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 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. 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. Brisk watercourse A foothill river with a gravel bottom and a fast current. Grayling and trout already thrive here. 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. 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. 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. 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. 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. 1object within 3 km Nearest: Odkalisko Orlov (tailings pond), 330 m from the water. 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. 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). 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. 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. 19sites within 3 km 19 landfills No environmental burden is registered within 3 km; landfills are only recorded. 5records within 5 km 4 deposits, 1 ore occurrence Geofond registers, the metallogenetic map and the mineral resources map. 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. 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. 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. 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 1 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 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 8.14typical 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. 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. 379mg/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–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. 47nGy/h in air 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. -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. -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. 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. 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 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: voda štrkoviska2007, 720 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: voda štrkoviska2007, 720 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: potok Vesné2007, 500 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: voda štrkoviska2007, 720 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: potok Hradlová2007, 420 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: potok Hradlová2007, 420 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: potok Hradlová2007, 420 m from the water. Comparison: percentile 34 of all samples in Slovakia. Highest value: potok Hradlová, 420 m from the water. Comparison: percentile 26 of all samples in Slovakia. Highest value: potok Hradlová2007, 420 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: potok Vesné2007, 500 m from the water. Comparison: percentile 26 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, 2.8 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1993, 1.9 km from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: prameň1993, 300 m from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 88 of all samples in Slovakia. Highest value: studňa1993, 1.9 km from the water. Comparison: percentile 86 of all samples in Slovakia. Highest value: prameň1993, 830 m from the water. Comparison: percentile 80 of all samples in Slovakia. Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 40 of all samples in Slovakia. Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 38 of all samples in Slovakia. Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 30 of all samples in Slovakia. 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. 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. 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 Ľubotínka 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 Ľubotínka watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the Ľubotínka stream
Rock under the water
Water according to the atlas
Elements in river sediment
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
Geological age of the rocks
Most common rock units
System Age Unit Points Quaternary Holocene fluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains 1× Quaternary cover
Regional geological division
Regional geological division (subunits)
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Main hydrogeological region
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
3.66 mg/lpercentile 600.129 mg/lpercentile 5766.8 mg/lpercentile 55224 mg/lpercentile 547.37 mg/lpercentile 4513.5 mg/lpercentile 4434.9 mg/lpercentile 427.05 mg/lpercentile 40Nutrients and organic pollution
0.0422 mg/lpercentile 211.94 mg/lpercentile 182.60 mg/lpercentile 130.0207 mg/lpercentile 10Metals
105 μg/lpercentile 800.140 mg/lpercentile 6377.3 μg/lpercentile 541.58 μg/lpercentile 9Elements in river sediments
Potentially toxic and trace elements
0.877 mg/kgpercentile 92131 mg/kgpercentile 9132.3 mg/kgpercentile 760.126 mg/kgpercentile 590.227 mg/kgpercentile 540.238 mg/kgpercentile 480.170 mg/kgpercentile 4678.9 mg/kgpercentile 3018.8 mg/kgpercentile 270.415 mg/kgpercentile 2658.0 mg/kgpercentile 246.66 mg/kgpercentile 224.66 mg/kgpercentile 208.65 mg/kgpercentile 61.53 mg/kgpercentile 6Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
0.958 %percentile 664,760 mg/kgpercentile 611.58 %percentile 602.11 %percentile 515.55 %percentile 470.840 %percentile 452.59 %percentile 44776 mg/kgpercentile 42723 mg/kgpercentile 33Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
35.5 mg/kgpercentile 7770.7 mg/kgpercentile 7628.7 mg/kgpercentile 5690.2 mg/kgpercentile 55431 mg/kgpercentile 48394 mg/kgpercentile 4756.7 mg/kgpercentile 411.21 mg/kgpercentile 38118 mg/kgpercentile 3311.4 mg/kgpercentile 29Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.38 %percentile 696.96 ppm33th percentile2.01 ppm8th percentile1,157 Bq/m²percentile 28Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Relief, climate and soils
Geomorphological units
Geomorphological regions
Susceptibility of soils to acidification
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
Chemical water types nearby
Water quality class according to the hydrogeochemical map
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median source 7 28,3 Bq/l 12.8 Bq/l developed spring 1 9,32 Bq/l 9.32 Bq/l stream, river 1 2,35 Bq/l 2.35 Bq/l well 1 9,60 Bq/l 9.60 Bq/l Mine workings, deposits and ore occurrences
Types of mining objects
Nearest old mine workings
Name Type Mined Ended From the water Odkalisko Orlov tailings pond gravelly sands 330 m Deposits and mining areas
Deposit Mineral Status and organisation From the water Plaveč – Orlov gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 410 m Plaveč – Orlov gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 410 m Plaveč I – Orlov II gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 570 m Plaveč I – Orlov II gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 570 m Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water S-1 engineering-geological 5.2 m 2758610 m V-7 deposit 6.3 m 288220 m DB-27 engineering-geological 1.5 m 8158940 m S-3 engineering-geological 3.5 m 2758640 m V-3 engineering-geological 2.5 m 8158940 m V-5 deposit 8.5 m 288240 m V-6 engineering-geological 7.0 m 2657040 m V-5 engineering-geological 5.1 m 4388140 m V-6 engineering-geological 5.4 m 4388140 m V-1b engineering-geological 2.5 m 2657040 m Orlov narrow-diameter borehole with ordinary drinking and process water 11.5 m 71849 102Ba51.pdf50 m S-6 engineering-geological 5.3 m 2553350 m Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Plavnica – Pl-2 53 °C 4.0 l/s 3500 m Na-Cl unused 5.7 km Plavnica – Pl-1 65 °C 5.0 l/s 3500 m Na-Cl unused 7.8 km Šariš – Š-1 28 °C 0.2 l/s 5000 m Na-Cl unused 9.7 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 19 3.0 km category b2 mineral water 15-22 5-15 1 9.2 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Ďurková 25 m² 1986 – 10 m Ďurková 40 m² 1987 – 80 m Orlov – 1986 – 300 m Ďurková 30 m² 1989 – 580 m Orlov – Ľubotín – 1986 – 590 m Šarišské Jastrabie 40 m² 1987 – 820 m Vislanka 30 m² 1989 – 1.2 km Vislanka 25 m² 1989 – 1.6 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
27from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
ChromiumCrextreme (top 1 %)
highest 15.0 μg/lmedian 1.00 μg/l4 samples75 % below the limit of quantification
AntimonySbelevated (top 10 %)
highest 2.00 μg/lmedian 0.500 μg/l4 samples75 % below the limit of quantification
BariumBaelevated (top 10 %)
highest 99.0 μg/lmedian 68.5 μg/l4 samples
ArsenicAsslightly elevated
highest 2.00 μg/lmedian 0.500 μg/l4 samples75 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l4 samples100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l4 samples100 % below the limit of quantification
LithiumLibelow half of Slovakia
highest 5.00 μg/lmedian 5.00 μg/l4 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.150 μg/lmedian 0.150 μg/l4 samples100 % below the limit of quantification
CopperCubelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l4 samples100 % below the limit of quantification
Silicon dioxideSiO2below half of Slovakia
highest 7.02 mg/lmedian 5.19 mg/l4 samples
LeadPbhigh (top 5 %)
highest 3.00 μg/lmedian 1.00 μg/l17 samples47 % below the limit of quantification
SeleniumSeelevated (top 10 %)
highest 2.00 μg/lmedian 0.500 μg/l17 samples82 % below the limit of quantification
ChromiumCrelevated (top 10 %)
highest 2.10 μg/lmedian 0.250 μg/l17 samples82 % below the limit of quantification
CopperCuslightly elevated
highest 3.60 μg/lmedian 1.30 μg/l17 samples
ZincZnslightly elevated
highest 375 μg/lmedian 8.00 μg/l17 samples6 % below the limit of quantification
LithiumLislightly elevated
highest 22.0 μg/lmedian 12.0 μg/l17 samples
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l13 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l17 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l17 samples100 % below the limit of quantification
AntimonySbbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l17 samples100 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l17 samples100 % below the limit of quantification
AluminiumAlbelow half of Slovakia
highest 0.00500 mg/lmedian 0.00500 mg/l17 samples100 % below the limit of quantification

