Today on the Ľubotínka watercourse

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

Average of the watercourse's fishing districts

Low activity · average of one fishing district

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

Best window today

15:00–17:00

Ľubotínka č. 1, window score 34.

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
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    Elevation profile of the watercourse

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

    Brisk watercourse A foothill river with a gravel bottom and a fast current. Grayling and trout already thrive here.

    4804905005100 km1 km2 km3 km
    Elevation profile of the watercourse: from 507 to 482 m a.s.l. over 3.7 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
    507 m a.s.l.
    Lowest point
    479 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.
    29 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.
    7.7 ‰
    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.
    1.16

    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 Ľubotínka from 2019
    2019imaged 26 Aug 2019
    Aerial image of watercourse Ľubotínka from 2022
    2022imaged 4 Aug 2022
    Aerial image of watercourse Ľubotínka 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 Ľubotínka watercourse

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

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

    0 of 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 Ľubotínka 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 (4 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 8.1modelled estimate

    water type Ca–HCO₃

    Mineralisation 379 mg/l, moderately hard water (12.4 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    2 from 15elements in the top 10 %

    highest: Molybdenum 0.877 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 92. Interpolation of the Geochemical Atlas of river sediments.

    20200

    Natural gamma radiation

    47nGy/h dose rate

    percentile 24 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

    1object within 3 km

    Nearest: Odkalisko Orlov (tailings pond), 330 m from the water.

    Gold in river sediment

    0samples with gold

    10 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

    1 from 9indicators in the top 5 %

    highest: Chromium 15.0 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (voda štrkoviska).

    Boreholes and groundwater analyses

    296boreholes within 3 km

    231 water analyses nearby

    Of these, 296 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    65°C at the wellhead

    3 geothermal boreholes within 10 km

    Warmest: Plavnica – Pl-1, yield 5.0 l/s, 7.8 km from the water.

    Environmental burdens and landfills

    19sites within 3 km

    19 landfills

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

    Deposits and ore occurrences

    5records within 5 km

    4 deposits, 1 ore occurrence

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

    Landslides and slope deformations

    65areas within 3 km

    5 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 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

    • fluvial sediments of floodplains100%SR 68 %

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

    • Typical thickness of the Quaternary cover7.5m
    • 5 – 10100%SR 20 %

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

    Regional geological division

    • Klippen Belt and the adjacent peri-Klippen zone100%SR 2.2 %

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

    Regional geological division (subunits)

    • Šariš section100%SR 0.0 %

    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 2 points on the water line.

    Hydrogeology: aquifers and groundwater

    Streams and rivers are fed by groundwater. Hydrogeological maps show in which rocks the water is stored, how permeable they are and what the water in them is like. The data come from ŠGÚDŠ maps, not from measurements at a particular water.

    Main hydrogeological region

    • paleogén Spišskej Magury, Ľubovnianskej vrchoviny a severozápadnej časti Spišsko – šarišského medzihoria a Pi…100%SR 2.3 %

    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 8.14typical 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

    12.4°dH, moderately hard

    Sum of calcium and magnesium (2.22 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    379mg/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

    • PotassiumK3.66 mg/lpercentile 60
    • FluoridesF0.129 mg/lpercentile 57
    • CalciumCa66.8 mg/lpercentile 55
    • BicarbonatesHCO3224 mg/lpercentile 54
    • ChloridesCl7.37 mg/lpercentile 45
    • MagnesiumMg13.5 mg/lpercentile 44
    • SulphatesSO434.9 mg/lpercentile 42
    • SodiumNa7.05 mg/lpercentile 40

    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

    • AmmoniumNH40.0422 mg/lpercentile 21
    • Chemical oxygen demandChSK1.94 mg/lpercentile 18
    • NitratesNO32.60 mg/lpercentile 13
    • PhosphatesPO40.0207 mg/lpercentile 10

    Metals

    • ManganeseMn105 μg/lpercentile 80
    • IronFe0.140 mg/lpercentile 63
    • AluminiumAl77.3 μg/lpercentile 54
    • ZincZn1.58 μg/lpercentile 9

    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

    • MolybdenumMo0.877 mg/kgpercentile 92
    • ChromiumCr131 mg/kgpercentile 91
    • NickelNi32.3 mg/kgpercentile 76
    • MercuryHg0.126 mg/kgpercentile 59
    • BismuthBi0.227 mg/kgpercentile 54
    • SeleniumSe0.238 mg/kgpercentile 48
    • CadmiumCd0.170 mg/kgpercentile 46
    • ZincZn78.9 mg/kgpercentile 30
    • CopperCu18.8 mg/kgpercentile 27
    • AntimonySb0.415 mg/kgpercentile 26
    • VanadiumV58.0 mg/kgpercentile 24
    • CobaltCo6.66 mg/kgpercentile 22
    • ArsenicAs4.66 mg/kgpercentile 20
    • LeadPb8.65 mg/kgpercentile 6
    • TinSn1.53 mg/kgpercentile 6

    dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile)

    Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
    • SodiumNa0.958 %percentile 66
    • TitaniumTi4,760 mg/kgpercentile 61
    • PotassiumK1.58 %percentile 60
    • CalciumCa2.11 %percentile 51
    • AluminiumAl5.55 %percentile 47
    • MagnesiumMg0.840 %percentile 45
    • IronFe2.59 %percentile 44
    • ManganeseMn776 mg/kgpercentile 42
    • PhosphorusP723 mg/kgpercentile 33
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • LithiumLi35.5 mg/kgpercentile 77
    • BoronB70.7 mg/kgpercentile 76
    • YttriumY28.7 mg/kgpercentile 56
    • RubidiumRb90.2 mg/kgpercentile 55
    • BariumBa431 mg/kgpercentile 48
    • ZirconiumZr394 mg/kgpercentile 47
    • CeriumCe56.7 mg/kgpercentile 41
    • BerylliumBe1.21 mg/kgpercentile 38
    • StrontiumSr118 mg/kgpercentile 33
    • GalliumGa11.4 mg/kgpercentile 29

    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

    47nGy/h in air

    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)K1.38 %percentile 69
    • Equivalent thorium (eTh)eTh6.96 ppm33th percentile
    • Equivalent uranium (eU)eU2.01 ppm8th 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 137CsCS1371,157 Bq/m²percentile 28

    Radon risk by isopleths

    • medium100%SR 64 %

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

    Geophysical fields: magnetics and gravity

    Maps of the magnetic field and gravity (ŠGÚDŠ) reveal what lies beneath the sediments and the surface: volcanic bodies, faults and crustal thickness. For an angler they are interesting indirectly: they show where the bedrock changes, and with it the water.

    SVJZ

    Magnetic anomaly

    -21nT

    range -21 to -21 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

    -40mGal

    residual +2.1 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 2,000 m depth65°C
    • Surface heat flow density65mW/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)432–736m a.s.l.
    • Average elevation of the units564m a.s.l.
    • Average slope8.2°

    Geomorphological units

    • Spiš–Šariš Intermountain Area100%SR 0.0 %

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

    Geomorphological regions

    • Podhôľne–Magura area100%SR 4.5 %

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

    Susceptibility of soils to acidification

    • soils not susceptible to acidification100%SR 27 %

    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.

    Odkalisko Orlov – 3 – tailings pond (330 m from the water)Ďurková – cannot be estimated (10 m from the water)Ďurková – cannot be estimated (80 m from the water)Orlov – cannot be estimated (300 m from the water)Ďurková – cannot be estimated (580 m from the water)Orlov – Ľubotín – cannot be estimated (590 m from the water)Šarišské Jastrabie – cannot be estimated (820 m from the water)Vislanka – cannot be estimated (1.2 km from the water)Vislanka – cannot be estimated (1.6 km from the water)Orlov – cannot be estimated (1.7 km from the water)Vislanka – cannot be estimated (1.9 km from the water)Vislanka – cannot be estimated (2.1 km from the water)Plaveč – cannot be estimated (2.1 km from the water)Plaveč – cannot be estimated (2.2 km from the water)Pasterník – Plaveč – cannot be estimated (2.2 km from the water)Vislanka – ulička – Vislanka – cannot be estimated (2.3 km from the water)Šarišské Jastrabie – cannot be estimated (2.3 km from the water)Kozelec – Plaveč – cannot be estimated (2.3 km from the water)Vislanka – cannot be estimated (2.4 km from the water)pri ihrisku – Šarišské Jastrabie – cannot be estimated (2.8 km from the water)Plavnica – Pl-2 – non-spa (5.7 km from the water)Plavnica – Pl-1 – non-spa (7.8 km from the water)Šariš – Š-1 – non-spa (9.7 km from the water)a1 (3.0 km from the water)a1 (4.8 km from the water)a1 (5.0 km from the water)a1 (5.3 km from the water)a1 (5.8 km from the water)a1 (5.9 km from the water)a1 (6.3 km from the water)a1 (6.6 km from the water)a1 (6.7 km from the water)a1 (6.9 km from the water)a1 (7.3 km from the water)a1 (7.5 km from the water)a1 (7.9 km from the water)a1 (8.1 km from the water)a1 (8.3 km from the water)a1 (8.9 km from the water)b2 (9.2 km from the water)a1 (9.3 km from the water)a1 (9.3 km from the water)a1 (9.6 km from the water)Plaveč – Orlov – gravelly sands and sands (410 m from the water)Plaveč I – Orlov II – gravelly sands and sands (570 m from the water)Plaveč – Orlov – gravelly sands and sands (410 m from the water)Plaveč I – Orlov II – gravelly sands and sands (570 m from the water)Čirč – building stone – sandstone (4.4 km from the water)ORLOV – Landslides (420 m from the water)– Landslides (460 m from the water)– Landslides (460 m from the water)PLAVEC – Landslides (480 m from the water)DURKOV – Landslides (500 m from the water)PLAVEC – Landslides (630 m from the water)– Landslides (740 m from the water)– Landslides (760 m from the water)PLAVEC – Landslides (760 m from the water)– Landslides (830 m from the water)– Landslides (890 m from the water)– Landslides (910 m from the water)PLAVEC – Landslides (1.0 km from the water)– Landslides (1.1 km from the water)– Landslides (1.1 km from the water)LUBOTIN – Landslides (1.3 km from the water)LUBOTIN – Landslides (1.3 km from the water)– Landslides (1.3 km from the water)– Landslides (1.3 km from the water)– Slope flows (1.4 km from the water)– Landslides (1.5 km from the water)– Landslides (1.5 km from the water)– Landslides (1.5 km from the water)– Landslides (1.6 km from the water)PLAVEC – Landslides (1.7 km from the water)LUBOTIN – Landslides (1.7 km from the water)– Landslides (1.8 km from the water)– Landslides (1.8 km from the water)– Landslides (1.8 km from the water)– Landslides (1.8 km from the water)– Landslides (1.8 km from the water)– Landslides (1.8 km from the water)– Landslides (1.9 km from the water)– Landslides (1.9 km from the water)– Landslides (2.0 km from the water)LUBOTIN – Landslides (2.0 km from the water)LUBOTIN – Landslides (2.0 km from the water)– Landslides (2.0 km from the water)– Landslides (2.0 km from the water)– Landslides (2.1 km from the water)– Landslides (2.2 km from the water)PLAVEC – Landslides (2.2 km from the water)– Landslides (2.2 km from the water)– Landslides (2.3 km from the water)– Landslides (2.3 km from the water)– Landslides (2.3 km from the water)PLAVEC – Landslides (2.4 km from the water)– Landslides (2.5 km from the water)– Landslides (2.5 km from the water)– Landslides (2.5 km from the water)– Landslides (2.5 km from the water)– Landslides (2.6 km from the water)– Landslides (2.6 km from the water)– Landslides (2.7 km from the water)– Landslides (2.7 km from the water)– Landslides (2.7 km from the water)– Landslides (2.7 km from the water)– Landslides (2.7 km from the water)CIRC – Landslides (2.7 km from the water)PLAVEC – Landslides (2.8 km from the water)PLAVEC – Landslides (2.8 km from the water)– Landslides (2.8 km from the water)– Landslides (2.9 km from the water)– Landslides (2.9 km from the water)– Landslides (3.0 km from the water)Orlov – úzkoprofilový vrt s obyčajnou pitnou a ú (50 m from the water)Orlov – úzkoprofilový vrt s obyčajnou pitnou a ú (60 m from the water)Ľubotín – úzkoprofilový vrt s obyčajnou pitnou a ú (100 m from the water)Ďurková – Ľubotín – úzkoprofilový vrt s obyčajnou pitnou a ú (100 m from the water)Orlov – úzkoprofilový vrt s obyčajnou pitnou a ú (110 m from the water)Lipany – Ľubotín – negative borehole (120 m from the water)Ďurková – Ľubotín – úzkoprofilový vrt s obyčajnou pitnou a ú (130 m from the water)Ľubotín – úzkoprofilový vrt s obyčajnou pitnou a ú (140 m from the water)Ľubotín – úzkoprofilový vrt s obyčajnou pitnou a ú (240 m from the water)Plaveč – úzkoprofilový vrt s obyčajnou pitnou a ú (270 m from the water)Plaveč – úzkoprofilový vrt s obyčajnou pitnou a ú (290 m from the water)Ľubotín – širokoprofilový vrt (Ø vŕtania nad 600 m (320 m from the water)Plaveč – širokoprofilový vrt (Ø vŕtania nad 600 m (320 m from the water)Plaveč – úzkoprofilový vrt s obyčajnou pitnou a ú (360 m from the water)Plaveč – borehole for a waterworks (360 m from the water)Plaveč – širokoprofilový vrt (Ø vŕtania nad 600 m (400 m from the water)Plaveč – borehole for a waterworks (430 m from the water)Ľubotín – úzkoprofilový vrt s obyčajnou pitnou a ú (430 m from the water)Plaveč – úzkoprofilový vrt s obyčajnou pitnou a ú (450 m from the water)Plaveč – úzkoprofilový vrt s obyčajnou pitnou a ú (570 m from the water)Orlov (780 m from the water)Orlov – SHMÚ observation borehole (840 m from the water)Orlov – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Plaveč – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Orlov – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Plaveč – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Šarišské Jastrabie – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Šarišské Jastrabie – negative borehole (2.8 km from the water)Vislanka – negative borehole (2.9 km from the water)Šarišské Jastrabie – širokoprofilový vrt (Ø vŕtania nad 600 m (2.9 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (770 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (960 m from the water)prameň – Groundwater springs (1.2 km from the water)prameň – Groundwater springs (1.3 km from the water)prameň – Groundwater springs (1.6 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.9 km from the water)prameň – Groundwater springs (2.0 km from the water)vodárensky využívaný prameň – Groundwater springs (2.6 km from the water)vodárensky využívaný prameň – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (3.0 km from the water)Orlov – source (1.2 km from the water)Plaveč – borehole (1.3 km from the water)Orlov – borehole (1.6 km from the water)Orlov – borehole (2.0 km from the water)Orlov – source (2.6 km from the water)Čirč, dolina potoka Olšavec, 1000m J od K663 – source (2.6 km from the water)Orlov – source (2.6 km from the water)Andrejovka – borehole (2.9 km from the water)Údol – Nad jamy – borehole (3.0 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.

    • ChromiumCrextreme (top 1 %)
      highest 15.0 μg/lmedian 1.00 μg/l4 samples75 % below the limit of quantification

      Highest value: voda štrkoviska2007, 720 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AntimonySbelevated (top 10 %)
      highest 2.00 μg/lmedian 0.500 μg/l4 samples75 % below the limit of quantification

      Highest value: voda štrkoviska2007, 720 m from the water. Comparison: percentile 91 of all samples in Slovakia.

    • BariumBaelevated (top 10 %)
      highest 99.0 μg/lmedian 68.5 μg/l4 samples

      Highest value: potok Vesné2007, 500 m from the water. Comparison: percentile 91 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 2.00 μg/lmedian 0.500 μg/l4 samples75 % below the limit of quantification

      Highest value: voda štrkoviska2007, 720 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l4 samples100 % below the limit of quantification

      Highest value: potok Hradlová2007, 420 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l4 samples100 % below the limit of quantification

      Highest value: potok Hradlová2007, 420 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l4 samples100 % below the limit of quantification

      Highest value: potok Hradlová2007, 420 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l4 samples100 % below the limit of quantification

      Highest value: potok Hradlová, 420 m from the water. Comparison: percentile 26 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l4 samples100 % below the limit of quantification

      Highest value: potok Hradlová2007, 420 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 7.02 mg/lmedian 5.19 mg/l4 samples

      Highest value: potok Vesné2007, 500 m from the water. Comparison: percentile 26 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)13 samples, at most 815 grains
    • Pyrite (FeS₂)8 samples, at most 55 grains
    • Anatas (TiO₂)4 samples, at most 55 grains
    • Limonite (FeO(OH)·nH₂O)4 samples, at most 55 grains
    • Magnetite (Fe₃O₄)4 samples, at most 1815 grains
    • Rutil (TiO₂)4 samples, at most 815 grains
    • Hematite (Fe₂O₃)3 samples, at most 55 grains
    • Ilmenit (FeTiO₃)3 samples, at most 815 grains
    • Monazit ((Ce,La,Nd)PO₄)2 samples, at most 5 grains
    • Cinabarit (HgS)1 sample, at most 5 grains

    Rock-forming and accessory minerals

    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)13 samples, at most 1815 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)4 samples, at most 4115 grains
    • Zirconium (ZrSiO₄)4 samples, at most 315 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))3 samples, at most 55 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)3 samples, at most 55 grains
    • Tourmalines (complex borosilicate)3 samples, at most 315 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-HCO36×
    • Ca-Mg-HCO32×
    • Ca-SO4-HCO31×

    Water quality class according to the hydrogeochemical map

    • class A8×
    • class B1×

    Metals in groundwater

    • LeadPbhigh (top 5 %)
      highest 3.00 μg/lmedian 1.00 μg/l17 samples47 % below the limit of quantification

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • SeleniumSeelevated (top 10 %)
      highest 2.00 μg/lmedian 0.500 μg/l17 samples82 % below the limit of quantification

      Highest value: studňa1993, 1.9 km from the water. Comparison: percentile 92 of all samples in Slovakia.

    • ChromiumCrelevated (top 10 %)
      highest 2.10 μg/lmedian 0.250 μg/l17 samples82 % below the limit of quantification

      Highest value: prameň1993, 300 m from the water. Comparison: percentile 90 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 3.60 μg/lmedian 1.30 μg/l17 samples

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 88 of all samples in Slovakia.

    • ZincZnslightly elevated
      highest 375 μg/lmedian 8.00 μg/l17 samples6 % below the limit of quantification

      Highest value: studňa1993, 1.9 km from the water. Comparison: percentile 86 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 22.0 μg/lmedian 12.0 μg/l17 samples

      Highest value: prameň1993, 830 m from the water. Comparison: percentile 80 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l13 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l17 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l17 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    • AntimonySbbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l17 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 40 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l17 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 38 of all samples in Slovakia.

    • AluminiumAlbelow half of Slovakia
      highest 0.00500 mg/lmedian 0.00500 mg/l17 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 30 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    source728,3 Bq/l12.8 Bq/l
    developed spring19,32 Bq/l9.32 Bq/l
    stream, river12,35 Bq/l2.35 Bq/l
    well19,60 Bq/l9.60 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.

    Types of mining objects

    • tailings pond1×

    Nearest old mine workings

    NameTypeMinedEndedFrom the water
    Odkalisko Orlovtailings pondgravelly sands330 m

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    Plaveč – Orlovgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená410 m
    Plaveč – Orlovgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená410 m
    Plaveč I – Orlov IIgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená570 m
    Plaveč I – Orlov IIgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená570 m

    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.

    296 boreholes in the 3 km zone, of which 30 hydrogeological and 266 other; with an archive report number 296.

    Borehole depths

    • up to 10 m253×
    • 10–30 m40×
    • 30–100 m3×
    • 100–300 m0×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    S-1engineering-geological5.2 m2758610 m
    V-7deposit6.3 m288220 m
    DB-27engineering-geological1.5 m8158940 m
    S-3engineering-geological3.5 m2758640 m
    V-3engineering-geological2.5 m8158940 m
    V-5deposit8.5 m288240 m
    V-6engineering-geological7.0 m2657040 m
    V-5engineering-geological5.1 m4388140 m
    V-6engineering-geological5.4 m4388140 m
    V-1bengineering-geological2.5 m2657040 m
    Orlovnarrow-diameter borehole with ordinary drinking and process water11.5 m71849 102Ba51.pdf50 m
    S-6engineering-geological5.3 m2553350 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
    Plavnica – Pl-253 °C4.0 l/s3500 mNa-Clunused5.7 km
    Plavnica – Pl-165 °C5.0 l/s3500 mNa-Clunused7.8 km
    Šariš – Š-128 °C0.2 l/s5000 mNa-Clunused9.7 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 5193.0 km
    category b2mineral water15-225-1519.2 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
    Ďurková25 m²1986–10 m
    Ďurková40 m²1987–80 m
    Orlov–1986–300 m
    Ďurková30 m²1989–580 m
    Orlov – Ľubotín–1986–590 m
    Šarišské Jastrabie40 m²1987–820 m
    Vislanka30 m²1989–1.2 km
    Vislanka25 m²1989–1.6 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

    • Landslides64×
    • Slope flows1×

    Degree of activity

    • Potenciálny44×
    • Stabilizovaný16×
    • Aktívny4×
    • With potential and active forms1×

    Current state

    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S14×
    • SD taken from archival materials, ktorá bola konfrontova14×
    • SD prebraná z archívnych materiálov (existuje inž. geologick8×
    • Processed only in the scope of registration on a scale of 1:25,0003×

    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. Orlov1 fishing district · 3.7 km27Ľubotínka č. 127

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