Fishing conditions score, the best window of the day and fishing districts from the best conditions Low activity · average of one fishing district 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. 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 Move the map with two fingers. In full-screen mode one finger is enough. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. For each fishing district you can see what it is made of, how well it is supported by data and where the data comes from. 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. Source: Open Topo Data (eudem25m), 4 Nov 2026. Gradient and fall are approximate and include only the sections of fishing districts. Loading the 3D terrain model… 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. 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 quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby 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. 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. 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. 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. 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. 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. 0objects within 3 km No old mine working is recorded within 3 km of the water. 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. 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). 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. 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. 2sites within 3 km 2 landfills No environmental burden is registered within 3 km; landfills are only recorded. 9records within 5 km 9 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 11areas within 3 km Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed. 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. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia The map covers 0 of 2 points on the water line. 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. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia 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. 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. 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. 246mg/l mineralisation Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds. Water type by dominant ions: Ca–Mg–HCO₃ Shares are in equivalents, the usual way of comparing the composition of waters. 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) 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. 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) 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. 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. 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. 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) marker on the bar: share among all sample points on streams in Slovakia 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. -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. -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. 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. 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. marker on the bar: share among all sample points on streams in Slovakia 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. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off. 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. 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. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 37 of all samples in Slovakia. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 34 of all samples in Slovakia. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 32 of all samples in Slovakia. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 26 of all samples in Slovakia. Highest value: Lomnický potok, 460 m from the water. Comparison: percentile 26 of all samples in Slovakia. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 22 of all samples in Slovakia. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 22 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Lomnický potok2007, 460 m from the water. Comparison: percentile 33 of all samples in Slovakia. 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. 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. Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: prameň1993, 1.1 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: prameň1993, 1.1 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 85 of all samples in Slovakia. Highest value: prameň1993, 2.1 km from the water. Comparison: percentile 85 of all samples in Slovakia. Highest value: prameň1993, 2.3 km from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: prameň1993, 2.3 km from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: prameň1993, 1.5 km from the water. Comparison: percentile 72 of all samples in Slovakia. Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: prameň1993, 2.1 km from the water. Comparison: percentile 41 of all samples in Slovakia. Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 38 of all samples in Slovakia. 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. 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. 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. Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. Who manages the fishing districts and where they are Bodrog basin and Hornád
By the water now
Today on the Lomnický potok watercourse
Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the watercourse
Elevation profile of the watercourse
Terrain in 3D
Historical images



Water pollution on the Lomnický potok watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the Lomnický potok stream
Water according to the atlas
Elements in river sediment
Heat underfoot
Natural gamma radiation
Old mine workings
Gold in river sediment
Trace elements in the stream water
Boreholes and groundwater analyses
Geothermal energy
Environmental burdens and landfills
Deposits and ore occurrences
Landslides and slope deformations
Geological structure beneath the water
Quaternary cover
Tectonic division
Neotectonic units
Direction of neotectonic movements
Regional geological division
Regional geological division (subunits)
Engineering-geological districts
Engineering-geological formations
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Aquifer rocks (hydrogeological map 1:200,000)
Aquifer type
Type of permeability (basic hydrogeological map 1:50,000)
Hydrogeological function
Main hydrogeological region
Geothermal groundwater bodies
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
0.0915 mg/lpercentile 37148 mg/lpercentile 3142.0 mg/lpercentile 299.24 mg/lpercentile 2926.1 mg/lpercentile 283.36 mg/lpercentile 151.18 mg/lpercentile 142.18 mg/lpercentile 11Nutrients and organic pollution
0.0455 mg/lpercentile 232.08 mg/lpercentile 223.27 mg/lpercentile 190.0210 mg/lpercentile 10Metals
107 μg/lpercentile 630.120 mg/lpercentile 567.32 μg/lpercentile 5311.3 μg/lpercentile 24Elements in river sediments
Potentially toxic and trace elements
107 mg/kgpercentile 850.579 mg/kgpercentile 7829.7 mg/kgpercentile 700.123 mg/kgpercentile 580.220 mg/kgpercentile 5769.9 mg/kgpercentile 540.217 mg/kgpercentile 500.518 mg/kgpercentile 385.72 mg/kgpercentile 372.29 mg/kgpercentile 340.168 mg/kgpercentile 2912.3 mg/kgpercentile 287.05 mg/kgpercentile 2869.6 mg/kgpercentile 1814.3 mg/kgpercentile 9Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1.12 %percentile 821.70 %percentile 774,932 mg/kgpercentile 675.93 %percentile 60884 mg/kgpercentile 542.70 %percentile 510.856 %percentile 47647 mg/kgpercentile 231.07 %percentile 16Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
37.6 mg/kgpercentile 832.01 mg/kgpercentile 8372.4 mg/kgpercentile 8099.8 mg/kgpercentile 7631.8 mg/kgpercentile 7059.6 mg/kgpercentile 52440 mg/kgpercentile 5113.8 mg/kgpercentile 48393 mg/kgpercentile 46109 mg/kgpercentile 23Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.36 %percentile 666.58 ppm22th percentile2.09 ppm10th percentile2,065 Bq/m²percentile 71Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Rock temperature with depth
Geothermal groundwater bodies beneath the water line
Relief, climate and soils
Geomorphological units
Geomorphological regions
Climatic-geographical types
Susceptibility of soils to acidification
Soil contamination (map 1:500,000)
Lithogeochemical types
Map of the corridor
Trace elements in surface waters
Major ions, mineralisation and pH
Gold and ore minerals in river sediments
Rock-forming and accessory minerals
Groundwater: chemistry, water types and radioactivity
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median developed spring 1 3,60 Bq/l 3.60 Bq/l source 6 23,9 Bq/l 9.86 Bq/l well 1 1,50 Bq/l 1.50 Bq/l Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Lomnička narrow-diameter borehole with ordinary drinking and process water 100.0 m 87964 102Ac8.pdf50 m DV-4 engineering-geological 3.1 m 87125580 m DV-6 engineering-geological 4.0 m 87125620 m DV-5 engineering-geological 4.0 m 87125710 m Lomnička narrow-diameter borehole with ordinary drinking and process water 17.0 m 21970 102Ac4.pdf870 m DV-7 engineering-geological 4.8 m 871251.5 km DV-2 engineering-geological 4.3 m 871251.5 km DV-3 engineering-geological 4.3 m 871251.7 km Lomnička narrow-diameter borehole with ordinary drinking and process water 13.2 m 13158 102Aa9.pdf1.8 km Lomnička narrow-diameter borehole with ordinary drinking and process water 12.0 m 10071 102Aa10.pdf1.8 km DV-1 engineering-geological 4.2 m 871252.1 km Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Vyšné Ružbachy – VR-2 20 °C 0.6 l/s 220 m Ca-Mg-HCO3 unused 7.3 km Vyšné Ružbachy – VRŠ-1 21 °C 17.0 l/s 1200 m Ca-Mg-HCO3-SO4 unused 7.5 km Vyšné Ružbachy – borehole 20 °C 75.0 l/s 200 m Ca-HCO3 in use 7.6 km Vyšné Ružbachy – VR-5 24 °C 2.5 l/s 330 m Ca-Mg-HCO3-SO4 unused 8.2 km Sources of geothermal and mineral waters
Source Type Water temperature (°C) Yield (l/s) Count Nearest from water category a1 mineral water < 15 < 5 17 4.9 km category b3 mineral water 15-22 16-30 2 5.4 km category b1 mineral water 15-22 < 5 4 5.6 km category b4 mineral water 15-22 31-50 1 6.2 km category c2 mineral water 23-38 5-15 1 6.6 km category c1 mineral water 23-38 < 5 2 6.7 km category Vyšné Ružbachy thermal baths – – 1 6.9 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Pri kasárňach – Lomnička – 1990 – 1.8 km Križava – Lomnička – 1986 – 2.8 km Landslides and slope deformations
Types of deformations
Degree of activity
Current state
How to read these data
Organizations and location
Organizations on the watercoursewho manages the fishing districts and what the conditions are there today
More watercourses nearby
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Salmonid (trout)Ľubický potok
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Salmonid (trout)Toporecký potok
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26from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l1 sample100 % below the limit of quantification
AntimonySbbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification
LithiumLibelow half of Slovakia
highest 5.00 μg/lmedian 5.00 μg/l1 sample100 % below the limit of quantification
ChromiumCrbelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification
BariumBabelow half of Slovakia
highest 22.0 μg/lmedian 22.0 μg/l1 sample
CadmiumCdbelow half of Slovakia
highest 0.150 μg/lmedian 0.150 μg/l1 sample100 % below the limit of quantification
CopperCubelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification
Silicon dioxideSiO2below half of Slovakia
highest 8.06 mg/lmedian 8.06 mg/l1 sample
MercuryHghigh (top 5 %)
highest 0.200 μg/lmedian 0.100 μg/l14 samples93 % below the limit of quantification
CopperCuelevated (top 10 %)
highest 5.60 μg/lmedian 1.05 μg/l14 samples
AntimonySbelevated (top 10 %)
highest 0.400 μg/lmedian 0.100 μg/l14 samples86 % below the limit of quantification
AluminiumAlslightly elevated
highest 0.0300 mg/lmedian 0.00500 mg/l14 samples93 % below the limit of quantification
SeleniumSeslightly elevated
highest 1.20 μg/lmedian 0.500 μg/l14 samples86 % below the limit of quantification
ChromiumCrslightly elevated
highest 0.800 μg/lmedian 0.250 μg/l14 samples93 % below the limit of quantification
LeadPbslightly elevated
highest 1.00 μg/lmedian 0.500 μg/l14 samples64 % below the limit of quantification
LithiumLitypical value
highest 15.0 μg/lmedian 5.00 μg/l14 samples
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l12 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l14 samples100 % below the limit of quantification
ZincZnbelow half of Slovakia
highest 15.0 μg/lmedian 10.0 μg/l14 samples
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l14 samples100 % below the limit of quantification