Watercourse

Lomnický potok

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
3.8km
region
Prešov Region
Aerial image of watercourse Lomnický 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 Lomnický 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

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

Lomnický potok, window score 35.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 05:04.

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.

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

    6007008009001,0000 km1 km2 km3 km
    Elevation profile of the watercourse: from 884 to 674 m a.s.l. over 3.8 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
    884 m a.s.l.
    Lowest point
    644 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.
    239 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.
    63 ‰
    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.
    1.08

    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 Lomnický potok from 2019
    2019imaged 24 Aug 2019
    Aerial image of watercourse Lomnický potok from 2022
    2022imaged 26 Aug 2022
    Aerial image of watercourse Lomnický 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 Lomnický potok 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 Lomnický 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 (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.

    510

    Water according to the atlas

    pH 8.1modelled estimate

    water type Ca–Mg–HCO₃

    Mineralisation 246 mg/l, soft water (8.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    0 from 15elements in the top 10 %

    highest: Chromium 107 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 85. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km35 °C65 °C

    Heat underfoot

    35°C at 1,000 m depth

    heat flow 65 mW/m²

    At a depth of 2,000 m about 65 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    46nGy/h dose rate

    percentile 20 in Slovakia

    Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ.

    Old mine workings

    0objects within 3 km

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

    Gold in river sediment

    0samples with gold

    9 ore minerals in the sediment

    No gold was found in river sediment samples within 1 km of the water. The samples do not cover every stream, so this does not mean there is no gold here.

    Trace elements in the stream water

    0 from 9indicators in the top 5 %

    highest: Selenium 0.500 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 46 (Lomnický potok).

    Boreholes and groundwater analyses

    11boreholes within 3 km

    182 water analyses nearby

    Of these, 11 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    24°C at the wellhead

    4 geothermal boreholes within 10 km

    Warmest: Vyšné Ružbachy – VR-5, yield 2.5 l/s, 8.2 km from the water.

    Environmental burdens and landfills

    2sites within 3 km

    2 landfills

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

    Deposits and ore occurrences

    9records within 5 km

    9 ore occurrences

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

    Landslides and slope deformations

    11areas within 3 km

    Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed.

    Geological structure beneath the water

    Which rock lies beneath the water line (Geological Map of Slovakia 1:50,000), how old it is, how thick the Quaternary cover is and in which tectonic unit the water flows. The bedrock decides the hardness of the water, the bottom, the turbidity after rain and the abundance of springs.

    Quaternary cover

    • deluvial sediments100%SR 16 %

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

    Tectonic division

    • NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

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

    Neotectonic units

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

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

    Direction of neotectonic movements

    • medium uplift100%SR 32 %

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

    Regional geological division

    • Inner Carpathian Paleogene100%SR 11 %

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

    Regional geological division (subunits)

    • Spiš–Šariš Paleogene100%SR 5.8 %

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

    Engineering-geological districts

    • region of sandstone-conglomerate rocks100%SR 3.4 %

    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 0 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.

    Aquifer rocks (hydrogeological map 1:200,000)

    • Sandstones100%SR 15 %

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

    Aquifer type

    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Sandstones)100%SR 15 %

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

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

    • intergranular50%SR 86 %
    • fissure50%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 Levočské vrchy100%SR 1.2 %

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

    Geothermal groundwater bodies

    • Levoča Basin – NE part100%SR 5.0 %

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

    Surface water chemistry according to the atlas

    Modelled composition of the water in the area the fishing district line runs through. The rasters of the Geochemical Atlas of Slovakia (surface waters) are an interpolation of measurements in sampled streams, so they show the typical background of the area, not a measurement in a particular stream.

    510

    Water acidity

    pH 8.09typical range

    Most rivers and streams in Slovakia have a pH of 6.5 to 8.5. More acidic water is found in streams on acidic rocks (granites, quartzites), more alkaline water near limestones.

    Water hardness

    8.0°dH, soft

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

    Dissolved substances

    246mg/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

    • FluoridesF0.0915 mg/lpercentile 37
    • BicarbonatesHCO3148 mg/lpercentile 31
    • CalciumCa42.0 mg/lpercentile 29
    • MagnesiumMg9.24 mg/lpercentile 29
    • SulphatesSO426.1 mg/lpercentile 28
    • SodiumNa3.36 mg/lpercentile 15
    • PotassiumK1.18 mg/lpercentile 14
    • ChloridesCl2.18 mg/lpercentile 11

    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

    • AmmoniumNH40.0455 mg/lpercentile 23
    • Chemical oxygen demandChSK2.08 mg/lpercentile 22
    • NitratesNO33.27 mg/lpercentile 19
    • PhosphatesPO40.0210 mg/lpercentile 10

    Metals

    • AluminiumAl107 μg/lpercentile 63
    • IronFe0.120 mg/lpercentile 56
    • ZincZn7.32 μg/lpercentile 53
    • ManganeseMn11.3 μg/lpercentile 24

    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

    • ChromiumCr107 mg/kgpercentile 85
    • MolybdenumMo0.579 mg/kgpercentile 78
    • NickelNi29.7 mg/kgpercentile 70
    • MercuryHg0.123 mg/kgpercentile 58
    • CadmiumCd0.220 mg/kgpercentile 57
    • VanadiumV69.9 mg/kgpercentile 54
    • BismuthBi0.217 mg/kgpercentile 50
    • AntimonySb0.518 mg/kgpercentile 38
    • ArsenicAs5.72 mg/kgpercentile 37
    • TinSn2.29 mg/kgpercentile 34
    • SeleniumSe0.168 mg/kgpercentile 29
    • LeadPb12.3 mg/kgpercentile 28
    • CobaltCo7.05 mg/kgpercentile 28
    • ZincZn69.6 mg/kgpercentile 18
    • CopperCu14.3 mg/kgpercentile 9

    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)
    • SodiumNa1.12 %percentile 82
    • PotassiumK1.70 %percentile 77
    • TitaniumTi4,932 mg/kgpercentile 67
    • AluminiumAl5.93 %percentile 60
    • ManganeseMn884 mg/kgpercentile 54
    • IronFe2.70 %percentile 51
    • MagnesiumMg0.856 %percentile 47
    • PhosphorusP647 mg/kgpercentile 23
    • CalciumCa1.07 %percentile 16
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • LithiumLi37.6 mg/kgpercentile 83
    • BerylliumBe2.01 mg/kgpercentile 83
    • BoronB72.4 mg/kgpercentile 80
    • RubidiumRb99.8 mg/kgpercentile 76
    • YttriumY31.8 mg/kgpercentile 70
    • CeriumCe59.6 mg/kgpercentile 52
    • BariumBa440 mg/kgpercentile 51
    • GalliumGa13.8 mg/kgpercentile 48
    • ZirconiumZr393 mg/kgpercentile 46
    • StrontiumSr109 mg/kgpercentile 23

    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

    46nGy/h in air

    range 45 to 47 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)K1.36 %percentile 66
    • Equivalent thorium (eTh)eTh6.58 ppm22th percentile
    • Equivalent uranium (eU)eU2.09 ppm10th percentile

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

    • Areal activity of 137CsCS1372,065 Bq/m²percentile 71

    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

    -23nT

    range -23 to -23 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

    -47mGal

    residual −2.4 mGal

    Negative values lie over thick sediments and under mountains (light crust), positive over dense rocks and thinner crust. It shows the structure of the Earth's crust, not the water.

    Geothermal potential

    The Atlas of Geothermal Energy of Slovakia records rock temperature and heat flow from the Earth's interior. It is the potential of the area, not the actual warmth of the water in the stream. Specific geothermal boreholes and springs near this water are in the geothermal energy section below.

    1 km2 km35 °C65 °C

    Rock temperature with depth

    35 / 65 °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 65 mW/m².

    Geothermal groundwater bodies beneath the water line

    • Levoča Basin – NE part100%SR 5.0 %

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

    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)539–1 132m a.s.l.
    • Average elevation of the units788m a.s.l.
    • Average slope14.9°
    • Average January temperature-5.8°C
    • Average July temperature14.8°C
    • Annual precipitation950mm

    Geomorphological units

    • Levoča Hills100%SR 1.1 %

    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

    Climatic-geographical types

    • mountain climate100%SR 33 %

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

    Susceptibility of soils to acidification

    • soils moderately susceptible to 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

    • Inner Carpathian Paleogene100%SR 11 %

    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.

    Pri kasárňach – Lomnička – cannot be estimated (1.8 km from the water)Križava – Lomnička – cannot be estimated (2.8 km from the water)Vyšné Ružbachy – VR-2 – spa (7.3 km from the water)Vyšné Ružbachy – VRŠ-1 – spa (7.5 km from the water)Vyšné Ružbachy – vrt – spa (7.6 km from the water)Vyšné Ružbachy – VR-5 – spa (8.2 km from the water)a1 (4.9 km from the water)b3 (5.4 km from the water)b1 (5.6 km from the water)a1 (5.7 km from the water)a1 (5.7 km from the water)a1 (5.8 km from the water)a1 (5.8 km from the water)a1 (5.8 km from the water)a1 (6.1 km from the water)a1 (6.2 km from the water)b4 (6.2 km from the water)b3 (6.4 km from the water)c2 (6.6 km from the water)b1 (6.6 km from the water)c1 (6.7 km from the water)b1 (6.7 km from the water)c1 (6.7 km from the water)a1 (6.8 km from the water)b1 (6.9 km from the water)a1 (7.5 km from the water)a1 (7.7 km from the water)a1 (7.8 km from the water)a1 (7.9 km from the water)a1 (8.6 km from the water)a1 (9.0 km from the water)a1 (9.3 km from the water)a1 (9.5 km from the water)Vyšné Ružbachy (6.9 km from the water)Ihľany – building stone – sandstone (3.2 km from the water)Jurské – building stone – sandstone (3.2 km from the water)Jurské – building stone – sandstone (3.3 km from the water)Jurské – building stone – sandstone (3.3 km from the water)Holumnica – building stone – sandstone (3.5 km from the water)Jurské – building stone – sandstone (3.5 km from the water)Ihľany – building stone – sandstone (3.5 km from the water)Jurské – building stone – sandstone (3.6 km from the water)Holumnica – crude oil, natural gas (4.5 km from the water)– Landslides (1.1 km from the water)– Landslides (1.4 km from the water)LOMNICKA – Landslides (1.6 km from the water)– Landslides (1.7 km from the water)– Landslides (1.7 km from the water)– Landslides (1.8 km from the water)HOLUMNICA – Landslides (2.4 km from the water)– Landslides (2.5 km from the water)JURSKE – Landslides (2.6 km from the water)STOTINCE – Landslides (2.7 km from the water)HOLUMNICA – Landslides (3.0 km from the water)Lomnička – úzkoprofilový vrt s obyčajnou pitnou a ú (50 m from the water)Lomnička – úzkoprofilový vrt s obyčajnou pitnou a ú (870 m from the water)Lomnička – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Lomnička – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (50 m from the water)prameň – Groundwater springs (1.3 km from the water)prameň – Groundwater springs (1.5 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.8 km from the water)prameň – Groundwater springs (2.1 km from the water)prameň – Groundwater springs (2.2 km from the water)prameň – Groundwater springs (2.5 km from the water)prameň – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (2.7 km from the water)vodárensky využívaný prameň – Groundwater springs (2.8 km from the water)prameň – Groundwater springs (2.9 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.

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

      Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 46 of all samples in Slovakia.

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

      Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 43 of all samples in Slovakia.

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

      Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 37 of all samples in Slovakia.

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

      Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 34 of all samples in Slovakia.

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

      Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 32 of all samples in Slovakia.

    • BariumBabelow half of Slovakia
      highest 22.0 μg/lmedian 22.0 μg/l1 sample

      Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 26 of all samples in Slovakia.

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

      Highest value: Lomnický potok, 460 m from the water. Comparison: percentile 26 of all samples in Slovakia.

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

      Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 22 of all samples in Slovakia.

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

      Highest value: Lomnický potok2007, 460 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 8.06 mg/lmedian 8.06 mg/l1 sample

      Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 33 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)8 samples, at most 155 grains
    • Limonite (FeO(OH)·nH₂O)6 samples, at most 55 grains
    • Magnetite (Fe₃O₄)6 samples, at most 55 grains
    • Rutil (TiO₂)6 samples, at most 815 grains
    • Anatas (TiO₂)5 samples, at most 5 grains
    • Hematite (Fe₂O₃)4 samples, at most 55 grains
    • Ilmenit (FeTiO₃)3 samples, at most 815 grains
    • Monazit ((Ce,La,Nd)PO₄)2 samples, at most 5 grains
    • Pyrite (FeS₂)2 samples, at most 5 grains

    Rock-forming and accessory minerals

    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)9 samples, at most 1815 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)6 samples, at most 4115 grains
    • Zirconium (ZrSiO₄)6 samples, at most 815 grains
    • Tourmalines (complex borosilicate)4 samples, at most 55 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)2 samples, at most 55 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))1 sample, at most 5 grains

    Groundwater: chemistry, water types and radioactivity

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

    Metals in groundwater

    • MercuryHghigh (top 5 %)
      highest 0.200 μg/lmedian 0.100 μg/l14 samples93 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • CopperCuelevated (top 10 %)
      highest 5.60 μg/lmedian 1.05 μg/l14 samples

      Highest value: prameň1993, 1.1 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • AntimonySbelevated (top 10 %)
      highest 0.400 μg/lmedian 0.100 μg/l14 samples86 % below the limit of quantification

      Highest value: prameň1993, 1.1 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • AluminiumAlslightly elevated
      highest 0.0300 mg/lmedian 0.00500 mg/l14 samples93 % below the limit of quantification

      Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 85 of all samples in Slovakia.

    • SeleniumSeslightly elevated
      highest 1.20 μg/lmedian 0.500 μg/l14 samples86 % below the limit of quantification

      Highest value: prameň1993, 2.1 km from the water. Comparison: percentile 85 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 0.800 μg/lmedian 0.250 μg/l14 samples93 % below the limit of quantification

      Highest value: prameň1993, 2.3 km from the water. Comparison: percentile 75 of all samples in Slovakia.

    • LeadPbslightly elevated
      highest 1.00 μg/lmedian 0.500 μg/l14 samples64 % below the limit of quantification

      Highest value: prameň1993, 2.3 km from the water. Comparison: percentile 75 of all samples in Slovakia.

    • LithiumLitypical value
      highest 15.0 μg/lmedian 5.00 μg/l14 samples

      Highest value: prameň1993, 1.5 km from the water. Comparison: percentile 72 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l12 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l14 samples100 % below the limit of quantification

      Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • ZincZnbelow half of Slovakia
      highest 15.0 μg/lmedian 10.0 μg/l14 samples

      Highest value: prameň1993, 2.1 km from the water. Comparison: percentile 41 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l14 samples100 % below the limit of quantification

      Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 38 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    developed spring13,60 Bq/l3.60 Bq/l
    source623,9 Bq/l9.86 Bq/l
    well11,50 Bq/l1.50 Bq/l

    Boreholes and Geofond archive reports

    Register of hydrogeological boreholes, other boreholes and geothermal boreholes. Each borehole has a report in the Geofond archive (geological profiles, pumping tests, chemical analyses of the water); the report number is in the table.

    11 boreholes in the 3 km zone, of which 4 hydrogeological and 7 other; with an archive report number 11.

    Borehole depths

    • up to 10 m7×
    • 10–30 m3×
    • 30–100 m0×
    • 100–300 m1×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Lomničkanarrow-diameter borehole with ordinary drinking and process water100.0 m87964 102Ac8.pdf50 m
    DV-4engineering-geological3.1 m87125580 m
    DV-6engineering-geological4.0 m87125620 m
    DV-5engineering-geological4.0 m87125710 m
    Lomničkanarrow-diameter borehole with ordinary drinking and process water17.0 m21970 102Ac4.pdf870 m
    DV-7engineering-geological4.8 m871251.5 km
    DV-2engineering-geological4.3 m871251.5 km
    DV-3engineering-geological4.3 m871251.7 km
    Lomničkanarrow-diameter borehole with ordinary drinking and process water13.2 m13158 102Aa9.pdf1.8 km
    Lomničkanarrow-diameter borehole with ordinary drinking and process water12.0 m10071 102Aa10.pdf1.8 km
    DV-1engineering-geological4.2 m871252.1 km

    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
    Vyšné Ružbachy – VR-220 °C0.6 l/s220 mCa-Mg-HCO3unused7.3 km
    Vyšné Ružbachy – VRŠ-121 °C17.0 l/s1200 mCa-Mg-HCO3-SO4unused7.5 km
    Vyšné Ružbachy – borehole20 °C75.0 l/s200 mCa-HCO3in use7.6 km
    Vyšné Ružbachy – VR-524 °C2.5 l/s330 mCa-Mg-HCO3-SO4unused8.2 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 5174.9 km
    category b3mineral water15-2216-3025.4 km
    category b1mineral water15-22< 545.6 km
    category b4mineral water15-2231-5016.2 km
    category c2mineral water23-385-1516.6 km
    category c1mineral water23-38< 526.7 km
    category Vyšné Ružbachythermal baths––16.9 km

    Environmental burdens, landfills and anthropogenic sediments

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

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom the water
    Pri kasárňach – Lomnička–1990–1.8 km
    Križava – Lomnička–1986–2.8 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

    • Landslides11×

    Degree of activity

    • Potenciálny11×

    Current state

    • Processed only in the scope of registration on a scale of 1:25,0004×
    • SD taken from archival materials, ktorá bola konfrontova1×

    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. VO Javorina1 fishing district · 3.8 km26Lomnický potok26

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