile of the watercourse

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

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

    2003004005006007008000 km2 km4 km6 km8 km
    Elevation profile of the watercourse: from 684 to 310 m a.s.l. over 8.3 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
    684 m a.s.l.
    Lowest point
    286 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.
    398 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.
    48 ‰
    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.
    1.18

    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 Jakuboviansky potok from 2019
    2019imaged 26 Aug 2019
    Aerial image of watercourse Jakuboviansky potok from 2022
    2022imaged 4 Aug 2022
    Aerial image of watercourse Jakuboviansky potok from 2025
    2025imaged 7 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 Jakuboviansky potok 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.

    • 1 to 2 indicators1

    Most polluted fishing districtsall with an unmet standard

    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 Jakuboviansky potok 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 (15 km of line in total): stream samples within 1 km, boreholes, mine workings and burdens within 3 km, ore occurrences within 5 km, geothermal sources within 10 km.

    Rock under the water

    Young sediments67% of the water line

    33% river alluvium

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

    510

    Water according to the atlas

    pH 8.2modelled estimate

    water type Ca–Mg–HCO₃

    Mineralisation 458 mg/l, hard water (16.3 °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 97.8 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.

    1 km2 km35 °C72 °C

    Heat underfoot

    35°C at 1,000 m depth

    heat flow 71 mW/m²

    At a depth of 2,000 m about 72 °C (increase of 37 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    51nGy/h dose rate

    percentile 57 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

    2samples with gold

    14 ore minerals in the sediment

    Up to 3 grains in one sample (90 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.

    Trace elements in the stream water

    0 from 7indicators in the top 5 %

    highest: Cadmium 0.300 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 90 (Orkucany).

    Boreholes and groundwater analyses

    187boreholes within 3 km

    533 water analyses nearby

    Of these, 187 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    90°C at the wellhead

    2 geothermal boreholes within 10 km

    Warmest: Lipany – L-1, yield 10.0 l/s, 6.6 km from the water.

    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

    16records within 5 km

    9 deposits, 7 ore occurrences

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

    Landslides and slope deformations

    21areas within 3 km

    2 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.

    • Young sediments67%SR 8.6 %
    • River alluvium33%SR 72 %

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

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

    Geological age of the rocks

    • Quaternary100%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains1×
    QuaternaryPleistocene – Holocenedeluvial-polygenetic sediments: clay-clay and sandy slope clays1×
    QuaternaryPleistocene – Holocenedeluvial sediments: predominantly loamy-stoney (subordinate sandy-stone) slopes and rubble1×

    Quaternary cover

    • deluvial sediments100%SR 16 %

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

    • Typical thickness of the Quaternary cover3.3m
    • 2 – 550%SR 48 %
    • 0 – 233%SR 16 %
    • 5 – 1017%SR 20 %

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

    Tectonic division

    • NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

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    Neotectonic units

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

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    Direction of neotectonic movements

    • medium uplift75%SR 32 %
    • large uplift25%SR 26 %

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    Regional geological division

    • Inner Carpathian Paleogene86%SR 11 %
    • Klippen Belt and the adjacent peri-Klippen zone14%SR 2.2 %

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

    Regional geological division (subunits)

    • Spiš–Šariš Paleogene86%SR 5.8 %
    • Šariš section14%SR 0.0 %

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

    Engineering-geological districts

    • region of sandstone-conglomerate rocks100%SR 3.4 %

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    Engineering-geological formations

    • flysch formation100%SR 13 %

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    Susceptibility of the area to slope deformations

    • Region of stable areas83%SR 95 %
    • Region of potentially unstable areas17%SR 4.4 %

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    The map covers 3 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)

    • Gravel50%SR 52 %
    • Sandstones50%SR 15 %

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

    Aquifer type

    • Zvodnence s prevažne medzizrnovým typom priepustnosti (prevažne nespevnené sedimenty) (Gravel; Fluviálne)50%SR 27 %
    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Sandstones)50%SR 15 %

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

    • intergranular50%SR 86 %
    • fissure50%SR 12 %

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    Hydrogeological function

    • aquifer100%SR 95 %

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    Main hydrogeological region

    • Paleogene of Spiš-Šarišské Medzihoria, Bachurne and Šarišská vrchovina in the Torysy basin75%SR 0.0 %
    • Paleogene of Čergov25%SR 1.4 %

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    Genetic type of groundwater

    • carbonate-silicatogenic groundwater100%SR 3.5 %

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    Chemical type of groundwater

    • Ca-HCO3 typ50%SR 5.1 %
    • Ca-Mg-HCO3 typ50%SR 5.5 %

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    Groundwater quality class

    • A100%SR 36 %

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    Geothermal groundwater bodies

    • Levoča Basin – NE part100%SR 5.0 %

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    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 8.22typical 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

    16.3°dH, hard

    Sum of calcium and magnesium (2.91 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    458mg/l mineralisation

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

    Ionic composition of the water

    Water type by dominant ions: Ca–Mg–HCO₃

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

    Major ions

    • PotassiumK9.50 mg/lpercentile 91
    • FluoridesF0.182 mg/lpercentile 76
    • CalciumCa83.9 mg/lpercentile 74
    • BicarbonatesHCO3268 mg/lpercentile 68
    • MagnesiumMg19.9 mg/lpercentile 65
    • SulphatesSO451.7 mg/lpercentile 62
    • SodiumNa9.66 mg/lpercentile 52
    • ChloridesCl9.63 mg/lpercentile 52

    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

    • AmmoniumNH41.10 mg/lpercentile 93
    • PhosphatesPO40.403 mg/lpercentile 75
    • Chemical oxygen demandChSK4.00 mg/lpercentile 67
    • NitratesNO37.07 mg/lpercentile 57

    Metals

    • ZincZn6.54 μg/lpercentile 49
    • ManganeseMn28.7 μg/lpercentile 48
    • AluminiumAl55.6 μg/lpercentile 46
    • IronFe0.0569 mg/lpercentile 26

    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

    • ChromiumCr97.8 mg/kgpercentile 80
    • AntimonySb1.32 mg/kgpercentile 77
    • NickelNi31.3 mg/kgpercentile 74
    • MolybdenumMo0.523 mg/kgpercentile 72
    • SeleniumSe0.297 mg/kgpercentile 61
    • VanadiumV66.3 mg/kgpercentile 46
    • ArsenicAs6.19 mg/kgpercentile 44
    • TinSn2.45 mg/kgpercentile 42
    • CobaltCo7.93 mg/kgpercentile 41
    • CadmiumCd0.130 mg/kgpercentile 36
    • BismuthBi0.181 mg/kgpercentile 35
    • ZincZn79.5 mg/kgpercentile 30
    • MercuryHg0.0684 mg/kgpercentile 28
    • CopperCu18.3 mg/kgpercentile 25
    • LeadPb8.18 mg/kgpercentile 5

    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)
    • SodiumNa1.09 %percentile 80
    • PotassiumK1.64 %percentile 69
    • ManganeseMn969 mg/kgpercentile 62
    • TitaniumTi4,537 mg/kgpercentile 52
    • CalciumCa1.99 %percentile 48
    • AluminiumAl5.44 %percentile 43
    • MagnesiumMg0.800 %percentile 41
    • IronFe2.41 %percentile 34
    • PhosphorusP661 mg/kgpercentile 25
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • BoronB68.8 mg/kgpercentile 73
    • GalliumGa16.3 mg/kgpercentile 70
    • BerylliumBe1.58 mg/kgpercentile 60
    • LithiumLi29.7 mg/kgpercentile 51
    • RubidiumRb87.3 mg/kgpercentile 47
    • CeriumCe58.2 mg/kgpercentile 47
    • ZirconiumZr371 mg/kgpercentile 39
    • StrontiumSr111 mg/kgpercentile 26
    • YttriumY22.0 mg/kgpercentile 22
    • BariumBa359 mg/kgpercentile 20

    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

    51nGy/h in air

    range 42 to 61 nGy/h

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

    Radon risk of the bedrock

    medium

    Radon is a natural gas from rocks. The risk concerns buildings and cellars, not the water in the stream; it shows what the bedrock is like.

    • Potassium (K)K1.48 %percentile 82
    • Equivalent thorium (eTh)eTh7.29 ppm49th percentile
    • Equivalent uranium (eU)eU2.36 ppm26th 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 137CsCS1371,318 Bq/m²percentile 39

    Radon risk by isopleths

    • medium100%SR 64 %

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    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

    -38nT

    range -63 to -24 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

    -28mGal

    residual +2.9 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 °C72 °C

    Rock temperature with depth

    35 / 72 °Cat depths of 1,000 and 2,000 m

    increase of 37 °C per km

    The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 71 mW/m².

    Geothermal groundwater bodies beneath the water line

    • Levoča Basin – NE part100%SR 5.0 %

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    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)243–1 157m a.s.l.
    • Average elevation of the units590m a.s.l.
    • Average slope11.9°
    • Average January temperature-4.8°C
    • Average July temperature16.6°C
    • Annual precipitation813mm

    Geomorphological units

    • Bachureň50%SR 0.0 %
    • Spiš–Šariš Intermountain Area33%SR 0.0 %
    • Čergov17%SR 0.0 %

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    Geomorphological regions

    • Podhôľne–Magura area83%SR 4.5 %
    • Východné Beskydy17%SR 1.3 %

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    Climatic-geographical types

    • mountain climate75%SR 33 %
    • basin climate25%SR 29 %

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    Susceptibility of soils to acidification

    • soils susceptible to acidification100%SR 31 %

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    Soil contamination (map 1:500,000)

    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A86%SR 45 %
    • relatively clean soil14%SR 53 %

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    Lithogeochemical types

    • Inner Carpathian Paleogene100%SR 11 %

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    Map of the corridor

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

    Šarišská Trstená – Jama PD – Šarišské Michaľany – none (1.3 km from the water)Ražňany – none (2.6 km from the water)Telek – Jakubovany – cannot be estimated (2.8 km from the water)Lipany – L-2 – non-spa (4.1 km from the water)Lipany – L-1 – non-spa (6.6 km from the water)a1 (430 m from the water)a1 (730 m from the water)a1 (2.5 km from the water)a1 (5.9 km from the water)a1 (6.4 km from the water)a1 (6.7 km from the water)a1 (6.8 km from the water)a1 (7.1 km from the water)a1 (7.5 km from the water)a1 (8.6 km from the water)a1 (8.9 km from the water)b1 (9.0 km from the water)a1 (9.4 km from the water)a1 (9.5 km from the water)a1 (9.7 km from the water)Lipany – combustible natural gas (4.7 km from the water)Lipany – semi-paraffinic crude oil (4.7 km from the water)Lipany – semi-paraffinic crude oil (4.9 km from the water)Lipany – combustible natural gas (4.9 km from the water)Orkucany – Buchanec – gravelly sands and sands (130 m from the water)Ražňany – gravelly sands and sands (280 m from the water)Orkucany – gravelly sands and sands (890 m from the water)Šarišské Michaľany – gravelly sands and sands (1.4 km from the water)Pečovská Nová Ves – gravelly sands and sands (3.6 km from the water)Uzovský Šalgov – brick raw materials (130 m from the water)Orkucany – brick raw materials (200 m from the water)Šarišské Sokolovce – brick raw materials (1.5 km from the water)Šarišské Sokolovce – building stone – sandstone (1.6 km from the water)Šarišské Sokolovce – building stone – conglomerate, breccia (2.6 km from the water)Lipany 2 – crude oil, natural gas (4.1 km from the water)Renčišov – brick raw materials (4.4 km from the water)– Landslides (130 m from the water)– Landslides (500 m from the water)– Landslides (1.3 km from the water)– Landslides (1.4 km from the water)SARISSKE SOKOLOVCE – Landslides (1.4 km from the water)PECOV NOVA VES – Landslides (1.7 km from the water)– Landslides (1.8 km from the water)– Landslides (1.8 km from the water)– Landslides (2.0 km from the water)JAKUBOVA VOLA – Landslides (2.2 km from the water)– Landslides (2.3 km from the water)UZOVCE – Landslides (2.4 km from the water)JAROVNICE – Landslides (2.6 km from the water)UZOVCE – Landslides (2.6 km from the water)JAKUBOVA VOLA – Landslides (2.6 km from the water)– Landslides (2.6 km from the water)– Landslides (2.7 km from the water)– Landslides (2.9 km from the water)– Landslides (2.9 km from the water)– Landslides (2.9 km from the water)RENCISOV – Landslides (3.0 km from the water)Jakubovany – úzkoprofilový vrt s obyčajnou pitnou a ú (40 m from the water)Ražňany – úzkoprofilový vrt s obyčajnou pitnou a ú (80 m from the water)Sabinov (90 m from the water)Sabinov – monitoring borehole (110 m from the water)Sabinov – monitoring borehole (180 m from the water)Sabinov – monitoring borehole (190 m from the water)Ražňany – úzkoprofilový vrt s obyčajnou pitnou a ú (230 m from the water)Orkucany – širokoprofilový vrt (Ø vŕtania nad 600 m (240 m from the water)Sabinov-Ostrovany – monitoring borehole (460 m from the water)Sabinov – monitoring borehole (480 m from the water)Orkucany – úzkoprofilový vrt s obyčajnou pitnou a ú (500 m from the water)Sabinov – monitoring borehole (500 m from the water)Sabinov-Ostrovany – monitoring borehole (580 m from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (690 m from the water)Uzovský Šalgov – širokoprofilový vrt (Ø vŕtania nad 600 m (750 m from the water)Sabinov – monitoring borehole (780 m from the water)Sabinov – úzkoprofilový vrt s obyčajnou pitnou a ú (830 m from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (840 m from the water)Okrucany – úzkoprofilový vrt s obyčajnou pitnou a ú (850 m from the water)Orkucany – úzkoprofilový vrt s obyčajnou pitnou a ú (850 m from the water)Ražňany – negative borehole (950 m from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.3 km from the water)Okrucany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.4 km from the water)Šarišské Sokolovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.4 km from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.5 km from the water)Sabinov – širokoprofilový vrt (Ø vŕtania nad 600 m (1.5 km from the water)Sabinov – širokoprofilový vrt (Ø vŕtania nad 600 m (1.5 km from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.6 km from the water)Šarišské Sokolovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.6 km from the water)Uzovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.6 km from the water)Sabinov-Ostrovany – monitoring borehole (1.7 km from the water)Orkucany – širokoprofilový vrt (Ø vŕtania nad 600 m (1.7 km from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Ostrovany – negative borehole (1.8 km from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Šarišské Michaľany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Pečovská Nová Ves – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Pečovská Nová Ves – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Pečovská Nová Ves – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)prameň – Groundwater springs (30 m from the water)vodárensky využívaný a monitorovaný prameň – Groundwater springs (40 m from the water)prameň – Groundwater springs (70 m from the water)prameň – Groundwater springs (80 m from the water)prameň – Groundwater springs (80 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (80 m from the water)prameň – Groundwater springs (90 m from the water)prameň – Groundwater springs (110 m from the water)prameň – Groundwater springs (120 m from the water)prameň – Groundwater springs (140 m from the water)prameň – Groundwater springs (230 m from the water)meteorologická stanica – Artificial hydrogeologically significant objects (250 m from the water)prameň – Groundwater springs (260 m from the water)prameň – Groundwater springs (300 m from the water)prameň – Groundwater springs (310 m from the water)prameň – Groundwater springs (400 m from the water)zrážkomerná stanica – Artificial hydrogeologically significant objects (450 m from the water)prameň – Groundwater springs (460 m from the water)prameň – Groundwater springs (470 m from the water)prameň – Groundwater springs (470 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (500 m from the water)prameň – Groundwater springs (530 m from the water)prameň – Groundwater springs (550 m from the water)prameň – Groundwater springs (550 m from the water)prameň – Groundwater springs (600 m from the water)pramenná línia – Groundwater springs (600 m from the water)prameň – Groundwater springs (650 m from the water)prameň – Groundwater springs (660 m from the water)prameň – Groundwater springs (660 m from the water)prameň – Groundwater springs (690 m from the water)prameň – Groundwater springs (690 m from the water)prameň – Groundwater springs (690 m from the water)prameň – Groundwater springs (700 m from the water)prameň – Groundwater springs (700 m from the water)prameň – Groundwater springs (710 m from the water)prameň – Groundwater springs (710 m from the water)prameň – Groundwater springs (720 m from the water)prameň – Groundwater springs (720 m from the water)prameň – Groundwater springs (740 m from the water)prameň – Groundwater springs (750 m from the water)horáreň Jakubovany,750m JZ od K744 – source (120 m from the water)dolina z Jakubovian, 1850m J od K809 – source (300 m from the water)Šarišské Sokolovce, dolina potoka Bernát – source (480 m from the water)Drienica, 4 km SSV – source (700 m from the water)Šarišské Sokolovce, 5 km S – source (1.1 km from the water)Šarišské Sokolovce, dolina Veľkého potoka – source (1.3 km from the water)Šarišské Sokolovce-dolina, 650m SZ od K 738 – source (1.5 km from the water)Šarišské Sokolovce-dolina, 1000m JV od K744 – source (1.5 km from the water)Jakubovany-dolina, 900m ZJZ od K738 – source (1.6 km from the water)Šarišské Sokolovce, dolina Veľkého potoka – source (2.1 km from the water)Šarišské Sokolovce-dolina, 750m JZ od K907 – source (2.2 km from the water)dolina z Drienice,lyz.vlek,800m Z od K848 – source (2.3 km from the water)dolina z Drienice,500m JZ od K762 – source (2.3 km from the water)Drienica, 800 m SSV – source (2.4 km from the water)dolina z Drienice na Lysu,1200m Jz od K1068 – source (2.5 km from the water)chata Lysá, 200m Z od K1068 – source (2.7 km from the water)Majdan, 3500 m VJV – source (2.9 km from the water)zlato 3 ks – gold (90 m from the water)zlato 1 ks – gold (110 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.

    • CadmiumCdelevated (top 10 %)
      highest 0.300 μg/lmedian 0.300 μg/l8 samples

      Highest value: Orkucany, 50 m from the water. Comparison: percentile 90 of all samples in Slovakia.

    • LeadPbelevated (top 10 %)
      highest 4.00 μg/lmedian 4.00 μg/l8 samples

      Highest value: Orkucany2003, 50 m from the water. Comparison: percentile 90 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 20.0 μg/lmedian 10.0 μg/l8 samples

      Highest value: Jakubovany2003, 70 m from the water. Comparison: percentile 84 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 1.00 μg/lmedian 1.00 μg/l8 samples

      Highest value: Orkucany2003, 50 m from the water. Comparison: percentile 82 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 3.00 μg/lmedian 2.00 μg/l8 samples

      Highest value: Jakubovany2003, 70 m from the water. Comparison: percentile 79 of all samples in Slovakia.

    • BariumBaslightly elevated
      highest 70.0 μg/lmedian 40.0 μg/l8 samples

      Highest value: Jakubovany2003, 70 m from the water. Comparison: percentile 78 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 2.00 μg/lmedian 1.00 μg/l8 samples

      Highest value: Ražňany2003, 50 m from the water. Comparison: percentile 75 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)21 samples, at most 315 grains
    • Pyrite (FeS₂)16 samples, at most 55 grains
    • Magnetite (Fe₃O₄)7 samples, at most 815 grains
    • Rutil (TiO₂)7 samples, at most 815 grains
    • Anatas (TiO₂)6 samples, at most 55 grains
    • Hematite (Fe₂O₃)6 samples, at most 315 grains
    • Ilmenit (FeTiO₃)6 samples, at most 815 grains
    • Limonite (FeO(OH)·nH₂O)6 samples, at most 815 grains
    • Monazit ((Ce,La,Nd)PO₄)4 samples, at most 5 grains
    • Gold (Au)2 samples, at most 3 grains
    • Chalcopyrite (CuFeS₂)2 samples, at most 5 grains
    • Auripigment (As₂S₃)1 sample, at most 5 grains
    • Kasiterit (SnO₂)1 sample, at most 4 grains
    • Markazit (FeS₂)1 sample, at most 5 grains

    Nearest samples with gold

    SampleGold in sampleFrom the water
    TP-42903 grains90 m
    TP-42931 grain110 m

    Rock-forming and accessory minerals

    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)28 samples, at most 1815 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)7 samples, at most 4115 grains
    • Tourmalines (complex borosilicate)7 samples, at most 55 grains
    • Zirconium (ZrSiO₄)7 samples, at most 1815 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)6 samples, at most 1815 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))5 samples, at most 55 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))2 samples, at most 5 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))2 samples, at most 55 grains

    Groundwater: chemistry, water types and radioactivity

    Hydrogeochemical objects (analyses of springs and boreholes), the geochemical atlas of groundwater (1996) and radiohydrochemical sampling. Groundwater feeds streams, so its composition also affects the water in the stream.

    Chemical water types nearby

    • Ca-Mg-HCO310×
    • Ca-HCO35×
    • Ca-Mg-HCO3-SO41×
    • Ca-HCO3-SO41×

    Water quality class according to the hydrogeochemical map

    • class A14×
    • class G2×
    • class B1×

    Metals in groundwater

    • LeadPbextreme (top 1 %)
      highest 17.0 μg/lmedian 1.00 μg/l41 samples46 % below the limit of quantification

      Highest value: prameň1992, 1.8 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • MercuryHgextreme (top 1 %)
      highest 1.10 μg/lmedian 0.100 μg/l41 samples88 % below the limit of quantification

      Highest value: studňa1992, 1.2 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AluminiumAlextreme (top 1 %)
      highest 0.220 mg/lmedian 0.00500 mg/l41 samples78 % below the limit of quantification

      Highest value: prameň1992, 300 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 2.90 μg/lmedian 0.100 μg/l41 samples76 % below the limit of quantification

      Highest value: studňa1992, 2.6 km from the water. Comparison: percentile 98 of all samples in Slovakia.

    • LithiumLihigh (top 5 %)
      highest 90.0 μg/lmedian 9.00 μg/l41 samples5 % below the limit of quantification

      Highest value: studňa1992, 2.4 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 0.900 μg/lmedian 0.250 μg/l41 samples98 % below the limit of quantification

      Highest value: prameň1992, 2.2 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ArsenicAshigh (top 5 %)
      highest 5.80 μg/lmedian 0.500 μg/l41 samples68 % below the limit of quantification

      Highest value: prameň1992, 120 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ChromiumCrelevated (top 10 %)
      highest 3.40 μg/lmedian 0.250 μg/l41 samples56 % below the limit of quantification

      Highest value: studňa1992, 2.6 km from the water. Comparison: percentile 94 of all samples in Slovakia.

    • ZincZnelevated (top 10 %)
      highest 660 μg/lmedian 5.00 μg/l41 samples15 % below the limit of quantification

      Highest value: studňa1992, 2.4 km from the water. Comparison: percentile 92 of all samples in Slovakia.

    • SeleniumSeelevated (top 10 %)
      highest 1.90 μg/lmedian 0.500 μg/l41 samples88 % below the limit of quantification

      Highest value: studňa1992, 2.6 km from the water. Comparison: percentile 91 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 3.60 μg/lmedian 0.500 μg/l41 samples

      Highest value: prameň1992, 770 m from the water. Comparison: percentile 88 of all samples in Slovakia.

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

      Highest value: prameň1992, 2.3 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    source921,8 Bq/l9.40 Bq/l
    developed spring544,1 Bq/l12.9 Bq/l
    well519,9 Bq/l6.70 Bq/l
    free-flowing borehole119,1 Bq/l19.1 Bq/l
    water source for public supply11,30 Bq/l1.30 Bq/l
    stream, river20,410 Bq/l0.245 Bq/l

    Mine workings, deposits and ore occurrences

    Old mine workings outside mining areas (Geofond register), deposits and mining areas, and the metallogenetic map. Gold, silver and other metals near streams can get into sediments and water.

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    Orkucany – Buchanecgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – S.F.Bouw, s. r. o.130 m
    Ražňanygravelly sands and sandsMined deposit – SUPOL, s.r.o.280 m
    Orkucanygravelly sands and sandsMined deposit – B&S s.r.o.890 m
    Šarišské Michaľanygravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – Bujňák A. – SVIP1.4 km
    Pečovská Nová Vesgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – PEhAES, a.s.3.6 km
    Lipanycombustible natural gasDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.7 km
    Lipanysemi-paraffinic crude oilDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.7 km
    Lipanysemi-paraffinic crude oilDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.9 km
    Lipanycombustible natural gasDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.9 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.

    187 boreholes in the 3 km zone, of which 113 hydrogeological and 74 other; with an archive report number 187.

    Borehole depths

    • up to 10 m113×
    • 10–30 m61×
    • 30–100 m6×
    • 100–300 m4×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Jakubovanynarrow-diameter borehole with ordinary drinking and process water25.0 m7836 103Cb1.pdf40 m
    Ražňanynarrow-diameter borehole with ordinary drinking and process water13.0 m9127 103Ca26.pdf80 m
    Sabinov6.0 m70491 103Ca67.pdf90 m
    PST-48engineering-geological2.5 m16140100 m
    Sabinovmonitoring borehole6.0 m77543 103Ca81.pdf110 m
    Sabinovmonitoring borehole6.0 m77543 103Ca82.pdf180 m
    Sabinovmonitoring borehole6.0 m77543 103Cc49.pdf190 m
    Ražňanynarrow-diameter borehole with ordinary drinking and process water51.0 m64508 103Ca62.pdf230 m
    JV-8engineering-geological6.5 m85354230 m
    Orkucanywide-diameter borehole8.0 m44732 103Cc38.pdf240 m
    OV-5deposit7.0 m34173250 m
    4-11A Ražňanyhydrogeological7.0 m101748320 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.

    BoreholeTemperatureYieldDepthChemical water typeUseFrom the water
    Lipany – L-251 °C4.5 l/s3500 mNa-Clunused4.1 km
    Lipany – L-190 °C10.0 l/s4000 mNa-HCO3-Cl-SO4unused6.6 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 514430 m
    category b1mineral water15-22< 519.0 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
    Šarišská Trstená – Jama PD – Šarišské Michaľany–1980–1.3 km
    Ražňany7 150 m²1996monitored2.6 km
    Telek – Jakubovany–1975–2.8 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

    • Landslides21×

    Degree of activity

    • Potenciálny18×
    • Aktívny2×
    • Stabilizovaný1×

    Current state

    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S12×
    • SD taken from archival materials, ktorá bola konfrontova7×
    • Processed only in the scope of registration on a scale of 1:25,0002×

    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. Sabinov1 fishing district · 16 km44Jakuboviansky potok44

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